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SR0084478_SSNL
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SR0084478_SSNL
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Last modified
12/9/2021 1:30:25 PM
Creation date
12/9/2021 1:22:35 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0084478
PE
2602
STREET_NUMBER
32521
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
25510026
ENTERED_DATE
11/15/2021 12:00:00 AM
SITE_LOCATION
32521 S KOSTER RD
P_LOCATION
99
P_DISTRICT
005
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. <br />The Site and surrounding properties are all 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 within San <br />Joaquin County. Recharge is calculated by first determining whether the average <br />monthly precipitation exceeds average monthly potential evapotranspiration. If so, then <br />the difference is the percolating recharge water into the aquifer. Runoff and stream <br />infiltration drainage are not factored into the calculation. This approach likely under- <br />estimates recharge to the aquifer and, consequently, over-estimates nitrate loading. <br />The closest San Joaquin County CIMIS station to the Site is Ripon (station 249). Data <br />from the Ripon station were available for 2017 through 2020; based on the calculation <br />shown, the estimated rate of recharge from percolating waters for the Ripon station is <br />determined to be 2.25 inches (Plate 15). A statistical error of 76 percent is associated <br />with this value. <br />Qualitv 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 2141 Page 10 <br />
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