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SR0080159 SSNL
Environmental Health - Public
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SR0080159 SSNL
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Entry Properties
Last modified
11/19/2019 2:40:14 PM
Creation date
11/19/2019 2:30:50 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0080159
PE
2601
STREET_NUMBER
13950
Direction
N
STREET_NAME
THORNTON
STREET_TYPE
RD
City
LODI
Zip
95242
APN
05514023
ENTERED_DATE
2/4/2019 12:00:00 AM
SITE_LOCATION
13950 N THORNTON RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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TSok
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EHD - Public
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Percolating Recharge Waters <br /> Background <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. For the Chico area, <br /> Hantzsche and Finnemore present an average rainfall of 22.5 inches per year and an <br /> estimated recharge of 16.8 inches per year; the recharge value is 75 percent of the <br /> average rainfall. The source of the recharge value is not cited in the paper. <br /> Since the 1992 publication of the Hantzsche and Finnemore paper, numerous <br /> consultants have attempted to apply the method to calculate nitrate loading rates of <br /> projects and developments. Most notably, the City of Chico has continued to use the <br /> method to calculate desired urban density (County of Butte, 2000). In a 1996 technical <br /> memorandum published to support Chico's urban density requirements, the consulting <br /> firm Dames and Moore has discussed that "recharge ... is comprised of two major <br /> components: applied water ... and precipitation and streams." <br /> Dames and Moore discuss three methods of calculating the rate of recharge from <br /> percolating waters, two of which are computer models (SWQCB and HELP) that <br /> consider measured water levels, soil types, irrigation, stream flow, and other factors, <br /> and the third of which is a monthly consideration of precipitation versus <br /> evapotranspiration. The report concludes that estimates using precipitation versus <br /> evapotranspiration "appear to be too low" when compared to those values calculated by <br /> the two computer models. Dames and Moore eventually determine to use a slight <br /> modification of the result of the computer modeling. This method of evaluating ground- <br /> water recharge, which includes recharge from a variety of sources, was found to be <br /> more applicable to the City of Chico's needs than the simplified rainfall-only method. <br /> The value Dames and Moore eventually select (18 inches per year), although derived <br /> by the modeling methods discussed rather than from rainfall alone, is equivalent 83 <br /> percent of the total rainfall (21.52 inches per year). <br /> Methods in use in San Joaquin County <br /> Within San Joaquin County, four methods have been identified to derive a value for the <br /> rate of recharge from percolating waters: <br /> • 100 Percent of Rainfall: This method involves identifying rainfall levels from the <br /> closest data station to the project site, and assuming that 100 percent of rainfall <br /> deep-percolates to the first saturated zone. This method likely over-estimates the <br /> rate of recharge from percolating waters. <br /> LOGE 1903 Page 9 <br />
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