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SU0000142 SSNL
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MS-98-06
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SU0000142 SSNL
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Last modified
5/7/2020 11:27:38 AM
Creation date
9/8/2019 12:36:11 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000142
PE
2622
FACILITY_NAME
MS-98-06
STREET_NUMBER
1560
Direction
W
STREET_NAME
OHM
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
25508002
ENTERED_DATE
8/14/2001 12:00:00 AM
SITE_LOCATION
1560 W OHM RD
RECEIVED_DATE
2/25/1998 12:00:00 AM
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\O\OHM\1560\MS-98-06\SU0000142\SS STDY.PDF
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EHD - Public
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" comparison to the low density housing and indicates the shallow soils in the area are not conducive <br /> to acceptable management of sewage effluent over long periods of time. This is primarily attributed <br /> to the tight, silty soils at the leachline depth. <br /> [3] SOIL PROFILE AND PERCOLATION TESTING <br /> One shallow percolation test was conducted on Parcel 1 according to San Joaquin County <br /> Department of Environmental Health regulations. No perc test was performed on the Designated <br /> Remainder per Department regulations. The perc test location is illustrated on the attached Parcel <br /> Map. Percolation test results can be found on the Field Test Data Sheet in the Appendix. <br /> Perc test results indicate a comparatively fast percolation after the four hour test period. Soil <br /> structures consists of a tight sandy silt (SM) throughout the shallow soil profile. No hardpan <br /> _ layer was encountered. The boring was pre-saturated the total depth, 24 hrs prior to starting the <br /> perc test to induce worst-case saturated soil conditions. <br /> Percolation test results indicate a perc rate of 7.1 min/in for Parcel 1. Considering the soil type, <br /> this rate can be considered favorable. It is our opinion that the material at the test depth of 42 <br /> inches is of sufficient porosity to allow water infiltration and percolation. However, repeated <br /> saturations from septic effluent in conjunction with the propensity of the soil to build up a biomat, <br /> leads to leachline failures as evidenced by the repairs. <br /> [4] LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The static water table depth, or the zone of saturation is located at approximately 55 feet below grade <br /> from the sounding of a domestic well on Ohm Road. The 1996 "Lines of Equal Depth" published by <br /> " the San Joaquin County Flood Control District does not reference the static water table depths in this <br /> area. It is possible there may be perched water table conditions under the subject property at a higher <br /> elevation than the static water level and this should be investigated if seepage pits are ever installed. <br /> There is no potential for septic impact to any surface waters, providing applicable distance <br /> requirements are followed. The property is not in the flood plain. <br /> Analysis of water drawn from the domestic well at the farm labor residences near the intersection of <br /> Ohm Road and Koster Road indicates a nitrate concentration of 22 ppm NO3. The Maximum <br /> Contaminant Level (MCL) for NO3 in drinking water is 45 ppm. The pesticides DBCP and EDB <br /> were not detected(ND). A nitrate concentration of 22 ppm indicates the underlying shallow aquifers <br /> have been moderately impacted from nitrogen contributors, such as agricultural operations, septic <br /> systems or rainfall. No well logs were available in the area to verify if clay layers may have helped <br /> attenuate the downward migration of nitrate molecules. <br /> 2 <br />
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