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SR0080262 SSNL
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SR0080262 SSNL
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Last modified
11/19/2019 2:14:04 PM
Creation date
11/19/2019 1:25:07 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0080262
PE
2602
FACILITY_NAME
BAVARO PROPERTY
STREET_NUMBER
19401
Direction
S
STREET_NAME
DAHLIN
STREET_TYPE
AVE
City
ESCALON
Zip
95320
APN
24713034
ENTERED_DATE
2/27/2019 12:00:00 AM
SITE_LOCATION
19401 S DAHLIN AVE
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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LOGE 1907: Bavaro SS/NLS Addendum 3 Page 4 <br /> March 15, 2019 <br /> method, it is our understanding that the source for both the precipitation and <br /> evapotranspiration data will be the California Irrigation Management Information <br /> System (CIMIS); data from the most recent five years will be utilized. Because a <br /> final determination on the recommended method has not yet been made, for this <br /> project a straight subtraction of monthly evapotranspiration from precipitation per <br /> year will be used to derive a recharge value. <br /> For the project Site, the local percolation and evapotranspiration rates are <br /> presented in Plate 1. The closest station to the Site that is also within San <br /> Joaquin County, Manteca (station 70), has been selected; the past five years of <br /> annual data were utilized. Based on the calculation shown (Plate 1), the <br /> estimated rate of recharge from percolating waters for the Escalon, California <br /> area would be 3.64 inches per year by this method. <br /> • Reduced Rainfall: For this method, rainfall levels from the closest rain station <br /> are multiplied by a percentage based on a reasonable assumption from the <br /> literature. Because the Hantzsche and Finnemore model utilized a value of <br /> approximately 75 percent rainfall as the rate of recharge from percolating waters <br /> in the Chico area (which is more geologically similar to San Joaquin County than <br /> the other two locations discussed in the paper), that value is applied to local <br /> rainfall in the project area. The San Joaquin County Environmental Health <br /> Department consistently approved this method from January 2017 through <br /> January 2019. <br /> As discussed in the 100 percent rainfall section (above), the average of the three <br /> closest WRCC rain stations yields an annual rainfall value of 12.46 inches (Table <br /> 1). Assuming 75 percent of this precipitation percolates to the aquifer (as <br /> Hantzsche and Finnemore did in Chico), the rate of recharge from percolating <br /> waters is calculated to be an average of 9.3 inches per year. <br /> • Regional Recharge from Percolating Waters: In 2018, the Eastern San <br /> Joaquin Groundwater Authority (ESJGA) commissioned a comprehensive <br /> ground-water model covering parts of San Joaquin County, northern Stanislaus <br /> County, and southern Sacramento County. In the model, percolating recharge <br /> waters throughout the Eastern San Joaquin subbasin (portion of the model area) <br /> were evaluated; a value of 650,000 acre-feet was used for ground-water <br /> recharge throughout the subbasin. This value was derived after numerous model <br /> calibration runs. By dividing 650,000 acre-feet by the total acreage of the <br /> subbasin (772,377 acres), and converting to inches, a regional rate of recharge <br /> from percolating waters throughout the subbasin was found to be 10.1 inches per <br /> year. This value should be viewed as an average for the subbasin area. <br /> Calculated Rates of Recharge from Percolating Waters for Project Site <br /> The following table summarizes the values for rate of recharge from percolating waters <br /> obtained from the methods discussed above for the project Site: <br />
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