ML19254D489
ML19254D489 | |
Person / Time | |
---|---|
Site: | 05000574 |
Issue date: | 07/11/1979 |
From: | Puno R PHILIPPINES |
To: | |
Shared Package | |
ML19254D482 | List: |
References | |
NUDOCS 7910260039 | |
Download: ML19254D489 (206) | |
Text
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Co.nicsion cu !!uclear Plants 11 July 1979 Page 1 3:30 - 4;00 p.m.
PISu!'PTI0li 0F EESSION At 3:30 p.m., the hearing was e:;uaed.
THE CHAIMAN. A few preliminary questions froa the Co:inission.
MR.CRONIN. Hay 1 interrupt you for a while, sir.
Tile CHAIMAN. You may.
la. CRONIN. Inaccuch as Westinghouse has presented all of the informations that we uanted to and 14r. Sitaans, Dr.FergandMr.WilgusallhavejobsintheUnitedStates, could,ue ask for the same consideration that we did with
!!.c. Call,14r. Scro and Mr. Arnold,that they be permitted toreturntotheirregularjobsandthatthepresentation of Ebasco, MFC and llayat, the physicist, to continue and if they can again be brought back after they have -
c::ught. up with.their day to day work.
THE CHAIRMAN. Nr. Cronin, the recepticn of these dissertalions of the Ebasco gentlemen is only to fill in this gap. The Westinghouse Panel is still the panel on the rostrua, so we are not suspending actually the 1~222 164 7910200 e
Commission on Nuclocr Plants 11 July 1979 3:30-4:00 p.m.
Page 2 Uestinghouse presentation and interpellat This is only whenever the continue in fact tomorrow.
Westinghouse panel is not under interpellatio e f going to use the rest of the af ternoon tol u We are not going to adjourn and So, we have m that ne can do whenever there is a suspension.
tomer ow they will be back for further The interpel We hope there is no misunderstanding about th Westinghouse panel is still under interpellat thie is merely to fill in the unused time for this afternoon, so that we can avoid any waste of tim We are now going to listen to the Ebasco paper.
Is it in the rollo? Will you please
,14ay ue have it.
come up and show us the page?
"We are taking up now the elaboration of l'PC to questions 5, 6, 7 by Ebasco fServices, d
!4ay we be in orme elaborating the tiPC position paper who will defend'this elaboration?
1222 165 .
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Ccamission on l!uclsar Plants 11 July 1979 '
Paga 3 3:30-4:00 P.!4.
FR. ITCH 0ll. I!r. Chairman, may we rer,uest that 14r.
Charles Healy, who is the Project f4anager of Ebasco for our nuclear power project be allowed to pre::eni the ex-perts that came from the United States.
Tile CHAIRf4A!1. Will if be only one or uill it be a panel?
"T. ITCH 0!l. This vill be a panel of three, lir. Chairaan.
THE CHAIR!>N1. Panel of three.
la. ITCH 0!). Yes, sir. .
TiiE CHAIRMA!!. 14ay ue have them, please. Go to the ros-trua so that they will be suorn in. 141nister Itchon, we remind you that we have that standing directive that all of those who give statements and dissertations are to be suorn ,
under oath and then they shculd submit a curriculum vitae showin~g thei'r qu'alifications.
l'R. ITCH 0il. Yes, sir.
Tile CHAIR!4All. Please submit that as soon as possible.
Let us have the gentlecen go to the rostrum and please state your respective names. The first gentlecan is...
1222 166
Co.uissi n ca :!uclear Plants 11 July 1979 Page 4 3:30-4:00 P.I.l.
!>R. lE!1Y. lly name is Charles R. Healy. I a Projset
!hnager of Ebasco Services, Inc. ll u 45 years old, and I a married.
THE CHAIR!.!AN. Residence?
Il.R.11E!d.Y. I a a resident of the Philippines.
Il!E CilAIR!ufl. Uhat particular place? Resident of what...
IS. helly. 14anila.
THE CHAlfduN. Street?
fir. IiE/1Y. Iliveat29RooseveltinNorthGreenhills, S:n Juan,!!anila.
TiiE C11AIRin!l. The next Gentleman.
I'2. GIU40RE. 14y name is Ja:r.es J. Gilmore. I a the Chief Consulting Civil Engineer for Ebasco Services, Inc.
I aa 51 years old, I am married; and I can give you either my business address or home address or both in flew York.
THE CHAIR!3N. Both.
MR. GIU.DRE. '0kay. Business address of Ebasco Services incorporated is !!ew York 10006, lieu York. My ho:e address is 40 Gaylore Drive West, Amadee Bell 11101, New York.
1222 167
Coedtaica cn I.'uclear Plants 11 July 1970 Page 5 3:30-4:00 P.I.I. hhk Il!E CilAIRMA.). The other Gentle an.
IS. IllfCRD. I:y nc:a is Noccan R. Tilford. I a.1 a geologist.' I a employed b Ebasco 3 Services. My business address is 2311 West Netherview, Greensborcugh,llerth Carolina in the IJnited States. My hace address is P.O.
Co.: 185 it1 Liberty. North Carolina, U.S. A. I a:1 carried.
I ca 44 ye:rs old.
iSE C! LAIR!!AI). Please raise your right hands and all of you uill be sucra sicultanscusly. .
ATJY. ,0FaViCLA. Do you s'.< ear to tell the truth, the thcie truth and nothing but the truth.
'A 1.'c do.
Tile CilAIRMid!. This is an elaboration of the LPC's ,
respcnses to questions 5, 6 and 7. The questien reads:
"In cise the~re should be an earthquake sicilar to that thich hit Mindanao in August 1977- this seems to be in-accurate - we vill refer back to the basic letter of instructions. ! uill call att:ntion to that point.
Itsays: "In case there Gould be an earthquake similar to the cne tha't hit !.lindenao in August 1977 uhich was of.
1222 iO
Cccaitsien en ::vclear Plants 11 July 1979 Page 6 3:30-4:00 p.m. j ?P !??f0'M3 :
! ;][uE v L d El:N rt 7.2 inicasily on the Richster ccale, uill the Bataan !!uclear Pl:nt be able to ulihst:.nd the shock uithout leak cr spillage resulting in nuclear contamination; can it uithstand a tsunami cr tidal uave caused by earthquake of teutonic crigin similar to the tsunami that hit !11ndanao in 19777 ihat is our first questica. You any proceed with your dis-sertation.
IdR. HEliY. 14r. Chairman and crebers of the Commission, if you uould please. I uould like to give a feu cinutes backgrcund about Ebasco to help set the tone of expertise.
thatte believe uns brought to the Bataan Nuclear Pouer Plant site saicciicn study.
THE CHAIR!!!J. For the record this is Idr. ...
14R. HEliY. Healy.
THE CilA]R:G. !!r. Healy, proceed.
!.9. HE.'iY. Ebasco Services is an independent operated subsidiary of Incearch Corporation of Dallas, Texas.
Ebasco is a full cervice censultant engineering constructicn orgtnization dadicated to the needs of the electric utilities e, a g .,a e- em a
Cod!ission on .!!uclear Plants g 3:20-4:00 P.fi. jk i h / ihrcughout the uccid. Ebasco is experienced in all aspects of en:rgy ccaversion ard energy system davelopaent. Ebasco has been in the energy business for 75 years. Me have been involved uith more than 500 clients throughout the uorld and ue have been involved in over 900 generating stations'. Of tha 200 ganaratir.D stations over 7CD have been.fessil-fueled units uith 200 of the 700 being over-ecasprojact.
Ebasco!.asbeeninvolvedinjustshortof200 hydro-clec,tric projects of thich appro::iaately 100 have been overseas.' t..!c have been involved in total uith about 120 tillica hilcuatts of generatica capacity. tot present Ebacouasirvolvedintuoenergyresearchprojectsin iha Vaited Staias. There are attempts to try to being .
r.eu types of generation to our society. One is a fusion test reacto. at Princeton University in fleu Jersey and the second is a research project on coal-gas location for the Deptrttent'of Energy and U.R. Grace Company.
Ebasco currently has in excess of 5400 employees appro-nc:.t.taly thich C0% are professionals. Our headquarters is ':su York Gity, United States, and we have principal 1222 )
1 Cc=.lecicn en i.'eclear Plants P' "; fmtpg l 11 July 1979 ib6t NNidO%l# L Pa;;e 8 ' 3:30-4:00 P.fl.
c.fficas at I,tir.nta, Georgia; !!2e;crt Beach, California; Jsrica, I!su York; Linbursa, Neu Jarsey. Ebasco also has a vsry spccial office in Greensville, North Carolina, uhich is our office that handles all geotechnical services of the earth sciences, which is the office that uas pri-carily inycived on the Dataan cite selection uork.
!!c have a petition uith NPC to eltborate on Questions
- 5. 6, a d 7. I uould like to express our appreciation ice pte indulgence for allcuing us your ti,T.e this ait:rncen to da ihat and ue uill en your time schedule.
Ue 1.nou it'is short and ue will finish by 5:00 o' clock.
Or prograa is that on questica !!o. 5, !!r. Tilford, our cor. alting engineer and geologis! uill handle Guestion 5; I:r. Gil:rra, cur chief civil censulting engineer uill hanula Cuestien No. 6 and uill return to I.!r. Tilford to finish up uith Guesticn No. 7. Our esticated time vill be about I hour and 5 cinutes. Uith your iadulgence I like to haJa !!r. Gilecre to take the sace.
Il!E CilA!.9:.;!.'!. Proceed, i.:r. Gilcare.
- 12. liEl.!.Y. Excuse se, l.lr. Tiliced.
1222 W
Jc :is!!a en ;.uclear Plants 111.ly 1979 OPOO nr Paga 0 3:30-4:00 P.l!. IdwiU;$php,l' Aru.
iiii Ci!A!R"'.*.!. 1'.r. Tilford.
'3.TILF0ilD. I a !!arcan R. Tilford. I ta identified cc a geologist. I probably shculd give you a little core I have sc:a 22 ye:;rs of experience ir.foraation a';out nyself.
as a pecfs:sional geologist; l hold Bachelor and Master h:rcas frca t.rizona Stats University. Dr. Ferg attende a c:dlier rival c:hcol. (Launhtar) 1 an registered as a Prof essicn21 Coelogist in the Staics of Arizana, California, Idaho and Cecrgia; I a a member of the Philippine Asso-clatDnofGeologists;theAssociationofEngineering G2clegists in the United States there I am Chairaan of th C.rclina S:ctica; I balong to the Gaological Society of herica; t;.e Intern;tional Associatica of Engineering Geclogists and the U.S. Ccuittee on large Dams.
!'1 pri.xry. areas bf interest cnd exper'tise are in evaluaticn of geological hazceds and economy and engineeringprojects. I have been with Ebasco for scce 10 years; ! have been acccciated uith the geology seis-aalogy, siting tnd cafety studies for the Philippine
!!uclear Reactor No.1 ice scrue five years. Beginning in the fall of 1974 I h:ve been involved in assessing
--=*%..
1222 172
Caissica a l:eclecr Plats 11 July 1079
.g %
IliUn by Page 10 - 3:30-4:00 P.N. 3d[y 9 alagic:1 htnrds ice th: tr.guna Verda 4.aclece Pcuer Plant in I.:x:!:o; I hav2 b:En a censulting g: ologist en i !
Efety Siudiesi on Preparation lleports fcr the PEPC0 0'ougl i
Poir.t Muclecr Pcuer Plant in Maryland; lbshington a
P:.'lic Pcuar System Saisop Muclear Pitnis 3 and 5; licucic:i ?cuer ced Light Ibc!ccr Pou r Plant at Allcns Crank and Ecrico Feral linit f6. 3 for CFC.
! t:.2nticn.d ti,at I have spent nou cpproaching soma iive yres of involv:::at ulih Pl.'P? unit 1. I have been pre;,cnt in ths P.':111ppinsa prob:.bly for a total duration cf ccte nina ;anihs during thct perfod of tice. I utnt la infara 0he Ca:ission cad the Senator of the depth
- .r.d i.ite.sity of the studies uhich eere directad at findir.] c sale site in aceting the regulatory require-caats,ulih regards to safety for this nuclear power plant.
In that connection, Ebasco has devoted 70-aan y.ars or some 810-aca conths or some 17,000 man-days of professicnal cciantific effort cupporting, resiting ud safaty sicdies related to the Philippina l'uclear uiui. 1 2 hric tt ena ciago in 1975 cnd 1975 14 pro-fessicnal cualificd earth cciantists in the Philippines g Ln \]b
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11 July 1970 Pcp 11 3:33-4:00 P.!Lf'uf.qqqinp(Odil di'ddb ucr!dng cc. 'his itch far c rc tha cna ycc. each. Sc:e of thass p=ple usrs iara for a c:: cess of it:0 yetrs. In 1t hat ccaacu..c a tnd in support of the re,aining respen-
.s.m x . .m. u.a u n..s . ,,. , N.. Ms . .w-5c"ea snd P., C, t have ,snu r-ticipigd in ih3 pecpa'ctica :nd issuanca of a ne: cr of ca,::ric, '.hs first of uhid '.= a ints. ia sita report v a.
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reSpC,.. i'512 iCr th3 site 007i."il !di0n l'epart thich uas issued ia J:::uuy of 1973 that ccasisted of one volene.
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"u. s:fe site in'.eslio.dicn report uns issued m v,uly ci .5,,,0 car.s s m, :g or , va3_unas and cur portion 3
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s..culdcodiecdlyicthecuhjectthatIc.risupposed to be adderci.1; t':ich is Ocestica 5. I.t this paint, I tculd li!:a to entcc into tha r(cords tuo ccreections that I halieve tre nacessary reg:rding that question.
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. . . '..} ...,,, .f. ,'...a4.,al ,.s. , s _ .. ,.'.,. , yr. .,s .. . .l g.n. u. ! 0 ...;) e.,s .. .. . a. a ..e3 (gf..( p;; . -; .. Jl' .. , . 3c- ... .', ON. ui ' s.. M .i l .k. . C ^Ci i "s o .. ., , . .,e, i , .J....u..-.,,. .,, ' . . ...J,h.-n,. faPCur;h-c . . '.t., ... . . . . . . iL.t .'. C ' '. .' i. .r. r.I Ulib. US ',.A..e.3 - -- I . . . - . ' . . - ......o, ...q.. . . 4.1.y...: .. . . . ; .0 1 .1 '61 _r.r.!.p E.'. u..'. rt "- : I Of . \N \
_s .. :. :...
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'. . . ,..,a. s , p . .. _. ...a. p s _ . . .. a9 _. .c. '. . .; .,.e...,,6 . . ' . . s tt ,, , .p, . . . . c u .1 r , g .,.,. ._.n ':c is id C:1 irao c.? ihe Depriaant of C2 ology at Ecrid : S:215; Dr. '.'ala DcSurn the uas Chairacn of the
- gr teai c.,7 G:clegy ci !.'aslern l'aiversity at that time
.. a . ei., .. u,...s.'u 4 .,. . c. . .. .- .. ;: _, . v. ,.,: , .c.. . , r _ .a s...w.. . .ga cs. gco-c! "::%-.: , er 29 in...;, cw ::asulie.ni uns Dr. l?cy z.. '. . .:3 t::...m c. .. acr. -
c de) tr.d re: ate t ensin.c.s
^*
t t. s f
..... m ..nay, ::no ter..uas et h. .'v.
ar i.n Caroliru. And
. . .. .t ':: c;; cut.' consuhtrde eho ac::isted us. Dr. '.!y;c was cw z.1:Ul '.a t 1:La '.:crked ui'h es in est;blishino. the . :1 _ a. '.::ci:' like to piat out th:t as this . s. ,.3..6 .. ....a e
1222 179
~
Cc,:n aiccion on 1:cl::ar Deactor Plar.ts 11 a c1 y l')'/'> - 4:GO p..a. I L I
. . .t.hous we did consult a t length with ML TILFORD.
I have special appropriate Philippinc government agencies. to the Cce. mission on Volcanology, to Icrerenca to PAGASA, taa Dureau cf Minas and to the faculty of the Ur.iversity cf the Philippines, the Philippine Coast and Geodetic Survey j , to the graph. I and Philippine Weather Bureau with respect c into the record simply entered this organizational chart l in the hope that it will illustrate for you in same detai s that vill support the study the organizational arrangement documents, tha safety of the site, and the things that are Frcm that point then, we are Loing to be presented to you. and thrash going back to the slides, with your indulgence, cut more ccmpletely Question No. 5. in our safety analysis This is a drawing which appears rcport.
~ "3-NPC".
THC C11 AIRMAN. We will mark this as Exhibit there will be Covernucat panel, please take note so that no improper interchange. score of seicmicity and tectonics
!:2. TILFORD. The in the l'hilippines have been considered thoroughly in the in Dataan. In this design of the Philippine nuclear plant d ~
study, it has been shown that Luzon, findoro and associate c'f:hore areas can be divided into distinct coastal blo The contents of.these blocks are 4 structural featuces l that clearly separate dif ferent geologic provinces a ong i major coastal lines or zones that have charsgcable attenuat on I 1222 180
C.n. ai s sis,n s.: thsclear De. actor Plants
- L .laly l ') 7 ') - 4:00 p.ne, n- o j ,,
i characturictics for earthquake wave generated outside Each boundary separates three that coastal unit. tectonic provinces: namely, Northern Luzon, Central . Dataan Penin-Luzon and Southern Luzon and Mindoro. au'a, the site, is in Central Lu:en tactonic province. I would like to point out that the US Nuclear negulatory Commission requires what we call a deter-ministic study to resolve what the cafe shutdown earthquake value should be in the nuclear power plant cite. Without complicating the issue more for you as to whather thic 1: juctified, let ne tell you that in achieving this daterminictic methodology, wo identified i the Lcundaries of the appropriate geolcgic and tecten c provinces in Luzon fcr the purpose of ausessing the
- The effects on the site of distant carthquakes.
cithodology involved is that we cust take the flindanao carthqushc from Mindanao moving L thousand kilcmeters and going ahuad to tta lino idcatificJ here as the Taal which Practure Zone, which is a cono coastal extension, has a fcvoralilo impression upon earthquake's motion generated on ene sido of the other with. respect to the qther side. We bring an earthquake, we place it along this boundary line at closest the approach of this coundar, line f aature through the site, and then we attenuate other yuakea to the site in terms of what
'ptv 1
1222 181
~ .~
Ca/m.n ::uic.n on !!uulcar 1(c. actor Plants 1 1 J '.. l y 3 '.* 7 ') - 4:00 p.u. 00 b i the grour.d motion should ba. That is true for any-
- whr.rc around this entire rc.jion.
T;10 C!!AITJ1AN. !!r. Til f ord, could you tell u no MR. TILFORD. Yes. It Vas identified as the Taal Fracture Zone, I believe, in a publication by Sovict ,and somcone else in about 1938. TIIC CifAIPJ4AN. What is the basis for it? Why tnat particular tcrainology? MR. TILFC3D. It is simply a desertitive phrase that i n ec;..nonly roccgnized by investigators in this scrt of study. Taal is the name of an active volcano-
, which forms a part of this line. The fracture zonc indicatec that it is a line along which the earth's ~
surface is broken ccamon y. And we knew in this ins-tance that 6his is a :one or coastal extension that is - two sidcc have fallca apart and therefore the rgocions
,frou carthquakes generated on this side tend to be attenuated pretty markedly or reduced pretty markedly on a coastal lina. ". . w ~;1 TAI PEN . In other words, Mr. Tilford, whenever there is an carthquako that aris,s, tha t usually is the line that would open. Is that correct?
- ... TILTORD. Ycs, it may open during carth-Y
].' l quakes associated with the zone. p
i (
~ Nim.i ncion on ;;m:u :,r Lc;ic t or Plant .:00 p.m.
I s 11 J t.l> 19/9
/ \1. . < j er J
T!IE Clit.I!U1A!I. That would be where the crack voidd appear. Ls, sir.
R . TI!.P0kD .
nes? connection with the other fracturc zo fault Yes, this is the Philippine MR. TILFC:1D . f the raajor active faults which many It cf you know is one oforras a qui in tile world. thern Luzon tectonic the dictinct10n Letwacn tha Nor nd the other provinces cr.d Central Lucen i provincesh isathe featurc ty here is the Manila trench whicbduction of location or site of the consu:rption h or suPhilippine the cecaa ficor plate bencath t e Ti.2 CI: air;:tJJ. The other fracture zoncs are Antonio Prac-Manila Day Fracture Zone, Sats entiticd: Zanc. ture Dr.e and the Iba l'racturo Ycs. h.: . TIL!'ORD. 9
'O.c !!cw , the Taal Fractura T!!E Ci! AID!AN. ould crack or op ..
would be tha approxin. ate line that w
. if the Taal volcano crupted.
It dccs not necessarily follow M9.. TILFCED. volcano raay or raay nct be the eruption cf a that Ir. most cases, the cartl.- accott.panied by carthquake. ctivi ty is very nic.. quake a:.n;ccie.Lcd with vcleanic a a
};% ,t.*
1222 183
.. _ e
Ccr.nif acien in: N::::i . c. r a. t cr F L:,,t:: 11 July 19/9 - 4:: 0 p . .. (' ,l. . z ~ T:!E C:lAIRMA:1. But the point is if there is
. c .1j- crack this s:Ould 1,c Ll.e usual lino.
MR. TILFC3D. It uuuld he the usual line for k i carthquakea cuociated with thic general alignment. The can.'a ic truc with the others. TIIC CIIAIREN. The same genera; alignment. I s The u! tr.acs wc.a referring to the areas around the Southorn Lunon, Mindc.ro t cctenic province. Is that Correct? *
! The peint, 7:r . Tilferd is that thfs particular j
dissertation ic being recorded in the stenographic notcu and whenever you say "this" without specifying w uhat particular reference, we would not be able to . knt,w in the stenogr? , hic notes. So, will you please reper.t taas r .cion so that when you say instead cf th i c. , yc u would specify the point of reference. M2. TILFORD. I tippreciate that co.v.:e n t . I l must apologize f;r thia. I t The Taal Fracturu Zone separates the Southern Luzcn and Mindoro tectonic province from the Central I.u on tectonic province. The Taal Fracture Zone is an w a...Gcd line along which earthquakc.a w.y cccur.
- It is a zone or extensio.. of the carth's crust and oi.c in which scit.mic motions from one part to the other s.nd arc reduced cr cquelched or attenuated as
$t /y . em . g 1222 15
I ' '
l, . . ! [l p." ' -l' ,; .
. ,I l r
- 4. ,r .; . .. i: ,
.i ., .i . ~ Con. sis h,3 o i o,d inclair Roactor Plan'.c 1 J u l y' .} ) l9 7 4 rGO pm. ,
p.. u i 4. ,,. ..osh . . , .. . . t j r ,0; . . I. .
.:Jy. ,. ,,. ..r 4 : . .: i . .,.4 p- . .~ ..
b .... . : ' Y. f$Q it c ss .t?at .ino. The Philippino fault separat as i . Tyh l. E . ;' .. l
.d.:. ti ntrh.1 Lukon t cton c province, the area of s '. . .< q l ./. .i . "romj the'Itorth]ern Luzon tectonic province 1:syerect, .
o \{ arl it' o f. 'h. .it e 4. i
. ,2rnent .l hi. g n.e... .'ppines l
J .' !p . i ;l;. *8', fei re which dominates the geology which is an active fault and along I
j which'rr ve'ry)ecemenly takes place daring majori j
i .* t Philippin}erearthquafesbacausetheyarethecarthquakes c: curring,t ;to j release stres:: along that fault. '.
.: .The, t.hir.d 'b. ound.a..ry., to the , Central Luzon to tonic province is the Manilh" Bay trench which separates tha' Contral Luzon ctonic province fro:n the South China f
Sea in a, geologicali senso. Interior to the Central
?
Luzon tec' tonic, province arc four' identified zonas of
~
a '._ 'i, . fracturing and' faulting. 'From the North, they are the
. u
- ILd Fractura*2one, the San; Antonio Fracturc Zone, the Manil'a D'h Fracturo Zone', a'll of which trenched generall,-
- * . .I cast-wast and *all of which represent presently activo faul' ting'along which'earthcluakos'have taken place during 'thcI' $iist'oric51 Ipast;32 '#*' ' ' .l
- There ls orte a'dhibion'al' feature that is not
~'
shown' 1* n " this ~i par'ticdli~r PASR- figure'. It is called the West;Luzon"tbo g@ anilit isi found offshore of Bataan but' not bn tho we' stern sido of' the Manila trench. It is'sonie'240 bilei.ste'rs^1n length and for purpoces of d'cto'rmina tiobi of5'rthiiuske a motions at the plant site
- ...; p. i p ,,f * . c.d 2 u, 2., .. ;o .,
p.;/
~' .1 , . n ..i . l.h .o i: , t. 0 . l'.
i
*..',; h.. . ;h . : r a c, n r ;., t e n . . sn .
l
..r .~ td .u t ' . 1 ' t. 2 e f 4 . ;: '. . , : . i I . .'.- 4 .. .i . ,
f 4 4; :) irit; 7 'eti:: 7i s.ttr. p;..t n .s, 7
.! A'. } c lO 1 ius tri u . ; ::s F lin e t .- '.; . '1 ' i) ~* . . ML'.w. - , . d'.d . s;.au. 3' :' . .Li. . .u.u: :.? .i P p.d:W 4 u f' y .:..
I w .a.' p . . , p .t at .1,.e 1 u .. a : a ., . c, ;.:' . .' t '.. .. ' , , l.
- i. . , ' .W ' .e : \' !R: '.S::.t.
( Cm M t. f ot. on !Juc1citr Reac t or Plants 11 Jaly 1979 - 4:00 p.m. f)o n 7
) , is censidered to repres.ent un active geologic fault.
[ H!C Cl! AIR.**A!1. '11 right, Mr. Ti;ferd, we Iw note fecm that sketch that oc have two other fracture 20".e s : the Iba Frac:ure "one and the San Antonio I'ractura Zanc. In fact, there is a third one: the Man 11s Day Fracture Zone. The line seems to ge hwyond the lands curface into the coa. Dces it raean has the cracking of the carth would include not only the dry land but even the ocean or seabed?
!-i R . TILTORD. Yes, that is exactly correct.
Mcw, once wa have established that the geologic features thich can produca carthquakes within this tecto::ic province, we must scake an assostment of the
- largcat carthquake thich cculd occur on each of theco featurec. And then determine what motion would he impartal into the fcundatien rock at the particular site in quactior.. In this case, the location of the Cataan Nuclear Plant. That process is completed and the. motion that would Le dalivered at that point frca
. anyone of thouc maximum cccur-ances is expressed as a percentage of the exhilaration of cravity of the poor.trt cet of the compencnts.to be r.. ore specific. !!cw, in that context, let nie discous the design f acters of thic plant ac they relate to the flindanao earthquako of August, 197G. To do that, let us look at a few u. ore . f,/
slides.
-.o.=== }22c lOdi
I
-Ccmmiscica im :;ucla z haanc: ?lants 21 July 10*/) - ::00 p,u.
tc r t i
/
s Tile Cl!AI.rCUdi. Mari; this diagram as Ext.ibit
' " 1 -N P C . tiait a n:inute. Them: has been a change.
1.'hich onO are va going to car:0 This one or that enc? MR. TII.rCnD . Uc can mark this or.c and identify I T!in C!lAIPJ1A11. Exhibit "4-NPC" rcprosents an I $ aerial view. Governraent panel, please take note. Please procecd. MR. TILFORD. As I have ir.entioned to you, we want
' dawn to ..adanao to investi;;ta the effects of the August, 1976 carthquaka. hic is a vieu which illus-trates the general nature of the arca where the earth-quaho produced the greatest damage, by specifying the' ,carthquake as cpposed to the tsunami which will be raffered. The earthqucke.did tha,createst damage in thic instance as it does in many other cases in the .scrld whara the land is flat, Icw-lined ar.d ccr. posed cf unconsoliJeted, unceacnted, gefr, nossy sediment which is cuturated with water.
As you can see in the picture at the background
- of thic particular vicw, the area around Cotabato is It is low-lined, sedimentary, un-just such an arca.
consolidated, ' saturated. This illuctratraticn is an acrial view shouing fissuring or cracking of t!;e earth's e r. /
~
- v. .
curface acar Cctabato. l
.. =.
1222 187
~
( Cc L.a i s a i t .a L.n t.. c l e i r lia;.i c t ., .'l at.L c 11 l a l y 1 *> 7 ') - : b u p . .is .
- pg B121 T :0 C!!A1;J4A:;. Jur.;t a r.tiau te . 'l.is
. is to be i .u k ed n Lxhiott
- S-r:PC", st.ow'19 an e.orial view and depicting ccconut trous.
Om. TILFO!Q. In t!.c conter of this photograph, you will Lac a crack in-the ground that is a feature that is c lled fissuring. It occurs during carthquakes very coi. ..only at even very Icu c::hilaration values in t.ncoasalidated alluviu:/. mat.crials which are saturated Ti!; C;!A!TJ ll!. (Ii.tec t-tinn.) For the record, we u uld 11ho tc invite observations cn this particiar picturc. 'I hu chairc'.n's obcarve. tion is that the crack is not a t.hrcu'!h-and-th: cugh crack . It extends and sccas t.o end fro.a the bottent of the picture up to,
,about a third .. na crack sce.nis to end at that spct.
Any cLacrvationa fecm the part of t!.c parties?
. Particip.nts? Senator Tanada. !!o corser.t frc Sanctor Tahada. The Cccaniccioncre? *;o cbservation frcm the cor.;nis cience rs .
MA. TILFCl!D . I confir:a tnc chairman's cLt er-
,vation. The chservation is correct.
This is another illustration. It is an acrial
- i. hot:cr:ph Ic 31ng forth at Cotabato en the sea coact at the mouth of the river.
T!! CIII.I DMI.II . l' ark th ca:nc as l'.xhibi t " G-t:DC" . ty
.')y F
1222 188
e .
- Cc;:. i: .;ica on iulnar :u.ac;ua P; ant ; .
- ,1 .5 . . ', 1 sh - 4: -Q v,m.
!!!! . TII.TORD. ( Con t i nui ncs . ) I uculd use this sli dcs to r.uka a point regarding the tsunami. He over- ' t.w a r.d Ic !;cd very caref:.;1 y at the entire coastal rcyicr. for prcper viewing of Cotabste and Leyend. We landud en several locaticna to incpect various kinds of detage. It was our observation that most ccmmonly nipa structures Lailt en stilt: or stands en shore at eleva-tion; of about ena to two unters above, Lei.wJ high tido, ucre not dicplaced. That to a lcng technical ..ay of a f r <; tl.A : n ..,c:: t of tha ridga of t: ic coact line, whe tr u.a a: in 1.c. very largo. The tsun.c.i c.:s exag-gerated an coastal embadments betweer. separated points or paninculac of lund whera a bore is formed . A hard horc which is actually a lcrgc wave recurs during the "approcch of tsunami giant waves to the secshore and in c:.cn tretches of Laach and particularly at the heads ~
cf peninsulas cr peintc. There was no obccrvable da .;a f re;7 tsuncmi. The damage frem tsunami incurred in a Lay and to that exter.t, I would point cut to you that the niga structurcs in the lower Icft of this phete-
, graph uhich you may have difficulty to see but which I can point out to the Cem.aicsion, are in fact, and they are surely no .ncro than.two maters above high tido. I pointh,d out to you in this connection that t!.e USNLC and their conLultants - the US Ceolcgical Survey, are at pracent rcquiring a pl nt design grade en the coast of Californi; in USA cf 15 metera alcve sca level.
pn./ O
, D
- c. . .6 ..
. . c ' : r. t :.
ii .h..- ; .' . - , . . .
-)
g M s.1 c.:it.pa c a t... C l i f orn . . ci taa ti.un alth that of the 9 ' uc c e. . . i c i .' c f u. t .. .' C.. L : i .::ni: haa the full fatch
..2-.... . r t. . ..; ch t r ua .t.1 giout waeca c.; ri -;n c f wl.
c.in re a.;.. t... t L .'. a . .1.:; pine. coastlina en the CoauiCL-- .- 6 tar.t rc h cr f atch only of the C:.i c.a . It is an appreciable dic taner. to tha rc.a. :ler,. dif f.:rar.ca. Tha h I f ar ... ... ; c 12a twar 1, O thcocand mile:s
- ..w C 3.
'd . ca w . 1......a ...: ; th ic 't you have to be awara cf . , i.at ha i..:cl.: n. p..in t in 3atasn hac a plant p; dc c' .-c;. . 10 .c t.;r; - . . c. c . levc2. So far as I liig.. cut clavctian clove Oca levcl
- .a : arc, ;.hs ; i: th at s.hi ;) a ..uclcc I Inc . :. ; hac been est:.Llished for cnc's couling in t!.. .ccri . Ac. ic wac ustnbliahoc at c:-:tra.:.a u.*cn aic pe:.alty cf puncir.g water f c; 50 years i:. " d is ;..:Ja in l.a19 .c L ... ' y bac aE u Of *.liu inSGG cn c.. f ;. - a . and safe-par. ;ite.
u t. . .... i .. ' h :, . . . ::. .c
. . .. a u r . 1 p .s tc..j r.. p; . cl, . bc l ievc. , l';;h iti t .. o , . w . .a a . .. - - . .
_ .s . 4* a . a >. s ,io . se 7 .t .; ..r. .s w ..oI?.v
...e..,,. .n..... , . . ,,. i . .. c .< a...c . .. .w. .c...._....p . . i s> .. .. ~ 1y ... .. .. ...e. .t. .o. . ...m c ,. s.. , .- ...
2,.v . . . . . . . . . ... ..... .. .. .. .- . . .
,, Iw. . . . .
