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i APR 101986 I [ES Filen
APR 101986 i
                                                                      ;fcject ilu 20.               -
I [ES Filen
MEMORANDUM FOR:         Thomas Clark                                                           -
;fcject ilu 20.
Advanced Fuel and Spent Fuel i                                   -
MEMORANDUM FOR:
Licensing Branch                     .o.                .
Thomas Clark Advanced Fuel and Spent Fuel i Licensing Branch
Division of Fuel cycle and                             :d-Material Safety, NMSS                   ,
.o.
FROM:                 Leon L. Beratan, Chief           -              -                  -
:d-Division of Fuel cycle and Material Safety, NMSS FROM:
Earth Sciences Branch             i
Leon L. Beratan, Chief
                                                                                  ^ 20 -
^ 20 -
Division of Radiation Programs-               ~ ' '
Earth Sciences Branch i
* and Earth Sciences, RES                         -
Division of Radiation Programs-and Earth Sciences, RES l
l t a .u5, . _.__N___.                   .
~ ' '
                                                                                            ~      ~
* t a.u5,.
_.__N___.


==SUBJECT:==
==SUBJECT:==
WEST VALLEY ENVIRONMENTAL ASSE$6 MENT - -
WEST VALLEY ENVIRONMENTAL ASSE$6 MENT - -
~
~
We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these comments should be addressed to:
We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these comments should be addressed to:
l Thomas J. Nicholson, Hydrology (extension 74039)
l Thomas J. Nicholson, Hydrology (extension 74039)
Jacob Philip, Geotechnical (extension 74604)
Jacob Philip, Geotechnical (extension 74604)
Richard McMullen, Geology (extension 74318) l Leon L. Beratan, Chief Earth Sciences Branch sion of Radadon hograms e604240344 860410 DR   ADOCK O270       3                         and Earth Sciences, RES
Richard McMullen, Geology (extension 74318) l Leon L. Beratan, Chief Earth Sciences Branch sion of Radadon hograms e604240344 860410 DR ADOCK O270 3
and Earth Sciences, RES


==Enclosure:==
==Enclosure:==
Comments Distribution /R-2811:
Comments Distribution /R-2811:
                /Chron       RMinogue       Econti       RMcMullen PDR         Dross         LBeratan     JPhilip B Sbj/Rd       XGoller (26nAMurphy         RKornasiewicz ESB:RES:mb       ESB:RES           ESB:RES   ESB:RES:gK ESB:RES        )          % j' h TNichplson       JPhilip [ RMcMullen RKornasiewicz AMurphy   ESB:REgLBeratan 3/p/86         a/25/86           3 /2i/86 4/4 /86           Oy/a7 /86         /l0/86 4
/Chron RMinogue Econti RMcMullen PDR Dross LBeratan JPhilip ESB:RES % j' h B Sbj/Rd XGoller (26nAMurphy RKornasiewicz
)
ESB:RES:mb ESB:RES ESB:RES ESB:RES:gK ESB:REgLBeratan TNichplson JPhilip [
RMcMullen RKornasiewicz AMurphy 3/p/86 a/25/86 3 /2i/86 4/4 /86 Oy/a7 /86
/l0/86 4


a
a
* l


==GENERAL COMMENT==
==GENERAL COMMENT==
S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS
S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS 1.
: 1. The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).
The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).
: 2. The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility. The moisture content versus leaching curves for the tumulus need to be provided   i and the design basis characteristics curves for the engineered layers with   !
2.
time need to be provided.
The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility.
: 3. The below ground options and failure scenarios for the trenches are highly restrictive and limited. Other alternatives which would provide for           ,
The moisture content versus leaching curves for the tumulus need to be provided i
longer pathways and travel times (i.e. , different burial geometries and     '
and the design basis characteristics curves for the engineered layers with time need to be provided.
locations) need to be considered and discussed.
3.
: 4. Insufficient site characterization and baseline data prevent a fair com-       l parison of alternatives for both the trench and tumulus options.             j i
The below ground options and failure scenarios for the trenches are highly restrictive and limited. Other alternatives which would provide for longer pathways and travel times (i.e., different burial geometries and locations) need to be considered and discussed.
: 5. Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.
4.
: 6. Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.
Insufficient site characterization and baseline data prevent a fair com-parison of alternatives for both the trench and tumulus options.
: 7. Differential settlement of the tumulus layers needs closer attention.
j i
: 8. A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.                                                         ;
5.
1
Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.
: 9. A soil moisture analysis should be performed on the site materials and geo-textile to determine hydraulic properties for the engineered layers. This work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.
6.
: 10. High moisture contents and water films on the waste canisters may create b   I a much higher leach rate than predicted and should be reassessed.
Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.
: 11. The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events. A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.
7.
Differential settlement of the tumulus layers needs closer attention.
8.
A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.
1 9.
A soil moisture analysis should be performed on the site materials and geo-textile to determine hydraulic properties for the engineered layers.
This work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.
10.
High moisture contents and water films on the waste canisters may create b a much higher leach rate than predicted and should be reassessed.
11.
The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events.
A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.
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S ON CHAPTER 3.0 0F DOE'S EA FOR GE0 TECHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.
S ON CHAPTER 3.0 0F DOE'S EA FOR GE0 TECHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.
However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally
However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally
(     flawed. Specific comments follow:
(
: 1. The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.
flawed.
Specific comments follow:
1.
The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.
This aspect is not addressed in the EA.
This aspect is not addressed in the EA.
: 2. Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc. Construction and design details of how this is to be accomplished are not described.
2.
: 3. Many vital engineering details are missing:
Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc.
: a. thickness and slopes of the different layers for both tumulus and trench designs
Construction and design details of how this is to be accomplished are not described.
: b. the safe free standing depths of trenches
3.
: c. details of bracing for trenches
Many vital engineering details are missing:
: d. details of piezometers, settlement plates, etc, (tumulus and trench) l                 and if these instruments will compromise the integrity of the system l          e. construction details e.g., how is the clay layer to be placed and compacted above the waste barrels in the tumulus design and the l                 construction sequence (tumulus and trench)
a.
: f. compaction details (tumulus and trench)
thickness and slopes of the different layers for both tumulus and trench designs b.
: g. QA procedures (tumulus and trench)
the safe free standing depths of trenches c.
I
details of bracing for trenches d.
: h. adequacy of filters to interface different materials of construction
details of piezometers, settlement plates, etc, (tumulus and trench) l and if these instruments will compromise the integrity of the system construction details e.g., how is the clay layer to be placed and l
: i. filling of voids between the waste to ensure "no" settlement of the wastes
e.
: j. degradation of the waste and accompanying settlement                     i
compacted above the waste barrels in the tumulus design and the l
: k. earthquake design for trenches and tumulus, seismic design criteria       '
construction sequence (tumulus and trench) f.
and dynamic settlement                       '
compaction details (tumulus and trench) g.
: l. details of layered toe drain of the tumulus
QA procedures (tumulus and trench) h.
: m. details of Geomechanical program SAGE and its verification (if any),
adequacy of filters to interface different materials of construction i.
filling of voids between the waste to ensure "no" settlement of the wastes j.
degradation of the waste and accompanying settlement k.
earthquake design for trenches and tumulus, seismic design criteria and dynamic settlement l.
details of layered toe drain of the tumulus details of Geomechanical program SAGE and its verification (if any),
m.
and applicability l
and applicability l
                                                                                          *t 2
*t 2


