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SR0081818
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4200/4300 - Liquid Waste/Water Well Permits
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SR0081818
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Last modified
3/16/2020 4:17:00 PM
Creation date
3/16/2020 2:13:06 PM
Metadata
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Template:
EHD - Public
ProgramCode
4200/4300 - Liquid Waste/Water Well Permits
FileName_PostFix
SSNL
RECORD_ID
SR0081818
PE
2602
FACILITY_NAME
LOPES PROPERTY
STREET_NUMBER
16520
Direction
W
STREET_NAME
VON SOSTEN
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
20938052
ENTERED_DATE
2/28/2020 12:00:00 AM
SITE_LOCATION
16520 W VON SOSTEN RD
QC Status
Approved
Scanner
TSok
Tags
EHD - Public
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water aquifer, it is possible that any remaining surface contaminants may be transported <br /> to the first saturated zone of the aquifer. <br /> Sources of Nitrate <br /> Dairies, orchards that require fertilization in sandy soils, and septic systems have been <br /> found to be the most significant sources of nitrate in ground water. <br /> Percolating Recharge Waters <br /> One of the most determinant factors in the Hantzsche and Finnemore equation is the <br /> rate of recharge from percolating waters, which mix with the downward-percolating <br /> effluent generated by on-site septic systems. In the original Hantzsche and Finnemore <br /> paper, only "average recharge rate of rainfall" was considered. <br /> Based on San Joaquin County Environmental Health Department policy (personal <br /> communication, March 18, 2019), the recharge input for the Hantzsche and Finnemore <br /> equation should be derived from average monthly precipitation of rainfall and <br /> evapotranspiration rates for the area; the data should be obtained from the California <br /> Irrigation Management Information System (CIMIS), preferably from stations located <br /> within San Joaquin County. Recharge is calculated by first determining whether the <br /> average monthly precipitation exceeds average monthly potential evapotranspiration. If <br /> so, then the difference is the percolating recharge water into the aquifer. Runoff and <br /> stream infiltration drainage are not factored into the calculation. This approach likely <br /> under-estimates recharge to the aquifer and, consequently, over-estimates nitrate <br /> loading. <br /> The project Site is located relatively far from any CIMIS stations (13.5 and 14.1 miles to <br /> the closest stations within San Joaquin County) but relatively close (5.0 miles) to a <br /> station monitored by the Western Regional Climate Center (WRCC). As a result, two <br /> scenarios have been run for the Site, the first using strictly CIMIS data, and the second <br /> using a combination of CIMIS and WRCC data. <br /> Recharge Scenario 1 — CIMIS Ripon & Holt Stations <br /> For the CIMIS-only scenario, the local percolation and evapotranspiration rates obtained <br /> through CIMIS are presented in Plates 12 and 13. The closest CIMIS stations to the <br /> Site are Ripon (249) and Holt (248), located approximately 13.5 and 14.1 miles away, <br /> respectively. Data for these stations were available for 2017, 2018, and 2019. Based <br /> on the calculation shown, the estimated rate of recharge from percolating waters for the <br /> Ripon station is determined to be 3.00 inches (Plate 12); the estimated rate of recharge <br /> from percolating waters for the Holt station is determined to be 4.04 inches (Plate 13). <br /> The values from these two stations are then averaged for a final result of 3.52 inches. <br /> LOGE 20-05 Page 10 <br />
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