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SU0001025 SSNL
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MS-92-167
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SU0001025 SSNL
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Last modified
5/7/2020 11:28:13 AM
Creation date
9/6/2019 10:57:27 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0001025
PE
2622
FACILITY_NAME
MS-92-167
STREET_NUMBER
8282
Direction
W
STREET_NAME
LINNE
STREET_TYPE
RD
City
TRACY
Zip
95376
ENTERED_DATE
10/10/2001 12:00:00 AM
SITE_LOCATION
8282 W LINNE RD
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\L\LINNE\8282\MS-92-167\SU0001025\SS STDY.PDF
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EHD - Public
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File No. 20-3683-01 k" K L E IN F E L D E R <br /> December 3, 1992 <br /> obtained for each property parcel are presented in the following table. The County <br /> approved percolation test sheets are included with this report. <br /> PERCOLATION RATES <br /> Percolation Rate <br /> Test Number Parcel (Mins/In.) <br /> P-1 1 30 <br /> P-2 2 15 <br /> P-3 3 30 <br /> Designated <br /> P-4 Remainder 30 <br /> ITEM C-3: <br /> "The depth and gradient of the water table;" <br /> During our surveys on November 10 and 20, 1992, we were able to measure <br /> groundwater in wells at three locations visited. The groundwater was measured at a <br /> depth of approximately 56 feet below existing ground surface in all three wells. The <br /> regional groundwater depth map published by the San Joaquin County Flood Control <br /> and Water Conservation District, Plate II, does not indicate the depth to groundwater <br /> in this area. <br /> Based on County requirements for a parcel split project such as this, we are not <br /> required to establish an on-site groundwater gradient by drilling borings. We are <br /> providing a general estimate of the groundwater gradient based on the published map. <br /> Based on the groundwater map showing lines of equal elevation of groundwater, Plate <br /> III, we conclude that the main groundwater gradient north of the site was in roughly <br /> the north to northeast direction in spring 1992. <br /> We note that our scope of services did not include a detailed evaluation of the potential <br /> for the septic systems to affect the quality of groundwater. However, the project <br /> involves only four possible septic systems within the approximate 30-acre site. <br /> Therefore, with groundwater at approximately 56 feet deep, in our opinion the <br /> likelihood of a significant change in the nitrate level of the groundwater beneath the <br /> site, because of a maximum of four additional systems, is remote. If additional, more- <br /> concentrated development is planned in the area, we suggest that consideration be <br /> given to completing a nitrate loading study. <br /> Copyright 1992 KLeinfelder, Inc. Page 3 of 4 <br />
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