- h;c .- A 1 ;4.c. J2 , 1 . sin .c enccc .c! .:d c7 t!. ace
.' . . . ..s ..c.., . .: a t s .. , t' .t- f c 10 }. . ,
- n w.c .... ,* caa 11.. i . . .-
- . c a l e:vul -c.o da c tr ac-7.[
1222 190
tl. i; s. 1.1. L . (*
-> J.,' ; 2 s ') - .:OJ }).
- r l
. J .: ;,. '. a L;1..ut2. '. l .1 J 1 :.i to ba L.. ' : ,o i c
- S .
' ' , L . .: .s i a) :' L. aria: vacu ...G u ..,r.nu.. t .r . . .. . ......uu " In ti.; center cf this pr.ctogra'ph, M. 't;L. O n3.
you i:111. .,aa e crac!: in-t!.c ground that in a featurc I'
's c ..cd Jicuuring.
It cecurs Juring carthquakas v t;. y c i.. ...;ill , a *. 1: .'en v e ry 1c .? a::hileraticn values in
4' * ..J :11uvat.. ustaricic shich cre esturatn0 Qg:.._- 'u~ . ) rcr ..;a record, 77 . . '. 2 .. ' ! .
ft,Ot( $ invite cbc :r .';:.1:n cn t r. n par tic.:l ar
'.. s i .; eu . 2 2 .. ..
p 0.ura, 11..; 0 ;.a ir.- . .n ' a cL: crv ticn is that ti.e It cxtcalu crn;:: i s .:. . thrcujh-an '- d : c" ,h crac.; .
.!.e picture up to, .nd L:.c.a t . 2.0 f rc..' t!:c Latar- cf e
tr > crac!: tc ::.ts to cr.d tit that spot. s oot:.; a third ... llc pact cf t!.c partics? 7 ".' U.c :rvat ion frct ,.,n.,.~~.
,.,.......,.,.i.i. .....u; a, e c . . ... u, . ....e..... . su . . . . . ~ . . ..
Obccrvation fic.; the
. .'. .. 2 2 . '. O Cc.. ::i c;ic:,ar a .
cc. .. tis ican r & . 1 C G . . . a .':.1
..s' ChJirthar. ' O CLLO!- '. .i . . .' l.*. O f. ., .
C.. s .: :v;.t i x . c.)::c:t.
.'a t ze .s . . - ; ; :.. .a t.. .
Illu;t *;icr,. It ic cn 23 rial
".': .1 1 r ..r i n g ic r '.h .a t pu .Lato en ti.c sea coact t' -r.
st t:m .:.ou t .: 0; tnu ri.ac. u.O as . :;l. j l,2 t " 6 -I; P C " , t
'. d . i. . ..4. .. .. *. .s I
0k 49 p
/
i 1222 191
., , ...L., ~ . . ...i.... . . .. . .
4 . ' . - . .C j.. l..,e t.' a M'. '.';II'O iO . (Cen t i nt:i no . ) I '.;culd use this s l ; e c. to...L a pcInt r e c, a r d i n g the tsunani. 1c cvar-
. i r. .s . . . . I c :. .;d vr.. j c f c f ;; ; j c :ne .:.fre cesstal a., i e :i .~ . ;.reper vitc..'ing at Cot :.;to cnl bayc.J. We lanu en .c aral 1:.,c:.ticn; to incpect various kinds cf g
5 L
" -. .: L e . It was cur observatica that sicst ccmmenly nipa mucture . Lailt on ct13 t.c or stands en 1.hoce at clev -
tion.; cf L.mut cuc to uro itcrs chave, Lei.aj high tide,
*;cre nc: dicplaced, That du : 1:ng technical ':Ly of 1.!. ;;. COOCE li:.C , . ' ' , ' 1: i .. ,U :; <,. t,. Lis i 1. d( . O f .~
J .. :a..-.' ; .; :.v . . a u g 1.r. . . ': hc t s. .:n :.... i wa s c:c. J-
, c r a t t. .i . ' cc.:s:cl c .h..Jr..cn r a hc.tt:acn separcted peintc cr s /. . . .. .d a -a of lun? '..erc. a tcra ::, forr.wd A hard ic rc '.Qic'.. 1; aclually a ic... . t; ave cccurs during the 's .. er oc. 'r Of tsunami gian'. ..avec to the secshore and in c;-e . . ;.tr.tc:ws cf L:.act er. parcicularly Lt the heads cf J'eni- c2 .; cr c,cintr.. '2harc ', as nc ob.:crvable .. . , . . 2.cn Laun.c.i. The d;.:ge f rca tsur. nL incurred e., a Lc.'; ...2 ts th:t 0.< t e n t , ! uculd point c u t. to ycu that tna r. iga ctructurca ia !.c lower left of this ph to- . e,ri r h . .ich j:n may have dif fic ulty to see but tihich -! cc.n pcir.t cut to the Cc.s.:i Lion, are in fact, and ti4ay arc curely nc ecrc ti.c.n ...;c materc aLcw birJ:.
s ida. 1 ;..;intqd ou t.c jeu 11. cais connccticr. ::. t llc UE; ~.C c:. . t'..m i r ccna i tar. .;; - ...; US Ceolcgical Survej, occ t ,. . .. c . : rc.q u _ r a. J p l .' . . C a. : iij n g r a cie On the
- s . c; C_liforni_ . U.. c. i-.ater; aLcve sca level.
/ } ,,g*
1222 192
. . . ..u..l... . ...;. .c .1.ints .t. '. 12!; - *eUJ a *;i c . - cc. ,. .'..s t e c r c .: r. n .; . . t ductruction on ! : ; 3. .;-.. ;, lic.htl';-con t cucted :-nd uncr.ginecred ,' ; ;;. . ; .: peo, . > bc
- nre in, ural in this
- t. ho
- . . ; ::' I , i nd t'..cro u.' r p r c. L '. / thousand of the::t scrc killed, uuro killed c:cause they ifvi.d in nips
- tilt-Lup,.cr ead s tructu cc .;uilt cver the Lay. They
. n .d cv L ...: . :tc N .. ,00: joic;s cf those ..ctLet..a a cc..mnly lu'. :. lad about 25 cantic.ctors .i..._.,_.a .. > . a ,. L. ..< 3. ..
e' mt'na.) ...: T Cc ..iccicn Ci . C.: '..~ T'. ".:J. (~ .. c; . c c .~ . n . 'h: cantuc ;.oction of ucu2a lihc . , c:: .
.ctual'.y cheu c that pi c :u.. e , !:r. Tilf o 7. , de,t c th..t c all ap s .. .. tcef? - " C.;JC*C. b. , . . .
It the.:s s ecllapi.e s. i. e.. e, ,a.a. .u.. 1,.
..3 . i....,. ...1 w. . 4.11ing c2 .... ..cr... ;1..
ad th .: you :,cu in tha e t.... .. . <-..i ,.
,..s... .. .c Ctu'"", .
- :. .a ..:. . . .g y ;u t h e . . .. ., . cf ' . dcch s ;r.d t.harvas a :. ._ ,. i er a . au : .w.. . . ., L.a. c >:te n t of ti.e da:.1;gc .
.11c: o2 toi. ;> .o tLcu::.nds c,f pcopic .. . u l '.... v.:.-
a .. r e .. 11..: ., thaf: ! .c .c.c ..t aidnig.- in cr.011 lig!.tly-
- - .. t. e n.. .
a'
- v
. . - . ' u- ... '. ..*...c . .~~~".
a 20. l.. ti. 2 cantcal part cf tr.i
*i . . .: Cf!?.I.' . . . . .y o t.13 r 2 n c t *. u C f. 4 C. f f.1 C LU . O , :L . 0 .12c;,, ,
- s. r .2 tm...
rc ... ci . i E ..c . asidas the ca.tc.- , ,, _
. f c;.] .... 1, .
- 4 *
.,p *w.* w b.
- p.,.3 e c -
1222 193
4 . . . . ...u . . . . . ,. .. . . a., s. .....
..n.
PGBR ORIGINAL
. '.C '."' 7.~.0 . Cis.c. t he d.. gee cf cara trich , . s .. ...c..c......, ... . ...u I . . a c i d e .. ,- . .. . . . a- d o.a. ' t .* :: . C. . 2. . . . :.o. i': ; ..ny the car. cr portica
- w. u. ... a. ._. . ~ , ,.. , n. ..
. . . .._... . e . . . . .. c. as. .i g s. s ' d- r o c.' ? ...w..s. . v.,,., .. l . . ...-.4., .~v . . cc... .. 1, .-.. . . . . 1c.....,.c..t.. .. u. .- ... , . . . . oe s. . ..u...c .: . . .. .. .. ,. <. . . .. . . . . . . .. . . . . . .. ..a. . . -. , A. .. . . . . ,..-...a. ,. . . . . . ,.. , c. .... .. s. w.... . .. 5,o ., n ,. , . , . . . , . .......s..,
s_.....
. . . .. w...-.g. . a.. ,.- . . , ., .. . . . ._ .. . , .._...i .m u.. . ...,. . .a. .6. ,. i....e. , . _ _ , ....: . . . _ut..-2 . . , m a la 1.- larta p rt ...i,, ... . u ~ - ..i . .3 ,
C.4-
. . . , . , . . . . . . _. . . . . . . . . . . .. .. a. .m _ . ... . . . . .s M -e , .. . C *., . . . . . . .. , * ~ ..a.
s.... . . .s
- .. . ..: D .L . . . . . it. c :. . .. . .* M 11 v i c'.i c :
.. -. .....w ......u..1 ..-. . c *. 4 .' .' .. . ..... N. .a c e. s , c.. p.. .: . pg.o'.., b.)..., P. ; .[ . . . . ..,, , ... i,. .t....e ..
s
.. a. a .. , .. . . w ' ..g.e- . . . . . . . . . . . . .. ,.. . . . L.. . .. w. . . 3 p. . ., ,.,.{,,.,.3,.4k. .6 .. . ,o i/
k' 1222 194
1
' . : L ;.
1 , . 4 .. . ; . . , , .
-o I-, .
I t'4r .* f** Q e9 ,3, - ' O l i' u. ,, . , 4uh Of0bn
- Tb.< , . . . . . -e. , t ii. .' 0 0 . In ..4 e ra; in ',..;J 1 0:00.1 of a
.. .'-- . -' .. 10 C '. ", J u :a C O L t. ;O .G e . ... ., . . . . c . . :. ..a .b. 2m. . sida, L y ; e n i n a.;; .-- cf ..a.. ..
a . . .l 0.i. . :. . ." e. f a.. ci.: :.rvations t: fore you go c. ,
< ..,.r 4 w a.. p.,... ...... 9...evo 1 , s .
s.. csf.;. w~..,
. . . ,., e. v 4 1. , .<.. a .,L..
(. . ; , ... .. .. i s'. \ ?' , . 05 .. . v Cr; DO L '" C .* C . '* T. O VCGO - .
. .. .. . . . . . . . .w.. ... . ...o. .s ...t., .... ,, ....,, .n.: ... .. . ; . , . t 1. . ,O . 1... .w. .. l t. .. . -...
w .i .c... . ...t..a....
. ...a t C..e .. ...s..,., ...e w t......s. ,. . 3 J
g..... . . . . . . .., ..
...~..e, L '. .C . ' . ' . .** ' . ' '.. . ' ' . ~.~ .' . d .'" O . .. ....i * \' . .0 . .J C l. ? . ... . ..w. .,2 ..La ,.s.
on u. ....'a ,
. a. . i .. u. 6.w .r '. G . ,. . . .......;'=.> . . . .. . . . . . . . .a .4- }. ., L.i. .t... , L ..-
M.s.J1 ., l LA *.
* . . . .. i,a . . . . . . . . .,.w.., . .. . . . .1 .w ,s
- w. Cs c..-** .
..3 s.+s.....
6-i . C. 6. ,
- .' 3 C L C O* UC ..'.1 .2v C O CU. . . . 10 iC .d LU . ...$
C . . .; r 1. ; t l . 1. ri. e :J .' i . ; , . . ; .? 1.* aV O J . . . . tC CVOTz 0*lCI e t e '! L..u .. .. 1222 195
. H t ' ll .
i.. i i ing fl' . i l t f
~ '
1, WI , Commission on'Nucicar Peactor Plants ' 11 ' July .1979, - 4 : 00 i p.ni. [o f 147 -
.t'.
i'* t . , i .*..i.
. p'. ii H! \' =
T!!E C11 AIRMAN. By overpowering, do you mean that
.a. . 'they rise hig' hor than ht'o top of the trees.
g j i - ... .. .i . i A . il [t- gg
; 4 0q[g(
1 . i . g , j"[ MR'. TILFORD. l The highest recorded tsunami in
'i i /
the world in' tistory occurred in 1964 on the coastal
- i <
Chile in South i, A.merica not recorded in actual meters. So,,,,,actually ,the answer generally to the question is g i i.....,,, . l}o. ,i,,Th.at is not 'the case; there is simply so much ,
;eq. .
water involved in.this way that it goes through the trees the wat'er simply p' asses. i TITE CIIAIRMAN. But would not the water go Eart'her' EnUard when there dro s o trees? i
,MR.' TII. FORD.' Sure. a p.; . ... ,
I le . .it..I e .
., I ' , Tl!E CilkIRMAN ' ' Sd,' it has an'ef fect.
t la t 12 in .oo. i
;,, q HR. iII. FORD; difhi'n' I:h'5' elevation ranges f
- t. here .a..r,e. c,cmhonly of' c6ncern, 5bupthe, ef fect is
- u. is.u.a. lly"..sma,'l.'l.!. B.ut,'I"
. 4 . u- agree i it has Ian e f fect. < .<r . -, . ia. I Wo% i. Tile.CIIAIRMAN, T Thank' you.] ;
3 ,, c si. li
' MR.. TII. FORD. This is another view looking in .. e ,
- the teth'er.di.rection at.Napot Point during the gruelling part of.gthe,,excayation,for the Bataan Nuclear Plant..
t ;t , . . i r. i , . , . i . .: i c . . i iTHE "- Cf1 AIRMAN. hrk it as is - Exhibit "10-NPC". '
).. ; I- . ,; i ,
MR. TILFOftD. May
.s 1.I show this again to illus-ti .
thate the natural. protection of.tbc site against * *
'. t'.. ,
ps,un,ami[. p,. , ,j 3, ),fitf= g , ; ,, ., *g *h! J . { k. I t
,y . .. . ..a.. . . ' t'ai - .; f. i . l . . i It lli:: ' f ar; n , ' ,I... . I p1.T111;'.d.'t.11J1.!
tf ir.,U j. p ;$ 1 ', trencei ti,l., t 1i W . .'t.
. i .fi .' .i}.,. pill./..'d. ; [' Y t 4 '3}'y on ' 1 t!"l:',t i,
I" i t ho cri,i io r ..ll i .e t i . . t- > ; i i
,1*i p gik. s g l . ' I,. . Lil ...: 7 jgf paa! L. ' G E . t t a g..,' ..:s,. . . . :i.;
f I /d
** 'I v' E ,, s k h . . .'.', , u p t'.'sjI~ n' ' f i
- T4*I' " .* .
i
. . . . . i....+. ,
e m,. j. .. . r
..s.m b,s e f a,., .wn.yi r.ei.
a gr .i i a
. 35 L d., l'.*u si t i,,y l p i 01, ire, 1,, a' aia .,k);if :i1- . .i
- I. s 't
- +.c '. . . . .
so- .. 'e . . I s ' ; *
- 8. k .. .
. {[;.p,t ,n: . oq, . m i.i i'. I: I '
(l q , f,' th A [ l . e4 t
- t }is, ,t ; ' ! .-
Conut uion on kiucl ear' ouctor Plants 11 July.1979 - 4:00 p.m. '
. ,1 e 'lb s . './ ; -
4..,.
. . .'. ; ! j '
t 'l-
, , 'i ' ,- l 1:II , i' . j,i '
j jTilECHAInHAN. Could. you, turn that back again just so we'cani make somo cbcervations. *
- i. ,
I t l I ". j* , ,, ,, f I
. . . , :0, s .' . o -This 'i,s. Exhibi.te. N. .o. "10-NPC".
A i.) d 5 t. hkkl j'i 8 ,1.. g', , f 'CCH. IVA.SQUEZ,,.That mountain up above thab I gM I
~... v.,8 turi.17. that 'Hount t;etib7 --....'g,. 'HR. TILFORD. 'No; that is Hount Mariveles.
t
- COM. VASQUEZ. Is it also a volcano? -
*n , < 4..f,g H R .. T.ILFORD.'rYos, it'is also a volca?.o. . .
COM. VASQUEZ. Hay we know the distance between the vo.cano and the site. MR. TILFORD. From memory, I think it is fiteen
, (15) pilometers..
COM. VASQUEz., t /Dyc air 4 6.- hrs.TILTORG. Yes,.i sir ii .
' O' CCli. ENUTISTN!' ilbb 3behind that is Mount Natib.
i . Behin6 Mc';nt'lMarivale sf. is t Mount :Na tib. *
} hrs Tff. FORD. Excuse me r. sir. Mount Natib is t Besido . to th6 .f a. f. t' 4 . g.pf,s phot.o, gya, ph,,,on a, pa th point.
s
- r.
- 8 the power plan is a depouit of rocks built up over sp 11put. . t #3 i, rp. , ,
more 'th.'.an':ene .hnd-a-half million years ago by the eruption df Mount Natib. Mount Natib is directly to - your le,$,t'a[h.o[l'ook itM* tee *Neture'. i i' '
,p U..'. j.l;'yb':d; i, ,.n. !g:.-W.L.ia; i< . :'- )
[.3.. Iglt'sy c,eh.% . .y. . . . .. o .. . t .a... 4
.. .. .a v. .. * , . .; ~ .? .
l
- l
'.4 If ' , ,_ ',.'-* Ty.. .m. .. . ; )T,i ,:c, kat E L*! :.v.v a i ',/ e s , tjc. . * *' t ~ *i,4 M tr. >,*s. . N.1pp:.f.
a w '..a . .".l .- ~#
.s!..*:
141 b.. n : iii g.3 pies y[:in in. )*h J 't:J. la ' NwiL r 61 L;,, ..;g;,;,!... . ;: ..
- w. .w , , . . r , t . . , ,, n
~ . '. _. {* r . G .kQe . h r.=a .~7;f t+q: ~ ;x.4..o%y.T.s.:' c:n 4'3?T,"W(47.0.g i 9 gr n..+,3 " ..
c w y -ct.:.y h ..y..w.... e p , m ,1.ag.: x g %w e esc. ...nv. Pmm,'. n.. .- ,. .
. 22,2 y % .p a a M .p.,e., n&M g!+e.M1W'W.H" u p .." .'-, '~
i ,..- i l
, i. * ' ' re s.1 I - i I . J Commisuiun on Nuc1 car 1(cacLor Plants 11 July 1979 - 4:00 p.in, jk',-y . 'g .
g t g . t. . : ,. . . . . *- .t 6 . .
,: . .i;. r. . .. ,. ' .1 . .t ii . , Sen.,,TANADA. Dut not very far from Mount ,i '(.', '
Par,1ve,los I;s. Mount Natib although it is at the lef t.
, F ; 14 MR. 'rILFORD. . Yes, i sir. ..g .< ~ .... t . y p r',e tl,TlIC CIIAIR}iAN. l On to t right part of this
- 3. i.' l 'it , . a. i l r; . .
rlp ictore; Mr.*f.Tilford, could you tell me if my observa-tion 1,s# accurate. There seems to be a sign of erosion Jak d in thip,;right part of the land jotting out.
. .....Mn. TQ. FORD. ,, Yay,, sir.; ,,.
as , .. I .. a- ti .i t . s , . . i. . THE Cf! AIRMAN. !!ow textensivetis cthdt etosion? . Did you~ observe?
'MR. TII. FORD.
Erosion actually is by clift-
. . . . . '.' .it..e 1 it s .. . . 6..-. ,
forming' waves.primarily during storm activity do *
- 61. .i . .. .( t .s.e. .t.ss a as....s. ..
= encroach - i upon the entire seacoast and the sculpturing I >' e,. *. . .
of the e, ntire seacoasf.... ..'is the result of this wave s ~ I. action. .The; erosion youisee2 1s_the erosion there at thei present .t'ime.i In.the past it has extended farther up totthe seasand.is. represented in the extcome right part of arsmall . outflow from there where yb.u ca.nnot T hese are the subsea
. .u 4,a . li esee here. 43-a : 4, . .
contouts of th'e land and this point extends up to
. 'i.i t Cid,1.il:t.t . ;tcu i :s t. r.s. i .r ,
the fight ... g!r i.. t w. oi . .< s t .4,
' /
- 7. D , - o
- I ' 1 118 kll Islili. t . r,n f en a es i. .
l .. i s . if.ip . ivi /.! .r p .o 1 . y d. . 41..i . e.. . ,
.pi:ri..th 3 ,o r. .. y nt.1 :.t s e s .1 p t. . . . , t ,
pp ti.i4',i,.ii; l'rj . alie i :a:t 'I q t 'i i .
. i s . .;t' 6 3"g{8 . . . f,'g' I 88' i,{,}8 . 4 ;i.hH y 'O '1 h ' ' 8 5. ' 'l. ,
il , f.[. if![j !@t . 't" ' ' f," ' [ f ' - .8 d . p;'ljeof, sg t::.. . ,T8? s Co n.\ s..a rg e . p.i . 4 i ,g, ;
,. ie ,. r tq ji . r li i l } . ar j. eij' s una.L4 o. 3 ... i. . t . t,. ...'.u l.3,*e. - _
gy,'.9.;.! g n ,Fif!!b v' '-'"'tr ,
': N' " 'I. " " "' }'2 2.2' l 9 0 - h'f. ..yQ..;{. f.i. ,( J bt: i .
- ...s.-
. . . i .; ; ,
l
. i . )j ' il ..
c. e , %' I Cl61ssion og l'eclear Plants ' QDDD MI jri p g 1) Pa, July 1979t- l l U di UH.I d ge . H.jgS0-5:00p.m.
, t >.. 9:,. t . . , goi i .
MR[Tip0RD.] ... to the r,ight as a soft seafloor point forappfoxidlely' one' kilometer.'
! ! iv : , l ' TH,E CHAIRMAfh l Mr. Tifford, hoh clatprial is that f::: 4 i j ructure.ofthdlandthadthis rea?
stabili,t'y MR.TILF0fl0!
- e. . : l'otthe)d!ilhe fact L. j l l that the lan'dlis presently a t
' s.u ,i 4 i peninsulaiMneffectaprooftestofstabliity. Theland ts adjacentto'.it'hassuccumbedtotheforcesoferosion,whereas i
th'is'.lind'hN', hbi l'ti $I$ength and stability by remaining
- 3. g i ,4 .,1.s .
availablet&usforyears. THECHIkMAS..Notwithstandin the signs of erosion that
.h. gi, ,i i
you. just . p.{:s . . d . . . i : 1 '
.a 3o@frited ou9 1t.i3 .o ya 1. ,, . NR.q .TILFORD,'l-).~. Erosion 41 . U l,is l .1,a lconstant p' .,
and ongoing process 1, sqrp : .i . i. , . , , , , inessentia4.yallpartsof'theearth! Theland
..i.i:i., q ir. : 4 .,,,:iu. e i r gi: p , . surface. , p .. , i, c; asses that.0ere . formally ' adjacent,u.o t 'this point oli both sides .1 u ;:; .; .. .- } .: uc t i n .. ua : o . .. ,,.
andextending.asfarastheMeecanseehaveerodedaway,
, ,:ti.sai n.g , .u i: a a pr ; i. :. L p ', t.. i n . i. l '. ,i thereas' thiEjioint remains. i i .. . ..iu.,p 13 h pp,.:in;ca.a;0u p the i st. . n! ,: k.. , . ' n'i g r THE CHAhidAN. Let us 9o to the next'Exhibi .i .
i L.oq,,gi.: :q un N y r,10 ti, anq p,;aa q ;,j -
' lll143. TILEORD. Now,-*we come backo Cotabato and I want - i ;,l* .i i ,
to show[ . i; . .;,g-you'hoqaschoolp.articularly we have pho and recor5sh nEny fAllil$sNf Col'atiato btitJthis is the Terrace'GFe$tr School. .! l' . IIIE CHAIRHAN. MM 'this ds'Eidiibit ll-NPC. ;
- . 13;m p ik.':1. ar .s of }th t.ario .,g . .
t i
,.j .. ... i,e3 illQ "d 10 7.ai.lf Si:jt.'cQnt to llg) ,. ' ;) .,
i a.
- . . d .cx}uldp0$n.~.ia .as in.) eye can 't. ,. h,.
i i..
- 3.. .5 f. . .i.l jefe 3 J ..
l Il I @l ! IC, _ B idI
;'C..).6)$U!,y.'.,4-'L%.platuthe,:.nl.c $ y f ' ,:.M' ;;~' ' .
UII- I .
'Y . 'Pi.?.ji . ;il)f'$h[p ((.t,,,..yI'f 'd ! @ gf';'.
i q,,,, e < 6 4(::
i h i ./ :. m . ,' ' .
,>..) , ' I ~ Co;. iss'itd hi! NuElebri.lagic- ,
i i? ie [{ .. I
- 0i ..I iv ,ap 3,s .
e i.- l, s. l
;', . , . g. .
n$l3TIL l"J.STbi9 $t)ucture fsiledlas a nul.ser' i l i g .> h c . 'i,- .. i of i oibor s[N$tudes - x,. in Cotabato,
- all 01 the failures . i' I , concret ) si.ructures U ': fs .. . ' '
weobservedwere[ . reinforce
- t. 'ji- ,
1 ratharI.han.jdo'ddii.or'd eta.Etructures:andth l is l buildingidkljichyousee,Lnaerialvieuoffers .
'an excellbn 1)ssan'.in eaNhquake engineering and .;... . - . .t y .
inh'oUtheMearchstructurefailed. Let ce point
- , , r. <
out again that where you see them in we were not more I titan'2 mete bbov'e' 's'eilii#ef,al1'ovek nany rasny' , I i I i alle'd"inlari.(,Iand'The'Yohnd 12 'd'satu' rated.I ' !. hen 'l ,
~ -took the pict'Ured'hsfociatid'Ufth"this 'dh the ground i uas stihdini.j 9 water.'.'Sd,1the. school land all i ; i I
of3he"ot'11er?'dtructtfres 'yodisdE here 'are built on
. .n e unclidsoNhTEd ~s'dthrdle'% .
d irid'.""' '4
.l. .. . :i . 7 ,e,.."G. tru luie,1~ t,iv oack again.
iil .Ivii.fi .,td.i'dij i [ lease brindn]5t.
. ., J .. iwA' not, yea t.e, Lie..: i '
un life left .of center we-fit,1d the difference bet-i 'a l l c .. ii . i .. i t
..a ? di rg ai n.'a 5:n in.1lf at that part, uidch ween t,he appcarance of the roo . ;e: i.ilicia sti; Tithe yu!rd it:
ii . I is different from roofs of,.:.1.m 'ilding en the the bu
- ..k il.:: ' ;! <! ji ; a siit.iil' cit'n ilu .n p right uii:.ch:see:ned t6 be intact. '. hat 'hacpened 16 .
i '. a h U il;. ;. j..fe i ,jf L 1,',X LI;. i l, ilW ti(; .' i l , i i m. i i! ' it ,,. i i,
..it- .l!Ili '[.tl ik. .)., h'rSigl'0!. -
le j'0!; Slit ilitrl! ;t.l; l i .- . li ,
- t .. uqal uj g. 4 - .:yp .
. g. .H u. .qp.
I II *. 'si, . p.g .. .. . . .
,' l tfil!.l! d}itLJ hGt i . P. .1232 200-i
- t .
g.. .- t i,
; p.1 J. :lji ..l li [ Ii' I i . ll;'!'; N Uj . i lj lj ,
Cbd.nis l'lants! .
'1, '. , i, ii' ll;A'l yI.9'h . . ' isiorf f oh flucletc,! C!I4 ' "l';l ' 'l '
I I i)ac.e e 3'.i.i it l 4..:$0 1 in.a. . :i0d . l i, ,
., n , i I: iit ,. - l .. * . ! .: , , .P ;i .. .. j th'is' port, ion.? Le't o'f 'ceriter,r, e ii.ir. Tilfoid. ~
- 10. TILRAS. 'This is the school structure which infactwaEinh,6rogressivestateofcollapse. The
- f tijk'bul9ilig"is'lldun"essehtisliy'on the ground,'thhfroMt.'o'fthe'buildingherereinainsal-most 1/it'acN .The external structure of walls of the .
- . nu ;. 1
' i .I Ir,i un p rear of tlI'lE. btdidirig have been thrown out and are Ifing!ere....' h in b.okeYconditionforthelargestpart.
The next.ijYiistration is a view of this fell struc-
, . v.
ture from, g,,oun! r f.taken, a,t .iao ', cu,t, yhgre,,1,, a, m pointer. .
.K Clr %.,,c @tJ. g t,nessir,efe y,ing to ,tjie i,
right
~
bottom: corti.er of thenpictore. . .ita , , I.:. i i .i o ,i
.cs. , : - - "'i,rl! Tilf0 Of. Nifik'you.u. n a.r. . $i . ,
TIMCii bdib $e*$ k[;thrickt dxlOit. tix- . hi'bki'12kd. Ih ehMIf'Nr5b'"EI,"Mri'f . e e i'ilfard.
. m. q mn i. , cia.n i..m w w ni. ., i . , a 4(. TILFU.,u. llere you see the view 11 proniise . .. . . .ir.tui.. u .un ci.;:o m .o i.x . : .. .
yhuofthiilbuilding. You ilave just seen an aerial
. . : . s u .. y .j.I,a-Ir.;ll.4.li4:3 4 V l E,i pi , ,, L, i , I .ii ,
view. lierdi.thebackofthe. building'isdown. The i .I' ' .' W. y*!.V...itt I .$I'll it, .JWTAll lis!t. . 4 i .i . . , front of tid building remains primarily in its ori-
.ii: i . t. u.. . m . . w .c:a r.cierr u, o pa ginal cond,ition'. The initiating.fai'lu,re in all of tiles'd"sfEidti. .1:
rei 2C8h"5'ai8;' and all of the failures i
.. : . i VI h:t yat:- - ' il}!F.!.
ih.. .
.l -
i ,;, i idid.'. !;'.
.. .iij' lina om .>..1222 : p1 i, } . ! '. Na $i ; Ei: i IM;[. ' j : 1.> l!, Ii i ,, __ . , . Tta n : i *l i 1, Tt! ,g C i ii.! .
I . ...
, . u J . . . ..r . y .I 2 ;g. i..o,wv..joq.:.n -
f;
.,s - *T- .
Coa.issioti3cn :tluulearI'lant;; i 11 July 1979 . Page 4 4:30-3:00 p
,p.,. -J I;
I ,r . - ,;., ,. ,,n-are on saktfr,'afed and consolidated sa'nd $s initiated ls 1 .i .i. bly shel arg,.... !or.bre'aking of the' icuerifloor beam or suhport aythi b'as'e' slab! bf. the first f'loor above.
. o . .
These ai'eF411. generally o' pen strudturisl; t!rf hav
%. 1 no interlifrl. walls and they, therefore, [succud at
- s' .
the top'fjirly easily to shaking. i. hat has hap-
. . + . ..'
p'ened'inf,ci;gny 'othe,r t . dildihgs is that this collapse c .. . has conti.,nuted; the lower floor has collapsed com-pletelyt[iiathasbuckledthesecondfloorconse-quently'thathascollapsedbuckling.thethirdfloor a e,...;. : t u.m % . ,. .,, _. .. ; . f,: ; - which' has'.
..; :. . ....y.y.'tolla.) . . r.i ..u sed; .ni.) iqbuckling .e ny i .the . i . 4th floor which has ..,cio col'lbf;;, -t sed. a. . a:There v. u o were i : n . iin . !excesst !.a of 25 reinforced . concrete: structure of this type. In Cotabato i all .. , . . . ,..i r u ,. ,, sun ..iruci. :. , , .
ofwhich>failedinthe'sameway;e,inthesameorien- n ; w,, u . 4
. . . u . , o. , .... i i, . r .. , . . ,
tation 'And 'in many t yand'in i.u . tthe same L)onfig;uration. c :.iu.. ng. . ine c .a._y n,n ,. cases eople were then livin n what have'been the
., ...a. p. ..p , .u. er g,n aq n.i.g. o.a n ; t, m ,. ; ,.,
roofa(. the 4th iloor and you can step 4.. up'on to it
. .:gli...
p 5 J.:i. T'u1 i. *; 7, 9 bya'heiphialmost'.notmuchhigherthan'theheight '
...i.. ,. . r . o , 2 :.a ..a ce n ; .. d' i of the ., . : . , v .
st' p.. airs..' il n;od,'I u ,,,ii. n ,m , , w'elcome cr your co l and. quest,itns en this exhibit.,;. f h ;, . i I
....p.-.... v .w , tm u.;g a .,. , i , . Tile.fueliUAN., Do cogment.s .from' th.e Commission. .:u dl%. Ih5 or iliou,tilet 'as.look, at what building-
- s unu,Jf.. ..m ri US c.i.e my; h ib. ... -
.i.e I ' pi nii: ),;1., hi. 's m c;f0 fit.!h d ii tq 222: '2 .a
_ Y . .j . l.) .I I.
,y* .* . E
(,nl d g. *j es. l 6, ~g ,'i, f ,
.8 .
l YiyA43iml,.ip.m mw>. ,.
,y. - , c, :<. -; , ,
i ~M - - - . . . . .
kr;l. . Co:.wission,,,pn delear Pl' ants ' !- ). 11 July 197R PF li d ' . v ' ' h 'i -
/
i Page6 t.Llim:, Pd .w.OO -Si ,. ,
. .. . y t ' ..r cs.'i-i .+ i . l. " ..
