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SR0081180 SSNL
Environmental Health - Public
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SR0081180 SSNL
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Last modified
1/28/2020 10:12:16 AM
Creation date
1/28/2020 10:04:35 AM
Metadata
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Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0081180
PE
2602
FACILITY_NAME
KUSALAKARI PROPERTY
STREET_NUMBER
9698
Direction
S
STREET_NAME
PRIEST
STREET_TYPE
RD
City
FRENCH CAMP
Zip
95231
APN
19322015
ENTERED_DATE
9/23/2019 12:00:00 AM
SITE_LOCATION
9698 S PRIEST RD
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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TSok
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EHD - Public
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is possible that any remaining surface contaminants may be transported to the first <br /> 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 /> For the project Site, the local precipitation and evapotranspiration rates are presented in <br /> Plate 15. The Site is located closest to the CIMIS Manteca station (70). Data for the <br /> Manteca station were available for 2014 through 2018; based on the calculation shown, <br /> the estimated rate of recharge from percolating waters for the Manteca station is <br /> determined to be 3.64 inches. A statistical error of 48 percent is associated with this <br /> 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 /> In May 2019, Live Oak collected rainwater during two storm events in Lodi; the samples <br /> were analyzed for nitrate by FGL Environmental of Stockton. Each sample was <br /> collected in a clean, dry, stainless steel bowl, then decanted into a plastic container and <br /> placed on ice for transport. <br /> LOGE 1938 Page 10 <br />
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