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ARCHIVED REPORTS_1999
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ARCHIVED REPORTS_1999
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Last modified
7/17/2020 3:53:20 PM
Creation date
7/3/2020 10:47:47 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1999
RECORD_ID
PR0440005
PE
4433
FACILITY_ID
FA0004516
FACILITY_NAME
FORWARD DISPOSAL SITE
STREET_NUMBER
9999
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106001-3, 5
CURRENT_STATUS
01
SITE_LOCATION
9999 AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_1999.tif
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EHD - Public
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TECHNICAL MEMORANDUM <br />Page 8 <br />June 3, 1992 <br />SAC31583.AC.ZZ <br />typically ranged from approximately 4,000 psf to over 10,000 psf. Based on these CPT logs, <br />a lower bound shear strength value of 2,000 psf was used in Insitu-Tech's stability evaluation <br />for WMU E (Insitu-Tech, 1987). <br />Groundwater <br />Groundwater levels could not be observed at the time of drilling because the borings were <br />drilled using drilling mud. In the Comprehensive Landfill Description report (CH2M HILL, <br />1992), the shallow groundwater in the vicinity of the site was reportedly encountered at 70 to <br />80 feet below ground surface. Groundwater measured during EMCON's subsurface <br />exploration in 1972 indicated groundwater at depths of between 55 and 60 feet below the <br />ground surface. In one of EMCON's boring, in the southwestern comer of the site, a one - <br />foot thick lens of perched water was encountered at a depth of 21 feet. Based on a review <br />of available groundwater data, there is, however, little potential for significant perched water <br />across the site. A review of the Comprehensive Landfill Description report (CH2M HILL, <br />1992) also indicated that the groundwater levels in the area have declined over the past 30 <br />years because of groundwater pumping for irrigation and domestic use and because of the <br />current drought. This reported decline in the groundwater level in the area partly explains <br />the higher groundwater levels measured by EMCON in 1972. <br />Based on these groundwater table depths and available history of groundwater levels in the <br />area, a groundwater table depth of 75 feet was assumed for purposes of the stability and <br />settlement analyses. <br />Results of Slope Stability Analyses <br />Method of Analyses <br />Slope stability analyses were performed using PCSTABL5M (J. Verduin, 1987), a computer <br />program for analyzing general two-dimensional slope cross sections by limit equilibrium <br />methods.: This computer program is a modified version of STABL (Siegel, 1975). This <br />program was used to determine safety factors against slope failure for static (gravity) loading <br />and to calculate yield accelerations for pseudostatic (earthquake) loading. Safety factors and <br />yield accelerations were calculated using the modified Janbu procedure. <br />Two cross sections were analyzed to estimate static safety factors. The location of these two <br />11 <br />
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