4 ,
, i lc ilt it y.t i..>
i . i;; -! .'i ilui l. ..q.il.' il M l.' . did not a s l'r, Cotabato in this earthquake.
- , l .3, , . .. . - ," THE ClldG,iAil. liark this Exhibit 13-NPC.
yt - lU. TILD)dil. , The illustration and I could have i
. . ,n .. . ,g .
i picked,any%fseveralhundredsofphotographsi j ra j haveofwoodsnstructureswhichwereessentially
.. .M+3 intact.show,s' dram,atically.therelationshipbetween typs%'fENtructionmaterialandresult. (Point-y ,
r .. . .. . , ingtoach_,u_rchintheslide.) __Ihis is a church in r . Cotabato and;the main section of the church is a V: . woodent cbns'truction.thit'stan's;.'jne d ' entire remain-vu dee pt i,he'.;phurg,h e,xc.epting t.he.,d,9,or joist are masonry and. cement.'61ock. None of themu,. stand. The door
.. i ; . .;.:.. i... .;'y :,. 1 . :i .
joist for the front entrance which is of wood is
. . . . i . m .. ....,. .j.:a in . :.. :., u., .
intact. ikiF, it could be ; argued from this' photo-
.. . i s. . ..,- .. . . . 2 .i.. a o s. ....
th grach
. , y u on,.b,...:is ,. . .r . . situation,y. .g.9 , # p. at o. we u i should 2 . a> build l power nuclear 'pliints bf.kobd out I tiiink. probably we have ,i,..,u..-..
i .
... # . y p. i.n. i a i .a a. . , . . . ,
a fir'.e. aprobl'em.':q' n t. m. n! :o.) ue: .i..; i
. !;99., lit me:'maka; wha,tt .lcgo.nsider tg _be,.the most dramatic pgin.t_ ,to..be mape3,fr9m.,a s,t,udy, .in that ,of t,he resul,ts, dfd.he_ Mindanao . earth. quake iinpugustof1976.
The, failure.s'you see, an,d I;.could have shown you, if.,- .
.1- 1, < t.:.. .
s p*,s s * ' n. . t . a . ....:: un ..o i I L. ;.I} t *, i UL..- .tf. f *;: I l l '
.. ! e 8 .* 6- ' $),
s L'.,$$! g
.1 . $ ..d g. . I * ') . .mj ;.:mi 'n 'ar.t , i.i i 15. . . > .. . : . ,o ,
I i 2 o . rJt.: .l .r j ti . i i: ij : l i U.: i i :, , .
- i ComissioI', q ,Nygl' ear .'lants ,,, g'. J m f ->
.llJqJy'ilE7 1 ' '~ 'l l CY / age j .ip.,,. 4:30@:0d.F' ;[bb1 UhLah ~
j (: , . l 1 lI k
. . , -t : . .. ,s, . . ,
W-hundreds iigef, Those failure occured'at groEnd ac-qeleratiori,sfof. . 085G., .085 less than 14 of the force ofgravity,','.l.layIremindyouthattheBataanPlant is designed'to~ safely withstand and operate during an esthqu'ak[hoddbiriflyoun'dNadng'nle'asured i a 403 ofallacEkleration.!Thesefailuresoccursatless than 1%.i This plant.is designed to continue to functian.'through.. strong.phakinginover40timesas strong'as the shaking which fell these structures.
~
Y' cur comments or 9tiestions, Mr. Chairman. JUoTid$fB$TibTA. :. hat is your participation in the.paking..,ofthedesignasage.
.,.. .,. su . .... ologist? .t > ., ,
l'? ' S
' k,t,.eTILFO.:0.J . lie par]ici, late very strongly in the delectionj.bfjthesfte;'in'inestudiesrelatedto , ,, 1.i- ... .ty.. , ~ provisir+ bf watet'..su,aply; .s'ftidies ,related t'o geolo- . p. s..n . t .... .. . . .. . , . .
gica,1haza'rds,, earthquakes.volcanicactivitiesinthis case,'landsli'es;slopefailures;sinkingofthe d t]rou' lids .asii' things of' thaFssaf.2"i..e"liave" absolutely r,w. . ~. C. . . . . . . . . . . .i.::, i e . 1 ..: .l.3 nothing to ,do with the ' design of t{1e pl::nt beyo.nd.
, , , , .,, . .. ....t,, . .. . . . . , ,
establishing the design condition, j .; i , which we du in
.l. I E , * ) ,# t is I,. .
specifying..thetearthquake .r.10,tions,, their strength, their durs'ilon, and their. frequency cunten,t and at
.c . , . , , , ,
that point ue turn this facility ulth that .,,# earthquake i;,. .i..p workingprf.itsfound.ationove._rt.othestructural
. . . . . . , , ..- . . . . . , .. ; ,y , . .. o 1 ,
1.., i... 4rn. n .ii. :,i:', ; .; . . C,i c,.ap ;u , .i . : J. , I;. .
, . Ij ll: 4. :ii ti liFC:3, , i.:..,. i . p .,,7.. . . .g . .. ..,. .. m : :..- . ,.. :i y w :I . : :.!i : ..' , o .
i: ..
, e ,'n.; 1 2 2 2 ' 2 0 4 .. . , a p r . #. p ...,. 9.::. w ..
i , i ' . , . . . i 1 , Comission oduclear Planis . 4c N" " 11 July:1979f;I>.V 4 3G ! Page J,....1.:ag,p.5':00
. ,;.ju . ri:cc p.c. m.q) e >:- ; . dd h vib..h. h' ,'ib. .J s; Nl 3 g.r m laf, I.!. ll r.-
i i eng!neers d[a,'.de' signed the plants. , l! I e.: e . ., , JUJTICGlAUT13TA. le woulo like t'o be clarlfied what yo me n.'.'by the $atadnbeing . Pla designed to withstandt$eho~rizontalacceleration'of4.0G? ' 0000 D lP ]filkNIlL. f, j ' I d u ll, OUniD l.!R. TILFdj(U. 40%ofthegravitythat4.0,if Imistatedft.'myself,I,am'sorry.4.0
,]J03 TIC $,s [hE How can you say that the plant to beinstallef,isinBataanisofthatkindwhenitis . y. '
our underst'a'n0in'g that it is'a' typical plant, it is i the 'same blarit tfiatthey put uianywhere irrespective .
; .. s I
ofgeo}ogicdI,bonditions.t..:u!u,.... .. L i ,
!IG; TilldiD. .YI havo.. imposed upon,th,e plant de- - sign'foi' 35f'.lof gravity', the' des,igner 'ahd constructor of the pl'an[has' elected to construct the jalant'to a . ...1 value of.401.of gra ity or 4:0G; 1.'can offer you no i .n ,
assurances. of'my. personal knowledge'that tiiis design ,
. . , . . i. e ,
conditi,on'is:.infactmet.,Ican'tofferyouas-
., ). ,
surances thaty.the establis.hment of.the design cen- , ditionhas'bWen-done. safely:andconservatively. '-
. JUSTICE yAKt!EZ. Your recoumen,dation is supposed .s.
to b,e translated b'y the maker of the plant as part
.. V "- ., .- .t. : t: .
i $; i ,
..g, .t...+ . , t. . q..- : e n . o. ..
222 205
. .. . . . ; f.> n .., t ;. i is i.u.. i i i.
u r.f. p . fl. .,._;.. . 1 . s +:. ..: 1.:t ..
,i!.i.9,. p h. i r . ... ! :i: i .l .>
I !- ,
s o' . ;
. :) ;,.. e .y Co=iissio4fbnlideletcelanta " '
11 Jdly l$7 l ' ' ' l l U " . , ' Page 8 :,;30,-5:00 @:.9 ! l I -[.f] '
.r' ' N., b' h [ 'd'I!,
G . of tha' %ggn .ofithb; pl'aht;itself.: il . g l,, j. id. 'T %F0.l0. I Tha 'is> correct 'and a y ques'tions on culd'of course be'propebly the de,s.igh.ffof'the plant s addres,sedifothedesigner.
,I t-JUSTICL'VASCUEZ. do you, for instance, say or j tellthed"thatyouhavetoaakethewallsasthick
- 7. >.
asameteriorseveral' feet.
-,, :!n. i. :
KW.Ti,dFGdd. l10, sir, we specify the m.otion that that planKr.us.t withstand. Itisth$jobofthe strNhtu'raie'ngiheeIt'ot'rin'sYat'ethatmotioninto - a design"flii'chlis safe under Ithose conditiens.
' :0-JUSTip5VARUtiZ. You'do'not tell thei exactly, what' tid 57..' . r c.
s k TILFuld. ilo, sir! -
~ - ; . . .. . : . : , . 1.a e . JU3Titif.VjiS:fdEZ., .aAre you aware, if your reces-mendations.ihave been follot:cd in the pr.eparation of
( , . . ' ' . '- 1. ,..,.: .: . i . ,,. l thedesign~Tof'thedataanPlant. . i , iS. IlLFU.'0. I aja s,or,ry,I don't, understand tne question.;.g ., ,,,,, .,
., . ,1 ' t JUSTICE V.iLiiEZ. )'oyri;r;ecomendation .
about what-
~ , . ,
to.dn.in neder to eithstand an earthquake of that
- ...w.
,,, ,99 .c 1: . i . . . .Ii : u , n .n L :., .!
; i ;f ' i . i n ,,, ' ij , .p ; j,i: ,': / f . . .p,'., , I ,' , . , , [ f Cod'ilss'idn'oit lluclear Plasts ,". I ' " i" .f. fp 't '
11Julyin6f'" F '~ '
,I Page 0 J;4:3d-5:00lj'" ;.
a I ,
!l, I, 4 ! p/., 7 ..- ! ,1 I
magnitudd.4 ,
~
n' . In this instance, our company is
'id. TILF0J6.
c'a'pable doing what we'do plus design the plant plus build it','plus l operate.1,t, .d .duj in this instance I t
-, l ' I l .J we have,Ifane a site reldted.s'tudies; dafety studies andwehjve.'establishedcertaindesigncondition, and one of those designed. conditions is the force ,-let's , spy:for.ce of .the earthquake that the plant e ,must be - :,
desi5 ned to withstand. 'de turn. that recom-mendations'and those criteria and conditions over to
. l. -
the..desi,gner .u, of the plant
.. . .. .,by . -way. of the L'ational Power Corporation who'.. participates,, and . .. . . . . . . , reviews and approves those condition.s. .The designer , . , .
of tM plant is the one who decides h.ow thick the concrete' t_ will
.,c,. . n. . . ..g.,
be; how mpch reinforcing..,steel i we we are going to .....
. , . . .. . , t .._.
and so.on.
.. oi,..g.,That . .- o . .is , psubject , .., a.:,u . oto review by the ibtiona I'0werCQrporation. ,
- t .
. :. . . t u.. s. .: . n . .y is.. .: 3. ;. .,
TilEJC#,l.,iM. t . '.ihat; Justice Nasquez, I believe,
- i. .I
,wanted 'ta a,sk is did you achech,yheti,ie, t r ,your specifica-i .
- tions. and _recp.inmen.dat, ion,s , sere , carried. out in the
.gataangNu.gle,ari l ?lar)ts} ,.tict,.alc g .,; . , , , , . . . .c .
grM.illLF6RD.i.4he;rsbnallyamnotqualifiedto1
, 9.- ,.
- u. n: ma.. ,u Sa. . an pc : l, iip. ;.f : ; u :, .
l
., 8 *[j , .;[ I (I b.,) r.tMl b$ ' O . ,. t- .
i
- e .,I.' ) b'. jt2 {. f, Ij's jbC , it' .fI g!. I g ., ;j l g .ie.. ng.r:.t; .n. 1222 207 Tir.,,m:,t.:. 'ig u s e .. q . . ,
, y-l , 'en; '
Co:mais'sion bt nu' clear clantc. 11 Jul'y 1970;,' id ,' ' Page 10 N:30 .s, .. n
.. . g .;.-5':00 p. n., . + , .,in . 4# P 61.op .n:. i .. - .rd a. , !
i
. i i .
judgewheththehlantwill,hgntinuefofunction. '
' IamnotqNNiifded.
p' I i n illE dij .dli.il. ifr. Tilford, the, question is very i I . . $ k 1{ very' v'eryj ffip1'e... . You laid d. .ownjertainspecifica-tions. Voi)3gave various recommendations. The only
.1 t-question 4jdi,dyougotheDataanPlantandcheck, verify whe'.ther'these specifications and recommendations .t wire'in f ci caftied ont?"
t
',il.R. Ty0.'0. Given~ a way the question '
is put
'" N @ " ' '
the answeri!is "no".'0' W ~ IIE bf.Ml.N 1.'ould you want to explain your O ' . l *' i- 1 !! -
- M' '
.ansv$r?' I '$Y . '
Itisl$pocsibloformetodeter-Iltt.TIlf0d0. i mine if tire' recommendation is beiay followed. I au
,.i assured b ;the llational i>ouer corporation, Westing-house,'thith6se~cecoddendations:are-implemented.
v.. , But I per}6nally an inc6mpetent to determine, if theyarebingimpleuented.s.:,. Tile C,1lAlsilill. Did anycne in your organization in Ebascoij'+ccked or verified whether ,this recocaenda-tionsand[specificationsarebeingcarriedout? I Z.1 Iti. flLF0i10. As an;experi.and not an official
,rc = . . ~ . ... ,...,. . 's. io.:r . ,.; , - {. , ! I'.l.- . , . , f p. : 4.r ,' t-s - . : w. ..' .1,. . m..w, 1222 208
; .'.f7 't 6 )I-
- Cor.uissico :en Nuclear Plants i 11 July 1979 ). ,
E 4,::d-5:00 p. a.of
, t Page .11 '
f e, :,: I, i ;
.. .. .' 'l' , f "' k l , I , ._
i ,:p,f.. % . ;
'l ,r j y .
of11}0coppanj.l.would defer ' that .iestion I to seg testi ' as an o,fIicial of the'capany. w w 1 ,.a j
. "n . ip.
u if II,'thehuEstionis,hetoce
;, t
[. 4 TdiIs~j . . .
ther[ ii,I.Ynys.,, ..'; you etnjustidentifyif',,the,re
( . (, 1 m. t is anyon)!.'sho did gake that verification and th o. checking',:! .
+
Md.WILF0isu. I personally am not able to make e 'thatde.l'ermination. Is there anyone in your panel Tile.CilAlibiAN. e , No one can who carf bnswer that question? -(Ulene) -
- .5 -
Nobody present in this hall,
- ansuef,that question. I anyone,inot present in this hall who can ans ' que, sti,o.n .from EdASCO.. .ht..IIEALY. ies, .i... ..i 'TNE.'CHAlfWiAll. The answer is "yes"[ lhe a giveniby i4r; liealy.. ;tiho.is that . person. Mr. H !%' .41Y. Mr. Co.missioner, there are three peoplf(here,on'this p'trel from dbasco~ and ' Tilfdrd the~ geologi'st:and he has already given h explin,'ation' of his understrinding of how it ge tran5Iate'd. The oth,er2 person is,Mr. Jam.es G .5 1 None of the and myself, .1- am a project Manager.
s ., . I d i .,
.,'f , e
- .> an . .
- r 1222. 2M
- - - - ~.
U ~ ~~ .
- 4.-' . ; . i.: . } ' . in.i. f. ' .!., , . . l..'..! ' . 1. , ,
- i. . ~
Cos.tissien;on Nuclbar. i'lants. 11 July 1979f Page 12 : .~. 4:30-5i00 ,;p..b:. . . i , ' '
- i. ,
i . .. t- i
.t. i .. . ,. , 4 . . . . .. e i 1 ~ l I i ' three of us., and I believe_t ,liati l. speak for Mr. ~ . Gil5/ ore'.' .
I
+..< ,
i ; T!iE ciiilMM. Is that correct?
'lp - p i . a.
l 11:3. GILUiiE,' Thatisjcorrect. TiiE,'C!lliisl,AN.
. , .t '
Uill you repeat your cnswe . Gilmore?%
-.4 . - .
y g DDgy [jg y q [ i UUd UEt ,Ll HnL , ' > il.<, $il ;6!<E. .
... .i.That ,is correct.
i'i.t. .i.iULY. None of the three of us here can give you a stMemen.t a .. that we understand f.roa personal kno q
' ledge .that that was checked.
I believe that within
' Ebasco tIEt there are people that can give a state-ment,on$ hat,'buttheyarenother9now, i L:. '..ho are they?
Tild/ditil.dinil. .
~
lit.M_ dl,LY. It Uculd'be sode'bo'$y froa the enginee-ring side' of the house, the name of the person is very a, diffico.1,t for me 'to give 'lo you right now. p .. . i de dill give you.your table of Tild, .v iia'liaiArc I- ; - ' organig.atlon, exhibit' ..'..;..L i , :. 1-I.i.iti;ildALY. That will not t' ell us. .
- 3.; - .. . , e . . : .
l'orhap ,
, i$,('UIN.t;.it. , Lycuse mu, Cummiddlunor l,
situation ,a little bit. This
- 1. cl.a.rDy t.h.e safetyi i .3n. q,.:
. . g. ... .i . ,
- 8) 'd .. ..s
. 10 ,!
g..
.- . _ . ... _ ~
b;'; n;.. i .p i' : i] ; v.5 i !! .. ' 't .i ' I 3
. .J 1.) [j t' . D . ., f : ' i_ . h d.i[I-..E i
I s- , - i
' :i . / 7 '
[, ' Commissionfopl luc 3ardiants , q'h .. 11 July 19]9'. 3 4 4;30-k00j p.:m, Page li
- r. 4. ' -
] ,r .,' , .,3:
b organizati'd1 cliart'is the organization cha
. 1 '4' .
Consultan}'s C vil ggineering Group who are Studies. The organiza-patin'knjiileSite03dctio i no' tionchar.t.ifortheentirecompanywouldbenecepsarg to icentih the group or individuals who aight h , As a co'm-partic'iphjdindesignordesignreview.
.pany we dr'e divided into departments andlthe f The departcer,ts have different responsibilities.
Consulting dngineering Department selects the sites n .. for all jypes of power plants;.aestablishing design - .
.n,, . 'criterigetc. The design Engineering departm the grou'pithht is responsible for the actual design . 6- - of ti.e buildings or the review of the design of the t.
i buildingsifthat,isacontractualobligation. 3 Tils.(CllAl. MAN. Uo you mean to say, iir. Gilmore,
. that this table of organization you have uarked h -
hibit 5-ikC.is only .a.part of a larger table of or-ganizafion? . .. M,0 GIU.lWE. That is correct. .
.e ' ili(CilXI AM. ' Add'Tn'ih0Jlarger tcble of or-i ganita,fion.'you wbulb HSE [c'eRaini,'officiels , .. :- ge: hvp , ip . . y ! " Ti k l' . . i ..
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1222 211
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( 9., , k 4 i Commission on !!uclear ' 'lanis " ' ' ' 11 July l@9 f i* age 14 . 'i 4:'iG-5:0d p. u. a,, . . i'. " that wouldI.go r. liigher up'in the hierarghy of : echelons in your orgadi'zation.
- f.!
. na.. Gip.0.',i, Thelo.ther, departments that I referred l &
to, lir. Clpirmarl, are in a parallel' level.
. k.:c Tili Cll.{ld.!'Jl. Yes, precisely, but they are all 1;n united und,er a higher authority.
i.id. G!iiu.,>i. That is correct. rr.., THiCh.iliJ.if61.Uell,whatanswercanyougivethe
;. t.
Comissi('now. Areyou.justtellingusthatyoudo. not knoulllfeth'er there has been a verification and a checkonkhofaithfulnessoftheconstructiontothe . it
. design an Crecommendation that 2basco made? .i . !!.d. Gib.bkl. Ebasco iias a contract with !!?C. There -
a;e very r.any groups in our company uno are uorking
.. .. . . , . . . .i, witn eClin implementing the contract. The questions 5, 6, and'T were designed to address the i.iindanao earthquake,. faulting, seismology and the depa'rtment that ,I is responsible for those questions is the departmebt inat is rc;:cesenting the company here today.
w Tild bl.\l.t.iu'i. kr. Giliaore, the point is statements i ., . ..
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t.
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Il ( .. i 712
.i . .< m., . .i . .,c. .: . .h . . . : .3 -.. , i .
I It . Cor.:.nissi$n on Nuclear Plants ' 11 July.'1979. ' i 9, , - Page 15]i,',- 4:30 - 5:00 p.m. , o
. .i ..v, .w a e hen G at d h se voicaM c aN sdsd e .a O Q a!
l phenocena;have been taken into consideration in regard
; r. l - to the design and the r'ecomendations of the Bataan i Plant. Jhat 'is clear.' So far, we have been told that i ; h -
3
?r ,)'noneof;thethreegenteen lbhere made any check or .' verificilion to determina thether those specifications andreco$hendationshadbeencarriedout.Andthisg..
isaskik,.kasimplequestion.Wouldtherebyanyone ifyout}agnotspecifyhimbynamecanyouatleastspecify. j hici by {!ie Office that he occupies so that we can seek 7 his statsment or testimony regarding this very important 0 point. , ,*:!
- t.
l/Jl.;,GilSORE. For gyself I will have to defer that toI!r.IlealyandtoNPC. Tile. CHAlfdIAN. .Does the NFC uish to answer the. I' questioj.[
?- . IG.;T0 TIRES. I!r. Chairman, ) art of the Ebasco consulthey services for.the NPC is a design review.
This is< service perforced principally by the engineer-ing group of Ebasco in New York. And this is the gecup
' that had.',ldone the checking. . ;2 . - e .1 -
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Comission ljJuly19794 ch, Nuclear Plants ,)gp)i[gl3,Og n, g,gg Page 16 U4:30-5:00 . r, . . THE CHAl.. IGN. So, there is . group that checks? i 1 la. TOR.RES.; Yes. . i THE CHA!RIMN. Where are they? I'.R. JOR.3ES. , Theycareb.asedinI,leuYork. THECHAiR!aN. In Neb Vork. Ilhy are they in New York when tha pliat is being ccostructed now? MR. TORRES. I refer to the design because the decign ofthisisb'd3ngdoneintheIJnitedStatesbyllestinghouse. Tile CHlifd4N. Yes, but Nr. Tceres, the ddsign in regard to the$ recomendations cnd specifications have alread{ . been submitted by EBASCO and actually. these designs are supposedly being carried out in the present construction stage of the Bataan Plant. Is , therenoEbicorepresentativeoverseeingtheconstruct-ion to see t;o it that these specifications are being carriedout? . IS. TORRES. For the construction checking that is
.n being done at the site, I refer to.the checking of the i
designby{b'asco, THE CHilR!MN. So, you have one Ebasco man here.
!j . :- : 'c . 1222.214
Co:.taissid,n on Iluclear ?lants 11Julyil7/9 Page 1/c- - iL 4:30-G :00 p. u. n-a3 ! IpQ c q i L 1.sb,u;n Uct , h i': . ..t l.'!t 1 L i l
. . 9 0...t ,. - ..e also have 'J,bacco a n here.
{. ' Tilit.CH.'. l . .!'la. . .; akin. 3 the verification. iUNf6a.C.Yes,togetheruiththe100. q ,-
.s TildiC.11Ali:,.Ali. !!ho is that ? llho is that uan?
i.:R.i:T0a.C. idr. Les Elliot.
- 3. -
4.- THEiCilAln..m. Mr. Les diliot of dbasco. iiit.';T02.rds. 6f Ebasco. Tid:CllAl31!.i;. lle is in the Philippines? iM.*iT0.ud.,.Yes, sir. If!!.'CilAlis.il. In Bataan? iM.[.Ju1IS. Yes, sir. - T! E CilAl i:l.ii. Checking uhether these specifica-tions are_being carridd out? iik. . 16ttaco. Yes, sir. - Tild: CiiAlha.;l. Can you. bring hDa before t.iis Con-mission? , Md.,TORdiS. Yes, sir. Tild CilAl%iM. Please do so. Thank ;cu. Continue. ii.; ,,fll l. N l !!clifi! } II;d lf) (;l'ID Ti } Illl0 r-);iflfl-
. . . . . 1..i; ,,
122~2 215
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Cc.aaicsion eq'l!uclear Plants 11 July 1979 -l.3.130-5:00p,.a. Ppge 18 , p represented.',h,ere are the onest who mak site and dc[braine the periceters as they called This is a pbcification on uhat is the earthqu the plant jliould withstand; and what can the site a[1ktherefore design the plant in ac uiththeihlindings. !!ou, the design itself of the plant is ria.'de by the engineers of llesti United StItes and that design has to be c by Ebasco to make sure that the design Now, once the design is completed, cons-the perirfeter. And therefore, again a revieu has to truction!.begins. dance with.
, be made (hether the construction is in accor It 'thisdesjdnandsotherearethreestagesthe is not caly a two-stage affair.
IllE Cl! AIR:.iAtl. Yes, but uhile it is bein ed sor.e Ebasco representatives is there these r' cow:endations are being carried out. i Yes, sir. And also frca PAEC. 13.';TORRES. IllE Cl! AIR!.!Atl. He avait the pr Centltrn before this Ccanission.
!! ark this neit diagraa or sketch as Ex l
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w 1222 216
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I; I ' ,
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3
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l I' l , l l-Cor.alssion on I;uclear Plants ), 5l9f 11 July 1979 g j. Page19 f.4:30 - 5:00 p.a.
) !!R. Tilf0RD. You have seen that we hav'e scientific-v ally dividad Luzon into appropriate segments ccncerning l -:
carthquake: activity. We have ccmpleted an exhaustive de-ter inisti process c which is that process uhich satisfies .
. }herequ'Irenantsofthe'U$.. NRC in establishing the ac-celeration value of the design safe shut down earthquake as it is called. A way of checking this deterministic talua-tica is to an attempt a probabilistic evaluation to see if the recults are comfortable. In such a process you study thehistoricals,eismisityoftheregionyoucountallof thecarthqdakesthathaveoccuredandyoudeterminetothe extehtpes'sible.theenergyreleasedduringthoseearth-quhs and keep in mind that in the Philippines you have a record t at is longer than 400 years aid that record is alcost Etdice as long as the record 1 -t is available tousinthhUnitedStates. So , using that 400 years ' '
of record,',' you can establish the areas uhich our earthquakehprone an'd you can 2 raw that is called a least jquare feet computermeter, create a'drau-ing ubich shous contours or lines of equal value for certainfrieselecteddata. This is a procedure authored b'y a scienti,et of the 0. S.' Geological Survey 9 n
- e. ,
I ( s .
..9 -
1222 217
g . .. IU t , I Corissienth:ntuclearPlanic l 11 July y1976 ; , Page 20 hI 4:30 - 5:00 p.m. IP i i s s ., in 1976, a0d un have essentially follouad his procedure
- 1. , .
in produciyg; that ue call the seismic risk cap, which is projectNJ before you. t!a can make this as complicated i or sieple ,$ ue like. Let's icy to keep it sicple depend-ing on you{f.huestions. In bort, these contours or lines shou the c:Eg'nitude or values of acceleration which are to be expe& fed in this particular locations one time in '.he next 10,00b'. years. The maxitu.a value of horizontal acceler: tion of each arca or point that vould be expected to occur one tiaeinca?h10,000 years. Okay? Ilou, each of these little squares ha{ a nucher and that nut.ber represents that acceltra-tion value'that we uould c::pect to happen one time in each 10,C00 yeaSc period. For those of you uho are further away including unfortunately the neubers of the Commission, grea is good, ul!ite is not quite so good; and red in general is pretty bad.l'j The acceleration that this method predicts uill occur once}ifach 10,000 years at the Bataan Plant Site is .E Let's compar'a that ... I;E CD.!PE!. Once every 10,000 years? L2. TILFORD. 'Yes, sir. gk.' e i4 g
- . i .
I , 1222 218
- 3. ..
30 e',' CC!0'IS310:1 Cf i UCLEAR FLA!!TS 11 July 197h'b
?
Page 21 {.4:30-5:'.00p.n.
I Tile CilblR!'.AN. E n did it last happened in Bataan?
113. Il! FORD. \le don't have any assurtnce as yet that it hasie'ver happened. The procedure uhich ue follcu-y ed to produje this evaluation sitply predicts that this level of acceleration may be e::psrienced once in 10,000 ye:rs. This is another way of saying that the probability of the occurence of that acceleration at that point is about 99.5% probably that it uill not occur in any given 50-year.perIodl... 4 0 0* em 9 9 9 S e G 9 0 m 1222 219
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Cdmmissiop on Nuclear lleactor Plants 11 July ;1979'- 5:00 p.in.
%t 1.'l ' '?
L
, MR. TII.?ORD.
c.#liave'no'informati n, there is no evidence on the $ Lke or near the s'te that it has' experienced
- e'. i. . .: s.
extreme.'stron'g motion in the past. We were satisfied u. as geo16 gists will probably have in the past, but thoseekidencesarenotavailable. Mr. Tilford, in the course of
,TiiE CI! AIRMAN.
the int'erpellations before this Commission, it was
- -tadmitted .that 'thei' life 'of the dinnt before decommis-sioningaor recommissioning would be from 30 to 40 .
years..You'just mentioned that you do not expect any such' upheaval within the next 50 years.
, g i. . e 1,.6 < > 4 - - .
y,.TI.LFOR. D.. , Fo. r ,t.h. .e.. .re.c..o. rd, I wc,ial d ma k e
,MR. .
c it clear, ,tha,t this is, a ,gzjaph,of probabilities el <cceded during
. . s.howi.ng . . .. t.h.at..,.this va. .lu.9 w.o.u.. ld .n.,ot bc. .s . anyi .50 y,e.a.r , .pe.ri.od ,a. t.. .- t.h.e. . :le.v.e,l. o f co. n fiden,ce of 9 9. 5 % . - 3??!.cep.,,ygw,,,,that,fs,th3;samewayofsayingthat we expect that this cyclo experienced 26 por cent $r, "tr.3 , sis :: '. i i : : , ,, , , . .
seisniog'raphically once in any given 10,000-year
! * .P.. 4.at 7. e . . .# 1. . 11 s t. s' s- ,
period.4.. .The. exhilaration value is .4G. We are gr a M t if
- r '. : .t* e i t i' r m. 1, i i . ..
saying'.'that' this' indicates that this methodology
. . ( ' l .: . 7.- ... 2 i n. o : . . ,4. , . . .f 8 i.
sh6w'th'at.it may expect'about 2/6 once'in about *
.. . i .i . . Y [.r 10,000 ' years:. tihe deterministic approach would, af ford a i , o . : . t i. .. t , . .;., :. , .'. . .; 15 ., . t t 2 . imr- .u... .(
a corisf'derably established value of .35G. So, ;
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- l. 3 Comiiss%5.*nis Nuhloar 'Deactor Plaitt.s 11 July 4*J79 ' . 5:00 p.mi j' ,
I i fg -)g. ..l w M. , . .o e i; 8 q 1. -l . I 'l '{
. i -i i ,t-.. f, [,. .within n !.
tM ;leve is we are talking about the deter-l
.. i ministi %,tho,d and probabilistic mcPhod do achieve I Il this obj6ctive '
of check 2ng onc another. Por i your information, some other values that this predicts I
.u once in 0,000, years at tlanila about .34, the highirat y .p . . ' . I -. 4 values ti,n'this, graph are in excess of .5 may be associat'dd with the active faults particularly. So, a
within C'entral Luzon unless you go far offshore up to..th.e. China.Se.a, the a.rc.a c.. lose . i i to the Dagae site
- is on1t ,,'.'the of least at risk frcm carthquake hazard which 1s;isimilar to an area norgt of the Zambales range Stitch is also most likely to feel a very
.s 't'r'b'n'g ' o't i o n.' ' ' ' ' ' ' ' ' I ' ' " 'J ' , - . . .cJ ... . . 4 a t 1 ; ai;: <. .. L e. . . i i . . . ".; ., filt' CH AI RMAN D . That is very= good, Mr. Tilford.
t t. a . . . n.. t .riJ . . . . . i s .u,, c :..: :o.. .a Dut now,:please answer my question. Will there be
- i. a .. ii. i- . . . . . . - s .1 u. . i. i . : 2
- an earttiquake or any uphe 2 val of that kind within *.e. 4. . . .e' . J .. . 3 2 ..a t the nexti '50 ' years? ... . ., ... .i , . . . e . .M. .- R..'
TII FORD .
.I.t .i.s e.xt.r,eme l y improbable. . . . . Ti1E CI! AIRMAN. .Not : impossible . You cannot
- guara'ntdd., it .. .a . t . . 36. .. .
- ~
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ar'e 'leYe s - oY 'probabDit'[or 'l'iNIS 1ood. J It is
- f,.
. . . ' . . i. ! f . . . . .a.: r o .s i 11Aeny a unlikely'in'tiin extreme that any strong shaking, J r . a. itu .i not to gention 40 per cent of gravity, will occur N's.; J .o...- ..!.11 112 .. ,, T. . . . t 3.. . m - ' . I/
pelt it. /Er.- 1. i '3.4c air Li.E t ; c,* liJen.1. l. . 1 ,i < i ;"- . . I 8- 4 0.E3 A 's JJ ,I C Is'f I pt.ea Val ! Of .l ,
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- Cotiunincion .oh titicload tusaet or l'ktintu i 11 July 17b - 5:00 p.m.l , ,
fe.yt 3..',,*". i .
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~~
b1 - g lM fl T11E 4CI! AIRMAN. Contr.arj to your oppraisal of , t>cobabilftiesand.pessibilitiesthiscarthquakeoccurs! l l within the. expected lifetime of the plant which is 30 to 40.y~ cars, Yhat liability would,EDASCO under-
- t take in vi,cw of the , assurances that it has corr.mitted itself? S I" .
