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SU0007861
Environmental Health - Public
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SU0007861
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Entry Properties
Last modified
1/6/2020 11:37:03 AM
Creation date
9/4/2019 10:03:24 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0007861
PE
2675
FACILITY_NAME
PA-0800105
STREET_NUMBER
9999
Direction
S
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
APN
20106003
ENTERED_DATE
8/11/2009 12:00:00 AM
SITE_LOCATION
9999 S AUSTIN RD
RECEIVED_DATE
7/24/2009 12:00:00 AM
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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SJGOV\sballwahn
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FilePath
\MIGRATIONS\A\AUSTIN\9999\EIR PA-0800105\NOP.PDF
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EHD - Public
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.Draft Environmental Impact Report Page IV.F-5 <br /> Forward Inc. Landfill Expansion <br /> Surface Water Quality <br /> The RWQCB Order R5-2003-0049 requires quarterly surface water quality monitoring at two <br /> points on the former Austin Road Landfill site, when surface water is evident. One of the <br /> sampling locations, SW-1, is located upstream of the landfill and represents background <br /> conditions. The other sampling point, SW-2, is located immediately downstream of the landfill, <br /> and is designed to evaluate surface water quality impacts from the landfill. Monitoring at the <br /> Forward Landfill is conducted only when runoff escapes the surface water collection system, <br /> which diverts surface water to the evaporation pond on the facility. <br /> Beneficial uses of Littlejohns Creek designated, as specified in the San Joaquin River Basin Plan, <br /> are agricultural supply, industrial service and process water, contact and non-contact water, <br /> recreation,warm fresh water habitat, preservation of rare, threatened and endangered species, <br /> and.groundwater recharge. <br /> The perennial nature of Littlejohns Creek means that the surface water samples are analyzed <br /> every quarter for the Austin Road Landfill monitoring. Surface water sampling and analysis is <br /> not always performed at the Forward Landfill because, at times, there is no water to sample at <br /> those points. The field parameters sampled for quarterly are temperature, specific conductance, <br /> pH, and turbidity. In addition to the quarterly sampling,biannual(twice a year) sampling <br /> occurs for total dissolved solids, total suspended solids, chloride, sulfate, dissolved oxygen, and <br /> nitrate. <br /> During the second quarter 2008 sampling at Forward and Austin Landfill units (Geo-Logic, <br /> 2008b)the surface water samples collected showed no detectable VOCs were reported. A <br /> comparison of he upgradient and downgradient surface water samples showed similar <br /> inorganic constituent concentrations, suggesting the landfill units are not impacting surface <br /> water quality. <br /> NPDES Stormwater Monitoring Program <br /> Forward and Austin Road Landfills both have current National Pollution Discharge Elimination <br /> System (NPDES)monitoring programs and Storm Water Pollution Prevention Plans (SWPPP)in <br /> place. These programs, overseen by the RWQCB, include storm water inspection, sampling, <br /> observation, and reporting. Previous discharge was to receiving waters at Littlejohns Creek but <br /> that has been replaced by use of the treated groundwater to: 1) use for onsite dust suppression <br /> and other operations uses, or, 2) use for artificial recharge reinjection into the local aquifer. The 1 <br /> aquifer replenishment versus discharge to the surface water eliminates the clean treated water �J <br /> from the groundwater treatment system from being discharged into Littlejohns Creek. As the <br /> landfill expands, the facility will be required to update its NPDES and SWPPP. ] <br /> Groundwater f� <br /> Regional Groundwater Conditions <br /> Underlying San Joaquin County is a portion of the vast subsurface groundwater aquifer system <br /> of the Central Valley of California. Groundwater occurs in unconfined and confined conditions. <br /> The upper regional aquifer is typically an unconfined aquifer within the Victor Formation <br /> geologic unit. A minor perched water table at an elevation of about 20 feet amsl was <br /> encountered while drilling one of the site wells;perched water tables in the area are of a limited <br /> extent. The Victor Formation consists of over 100 feet of clay, silt, and fine to coarse sand and <br /> gravel. Sedimentary formations underlying the Victor Formation include additional, <br /> productive confined aquifers. Groundwater within one mile of the site is tapped by irrigation <br />
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