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SU0000560 SSNL
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SU0000560 SSNL
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Entry Properties
Last modified
5/7/2020 11:27:47 AM
Creation date
9/5/2019 10:51:30 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000560
PE
2622
FACILITY_NAME
MS-91-83
STREET_NUMBER
29554
Direction
E
STREET_NAME
GROOMS
STREET_TYPE
RD
City
OAKDALE
ENTERED_DATE
9/21/2001 12:00:00 AM
SITE_LOCATION
29554 E GROOMS RD
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\G\GROOMS\29554\MS-91-83\SU0000560\SS STDY.PDF
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EHD - Public
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[4] SOIL PROFILE AND PERCOLATION TESTING <br /> Soil profile information from the drilling of domestic wells, and <br /> the installation of septic systems in the area of the subject site <br /> were obtained from the San Joaquin Department of Environmental <br /> Health. The Well Logs illustrate a soil structure of primarily <br /> clay lenses, sand and shale. There is a hardpan layer <br /> approximately two to three feet under the subject site. The <br /> exploratory Log of Boring performed on the subject parcel <br /> illustrates the soil structure under the proposed leaching area, <br /> and it accompanies our percolation test data. <br /> The percolation tests conducted by Quality Control Inspection, Inc. <br /> were performed in accordance with San Joaquin Environmental Health <br /> Department regulations. The test results can be found in the <br /> Appendix. The percolation rate, as tested for the deep test boring <br /> (8 ft, 8 in) , was calculated to be 1. 6 minutes per inch. <br /> The predominate soil type encountered during the drilling to <br /> conduct the percolation tests was a sand formation found under the <br /> surface (2-3 feet) hardpan layer. This sandy soil structure <br /> produces a relatively fast percolation rate for sewage effluent as <br /> evidenced by the above percolation rate. <br /> [5] LOCAL GROUNDWATER INFORMATION <br /> The 1990 "Lines of Equal Depth of Water in Wells" map produced by <br /> the San Joaquin County Flood Control and Water Conservation <br /> District indicates that the static water level is located at <br /> approximately 80 feet in the area of the subject parcel. An <br /> exploratory test hole was drilled in the lowest point of the two <br /> parcels to a depth of 25 feet, revealing no indication of moist <br /> soil or any past history of a water table at this depth. The <br /> groundwater flow according to the District maps appears to be <br /> towards the northwest, although many factors can influence this <br /> general groundwater directional flow. <br /> 3 <br /> .e QWlity 10ntrol Inspection <br />
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