==GENERAL COMMENT==
==GENERAL COMMENT==
S ON DOE'S EA WITH RESPECT TO GE0 LOGIC ASPECTS
S ON DOE'S EA WITH RESPECT TO GE0 LOGIC ASPECTS 1.
: 1. SCR, page 4-19, last paragraph, and page C-2, second paragraph.
SCR, page 4-19, last paragraph, and page C-2, second paragraph.
,              Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches:     (1) stress release related to move-ment along the Clarendon-Linden fault system, and (2) post glacial uplift.
Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches:
Either of these explanations indicate tectonic or other deep seated regional stresses that were active in the late Pleistocene and Holocene, and may be currently causing deformation in the region. If ongoing, the significance of this phenomenon to the integrity of the disposal sites should be addressed.
(1) stress release related to move-ment along the Clarendon-Linden fault system, and (2) post glacial uplift.
: 2. EA, page 3-11, section 3.1.1.5.
Either of these explanations indicate tectonic or other deep seated regional stresses that were active in the late Pleistocene and Holocene, and may be currently causing deformation in the region.
l             The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.
If ongoing, the significance of this phenomenon to the integrity of the disposal sites should be addressed.
: 3. A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.
2.
: 4. It is indicated in several places in the SCR and EA that a seismic analysis               ,
EA, page 3-11, section 3.1.1.5.
was performed. For example, on page G-24 it is stated that, with respect               I to the stability of the tumulus, the Factor of Safety is greater than 2.0.
l The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.
3.
A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.
4.
It is indicated in several places in the SCR and EA that a seismic analysis was performed.
For example, on page G-24 it is stated that, with respect to the stability of the tumulus, the Factor of Safety is greater than 2.0.
The seismic analysis should be presented along with the input data.
The seismic analysis should be presented along with the input data.
: 5. On page G-25, first paragraph, it is stated that after the containers begin to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover system resulting in increased infiltration.       Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.
5.
: 6. Page G-24, Section G.3.1.2.
On page G-25, first paragraph, it is stated that after the containers begin to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover system resulting in increased infiltration.
Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.
6.
Page G-24, Section G.3.1.2.
The second paragraph states that although vibratory ground motion might be experienced at the site, there is no likelihood of faulting or fissuring.
The second paragraph states that although vibratory ground motion might be experienced at the site, there is no likelihood of faulting or fissuring.
What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?
What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?
I
I 7.
: 7. Have the effects of ground motions in a shallow soil wedge over sloping                   l bedrock surface been analyzed (amplification, focussing)?
Have the effects of ground motions in a shallow soil wedge over sloping bedrock surface been analyzed (amplification, focussing)?
: 8. Page D-13.
8.
In addition to buried settlement plates, monuments should be installed         .,
Page D-13.
prior to excavation of the trenches to measure heave as the site is unloaded.
In addition to buried settlement plates, monuments should be installed prior to excavation of the trenches to measure heave as the site is unloaded.
  ;      9. In-situ sampling and testing of the soils to confirm physical properties
9.
  ;            should be carried out during excavation of the trenches as well as testing the soil for radionuclides.
In-situ sampling and testing of the soils to confirm physical properties should be carried out during excavation of the trenches as well as testing the soil for radionuclides.
3
3
      ?
?
: 10. What techniques of compaction will be used to consolidate the backfill material between the waste packages? What criteria and QA and QC r.ethods           l will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?                       !
: 10. What techniques of compaction will be used to consolidate the backfill material between the waste packages? What criteria and QA and QC r.ethods l
: 11. Page D-12. A vibratory compactor is to be used on a 0.6m of clay placed           !
will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?
over a filler fabric above a 0.5m layer of pea gravel on top of the waste.
11.
How will it be determined that the inter-container voids are completely             j filled with gravel? Vibratory compactors will likely compact the gravel           '
Page D-12.
(if not too deep) but they are relatively ineffective in compacting clay.
A vibratory compactor is to be used on a 0.6m of clay placed over a filler fabric above a 0.5m layer of pea gravel on top of the waste.
Therefore, there is a possibility of voids after the gravel consolidates.           I
How will it be determined that the inter-container voids are completely j
: 12. Seepage is always greater along interfaces between penetrations and the             f natural soil.     This seepage is usually hard to predict. This is also pos-       1 sible along the interface between backfill and natural soil.
filled with gravel? Vibratory compactors will likely compact the gravel (if not too deep) but they are relatively ineffective in compacting clay.
: 13. Figure D-19. It is not shown how the drainage blanket connects with the perimeter drainage system. This is an important connection.
Therefore, there is a possibility of voids after the gravel consolidates.
I
12.
: 14. The French experience with the tumulus concept should be described, along           I with any other available case histories.
Seepage is always greater along interfaces between penetrations and the f
                                                                                                )
natural soil.
: 15. D-21. One of the barriers against future intrusion into the burial facility i
This seepage is usually hard to predict.
is cited to be the presence of rip-rap intruder barrier, because it will immediately appear as an unnatural feature. Human nature being what it is, it will probably promote continued and even accelerated excavation.
This is also pos-sible along the interface between backfill and natural soil.
l l      16. Summary core boring logs should be included in the SCR.
13.
i
Figure D-19.
: 17. SCR, page 4-26.      The second paragraph implies that the Attica Earthquake was a MMI VII.      This earthquake is officially classified as MMI-VIII (USGS).
It is not shown how the drainage blanket connects with the perimeter drainage system.
This is an important connection.
14.
The French experience with the tumulus concept should be described, along with any other available case histories.
)
15.
D-21.
One of the barriers against future intrusion into the burial facility is cited to be the presence of rip-rap intruder barrier, because it will i
immediately appear as an unnatural feature.
Human nature being what it is, it will probably promote continued and even accelerated excavation.
l l
l l
16.
Summary core boring logs should be included in the SCR.
i 17.
SCR, page 4-26.
The second paragraph implies that the Attica Earthquake was a MMI VII.
This earthquake is officially classified as MMI-VIII (USGS).
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DETAILED COMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046
DETAILED COMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046 1.
: 1. Page 3-2 second line from last.
Page 3-2 second line from last.
What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.
What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.
: 2. General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.     These figures are not legible.
2.
: 3. Pages 4-12, 13, 14, pages 5-29, 30, 31
General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.
:              Show the phreatic surface on these cross sections.
These figures are not legible.
: 4. Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface. Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site. In this regard it is important that more representative values of Specific Gravity, Gs, be determined.
3.
: 5. Figure 5-1 Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward gradient is implied by the displayed pressure head elevation relationship."
Pages 4-12, 13, 14, pages 5-29, 30, 31 Show the phreatic surface on these cross sections.
: 6. Figures 5-2, 3, 4, 5 The reasons for the erratic behavior of the tensiometers has not been described. Is there the possibility that they were not performing as expected due to faulty installation or equipment problems or both?
4.
: 7. Figures 5-6, 7, 8 Have all available data been analyzed to plot the piezometric contours?
Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface.
1
Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site.
: 8. Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometric contours of the site?
In this regard it is important that more representative values of Specific Gravity, Gs, be determined.
: 9. Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).                             "
5.
: 10. Provide working drawings for Fig's 5-11 to 34.
Figure 5-1 Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward gradient is implied by the displayed pressure head elevation relationship."
5 l
6.
Figures 5-2, 3, 4, 5 The reasons for the erratic behavior of the tensiometers has not been described.
Is there the possibility that they were not performing as expected due to faulty installation or equipment problems or both?
7.
Figures 5-6, 7, 8 Have all available data been analyzed to plot the piezometric contours?
8.
Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometric contours of the site?
9.
Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).
10.
Provide working drawings for Fig's 5-11 to 34.
l 5


                            .--                        . _.          =       ..        _            .                    . _.
=
: 11. Page 6-5 Relating quto blow counts is an approximate if not a crude method to compute q f r a clay soil.
11.
u
Page 6-5 Relating q to blow counts is an approximate if not a crude method to u
: 12. Provide a working drawing for Fig. A-1, Appendix A.
compute q f r a clay soil.
u 12.
Provide a working drawing for Fig. A-1, Appendix A.
~
~
: 13. Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and Figures B-5, B-6, B7, B8, Appendix B.
13.
Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure i                               head.
Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and Figures B-5, B-6, B7, B8, Appendix B.
: 14. Please discuss the reason for not including ground and surface water model-ing of the tumulus design.
Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure i
I
head.
: 15. Page 4-25, Section 4.6.2 Flooding The discussion needs to be extensively augmented to include the flooding potential within and adjacent to the FDA. For instance, the runoff generated by local intense rainfall up to the PMP should be analyzed and provided.             Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and I
14.
Please discuss the reason for not including ground and surface water model-ing of the tumulus design.
I 15.
Page 4-25, Section 4.6.2 Flooding The discussion needs to be extensively augmented to include the flooding potential within and adjacent to the FDA.
For instance, the runoff generated by local intense rainfall up to the PMP should be analyzed and provided.
Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and I
relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.
relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.
: 16. Page 4-26, Section 4.6.4 Mass Wasting i                               Again, this discussion is too brief and misses the real problem which is mass wasting in and around the FDA, and potential for future gully develop-ment and mass wasting.             Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.
16.
: 17. Page 4-29, Section 4.6.5                 Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.
Page 4-26, Section 4.6.4 Mass Wasting i
The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade. Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the i                               potential for future gullying.
Again, this discussion is too brief and misses the real problem which is mass wasting in and around the FDA, and potential for future gully develop-ment and mass wasting.
3
Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.
: 18. Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity Relationships of unsaturated hydraulic conductivity R and R versus mois-                           s turecontent,andpressureheadviacharacteristiccufvessh6uldbe presented for the (1) weathered Lavery Till, I
17.
Page 4-29, Section 4.6.5 Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.
The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade.
Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the i
potential for future gullying.
18.
Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity 3
Relationships of unsaturated hydraulic conductivity R and R versus mois-s turecontent,andpressureheadviacharacteristiccufvessh6uldbe presented for the (1) weathered Lavery Till, I
6
6
          . - . . _ _ ,                -.<-.------..-r       -
-.<-.------..-r n
n --nm-   --    ---m---   - - - - - ,  ,----w - w.-n----,     e<---~r"m--- - - - - - - - - + + - ~ - - ~~
--nm-
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,----w w.-n----,
e<---~r"m---
- - - - - - - - + + - ~ - - ~~


