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SU0012695 SSNL
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SU0012695 SSNL
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Last modified
12/18/2019 11:25:51 AM
Creation date
12/18/2019 11:21:19 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0012695
PE
2611
FACILITY_NAME
SU-90-18
STREET_NUMBER
2984
Direction
N
STREET_NAME
WHITE
STREET_TYPE
LN
City
STOCKTON
Zip
95205-
APN
10108005
ENTERED_DATE
12/17/2019 12:00:00 AM
SITE_LOCATION
2984 N WHITE LN
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\gmartinez
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EHD - Public
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k'q KLEINFELDER <br /> File No . 20-2182-24 <br /> February 20, 1990 <br /> FIELD EXPLORATIONS <br /> The field explorations for this investigation consisted of drilling <br /> 5 test borings on January 25, 1990 to depths of approximately 10 <br /> to 15 feet below existing ground surface and performing one 3 foot <br /> deep percolation test at each lot on January 31 and February 1, <br /> 1990 . The test borings and percolation test holes were drilled <br /> with a truck-mounted drill rig using a 6-inch diameter continuous- <br /> flight auger under the direction of a representative of our firm. <br /> A continuous log of the soils encountered in each boring was <br /> maintained. Relatively undisturbed samples of the soils <br /> encountered were obtained at various intervals for visual <br /> examination, classification, and laboratory testing. Soil samples <br /> were obtained by driving a 2-inch inside diameter sampler into the <br /> soil using a 140-pound hammer falling approximately 30 inches . The <br /> number of blows required to advance the sampler into the soil are <br /> presented on the Logs of Borings, Plates III through VII, at the <br /> corresponding sample locations . The percolation tests were <br /> performed according to San Joaquin County guidelines, and the <br /> procedure and results are discussed in a following section of this <br /> report. <br /> SOIL CONDITIONS <br /> The surface at 4 of the locations explored was covered with <br /> approximately 6 to 12 inches of silt, clay, sand and gravel fill <br /> that contained some debris . The surface fill materials were <br /> underlain by dark grey-brown silty clays that extended to depths <br /> varying from approximately 2 to 4 feet below existing ground <br /> 3 <br />
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