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SR0083332_SSNL
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SR0083332_SSNL
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Last modified
3/3/2021 10:06:19 AM
Creation date
3/3/2021 9:45:35 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0083332
PE
2602
FACILITY_NAME
76 W BOWMAN RD
STREET_NUMBER
76
Direction
W
STREET_NAME
BOWMAN
STREET_TYPE
RD
City
FRENCH CAMP
Zip
95231
APN
19326019
ENTERED_DATE
2/25/2021 12:00:00 AM
SITE_LOCATION
76 W BOWMAN RD
P_LOCATION
99
P_DISTRICT
003
QC Status
Approved
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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. Several orchards <br /> are located to the south and west of the Site. <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, "average recharge rate of rainfall" was utilized. <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). Recharge is calculated by first <br /> determining whether the average monthly precipitation exceeds average monthly <br /> potential evapotranspiration. If so, then the difference is the percolating recharge water <br /> into the aquifer. Runoff and stream infiltration drainage are not factored into the <br /> calculation. This approach likely under-estimates recharge to the aquifer and, <br /> consequently, over-estimates nitrate loading. <br /> The Site is located closest to the CIMIS station at Manteca (station 70). Data for the <br /> Manteca station were available for the past seven years; based on the calculation <br /> shown, the estimated rate of recharge from percolating waters for the Manteca station is <br /> determined to be 3.23 inches (Plate 12). A statistical error of 58 percent is associated <br /> with this value. <br /> Quality of Rainwater <br /> Hantzsche and Finnemore listed 1 mg/L-N as the nitrate concentration of rainwater for <br /> their original calculation; in the past, Live Oak has also utilized this value for the nitrate <br /> loading calculation. <br /> To determine a more accurate local value, Live Oak has collected rainwater during <br /> several recent storm events in Lodi. Each sample was collected in a clean, dry, <br /> stainless steel bowl, then decanted into a plastic container and placed on ice for <br /> transport. The samples were analyzed for nitrate by FGL Environmental of Stockton. <br /> The results of the rainwater sampling are as follows: <br /> LOGE 2109 Page 9 <br />
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