(2) unweathered Lavery Till, and (3) Lucustrine unit.
(2) unweathered Lavery Till, and (3) Lucustrine unit.
The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.
The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.
: 19.       Pages 5-5 to 5-7, Section 5.5 Porosity
19.
,                  Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.
Pages 5-5 to 5-7, Section 5.5 Porosity Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.
Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed. Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.
Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed.
: 20.       Page 5-14, Section 5.2 Piezometric and Tensiometric Data l                 This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present. At present, information on the           ;
Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.
site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site-wide perspective. The best         ;
20.
potertial information source on the fractured system is missing and needs         1 to be included (i.e., TBP-kerosene plume monitoring well data).
Page 5-14, Section 5.2 Piezometric and Tensiometric Data l
: 21.       Page 5-19, Section 5.2.3     Soil-Moisture Tension Data The interpretive picture is muddled. Recently collected data (since               !
This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present.
October 1985) may help to resolve inconsistancies in the presented report.
At present, information on the site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site-wide perspective.
The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent l                 data. Perhaps the data suffers from an early period of instrument adjust-j ment, or that tensiometers need to be routinely tested for reliability           .
The best potertial information source on the fractured system is missing and needs to be included (i.e., TBP-kerosene plume monitoring well data).
21.
Page 5-19, Section 5.2.3 Soil-Moisture Tension Data The interpretive picture is muddled.
Recently collected data (since October 1985) may help to resolve inconsistancies in the presented report.
The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent l
data.
Perhaps the data suffers from an early period of instrument adjust-ment, or that tensiometers need to be routinely tested for reliability j
and accuracy.
and accuracy.
: 22.       Page 5-27, Section 5.3.1     Flow in the Lavery Till l_               The authors acknowledge the use of data from different time periods in order to develop the potentiometric contour maps. The use of data from l                 the same time period (i.e., daily data from the well records) is crucial.
22.
Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important. A 2 year continuous data base is very important for this very reason. Calibration and later validation of the conceptual models are dependent upon a common data reference point.                                                             ,
Page 5-27, Section 5.3.1 Flow in the Lavery Till l_
: 23.       Page 5-34, Section 5.3.2     Flow in the Lacustrine Flow                       ,
The authors acknowledge the use of data from different time periods in order to develop the potentiometric contour maps.
The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct.       The contour map of Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.
The use of data from l
the same time period (i.e., daily data from the well records) is crucial.
Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important.
A 2 year continuous data base is very important for this very reason.
Calibration and later validation of the conceptual models are dependent upon a common data reference point.
23.
Page 5-34, Section 5.3.2 Flow in the Lacustrine Flow The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct.
The contour map of Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.
l 7
l 7
t l
t l
l
l


l               24. Page 5-34, Section 5.3.3 Flow in the Unsaturated Zone i                     The discussion needs to be updated and related to Section 5.2.3. The dis-cussion on recharge and affects on the shallow flow (water table) system l                     should be included.
l 24.
: 25. Page 5-39, Section 5.5.3 Methodology The modeling is performed using 2-D cross-sectional configurations. The i
Page 5-34, Section 5.3.3 Flow in the Unsaturated Zone i
location and orientation of the modeled areas (2-D, 1-0 or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed.               (It is not sufficient to cite economical considerations).
The discussion needs to be updated and related to Section 5.2.3.
Section 5.5.?               Introduction The objective, not cited, which needs to be addressed is the need to fully model the present ground-water flow system in and adjacent to the FDA l                     before new activities and their alternatives can be discussed.
The dis-cussion on recharge and affects on the shallow flow (water table) system l
: 26. Page 5-50, Section 5.5.4.1 Calibration This section is incomplete. Information on calibration studies for all of the cross-sections modeled, and for comparison to more than just infiltration rates are needed (e.g., K and         y K values h
should be included.
or observed heads).
25.
Page 5-39, Section 5.5.3 Methodology The modeling is performed using 2-D cross-sectional configurations.
The i
location and orientation of the modeled areas (2-D, 1-0 or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed.
(It is not sufficient to cite economical considerations).
Section 5.5.?
Introduction The objective, not cited, which needs to be addressed is the need to fully model the present ground-water flow system in and adjacent to the FDA l
before new activities and their alternatives can be discussed.
26.
Page 5-50, Section 5.5.4.1 Calibration This section is incomplete.
Information on calibration studies for all of the cross-sections modeled, and for comparison to more than just infiltration rates are needed (e.g., K and K values or observed heads).
y h
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i l
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4 --
4 APR 101986 MEMORANDUM FOR:
APR 101986 MEMORANDUM FOR:         Thomas Clark Advanced Fuel and Spent Fuel Licensing Branch Division of Fuel cycle and Material Safety, NMSS FROM:                   Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs and Earth Sciences, RES
Thomas Clark Advanced Fuel and Spent Fuel Licensing Branch Division of Fuel cycle and Material Safety, NMSS FROM:
Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs and Earth Sciences, RES


==SUBJECT:==
==SUBJECT:==
WEST VALLEY ENVIRONMENTAL ASSESSMENT We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these coments should be addressed to:
WEST VALLEY ENVIRONMENTAL ASSESSMENT We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these coments should be addressed to:
1 Thomas J. Nicholson, Hydrology (extension 74039)                           ;
1 Thomas J. Nicholson, Hydrology (extension 74039)
Jacob Philip, Geotechnical (extension 74604)
Jacob Philip, Geotechnical (extension 74604)
Richard McMullen, Geology (extension 74318)
Richard McMullen, Geology (extension 74318)
I l
I Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs and Earth Sciences, RES
Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs
!                                                        and Earth Sciences, RES


==Enclosure:==
==Enclosure:==
I           Coments Distribution /R-2811:
I Coments Distribution /R-2811:
Circ Ch on       RMinogue     EConti       RMcMullen DCS PD           Dross         LBeratan     JPhilip ESB   j/Rd       KGoller IN vAMurphy         RKornasiewicz ESB:RESy h
Circ Ch on RMinogue EConti RMcMullen DCS PD Dross LBeratan JPhilip h
ESB:RES:mb       ESB:RES         ESB:RES   ESB:RES:MK     ESB:REgLBeratan TNicholson       JPhilip [       RMcMullen RKornasiewicz AMurphy g /Est36       J /yd86 4/4 /86           Oy/a7 /86     /l0/86 3/Q/86
ESB j/Rd KGoller IN vAMurphy RKornasiewicz ESB:RESy ESB:RES:mb ESB:RES ESB:RES ESB:RES:MK ESB:REgLBeratan TNicholson JPhilip [
RMcMullen RKornasiewicz AMurphy 3/Q/86 g /Est36 J /yd86 4/4 /86 Oy/a7 /86
/l0/86


