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SU0005702 SSNL
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SU0005702 SSNL
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Entry Properties
Last modified
5/7/2020 11:31:42 AM
Creation date
9/5/2019 10:49:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0005702
PE
2631
FACILITY_NAME
PA-0500676
STREET_NUMBER
5555
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
APN
21317039
ENTERED_DATE
10/17/2005 12:00:00 AM
SITE_LOCATION
5555 W GRANT LINE RD
RECEIVED_DATE
10/12/2005 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\G\GRANT LINE\5555\PA-0500676\SU0005702\NL STDY.PDF
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EHD - Public
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r <br /> August 22, 2007 <br /> NOA Project Number: E07109A <br /> Hantzsche and Finnemore found that over a long period of time,water quality in the upper <br /> p saturated ground-water zone closely approximates the quality of percolating recharge waters. They <br /> believe that their method is a good planning tool to estimate the potential impact to groundwater, <br /> and provides useful information to planners and local officials but with some real limitations. In <br /> their article published in Ground Water, Hantzsche and Finnemore mention that "...the equation <br /> P� ignores dispersion,lateral flow, and mixing with ground water flow from up-gradient areas. These <br /> processes would generally contribute to additional reduction of nitrate-nitrogen concentrations in <br /> ground water to the extent that the nitrate-nitrogen concentration of ground--water flow from <br /> up-gradient areas is lower." <br /> The Hantzsche and Fennemore approach is "...a conservative (worst case) first approximation of <br /> ground-water nitrate-nitrogen concentration resulting from the combined effect of on-site sewage <br /> disposal systems and precipitation. This (the equation and approach) is for estimation of long-term. <br /> } effect (i.e., over years) on ground-water quality, and is not intended for prediction of seasonal <br /> changes" (Hantzsche and Finnemore, 1992). <br /> The method takes into account the development area, soil denitrification factor, rainfall volume, <br /> Fli rainfall nitrate concentration,waste effluent quantity, and waste effluent nitrate concentration. The <br /> { formula, assumptions and calculations used for the analysis are shown on Plates 9 and 10. The units <br /> jof nitrate used in the mass balance equation are nitrate-N,whose maximum drinking water <br /> l 1 contaminant level is 10 mg/L. <br /> F1.0 CHEMICAL AND PHYSICAL PROPERTIES OF SOIL <br /> 1.1 Chemical and Physical Soil erties <br /> I <br /> Fj <br /> Five shallow percolation tests and an 8.5�the�urface <br /> tgroundwater boring were excavated by out office on, <br /> the site on July 26, 2007. The soil from of the ground to a depth of approximately 8.5 <br /> pfeet was a dark grey clay with some silt— he percolation tests were conducted for the shallow <br /> borings on the site on July 27, 2007 in accordance with the requirements of the FHD. A -' <br /> Fation of four hours was performed for each hole. Please see G1 on thepercolation test with a dur <br /> Design and Layout of the septic system for more details regarding location of the percolatjon tests. <br /> The last half an hour was observed by Mr. Nick Weisman, of the San Joaquin EHD. <br /> � For more discussion of on-site soil properties, refer to Section 7 of the SSS/NLS (Kleinfelder, <br /> E.± 2007 . <br /> a ) <br /> �i F1 <br /> F14 <br /> 3 <br /> F <br />
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