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2013-07-25_REVISION - M2008078
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2013-07-25_REVISION - M2008078
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Last modified
8/24/2016 5:22:54 PM
Creation date
7/30/2013 3:27:40 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M2008078
IBM Index Class Name
Revision
Doc Date
7/25/2013
Doc Name
GP Aggregates LLC West Farm Pit Technical Revison no 2 Request
From
J&T Consulting Inc
To
DRMS
Type & Sequence
TR2
Media Type
D
Archive
No
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CESARE, INC. <br />Rapid drawdown of the reservoir was analyzed with a drawdown rate of 1 foot per day. Pore <br />pressures were computed using transient seepage analysis. Slope stability analyses were performed <br />during drawdown which generated a minimum factor of safety versus time plot. <br />SECTIONS ANALYZED <br />Two sections were chosen for analysis to capture stratigraphic differences across the site. Boring <br />IT-B9 at Station 31 +52 was chosen to represent areas within the site covered by relatively deep <br />sand and gravel deposits. This section contains a relatively deep deposit of permeable soil and <br />represents areas where seepage potential is expected to be the highest. This section was analyzed <br />for both steady state seepage and slope stability during rapid drawdown. <br />Boring IT-B12 at Station 44 +60.39 was chosen to represent areas within the site covered by <br />relatively deep clay deposits. Because the clay soils were assigned the lowest shear strength <br />values, this section will represent areas where the risk of slope instability is the highest during rapid <br />drawdown. This section was analyzed for slope stability during rapid drawdown. <br />Bedrock and groundwater elevations were judged to be relatively stable across the site and were <br />not significant factors in the choice of sections for analysis. For conservatism, a groundwater <br />elevation located at the top of the gravel /sand layer was used in our analyses. <br />MATERIAL PROPERTIES <br />Hydraulic conductivity values for analysis were developed. For the weathered shale bedrock, <br />hydraulic conductivity values were based on the Packer test results performed in Borings IT-B1, JT- <br />B3, JT -B5, JT -B7, IT-B9, IT-B11, and 3T -B13. The results are presented in Table 2. <br />TABLE 2. Packer Test Results <br />soling <br />—61 <br />K (Crr1 ) <br />-- - -- <br />Layer (fea below <br />ground level) <br />-8 <br />T- <br />0 <br />_ 72 - 9 -- <br />3T -B3 <br />72.5-82.5 <br />8.46 x 10' <br />JT -B5 <br />70-83 <br />1.59 x 10'5 <br />- JT -B7 <br />76.5-85.5 <br />1.44 x 10 "5 <br />3T -B9 <br />69-76 <br />9.53 x 10'5 <br />lT -B11 <br />72 -8 4 <br />72,90- <br />2 - 90 <br />9.74 x 10-1 <br />0 <br />JT -B13 <br />For sand, clay, and gravel, hydraulic conductivity values were based on Seepage, Drainage, and <br />Flow Nets, 3rd Edition by Cedergren. For the slurry cutoff wall, the hydraulic conductivities of 1x10- <br />6 and 1x10'' were evaluated. Presumptive ratios of horizontal to vertical hydraulic conductivity for <br />each material were assigned as found in the USACE /CA DWR guidance document. <br />The unit weight, cohesion, and friction angles of the materials encountered are estimated values <br />based on published literature and our experience in the area. <br />11.124 GP Ranches Memo 03.21.1303.21.13 2 <br />
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