T. o MR. I,"TILf 0RD.There are two parts to the answas
.. i tp that que.stion.' One is the part which would define what it mean ..J t.* 1 by the spread of waiver. If the spread of waiver you mentioned *is 40 per cont gravity strong ,
m.o t.i.on t. ha t is the.de. fine.d safety.. shutdown carthquake 1 .... this requires that the plant be shut down for examina;
- as s" .. , is 1r i v. t .is y ; :. .
ti o n'. And there are requirements frankly which we
,....i . e si .2 ... . i i . i. 2 . . i .,a .. 'are not terribly committed with. Then the next part . . . . . . i....- .
pte . .2is a l.
~
has to do/with what is EDASCO's liability. And to
. . .. + .... . . . . 6 .. , 1 .I that, I would sp.eek as an expert and not as an official n . . . . . .
i.l .^ ,s . . of the copp,any. ; ,
. T!!C CITAIRMAN. Who would that be? .n .,, . , d, n' , :..,, s ::: .i.4 g I don't t 6. i MR. 3 '.' TIIT.ORD. .. . .I can.',t te.i l.], you.
i. e consid,cr iiikself *I {in, a,,fpositpn,a,s,,an offi_ cia,1 of the a a , . 4n,, f ac,t ,I(, ,,ng :,nu g,jg,o,f(ict.r but I can tell
~
comp,,ny. ,,
..Y0tl wha,t,,pur cgr),tra,ct,!,llabi,114y, ,is. A,nd.our, contract . liability,,j,s rq-perfprma,nge qf the wogk ,and not con- .,s.. ', . 4..e . s i . 6 .i r . i,i . i i .e . - 1 i o ..,j. * .; tin 'i,.5: ,,j b .i... t , . y I ..o i s . .. .. . i p . , , . u . .. , . . .. c.i: u:o., ii. i. .,, ..o.e .-
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,., ,s . . ' l *ll Omwincion c',if.flucleiar itsaactor Plant.s l1 11 July 19)h.- 5:09 p.ta. . ;lI
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'8 ,
sequential d'apag'c. - !. l
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Tile ,blhIlihAN. In other words, y,t! will not ancuer if a damage occur as a consequence of an carthquakc* . . ,. a q or. .a similar disaster contrary to your
.J . . r prognocticatitir st.' .,k ,i.
That is correct, unicss there
. )1R. '1'ILFORD.
is someth'ing.' wrong with the work we performed.
.e . , . . .s Are we through with . .s. ,, TIIEfilAIr@AN. .Thank.you. t .p thic graph 7'.'
HR. rILTO RD. Yes, sir. f' Tile 'CI'! AIRMAN . It is 5:07, so we will adjourn
- 3. . : .t.a-We still have two panels
- up to tomorrow at 1:30 p.m. , .,
r c v... an 'd .EDASCO panel. We
.' . .-'u on tho'.es tand;s clie .Wesk.ing s ho.use wil'1 contidho 'Eith 'th'M NDASdo d'is'serta't'lon and then .woifdback,YothN"WeYtinljho's'Ifor'tho'contiriuation of 'tilin' TaTUda liitorpe11ations. , The:.sosnton was adjourned at 5:00 p.m. ;r: . . . . . .... u ..t.i. t : . i c. g. ' 4 . , . , 's' ' ,3 . .,-' Tor the T.r..ans.cr. ; .. ipt.: #>
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1 i 12'22 223
1 UBLIC CF THE Pl!ILIM INE 2 COMIJSION ON t UCLint !4.CrOR 1% ANT
'(( f hg(\
thilippino International Conventien Coe.tcr Building Metro M: nils TF.;J:303IPT 0/ THE ST130GRAP!!IC fiOT A.3 TAKEN DC,eN DURING Tlis S233ICN OF THE ALOVE-L1' TITLED CWJIISSICN Br/CRE 0:!E MONORAELE RICARDO C. PUNO, CEAIIC'AN, HEL3 ON .nJLY 12, 1979, AT ROCM 4, PICC SUILDING, MET.10 MANILA. h*WaB PA:3E*it: Hon. Ricardo C. Puno -- Chair an Hon. Conrado M. Vacque: -- Mc=ber Hon. Jose G. Eautista -- Member . APPE.tR ANC E3 : Atty. Lorenzo M. TaEada Atty. Joker Arroyo Assembly:an Antonino Ro=an, Jr. ' Mr. Walt er '.Jelgus Mr. James Voeber Mr. John Hankowsky Minister Gabriel Itchen hinister Cle ente Gat =aitan Dr. Zoilo Bartoleme Dr. Carlito Aleta Mr. Aura A. Sinnons Dr. David Ferg
,.33 *C:? s, Mr. Ja=es Moore 'Mr. Gerald Carrol Mr. David Call Ilr. Raymond Sero Dr. Se.r, undo Roxas Minister Geronimo Velasco Dr. ..illir.n Ucward Arnold Mrs. Nora Petines Mr. 4.ngel Lazaro Dr. Salvador Roxas Gon: ales l
so .e 1222 224
Joemission on Duclear Heactor Pl: nts 12 July 1979 - 1: 30 ps - 2:C0 pm Psge 2-3 OPENIUG OF SE30 ION (The sessi6n commenced at 1:30 D.c. with the Honorable
- Aicardo C. Puno presidit .) ,
THE CLERE. Ladies and gentlemen,,pleaco rise. The Jo.niscion is nou 4n session. Everybody is enjoined to ob-serve silence and proper decorum. FEE CRaIRMAN. The session is now open. Call the roster of regular appearances. THE CLERK. (Readinc) Atty. Lorenzo M. Tanada .........Present Atty. Joker P. Arroyo ..........Present
. Hon. Antonino P. Roman, Jr. .....Precent Mr. Walter Vilgus ...............Present Mr. Gerald R. Carroll ........... Absent Mr. J ames C. Woeber . . . . . . . . . . . . . Pre sent Mr. John Hanskowsky .............Present
)hf!{} b($!f%!,hlkil* Ut k uhkE(uke
- Mr. Daniel d. Call .............. Absent Mr . Raymo dd S e ro . . . . . . . . . . . . . . . . Ab s e nt Minister Gabriel Itchen .........Present Minister Cle= ente Gatmaitan .....Present Dr. Segundo Roxas ............... Absent Dr. 2 'cilo Bartolo=e .............Present Dr. Carlito aleta ...............Present Mr . nur a A . S i==ons . . . . . . . . . . . . . Pre s ent Dr. David Ferg ..................Present Mr. James Moore ................. absent Mrs. Nora Petines ............... Absent Minister Geroni=o Velasco ....... Absent Mr. an.tel Lazaro ................ Absent Dr. Salvador .4cxas Gonzales ..... absent
. Dr. illiam Howard arnold . . . . . . . Abs ent I
Commission on Nuclear Reactor Plants 12 July 1979 - 1:30 p.m. - 2:00 p.m. Page 4 THE CHAIRMAN. May we know if there are any other additional exhibits to be presented by Westing-house panel among those to be amended or corrected' or otherwise submitted? MR. FERG. Mr. Chairman, I would like to re- , submit the third page of Exhibit "14-B". I failed to inelude the footnote on the copy I turned in yesterday. I want t.1e footnote to show that that information was reconstructed, using the U.S. NRC report NUEG-0560. THE CHAIRMAN. So, this is an amendment to the third page of "14-3-1". MR. FERG. "14-B-1". THE CHAIRMAN. Mark it as "14-B-2". Is that a "14-B-2"? There is no "14-B-2" yet. "14-B-2". Is that all? No other papers? We are still awaiting the North Ana NucLaur Plant E
- = =
F
r Ccmmission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 5 report. MR. FERG. I would like to ask you again if I could have the Nuclear Ana report which you nave referred to when you brought that right. THE CHAIRMAN. We shall deliver that during the recess. MR. FERG. Thank you. THE CHAIRMAN. For this afternoon, we shall first ontinua with the EBASCO dissertations after which we shall resume with the Westinghouse panel inter-pellations. Mr. Stilford still has the floor. MR. TARADA. What is the f0otnote there? THE CHAIRMAN. May the Commission inquire if the exhibits thus far indicated yesterday have already been reproduced and marked fer marking for today's g22 221
Commission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page G hearing? MR. FERG. Thq(are in the process of being
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prepared. So, they are not yet ready? THE CHAIRMAN. MR. FERG. They are not yet ready. We have our Exhibit "14" which is the seismic risk map which 8 is ready. And perhaps, it might be useful if we were to serve that particular exhibit so that the Commission for a moment because I and others would look at that would like to make that a point. THE CHAIRMAN. Very well, reproduce that Exhibit "14", NPC. MR. TORRES. Mr. Chairman, in yesterday's proceedings, there was a question on the role that EDASCO plays with respect to ascertaining or verifying that the design site characteristics and parameters that they have developed from the NPC are being used e e.. e O
Commission on Nuclear Reactor Plants I2 July 1979 e li 30 pm - 2 : 00 pm Page 7 in the design and contruction of this plant. THE CHAIRMAN. And carried out. MR. TORRES. Ani carried out. And if the Commission pleases, since I furnished the answer to that question, I would like to make a short statement to further clarify those made 3esterday.
~
THE CHAIRMAN. You may do so. MR. TORRES. In assuring the safety of the plant after the site characteristics are determined a'nd furnished to the designer, the owner -- that is the NPC -- the designer, manufacturer and the constructor of this plant -- that is the Westinghouse -- the re-gulating agency, the Philippine Atcmic Energy Com-mission and the cperator which will te the NPC, in order that they may assure that the installation can be constructed and operated withcut posing undue risk and hazard to the health and safety of the public, 6 m MO i etc cc
Commission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page S must right from the beginning assure that these pro-cesses of utilizing the parameters developed from the i site investigation are indeed inputed and utilized by the designer. The way this'is done and the way the consultant plays its part can be briefly described - as follows:
. Before the regulating agency -- that is, the Philippine Atomic Energy Commission -- grants the owner a construction permit, the owner has to submit a docu-ment which shows that among others the design of the structures, the components, equipment and system will comply with the design criteria that the regulatory body has issued and which must be complied with. This docu-ment is part'of a more extensive one that covers other subjcets. And in the preparation or submission of this proof to the regulating body that such is the case, this is embodied roughly in one volume of a 16-volume 6
m
Commission on :Juclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 9 report that we have submitted. Ir this perticular volume, which is also one of the chapters, we show that we have -- that is, the National Power with tne assistance of its consultants, EBASCO -- determined and confirmed that the identification, description of the systems and the utilization of the data and, in particular, with respect to the question yesterday, the' use of the seismic information that has been estab-lished will be reflected in the design and that the right kind of de' ign analysis and design procedures and methods will be used. On the basis of this docu-ment which had been submitted to the Philippine Atomic Energy Commission and the evalua*f- ;f this report, the National Power Corporation has been issued a constructive permit. Now, during the course of the design and construction 4 1 e g - M
Commission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 10 of the facility itself, the National Power Corporation has in its organization units thac continuously monitor and assure that these are being done in accordance with our commitment embodied in this document submitted to the regulatory body. In this respect, EBASCO advisers are piso utilized. And yesterday, I think, the question was directed to the particular activity going on in the field on how EUASCO plays a role in this process of seeing to it that the constructio.7 will be inaccordance with the criteria and ccnditions that are imposed on the design of this project. At the field, it is not the EBASCO man alone who does this. It is really NPC's responsibility and it has a construction group that performs this. How-ever, because we have available to us the exp.rtise of EBASCO, we see to it that they have a man assigned through the field so that we have advisory services 0
._ _ m w-D
Commission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 11 available on a day-to-day basis. It is with respect to this that we have brought this afternoon, Your Honor, the EBASCO man in the person of Mr. Elliot. who will be alsS available if the Commission pleases to question him. THE CHAIRMAN. Will you please verify if Mr. Torres has been sworn in connection with his position paper? (Af ter a pause.) Not yet. He was sworn in connection with the dissertation. MR. TORRES. Dissertation. THE CHAIRMAN. Please swear Mr. Torres. CLERK. Do you swear to tell the truth, the whole truth and nothing but the truth in this investi-gation? MR. TORRES. I do. THE CHAIRMAN. Do you confirm under oath what you just stated prior to this? 8
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Commission c.. Nucicar Rcactor Plants 12 July 1979 - 1: 30 pm - 2 : 00 pm Page 12 MR. TORRES. Yes, sir. THE CHAIRMAN. You stated that there is an E3ASCO man and there is an NPC man charged with the verification and checking of the construction to sce to it that it complies with the EBASCO recommendation? MR. TORRES. There is an NPC organization, not only one man. THE CH7.IRMAN. !!r. Elliot is the EBASCO man? MR. TCBRES. Yes, Your Honor. THE CHAIRMAN. And who is the head NPC man? MR. TORRES. We have at the site, uncer our site manager whom you have met before under a cons-truction division headed by Mr. Eleuterio Gatus. THE CHAIRMAN. Eleuterio Gatus. (At this juncture, the Chairman is spelling the name "GATUS".) = ew a p
Cerc. mission on ?:uclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 13 MR. TORRES. Gatus. THE C!! AIRMAN. All right. So, Elliot and Gatus. Now, Mr, Tilford, you may continue with your dissertation. May we have the exhibit? The Commissioners here have not been given any copy. We have the figure marked as Exnibit "14", NPC, being flashed on the screen.
.aase proceed.
MR. TILTORD. Since the news media df not put my records to this ficare correctly, Mr. Chairman, I thought of the porribility that their misunderstanding might be more ..despread. If I can refer to the lower lef t of the figure to the note that you have, that note reads:
" Cont. curs and numbers at ridge point represent horizontal acceleration expressed as presented gravity with 99.5% probability of not being exceeded in fifty (50) years. This is equivalent to a return period of M 'w=,
commission on Nuclear Reactor Plants 12 July 1979 - 1:00 pm - 2:00 pm page 14 10,000 years." 4 I would like to explain that that means that an earthquake affecting the site'with accelerations greater than .26g has a return period of 10,000 years. This does not mean that smaller accelerations can occur during shorter time spent, tiam is, an earthquake could cccur next week, yielding an acceleration of .lg. But this simply means that at a high level of probability, these values will not be exceeded in fif ty (50) years, and that is another way of expressing a return period of one in ten thousand years. t Before we move on away from this figure and this subject, I would like to correct something that I mis-stated yesterday. I reported to you that the horizontal accelerations experienced in Cotabato during the August 1976 earthquake represented .085% gravity. I indicated to you that this was exactly 140th, the
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Cor-aission on truclear Rcactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 15 i i design value of the ho,rizontal acceleration of gra-I In fact, vity at Napot point. That is not correct. it approaches one-fourth (1/4 to one-fifth (1/5) That in terms of the design value at Napot point. of energy involved, the statement that this is essentially 140th of the energy that will be in-volved remains close to be incorrect. Before I move on away from the issue of seismicity, I would like to make one other point. [he1971 additional,theNationalStructureofCode for Buildings in the Philippines which was af t.er the 1976 Mindanao earthquake, would require that in ccm-pliance with the Code, if you are building a one or two-story building on Bataan, the horizontal design acceleration would be between .08 and .lg, depending on the type of bracing system being used, and I simply point this out to suggest in one more way that I 1) s't,1
Commission on Nuclear Reactor Plants
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12 July 1979 - 1:30 pm - 2:00 pm Page 16 i t plant-the design acceleration for the Napot po n d being a factor of, four greater than that Code re-r tive de-quirement is ar essentially quite conserva sign basis. I think t hat concludes my remcrks on the ay subject of sef amicity and I am sure that there m this be question', which I should try to address at point. You are concluding your dis-THE CHAIRMAN. . sertation, Mr. Tilford? I am concluding the discussion MR. TILFORD. I am going to proceed briefly to of seismicity. there discuss volcanic activity and I thought perhaps eis-
'might be. questions related to seismic Assue or s tion that micity though, and I would like your atten that that was the end of it.
Justice Bautista. THE CHAIRa?N. + b a O'W
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Comniccion on Nuclear Reactor Plants 12 July 1979 - 1: 30 pm - 2 : 00 pm Page 17 Mk. BAUTISTA. May I ask if you know if this is the f'est site that you were asked to make a study with respect to' nuclear plants in the Philippines? MR. TILFORD. With respect to nuclear plants in the Philippines, this is the first nugicar plant and, , therefore, this is the first site. MR. BAUTISTA. You are referring to the site at thpot point, Morong, Bataan? MR. TILFORD. We earlier contributed to a study of a' number of potential sitts in Central Luzon. The site that was finally selected and that we actually confirmed was the Napot point site. MR. BAUTISTA. Did you not study another site semewhere in Bagac or seventeen (17) kilometers away from Napot point?
!!R. TILFORD. If you will give me twenty seconds, l
l ts Commission on Nuclear Reactor P an 2:00 pm 12 July 1979 - 1:30 pm - Page 18 . t were, in fact, I wili get you a list of sites tha studied. r fers to his (At this juncture, Mr, Tilford re papers . ) . letion of the We did study to one level of comp The more complete other fairly large number of sites. Mr. siting plant will be covered under history of the But in the immediate Gilmore's discussion to follow. of Zambales peninsular
. i area, we studied the southern t p f Bataan peninsula, which we studied the southern tip o .
and we San Jose point; was typified in that study by kilometers of the within ten (10) studied the area Bar*io of Bagac. That included a number of locations eninsulas or points, and tha t could be designated as p locations, primarily also included a number of other h rice cultivation. low-laying locations associated wit So, you made a study of the Bagae MR. BAUTISTA. l
-mW *8 owe
Commission on Nuclear Reactor Plants 1 12 July 1979 - L.30 pm - 2iOO pm Page 19 point, that is where the housing site is now located? MR. TILFORD. It ,was fairly close to the present f housing site. This was the site that was considered to be the primary site at the time EBASCO was engaged to ec.mplete the siting evaluation. We call that Bagae 1. . That site was near, as I said, let us say, three (3) kilometers at the existing housing site. MR. BACTISTA. Why did you choose the Bagac site? MR. TILFORD. That site from the point of view of the development of a nuclear plant has a number of ailments. MR. BAUTISTA. Will you enumerate what are these ailments? MR. TILFORD. First, the site ground surface was an elevation of two (2) meters above sea level, sir. That is an entirely unacceptabic great level for a nucle.ar
.k plant in this kind of con'dition because of Tsunami. This '
t site was located in flood point of two rivers which l
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Ccamission on Nuclear Reactor Plants 12 July 1979 - 1:30 pm - 2:00 pm Page 20 - diccharge into the South Chin; sea between the present housing area and tha't site. The flooding in those rivers t . during the monsoon season is a continuing major pr'oblem for ready access to any site. Asie, it is located on that flat plane which would have created a need to develop , an enormous system of devotion around the site. The site was located in a saturated ground with essentially twenty (20) meters around consolidated sediment underlying the ' land surface. It was some six hundred (600) meters from the seashore. I have asked you to v..sualize then an excavation twenty (20) meters deep and uncensolidated luvium which would leave you eighteen (18) meters below sea level at one founding level of the plant.
- hey were not only the safety issues associated with that, but of course, the very real construction and design problems that would be asscciated with it. You 'could be trying to pump e
1 s111
Commission on clear Rcactor Plants t 12 July 1979 - 1:30 pm - 2:00 pm Page 21 the South China Sea dry in order to keep such an excava-tien dry. The site was located, as I mentioned, in rural valley which was eminently exposed to volcanic ash flow.
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The site was not a highly desirabic site from many pcints o f view. MR. BAUTISTA. When you made that study at Bagsc reint, was tr.e housing site alread.y under construction? MR. TILFORFD. With the cooperation of MpC, we were able to get constructed for our use and study sixk6) temporary pre-cast buildings which we used to house our geology-seismology and environmental staff which at one time are occupied with some twenty (20) of our people. There was no permanent construction at the existing housing area at any time during the carrying out of the study. MR. EAUTISTA. Tha t is all. THE CHAIRMAN. Please proceed to your next one. a O
Commiss4.on or ue 12 July 1979 - 1:30 pm - 2:00 pm Page 22 c MR. TILFORD. I will make reference now to the CO:;VOL re.=,anse to the Cr mission. I THEI CHAIR:!AN. It this a new exhibit? MR. TILFORD. Yes, sir. This is a new exhibit. I believe it will be No. 15. , THE CI!AIRM.AN. Is that the correct number, Exnibit "15", NPC? MR. TILFORD. You can identify this exhibit as
" site-looking air-blown radar museum". The Commissien is most welcome and, of course, invited to look at this more closely. There is a lot of information in it.
I would like first, just briefly, to address one of CONVOL's most important comments as we view it. We will address each of their comments, but let us go to their response No. 5 initially.
"CONVOL believes that eruption f rom any of the volcanic complexes in the area is possible not only fren h - - ~ ~
l
Commiss2on 'uutua. . --- - 12 July 1979 - 1: 30 pm - 2 : 00 pm Page 23 . the presently cbserved craters and vens but virtually from any point in the peninsula, Bataan having formed Natib oy the coalition of two dormant volcanoes - Mt. and Mt. Mariveles. This possibility is exemplified by Taal. It did not only crupt f rom the main crater in 1911 cruption cut also recognized ncmcrous parasitic craters; . for- example, Benintiang Manti and Benintiang Malaki alternately erupted before 1749 but was able to make open its southwestern plank and posted the eruptions from 1965 to 1977." Now, let us move at Taal for a moment. I regret that in this particular response, we are unable to agree with CONVOL. CONVOL mentions that the main cratcr of Taal on volcano island was the site of the 1911 cruptions. This was confirmed. There are ...
*"- o -
- c;.iction on I!uclear .;e ctor Plant.c 12 . uly 1579
.cuge 1 a:GU p .1 . - .2. III2CSD. There are nur.orcua niliccous on voler.no t t1 .ptio. T i 1at .! . a. "'ll po n i te t hey all takte p1sce within the r.ain caldera of the vc1cano.
c:.lders, uithin the Ilone of the cruptions hs.d noved out of th t period recorded hictory. And in fact if you look around the re-cien of Taal even on this radar in. ace you will find thac there are not uhat you would strictly call .iura;.,hrmic vole nic struc-turca iLacdiately associated with the caldera. by point here ic .h.: cvorything that hac hoppened in 1'asl in historic times has .ap;tened within the lit. Matib calihera. i.e co up here to Ilt. Natib -- the c .1dera of uhich 10 4 shewn sicht here -- und I uill shou that t o ,rou in a lart,er
.1 hat Cu.VCL ic se le on another r..dar imato in a nun.ent.
/ s ;. q about Taal is that f rom 1911 the 1956 and l')?6 vents that movec abcut FCC ucter; in a southe.icterly direction. is prfectly true. But all of th4t activity reo.ained with- _a the .. vin calt.cra and the developent in f.t. Ih.tib of an
. , tic cene on the ,.ccturn ;>1ank in not cow ider<td by uc w . .- a .
ce nible event and 1 uilt d.. Cine th,i. aa .. n - v u n'
' ith a prob:.hility of occurrence (,r. c.t .r th n once in one and if I may, I will rillion yearc. Let ue explain ut.y.
read souc of thuso materir,ls because it is probably r. ore lu-1222 246
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onogMain IO Iiecent scientific studies of a.re: nger ; csui by a r.s-nev.cc. volc :.ic activity of r.t. Ahtih volcn.i co .pl .x e xi s t:, .
- 1. 2 , i s,c t;u sh., ':t a?
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d re:r.in ;, 1.0. 5 c.. the followini; p ,,0. believes 1,n.st uruption fecu any
. lL. C . 1.ii ..a . CCI.VCu Den't ./ou of the vr.,1c5ni c ccaplexes in the :.rea in' rou itl . '
1222 248
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. .. . , :.rocr.Th sid c h 3 :.j:.15.: pr... !ic: . L.. f. : e :.l ... : .i .e ... 1- ,,w .st?....;*;i.tij ? ... '_'II sv :J. an cert:inife.... R. r c t v:n c. .r. , i . c ).
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v: of t i,o I.6. .. . s:,T o t y i it,: 1,m tic.t t .;e- 1.u ; o;<. . L:
" n;<. .*d vcice.ic activity of I.t. : it ih v.1.w;.i c co ;.le::
1.r a t: .e
. :. . . '.IL70 !) . I r. Chair: an, would ;,ou .d ::o. .d :.i - *'CL ::c . 4? 23ee.2:e in CG.VOL 1:C. 14, ccu ri:1 0;c thv.t th<. ;r e.ru ~ tions f er u tha J
li etir.aa s /t.t . ih:tlb caldcri. au 1 nardt. t,o L h; :.:1tc oth n ta.n
%:, v 1. Tu11. '. . ., O . . 1 ;t .'.. . .Tust a few b ck,"., rid ;iiu ';ti t . , . . . . .11-f 0 "d . iri 2n ; ou .e 10 g, our utudies , did ; ou c .iortli: s t.: with
- m. ..,7 m
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- 1 N a r c o- - ;i on r , t.he Ohn.i c ar e f th.. ;in :n < n
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t:. c : t:1::1 CC'.'.VCL to *. rap up the ciur.< o T a L. . ;;< .
. . 0:'..d ;u'..i! . . re ; cu tryi:.; to s s ti. tr. th .t ..r. Grt-e .ED**
1222 249
% .A.3 , As c. e auclear acactor 1lanto '
12 July A979 Pace 3 2:0 0 p .Li. gorio Andal, who wris later appointed a Connicsioner, had ns access or did not know of the co'.luboration betucen your cc:- par;y and CC1.VOL? I3. TIIdC.tD. I cannot perconkily anstmr your question. h} ,! [ I have not per onally interviewed I.r. Anial. I iJi }{ j j' i i Citi Clialid.,Ji . Uo you do not know the reason 0 arid the bases for the statements made by Cc:missioner Aradal in Docu-
- ..ent lio.17?
1.d. T]L2CtiD. I have not discu:ncr1 bis fi ndincu or his ctateuent: with him -- no, sir.
- ?!L:, Ct!AI.iladi. You huvo not inquired into the bani., cf this stater. tent?
I's. TIL/ cad.. I believe that he state:, that the baaic for i:is stater:ents fairly clear in Lho M tial p:aracraple of his letter.
.I c C.:AIa ili. But these t.r* the conclusiens of his prc ai ses and the precises will involve the :.;tudies tiiat ucre
- 1:5e.
. . .' . T. I X ..J . t' hat ic correct.
ci. C. mI . . ..C . You did not , a : c e :., r. t.. t.! . . r .: udit-t?
. . . . Ci:..l .: : di . .;c havu had ;ccoua, 1 b.Iicv., ::o 11 o t' the CsI VGL inf arsatien that al e avail:ible. ' lid C:1AIic.ir'. Do you havu thout with jou?
1..:. TIf/C:iD. Iio, cir, I do not.
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Ga... u:ioa on .. n r :: cur 1or 21outu
* '. 1y 1';.? ,'
12
?:L0 :.n, i .. . . ;;.' O.a!".'J .il . Che point,I.r. Ti) ford, 10 in order th.2t that we can tl.cre .<ill be a a ?cting of the einds, in order i.inroi$t the areas of dispute it nic.ht h:4ve been botte*r to I will ask et forth the t.2::es of thc0c CLI.VCL conciusions. '
fety I.iociou a cirilar question e in connection uith I,..s va be c ..usie this Docum. int 14o.17 utates that CO .VLL n.ornly c . ares 4 gJ l , Did jou have access to the B
= the view of IAOs .afety hission.
1 ctadites nade by IAta Safety hiccion that proa.pted thise to .
'a..c those conclusions with which CClR.L acreus?
vafety
'.le h.sve appeared before the I.~.
I '.. . ?"LPC20.
'd,,: L _.
I;i cien curing a 3-d:4y mootint,in Vienna in 1970. i iaitial Afoty I;iscion visited the site one day during the r
.o have, I believe, 9-d.4yI visit to the l'hilippines in Ir;77 * 'he the data considered by the la ;n tc. n. f enri 1.is ;r .ts , CEair..;ionel- iuidal will b.e '
t o t '..; f e '.t r '.0
..Gd WC just C,ll att :#Lioq ICCition Wper.
e ta.c e ', to
- 1. s task ahould t,o rondered <saci<:r by e: met ivf r t:. .:
~o, a r ;/ wo su_. :c:t.
these conclunions that he derives. 1222 251
1.: July ly/ .e 1:.ce ? 2:CC p.ni. you .,;o back to 1.0. 3 so that we uj11 proccc:1 in prop;r or-der as the numbarin;, indicates. f..i. 2IL/O:iD. With your perr.i.;ul on, nir, I t.ill Lc h,57 ' o Go hach to I*o.1.
?!:.:: C.'-.IIC :.." . 1.*6 1 wu cly cayn that v. lc,ciola;r ic
- .ot :. exact oc '.er.co. G y'oe we c..n car. code Ll.n.t and;. .o to ti.. :.: ore exact conclusion beenttae the cencinaion 1:3 ore p:ecice in IIo. 3, thr renat.ed volcanic activity ir.1.t. ..atib volcu::ic conplex exists.
iG . 211.FO.:'J . Yo a , air , and ;. ou w i l l no l.c t.'.:a t in .uec-tion ;!c. 2 the CC .VvL has i ndicated Livet <n.r teor'<. is ennci-Jered b-: them to be at the stand:.rd with t.he . ire:.cnt utate to De Lt i. 7
. .. e C.iAIIu ;.. 'lec, we lu.vc 1'o. 2, but in .:c. thry dic-g reed .zith year conclusions. ..i . 7 ..~.FC J J . .lic not.d that theu J m i: . loner c;:me tc ua:.h to a;ree with rvery one.
2ds Or.'tI:;-.11. .' hat i s a ve ry 'an .cin. ' c .. . t e..<> r.t , r.r. Jil-i': r:1. s.. .auw.u.
, i- . 9 .
I a' .sorry.
. . ., J. d in .. . ..c chall r:v . . . ..j : .. : ' . . r ' n :nt
- c , t tc naho that observation.
...i. OII2C.I .) . It was not intended nc er. un.-;na cou cnt, sir. ! 1222 252
Ceraisaien on ::uc1%r Reactor Fis.nt.: 10 July 1079 1:.ce 7, 2:CC p.m. s TM. CIUIitt:AN. f.r. Tilford, please reciprocate with the cane hospitality that we have chowa you the sa.?.e courtesies to which you hdve been subjected. 121. TILFCUD., I appreciate your couaents, Ilr. Chairman, and will attempt to honor them. 154 CHAIM1A!I. This Co::tianion has not indicated any acrec=entwith!anyono,thatispreciselythefunctionofthis . 1 Cc= :iscion to find out what is the truth and when we noke state-I u::ts
- hey are =erely invitations for contlemen who are parti-cir at .v; here to enlimhten us. When we say that a certain cen::issioner or a certain official cade a statement, it does We invite you to not mein that we scree to that state =ent.
to that cive ,,our opinions, your explanations with respect state =ent. I'3. TIIJORD. I appreciate the sense of the Chairuan's comments and will truly attempt to honor them in spirit as well as in fact. The response No. 3 cf CC:!VGL which we are addressinC can.be read and states that C0tiVCL shares the view of the IAIA 3arct; IIission that the deacer posed by renewed volcanic activity of the 11t. Natib volesnic complex exists. Our responso would be, we refer to our coerent above on response No. 1 and I wish that we had made some co=. ents in response to No.1 recarding the uncertainties of volcanic prediction. To go on, it has been concluded I222 253 0 I
Cennission on U icar Reactor Plants 12 July 1979 Pace q 2:00 p.m. as a result of our studies that the next to stront creund l notien during seismic chaking volcanic events represent the =oit credible geological hazard to the plant. As a EeoloC i cal ha:ard, volcanism differs frca scis-reco nised
=""""'""*"""""""""" ="=""'"-
P00RL,.RSINA tructiveness and develop catastrophic effects over nuch s= aller areas. Furthermore, volcanic vents lasts much a lencer than seismic vents. Any structure located at point where a volcanic vent develops would be destroyed. The likelihood of occurrence of this event is extremely s all'for any given point. Compared to the broad areas catastrophically affected during earthquakes the areas seriously affected during short time periods by volcanic events is small, thus reducing the any probability of occurrence of catastrophic effects at civen point. Conpared to destruction during seisnic ground shaking uhich occurs in a =atter of seconds the destructive effect of volcanic events or episodes is co:amenly .q; read over weeks, conths or years. A particular volcanic center
- .ay develop in weeks or =enths I,ut imajor vole:.nic <idifices cost con =only evcive over periods measured in hundreds of thousands of years.
1222 254 - = .
12 July 1979 ; I
. -ce l0 2:00 p.n.
i
.t I
as st&ted'in;our cor.mbnte on response No.1 above, we h;ve detorcined that only threc =ajor volcanic evente are A liholy to occur in any 1CO,000-year period on Dataan.
~ level of risk we find acceptablo in view of our GCreement \
si:h the next CC1.VCL finding that the Mt. Napot site ia pre-tected frcm effects of tit. Natib volcanism other than ash s fall.
.l . ' CJKVCL's response No. 4 reads: CChVOL believes that thculd an eruption take place at the main crater (caldera)
- '.. :.stib's cuf ficient na] ural barriers, for exar.plo (draina;e c;r.: ;al$c and brid. ; ec) exist to protect the plant site frca the:
.iircet effectc of pyroclastic flows, clowing avalanche, lava flows snd direct impact of volcanic ejecteent.
Cur coie.cnt on this responsc a this conclucion is the cano as t;u reached dt. ring our study an1 recorded in the 1.reliminar,y c.rety anslysis report. At this poir.t, it ic our underctand-that there is scue
..; th t both CCi.VCL and we arc in acreement I. l.it:, which we nue of renewed volcanic activity f rom ht..
i 3 0,11ry .s being coco part of an expecte d three vole.aic evca ta
.a h L ,Cv0 year un hat *,an; cnd Lhat th9 an.naission anel we are 2:. .creeue.
that even should cach eruption e/.ists from the existing caldera, chould it occur, that the site is i.aturally I beli.ve I ratceted from volcanic hazards other than anh fall. exists tc-tcat is a corr'ect statement of the acrecment that I 1222 255
- = - . . . . - _ . . . . _ . - - .