==GENERAL COMMENT==
==GENERAL COMMENT==
S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS
S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS 1.
: 1. The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).
The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).
: 2. The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility. The moisture content versus leaching curves for the tumulus need to be provided and the design basis characteristics curves for the engineered layers with     1 time need to be provided.
2.
: 3. The below ground options and failure scenarios for the trenches are highly restrictive and limited. Other alternatives which would provide for longer pathways and travel times (i.e., different burial geometries and locations) need to be considered and discussed.
The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility.
: 4. Insufficient site characterization and baseline data prevent a fair com-parison of alternatives for both the trench and tumulus options.
The moisture content versus leaching curves for the tumulus need to be provided and the design basis characteristics curves for the engineered layers with time need to be provided.
: 5. Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.
3.
: 6. Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.
The below ground options and failure scenarios for the trenches are highly restrictive and limited.
: 7. Differential settlement of the tumulus layers needs closer attention.
Other alternatives which would provide for longer pathways and travel times (i.e., different burial geometries and locations) need to be considered and discussed.
: 8. A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.
4.
: 9. A soil moisture analysis should be performed on the site materials and geo-   )
Insufficient site characterization and baseline data prevent a fair com-parison of alternatives for both the trench and tumulus options.
textile to determine hydraulic properties for the engineered layers. This     l work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.                                                               ,
5.
: 10. High moisture contents and water films on the waste canisters may create . ' ,
Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.
6.
Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.
7.
Differential settlement of the tumulus layers needs closer attention.
8.
A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.
9.
A soil moisture analysis should be performed on the site materials and geo-textile to determine hydraulic properties for the engineered layers.
This work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.
10.
High moisture contents and water films on the waste canisters may create. ',
a much higher leach rate than predicted and should be reassessed.
a much higher leach rate than predicted and should be reassessed.
: 11. The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events. A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.
11.
The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events.
A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.
1 e
1 e
l l
l l
Line 248: Line 362:
==GENERAL COMMENT==
==GENERAL COMMENT==
S ON CHAPTER 3.0 0F DOE'S EA FOR GE0TLCHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.
S ON CHAPTER 3.0 0F DOE'S EA FOR GE0TLCHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.
However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally flawed. Specific comments follow:
However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally flawed.
: 1. The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.
Specific comments follow:
1.
The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.
This aspect is not addressed in the EA.
This aspect is not addressed in the EA.
: 2. Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc. Construction and design details of how this is to be accomplished are not described.
2.
: 3. Many vital engineering details are missing:
Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc.
: a. thickness and slopes of the different layers for both tumulus and trench designs
Construction and design details of how this is to be accomplished are not described.
: b. the safe free standing depths of trenches
3.
: c. details of bracing for trenches
Many vital engineering details are missing:
: d. details of piezometers, s'ettlement plates, etc, (tumulus and trench) and if these instruments will compromise the integrity of the system
a.
: e. construction details e.g., how is the clay layer to be placed and compacted above the waste barrels in the tumulus design and the           -
thickness and slopes of the different layers for both tumulus and trench designs b.
construction sequence (tumulus and trench)
the safe free standing depths of trenches c.
: f. compaction details (tumulus and trench)
details of bracing for trenches d.
: g. QA procedures (tumulus and trench)
details of piezometers, s'ettlement plates, etc, (tumulus and trench) and if these instruments will compromise the integrity of the system construction details e.g., how is the clay layer to be placed and e.
: h. adequacy of filters to interface different materials of construction
compacted above the waste barrels in the tumulus design and the construction sequence (tumulus and trench) f.
: i. filling of voids between the waste to ensure "no" settlement of the wastes
compaction details (tumulus and trench) g.
: j. degradation of the waste and accompanying settlement
QA procedures (tumulus and trench) h.
: k. earthquake design for trenches and tumulus, s,eismic design criteria and dynamic settlement
adequacy of filters to interface different materials of construction i.
: 1. details of layered toe drain of the tumulus
filling of voids between the waste to ensure "no" settlement of the wastes j.
: m. details of Geomechanical program SAGE and its verification (if any),
degradation of the waste and accompanying settlement k.
earthquake design for trenches and tumulus, s,eismic design criteria and dynamic settlement 1.
details of layered toe drain of the tumulus details of Geomechanical program SAGE and its verification (if any),
m.
and applicability
and applicability
                                                                                          *f
*f
                                                                                            *t 2
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i l


GENERAL C0pmENTS ON 00E'S EA WITH RESPECT TO GEOLOGIC ASPECTS
GENERAL C0pmENTS ON 00E'S EA WITH RESPECT TO GEOLOGIC ASPECTS 1.
: 1. SCR, page 4-19, last paragraph, and page C-2, second paragraph.
SCR, page 4-19, last paragraph, and page C-2, second paragraph.
i Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches: (1) stress release related to move-(         ment along the Clarendon-Linden fault system, and (2) post glacial uplift.
i Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches:
l         Either of these explanations indicate tectonic or other deep seated regional I         stresses that were active in the late Pleistocene and Holocene, and may be i         currently causing deformation in the region. If ongoing, the significance of this phenomenon to the integrity of the disposal sites should be t
(1) stress release related to move-(
addressed.
ment along the Clarendon-Linden fault system, and (2) post glacial uplift.
: 2. EA, page 3-11, section 3.1.1.5.
l Either of these explanations indicate tectonic or other deep seated regional I
stresses that were active in the late Pleistocene and Holocene, and may be i
currently causing deformation in the region.
If ongoing, the significance t
of this phenomenon to the integrity of the disposal sites should be addressed.
2.
EA, page 3-11, section 3.1.1.5.
The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.
The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.
: 3. A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.                                                                   l
3.
: 4. It is indicated in several places in the SCR and EA that a seismic analysis was performed. For example, on page G-24 it is stated that, with respect to the stability of the tumulus, the Factor of Safety is greater than 2.0.
A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.
l 4.
It is indicated in several places in the SCR and EA that a seismic analysis was performed.
For example, on page G-24 it is stated that, with respect to the stability of the tumulus, the Factor of Safety is greater than 2.0.
The seismic analysis should be presented along with the input data.
The seismic analysis should be presented along with the input data.
l
l 5.
: 5. On page G-25, first paragraph, it is stated that after the containers begin     j to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover         i system resulting in increased infiltration. Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.
On page G-25, first paragraph, it is stated that after the containers begin j
: 6. Page G-24, Section G.3.1.2.
to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover i
The second paragraph states that although vibratory ground motion might         l be experienced at the site, there is no likelihood of faulting or fissuring.
system resulting in increased infiltration.
Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.
6.
Page G-24, Section G.3.1.2.
The second paragraph states that although vibratory ground motion might l
be experienced at the site, there is no likelihood of faulting or fissuring.
What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?
What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?
: 7. Have the effects of ground motions in a shallow soil wedge over sloping bedrock surface been analyzed (amplification, focussing)?
7.
: 8. Page D-13.
Have the effects of ground motions in a shallow soil wedge over sloping bedrock surface been analyzed (amplification, focussing)?
In addition to buried settlement plates, monuments should be installed     .I prior to excavation of the trenches to measure heave as the site is           ,
8.
unloaded.                                                                   .;
Page D-13.
: 9. In-situ sampling and testing of the soils to confirm physical properties should be carried out during excavation of the trenches as well as testing the soil for radionuclides.
In addition to buried settlement plates, monuments should be installed
.I prior to excavation of the trenches to measure heave as the site is unloaded.
9.
In-situ sampling and testing of the soils to confirm physical properties should be carried out during excavation of the trenches as well as testing the soil for radionuclides.
3 i
3 i
: 10. Wh:t t:chniques cf compactirn will be us:d to c:nsolidate the b:ckfill materic1 bitwe:n the w;sta psckages? Wh:t crit;ria cnd QA cnd QC methods will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?
: 10. Wh:t t:chniques cf compactirn will be us:d to c:nsolidate the b:ckfill materic1 bitwe:n the w;sta psckages? Wh:t crit;ria cnd QA cnd QC methods will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?
: 11. Page D-12. A vibratory compactor is to be used on a 0.6m of clay placed over a filler fabric above a 0.5m layer of pea gravel on top of the waste.
11.
Page D-12.
A vibratory compactor is to be used on a 0.6m of clay placed over a filler fabric above a 0.5m layer of pea gravel on top of the waste.
How will it be determined that the inter-container voids are completely filled with gravel? Vibratory compactors will likely compact the gravel (if not too deep) but they are relatively ineffective in compacting clay.
How will it be determined that the inter-container voids are completely filled with gravel? Vibratory compactors will likely compact the gravel (if not too deep) but they are relatively ineffective in compacting clay.
Therefore, there is a possibility of voids after the gravel consolidates.                             j
Therefore, there is a possibility of voids after the gravel consolidates.
: 12. Seepage is always greater along interfaces between penetrations and the natural soil. This seepage is usually hard to predict. This is also pos-sible along the interface between backfill and natural soil.
j 12.
: 13. Figure D-19. It is not shown how the drainage blanket connects with the perimeter drainage system. This is an important connection.
Seepage is always greater along interfaces between penetrations and the natural soil.
This seepage is usually hard to predict.
This is also pos-sible along the interface between backfill and natural soil.
13.
Figure D-19.
It is not shown how the drainage blanket connects with the perimeter drainage system.
This is an important connection.
: 14. The French experience with the tumulus concept should be described, along with any other available case histories.
: 14. The French experience with the tumulus concept should be described, along with any other available case histories.
: 15. D-21.                 One of the barriers against future intrusion into the burial facility is cited to be the presence of rip-rap intruder barrier, because it will immediately appear as an unnatural feature. Human nature being what it is, it will probably promote continued and even accelerated excavation.
15.
: 16. Summary core boring logs should be included in the SCR.
D-21.
: 17. SCR, page 4-26. The second paragraph implies that the Attica Earthquake was a MMI VII. This earthquake is officially classified as MMI-VIII (USGS).                           j T
One of the barriers against future intrusion into the burial facility is cited to be the presence of rip-rap intruder barrier, because it will immediately appear as an unnatural feature.
Human nature being what it is, it will probably promote continued and even accelerated excavation.
16.
Summary core boring logs should be included in the SCR.
17.
SCR, page 4-26.
The second paragraph implies that the Attica Earthquake was a MMI VII.
This earthquake is officially classified as MMI-VIII (USGS).
j T
1
1
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_ _ _ _ ~. - _ _


