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SR0081894 SSNL
Environmental Health - Public
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SR0081894 SSNL
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Entry Properties
Last modified
4/15/2020 5:03:25 AM
Creation date
4/14/2020 3:05:11 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0081894
PE
2602
STREET_NUMBER
6565
Direction
W
STREET_NAME
HOWARD
STREET_TYPE
RD
City
STOCKTON
Zip
95206
APN
18922003
ENTERED_DATE
3/16/2020 12:00:00 AM
SITE_LOCATION
6565 W HOWARD 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 /> Clayey soils, like those found on the Site, are known to restrict downward movement of <br /> water, and may provide nitrogen reduction through adhesion to the soil particles. <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 percolation and evapotranspiration rates are presented in <br /> Plate 15. The Site is located closest to the CIMIS Holt station (248). Data for the Holt <br /> station were available for 2017 through 2019; based on the calculation shown, the <br /> estimated rate of recharge from percolating waters for the Holt station is determined to <br /> be 4.04 inches. A statistical error of 21 percent is associated 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 /> 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 /> LOGE 20-08 Page 9 <br />
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