I
l Occciccion on 1:ucle r Scactor ?lanto 12 July 1979 I' age 11 2:00 p.n. tween the chair:aan of CCliVOL and our cives. It is in the arca of question No. 5 which we have carlier read, that there is sone source of dicacreenent.
~
And cur basic position in that natter must be that the for-near or at the plant site is not a credible event because it has not happened during the five nillion past years of the opportunity for the formation of such event. I have elaborated the renainder of our reasoning on that particular hazard. CLhVOL responce Io. 6 reads: CCP.VCL acrees with the IA 3 succestion to install a volcanic nonitor-inc systen in nt. Natib and possibly in the adjoining vol-canoes for the purisoso of predicting future activities.
..ith this it ic expected that tircely warning cpuld be is-
- ,ued before any impending eruption thereby allowinC time for the ir;.aediate shut down of the power plant and our con-
- .ent would be at the direction of PaJC, :70 will design and install a bonitoring systen at Ist. lis tib.
CC1.70T .s response llo. 7 reads: In conjunction with Iau C the cuscostion of IA1:a to establish an off-site fuel stora e wherein radioactive materials would be duposited ir. %e event that the plant is endancered by volcanic acti-vity, should be concidered. 1222 256
Concission on !.. clear Reactor Planta 12 July 1979 Psce 11 2:00 p.m.. Cur cor.nent would bei as directed by President Marecs, a covernstnt panel has been active for c: ore than two years in the' initial phases of selection of such a site. CCI VOL reuponso No. 7 CChVCL believes that the pro-bien on volcanic risk has been sut'ficiently discussed and studied by parties concerned and that it is just a natter p , cf i=plenenting roconnendations. ldl I 'if 4 W b , j' l 'Je agree. PisFC, the responsible licensing and regula- - tory bcdy, has recolved outstanding iscues raised by res-posible reviewers and has provided such stipulations in the ecnctruction por.ait as found necour,ary for cenplissce by 30. l'he final par.acraph reuponse by CCINCL re.4ds: With recards to seisnic risk while CCINOL has sou:, d:4ta on tec-tcnic earthquakes in connection with its study on relation-ch.p between t2ctonic earthquakes and volcanic eruption cv.c data nay h::ve bcon u::ed in cei::nic ris:: nducted by the prCponei.t.
':'ho study oa tectonic earthquakes f.11 under th.: res- , a sn ibility of 1..s..a.. houcver, CG13CL 1,r.li<-vec t.h t the , relen has been well discuused and rocca aene. tions by Lsh 1.iccion en this rocard should be considt. red. Our couewn:
vould be that F.tdC has taken the Ia2A Missien reco:2.cndaticns 1222 257
12 July 197() , ; ' Is.cc 13 2.00 t.u. I into account in Octablishing stipulations to the project construction perait. Cutstanding issues aro, therefore, nou resolved. hat concludes the material I had.
. l-I <sk your indulcence. To pre'j:ent en th: subject of volcs.nism, we have used the CChV0L res;cnse to the Commission primarily as a te'ating f acility, as it were , in o:dtr to brini; f orward the iscue of volcanic hazards which are on the sinds of =any. We are aware that volcanics has not been onc of the nine questions posed, but we felt certain th: : the Cc=uission would wish to be informed as to the various poccibilities and positions related to such activity.
i.ith that I thank you for your courtesy and your ti=c. I now yield to Mr. Gil= ore, if you have no more ques-tiens of ac. M3 C.!AIlc idi. ,,uestions by Juctice Vasquez.
.;. V4 6UEZ. I believe you have :ncationed earlier, I thi n'.: it was yacterday, that ycu have c.ade studies of t.it oc for nuclear reactor plants in so t.iary places in the world.. Is that correct?
l -( . IIIdCD. I believe tha t br. unaly indic.ted that ti.e ec. pony has made siting studies, ycs, rir. h.i. Va.s sUZ4. Are you aware of any nuclear pl:,nt any-i;here in the world as close to a volcano as the one in 1222 258
32 July , 979 Fately 2:C0 p.n. .
}
4 Istaan which is only nine kiloneters away frc Ut. Natib? MR. TILFG.C.D. The Trojan liuclear Plant in the United States is very close to IIt. Hotl which is a dernant vol-a cano like Mt. Natib. The issue is a very conplic-ced one, but let ne say that any plant located near un igneous rock bcdy is close gnr rt Dona Ql { ! to a volcano. But the real facter is when that volcano was last active, and in nost cases it has been =any nillion of years since that tine. I can probably devole; a list of Japanese plants in their relationship to volcanoes and pro-tably sone others as well, but I personally do not know of a plant closer to a volcanic structure than Napet. I3. VAS,U~.'. In the paper sutnitted by the IAG 3afet;- liission a statencnt was made to this effect: the U. pot site is unique to the nuclear industry insof ar as the risk asco-ciated with eruption of nearby volcanoes. The only codern plant which is designed to account for volcanic eruption is the Tabon sprinc plcnt in the United Statec. Onis point is located 123 klloneters fzcu the nearest volesno and, con.ce-qt.cntly, ssh fall is a consideration. .s t 15e i E.qot .,oint site the nearest volcano is only 9 kiloneters ausy. Jo you h ve anythinC to csy to that statement? I.R. OlLFUdD. Yes, sir. I uppreciate the opportunity.
.- mem _ e-*-- = + = , - - = = = = .. e-
' ~ ~ ~ ~
12 : July 1 '9 h.; e. If .h O p.m. ,
' i '.% bon springs is not a plant tihich is un<!cr construction.
i l It is k plant which was under!desicn in the eastern part l of the State of Cregon, just houthoftheColunbia .tiver. e Ti.e 1.lant cite is located, as. cta ted, approximately 1C0 ulles fren active volcanoes which crupted within the lact i feu y.eers. I
'The state::,cnt that Mt. Natib is an active volcano is 6
tech:fically and conpletely erhoneous. The last cruption of I T.t . htib, and I think we have a very clear racord of that and se can de: anctrate it, occurred 70,000 years aco.
, In the United *.itates we do noi, have regulatory t :xt
- .hich covers re.tuirenants for investication associ,ted with volcanisn, They approach volcanica as an incue on e cace to cdse basis. However, by analogy the requircr..ent for non-c pability or inactivity as it relates to faulting 10 ti.at f a t.l t ing- tu.st not ba,ve occurred on c civen fault within the lact 35,CCC yci,rc. If it has not occurred within the la s:t 35,0C0 years, the entire titing and reculatory prr., cess ic-neres it. Therefore, within that context and using that u:. 410: y the last eruption of ist. Ilatib was uare t::sn twice
.sc long, aco as, is required in U.S.1,rac ice to de. onstrate incapability. P00R.OEiNL m . .. mn... e..w. 2.>
... . g. . ~,-e22 ...; f..y;:.
24.. p. .
Cearission on Iuclear Reactor Plants Ce C p.=. [s
. o h2. VAsqU2'.4 1s a geologist, would you tell us if I
4 it is not a fact that dernant volcanges can also erupt? LR. TIL70ED. Dormant volcanoec can erupt, yes. ha. VAS4UJ4, So, Mt. Natib =ay poscibly crupt?
- 13. TILFC2D. Yes, it is possible.
MR. VAS,UJS. But nobody could cay if and when? MR. TILFCED. We have tried to assess the likelihood of that possibility. And that concluded through a set of l co= plex studies that there are likely to be three major vol-canic events on Eataan peninsula in eact 100 :CCO years. Tnat includes Mt. Mariveles, Mt. Natib, and all of the satellite or ancillary structures or volcanic edifices associated with them. Ve believe that we .'iave nade kn appropriate assessment of the likelihood of an eruption fron Mt. Natib. ILI. V.J4Uc4. And you are basing that opinion only on probabilitie ? 1.2. IILFCED. Frobabilities auccciated with the past iatory of eruption on Bataan penincula. -e ILve saarled erproxi=ately 100 locatios on the peninsula representin; dicercet volcanic flows er events and have determined their sctual acc. We have assuned that each one of these -- we have sa pled all that are available -- represents a discrect and najor event, although that i: not recessarily trae, but {}
Oct.:c.a.:sion Juclear heactor 11snta 1_' July 1979 1.. a 171 t it is the t.o:', conservative or safe ascu;:ption you can nake. Je have from the ages when those thincs occurred t:dn assessed the nwiber of events that have occurred in unit tic.c, which I reported to you .s during the last TCC,CCC years, probably, five to ten ira,jor eruptions. And the probabilistic aspect of this is nw.terically fore-casting what would happen then in the tuttre fran that historical or geological data. F.H . LJ ,U C . You were dir, cussing only the prob: ability Of %c eruption of !!t. Kati'. You have not told us if the soie thin 's true with ?'.t. I:ariveles.
..R . T I'!CRD . Cur statements have been t:.st we believe that there :aay be us many as three crupticas on Estaan p.ninsula in 1CO,CCO years. ..'e b.ive not di.scriaina ted be:.. 2en ..t . Iiatib ar.d ht . IIarivelec bec us.,e cur sample distribution was unsvcn. L'h.it ic, we were able to rr: cover .:. ore ca:.ples frca ?;t. IIs tib than frcn I.t. ?'ariveles. And, thereforo, our result would be biase:d.
b G
r Cctsic:lon on Nuclear Eoactor Plants 12 July 1979 - 2:30-3:00 p.m. Pc;c 1 J. TI'IJORD. ... Mt. Mariveles , tecause cur i sar.ple distribution was uneven. That is where we were j l able to recover hore sa=ples from Mt. Natib than fren Mt. Marivele's. Therefore, our result will be biased in the direction of Mt. Natib. So, we just used all thosesamplesandincludedallofthevolcani,eedifi(es on Entacn. MR. VASQUZZ. You mean to say that you do not have sufficient data to tall us that Mt. Marivoles cay not also in all likelihood erupt within the next fifty years? MH. TIIJORD. Ve have all of the data that we Icel is available to be collected frem the Eataan peninsula from both Mariveles and Mt. Natib. I said, ue were able to collect mora sc=ples from Mt. Natib, that is true. But to eliminate a bias on the
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Cencission on Nuclear Reactor Plants 12 July 1979 - 2:30-3:00 p.m. Pege 2 data than we have considered the data representativa of all volcanien on Bataan. That includes both Mari-veles and Natib. So, when we state that appeared to be the right probabilities, we cannot narrow those down to some of these are fron Mt. Nati~o; so=e of these are fro: Mt. Itariveles; so=e of these are fron Sa=at. But over the volcanic features there are on ths peninsula we feel that we can nake some legitimate state =ent ned that is where ve attempt to do it. MR. VASQU2Z. Would you be in a position to tell us which of the two volcanoes, Natib and Mariveles, is
= ore dcngerous than the other, insofar as the possibi-liry of eruption is concerned?
MR. TILFORD. No, sir. I really could not. The ycungest eruption that has taken place on Mt. Mariveles git?.7. 7 64
i Co::iccion on Nuclear Reactor Florts 12 July 1979 -2:30-3:00 p.n. Pago 3
- occured almost cxactiy tw> hundred thousand years i
ago. The youngest efuption on Mt. Natib blankets the ecstern side from Vent 3. Let ne point out that to you. ' This is the material that was erupted from Vent i 3 That this vent right here, you noti:e it is east of tbs = sin Cordero, durin6 the event so=e seventy thousand years ago en Mt. Natib. The material that is the lower, s=oother blanket =aterial on the east side of Mt. Natib, is the material frcm the event seventy thousand years ago. TiiE C'3.LIEMAN. From the record, the word "here" repectei mary ti=es was stated by Mr. Tilford, point-ing to the central part of t e picture. MR. TILFORD. And the east, Mr. Chair:an. Et Mariveles whose crater I as not pointing at e
i Connicsion on Eu laar Ronctor Plants 12 July 1979 - 2:30-3:00 p.m. PcE0 4 i i last erupted fron that central crater 190,000 to 200,000 years ago, at which tine this valloy which goes p to 'the center of the peninsula on this Exhi-P bit,ifron Mt. Mariveles, Mt. Mariveles cone is i il bridged, this valley was for=ed and probably run up to tLe east of Manila Bay. As you can see that val-
.l .
ley in a snall region, has been filled in by the
. naterials from the 70,000 yeqr old eruption of Center 3 on Mt. Natib.
THS CRAIEMAN. Mr. Tilford, will you please re-peat that lest paragraph and indiente what you nean by the words "this" and "that" in order to help the reqcrds. MR. TIIFORD. The Mt. hariveles cone was bridged about 190,000 years ago for=ing a pro =inent valley or sir. I canyon which can be seen on this Exhibit,
. _ _ . . . . _ . . . . . . . _ . _ _ .... . \' 2 1 _ _ _
Connionion on bucicar Eoactor Plants 12 July 1979 - 2:30-3:00 p .c. Page 5 i believe'wo have not identified;this 2xhibit. I t TE CILI 1EMAN. At this poirA, if yc2 cannot des-
- I cribed it, vill you please point to where you were indicating when you said "this".
MR.TILFdRD. The canyon, 1 think I said, this
' canyon.
The canyon was fornerly opened fren the cen - I
- ter of the peninsula to the eastern side of the penin-sula entering into Manila Bay. It is now filled.
TE CliAIR'"Zi. Mr. Tilford, we are trying to explain to you that when you say "this" or "that" or "here a ; it does not mean anything in the record, unless You what is =eant by these prnounce is indicated. can talk at length on this dia;ran. And, unfortunate-ly, we cannot even nark any sub-narkings en this, So, if because tho docunent has not been presented. you wish to aid the CSnnission, will you pleneo try e
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Co::icsien on Nuclear Reactor Plants 12 July 1979 - 2:30-300 p.m. Page 6
'a'ill 'w e to =ahe this understandable in the records.
try again, please, that last paragraph, MR. TILICED. My probles is that I don't re=es-I was attempt-ber exactly what the last paragraph was. ing to describe the fact that Mt. Natib has erupted This since the last major eruption of Mt. Mariveles. i_s proven by the fact that =aterial from the eastern
' fic k eruption of Mt. Natib, which occured 70,000 years eso, fills a canyon which was scattered and ero-ded at the time of the last eruption from Mt. Marive.
len. A think that was the one I was trying to convey, sir. THE CHAIR:".AN. Proceed. I also noted from the position MR VASQUEZ. paper of theCONVOL that they have made these statement e 1 g222 .
Co :iscice on 1:uclear Reactor Planta 12 July 1979 - 2:30-3:C0 p.m. Page 7 , I uich you would tell us if you agree with then or not. Thct the 'Bataan is for:ed by the cealition of two'dcr: ant volcanoes? MR. TILPORD. Yes, sir. That is correct. MR. VASQUEZ. That eruption is possible from acy point in the peninsula? MR. TILFORD. Mr. Cc::issioner, that scas the sub-
. ject of =y latent discussion of question of their statements.
MR. VASQUEZ. Yes. And I recall you said that if there vill be such an eruption, it' will be to the ecstern side? MR. TILTCRD. Yes, sir. R. VASQUZZ. The side away fro: the Itapot point. MR. TIISORD. Yes, sir. a MR VASQUhZ. Now, suppocing =uch an eruption will p
.. . . - ... - - . - . . . \ gl ' . .
Cennission on Nuclear Roactor Plants 12 July 1979 - 2:30-3:00 p.=. Pago 8 cccur on the eastern side of the peninsula, are you inplying that the plant site will no longer be in dan-ger duct because the eruption in to the east side of the peninsula and not to the eect of the existing volcanc? MR. TILFORD. In erv.ption on the east will not produce lava flows or flow s of hot doulders, ash and cinders 1hich could engulf and cover the plant. And if such an eruption at an appropriate location on the u? stern sido en Mt. Natip could produ:e such an ef-feet, the ultinate such condition would be the forna-tion of c volcanic vent at the plant site, in which caco, the plant would be conpletely destroyed. It is the eruption occuring on the western side of the penin-sula including h:. Hatib, we consider to he not credi-blo.
** * * " * * * -o .m.
Ccrniccion on 1:uelear Reactor Plants 12 July 1979 - 2:3023:00 p.=. Pcgo 9 W.E CEAIL*Jll. The NPO panel is hereby instructed, t; hen this Exhibit is finally reproduced and presented, to the piece on this Enhibit, the nanes of the volc anoes or other natorial porticis of this topography to help us underctand the dissertation when we read the se.ne aneu in the records. Minister Itchon, is that quite clear. Atty. Ilao. An7 questions fron ... MR. VASQUEZ. I would like ta ask one nore ques-tion. I could liko to go back to earthquakes which is the subject of your first part of the dissertation. I recall the chart that you showed here. I think it was tho.first one which depicted the faults around Eattan peninsula, IG. CI'JORD. Would you like ne to jat that back on, sir.
- 12. , Vaby,UEZ . Please.
Cenniscion on Nuclear Reactor Plants 12 July 1979 - 22,.D-3:00 p.n. P:ge 10 ME. TAfi1DA. As Exhibit "3", ITPC. TFE CHAIICiAN. Was this previously narked as [ p' I i I n Ukl d j" 1 dahibit "3"?, Make it of record that the picture being flashed on the screen corresp<,cdn to ixhibit "3", HPC, in cennection with the questions 6f Justico Vasquez. hS. V.'SQUEZ. I seen to notice that Eataan is al-nest enclosed by faults. There is one to the west which you call the Manila trench; one .;o the south uhc1h you refer to as the Taal fault; and two others to the north. Io that correct? MR. TIISORD. The closest fault to the north is rho San 1.ntonio ravine. Olosest fault to the west is *he western Luzon trough , which is not id mtified en this particular illustration. And the clocent to the couth is the Manila Bay fracture zone and those others you contioned are en the chart. k
Conniccion on Nuclear Reactcr Planto 12 July 197.1 - 2:30-3:00 p.n. Page 11 i MR. VASQUEZ. Now, did I get you correctly that because of the cristence of these faults, the earth-quttes that night occur outside of this shaded area in the crag would be attenuated ,or lessened in severity once it would reach the faults? s. MR. TILFORD. That is true of the Taal fracture
=cae. That is not necessarily true of any of the 6
others. The taal zone is nuperJy unique zone and that it is a zone in which the cruet of the earth is
, extending in this crust. And because of that earth-T quake shock is attenuated acrosc that zone. The others are not necessarily in that condition.
MR. VASQUEZ. I wish you would really enlighten us on this point because it seens to be the ccnnon inpression that if an area has several land faults, it is noro dangerous for earthquakes . G
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- ew...
I { Consissicn en liue?. ear Reactor'Flants 12 July 1979 ->2:30-3:00 p.n. Page 12
. MR. TILFORD. That is a correct inpression, sir.
The desiEn cecoleration for the plant at Bataan is one of the highest accoleration for any nuclear plant in the Iworld. That is true because the plant is located in 6 a region which is seis=ically active and in which there are faults. I have probably conplicated the issue un-necessarily by, stating that the Taal fracture line is a i zo.no of extension which tends to reduce or attenuate earthquake notions. If you will forget, sir, that I said that because it is probably not naterial at this point. Then you can continue with your i=pression that the fact, that a region contains active capable faults thus, require more careful address to earthquake. That inpression is correct. r31. var,qUEZ. And it is a f act that Bataan peninsula is such an area? O e
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Cennicsion on Iucicar Reactor Plants 12 July 1979 - 2:30-3:00 p.m. Paso 13,
. i,
' MR. TILFORD. Yes. Bataan as a part of the Philip-pines and the Philippine archiepelago is Eenerally consi-dered to be one of the more active areas of the world as f ar as volcanies and seismisity is concerned. The fact rennine!that like California, in the western United . l States, it is possible to select sites where sensitive
't installations can safely be built. And the Bataan penin-sula and, specifically, the Napot point site, in our professionni judsnent, is probably the best nuclear power plant site in Central Luzon, largely because of its re-latively low historical seisnisity.
MR. VASQUE3. And that is precisely the reason why you recen= ended that the site of the plant be such that it will withstand the strongest earthquake? MR. TIL?ORD. Yes, sir. t MR. VASQUEZ. I have no more question.
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Corniscio on Nuclear P.eactor Plant. ! 1T July 1979 - 2:30-3:00 p.n. .
.Pago 14 !
I i TE CEAIPAAN. Justice Eautista. Ia ER. EAUTISTA. Clarificatic'n, Mr. Tilford. In theletterofInstructions876cfthePbecident, the i . Question 1:o. 6, is the Bataan Nuclear Plant located in l a fault in the earth surface? 'Eill you answer that I cate60r77 , b MR. TIISOED. No. ME. EAUTISTA. k' hat would be the reason for your answer? MR. TIIJORD. That is a presentation of Mr. Gilnore has been prepared to nake. If that is your only ques-tien of no, I wouldp efer to allow hin to addr<>es that question 6. ME. BAUTISTA. So, your answer to the question is, the Batcan liuclear Power Plant is not located in a fault in the earth's surface. l 1221 6 _ t
Connission on Nuclear Booctor Plants 12 July 1979 - 2:30-3:00 p.m. Pago 15
+
MR. TIL?OED. That is correct. MS. BAUTISTA. Now, just to catisfy questions fren our conio$ people, the can in the streets, and since you said, you were able to otudy different sitea for a nuclear power plant in the Philippines, particu-larly, in Central Luzon, the connon question ic, why una not the nuclear site rather chosen the Sierra Madre Mountain or the Cordillera Mountain? What would you answer ne? MR. TILFORD. Firstly, the seis=ic risk in that region ac shown on inhibit "14", is hi E her than the ceisnic rick at Bataan. THE CEAIEMAN. For purposes of thio questien, Ex-hibit "14", HPC hen been flashed anew en the screen. MR. TILFORD. 1 believe your question refers to the area enet of Manila, is that correct?
******"***"we em e.... .,. , , ,, ,
Connission en Nuclear '.haetor Plants 12 July 1979 - 2:30-3:00 p.n. Page 16 t MR. BAUTISTA. Yes, yes. MR. TILFORD. A4 you can see on the illustration in the arec to the east of Manila, the seie=ic risk is higher than 'it is in Battan. You really only have to be able to distinguish between the colors: red, white and green. Rod is the area of hiS her seisnic risk; white is an crea of conewhat lower seisnic risk; 6reen is the area of lowect seisnic risk in this area. That is the prinary reason, sir. hR. haUIibTA. So that when you =ade your recon-nendation that the Bataan site is the nos logical and safe site for a nuclear plant, you have considered all the othc5 sites or pinces in the island of luzen? MR. TIIJORD. I believe, that Mr. Gilnore is better prepared to answer that questien in detail than I. I think, he would like to discuss the other sites
. . . ..w ,
Co::incion on !!aclear Feuctor Plcots 12 July 1979 - 2:30 3:00 p.m. Psco 17 P00R OMIMI-that were proTooed and have been studied by the earlier IAEA 4 sission stcrting in 1965 With your indulgence. I would prefer
' to refer that question to his presentaticn.
MR. BAUTISTA. Thank you. TF.E CVAIRMAN. You are excused Mr. Gilmore. HR. GII.MORE. Excuse me, Mr. Chairman. I will just re- , trieve some of my materials. Following the manner established by Mr. Tilfort yesterday in the expectation that that is the wich of the Chairman and of the Commission, I will make the f'ollowing co=ments and elaboration of the many biographical data that was presented earlier. I was educated at Man hattan College in New York City; received a Bachelor of Civil Engineering Degree in 1952; per-forned graduate studies in Civil Engineer!eg during the period
.a... rue,1:-
1955-56 in the cel),e,. cf tie citj cf :ce. . ::. ; I ture.1 ctcfwssional Engineer ia t! .: t t se of i: w 7..rk, Idaho chington; l'ennsylvu.is, l'.inne. ot. ,1%..tr.ne, Oregon, Utah and I as a cc. ber cf the A=erican So:iety of Civil Enginecr!.; lll l
Ccr -ine.icn on ::acle 2- Reactor 11:n s 12 July 197" - 2:JC-3:fC r.n. i j j L*niteil States Commissioner at-large, Association of E..gineer-ing-Geologist. I recently completed my 26 sesr with EBAS"O and presently, I cm chief consulting Civil Engineering and I have been in that position since the middle of 1971. The question that I have prepared a responoe to, ie. Question No. 6: Is the Bataan nuclear plant located in a fault in the carth's surface? Mr. Tilfort has answered that euestien s by s. tying, r.o. I kould reiter..te hia une.w.c by also saying, no. J.n d in the sense that is a short answer, but se lisve prepared infernaticn to cerivry to the Con:iuuicn e, rid tc ct):+r.. the reason why we scy, no, with a c ertain degree, with a degree of confidence. Since the very outset of the siting st a.2ir e for P.NPP No.1, which were initiated du-ing tne mid 11e 1C05, it us been recognized by all investicater: ti .at g- logic aa.! aci.aiohg'. . 1 charac teritst ; n of any site in 11o v:.ii . . no. any site in Luzon would be the primary sitar.g conecras. Pri-1222 z80
Cc==iesion on !!uclect Reacter Plants t,I,Q1 Q1 ' 12 July 1979 - 2:30-3C0 p.m. n n y['t [jiL; l i-I
- Pa58 13 mary parameters which would have to be addressed during tho
- proceding studics. During the latter part of 19%, under the suspices of the Internatiend Atenic Energy Agency, a pre-investment s.tudy on I power, including nuclear powr, in 1.u ,on c was un:!crtaken. acted in coll bnatian with the nuclear power etudy co=mittee Tnese sites are that selected four potential reactor sites. shown on the first figuro -- Figure Nc.1 -- in a paper which was effered by personnel of both EBASCO cervices and the National Power Corporation. THE CHAIRMAN. Is this a new Exhibit, Mr. Gilcore? HR GILMCPI. This would be a new Ixhibit, Mr. Chair:an. THE CHAIF".AN. Harx it as Exhibit "16", NPC. Just a MR GILHC~tE. Hay I interrupt, Mr. Chairman. c.c=ent. This figure is a fi ure E from this paper whien I intensed to enter as an Exhibit. TES CdAIR;;AN. Hark the .. Is that the text? Md. CILHCR2. I could giv., you th* titic of the j e .c a:ul ccericte JoCail. 1222 281
i C ur.iaisr. cr.Iuclear Reactor Plants 12 July 1979 - 2:30-3:co p.s. Pago 19 THE CllAIRMAN. The paper will to marked as Exhibit ... This is part of that paper? MR. GILMORE. That is correct, sir. h THE C11 AIRMAN. The whole paper itself would be marked as Exhibit "16", HPC. And this particular diagran, as "16", Up0. This depicts a nap. MR. GILMORE. Figure 1 fron the paper depicts a map of Lu':en and identifies the candidates' sites that were selected for consideration tack in the riddle of 1960's. The sites were located on Bataan peninsula and included Bacac and Limay. In'Que:cn province, cites identified as Padre Bargos and Ati=cnan, were also identified. At an early phasa of the siting cogsiderations or studies in the Philippines, thert was, of coarse, no sites, specific data available concerning populatica distributien, Ecology, seicmology, surface and ground-water hydrology, oce.s current patterns, typhoon severity, and this is very typical in the U=ited States and in any parts of the w:rld, whether siting ct the very inception of s. ting studies,
co= mission ca :iaclear Reactor Flants 12 July 1979 - ;:30-3:00 p.=. Fogo 20 studies for a nuclear power plant or for some other major it.dustrial power generation facility. The IAIA =icsion, howerer, did have made available to it regicesi data which was provided to the= by the Philippine Atc=ic Isergy Cozsission, by the Philippine Bureau of Mines, by the L'an*.hcr Bureau and by the Bareau of Custo a and Geodetic Survey. Occasionally, the I'.ZA mission also visited ecch of the sitos and cado st.at I have learned to be called " ocular-1:spectien" although that was not the term I =yself used. This cdvicory panol of exporta met in Manila during the period 15 to 26 February 1965 The conceptionc. question of safety was addressed by the mission by developing ::jor questionnaires whleb would require detailed answers during later phases of the siting studies, which uculd be or which were anticipated to be required for the power plant. Tnese later phases, these latur studies, were to addresa questions of populatics, surface and ground
Co m iccion on Nuclear Resctor Plant: 12 July 1977 - 2:50-):00 p.m.
'c;c 21 r
sater hydrology, meteorology, seismology and fou.idation. From these re:o.-=endations and consideratio.is, from reference L to Exhibit "14", NPC and also Exhibits "15" and "16", ;iEC which are the radar images, it is cleur that seicmocity, even in the very beginning, was being given careful attention by the original investigators. The results of the invettiga-tions in 1955. . . THE CHA!RMAN. Is this still part of the text? MR. GII.MCRE. This is still p.ir t. of ilu t. c '...e.
.:... i rt o n.
IHE CHAIP. MAN. So, make that Eqhtbit "16 -3", NPC. M2. GILMCRE. At tnis stage of any investigation, the a s s e c er.e nt a s , the evaluations of necessity have to be of a qaalitative nature. The four sites that I have icentified earlier on Bataan peninsula, Bagae and Limay are Indicated st tne top of this coluen. In yuezon Province, we have Ati= nna and Padre Burgos. Tha scpects of siting which were considered by the 1222 284
Cozeission on Nuclear Resetor Plants 12 July 1979 - 2:30-3:00 p.r.. Page 22 mission included economic consideratiene and safety concidera- , tions. The economic considerations address questiens of transmission, site develop =ont and transportation access r which are, of course, the normal -- are a normal things that are considered in siting any major facility. In addition, safety considerations will either be population centers as part of 1960 census; the avera6e population density; surface and gacund water hydrology, meteorological factor; geology; seis. ology;sub-soil structure were addranced once again, as I soid earlier, in a qualitative fashion. Going through the list, the Bagne site had so=e advantages as did Limay, due to their proxi=ity to the Manila load center. Atimonan also was comparable to the Padre largos site did not present any information and reports a vailable . The site develop =ent does not really have a criteria other than Padre Burgos which has a very shallow 5 off-shore facing on tha sea. That of course, would in fact, negatively under the development of a cooling water system ... g
- Commission Cn !!uclear Reactor Plants g 12 July 1979 l Page 1 3:00 p.m. J l
4[}( Md. GlLh0R2. Transportaticc we find inadeqcate
- for Lacce, advantageous for Lizay. There ic un exist-ing thermal powcr station located in Lizay area and na inforcation in the two potential plant sites of Que:cn p rovince . The populrtion densities on Estaan were re-latively or quite a bit lower than the population den-sities in Atimonan or in Fadre Burgoc. ona the ave-rago population density reflects tnose nunburn, both Ati=onan and ladze Burgos deficed as relatively high, average populatic:. density at Eagac in the report ican-tified as 30 individuals per square kilometer, altnough it was not stated in the report, essentially the came for Limay. Atimenan was identified as fac'ng a poten-tialseicmonicbazarhe Also increased typhece expcsure there were thou eht to be possible unfover.* tic, unsurc cccurrence during the southwest monsoons for the ma s:
plant; posuihle faulting was =entioned for the hataan Ilant. Aticonan on the other hand, was definitel. near identified e.tive faulting.. 'iith
< recpect to the sub-
[
Cen=issicn on l' ~ ar Peacter F1:nts .) i j 12 July 1979 I f I Fago 2 p.m. 1} gg hu scil r.truct2.:. 1 bed . 12 cr. - ted in the Sagae area, more uncertain ir Li=ay and the areas in Ne:en province was so=ewhat doubtful. In any event, on the basis of the inspections by the mission and on the basis of the recional in-formation available to them, on the basis of their i judgment, they rank these four sites in the following crder: Fo.1, Li=ay; No. 2, Bar;ac; No. 3, Fadre Eur-Gos; and, No. 4, Ati=or.an. You still forcive me , sirs, f I c:a pronouncing some of these local words in-actly. 2he second phas;' of the siting studies was es-I acn.ially initiated on 23 June 1971, when President Marecs issued Administrative Order No. 293 creating
- ccrdinating cc==ittee for nuclear power. This cccrdinating cc ittee established a sub-cc aittce unich was established to formulate a site selection critoria to make si;a recognizance , to collect avai)-
a'cle site data, and, to ret. der a rep rt to che cc:- Q
Con:nnsion on uclear Re ac tor Plants 3:00 p.u. i 1c d cittee and to the International Atomic L'nercy AJoney, l'ic. ire two, the next figure shcws tne site.; that were identified by the sub-cor.icittee. These incitaded the Phase One sites which had been discucsed ?:irlier
/
and which had been selected by the 1965 cottissica or _ission, and.added a site at San Juan in Eatancas pro-vince, and another site in Ternate located in C vite , province. C2tAllr.A11. Mr. Gilmore, the first one that ycu flashed was figure 1. Was it? Mil. GIllwRi:. Figure one, yes, sir. C!fAI4:X!. So this is figure 2. 1: ark this as Mark it. (Chairman a.idrescini., the Ixhibit 16 C-1.~rC. request to1. tty.Ar.jliola) Mll. GIlllCS2. The site selection ud. c . c ~ t t e t, as I indicated in 1972, starting fran tne 1969 work of the Ild:A Siting hission addei to the hav. , Li.cn, Atizionan and Padre eurgos sik;cs , the San Juan c2id Ternate sites. In addition to adding two sites in
Cocciosion on 9.uclear Reacter Finnts 12 July 1979 3:00 p.m. Face .h implecentation of their candate, they icentified cr developed selection criteria for the evaluatien of these candidate sites. This criteria inc luded de-velo;: cent cocts for the considcied aite, one; .;o. i 2, potentially' disruptive and/or hazaricus pr.ysical and environmental effects; No. 3, the sceio-econcaic character of the study area, and, censicered the it-pact of future detailed studies uhich woulc be re-quired, including hydrographic surveys, accretion studies, erosion and siltation analysis, evaluatien, censideration of present and future land use, a".d neteorological studies. which is Table We now will show the next exhioit 2. CliAIPJUtN. Mark the same as Exhibit 16-D-SPO. MR. GIlf.CP.E. Exhibit 16-D, Table 2 in the papr once again presents what is still a qualitative as-sessment or evaluatien of the candidate rites by the cut:J11shed by the sub-ccc2mittee to the cc:mittee _ _ N Whilta > ,
Ccrmission en I- :lcar Osactor Plir.ti, 11 July 1979 Tac.;e 6 5:0C p.m. Precidential Order. The parameters have chan:,cd son :- what from the original 1965 work, now addrcused ac-cecsibility by both land and sea, identified as poor ror Cernate, das Juan 25 kiloceters from a nat2 onal 2 kilometers off the nearest paved road; and, Limay not stated, although with some confidence I know there is road access to that area.
