ML18194A092

From kanterella
Revision as of 20:10, 2 February 2020 by StriderTol (talk | contribs) (Created page by program invented by StriderTol)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Jump to navigation Jump to search
Log of Boring PV-43C
ML18194A092
Person / Time
Site: Palo Verde  Arizona Public Service icon.png
Issue date: 08/06/2018
From:
Arizona Public Service Co
To:
Office of Nuclear Reactor Regulation
References
Download: ML18194A092 (1)


Text

NATURAL GAMMA LOG INCREASING RADIATION ~ BASIC PROPERTIES SOIL LITHOLOGIC DESCRIPTIONS DATA UNITS V CARBONATE CONTENT PALEO-MAGNETIC POLARITY No COUNTS PER SECOND down-hole peophtsicol lope Ior this honnp Ol 2 l20 Borinp located ECEV. 9SC'+

25 South of PV-DH-45 SILTY SASID Ah'0 GRAVELLY 0+

IB POslTIYE e NEGATIVE brow n, sub angvlor, medi unr SSND,'sm-SP/,

20 dense, stratified; occosionel mmdy sr'll iirier beds, prove/ to lndioerntar.

40 SANDY SILTAND SILTI'AIVDlfklL-SM/, brown, rrolrplasttc ro low plastiotty,onpvlor, dense or vary

. Ilf, moist, stratified/ loco/iced gravel horttonm 60 frc-SM/,

sicrr cLAY AIVD brown, siLTr spho; nonplus/la to nredium ptaslt itytrsry a/i/for dsesa,moist/ abuse'ont colich ~,

60 brow~,CLor/fd'I:

SILTY medivm CH/, bros n to red-fo high plcstlaily, very stiff, moist; scot/ared Mn specks.

I 20 fCL-AIL/,

srcrr cLAr AND cLArEr sldrf Drown, low to msdtvn plosttciil, rsry stiff lo herd, moist/ clay predominates; sent/ared grovel ond coliche l40 eoc'utes, l60 FCLAI'Er SILT AND SIL, Y CLAY;

.I I'nt -c'Ll, orna u, very stiff,muivti dl I'l'edoril'c'fee 'uet/sl'ed Mn specks ond coiichs nodules.

sH. Tr sAND ADD sANDr std TT fsN-SfL/i brorm nonplastic lo low plasttctty, or pa/or, dense, moist 240 rc d.brows SILTY CLAY; (CL-CH/, lirown to medium to high pro liciiy, very stiff, muist/

scattered Mn specks ond colichu sodvlest occasionol silty zend and sandy . Iit Inter beds.

00 SILTI'ANLAt//i SANDV bravn,nonplaztlo to SILT'SM"/SL),

low plrsticify,dense or verr ztift, moist/ scoifered osliob ~

nodules.

. 0, 'p 540

'c. 0

./2 560 Cl T ~

D 'LSL

~o,

.'4 I'0 h

L 400

: ..UL 24 . +2

a. FA/IGL OL/ERA TE, brown, hor d I poorly so ted volcanic ciusi'a 42 2 CL C' m os ity ourrd mol'mul ciosta

. Crhh o a praryomittunttr basal) and ottdesrto.

iuc 440 Mair v otiongiomerate changes to

+4- + awh te tuftaceo s sandstone wth eone de ab/e cloy/grove/ to

+ + 'Lboutde arzed cioete eh//present l

DEvfrRIFISD ASH, TCL CN/ whrie, 460 quartz,m ca, feldspar ond volcanic'o ck frogmanta abundant.

AAIDEsITIc DA5A/T P 460 TD.

454'00

/VOTE:

Geo/opy from 0 /o 4/0 tt ferrso from <<d/4. Sr/

hole FV-43'20 540 SAMPLE LOCATION ~ DEPTH (FEET) ~

SYM BOL EXPLANATION ENGINEERING PARAMETERS PALEOMAGNETIC POLARITY Pl plasticity indes ssrM osss (tarsi Incitnattor of remnant magnetic vector in gsnerol opreemeni with f GI/ oi opposition Io f (3/ Ihe presenl magnetic

~

minus 200 percent passinp EOO sieve SSTM Dt2S W/0 percent moisture nsTMI Dots Itsl'tl /laid Sd dry density ns Tsrl o skirl-tl 8 Mognekc vector h determinate SAMPLE TYPE Drive Sample Pifc*er Tais Sample Nk'ore, Nienber Indicates % /recovery Poisomagnetic Reversal 9 iss ID v w

D E 5 0 R 9 T 0 N5 I I depth elevation ss Standard Penetration Test, 'hi"value nsTM otzsa itT Lithotopic descrip/lone were complied from peolopisls /isld lope, CARBONATE CONTENT loDoralory test data, and down-ho/e peophysics Field lope were No Reaction prepared tn accordance with ASTM 02499-99 Classifications

+

Sliphtil'rench'vs Dosed on krDoratary tssl data are in accordance wifh ASTM Dpopy-69 Irock descriptions follow procedures outlined In the I/eccl/vs IB

+

+

Moderately Hiphly lreoclive QUARTERLY OF THE COLORADO SCHOOL OF MINES; Volume 50, Na I Descrptions for rotoiy Dorings ore based upon cvtlinpt (Dosed on sample reaction Io cr /0% HCI solution/ samples, geophysical lope ond dr/liars'cmnmenls UNITS Vnils column refers to penerai slrohgrophtc dr'visions identified wtthin Ihe basin sediments LOG OF BORING PV-43C