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SU0005296_SSNL
Environmental Health - Public
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2600 - Land Use Program
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PA-0200364
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SU0005296_SSNL
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Last modified
11/19/2024 1:52:16 PM
Creation date
9/8/2019 12:59:53 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0005296
PE
2626
FACILITY_NAME
PA-0200364
STREET_NUMBER
5480
Direction
N
STREET_NAME
STATE ROUTE 99
City
STOCKTON
APN
08703018
ENTERED_DATE
8/15/2005 12:00:00 AM
SITE_LOCATION
5480 N HWY 99
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\sballwahn
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FilePath
\MIGRATIONS\N\HWY 99\5480\PA-0200364\SU0005296\NL STDY.PDF
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EHD - Public
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MKLEIN FELDER <br /> b. 5. SOIL PROFILE <br /> ., The subsurface conditions within then new leach field area were explored on January 28, 2004, <br /> by drilling one boring to a depth of approximately 25 feet below existing grade. The boring <br /> was drilled using a Simco 2400 truck-mounted drill rig equipped with 6-inch O.D. solid-stem <br /> auger. The approximate boring location and approximate dimensions from a reference point <br /> are presented on the site plan (Plate 1). <br /> Based on our findings, the subsurface soils encountered consisted of moderately- to highly- <br /> plastic silty clay to a depth of about 11 feet below existing site grade, followed by low-plastic <br /> sandy silt and sandy clay to a depth of about 16.5 feet. These soils were followed by silty sand / <br /> �- and sandy clay to a depth of about 18.5 feet, silty sand to a depth of about 24 feet, and sandy <br /> clay to a depth of about 25 feet, the maximum depth explored. A detailed description of the <br /> subsurface conditions encountered during our field investigation is presented on the attached <br /> Log of Boring(Plate 3). <br /> The Soil Survey of San Joaquin County, California published by the U.S. Department of <br /> Agriculture, Soil Conservation Service (1992) refers to the near-surface soil within the project <br /> area as belonging to the Hollenbeck and Stockton soil series (Map Symbols 173 and 250, <br /> Lrespectively). The soils are described as having slow permeability characteristics due to high <br /> clay content. Other attributes are given in the table below: <br /> s_ <br /> Map Available Water Capacity, Organic <br /> Symbol Soil Name inches/inch PH <br /> Content, percent <br /> 173 Hollenbeck 0.14 - 0.26 6.6 - 8.4 1 - 2 <br /> ` 250 Stockton 0.14 - 0.17 7.4 - 8.4 2 - 5 <br /> 6. PERCOLATION TESTING <br /> Two 6-inch diameter percolation test holes were drilled directly adjacent to the soil profile <br /> boring to depths of about 3 and 21.8 feet below site grade on January 28. 2004. Following <br /> drilling, the sides of the holes were scored and significant loose material was removed from the <br /> bottom of the hole. The percolation tests were then prepared by first placing about 2 inches of <br /> fine gravel at the bottom of the holes and installing a 4-inch diameter, perforated PVC pipe. (6 io <br /> About 12 inches of water was then placed in the holes for pre-soaking. Since we could not <br /> arrange to perform the tests the followinda the holes were again pre-so ed with about 12 <br /> inches of waterefore9.00 AM on J 04. The percolation tests were started at <br /> 11: 05 AM under sunny and warm weather on January 30, 2004, in accordance with SJCEHD (4- <br /> accepted guidelines using clear potable water. None of the holes exhibited sloughing or caving. <br /> L The holes were empty of water prior to testing. From a fixed reference point (a marked <br /> location on the side of PVC pipe), the drop in water level was measured in approximate 30- <br /> minute intervals for a period of four hours, refilling as necessary to maintain the prescribed�L 5 <br /> amount of water over the gravel (SJCEHD Procedure #2). Under the observation of a <br /> representative from the SJCEHD, the last 30-minute reading of the four-hour period was <br /> 40141.G01/ST04R206 February 24,2004 <br /> ©2004 Kleinfelder,Inc. Page 4 of 7 <br />
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