.The sea access was not stated for the said sitec, Padre Burgos, San Juan, nor for Licay, or Bataan, and was identified as being potentially good fr- both N-sac and Ternate. Cooling water supply for Dagse was thought to be good froni the south China dea; a:.d with Ccod potential for fresh water fron rivers and wells.
The same was pretty much true for Ternaie. BW: :2r. Ses on the other hand, while cooling water was tnought to be plentiful'from the ocean, fresh water availabi-lity which is of course of para =ount importance, was
~
considered to be' scarce. As was also in the case un l
Commi:.;sion on acl..ar Reactor P! ants 32 July 1979 Fage 6 3:CO p.m. felt that a Lan Juan, additionally the sub-cor.2ittea
=ajor infrastructure would be required to meet sc:e ' of the ccnditions I referred to earlier concer.ung Limay, the re; ort challowness ci off-shore u ter.
g lg stated good coo'lin$ water from the ocean, Linay of course f acer; Manila Bay and the bay is quite shallow. Fresh water from Wells was thought to be available. The trans ission was not stated in several cases but not really of significance. Populationc were iden-tified, the minimum 3,000 within a 20 kilometer radius ct San Juan; 35,000 Licay; 31,400 Ternate; 24,000 Padre Burgos; 16,400 3agqc. Some information conecrning the site area and ownership is included in the evalcation. The coology was defined with four regional tectonic features cvfined at Bagac,five at Ternate, tuo at at dan Juan, Fadre Burgos , two, including the tow line and with no information for Licay. So:e informat' ion, very preliminary cnd clete - tary -- not elementary -- br relatively a li.:,ited se-infor:ation concernin;; scis= ology cuggested that
Cenninut.,n o$. i!ucicar Ifecctor Plants la Jt.ly 1979 3:00 p.m. Page p t r.o site, veral earthquakes since 1907 Int;nsity V at sinilar to Batangas where they recc raended accelera-tion of .25 to .3g for Ternate, the 19c8 carthi!uate 1 which resulted in Ir. tensity V at the site, also re-
~
sulted in Intensity V at the site at Tadre Surrics, 4 to $ San Juan and not stated for Licay. Foundations generally were thcu;;ht to be good below the weathering level for Eagac, feasibic for all the other areas. For soma information concern-ing the present land use. And once again on the ba-ci~c of obsc: vatica in the field , crperi ence , ciud c-
- cent, regional inforcation made available to them by various Philippine Governuent agenciec, the sub-cenaittee ranked the sites in ti.e following sequence:
I;o.1, Bagac; lio. 2,f2rnate; lic. 3, Padre Lurges; No. 4, Jan Juan, and,1;o. 5, Lincy. If we ccncider the cc pletion of that phase cf the sut-cor.;cittee work as Fhase 2-A, we can state that follouing that work, a phase which I havc described as 2-B in the 1222 292
. coral. aon en :.aclear Reactor Plants 12 Ju.y 1979 lage e 3:00 p.m.
paper, was initiated by the National. Power Corporation who ir.itiated studies, field studies in geology and fcundations in seismology and in water supply -- fresh g studies resulted'in a report in the January -- actual-ly two reports -- and February 1972 area, and a re-ccancr.dation uas made thet the Bagac arca Le civcn priority for future studies, including geolo;;ic nap-in;, drilline;. test pits and a test well pronran . tith rernect to the water supply. Phase 3 began in 1972 when the International Atonic Enerc-/ Agency sponsored by the Philippine Atomic Encrcy Cenniscien and with the assictance of the United Nation 4/ Development Program, implemented a feasibility study for a nuclear power plant in Lucon. Phase One of_this development prcgram, this feasibility study, resulted in the visit of an IAEA citing mission to the Philippines during the pericd 1 throuch 17 lIarch 1972. Their tission was to rank m D
Cerission oli .aclear Henctor Ilants 12 July 1979 - 1er y e 9 3:0 .p.m. in orcer of acceptance the sitec uhich had toen iden-
'fhe sub-tified by the Site Selection 1.iub-Coutaittee.
cc ittee forsed in response to the Presidential Cr-L . dji six der, un the ucrk of which had resulted in tite sites. I could' list the six sites if it is i:pertant, f cr the record, si
- CE/.Inl9d'. Fleese do so.
I;R. GII20.2. I should say, five sitec, sir.
-he Bagac nraa, the Ternate area, the F2cre 'curces area, the Can Juan aren, and, the Linay area.
ChaIRIUd. Are you referrint, to Table 3? 1C1. GIL".OH2. Excuse me for juct a eccent.
'40 are not
( r. 'Jilnore referrin;; to his papers.) . ret in 2able 3, sir. I was just identifyin; the sites cr:er ci pre-nat the IA2A Mission was to rank in t.".c f o re::ce . They were the sites that resulted fra..t the inase 2 investications by the citing cin-cco ittee
.:hich were lator,supplementcd by work cf ino ..ation. l Ec cr Corporation on two of the sites.
a .: J uiy en , ;:00 p.c. Foce 10 Fricr to I.hc initiaticn of ti.0ir activitics, r.ncrcy A..;ency Siti .C Mit-the International Atcric both sion stated that they would place a byrcline on s International Atetic Energy A$ency and United State d ob-I;uclear .<etylatcry Cotr.:ission Require:ents an earlier and as served -- as we have pointed cut the most important and cany have pointed out -- that Luton critical paraneter in sitini, and design of the
;ue31ar PcWer Plcnt was scismicity. 'A'he siCnificant citing paraccters '-thien t.ere . included addressed by this 1972 IAEA siting mission i hips, tectonic provinco , seismo-tectonic relat ons th9 site arca, the the seismic history of the site or the e ex-ccelerations, respend spectra taxitu Ground a defects, colograss, geologic faulting, volcr.nisu, wind Additicnal citing tsumani and wind generated uaves.
ne-para:nters considered to be important but of not as t.coe cecarily the c me critical decree of i port.ance included site floodin , micro-I have just enumerated, 1222 295
Cc cicsion e i i<uclear acactor rum , 12 Jt ly 197 1 age 12 3:00 p.m. the same ao the cricinal ficure 2, Mr. Ch air an, so it should ha-te the sa=e number,16-C. I chow it again just to rc=ind the Members of the Cc= _ission of the location of the five candidate sites. This slide is Table 3 in the paper and accord-ing to EEAS00 information s'.tould be 16-E. CHM 'diA'I. Page 10 of the text. Ilark it as Exhibit 16-E-!COC. MR. GIIJ20Fl. The IAEA Siting Missiaa in 3970 developed this ranking table for the five sites: Sagac, San Juan, Ternate, Padre Eurcos, and, Li:sy. the first was The siting paraceters considered, foundatich, and across the board we see 1:o. I which ceans ccst acceptable. That was the judL=cr.t of the IAIA Siting Mission. 'Jith :espect to micrc=eterology, all sites other than Limay received Ilo. 1, cost ac-ceptabic, Limay was censidered to be acceptable.
' lith respect to volcanic activity or hazard, EaCac, Padre !!urgos and Litay were considered tc ce sost i
N
..., 4!
29 6 1222
-- . . . . . . Msg
w.. m . . . . . . , . . . c c.. :n r.31 vn r n .. c u.w , 12 Jd y 19 t ia,e 13 3:CO p.u. ecceptable, *,::ile San Jucn and nrnate were co2.cidered to be acceptable. . lith 2:ccpect to flooding tne IAEa San 1;incion uas lachlag in information eencernine considered L;;r.c ac-Juan, Padre Burcos and Licay, but P00R Fit,BINj'[
" ceptable and Tjrnate leact desirable. !!o inforcation again was available to them on wind conditions -- I:a-xinuu wind conditions. '. lith respect to populatien centers ol' densities, San Juan and Fadre Eurgoc ucre ecnsidered to be =ost acceptable; Bagcc anc Ternato ac'ceptcble; Licay was leact desirable.
The ocean currents. The two tr.oct favored cites are San Juw.a and Padre Burgos; hatrac acceptabic, Ter-of nate leact decirable , and Limay primarily tec ince tr c sha,'llownecs of F.anila Day is probably unsecept-able. Tcunati hazard, most acceptab e at Gan June , Padre dur';os and Limay; accc; table at 23Gac and Ter-nate. Grcund chaking -- another way of saying severity a c;'o s s cf earthquake -- are censidered to be a proble.2 the teard for all of the sites which cnce ag.uu is
, . . -:v- :- ' ~ :. ;v u . ,c. . . s. ~
1222 2N
Cct.: nLucn on 14uclerr :tcactor 21an:.s li July 19/5
- h:;2 14 9:00 p.m.
consicLent with the findini;s ci both earlier and later inve ctiicatc ro. With respect to the effect on Manila, Litay was 4 considered probably unscceptable; Tornate lesce decir-able ; Fadra burdos, s.ian Juan, and liagac, noct accept-3 j ab2c. Sau3 ting;, for both Padre Bur,;os and Limay was thott;ht to be sufficiently severed in the proximity of the site to render it probably unacceptable; Bagac wnc ranked as acceptable; and, least decirable, can Juan und Ternate. The final ranking by the mission was in the crder across the top of the table. No. 1, Bacac; bo. 2, aan Juan; lio. 3, Ternate; llo. 4, Fadre Hurcoc; ana, Nc. 5, was :cro because the sitinr, missio: consiaered Iimay to be unacceptable and eliminated it from further cen-sideration. Cli..I&.A.! . Ilow, Mr. Gilmore , ac a Univerci ty professor I an acquainted a little with t; hat we csll, tests and mencurcE.ents, anu tiia ir a va ry ici,c o r t.. i t graph ee would like to find out .: hat guided you in ycur chcice of 1:a;;ac. You sec , one very cir..r lu .y
\
C ee..; _ . .. : ,c.. v: lear ileactor l'In:.1 u 1: J '.ay l'f/') % E
' a. c 16 - 9:00 p.n. 4:$ -
Ob Il g JN c: ,.ac..ing thue tests and ceasurenunts, cince you are graainl; the cost ideal or the most perfect with
!.e lo.ost Grade, one way of doing it would be to ,just as the numbers. Ana if we were to do 01:a;, it wculd appear like San' Juan has a total of 14; Fod.ro "urcos has a total of 14; definitely Ternate an:t Licay have But very hit;n totals with 23 and 21 respectively.
Ba;-ac has 17 which is much higher than San Juan and b -- Fadre Eurdou. The difference which is notable is in c;nnection uith f aulting uhere E:'gac has 1.'o. 2 a h1cher ratip.: than San Juan which has No. 3, arc Pa.:re cuc;;cs b whic1 hush. Could you enlichten us on the re.lative evaluatic,no cf .our ratinCs which gave th3 nod in favor of Bagac.
;ti. G1 DICA. 'Jitu ;. cur per=icsien, .ir, I ,,culd like to correct unat I believe cay be a mis-ic.pressicn.
Thi.s is a table prepared by tl.e IAiA Siting, I.is-cien in 1972. ESASCO at that paint in tiuc, had nc participaticn in any of thia worx cr in any of tr.e
~
cc.nnasi..n ca haclear Reactor 1 lar.t:. 12 July l'//9 Face 15 3:CO p.u. of gau.7,ing these tests and cea:urent.:nts, since ycu are grauin;; the most ideal or the most perfect with the louest grade, one way of doint; it wculd be to just add the numbers. Anc if we were to do that, i t. wculd ? appear like San Juan has a total of 14; ;-adro !!urcos has a total of 14; definitely Ternate and Linay 1.a/e very h!Gh totals uith 23 and 21 respectr.ely. But t Bagac has 17 which is much higher than San Juan and Padr- Eurcos. The difference whict. is notable id in connection with faulting where Bagac has Uo. 2 a hic,her rating than San Juan which has No. 3, ana Padre hurces whicli has\ d. Ocuhdyouenlightenusontherelative evaluations of your ratings which gave the nod in favor of Bagac. Pa. GII.M010.:. With your per=issicn, . sir, I would like to corredt.whav I believe may be a =ic-inpressicn. This is a table prepared by the IAS.1 siting his-sion in 1972. EEAsco at that point in time, had no participation in any of this worx or in any of the 9
Conuiscier, on Lucicar riants 12 July 1(, Face 16 3:00 p.m. work I described up to thic point in tine. If you will bear with the dissertatien, sir, durin; the 1 ster protions of this procentation, we do have an uddress to the question that you :.sked which will present the f3AS00 rankin5 approach and will I think ... CiuIFF.AN. An explanation of your ratings. 1t1. GILHO22. Hight, sir. P00R ORM dp1 Ciu,IR?ddi. We shall await the.s.
. MR. GIL:CRE. In addition to ranking the sites 'and clininating the four sites and elininating Linay, the IAZA recoinended further studies. The studies e:ere to include field investigatienc cs per the graph IAEA report, earthquato guidelines for reacter sites, to include f au'lting and ground f ailure ccnciderations, volcanic tcetonic, volcanic history, and physic-chonical studies, and with that we Iass to Phase 4 Phase 4 was initiated upon conpletion of the IAdA siting assignnent or mission as.:ignnont and d.. ring tnis phasc a feasibility for nuclear power plant in ._..___\1 Q _
Coc.aiccicu en I!uclear 1:cactor F1 utt.c 10 Jily 1979 Iv.,e 3 9 3:00 p.m. Luzon was devolcped and issutd in 1973 2 h is docu-cent uas in depth document and considertd the pre-
. ject feasibility fron both financial and tachnical e b -j Conuidered in the feasibility report, were electric load projections, the sizing and phacing of new generating units of all types, an inter-con-necped syctes analysis in the Philippines, anc also sc:e addressed to site cencideraticns. .etn rc;pe:
to sito considerations this 1973 feasiblaity .tport ccnsidared only the two ucct acceptable sitec -. t '. . at is, the bacac site anc the dan Juan site. Co:;1etion ci this nhase, the feasibility report, led to the I,ational I-o.ter Corpcrati:n ir.itiation of explor.itory drilling and the i=planentation of a tent pit a:.d cecihysical programs at tha bagae sits.. hc sacac site has developed in the feasibility report unice. in shown in the ncht slide which is figare 'i in the papcr.
Commission on z!uclear Reactor Plants 12 July 1979 - 3:30 pm - 4:00 pm Page 1 , MR. GILMORE. ... only an engineering problem. It is a process which must incluce nuclear licensing ccasideration and also environmental consideration. So, in offect, it becomes a multi-disciplino activity. And in the Philippines, on the Philippine nuclear pcs.*ar plant, as is ccmmon in our country, all of these re-disciplinec participated in the studica. I will show you, without going into the detail or the descripticn of the studies which I would say arc rather fully covered in the report, a conceptional cito development layout for each of the sites that we ccasidered in the vicinity of ... THE CHAIRMAN. Mr. Gilmore, so far, you have been sc.T.marizing what' is already contained in thi_ book that you marked as Exhibit "16", NPC? MR. GILMORE. That is correct, sir. T ll
ccr r.1s:;2ca un ..ce2cor nu a uur c.anw= 12 July 1979 - 3:30 pm - 4:00 pm Pago 2 PDDRORGNa . THE CHAIRMAN. Am I to understand that for the rest of this dissertction, it will just merely be a verbali::ation of what is already contained here? MR. GILMORi;. I was trying to avoid that by showing you some exhibits with minimum verbalization, and then to show you the ranking methodology that was used to identify Napot Point. THE CHAIRMAN. Perhaps, you can go SM t.- ,t to that ranking methodology, becauso whtit se intend to do is look over this Exhibit "16, NPC to see whether it is understandable and if we have ar.y cuestions, we are going to ask those later. Uculd you go straight to your methode,lo;7 .ad cali-hten us cn these points? MR. GILMORE. I will be happy to de that, sir. A minor method of introductory ccm:nontary is, I bc. lie v u ,
Cor. mission en Nuclear Reactor Plante 12 July 1979 - 3:30 pm - 4:00 pm Page 3 ~ necessary to make sure that the methodology is clear. By process described in the paper ... What page is this, please? T1!E CHAI'RMAN. Page? MR. GILMORE. This is frem a different report. This will require a separate marking.
"17", NPC.
THE CilAIRMAN. Mart that as Exhibit Proceed. MR. GILMORE. By a refinement of the work that have been done by others, EDASCO conclui.ed that the most favorable location for construction of a nuclear power plant in Luzon would be located in the vicinity of Bagac. We identificd in the vicinity the original a site at Saysayin Point; Bagac 1 site; a Cagac 2 site; and a site at Napet Point. a site at Mapalan Point; Conceptional development of each of these sites ucro 305 1222
- -~ ~ - - - -.
Cctreiscion en f:uclear Reactor Plants 12 July 1975 - 3:30 pm - 4:00 pm Page 4 prepared for purposes of developing differential , cost data. I THE CHAIR:1kN. This is another documst? MR. GIL!! ORE. This is another document.
'THE CHAIR 11AN. !! ark it as Exhibit "lS", NPC. !!R . GIC! ORE. . This is t!apot Pointecrmptionali.:ed and there are some similarities in the present deveelep-ment.
The next is the development of Mapalan Point, conceptionalized also in a new document. Mark this as Exhibit "19", NPC. THE CIL\IR'!AN.
?!R. GIL!! ORE. Eagac 1, a new Exhibit t:hich cnce again is the original site.
T!!E CHAIR'IAN. Mark it as Exhibit "2J", NPC.
!!R. GIU! ORE. Dagae 2, which w.7s a nudif(ca-tion of the criginal Bagac site is an attc.npr to evercome some of the problems identified by \l[2 v
Cor.c.issien on !!uclear Ecactor Plants 12 July 1979 - 3:30 pm - 4:00 pm Page 5
/
Hr. Tilford earlier. THE CHAIRMAM. Mark it as Exhibit "21", NPC. MR. GIL:! ORE. And finally, the Saysayin Point, the fiaal of the new exhibit. TI:E CIIAIRMAN. Mark it as E):hibit "22", NFC. MR. GILMORE. The first category of ranking of'the sites was identified as in our le):1 con list engineer cost related items. What would it ta::o to develop this site as compared to another sitc7 The results of these analysis and studios are centained on this table uhich is from the paper listing. It's on page 44 of the paper. THE CHAIR:iAN. .V. ark it as Exhibit "16-G", NPC. MR. GIL:! ORE. This table develops differential cost for the various aspects of site developr.cnt in-cluding the civil engineering and other ucrk associated 3
\'lqt
Ccmmiscion !!aclear Ecactor Plants 12 July 1970 - 3:30 pm - 4:00 pm Pa;c 6 uith the development of the site, the development of a circulating water system, trancmissien lines and engineer safety features. The comparative costs are included in ,the lines just about the bottom. By a i hrocess of inverse ratios, the sites were ranked en I the basis of their cconomic cost of development and the results show that the Mapet Point was the most vavored site. Bagac 1, 2 and Saysayin Point were more or less of a kind with respect to cost, and that Mapalan Point would be the most expensive of the five sites to develop. The next phase or portion cf the ...and there are quantified numbers. The next consideratien is en page 49 cf the paper and addresses in a quantitative way the varicus nuclear licensing considerations. And I think this is the first oppertunity I will have 1222 308
Co.raission -a !ucicar Acactor Plants
~
12 July 1979 - 3:30 pm - 4:00 pm Pcgc 7 to try to address your question befcre. ThE CI:AIFJiA!I. Table 6. MP.. GI:2:03E. Table tio. 6.
/ Proceed. Mr s . O rc: .t!.olt ,
THE CHAIP24Att.
"16"-H.
Prcceed. will you please mark my copy? Under nuclear liccasig consi-MR. GIL:!ORI. derations, wo identified various main headings to ified the population and dosage under which wa ident radius minimum exclusion radius; identified as chat s%ch
. t radiation does its use to human beings standing at that foundry, would not exceed regulatory guidelinec.
The low population zone Leing defined as ti.at zone being under the direct control of the
!:sticnal Pcwer Corporation, with population charac-tcristics permitting ready cvacuation in the event of a maximum hypothetical accident in the populc. tion 7 }
Cecr.1 s c i ', n :h: clear Reactor Plc nts 12 July 1979 - 3:30 pm - 4:00 pm 1>ago S center districtc, which is the distanco measured frca the reactor to the beundary of the nearest population center with a projected populatien -- projceted during the life of the plant of 25,000. And the distanco must be at least 1.32 times of the low population zer.a. These are all on Philippine Atomic Energy Ccamission requiramonts.
, The other categories we included are regional land use, meteorology, hydrology and the subject of much interest to all of us, geology and seismology.
In an attempt to avoid just adding up numburs, we devaleped a ranking system in which relative weights
- cre given to each of these five main categories.
As you will note,,looking at Table 6 on the screen, the relative weight for geology and seismology was 50%. That was broken doun'into vari; : -- th a t is, o
. .... . ~ . . --...- - -. . \iti!2. J
Cc.mic:!en on 11uc1 car Resctor Plants 12 July 1979 - 3:00 pm - 4:N P racc 9
$j j' cub-veighta situ st.1bility, 1 *. m J..rm,'le , ha 1 - e igt.t ~
4 If you will excuse me, I will have to go to the board and it will be easier. Of the sixty (60) points for gc.>1ogy and scis= ology, sites r.tability for ttose dept.'. tv groun veter, four; foundation quality, four; electric .ccion, four; except for dcun through this column. The sue cf th:sc adda up to six. The sa=a is true for hydrology,10; ceteorolo g , 10; regiossi land use, 10; and population
.r.nd dosage, 10 Of the available points in this coluco and on the h:st:
cf t;alti-discipline di:cussions, I g1sess c.ad e.syte, th=y could to defined in sc=o hases of artu;.zt.ts. k*e arrived at the cu=ber of points ti.at should be evarded to cach of the caniidstes of the available nu=bor and that is reprecented by the rest of tae radius. And va can 'see indications or situatior.a and whcre so=s citen rc:=ived zero point out of wk.st s.as
, _ _ _ . . . . . . .... -~
vo; n cica en ..ur lo..r teac to c 1 Ir.nt.3
.12 July l'H9 - 5: A p: - 4:C0 ;. .2 Pcco 10 POORORGNAL available.
Other cites received all of the a' rail.ible point.in a particular cater.ory.
!.t that point and ti.:e, after havicc assessed or attempted to rank or by 4'cicht or r. erit, the v:ricus parameteds, then we vent to more or less en an addition process, and the results are show.t on the bottom here with Napot Polut and Mapalan being the : ost favored sites; Sayscyin Point next; Bagne 2, 4th; and Bagac 1, a rather poor 5th.
So, Mr. Chairman, you can say why 60. And in fact, we did.ourselves why 60, so wu perfor=ed what we called consti=cc the sensitivity analysis or parametric analysis
- -ni we sddressed these numbers. 'Je unid, well maybe, yd ro i t.
. chould have = ore inport:.nce and we cive it . :itially and geolor:y less.
So, we uent throur-h this kind f La exerciso a .d uhile it ic not in the paper, ue aluays
. ; r. 3 out with the sso recult. We thour;ht that Justified .a celection of the relative wei:zhtc.
The last cection of the last evaalating facter in
.b p;per is en pcge 52 an:! it is Table ilo. 7. a table now en the screen and addressr:s cnvironmental ec:... ice;ra- .
c. 1.nd those were divided into four (4) catocorlec: 1
\oll '\1
Co ..macion c. Uitclear Heactoc Plante 12 July 1979 - 3:C0 pn - 4:00 pn g j aquatic ecolo;y, terrestial ecolocy, ccean hydrodynamics and frech uater usage. The relative weights to aquatic ocelegy, 35fs. THE C.%IM!AN. Just a moment pleuse. Mark this as Exhibit "16-I", NFC. Proceed. 121. GIU.0;lE. The terrectial ecolog/, 15?a; fresh
.vutcr ucage, 15f5; and the ocean hydrodyn1nicc, 35?s. Ine cun of the aquatic ccology and ocean hydroc7.aanica, a t0tni of 70;s cut of this total of 100.
Going through the ca:e process as addrocuca e.t Cable 6, we see that Napot Point and !!apalan l'oint once cGain are very cloce centenders. Bagac 1 and 2 and 5;ycayin Fcint are in a photo-finich for enird place or coccud place actually. Table 8 as chcun on P'ge 53, 4ili Le the next and the lact exhibic. TIC CIL ."..' ..'.l . Mark it as Exhibit "16-J", ;OC. Proce6d. , h .~ . G ILC.il. . This last exhi'.it raakc 'uw a Ave (5) cites en the bacis of the three earlier naf: top;cca
. u.
encincerin; cost related itcns; the nuc1::.c lim nsin; cu .ideratio7c; ann the envircnnental con:1d.r:ci.cas.
.a in all casec, Uspot Paint ranks Uv. 1. < } \1 }
0 , .1:2: ica ' aucle:.r deactor cl;.nts 12 July I')?9 - 3:!O p. - 4 :C0 in l',cc 12 Connequently, thereco:nnendation to the :Taticnal 2cuer Corporation for develegnent of the nuclcar pcwer plant on 2ctann ucc for !!apot Point. .6nd you can ::ec by 10 thin; s; the con.nositely readin; Juct ai;ove the r.:n':ing lir.e that the differences were relatively si.nifican.. i TRS CIU.I.9Cd'. We will cucpend y.,ur diccerta::ica fer cur own interpellatien for tancrrow nerning. .se will rececc for ten r.inutes after which we will recune with
*he interpellt.cien of the Ucstinchouce panel by the .%I.s da p an el . '.,'c reccca for ten ninutes.
It ur.c 3:45 e.n. i1 f g
9 0;.2.1.,aion c.. ;.u;1:ar 2 actor 1lanta 1 Culy 1FJ9 hce 1 4:00 p.:a. 3.~. L. , , -ava.
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(At 4:0. 0 n .n. the se cc.i on was .re stnvd wi th the Ch ai -
. .. n ,. :.on . 4e c .. -d oT ru n o , precidinc.)
r .. . ., . . . . . ,
. u .r. .L .u _6.. . T.,.e cession ic recu::ed.
I2. T:I./O:0, the COL: iccion understands you unnted to 4
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Ia g>Ji hdb 12. TII.FC2D. I feel that I .uy have created an in-ecrrect inprescien and I would like very nuch to correct thxt and to apolo';ize for having created that i::.prescien. I nado the rc:. ark at or.e point in our exchance that I felt the. 0or:icsicncr of Vcle,nolog, lir. Andal, had atte.:pted to ; gree with a number of positiona and in so doin; h J i l aced hincelf in n positica of agrc:.inc s.ith sca.c folks uha disacreed uith each other. It ..as an atte:pt at huncr sna was ccrtainly not intended to cc offer. Live to tlc Cea-
-.ics.cn -- to ti.ic Vole.'nolocy nor to thic Con.w.cien v.or
- o on; one cice. I an fully aware of r:y statuc 2c a cuact ni I bclieve I do not have n rcI.utatien of St.e?,,ing c:. the toca of ::7 friend.c and I do apolocize for the nicunderstand-in: cir. .
i5u C:!!.IM*A;i. , The .tord "0:nr.issioner U:.c :s .,nouc. s i n:. t in the reacon why the reaction uas in t..: ..':_:.; r i t c an . . 2.e '.c:l "O.1-. c:ioner" wa s ue 'd , i; did c.st spacif;' Cc i- _
..i c ,1:7.cr ..:d l.
1222 N
c u.:. : . . .. n ~ 1:1r: r U. .c:cr rl: nts i: alj 1, r.; E 2 4:f,C p.n. 1..i. OILiCJD. And I :culd not u:.nt even to ce offencive to Oo .:aic.:.ioner Andal. I:y reference was intended to be t, 12;,-ht o*- indicating that he had ocreed uith uu in a cortain ca.. c .1nd wit;i concens c1::c :n ..:Tothez cace and L:.ve thuc :: hi sif in c. pocition of si reeinC with pecplc who disc, : eed ui:L occh cther. And I stepped richt into a scrious poten-ti.:1.ticunderstandinc and I want to be cure thst you :.ecept
.;/ ' opolociac, sir.
2::3 CI'i. ink! 'i.
. Mr. Tilford, we snall not he any lacs ..en :'cus and sn.r less courtcouc. If we accc- i - cur s c:c,. lana-ci:.n- thet by "C:m:.1iscion r" you clid not .::n this Ocnniccio'2-'
cr !ny of the Co.:niccioners, and if you are r: ferring to Cor.- a.cci::ner .-dal, it was an at'cupt at huncr, .te chall t:.!:e that e:qilanatlen on its face value and uc thcnk llo-l. far it. I': tchtc courace to nake a rublic apolecy. . J .' thank you .'ad u- rc cyt the ca.o. In cc:.q.liance ..ith the request Of the '.ie.: ' ...cheus e ' .nci 00 the Ucrth Ana nuclear Plant incident, ue are handinc cv- r thic itc.1 frou the Elsnt Operating 1.x,'erience ni .:.cenctica, Chu panphlet of th? ::ucleaunics , beck .3pecial acpc.'t ,3 riec "c. 9 For 1: ek of copics uo uill only fur:. c tha '.!cc ti::c-v2.o Fanel and the 0:..:.ad: Fanol and se c a:. c . vc. thu 11 0
..nul, the cc,v e r:_.c n: l anel, one co,ry and '.'c invi t.- t h- "io :. + - . . . .,
1222 316
. c ri .. i :. . .. .:c l . o r .n .. .; , o e 13 . n ; u .6 a.. . . , . -)
1..;u y :LC :. 21.
?_:a1 to ....;; ne in cur o t'fice fe,r thcir cun copy.
1r. yer., haa his copy ulrc:dy, ue will .;ive t..e d:r.pn par.f,1 th2ir copy.
.!c ,ri] l acJ.c c t hi t., , fcr ; urpouc:: cf the Iroceedi.;t,
- .a 1ccuncnt :::. 14-D.
A'he Tafiada Fasel may proceed with the questicns.
.1 'IA2. 2 A . If Your Honors, please, it 1: with deep re;rct that ue caru st undertake a cross-c:.. ains tion cf the .. i:r.c t:: e of det.tinchouco for the following rencons: ... . . .e C:J.IL dt . Were the craphs broucht t the office c f T c nat:r Ot f.:. d:: 7 2.E . F :.G . Yes, sir, they were troucht to the offic c2 u.e C .stor yesterdaf r;orning.
i;i. 'f * .. A Ja . It is only this afterncon that we re-c >.ved these :tonographic notes, or tranccript of the ateno-t.. .;,.ic n: t e n . ' he cubject to:;tified to is t:chnical :nd
.....1y ccrplex.
It is a matter of cenera. ::nculed;c and t crecir.lly knoun to the Chair::an and the I:ent :rs of the 00.:-
- ..c: ion, that in ustterc like this, the opp;cic.c larfcr is
- J. .isy s c_ von a reasonable time to study the ctenaryaphic
.cto: tcrora h< undertakes his crosu-exar.ina'.icn.
Niiav:, if Your lioners , yl-sce, :nat i f t.e t r. t:
.. u rc:r.-s::;nine the Octinghouce uitn essec ',.c '.eill be uaivia:
c ;- richt to rw a conable tino f or crer:-c> ;.r' . i ticr . < c <::.11 1222 M7
, i t. UC .U c l' ' '(cas Lur ria:U. ;
ih v'id ') . '/;) 1.. '-O de 6:CL p.M.
.. e ..aivin; our purpose in ca.m ing to these proceuttnce, a:N that is, to sdcquately help in asc c Mininc tl.c truth and.nothin,but the truth. Uc will be cacrificing tha beat inte_;ct ;f our people if we try to crosc-cxo: :nc thcoe
' ...:nc._c:;, considerinc the len u th of thic tr n .cript of ctenom raphic notes. Considering also the chancing recition of ..Matinchouce -- I refer to only one and that is witl. res-Cc;2iccio; , ..ct to 1..-s-1 -- I pointed out to this c.oncrablo
- ..t in their cpinion there was no hydrocen bubble. ied to crate-;.unine them now with thic ch.uce that they are ncw I uttin; up -wihydroCen bubble -- will be to uc ver;. difficult, darthcrucro, in the two-hcur conference that we had tnis nerning -- very exhausting conference frcn 9:CO o'clucc to ainost 11:45 -- with the representatives of Uectinchuuco,
' c.o . ere hind enouch to unfold to us the pl.nte, Messrs. C.
Cnancy and J.n.:c Uctor, I cannet still see practically t.i.at
- uant to see, and that is, the artistic illuctraticL of the plant in Bataan That is one of the r.oct inportant evidenc-in thece proceedings and it is not availabla. Dr. Lin.:cns caid that it vill'be available af ter two ncnthe .nd a half. 'le are willing to usiit , if Ycur hs:ars , pl e. r . .:e will So,*.se recrat to announce th:.t henceforth, ;. o t avail cf the invitation te croca-:x.e:ine .:it ne c c e c uni.cs we have be.n civcn a rea. con ile tice , s ctun the 1222 3I8
C a :ti .: i c n c 1 .* -ler.r Resetcr p?o:tc
.6 ~.
w.. ..; . cs.s o .n l'.oic & 4:CO p.m.