    .                      DETAILED COMMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046
DETAILED COMMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046 1.
: 1. Page 3-2 second line from last.
Page 3-2 second line from last.
What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.
What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.
: 2. General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.           These figures are not legible.
2.
: 3. Pages 4-12, 13, 14, pages 5-29, 30, 31 Show the phreatic surface on these cross sections.
General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.
: 4. Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface. Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-                         i sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site.     In this regard it is important that more representative values of Specific Gravity, Gs, be determined.
These figures are not legible.
l
3.
: 5. Figure 5-1                                                                                       l
Pages 4-12, 13, 14, pages 5-29, 30, 31 Show the phreatic surface on these cross sections.
;                            Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward
4.
;                            gradient is implied by the displayed pressure head-elevation relationship."                       1
Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface.
: 6. Figures 5-2, 3, 4, 5                                                                             l The reasons for the erratic behavior of the tensiometers has not been described. Is there the possibility that they were not performing as expected due to faulty installation or equipment' problems or both?
Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-i sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site.
: 7. Figures 5-6, 7, 8 Have all available cata been analyzed to plot the piezometric contours?
In this regard it is important that more representative values of Specific Gravity, Gs, be determined.
: 8.     Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometrir..
5.
Figure 5-1 Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward gradient is implied by the displayed pressure head-elevation relationship."
l 6.
Figures 5-2, 3, 4, 5 The reasons for the erratic behavior of the tensiometers has not been described.
Is there the possibility that they were not performing as expected due to faulty installation or equipment' problems or both?
7.
Figures 5-6, 7, 8 Have all available cata been analyzed to plot the piezometric contours?
8.
Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometrir..
contours of the site?
contours of the site?
: 9.     Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).                                   ''
9.
l
Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).
: 10. Provide working drawings for Fig's 5-11 to 34.
10.
Provide working drawings for Fig's 5-11 to 34.
4 5
4 5
      'a i     /
'a i
              - ,- --               -                               -   w,_
/
                                                - ,- =--- -  ,-                .-        ,    _      _
-,- =--- -
w,_


  -      11. Pag 3 6-5 Relating q to blow counts is an approximate if not a crude method to compute q,ufor a clay soH.
11.
: 12. Provide a working drawing for Fig. A-1, Appendix A.
Pag 3 6-5 Relating q to blow counts is an approximate if not a crude method to compute q,ufor a clay soH.
: 13. Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and
12.
:-          Figures B-5, B-6, B7, B8, Appendix B.
Provide a working drawing for Fig. A-1, Appendix A.
Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure head.                                                                         ,
13.
: 34. Please discuss the reason for not including ground and surface water model-ing of the tumulus design.
Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and Figures B-5, B-6, B7, B8, Appendix B.
: 15. Page 4-25, Section 4.6.2 Flooding                                             l The discussion needs to be extensively augmented to include the flooding       j potential within and adjacent to the FDA. For instance, the runoff generated by local intense rainfall up to the PHP should be analyzed and provided. Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.
Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure head.
: 16. Page 4-26, Section 4.6.4 Mass Wastina Again, f,his discussion is too brief and inisses the real problem which is mass wasting ir} and around the FDA, and potential for future gully develop-ment and mass wasting. Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.
34.
: 17. Page 4-29, Section 4.6.5   Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.
Please discuss the reason for not including ground and surface water model-ing of the tumulus design.
The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade. Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the       l potential for future gullying.
15.
1
Page 4-25, Section 4.6.2 Flooding The discussion needs to be extensively augmented to include the flooding j
: 18. Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity                       - I Relationships of unsaturated hydraulic conductivity R and R versusmois,(
potential within and adjacent to the FDA.
For instance, the runoff generated by local intense rainfall up to the PHP should be analyzed and provided.
Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.
16.
Page 4-26, Section 4.6.4 Mass Wastina Again, f,his discussion is too brief and inisses the real problem which is mass wasting ir} and around the FDA, and potential for future gully develop-ment and mass wasting.
Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.
17.
Page 4-29, Section 4.6.5 Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.
The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade.
Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the potential for future gullying.
18.
Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity Relationships of unsaturated hydraulic conductivity R and R versusmois,(
turecontent,andpressureheadviacharacteristiccufvesshhuldbe presented for the (1) weathered Lavery Till, 6
turecontent,andpressureheadviacharacteristiccufvesshhuldbe presented for the (1) weathered Lavery Till, 6
r 3
r 3'


(2) unweather;d Lcvery Till, cnd (3) Lucustrine unit.
(2) unweather;d Lcvery Till, cnd (3) Lucustrine unit.
The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.
The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.
: 19. Pages 5-5 to 5-7, Section 5.5 Porosity Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.
: 19. Pages 5-5 to 5-7, Section 5.5 Porosity Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.
Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed. Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.
Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed.
: 20. Page 5-14, Section 5.2 Piezometric and Tensiometric Data This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present. At present, information on the site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site wide perspective. The best potential information source on the fractured system is missing and needs to be included (i.e., TBP-kerosene plume monitoring well data).
Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.
: 21. Page 5-19, Section 5.2.3 Soil-Moisture Tension Data The interpretive picture is muddled. Recently collected data (since October 1985) may help to resolve inconsistancies in the presented report.
20.
The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent data. Perhaps the data suffers from an early period of instrument adjust-ment,   or that tensiometers need to be routinely tested for reliability and accuracy.
Page 5-14, Section 5.2 Piezometric and Tensiometric Data This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present.
: 22. Page 5-27, Section 5.3.1 Flow in the Lavery Till The authors acknowledge the'use of data from different time periods in order to develop the potentiometric contour maps. The use of data from the same time period (i.e., daily data from the well records) is crucial.
At present, information on the site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site wide perspective.
Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important. A 2 year continuous data base is very important.for this very rea ;on. Calibration and later validation of the conceptual models are dependent upon a common data reference point.
The best potential information source on the fractured system is missing and needs to be included (i.e., TBP-kerosene plume monitoring well data).
: 23. Page 5-34, Section 5.3.2 Flow in the Lacustrine flow The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct. The contour map of         "
21.
Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.
Page 5-19, Section 5.2.3 Soil-Moisture Tension Data The interpretive picture is muddled.
Recently collected data (since October 1985) may help to resolve inconsistancies in the presented report.
The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent data.
Perhaps the data suffers from an early period of instrument adjust-ment, or that tensiometers need to be routinely tested for reliability and accuracy.
22.
Page 5-27, Section 5.3.1 Flow in the Lavery Till The authors acknowledge the'use of data from different time periods in order to develop the potentiometric contour maps.
The use of data from the same time period (i.e., daily data from the well records) is crucial.
Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important.
A 2 year continuous data base is very important.for this very rea ;on.
Calibration and later validation of the conceptual models are dependent upon a common data reference point.
23.
Page 5-34, Section 5.3.2 Flow in the Lacustrine flow The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct.
The contour map of Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.
7
7


            .,
24.
* 24. P:g] 5-34, S:ctirn 5.3.3 Flow in th7 Unscturated Z'ne The discussion needs to be updated and related to Section 5.2.3. The dis-cussion on recharge and affects on the shallow flow (water table) system should be included.
P:g] 5-34, S:ctirn 5.3.3 Flow in th7 Unscturated Z'ne The discussion needs to be updated and related to Section 5.2.3.
: 25. Page 5-39, Section 5.5.3 Methodology The modeling is performed usirg 2-D cross-sectional configurations. The location and orientation of the modeled areas (2-D, 1-D or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed. (It is not sufficient to cite economical considerations).
The dis-cussion on recharge and affects on the shallow flow (water table) system should be included.
Section 5.5.2   Introduction The objective, not cited, which needs to be adcressed is the need to fully model the present ground-water flow system in cad adjacent to the FDA before new activities and their alternatives can be discussed.
25.
: 26. Page 5-50, Section 5.5.4.1 Calibration This section is incompitte. Information on calibration studies for all of the cross sections modeled, and for comparison te moie than just infiltration rates are needed (e.g., K yand K hvalues r observed heads).     .
Page 5-39, Section 5.5.3 Methodology The modeling is performed usirg 2-D cross-sectional configurations.
The location and orientation of the modeled areas (2-D, 1-D or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed.
(It is not sufficient to cite economical considerations).
Section 5.5.2 Introduction The objective, not cited, which needs to be adcressed is the need to fully model the present ground-water flow system in cad adjacent to the FDA before new activities and their alternatives can be discussed.
26.
Page 5-50, Section 5.5.4.1 Calibration This section is incompitte.
Information on calibration studies for all of the cross sections modeled, and for comparison te moie than just infiltration rates are needed (e.g., K and K values r observed heads).
y h
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Latest revision as of 01:24, 8 December 2024

Forwards Branch Comments on West Valley Environ Assessment Rept.Onsite Storage Alternative for Time Period Specified Should Be Given More Consideration Based on Listed Reasons
ML20203E715
Person / Time
Site: 02700043
Issue date: 04/10/1986
From: Beratan L
NRC OFFICE OF NUCLEAR REGULATORY RESEARCH (RES)
To: Theresa Clark
NRC OFFICE OF NUCLEAR MATERIAL SAFETY & SAFEGUARDS (NMSS)
References
NUDOCS 8604240344
Download: ML20203E715 (16)


Text

-

i.

APR 101986 i

I [ES Filen

fcject ilu 20.

