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SR0086726_SSNL
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2600 - Land Use Program
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SR0086726_SSNL
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Last modified
6/20/2023 3:50:36 PM
Creation date
6/16/2023 2:03:29 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0086726
PE
2602
STREET_NUMBER
17050
Direction
E
STREET_NAME
LONE TREE
STREET_TYPE
RD
City
ESCALON
Zip
95320
APN
20321005
ENTERED_DATE
5/17/2023 12:00:00 AM
SITE_LOCATION
17050 E LONE TREE RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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aquifer, it is possible that any remaining surface contaminants may be transported to <br /> 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. Five dairies are <br /> located within two miles of the Site, and most nearby properties are orchards. <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), 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 closest CIMIS station to the Site is Manteca (station 70). Data for the Manteca <br /> station were available for the past nine years; based on the calculation shown, the <br /> estimated rate of recharge from percolating waters for the Manteca station is <br /> determined to be 3.56 inches (Plate 16). A statistical error of 55 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 14 <br /> recent storm events in Lodi. Each sample was collected in a clean, dry, stainless steel <br /> bowl, then decanted into a plastic container and placed on ice for transport. The <br /> samples were analyzed for nitrate by FGL Environmental of Stockton. The results of <br /> the rainwater sampling are as follows: <br /> LOGE 2307 Page 9 <br />
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