- cuti:aony by readin;- the transcri:;ts.
, Finally, I uould like to stato th:.t wc also regret .......a.,-ws , 3.ac not Civan us a copy of the pecthlet on P kt} E.j i i fib 'tich Dr. Tilford has testified.
Thank you very auch. 21 C?.i!L J. Do you have an extra copy of that pan-
;.h2et, Mr. Tilford? You 1. ave civen four ec;ics tc the Oct-I incicn. Give ene of the Cc: mission s copy to Sancter Tc?.a d a .
You sro not ceinC to crcas-exanine even en the basis of tr.e stenocrsphic notes that you received this sf terncou, Sc ator? I'.li . '21... ?.01. . I ju::t received this. I have not read
- .e .
O:1 w:.!. G.N. 'iculd
. you e:< poet to be re.:dinc prt cf th:. snd ; hen ec:cence a fa.i on the points :. tc orrou's b.arin;? ::e matter how brief it uculd be.
l.R. CA...:.L. ' a f eu questions , perh:.ps , Ycur tiener,
.act to acco-. cd te the Cc a iccion.
Ti!L 0.i..:.. .!!. Sc, you can cc.ntinue tc cr.ow? C. . ';. . J.D.. . Yes, Your :fonor.
- 1 C.i..:d _:. 7 cry :all, f .'r tc aorre.. then the cen-1222 M
.2.;ric . on 'htcle:.r !?cc ctor I'lant: ' !. J u:;/ 1'//9 . ;. j 5 4:00 p.:a.
1;j.ucticn of the questioninc en the Nectin; house Panel
. :.1 t h< centinuation of the dissertatienc fer iba.CC. 'acc.sion is adjourne.'. until d:C0 o ' cloci: toaorrow e rr. i nt, . , .I_t _ t:
33 4:10 p.m. 1 L<2IFIC.?*C:
- . . .vy certify to the colrcat..:sc cf the fore- ,.oing trar.se:1pt.
Jttaceraphers:
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l'a g c - L-Op1 NJ::G 01: Till lil:Altl!.G (At 9 : 00 a :a . , the 1.c ar it:p, ci' the Coi i..in si c n on Nucl eai i!cacter Plants has convened) T1.c Chair-TliE Cl.11:K. 1.adic> and Gentleinen, please rise. 1:...n and the ractabcts of the Conur.ission. . The Coinmissien is now in session. Everybody is enjoir.ed te observe silence and proper decorum. Tj:E CllAIR!LAN. Call the roster of general and special ap-pcsrances.
'll!E CLERK: A'.torney Lorento Tr.nada - present Attorney Joker P. Artcyo - present llen. Jintonino 1:orun, Jr. - bsent N r . J ai.;c s S . Mo o r e - present Mr. Walter tlilgus - pre >cnt 1
( Nr. Ccrald Carroll - present
!. , 3 .d'lJl Mr. Jcnes 'l. Cronin - present 's C LI O Nr. Aura A. Simons - present 11r.11 avid ferg - present Nr. !;anicl W. Call - present Mr. 1:ayiuond Scro - Jl,sCnt Mir.ts t er I tchan - prescat Minis te r Catinaitar. - abrent Dr. iloxas (represented by Ms. ;cles) .lintster Velasco ' - absent lir , ba r tc l eti.e - alis c n t l' A l e t i. - prescot . : 3. .Nora Pctinc: - ,:li s e n t ':r. Tilford - pic> cut . C.i l r.io r e - p rest rit 'J. r . IIcal) - recscnt I
( *
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Ce ::i r s a c : . . . .. lear Rcactor PJ rnt s 13 July aph 9:00 A.M. Page - 18'- t iil C:i A 11;.'. s. . ?!ay the Ccmnissacn inquire if there are ad-dit:cnal Jo :uracnts or exh2 bits that will be presented by the i.e s t i ngt:c us e ? 1:R Cl.0 N I N . hone, Mr. Chaar::.an. 11!E LilTIID a N. J hc addendu:a is not yet finishedt MI: CRONI.s. We have received the intormat2on f rom Pittsrurg en the addendum. Tl!E Cl!AirO!AN. Nr. i.,ilinore, will you please go back to the rostru:n for additional questions. cuesticns from Justice 11autista? JU:>TICT. BAllTISTA. Nr. Gilmore, will you please open this 1xt.ibit "16", e n pa ge "lb- F"; I am referr2ng to page 12, Nr. Gilrao r e . Mi' . GILMC1'l:. Page 12. Jl:dTICE BAUTISTA. Exhioit "16-r-nPC". You will notice tren the d2agram of this conecptual plot plan of nuclear ger.cra nog station in liagac arca, there are two rivers, one on the north and ancther cn the south, and it saye " river diver:,1cn". I di.pposc that those two rivers are the Bayong(?) river and the K:.bayo river ? MR. CILMORE. 'I h a t is correct, sir. JUSTICE DAUTISTA. hhat I want to know is, do thesc two rivers c.stend to the p2cscnt site at Napot Point, Morong, Datuan?
.G GIL.MORh No, sir.
JiiSi l C1. II Airi l hTA . hhat woulJ he t he ;i gni fi . .nce c f t i.coe two ri'.cr8 if they wcru prescnt at the Na Ot Point? Dad you con-sider these factor 8 in ::aking Dague the most acceptable site? l 4l ,
\Ln .
e
Cet.cti r 31cn cn taa lcar Mcactor pl.utt s 13 .foi3 1979 9:00 A.M. page - '- 3:1, C Ilf.101:li . Mr. Commissioner, we did not nake Bagac the
- .c s t acceptable site. We made Napot point the most acceptabic sitc.
JUSTICE BAUTISTA. Yes, that was on the third page of the study. I think before you chose Napot point, there was a sc-lee r s en of 1:agae as t he most acceptable site. MR. CILN0ltE . By carlier investigation, that is correct, sir. JUSTICE BAUTISTA. Yes, by earlier investigation! MR. GILMolth. In our selection and recomicndation of Napot )
' peint a t, the r..o s t acceptable site, LDASCO did consiocr the impact of the Bagac cf the Laye 4g (?) and Kabayo river on development r ite
- JUSTICli H.tUTISTA. That means the two rivers contributed fate ably to the selection of Bagac site?
NR CI LMOR!! . Thcy contributed unfavorably, JUSTICL liatrilSTA. Unfavorably? MR GILMORL. Unfavcrably. JUSTICE HAUTISTA. In what sense? NR CILMCRL. In the sense that the rivers during monsoon scaun carry t rer1cndous quantities of water and the development ris, of the Sagac site would have had to face the very important cf f1 ceding during the construction. The adequate foundations fcr the r,agac site would have been developed or have had to h:iv 1 es: developeu at an cicvation apprcxtuately 4'? me t e r:, below ths 6.sisting grave. The materials overlying tne good foundation materials are fully consolidated materials and are saturated with water. Consequently, the stability of such materials woul. 8 l
\1&e 'l2 _
,; lear Heactor plants .
g g, g,, 9:00 A.M.
,l... 1 :> 7 .,
33 Y.e ,, s 3 - an additicnal concern related to the potential for damage, point i.ypothetical volcanie events as Mr. Tilford pointed, Napot
- = on a peninsula at a relatively high cicvation. The Bague site is a valley between two peninsulas and is at a very low elevation. Consequently, any hypothetical materials which might 1e e,iccted from the volcano could be guided topographically as 2t flet,s down the-side of the mountain into the valley.
Locating the power plant in a valley would have censc-(;uently exposed it to the possibility, in the highly unlikely in event ei any activity, to impact volcano materials. No have, g ; 12ne with this answer, a modci - a topographic model constructc2 Ml jrgj L P0D of the Bataan area to a natural scale. It is designed to show the .3pography, the topographic control of the relationship of the mountain, the peninsulas, the valleys, to the power plant. on ihat model will be received at Manila International Airport Sunday, and we hope to be abic to bring it to the Commission's
- eet ing or hearing on Monday. Ilut for the resent, locating the power plant in va11cys with respect to considerations of Lc1cano natcri:ls, we felt would be quite ha:ardous, much more a:ardous than the present location.
meters
.lubTICL BAUTISTA. Ilow many/ above sea Icvc1 is flagac?
MR. GILMORE. It is 18 meters above sea Icycl. JUST1G BAllTISTA. I am referring to the original llagac
-ate, nat the !apot point. ';l: . G I LNOHl; . The original lla g ac site was sciie t t.o tu thr..
reters abcvc oca level. JUsilCE ltAUTISTA. 'ra about the Moror.g Napo t poin;? Mi GILM0kt: 18 ueter8; much higher, and much h2gher in t en t ion. illy . I 2' 9u 725
Cornu : d ion o' ':uclear I;eactor Plant-a 13 July 1976 9:00 A.M. Page -0 - JUSTICD BAUTISTA. Let us turn to page 8 of this Exhibit "16". On the first paragraph, it speaks of a safety mission s,hich r.et in the Philippines sometin:e March I to March 17,1J72 to es.:lt. ate the suitability cf two sites for a nuclear pcher I ara not very cicar if these two site s is for a plant. nucle.tr power plant. Docs it refer to.two nucicar power pl..nts to be establishpd in one sitc? MR. GILMORE. I would like to explain to the Comnissicn that I personal'.y and EBASCO were not involved at that point in time. Ilu t I belicyc that the situatioi .s as follows:
, the icasibility report- - I am sorry. 1he site selection sub-committec had, as their mandate, rar.ked oc actually selected the sites which have been shown aircady as Eagac, Ternate, fr.
1urgos, S.in Juan, and Limay. JUSTICE BAUTISTA. You will nocice in the end of the second parar,raph, the last sentence of the seccnd paragraph, it says:
"the >iting mission mandate directed the installation of a >ccend unit of the same capacity shoulJ be considered a p c = ., i -
n21 sty at the selected site. M.1 GlLMORE. That is correct. JUST!CE BAtlTISTA. Did I get you to mean in this report that then you selected the Bagac site orip.inally and latcr on
.~.i :c t point in Morong, your fc.asibility study sways to the 6 s t blil i shraent of two units of nucicer plant reactor' m . C.itMolu. 1he siting hosL that ha ve bees. .'ene pr ar tc ! . ld S t d ' .- participation and dubsequent to 1.l:ASCO' par.tci- , s.t lea anticipated the potential addition of a securd unit to the aste. That is quite a comnon proceJure in sit 2i.g analysis.
P00R OR. BEL
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Cpaiisticn t Nuclea llenctor Plant 8 13 Ju1Y 1979 9:00 a.m. g Page 7-JUSTICE BAUTISTA. Two units in the same arca? fil: CIll!CRI.. That is correct. JUSTICli liUATISTA. We go now to... will you explain to the ccmmission how does this characteristic of off-shore ocea. current patterns in the vicinity of the proposed f.ite affect the selection of Napot point in Morong as the ciost acceptabic? I have Ml;. GILMolui. If you will hear with me a moment. to find the appropriate materials. Theccean hydro-dynamics i:: pacts a particular site location, any site location, are b:- sically two ways: first, is the ability of the receiving body of s ater to rcccive an anticipated wastage generated by the pos:cr plant, while at the same; time causing the Icast arount
~
af impact to the ecology of the area. As a second considera: ion, rc-circulation potential docs exist. And by re-ci rculating ; a-tential, I rean, the possibility of the discharge water re-turning at a short half to the intake arca for use in coolin;, or condensing of the stcan in t he plant . This can Icad to insfficicnt operation of the condenser cooling system, and w.uld in addition, be detrimental to aquatic life. 11c8c factors here given great weight in the selection of the sites and resulted in, as the evaluation shows, the Sai et point site being considered superior to the other cand-d.::c sites with respect to that perimeter. All sites were evaluated on the basis of its receiving capability and re-circularion potential. The parameter i.s given a very signif;- cant acight in the ranking process and Napot point was ccns.- dered to be the :nost f avorabic of all and P. ague 11, whicl. w_s tl.e slight modification of the original Bagae site, nas ju ' d to be the Icast favorabic; the next 1 cast favorabic was the Bagac 1. f
}222 327
n: wi- .lon en 'ucle.ir 1,cactor l'lants 13 .i .1 t ;. 1971s 9:00 A.Fl. i i,. e - s.
.'l'S ilCE BAU11STA. hhcn you conducted your feasibility study, Jid you envision the fact that the nuclear reactors P2 el'35eJ to be estohlished would get uater frem the occan; fra. ii.e sca? *:n. GILN01:L. That was the basic asstinTtion, yes.
JUSTICL 11AU'lISTA. You were awarc of that, that the vs..s t ers would np d voluminous wat er? 3:n. GIL.NORE. That is correct. h'c anticipated what is c.:!'ed a once=thrcugh cooling water system, drawing water j i JUSTICL liAU11STA. Now, what would be the significance g .i : c 'particular area of off-shore sea has ocean currents?
.V R G I I..MO RI. . I am not sure I undcrstand the yucstion.
Jt:511CE BAUTISTA. You said that you were aw:.re that this ut: clear reactor plant would use voluminous water frem the sea. MR. G I L.MO RI: That is correct. JlSIICE DAllTISTA. All right, i f t he of f-shore ocean curreat pattern in that vicinity is enormously discharged,
..sula that affect the selection of the site?
CR C ll::URL The quantitics of water th.it we are spe.iLin.; of and which you described as voluminous arc, rcr -i. Imint of view of the plant, yes, very large. But
;rs tin peint of view of the south thina t e.i , they are re- . . . '. 1 ..i.ill, and a properly dysigned circulating water . :. t i . ..It h approps iatcly designed intake and discharge 1222 328 .~
Co . u 2 :,sion ol 'inclear l'eactor Plants 1~> July 1979 9:U" A.M. p.i;' e . facilitics should result in minic.un impact to the, minimu , if any, impact to the nornally occuring ocean current pattern
- You ate sbper-imposing a relatively minor physical event on a jkj p vc ry, very ::ajor regional syst em.
JUSTICI: 11AUTISTA . On your page 9 of 1!xhibit "16", . there is a statement here rogarding th_c suggestion of the Intern.itional Atomie Energy Agency of the two ma in danger:, in the site selection, and nunbcr one is the possibility that new volcanic cones could upon up in the immediate vicinity of the plant and so endangering it with lava flows. hhat do you say to this finding of the I Al:A when you conduct.d your stuJy? MR. GIL'! ORE . With your permission, I would like to suggest thct it was the suggestion by the IALA and it was a su gestion that he truly agree with. As a consequence of the interpretaticn, the valuntion by the IAEA, the siting
.cassian recon:acnJed volcanic, tectonie, volcanic history and physical physiochemical studies of t hese. After the b : cin t ion of Napnt point, they were act ually perfon.cd in t.xtrene great depth by F.l!ASCO.
Mt. Tilford reported earlier that the actual studies and the sub>equent feasibility studies and respondir.g to the questions raised by both the Philippine Atouic incrgy L'c::m u .< i on a n d o t h e r s , I aggregated .some 79 years of cife rt , *l h e very major t.omponent of over .ill ri fort was
. . .h e r .. e d t o the two main danger.s identificJ by the I A t .'i ht.nber one is the possibil2ty that new volcanic cones tculd ci en up in the in. mediate vicinity of the plant and so en- ^{o, 1222 329
Cea r.*i s. ion i Nucicar Ieactor Plants 13 . lull 1979 9: 00 A.M.
..ir,e 6 10 - ,f. anger 2ng it with lava flows. And number two is possibility that ash flows erupted from volcano would enmesh the plant.
The result of our studies, and they were indeed ex-haustive, (in cur view, at 1 cast that exhaustive, and pro-Lahly raore exhaustive than any study that have been performed anywhere in the world for this type of project) were that 6 1 wVI\ of the Napot point very effectively protected it frt'm the very rer.ete possibility of having to facc the hazards of new vol-canic flows of any type from the volcano. USTICE BAtiTISTA. I rora your unsucr, can we say that t;.e:e tuo velcanos, nine kiicme,ters from the site, the Natib and Mariveles Nountains, are not extinct volcangs? MR. CILP.0RI: I did not say that. The volcanoes have been defined by COMYOL as dormat. As considered by L3ASCO, and as reported Gn in the TSAR, uc cannot preclude the possi-bility of volcano activity associated with the volcano, licw-et er, en the basis of very exhaustive samp]ing and scientific study, we have euncluded that the probability of such an escat is highly remotc. In the unliLcly event that any au-I tavat) might occur associated with Nt. Natib, he believc that, that activity would have to be physically limited to
- t.c cast side of the mountain where the last cruption occurced e s'70,u00 ysars ago. The materials ejected from the vul-co;.e er the east side of the mountain would pose no ha:asd t c t h e :,i t e . The one volcanic ha:ard which we feel that --
we teparted that the plant must be designed is for ash, and 1222 330
le.ir I;cactor Plants t:c...i-rion en . 1.; .luly 1979 9:00 A.M. I .g c that is not necessarily ash cir.anating from the nearby sole. inn ; it could be from other volcanoes in the vicinity. Thes e are n:any volcanoes in the Philippines. 11:STICl. ItAllTibTA. You werc a member of the group t h.i t undertook this study on several phases? All the tire y et: were a r:cnber? MR. GILMOR' . I was a member of LDASCO anc $1 LAM and S :ty work and the work of EBASCO with respect to PNPP 1 ini-ti.ted in the late fall of 1974 Jt:STICl; llAllTISTA. hhen you participated in that study, did you have in r:ind, in selecting Napot point in Morong
.u the site of the nuclear plant, tht actual situation of
- i. Iicld and Subic Day?
- ndiC0!tf. - C'WJ cld-mQ %b i.:._ ca y -s tcc Wh P08il DMGIN
. l p
- Omi s. i on On .' uc lea r Itcac t or l't.in t s 13 .luly 1 J 7> -
): 30 a.m.
I'. ge 10 JtiSTICE VASQUEZ. And what is supposed to be the
-ecpe of the work for which your services have been hired M *.PC ?
MR. GIL?iO:lli. I would have to...
.ll!5TICE VASQUr.Z. Just tell us in brief.
NK. CI D:0 Rl! . I may answer part of the question D t L.vc to answer that question. JUSi1CE VASQUL2. Let mc limit it to site selection. ti. GI L!!0R E . We were assigned the responsibility f:: preparation of Chapter II of the Preliminary Safety
',...i l p i s llepo r t or commonly cal!cd t he l'SAR (:1.a p t e r il u s la r.es the site characteristics and incluees detailed discussicn of geography, demography...
JUSTICE VASQUE2. Well, I think t.c will be insting lat of unnecessary time if we go into technical details.
.s are 3 tis t int 2 rested on this particular: whether you .w r e hired to investigate one particular site or four or itvc other sites or to choose any other site which .a be the most suitable for the c>tablislucent of u.. reactor plant. ' ut . G I LMORI. . lihen EUASCO was engaged, we werc sn.,ap d to prepare the PSAR, Ch.ipter il fc- the ., i t e e, a on l'igure 3, page 13 o f 1.x h i h i t " 10 .'. P t : "
Jt:SitCE VASQtit;. I do not talk your language
.a' ..pparently rca don't talk sine. \q22 >
Cemnission en Nuf! car Reactor Plants 13 J u l y 19 7 '.) - 9: 30 a.m.
" ige 9 MI.\1STr.rt ITC110N. Perhaps, it will help the one naking t he t est ir.iony. The confusion seems to be that there has been a precise identification of a llagac si[eanda Bagac area. So, the confusion arises
{hQ{ I l 08 4ibly on this connectier, and t nis is the reason ~ .f) bI j!,,M("i L uia he has dif ficulty in sayir g that !!nASCO was c e ra - g ti.<sioned to investigate not only the area aroun'd Sagac, including Bagac,but also even adjoining arcas heyend the initial Bagae site pinpointed by the I AF. A anJ recom:aended by the I Ai! A. I think there is a con-fusion here, Mr. Com:aissioner, because the Hague site 2 .4 , specific site that was investigated. JUS TICl. VASQllr.Z . I have always taken to rican the Bacac site that he was mentioning to include not only t ';; Dag:c-1 site but the general area to include Bagac al,
. .: c a c - 2 , .\ s p o t point and another point in the same arca 2 .!uding the present site.
Tt. C l !.sinR L: . That is, I thiak, possibly the cause cf car ntsund rstanding. JL:SrICE VASQUE . Is that what you mean?
':;i . C I I.'*J! li ! have been defining the liagae site a, that .hown on Figure 3, page 12 in Ixhibit " 16 .': :' C . "
JllSTICl! V.\SQUli!. Hut, at any rate, let us make thi> e l. a r . You here hi red by N1'C? T;. G i l.'iORI . That is correct, J:JS l i Cl: V\SQUC2. Not by pal;C?
'.s. C I L':0;il: . LUASCO services were engaged by .\PC.
Cor..:ai s $ inn en Nuc! car Reac t or I'lant s 13 July 1979 -
)' : 30 a.m. !'a ge S JUSTICE VASQUE;. So, it is cicar that it was mercly the job af LBASCO to find cut where in that general area of Bagac the plant would Lc, not to choose any other
> site. Is that correct?
. !R . G I L'40 R C . May I refer to a page in Lxhibit "lo-S.I'C", page No. 13. In the center of the pa3;e, there are listed some of the concerns I presented in the catlier testimony and the paper states that while none of the.<e concerns would in thensclves automatically preclude development of the site, experience strongly suggested that implenentction of the requisite engineering solutions ccald prove to be quite costly. .\ t that tir.c, we reconmended to the National Pcuer Ccrporation that in impicmentation of the work associated with P.agac and to insure the availability of a variable site for development , we broaden the scope of onr investigation somewhat to include confirmat ion of t he .i::ac site or, alternatively, identification of .inother daz!thic site in the vicinity. The National Power Ce:paration accepted our recommenJat ion and the work proceeded on that b.: s i s . !USTICli VASQ111'I. .
I have not received a c.stegorical an.,wVr to my question.
%. G il.'h ml . I am trying to slo t ht- hi s t I c.i n , *h, lac! ice.
- l N I S Ti.- R ! TC110N . Mr. Chairman, may I p l c .s > c . . .
lill. Olil mi\N. Minister Itchon.
. yL71 '
Co iai.oien on Nuclear I;cac tor i'lant s 1.t .luly 197'1 . 9: 30 a.m. p.i g e 7 3agac-1, Dagac-2, Napot point and another placc therc. Mi; . GILMORI:. Nell, what I really mean is that we g censiJer the arca from the Zambales peninsula to the
- .0.r.hern tip of Bataan. Ilowever, I would like to point out that in giving carciul attention to that arca, e dij review all of the available work performed by the original investigators.
And we also reviewed all of the original data j av.lilable through the auspices of' the various pl ilippine j tl. a.cencies and concluded that the early work do in site investi;ation had properly located the powcr plant in the et w r.il vicinity between the Zamhales peninsula and the Southern tip of Bataan.
.IUSTICli V ASQUEZ. You merely relied on their studies.
Ycu Jid not conduct personal examination and investiga-t ion Y f the oti er sites?
\M: G I Li!O::L Such as *.timonan as an example?
- UST ICr V '.SQUE . As those that you mentioned.
\m. GILMcP.L. he did not. I personally did not.
Gir s t a f f , gec log i ca.' staff, h..d essentially travelled
- !! ct sr the philippines and are quite f amiliar with
- r.e a;ea; l'u t the siting parameters r levant to the
.. J . loc.it icn of the nuclea r power plant , t he fault ing, w reisn icity are all relatively well defined in the li:crature and, on balance, the Bagac area is the Icast a-t:ve area ir. the Philippines.
q b gLu '
c .e.ission on Nuclear Reactor I'lant:, 13 .luly 1979 - 9:30 a.m. Page to first l'hilippine Nuclear Conpess w.is convened in
*:anila, actua!!y, in this building.
- Dr. Ibe, the Chairman of the Philippine Atomic r u r;y Coumission, requested that C3ASCO preparc a
;..mer f or prescijt at ion at that meeting describing the sit ,ng of the Philippine Nuclear l'ower Plant.
I personally prepared the parcr and it is a historic document really defining the entire process by which the Philippine Nuclear l'ower Plant site was selected. Prior to 1974, it wa s :r.y at t emp t to define lin.tery based on reports that were available to us. JUSTICI! VASQUC;. So, it scens cicar - and you can correct me if this statement is wrong -- that when 1.MSCO came into the picture it was aircady a foregonc ennelusion that i agac will be the site. M:: . G i l..01: E . hhen CBASCO c.une into the picture, t.., e.ir1ier work had ident i fled Itarac as the sit u o f t h s:
. ie l e a r l'o..er P l an t . That is correct.
JUSTICC VASQUCZ. And that is why you examined cuity Bagac as the possible site of t he nuc! car plant? Mii G I I.'l0lt h We examined Bagac and really the i.a :aC .i rc a .
.hlsT I Cl. O S Qti!. . And by that you me.in you include P?@ gg y .
s222 '
Cormi ss ion on Nuc le.ir Ucac t or Plants 13 .luly 1979 - !':.W a.n. Page 5 of the Philip [iines, who had concluded that t he !!agne site was the most favored site. 1;ilASCO has engaged as a consultant by the National Power Corporat ion to prepare the necessary rep datory reports necessary to f) . NT. license outside.
.IllST I CC V,\SQttr. '. . You will pardon me, but i get more cont'osed everytinae you answer :ny quest ion. My question simply is, when you were hired by ':PC, your job was simply t c, e.xamine and evaluate the llagac site and no other site.
Oi, did you have a hand in choosing any other site aside from Bat;ac?
, MR . GI LMORl; . At the time T.IIASCO was engaged by tiu National Power Corporation, it was assumed by the Nat:onal power Corporation and others that Dagac was the site.
EBASCO did not participate in that decision at that point, or prior to that point. JilSTICl; VASQl!!!!. Now, if you were on!y suppose to examine and evaluate the Itague site, why is it that ycur charts show comparisons between the Bagac site and ical for othcr sites, like San Juan, Limay, Aticonan,
.~ a : tate.
What would have been the basis of the data
- t. .: you put in those charts, if >ou did not examine them?
.it R . G I LMORl: . The document, fixh i b i t "16-NPC",is et .1 f oi ma l report prep. ired as pa rt of t he PNPP hurt. .:a t he r , i n 1)ecen:her o f 1970, under t he sponsorship of t he 'h i l i ppi ne At omi c 1.nergy Connai s s i on a nd wi t h t he p.irt i c i-p.- '. i nn o f t h e int erna t iona l Atomic linergy Agency, the
i ot..it ss ion nn Nuc lea r He.se t or Pl. int s 13 July I 'J 7 9 - 'J : 30 a.m. I'.i . e 4 IAl.A Mission in 1905. They were subsequently expanded by the subcommittee established by t he l' resident ial Order and the Que:on Province and 1:atangas sites
., c r e ident i fied by es sent ial ly t he subcoir..ni t t ee.
l .!US T ICI'. V ASQUlII . When 1:P.ASCO cane into the picture, t hose sites were ai rcady Jct eimined? MR. C I I.MOR1. They have been determined and"the subcommittee and the 1972 IA1:A Siting Mission had eeneluded that the llagac area was t he inost favorable location for a power plant sit e. . JUSTICE VASQUli2. If you will just a n 3 >.c r r.iy u ue s t i o n as I asked the question, rnaybe it will take less tir.c. 1 .t m j u .< t asking t,hether when you came int o the picture -- I mean i:llASCO -- you wcre already told these sit es that you were supposed to study. You had no say in el.aosing other sites other than those mentioned? SIR . G I LMORii , l.'c were not told, to my knoieledge, to study any site. We were b.isically init lat ing work the !!agac s it e . Our original nanJate was to develop
.i -afety analysis report f o r !!agac ,
JllSilCl! VASQUIC. Ycu mean t < < ell us that you were
< . l y told t o s t t.dy t he Itagae s i t e , nathing else? *tu G i l.\;M L . ho, he ucre not t o l d . ins t h t :6 of t: ,
tspe, *Ir. L:c.ua i n s i o n e r , he teir ent ri i ng into .. 3ite scleetion process t h.it h.id been going on for in s e. irs by responsible agencics, both i nt e rn.it inn il and
\1b
Ca...:r. i > s io n o n No e l ea r itca c t o r I'l a n t s 13 .laiv 1979 - 9:30 . ia . i' a : . 3 sunsequently a bunker which we rented in a barrio of liagae, reconoitered t he entire area and we selected the 5ites. Jt!STICL VASQ'JEZ. lihich sites? SIR . G i l.310!!E . The sites that were selected were a c t u.i l l y d i x : , Starting f rom the nort h an 1 working scuth, they were Napet point, Maba lor. point . Bagac-1 ra n Ok site was scicercJ since it had been previously selected. e: S I .).3(fa5 u 44 rw . : wu yy 5 11.i g a e - 2 wa s included as a possible close alternative to l'agae-1 and Saysayin point. In addition, another point or peninsula to the' Scuth, Caybobo point, was considered as a potential
.- u e b u t was eliminated relatively early in the studies a n.1, c on sectuent l y, is not included in the repcrt.
That is the site, sir, in the inmediate vicinity
,. lu gae se lect ed by 1.11ASCO. .ItlST I C1' VASQtil.: . . I think we are not speaking the .une language.
31:1 G I I.MO'il' . . I am sorry, sir. JUSTICl! VASQUr.Z. I am only asking who che>c the
- s c sites that you mentioned in your paper here which
- :uded San . Juan, llatangas, Tarnate... '!R C l LMulti. (1h , I am sorry. .IliS !' I Cli VTSQ1U . ..Cavite, A t i nno n.i n in tjue ;o n , . . .U ga e ite, J. i nia y , 'IR C. l l .MO R I-. Ilot h site were selcet ed eit her hy
Co n. . i s s i on o.. Nuclear Rc.ictor Plants 13 July l 'J 7 9 - 9:30 .t . m . Pay 1 MR. CILMORI. I would h.'ve to say that they were chosen by myself and Mr. Tilford. I could explain 8 possibly the earlier question concerning the suitability of t he Bagac site with my service preamble to my answer to your question.
, In February of 1975, Mr. Tilford and I came to the Philippines for the first time to make an ocular ins-k pection of the site arca and to review the results of the on-going field programs.
During that visit, we inspected the test pits that had been excavated. No observed the enrcs that had been recovered during the drilling process. We chscrved the fact that cach of the holes that have been drilled was producing water under pressure at volumes in the order of 80 to 100 GPM. This water was heated, h ving an average temperaturc possibly in the vicinity of,115 degrees and was alkaline in naturc. 1 mentioned earlier that we had concern 3 regarding the suitability and stability cf the materials. I had
. inn.cred earlier that we were concerned about the flooding of t he excavation by the Payong and the Cabayo rivers.
JUSTICE VASQUE2. May I interrupt, Mr. Gilmore. I un j u.e. t interested in finding oat who chose the five c..n'Jidate sites that you studied en t he possible site of the PN i' P - 1.
.MR. GILMORC. After our inspection, Ir. Tilford and 1, using the National Power Corporation helicopter and e e=-e w% ___ -h a e e up ,- e
C. caission on Nucicar !!cactor Pl.ints I; July 1979 - 9:30 a.m. Pa;,e 1 MR. CllMORE. Clark Field and Subic !!ay surely esist. They were surely considered in the siting studies.
) if ['g gg j[gg 1 hey were considered by !!BASCO from the point of view of i
ww n IJb g, inpact of the aircraft on the site area. In the United States, location of nuclear power plants in the airficid, si an exanple, is carefully considered; and, unofficially, the US NRC will not
.trongly question a site.for a nucle.ir power plant as long ;is it is in excess of five miles from the nearest runway. This is an unofficial position, of course, but it is based on the results of very exhaustive probability analysis, studying the crashes of airplancs -- of lanJing and taking off frcr airstrips. *nd unofficially , the NRC feels that if a plant is located more than five . i l e .s frca the end of an active runway, either inecming er outgoing, there is no credible hazard for impact of aa .i: rcraf t on site.
JUS'; lCE B AU riSTA. Thank you, Mr. Gil nore. lill; CilAllDIAN. Justice Vasque:.
.luSTICl! V ASQllf.:. Sir. Cilmon e or I)r. Gilmore?
SIR . G i l.MO R f. . Mr. Gilmore. Ills fiCl; V ASnlll; . Mr. Gilmore, I heard you s.s y there w, , ah0nt four or five candiJate :, i t e :, that you studicd? 11 2 . G I L\t0R t: . That is correct. JtlSTICli VASquf.2. Now, thcsc sites, these candidate 8ce, were they chcsen by you or by somebody else? e
\111
l'- !i 4 ? I oll en ' ale le.I r h'v.le t o r I'l . a t s 13 .luly J:iN - 9:30 a . ni . P'e , 11 M:i . T0::R L:5. Mr. Chairman. Till: Cil il l: MAN . Mr. Torres. 5:!; . 10 f:K r.S . May I attempt to assist the quest ioning ! kj u;,. d f.11 w 51'$ Com issiones , LSASCO was hired af ter the NI'C had already cl o -( n a site which was lia ga e . The services that were required of I'BASCO would be to use this site to develop or proceed with the rece3sary investigat ions and cotine up wi th t he iequired it. characteristics that we have to define in t he sa fet y document he tr.u s t submit. In thc process, I.BASCO carly enough had some findines s.:: t ch made t hen conc lude t hat it would he prudent and not on t: necessary but also advisable that we do not end up
- s. i t h Bagae but to broaden the investigation while the o ppt riunity still existed of inve tigating other . ire.is
- 1. - the vicinit y hee.iuse o f probleus that were aiscady a ins uanit'e led by the intensive invest igat ion that pro-cc.acc.