MEMORANDUM FOR:

Thomas Clark Advanced Fuel and Spent Fuel i Licensing Branch

.o.

d-Division of Fuel cycle and Material Safety, NMSS FROM:

Leon L. Beratan, Chief

^ 20 -

Earth Sciences Branch i

Division of Radiation Programs-and Earth Sciences, RES l

~ ' '

  • t a.u5,.

_.__N___.

SUBJECT:

WEST VALLEY ENVIRONMENTAL ASSE$6 MENT - -

~

~

We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these comments should be addressed to:

l Thomas J. Nicholson, Hydrology (extension 74039)

Jacob Philip, Geotechnical (extension 74604)

Richard McMullen, Geology (extension 74318) l Leon L. Beratan, Chief Earth Sciences Branch sion of Radadon hograms e604240344 860410 DR ADOCK O270 3

and Earth Sciences, RES

Enclosure:

Comments Distribution /R-2811:

/Chron RMinogue Econti RMcMullen PDR Dross LBeratan JPhilip ESB:RES % j' h B Sbj/Rd XGoller (26nAMurphy RKornasiewicz

)

ESB:RES:mb ESB:RES ESB:RES ESB:RES:gK ESB:REgLBeratan TNichplson JPhilip [

RMcMullen RKornasiewicz AMurphy 3/p/86 a/25/86 3 /2i/86 4/4 /86 Oy/a7 /86

/l0/86 4

a

GENERAL COMMENT

S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS 1.

The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).

2.

The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility.

The moisture content versus leaching curves for the tumulus need to be provided i

and the design basis characteristics curves for the engineered layers with time need to be provided.

3.

The below ground options and failure scenarios for the trenches are highly restrictive and limited. Other alternatives which would provide for longer pathways and travel times (i.e., different burial geometries and locations) need to be considered and discussed.

4.

Insufficient site characterization and baseline data prevent a fair com-parison of alternatives for both the trench and tumulus options.

j i

5.

Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.

6.

Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.

7.

Differential settlement of the tumulus layers needs closer attention.

8.

A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.

1 9.

A soil moisture analysis should be performed on the site materials and geo-textile to determine hydraulic properties for the engineered layers.

This work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.

10.

High moisture contents and water films on the waste canisters may create b a much higher leach rate than predicted and should be reassessed.

11.

The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events.

A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.

1

.I

t

GENERAL COMMENT

S ON CHAPTER 3.0 0F DOE'S EA FOR GE0 TECHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.

However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally

(

flawed.

Specific comments follow:

1.

The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.

This aspect is not addressed in the EA.

2.

Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc.

Construction and design details of how this is to be accomplished are not described.

3.

Many vital engineering details are missing:

a.

thickness and slopes of the different layers for both tumulus and trench designs b.

the safe free standing depths of trenches c.

details of bracing for trenches d.

details of piezometers, settlement plates, etc, (tumulus and trench) l and if these instruments will compromise the integrity of the system construction details e.g., how is the clay layer to be placed and l

e.

compacted above the waste barrels in the tumulus design and the l

construction sequence (tumulus and trench) f.

compaction details (tumulus and trench) g.

QA procedures (tumulus and trench) h.

adequacy of filters to interface different materials of construction i.

filling of voids between the waste to ensure "no" settlement of the wastes j.

degradation of the waste and accompanying settlement k.

earthquake design for trenches and tumulus, seismic design criteria and dynamic settlement l.

details of layered toe drain of the tumulus details of Geomechanical program SAGE and its verification (if any),

m.

and applicability l

  • t 2

GENERAL COMMENT

S ON DOE'S EA WITH RESPECT TO GE0 LOGIC ASPECTS 1.

SCR, page 4-19, last paragraph, and page C-2, second paragraph.

Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches:

(1) stress release related to move-ment along the Clarendon-Linden fault system, and (2) post glacial uplift.

Either of these explanations indicate tectonic or other deep seated regional stresses that were active in the late Pleistocene and Holocene, and may be currently causing deformation in the region.

If ongoing, the significance of this phenomenon to the integrity of the disposal sites should be addressed.

2.

EA, page 3-11, section 3.1.1.5.

l The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.

3.

A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.

4.

It is indicated in several places in the SCR and EA that a seismic analysis was performed.

For example, on page G-24 it is stated that, with respect to the stability of the tumulus, the Factor of Safety is greater than 2.0.

The seismic analysis should be presented along with the input data.

5.

On page G-25, first paragraph, it is stated that after the containers begin to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover system resulting in increased infiltration.

Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.

6.

Page G-24, Section G.3.1.2.

The second paragraph states that although vibratory ground motion might be experienced at the site, there is no likelihood of faulting or fissuring.

What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?

I 7.

Have the effects of ground motions in a shallow soil wedge over sloping bedrock surface been analyzed (amplification, focussing)?

8.

Page D-13.

In addition to buried settlement plates, monuments should be installed prior to excavation of the trenches to measure heave as the site is unloaded.

9.

In-situ sampling and testing of the soils to confirm physical properties should be carried out during excavation of the trenches as well as testing the soil for radionuclides.

3

?

10. What techniques of compaction will be used to consolidate the backfill material between the waste packages? What criteria and QA and QC r.ethods l

will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?

11.

Page D-12.

A vibratory compactor is to be used on a 0.6m of clay placed over a filler fabric above a 0.5m layer of pea gravel on top of the waste.

How will it be determined that the inter-container voids are completely j

filled with gravel? Vibratory compactors will likely compact the gravel (if not too deep) but they are relatively ineffective in compacting clay.

Therefore, there is a possibility of voids after the gravel consolidates.

12.

Seepage is always greater along interfaces between penetrations and the f

natural soil.

This seepage is usually hard to predict.

This is also pos-sible along the interface between backfill and natural soil.

13.

Figure D-19.

It is not shown how the drainage blanket connects with the perimeter drainage system.

This is an important connection.

14.

The French experience with the tumulus concept should be described, along with any other available case histories.

)

15.

D-21.

One of the barriers against future intrusion into the burial facility is cited to be the presence of rip-rap intruder barrier, because it will i

immediately appear as an unnatural feature.

Human nature being what it is, it will probably promote continued and even accelerated excavation.

l l

16.

Summary core boring logs should be included in the SCR.

i 17.

SCR, page 4-26.

The second paragraph implies that the Attica Earthquake was a MMI VII.

This earthquake is officially classified as MMI-VIII (USGS).

l l

l l

l t

I 4

1 1

?

DETAILED COMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046 1.

Page 3-2 second line from last.

What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.

2.

General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.

These figures are not legible.

3.

Pages 4-12, 13, 14, pages 5-29, 30, 31 Show the phreatic surface on these cross sections.

4.

Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface.

Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site.

In this regard it is important that more representative values of Specific Gravity, Gs, be determined.

5.

Figure 5-1 Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward gradient is implied by the displayed pressure head elevation relationship."

6.

Figures 5-2, 3, 4, 5 The reasons for the erratic behavior of the tensiometers has not been described.

Is there the possibility that they were not performing as expected due to faulty installation or equipment problems or both?

7.

Figures 5-6, 7, 8 Have all available data been analyzed to plot the piezometric contours?

8.

Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometric contours of the site?

9.

Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).

10.

Provide working drawings for Fig's 5-11 to 34.

l 5

=

11.

Page 6-5 Relating q to blow counts is an approximate if not a crude method to u

compute q f r a clay soil.

u 12.

Provide a working drawing for Fig. A-1, Appendix A.

~

13.

Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and Figures B-5, B-6, B7, B8, Appendix B.

Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure i

head.

14.

Please discuss the reason for not including ground and surface water model-ing of the tumulus design.

I 15.

Page 4-25, Section 4.6.2 Flooding The discussion needs to be extensively augmented to include the flooding potential within and adjacent to the FDA.

For instance, the runoff generated by local intense rainfall up to the PMP should be analyzed and provided.

Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and I

relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.

16.

Page 4-26, Section 4.6.4 Mass Wasting i

Again, this discussion is too brief and misses the real problem which is mass wasting in and around the FDA, and potential for future gully develop-ment and mass wasting.

Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.

17.

Page 4-29, Section 4.6.5 Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.

The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade.

Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the i

potential for future gullying.

18.

Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity 3

Relationships of unsaturated hydraulic conductivity R and R versus mois-s turecontent,andpressureheadviacharacteristiccufvessh6uldbe presented for the (1) weathered Lavery Till, I

6

-.<-.------..-r n

--nm-

---m---

,----w w.-n----,

e<---~r"m---

- - - - - - - - + + - ~ - - ~~

(2) unweathered Lavery Till, and (3) Lucustrine unit.

The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.

19.

Pages 5-5 to 5-7, Section 5.5 Porosity Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.

Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed.

Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.

20.

Page 5-14, Section 5.2 Piezometric and Tensiometric Data l

This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present.

