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SU-2601418_SSNL
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Entry Properties
Last modified
7/9/2026 2:47:00 PM
Creation date
7/9/2026 2:44:42 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU-2601418
PE
2602 - SOIL SUITABILITY AND NITRATE LOADING STUDY REVIEW
STREET_NUMBER
23304
Direction
S
STREET_NAME
HANSEN
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
20936002
CURRENT_STATUS
In Review
QC Status
Approved
Scanner
SJGOV\gmartinez
Supplemental fields
Site Address
23304 S HANSEN RD TRACY 95304
Tags
EHD - Public
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of the ground-water aquifer, it is possible that any remaining surface contaminants may <br /> be transported to the first saturated zone of the aquifer. <br /> Clay-containing soils, like those observed on the Site, tend to inhibit downward <br /> movement of nitrate due to adsorption of the nitrate ions to the soil. <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. The Site is located <br /> within a residential neighborhood that relies on septic systems; orchards lie to the east, <br /> west, and north of this neighborhood. <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 project Site is located relatively far from any San Joaquin County CIMIS stations <br /> (13.5 and 14.2 miles to the closest stations) but considerably closer (5.2 miles) to a <br /> station monitored by the Western Regional Climate Center (WRCC). In addition, the <br /> CIMIS stations are located east and northeast of the Site, while the WRCC station is <br /> located northwest of the Site; as a result, data from the two sources have been <br /> averaged to present a reasonable representation of rainfall levels near the Site. <br /> CIMIS Holt and Ripon Stations <br /> For the CIMIS data, the local precipitation and evapotranspiration rates obtained <br /> through CIMIS are presented in Plates 15 and 16. The closest San Joaquin County <br /> CIMIS stations to the Site are Ripon (249), located approximately 13.5 miles east of the <br /> LOGE 2637 Page 9 <br />
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