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COMPLIANCE INFO_2008-2010
Environmental Health - Public
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4400 - Solid Waste Program
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COMPLIANCE INFO_2008-2010
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Last modified
7/14/2021 10:20:33 AM
Creation date
7/3/2020 11:10:21 AM
Metadata
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Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
COMPLIANCE INFO
FileName_PostFix
2008-2010
RECORD_ID
PR0440068
PE
4434
FACILITY_ID
FA0001871
FACILITY_NAME
CALIFORNIA CLAY LANDFILL
STREET_NUMBER
3242
Direction
S
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
17702029
CURRENT_STATUS
02
SITE_LOCATION
3242 S EL DORADO ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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SJGOV\sfrench
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FilePath
\MIGRATIONS\SW\SW_4434_PR0440068_3242 S EL DORADO_2008-2010.tif
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EHD - Public
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3 TECHNICAL EVALUATION OF UPGRADIENT <br /> MONITORING WELLS <br /> The current wells potentially considered for use as upgradient monitoring points include MW-5, <br /> MW-6, MW-7 and MW-8. The WDR specifies MW-5 as the upgradient well but also requires an <br /> evaluation of the appropriateness of this designation. The following table presents the original <br /> breakdown of site strata defined by Kleinfelder and the zone accessed by each of the existing <br /> wells at the site. <br /> Monitoring Well <br /> Zone Hydrologic Layer Lithology Screened in <br /> Interval <br /> I Vadose Zone Clay and Silt MW-5 <br /> II Vadose Zone (Semi-Confining Unit) Clay <br /> III Uppermost Water Bearing Unit Fine Sand to Silty MW-6 8,MW-7 <br /> (Aquifer) Sand <br /> IV Aquitard Clay and Silt <br /> V Lower Aquifer (Semi-Confined) Sand MW-2A, MW-3A, <br /> MW-8, & MW-9A <br /> Figure 2 illustrates the existing monitoring well network. The following subsections discuss <br /> the status of the wells at the Site. <br /> 3.1 MONITORING WELL MW-5 <br /> Monitoring Well MW-5 was originally installed to monitor the shallowest occurrence of <br /> groundwater at the Site and is approximately 28 feet deep. The interval of saturated soil <br /> accessed by MW-5 was only encountered in the area of MW-5, was defined by Kleinfelder as <br /> "Zone 1", and was interpreted to be within the vadose zone. Because the occurrence of <br /> groundwater at this level is unique to this specific area, the chemistry of this water cannot be <br /> appropriately compared to wells accessing water from deeper,separate zones. <br /> The proximity of MW-5 to Duck Creek suggests that water in this zone is likely related to lateral <br /> infiltration from Duck Creek. The chemistry of the water in Duck Creek is related to the runoff it <br /> carries, which is sourced from a large drainage to the east, including agricultural and industrial <br /> sites upgradient of the site. Because the water within MW-5 is suspected of receiving influence <br /> 3 AW t F0 BRlOI�KS <br /> .?ae. <br /> P:\707 Cove Contractors\WDR\Tech Report and WP 2008\Tech Report and WP_PINAL.doc <br />
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