At present, information on the site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site-wide perspective.

The best potertial information source on the fractured system is missing and needs to be included (i.e., TBP-kerosene plume monitoring well data).

21.

Page 5-19, Section 5.2.3 Soil-Moisture Tension Data The interpretive picture is muddled.

Recently collected data (since October 1985) may help to resolve inconsistancies in the presented report.

The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent l

data.

Perhaps the data suffers from an early period of instrument adjust-ment, or that tensiometers need to be routinely tested for reliability j

and accuracy.

22.

Page 5-27, Section 5.3.1 Flow in the Lavery Till l_

The authors acknowledge the use of data from different time periods in order to develop the potentiometric contour maps.

The use of data from l

the same time period (i.e., daily data from the well records) is crucial.

Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important.

A 2 year continuous data base is very important for this very reason.

Calibration and later validation of the conceptual models are dependent upon a common data reference point.

23.

Page 5-34, Section 5.3.2 Flow in the Lacustrine Flow The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct.

The contour map of Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.

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Page 5-34, Section 5.3.3 Flow in the Unsaturated Zone i

The discussion needs to be updated and related to Section 5.2.3.

The dis-cussion on recharge and affects on the shallow flow (water table) system l

should be included.

25.

Page 5-39, Section 5.5.3 Methodology The modeling is performed using 2-D cross-sectional configurations.

The i

location and orientation of the modeled areas (2-D, 1-0 or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed.

(It is not sufficient to cite economical considerations).

Section 5.5.?

Introduction The objective, not cited, which needs to be addressed is the need to fully model the present ground-water flow system in and adjacent to the FDA l

before new activities and their alternatives can be discussed.

26.

Page 5-50, Section 5.5.4.1 Calibration This section is incomplete.

Information on calibration studies for all of the cross-sections modeled, and for comparison to more than just infiltration rates are needed (e.g., K and K values or observed heads).

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4 APR 101986 MEMORANDUM FOR:

Thomas Clark Advanced Fuel and Spent Fuel Licensing Branch Division of Fuel cycle and Material Safety, NMSS FROM:

Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs and Earth Sciences, RES

SUBJECT:

WEST VALLEY ENVIRONMENTAL ASSESSMENT We have reviewed the draft West Valley Environmental Assessment report which you distributed. Attached are our comments. The comments were provided by the members of the Earth Sciences Branch. Any questions concerning these coments should be addressed to:

1 Thomas J. Nicholson, Hydrology (extension 74039)

Jacob Philip, Geotechnical (extension 74604)

Richard McMullen, Geology (extension 74318)

I Leon L. Beratan, Chief Earth Sciences Branch Division of Radiation Programs and Earth Sciences, RES

Enclosure:

I Coments Distribution /R-2811:

Circ Ch on RMinogue EConti RMcMullen DCS PD Dross LBeratan JPhilip h

ESB j/Rd KGoller IN vAMurphy RKornasiewicz ESB:RESy ESB:RES:mb ESB:RES ESB:RES ESB:RES:MK ESB:REgLBeratan TNicholson JPhilip [

RMcMullen RKornasiewicz AMurphy 3/Q/86 g /Est36 J /yd86 4/4 /86 Oy/a7 /86

/l0/86

GENERAL COMMENT

S ON DOE'S EA WITH RESPECT TO HYDROLOGIC ASPECTS 1.

The on-site storage alternative for a given period of time (e.g., 5 years) should be given more consideration since (a) there is a lack of experience with the tumulus methodology; (b) there is lack of experience with " success-ful" trench methodology; and (c) there is a lack of ground-water and surfi-cial erosional data base for the site (a minimum of 2 year background surveillance).

2.

The leaching rate for less than saturated conditions (i.e., high moisture contents) that would provide sufficient leaching to equal the overall radionuclide release performance of the tumulus for comparison to the trenches should be provided for the lifetime of the waste facility.

The moisture content versus leaching curves for the tumulus need to be provided and the design basis characteristics curves for the engineered layers with time need to be provided.

3.

The below ground options and failure scenarios for the trenches are highly restrictive and limited.

Other alternatives which would provide for longer pathways and travel times (i.e., different burial geometries and locations) need to be considered and discussed.

4.

Insufficient site characterization and baseline data prevent a fair com-parison of alternatives for both the trench and tumulus options.

5.

Failure scenarios to be assessed for the tumulus should include " clogging" of the toe drain and local saturated conditions in the base of the tumulus that would allow a high leach rate for the entombed waste.

6.

Stability of the trench, both for cap settlement and waste subsidence, needs closer attention.

7.

Differential settlement of the tumulus layers needs closer attention.

8.

A detailed analysis of local intense rainfall events for both the tumulus and trenches for analyzing erodability, and ground-water recharge scenarios needs to be analyzed.

9.

A soil moisture analysis should be performed on the site materials and geo-textile to determine hydraulic properties for the engineered layers.

This work is presently underway for the weathered Lavery Till and should be the baseline data for the ground-water flow and leaching analysis of the tumulus.

10.

High moisture contents and water films on the waste canisters may create. ',

a much higher leach rate than predicted and should be reassessed.

11.

The gully development analysis does not include a PMF event nor other long-term severe hydrometeorological events.

A very limited period of observa-tion makes a more detailed hydrologic analysis critical for adequately assessing the erosional scenarios.

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GENERAL COMMENT

S ON CHAPTER 3.0 0F DOE'S EA FOR GE0TLCHNICAL ASPECTS This chapter gives some conceptual details of the trench and tumulus design.

However, details of the different elements of the design (not provided) are vital if one has to decide whether the concepts described are viable or fatally flawed.

Specific comments follow:

1.

The quality of and the long term durability of the geotextile fabric is vital if both the trenches and the tumulus are to function as designed.

This aspect is not addressed in the EA.

2.

Both the tumulus and trench will have to be designed for virtually zero settlement (static and dynamic) in order not to compromise the integrity of the textile, drains, etc.

Construction and design details of how this is to be accomplished are not described.

3.

Many vital engineering details are missing:

a.

thickness and slopes of the different layers for both tumulus and trench designs b.

the safe free standing depths of trenches c.

details of bracing for trenches d.

details of piezometers, s'ettlement plates, etc, (tumulus and trench) and if these instruments will compromise the integrity of the system construction details e.g., how is the clay layer to be placed and e.

compacted above the waste barrels in the tumulus design and the construction sequence (tumulus and trench) f.

compaction details (tumulus and trench) g.

QA procedures (tumulus and trench) h.

adequacy of filters to interface different materials of construction i.

filling of voids between the waste to ensure "no" settlement of the wastes j.

degradation of the waste and accompanying settlement k.

earthquake design for trenches and tumulus, s,eismic design criteria and dynamic settlement 1.

details of layered toe drain of the tumulus details of Geomechanical program SAGE and its verification (if any),

m.

and applicability

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GENERAL C0pmENTS ON 00E'S EA WITH RESPECT TO GEOLOGIC ASPECTS 1.

SCR, page 4-19, last paragraph, and page C-2, second paragraph.

i Possible explanations are given for the mechanisms causing the second set of fractures mapped in test trenches:

(1) stress release related to move-(

ment along the Clarendon-Linden fault system, and (2) post glacial uplift.

l Either of these explanations indicate tectonic or other deep seated regional I

stresses that were active in the late Pleistocene and Holocene, and may be i

currently causing deformation in the region.

If ongoing, the significance t

of this phenomenon to the integrity of the disposal sites should be addressed.

2.

EA, page 3-11, section 3.1.1.5.

The criteria by which developing problems are identified through the short and long term monitoring program, when it is necessary to initiate a fix, and what type of fix will be done, should be provided.

3.

A provision should be included in the report to geologically map in detail, the walls and floor of the trenches and the cleared earth surface below the tumulus.

l 4.

It is indicated in several places in the SCR and EA that a seismic analysis was performed.

For example, on page G-24 it is stated that, with respect to the stability of the tumulus, the Factor of Safety is greater than 2.0.

The seismic analysis should be presented along with the input data.

l 5.

On page G-25, first paragraph, it is stated that after the containers begin j

to deteriorate, the seismic activity expected for this long-term period might trigger settling of wastes and disturb the integrity of the cover i

system resulting in increased infiltration.

Describe the expected seismic activity and the potential consequences of increased infiltration caused by seismically induced settling of wastes.

6.

Page G-24, Section G.3.1.2.

The second paragraph states that although vibratory ground motion might l

be experienced at the site, there is no likelihood of faulting or fissuring.

What maximum level of ground motions are likely to be experienced at the site? What will be the effect on the waste packages? Will the canisters contact one another (banging) during earthquake groundmotions?

7.

Have the effects of ground motions in a shallow soil wedge over sloping bedrock surface been analyzed (amplification, focussing)?

8.

Page D-13.

In addition to buried settlement plates, monuments should be installed

.I prior to excavation of the trenches to measure heave as the site is unloaded.