This is how the studies of ot her point - in the general a r e .. l i k e itap.ilan poi n t , .N a p o t , Saysayin cane .ihout. ' li.e .Na t i ona l Poher Corporation a;cepted the r e c oma. : n -
,' a : ..nai I B ASt't) to do a broadenet! 34:e i n ve t i n.i t i csn oi,,
was not limit ed to Cahayo point in H.i g.ic . \ad
- i - i3 why we ended up with Napot point.
.!ilSl ! Cl. V.\SQUF.Z . i think you till n i sus.d c r s t a nd I aa t ryli.g to drive at. 't h i s i3 the difference 1
f0'
Coualision on Nuclear Iteacter Plants 3 1 July !!i7-J P.i ge l'
- 9: 30 a.m. }' ll J ) h Mg, d ,7 1 ; . .s between technical iaen and laymen like ourselves.
Mit . TORl;C S . I am sorry. JUSTICE VASQ!!EZ. Let me put it in another way. 5:r.ybe we can go to what I really wanted :o arrive at. t..:/dC0 had no say in comparing the Ba'gac site area --
. .i .i t would include all of those points mentioned -- with other sites, for example, a site in Cagayan Valley, or in Central Lu:en, or in the Bicol area. You have nething to .<.iy about tila t ? ' t.i . G l i.' Olm . he were not involved in that.
JUSTICE VASQUE2. You were r.:crcly told to see if t.c site previously selected by NFC was good enough for a reactor plant. Is that correct?
':11. GILM0itt. In a sense, yes, sir.
JUSTICE VASQUE2. And were you free to tell t h er.' , . i f yon e i nve s t iga t i on
- t. i ll so determine the existence o'
ecriain defects of the site, " lion ' t put it there." s' ,
- s. e r s ycu only supposed to inJieate in t. hat pa r t i c u ! .2 r y .ic e in the area you here supposcJ to examine the plant
. . ' . he put up? ! G I LMC!J . Ne Were frec to ma ke reco:r.r.cnd.it ions ,
y e. And in fact, he did.
- llST I C1. '. A5Q'!E; . To reject the entire 2rea?
i:/ G i l.'.M::E .N o , t.e dad not i... L e t h.i t r.co..miJiti a.
"JS'i ! Cl.' V \5Qll!.: . I ccan, you could have told thct. 'l:: G i l.'lJ h i. We could hatc, yi -
t6 .138i0:'. On . .!C l e.i r G e..e t e r l') .i n t s 1I .ja!y I '.3 7 ? -
'.) : .3 n a . m .
i' , . 13 JUSTICl. VASQUEI. And you ca.:.c up in t h t!.c finding t: at t he site teas good coeu,;11 if > cu twould put it at
- s a i'0 ! point ?
' tii . G : L'ml?ii . tic found thru our work that the site .a s the site defined, as you are defining it; and of all the points i t. .the area i- w a .. most likely the best :ite i:' the philippines.
JUSTICE VASQUEZ. The best site in the philippines er the best site in the liagac arca? L: G 11.'.m!:li The besL site in 1.n : o n . < . . , 4j
- j g JJS!!CE VTSQUEZ. 11 0 .- can you say that when you did
..at ex.mine the other places?
Lt. G il." Hil: Thi* s on the has . o f qu.i l i t a t i v e c o:w .d c r.i t i o n s . You tall rem aber yesterday when I w::s d..scr:bing the work of the earlier investigators, it
.as on a qualit at ive basis. I're l t n i n.i r; piia e.s o f s i t i t.g .'e s t i .. t i o n are done on tht basis of avai l ihl--
c.t s'.' ion n.f j u g tne n t a ntl e s ;'er t ence. le au cx! rple, t he .\t i aca. n site is loc::t ee ve rr
- ? .3 the !"li l ippine f.:u l t . It does not to ai re s cr y re.iearch of the literature to leara :l.a t t i.e ri t iirnine fault is one of the *:ajor tectonic structures of de .orld ar.d very, very active in a sci c.c sense.
ti
-equent1 , an enp.incer experienced in :-lli.e: woul1 e m : .- i d e r laca-ion of a nuclear pa er l' ! a n t in .U' . Itie t I.a t , ..W. i I t ' V W.M. ; . But did you n r. t say t i.a t you en!y \
t'o.":i s 4 ion on Nuc lea r Reac t o r l'ia nt s 1; .luly 1979 -
)' :30 a .m.
page 1 -1 c sa:nined the flagac arca? Nhat could be the basis of your comparison between the llague are:i and the four or five 3 Q ghW 3 Q ig,h e.: he r sites that you are mentioning? It is related to the regulations of the MR. Cl!J101:li. Ui .Ni:C, particularly Appendix A to 10-C Fil 100. In studying a nucle .T power plant site, one, in point of f act, actually has to study the various levels of depth. An area having a radius of 200 kilometers centered on t he s i te. . . JilSTICl! V ASQLil!!. l.c t me interrupt, Mr. Gilmore, iour finding as to the Itagac area was because you or In other words, ycur staff actually examined that arca. tt ,is first hand knowledge. Now, your evaluation of the other sites was based on data not secured by your aen but frca the studies of other pcopic. Is that correct? that is the inpression I get. Mll . G I LMaitli . Much of t he dat a available in the taily phascs was available from other people al o -- in I am not trying to be t he case of the L'J ASCO studics. sitfiteuit. JUS' ICE VASQUli!. I only wish you could meet me head on with the questions that I am asking so we will bs -aving a lot of time, I am sure, Mr, Gilmore.
\ll: Gi l.M01;l . We had significant literature, .ehnical literature, available for all of t he l'h i l i pp i ne .irca in a radius of 200 kilometers centered on 15agac.
That included all of the site arcast so, we did know 4
=
1 f 0 'h
Conmission on Nuclear Reactor 13 July 1979 - 9:30 a.m. page 15 quite a bit about them. { Q $,J Ne concluded on the basi,r. of that review of the
'4 6*h ]
u' U$ Nd i s L. previous work that the Bagac arca was, in f act , a very i suitable location for siting ;a nuc] car power plant. It is true that we did not drill holes or excavate trenches or pits at the other site areas. liu t that is r.o t necessarily required in the early phases of siting investigation. JUSTICC VASQUl!Z. Now, when you reco:anended the Bagne site, was it because you think it was good encugh or there is no better site in the Philippines? NR. GILMORE. We belicvc that the Bagac site, as per your definitier., is the most suitabic site that has been identified la Lu:en or, with all things being considered, for the development of a nuclear power plant projcet.
.lllST I Cl V ASQUlIZ . Ilow could you say it is the best tn Lu:on when you did not examinc any other site?
MR. GILMORE. May I refer to Exhibit "14-NPC," which is the colored photo;;raph, as an example of a scismic risk analysis. That diagram, although not ava,ilable at the time of the 1 ': ' studies in the detail that it is presently available, was generally available.
'md reference to L xhibit "14-NPC" will show that with respect to scismisity, we acre quite knowledgeah'c concerning the scismic activity in Lu:on. The same ,o),v tab \v-
Conr:ission on Nuclear Reactor l'! ant s 13 Jcly 197!) - !):30 a.m. Page 16 ceald he said for oti.cr types of geologic knowledge. In studying a site,tfr. Commis;ioncr, you don't just study the site. You have to study the region in which the site is located so that you can understand adequately and completely the problems that might lie associated with' developing the site. - A PDBR Dil!G! Nil 9 s-xv
Co=miosion en ?luelear 10:00 Reactor Planta a.m. 13 July 1979 , Eage 1 N q GILMC32.- . . r.-developta?) theLaite. JUSTICE VASQUES. ' Were you made to understand that the site t from Manila? rust be within a certain distance
- , - "e"-
agg gkguL I JUSTICU VASQUEZ. In your study lof the arose in the FPilippines as to their - I cannot use the term'that you are using '- as to their possibility of being affected by earthquakes or volcanic activity, did you not find any other place in Luzon which ic not as prone to be cubjected to cuch activities compared to daEac? MR. GILMCRE. As shown on Exhibit "ll+-NPC", there is an area of r'elatively li ht 5 seicraic activity located in northern Luzon, if that ic the question you are asking. With the exception of that general ares, all other areas in Luzon are much more active in ( sei.mic termo. JuaTICE V ASsU ::Z. That i- quite far from !!nnile? lla. GIIJ:Ch'U. It is quito f ar f rom Manila, yes, and in an engineerin5 sense, one has to consider where the power that will be g r.erated is to be used. JUSTICE VALaUdZ. In short, the plant must be comewhere necr Mnnila for certain economic reascns? MR. GILMC3Z. The Plant or a power plant would no mally be located with renpect to the power distribution ayotem of the utility. It has to be, located sosewhere where it can be tied into the distri-bution network. ' yh gU '
Co= mission on Nuclear Reactor Plants ' 13 July 1979 10:00 a.m. PaEe 2 JUSTICE VASQUES. And of the places around Henila and near enough to !!anila, Bataan is about the boat? MR. GILMCRE. I am not sure I understand your geographical definition of "within the vicinity" or#near to Manila". JUSTICE VASQUEZ. Well, it a radius around Manila, as far as
/
Bagac is to Manila. MR. GILMCRE. I would agret with what your statement is. JUSTICE VASQUEZ. So, you have to take Ba6ac as is, with all its advantages and disadvantaSea; with all its volcanic possibilities; , with a'll the faults lying in the ocean floor and other hazards? F.R. GILMCNE. I have tried to explain that the hazarda, the faults in the ocean floor, we are well aware of them. In fact, we located one of them during the study, the Manila fracture belt that All those faults, have det previously been identitied by anyone. I have had associated with them, major earthquakes en a postulated valuation risk and the acceleration /Kalucz that have been de.-ived for design of the plant are based on the existence of the faulta. JUSTICE VASQUs2. I will simplAfy the question. If the plant
.111 have to be established around Manila or in the radius equi-v ale r.t to the diotsnce from Muriin to Bogsc, the only possible place, or I would say tne best site would be Eagac?
MK. GILHCHJ. l'es, Sir. THL C!!AIRM AN. Atty. Ilao, you wish to say something? m
Co=-ission on buclear Reactor Plants 13 July 1979 10:00 a.m. Ioge 3 ATTY. ILAO. Hr. Chairman, may we request' for a suspension of five minutes because we would like to confer with Dr. Gilmore. I think ho is all confused by the questions of Justice Vasquez. . THE CHAIKMM4 Session is suspended for five =inutes. It was 20:05 a.m. , f RESUMPTION CF SEOSION . At 10:11, the session was resumed. THE CHAIRMAN. Session io resumed. ATTr. ARRCYO. Mr. Chairman. THE CHAIRM AN. Yes. Atty. Arroyo. ATTY. A320YO. We just want to make this observation, namely. af ter the recess was called, Mr. Gilmore was surrounded by the NFC staff, NPC lawyers Lad they wonferred. We thought there was a ruli=g here established in the case of Vestinghouse, that when an expert testifies, he may not confer. THE CHAIRMA:4 That was the rule at the request of the Tanada Panel while they were cross-examining. Now, at this stage, it is the Cc==ission that is asking the interpellation and we are taking the sese view that Senator Tanada originally took in the beginning. If you will recall, in the beginning snen there were ciesertation, the oriS inal attitude of Senator Taf.ada was, they could confer -- anyone could answer 'uecause the only thing that they are after is the truth. You =ay set your own rules when you make your interpellatien. GN
Co :ission on !!uclear Fenctor Plants 13 July 1979 10:00 a.m. Page 4 . ATTY. ARROYC. No, we are not asking.... except that we thouEht that the understanding was, if a witness is unable to answer questions, then he may refer it to another witnces, which we have no objection. THE CHAIRMAN. Let us have the NPC panel make their own reply to the statsment of Atty. Arroyo. gi)' q ( 0U ! thi j
~
da ATTY. ILA0. Mr. Chairman, this representation asked for the cuspension of the hearing purposely to acquaint Dr. Gilmore of the nature of the proceedings and the way it should be answered. The NPC Panci just gave him the direction to which wo believe that Justice Vasquez was leading to and no more. TH: Ci! Allu. AN . Any further remark from Atty. Arroyo? ATTY. ARROYO. No remarka, Sir. THi; CH AIRMAN. 'eie may proceed now with the interpellation. Is there a pending question or do you want to rephrase it, Justice Vasquez. JUSTICE VA3(UEZ. I think I nave already been clarified e=ough. I have no more questions unlese Mr. Gilmore wculd like to clarify hl=celf. G. GIL"CIG. Atty. Ilao basically told me to stop acting as an eniir.eer and just say "yes" or "no" a6 much as possible. I truet that I have clarified,that you understand my answer, Mr. Juctice. T35 CI:AIHMAN. F.arther questions from Juctice Bautista? JUSTICE BAUTISTA. Junt one question. If my memory serves ce 4 I h
Cc:r.issior. on !!uclear Reactor Plants 10:00 a.m. 13 July 1975) Tage 5 this feasib-right, I read from the newspaper about the time that ility ....; of sne site is being made that San Juan Batacgas is ene of the candidate oites of the nuclear plant. The people of San New,
- Juan, Estangas objected to the construction of the site there.
i Mr. Gilmore, during the time that you were conducting your studies, didthisnewsite[cometoyourattention? . MR. GILMORE. San Juan, Batangaa? to JUSTICE BAUTISTA. Yes, that the people thero did not like have the plant constructed there.
. R. GILM0!!d. That was not brought to ey attention.
JU2TICL BAUTISTA. Now, I will give you a last chance to answer i ! - what seems to be confusing your mind. The question is, since you 1 w N 06k2U P La* did not make an actual study or ocular inspection of other placcc in the Lu:en island where to construct the site, what could have been your basis in stating that this Napot point or Bogac site is the nost acceptable among the candidate attes? MR. GII. tCRE. Starting in 1965, local acd international res-rencible agencies identified various candidate sites and concluded that the Sagac area as the cost suitable. Therefore, other candi-In the Bagac cate areas in the Philippines must be leos suitable. area, our work satisfied EBA000 that the Napot point site in the test area in the Eagac area. Consequently, for purpocss of this r,tudy, the Napot point site cust be concluded to be the test site la Lunon.
\1N
Cc..ciobion on Nuclear Reacter Plants 13 July 1979 10:00 a.:.. Page 6 - JUSTICE EAUTISTA. When you said you studied it, what reference is that to this document that you submitted, this Exhibit "16-NPC"?
!!R. GlLMCRE. Our studies could be described starting on paEe 12 under " Phase 5-A". Essentially, from that point to the end of the paper, there is a description of the work that E3ASCO performed.
e
;USTICE BAUTIsTA. That will be all.
THE CHAIRMAN. Do you have any concluding staterent Mr. Gil= ore? Md. GI LMOR E. I do have the slides of the rivers that you have requested, Mr. Chairman. I could show them to you. THE CHAIRMAN. May we have them. You mean they are slides, not docu=ents? MR. GILMCRE. They are alides. T!!E CH AIRMAN. Tb' was in answer to the question of Juotice Bautista? F.R. GILMORC. That is correct. You asked for the slides; we have them here. THL CHAIHMAN. Very well. (First picture was flashed.) Pk. GILMcKL. This is a photograph of the first exploratcry crill hole by the National Power Corporation wl.ict6 was lcented at the central line of the containment building for PiFP-1. THE CHAIRMAN. Mark this as Exhibit "23-NFC". Please give Justice Bautista time to interpret while each figure is flashed en I
Cc:missien on Nuclear Reactor Plants 13 July 1979 10:0C a.m. Page7 the screen before you go to another figure. JUSTICS BAUTISTA. This photograph has connection to the question of the Commission on the two rivers? 9 ER. GILMLRE. It is the two rivers and the ground wcter that
! we were discussing. l ~
ed wiss.m .. ; e - JUSTICE BAUTISTA. You may proceed;and identify whether the river mentioned in the question of the Commission is reflected in that photor,raph. . I
!! A. GID' CRC.
Un fortunat ely, one of the rivers is to the right, the other is to the left. They are not specifically included in the' photo-raph. JUST.;E 3AUTIOTA. You may proceed. (Another picture was flashed.)
' TII: Ci! AIRMidi . Mark this picture as Exhibit "2!+-!&C". . ill you p.enne describe it for the record Mr. Gilrore.
P.R. GILMCRE. This is a photograph taken looking upstrea, of v.at I believe sculd be the Kabayo river during the non-mons :7 eensen. Tris Cil AlitM Ah. Is that a bridge? f:.<. G iLMC J d' . That is a bridge crcosing the river leading to the office area of the National Power Corporation. 7114 Cd AIRMA:.. Justice Eautista, any question? JUSTICE 31.UTISTA. And that is the bridge construc ted by fiPC7 U. GI L!!C C . That is the bridge constructed by NN.
Ccemircion on Nuclear Reactor Plants 13 July 1979 10:00 a.m. Page 8 JUSTICE BAUTISTA. khat wa,a the nececeity of constracting the bridi;e when the site has hot yet been selected ma the rest suitable site 7
):5. GILMCRE. The offices'I am referring to, Justice, were the field offices. They were not permanent typo of office facilities you r.sy have seen during your field inspection. They w'ere located by the GC for what reason I do not know.
JUOTICE BA"TISTA. How big is this river reflected just behind that bridge?
- 13. GILMC3E. You mean the width?
JUOTICE B AUTISTA. The width. Aro they big rivera.?
!!!'. GIL}:CRE. Not really very, very large - average size during the dry season.
2CJTICE SAUTISTA. Did you soy the presence of these rivers scul: tc disndvantageous for the wise selection of the site 7 h.i. J: LEcita. I didn' t catch all of the questior.s. Hr. Justice. JCSTIOi. BAUf!STA. Tc.u said be fore that the presence of these t.o rivers do not add to the feasibility of choosing Dacac I as the site.' i;. 01L:.t,W4. That is correct. JUOTIOi BAUTISTA. Will you elucidate why, since the water supplied by these two rivers con help the project free a layman's point of view.
\ .o,
Coer.ir.,sicn on fluelear Heoctor Plants , 13 July 1979 10:00 a.m. i Page 9 - i:n. GILf 0D;. Hay I elucidate by goinE to the next slide and
'then come back to this slide?
JUSTICE BAUTISTA. You may. p* "knu .; pk g g M
- - - <1 >
T!!E CliA!HMAN. Mark this as Exhibit. "23.NPC". That is very obscure. Cat we have some more light on that or is that how the photogre;h is? MR. GILhCRI. I believe that is how the slide is. TH E CH All(M AN . Very well. Justice Bautista. JUSTICE BAUTISTA. One of the factora mentioned in this Table I of Exhibit "16-B" is the presence of ground water - curface and ground water. Did that not include the presence of rivers? MR. GILHCRE. Yes, it included the presence of rivers.
-JU3TICE LAUTISTA. And, therefore, the presence of a river is a factor in the selection of the site; it is a good factor; favor-able to the selection of the site.
t Ka. GILMC3E. I was attempting to answer your earlier question by showing this slide, Mr. Justico. This photograph is also taken from the bridge looking upstream to the Kabayo river showing the Kobayo river in flood during the monsoon season. 'ahat you recollect havicg seen earlier is a relatively small stream carryir.g approxi-mately one cubic foot water per second or in the order of 500 galloon per =inute in the dry season. During the monocon, they are .a very t
Cc, emission on Nuclear Reactor Planta 13 July 1979 10:00 a.m. i L' age 10
=uch larger stream, carrying very large quantities of water.
USTICE BAUTISTA. That will be all, Mr. Chaire.an. THE CHhlRMAN. .Are those all the slides or you have others? Md. GILL! ORE. I have two more.
" it ,. s PBb" O iN THE CH AlithAN . Go to the next islide. ('Another picture was flashed.) Hark it as Exhibit "26-NPC".
J.USTICE BAUTISTA. What is depicted on that? I If3. GILMORE. This is a photograph taken from the same bridae s looking downstream along the Embayo river during the dry ae. son. JUSTICE 3AUTISTA. How deep is this water level from the are. acovo?
~
MR. GILMCHE. It is very shallow. In fact, you can see to the right of the picture ene of the local people working on the maintenance of his irrigation diversion scheme near the water. JUSTICJ BAUTISTA. Are there some more slidos that you brought?
- '. d . G
- LI:CR d. There is one sore. (another picture was fIsshed.)
ra Cai Al;lM A 4 Hark that as Exhibit "27-bi'C". MR. GILMCRE. This is a photograph of the same spot on tne ss-e bridge locking downstream during the monsoca season.
-owTlC:. 51sU11STA. What is represented here?
- s. GILMQhd. This is a flood, tremendous a:scunts of water co:r.- towards the original sito area.
JU;TICE B AUTISTA. That is all.
\s 1
Com-icsion on Nuclear Peactor Plants 13 July 1979 10:00 a.m. Pace 11 THE CHAIRMAN. Justice Vasquez, any ,questien? 5 JUSTICE VASQUh;Z. None. y q l 9i; N#b I,I
"!h., CH AIHMAN. Next slide. ~
MR. GILMORE. Tho'next slide is with reference to the ground water that you questioned. , I i TMS Cil AIHMAN. Mark this as Exhibit "28-NPC". t j ; IIIi. GILHCFE. This is a slide showing the first test-pitithat I , was ex:cyated in the 'ofiginal site cree by the listional Power:Cor-ti cration. You;will observe the ' alluvio material, unconsolidated i clluvio materials that are referred to as the four-foundation mater-tale cnd you will note that the pit is full of water. That is the ground water I was referring to. j Yif a Cil AIHMAN. You said, Mr. Gilmore, that you were going back to another sliae in relation to one of the questions of Justice 1: au ' 1 s t a'! b . CILMORC. Justice Bautista has asked about the ground water.
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I can return to the first clide. Trti "li AI RM A.'i . 'Je are now back to h.xhibit "2 3-N1 C" .
' ~ ~' . 31 Lh0WJ. This is a slide showing the complete exploratory 9
drillan<. the first exploratory drilling which was located 6t the central line of the reactor building for the originally laid out power plant site. You will see that the hole is making, water. I re..tioned earlier, under pressure, at high temperatures and at large x1 ]b
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Oc--iz.ston en Nuclear Heactor Plante 13 July 1979 10:00 a.m. loge 12 quantities. You will also note that the gentlemen stonding thero - Q gg one of them a member of the HPC, one frora EU ASCO - are basically ,'J ik 0 h' ( lI
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( ) %# 8 $j'}jlg ster. ding in water. JUOTICE EAUTISTA. Thic dtilling was mado at the Napot point rate already? , MR. GIL::CRE. No, this was made at the original Bagac site shown on Figure 3 of Exhibit "16-NPC". I JUSTICE DAUT10TA. And in erite of the finding that the facility cf snt er is good, you did not select the cite? M'.I GIL!!C2b. Water can le Sood. Mr. Justice; it can also be tcd. It is a servant of man just as is fire. JUSTICE BAUT16fA. In this particular case, will you clucidate sny thic existence of good water, plentiful water would be had for tt u r. i t c 7 Mh. GliMGds. It is related tc constructability. 4 S NTD .
Cowii8sion on Nuclear Reactor Plants r O d(j$ (Jhg 13 July 1979 - 10:30 am ,. j fage 1 , 1
> i Itts related to construc*ihility.
5111. C.!I.310Rli I .l. she ennstruction of a major f acilit y, such as a nuclear ! i power plant, is an undertaking that takes, years and would
- 1 r,' quire the construction to proceed during several s
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- i Consequently, the construction site would have been t
exposed to the flooding of the type that you saw on the 81idef, particularly, the one downstream of the bridge.
' I in addition, the existence of the types of material shown in the slide of the test pit, Lhen saturated, is sery unstahic, in addition, the watcr shown in the pit weuld have to be removed from the excavation area down to a level some 20 meters -- actually more than 20 r..eters -- below the existing grade to permit the const ruction work to proceed.
Illl! Cil.\ list \N. No more questinns, . lust i ce Vasque:? ieu . ire excused hlr. Gilmore.
' lay we have htr. licaly. Slay we inquire if the charts and pictures of yesterday have already been reproduced? R . Ill! Al.Y .
Alr. Commissioner, the charts have not l'e e n reproduced. We intend to take them to the reprodue-t ion facilit y following the ses., ion today and the reason to.it we haven't taken them yet, is, we t hou;;ht in the interpellation that you might wish to go hack to some of the exhibits and we wanted to have them here.
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i Commission on Nuclear Reactor plants 13 July 1979 - 10:30 a.m. P.i ge 2 THE CHAIRh!AN. You are going to. dwell on question
.\o. 7?
MR. IlE ALY. Yes, Mr. Commissioner, hith your indulgence, Mr. Tilford is prepared to handle that question. Tilli CIIAIR.n FAN. Who is he? MR. IIEALY. Mr. Tilford. Tile CilAIRMAN. Oh, finc. We call MR. Tilford ()] q ,) ; j g g m back to the rostrum, MR. IIEALY. Thank you. $k k f ,. Tile CilAIRMAN. Proceed. MR. TI Ll?ORil. I will try t o honor t he Commission's wish for brevity. The historical earthqt akes in the site region were examined to determine the scismic design hasis for the nnetear plant site. We have used the early data, which we have mentioned earlier is unusual in the world, showing that you have a very long carthquake history, count ing to some 400 years stretching hack to the late 1500s, early lo00s. We have used all of that historical information in developing the scismic design hasi3. We have also used all of the available instru.nentally recorded data and we have included all of t hat data in our eartiatuake catalogue. Liasi'ay, e we concur with the list of locally felt earthquakes repo.ted to you by the l'ACASA response to the question to the extent that if there is any difference 0 1223 001 o m em em
Con. mission on Nuclear Reactor Plants 13 July 1979 - 10:30 a.m. ; . til ; i Page 3 between the list that they have given you within the last few days and the one which we have submitted to you, it is lieeause of a definition. We have listed only those which were listed as having been felt in Bataan ar.d report ed f rom Hataan or they have included a few events which were not spccifically reported from llataan but which could reasonably be expected to have been felt in Bataan and we concur in that approach as well. Basically, the history of rthquakes in the parti-cular site of this plant is very slight. The Bataan peninsula occupics what almost might he described as a windbw, an open space, in the historical record of e.'ismicity in Central Luzon and is almost unique in Central Lu:on in that aspect. There have been very few e.arthquakes which have created any destruction on Bataan, i.e t me read /you very quickly the description of the worst of those which we considered to be the 1852 carthquake of Septemhcr 10th. The repor. states that Balanga su f fered cons iderably. The royal house had some cracks and fractures. The t'hurch t ower and turret roof of Orion were ruined. The entare roof, the choir, and part of the tower of the church
.'i Orani were down. The churches and pari.h houses ot Wu e.t y , Pilar, Mariveles and Balanga suffered considerah c loss.
1223 002
l !'f Commission on Nuclear Rea: tor Plants 1 ct?uk d] g 13 July 1979 - 10:30 a.m. ( . Page 4 Our comment with respect to that report is damage that we believe that a great majority of the eceurred because the structures were founded on soft mud and sand associated with Manila llay. The nuclear plant is, of c'ourse, on the other side of the peninsula on hard competent rock. I would conclude my remarks in the interest of brevity at that point and be happy to try to address any questions of the Commission. TilII CllAIRMAN. Questions by Justico Vasquez? JllSTICl. VASQUll . I have no other question. Till! CilAIRMAN. Questions f r.am Just ice Haut i.s ta'l JUSTICE BAUTISTA. No questions. Tilli CllAIRMAN. Mr. Tilford, wherc did you get your naterials relative to your response to Quest ion No. 7? MR. TILFORD. The information availabic on the earthquake history of the region coacs primarily from the catalogue of Raf fety and the subsequent catalogue, 1 believe, cf Sobia and others, prepared by local people, primarily from records of the church. That record hcgins, I think, with the first entry, which is 1599 or 1000, and is complete through the early p.i r t of this century, instrumentally reco ded carthquakes are available from the US National Ocean and Atmospheric Administra-tion tape files. We relicd on that file a good Jeal in 8 1223 003
Comnission on Nuclear iteactor Plants QQ Ql - 5l 13 July 1979 Page 5 10:30 a.m. g gTy pl Jeveloping the instrumental history, instrumentally reco ded history. We have also consulted with Fr. Suc in the Manila Chscrvatory. We consulted with, of course, the PAGASA. No have consulted the catalogues of ISC and we have used some data that have recently bec ne-available from the Russian observatories for carthquakes recorded after about 1954. I believe our carthquakc catalogue is agreed , by alI to be a completely comprehensive one. TiiE CHAIRMAN. Do you have copy of that cataloguc? MR. T!!. FORD. Yes, sir. The catalogue is contained in the Preliminary Safety Analysis Report. I believe it is volume VII. Tilli Cl! AIRMAN. Already submitted? MR. T i l. FORD . No, sir. In the sense that the ent ire Preliminary Safety Anlysis Repo.t has not been submitted, that part of it has not. We can certainly have it available to you. TilF. Cil AI RMAN. When may we have this? We would Iike, Mr. Tilford, to have the documents -- cither xeroxed copics thercor or whatever manuscripts you can suppiv this Commission for our gtiidance. Is that ims3ihte? MR. f I I.l'C Rii . We wilI supply you wi t h se t t ions 2.1, 2.5, .l.1 of the PSAR.which cor.tains the entire dis-cussion of the scismic design basis for the project I 1223 004
Commission on Nuclear Reactor Plants ! : 13 July 1979 Page 6 . 10:30 a.m. ild . lb (3 jldf1" In addition to that, we will supply you with the appropriato appendix containing our carthquake catalogue. Yes, sir. And that should be availabic to you by this afternoon. It surely can be availabic to you casily by Monday morning. Tile CllAIRMAN. Plcsso present those so that we can
-. # them in evidence. No more questions?
ATTY. ARROYO. Mr. Commissioner. Tile CllAIRMAN. Just a moment. At this stage, ' before we declare another recess. After the continuation of aur proceedings, we will commence with the last stages sf the interpellation of Mr. Simmons. he tote that the adversa position paper of the TaSada Pancl to the NPC and pal:C position papers has already been submitted. After the Westinghouse Panel has been questioned, if there is still time, we will begin with the elaboration of the NPC and pal.C Pancis in the light oi Taflada adverse position paper. No will declare a recess for ten minutes. ATTY. ARROYO. Just a littic clarification with respect to Mr. Tilford. It has nothing to do with this dissertation. Titr. CitAIRMAN. Yes. ATTY. ARROYC. liith the permission of the Chairman, . I would just like to ask I.r. Tilford whether he said that the Preliminary Safety Ar. lysis Report, Chapter VII. has not yet been submitted. f 1223 005 _
a rotamission nn Nuclear tienetor Pla. 1; .iniv 1517 0 -- 10 10 n.m. Pace 7 M2. 7T15000. Nnt Chanter Vli, Vnlume Vii. line i sniel that in the 1est of mv innwleslue the Preliminarv Caf tv Annivsis Rennrt has nnt been s u . .m i . t e .'. en .he enmmissinn
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SUSPENSION OF SESSION THE CHAIRMAN. Is the procedure for the rest of the. morning cicar? We deciste a recess for ten minutes. It was 10:40 a.m. RESUMPTION OF SI:SSION At 10:55 1.m., the session was resumed. Ti!E CllA!!U!AN. The session is resumed. Mr. Simmons, you may sit down. The Taiiada Panel is not yet in the :.ession hall. t.lfter a few minutes.) The Senator is coming. Mr. Siumons, please take the stand. 8 1223 006
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Commission on Nuclear Rc..ctor 14 ants 13 July 1979 - 10:3 0 a i ra . Page S JUSTICE VASQUEZ. Before the continuation of the interpellation, may I ask a few questions to Alr. Simmons? Tile Cil.\llu!AN. Yes. Proceed, Justice. JUSTICT. V Q UEl. 1.just want t a i- 1;Lrify4 h h po i n t cr menti 5hhk.by h q s 3M WI iW [ 9 k 1223 007 J
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Coir.:aission on Nuclear Reactor Plants 13 July 1979 - 10:30 . r.i. Page S JUSTICE VASQUEZ. Before the continuation of the interpellatjon, may I ask a few qacstions to Mr. Simmons? TIIC Cil.\llD!A.N. Yes. Proceed, Justice. J UST ICI:. V.QQtlE Z . 1. j iis t i.'a n t t o,1;11riLg t h is po i n t sh "Jt Di%hdric e n r ahi e r in e n t 13 ndi.b y-,' : r Zigs iw v N A ... P00RORIGINil 1223 008
Coenission en Nuc1cra Kcactor Plants 13 July 1979 12:00 .'. con - Q 7 Pase - - b(,{g( Q7IM.y asking for further information in that regard, is difficult for 4 us to understand, but if in the opinion of the Commission, it is important, our men will stay. Tile CHAIRMAN. Just a moment. (Conferring with the two rmenbers er the Commission) Senator Tunada, can you terminate tnis in about a day, on Monday? We will give you the entire
..iterncon on MCnday.
MIP.' TASADA . Possibly, Mr. Chairman. But certainly, I weuld like to inform Mr. Cronin that all my questions were N.sec. en their own statement because we cannot accept their statement en their face value. Til'E CilAIIB!AN. On Monday then, we will begin from 1:00 until 5:00 for the continuation at the TaSada interpc11ation. The Chair wculd like to request that all the parties remain for a few minutes after we adjourn this hearing, to piek up tnear ccpies of threc-rows resolution that the Commi>sion ha.s
;.ramulgated, one of vehich resolution denis with the motion to ruipend the hearing filed by Attorneys Arroyo and Tanada, h'e also would like to remind the EGASCO Panel tnat in all prehability, the questions on 5, 6, and 7 will be coe.menecd cn hednesday, n which time we expect the Tanada adverse posi-tion paper to be submitted. That the NPC and PALC Pancis will oc e.steeted to present their position papers at t he t era.ina t ier.
of the TaSada interpellations of the Westinghouse, which will either be on Monday, if Atty. Tanada finishes carly or on Tucsday.
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