9.

In-situ sampling and testing of the soils to confirm physical properties should be carried out during excavation of the trenches as well as testing the soil for radionuclides.

3 i

10. Wh:t t:chniques cf compactirn will be us:d to c:nsolidate the b:ckfill materic1 bitwe:n the w;sta psckages? Wh:t crit;ria cnd QA cnd QC methods will be used to assure that a high quality job has been done? What frequency of testing, and what kinds of tests will be used?

11.

Page D-12.

A vibratory compactor is to be used on a 0.6m of clay placed over a filler fabric above a 0.5m layer of pea gravel on top of the waste.

How will it be determined that the inter-container voids are completely filled with gravel? Vibratory compactors will likely compact the gravel (if not too deep) but they are relatively ineffective in compacting clay.

Therefore, there is a possibility of voids after the gravel consolidates.

j 12.

Seepage is always greater along interfaces between penetrations and the natural soil.

This seepage is usually hard to predict.

This is also pos-sible along the interface between backfill and natural soil.

13.

Figure D-19.

It is not shown how the drainage blanket connects with the perimeter drainage system.

This is an important connection.

14. The French experience with the tumulus concept should be described, along with any other available case histories.

15.

D-21.

One of the barriers against future intrusion into the burial facility is cited to be the presence of rip-rap intruder barrier, because it will immediately appear as an unnatural feature.

Human nature being what it is, it will probably promote continued and even accelerated excavation.

16.

Summary core boring logs should be included in the SCR.

17.

SCR, page 4-26.

The second paragraph implies that the Attica Earthquake was a MMI VII.

This earthquake is officially classified as MMI-VIII (USGS).

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_ _ _ _ ~. - _ _

DETAILED COMMENTS ON DOE'S SUBSURFACE CHARACTERIZATION REPORT, WVDP-046 1.

Page 3-2 second line from last.

What were the engineering test data used to conclude that fractures can-not exist as open cracks below depths of 15 m.

2.

General Comment Working drawings should be provided for figures such as A-1, 4-5, 6, 7, 13, 5-2, 3, 4, 5, 6, 7, 8, 9, 10, etc.

These figures are not legible.

3.

Pages 4-12, 13, 14, pages 5-29, 30, 31 Show the phreatic surface on these cross sections.

4.

Table 5-2 Page 5-7 Some of the values of soil saturation (S) shown in this table indicate S as being below 100% (e.g., 90% and 96%) for samples at 16.1 and 18.3 meters below the surface, while S is over 100% in soils within 2 meters of the surface.

Does this indicate that some samples dried out before testing or is there an error in the dry density measurements due to sample extru-i sion from the borehole or is there some other reason for this apparent discrepancy? Correct determination of S is essential to delineate the phreatic surface at the site.

In this regard it is important that more representative values of Specific Gravity, Gs, be determined.

5.

Figure 5-1 Pressure head variations for dry periods and other wet periods should be shown to verify the trend that (page 5-19 first para) "a clearly downward gradient is implied by the displayed pressure head-elevation relationship."

l 6.

Figures 5-2, 3, 4, 5 The reasons for the erratic behavior of the tensiometers has not been described.

Is there the possibility that they were not performing as expected due to faulty installation or equipment' problems or both?

7.

Figures 5-6, 7, 8 Have all available cata been analyzed to plot the piezometric contours?

8.

Figure 5-9 and page 5-28 last paragraph Have all available data been analyzed to plot the generalized piezometrir..

contours of the site?

9.

Provide Tables 5-8 and 5-9 (pages 4-45 and 5-56).

10.

Provide working drawings for Fig's 5-11 to 34.

4 5

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/

-,- =--- -

w,_

11.

Pag 3 6-5 Relating q to blow counts is an approximate if not a crude method to compute q,ufor a clay soH.

12.

Provide a working drawing for Fig. A-1, Appendix A.

13.

Figure A-3, Appendix A, (Typical Pneumatic Piezometer Installation) and Figures B-5, B-6, B7, B8, Appendix B.

Described how the bentonite seals were installed to prevent clogging of the backfill sand and consequently erroneous readings of the pressure head.

34.

Please discuss the reason for not including ground and surface water model-ing of the tumulus design.

15.

Page 4-25, Section 4.6.2 Flooding The discussion needs to be extensively augmented to include the flooding j

potential within and adjacent to the FDA.

For instance, the runoff generated by local intense rainfall up to the PHP should be analyzed and provided.

Reference to the sections on 4.6.4 Mass Wasting and 4.6.5 Potential for Gully Development at the Disposal Site should be made, and relate surface runoff and rainfall infiltration as generating mechanisms for mass wasting and gully development.

16.

Page 4-26, Section 4.6.4 Mass Wastina Again, f,his discussion is too brief and inisses the real problem which is mass wasting ir} and around the FDA, and potential for future gully develop-ment and mass wasting.

Any new construction and/or stabilization of either trenches or future tumulus will affect surface gradients, drainage, and topographic relief which act to drive this endemic phenomena at West Valley.

17.

Page 4-29, Section 4.6.5 Potential for Gully at a Disposal Site This section appear to be far too biased towards present gully geometries and therefore appears to be a " static analysis" of a very dynamic activity.

The potential for gully development should discuss the generation of new gullies in and around the FDA, particularly for the options of (1) tumulus construction and (2) removal of the railroad grade.

Road construction along the FDA has already modified the present gully, and its analysis should be a good indicator of how future human activities may affect the potential for future gullying.

18.

Pages 5-2 to 5-5, Section 5.1.1 Hydraulic Conductivity Relationships of unsaturated hydraulic conductivity R and R versusmois,(

turecontent,andpressureheadviacharacteristiccufvesshhuldbe presented for the (1) weathered Lavery Till, 6

r 3'

(2) unweather;d Lcvery Till, cnd (3) Lucustrine unit.

The area affected by the solvent plume should be mapped, and increased permeability factors should be provided for the pathway analysis.

19. Pages 5-5 to 5-7, Section 5.5 Porosity Please provide discussion as to why % saturation exceeds 100% in the table on pg. 5-7.

Learning from the TBP-kerosene plume studies, the effective porosity, ne, of the weathered till needs to be reanalyzed.

Using tracer data, an ne could be calculated that would be more representative of the fractured weathered till.

20.

Page 5-14, Section 5.2 Piezometric and Tensiometric Data This entire section, which is crucial to understanding the FDA and sur-rounding hydrogeologic system, needs to be updated to include all monitor-ing well data collected to the present.

At present, information on the site data is missing although both USGS and NYSGS reports, and collected well records would allow a more complete site wide perspective.

The best potential information source on the fractured system is missing and needs to be included (i.e., TBP-kerosene plume monitoring well data).

21.

Page 5-19, Section 5.2.3 Soil-Moisture Tension Data The interpretive picture is muddled.

Recently collected data (since October 1985) may help to resolve inconsistancies in the presented report.

The relationship between recharge, infiltration, and deep percolation has not been fully discussed and resolved due to the apparently inconsistent data.

Perhaps the data suffers from an early period of instrument adjust-ment, or that tensiometers need to be routinely tested for reliability and accuracy.

22.

Page 5-27, Section 5.3.1 Flow in the Lavery Till The authors acknowledge the'use of data from different time periods in order to develop the potentiometric contour maps.

The use of data from the same time period (i.e., daily data from the well records) is crucial.

Gradients in the upper till are especially susceptible to change and therefore an identical time period for' analysis is important.

A 2 year continuous data base is very important.for this very rea ;on.

Calibration and later validation of the conceptual models are dependent upon a common data reference point.

23.

Page 5-34, Section 5.3.2 Flow in the Lacustrine flow The discussion is excellent but needs to examine recently collected data to verify that the conceptual model is correct.

The contour map of Fig. 5-1 attests to the general lack of data and understanding, and needs to encompass more of the site monitoring wells.

7

24.

P:g] 5-34, S:ctirn 5.3.3 Flow in th7 Unscturated Z'ne The discussion needs to be updated and related to Section 5.2.3.

The dis-cussion on recharge and affects on the shallow flow (water table) system should be included.

25.

Page 5-39, Section 5.5.3 Methodology The modeling is performed usirg 2-D cross-sectional configurations.

The location and orientation of the modeled areas (2-D, 1-D or 3-D), need to be discussed, and their inherent assumptions on flow directions and dis-charge rates need to be listed.

(It is not sufficient to cite economical considerations).

Section 5.5.2 Introduction The objective, not cited, which needs to be adcressed is the need to fully model the present ground-water flow system in cad adjacent to the FDA before new activities and their alternatives can be discussed.

26.

Page 5-50, Section 5.5.4.1 Calibration This section is incompitte.

Information on calibration studies for all of the cross sections modeled, and for comparison te moie than just infiltration rates are needed (e.g., K and K values r observed heads).

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