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SU0003863 SSNL
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SU0003863 SSNL
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Entry Properties
Last modified
5/7/2020 11:30:10 AM
Creation date
9/9/2019 10:17:50 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0003863
PE
2622
FACILITY_NAME
PA-0300678
STREET_NUMBER
24720
Direction
N
STREET_NAME
SOWLES
STREET_TYPE
RD
City
ACAMPO
ENTERED_DATE
5/11/2004 12:00:00 AM
SITE_LOCATION
24720 N SOWLES RD
RECEIVED_DATE
2/3/2004 12:00:00 AM
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\S\SOWLES\24720\PA-0300678\SU0003863\SS STDY.PDF
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EHD - Public
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~ v kn KLEINFELDER <br /> — We do not know of groundwater contamination issues at the site at this time. The potential <br /> exists for groundwater to be contaminated through the use of pesticides and herbicides. <br /> Potential sources of nitrate include fertilizer that may be used in the area, as well as septic <br /> usage of the nearby single-family residences. <br /> 5. SOIL PROFILE <br /> The subsurface conditions at the site were explored before noon on March 18, 2004 by drilling <br /> two borings to a depth of about 15 feet below existing grade. The borings were drilled using a <br /> Simco 2400 truck-mounted drill rig equipped with 4'/2-inch O.D. solid-stem auger. The <br /> approximate location of the test borings and dimensions from a reference point are presented on <br /> -� the Plate 1. <br /> Based on our findings, the subsurface soils encountered in boring B-1 consisted predominately <br /> of moderately plastic sandy clay to a depth of about 7'/z feet below the existing site grade, <br /> underlain by silty sand to the maximum depth explored. The silty sand encountered was <br /> weakly cemented to a depth of about 12% feet below the existing ground surface. <br /> The soils encountered in boring B-2 generally consisted of highly interbedded strata of low- <br /> plastic sandy silt, moderately-plastic sandy clay, and fine-grained silty sand to a depth of about <br /> 11 feet below the existing site grade, underlain by relatively "clean" sand to the maximum <br /> depth explored. <br /> More detailed descriptions of the subsurface conditions encountered during our field <br /> investigation are presented on the Logs of Borings, Plates 5 and 6. <br /> 1/ 6. PERCOLATION TESTING <br /> Shallow and deep percolation test holes were installed in each of the proposed parcels with the <br /> same rig used to drill the soil profile borings, only equipped with a 6-inch diameter auger. The <br /> approximate percolation test locations are presented on Plate 1. Following drilling, the sides of <br /> the holes were scored, and significant loose material was removed from the bottom of the <br /> holes. The holes were drilled and prepared before noon on March 18, 2004, in accordance <br /> with SJCEHD criteria. Approximately 2 inches of fine gravel was placed at the bottom of each <br /> test hole, and the holes were presoaked with a minimum of 12 inches of water at that time. The <br /> percolation tests were started at about 10:00 AM under sunny and warm weather on March 19, <br /> 2004, in accordance with accepted guidelines using clear potable water. The approximate <br /> depth of each percolation test below existing site grade is shown on the following table. The <br /> holes did not exhibit sloughing or caving. At the time of testing, standing water from the <br /> presoaking remained in the shallow hole at location P-1 and at the deeper holes at P-2 and P-3. <br /> From a fixed reference point, a marked location on the side of PVC pipe inserted into each <br /> hole, the drop in water level was measured in approximately 30-minute intervals for four hours, <br /> refilling as necessary to maintain the prescribed amount of water over the gravel (SJCEHD <br /> October 15,2004 <br /> 42270.G01/ST041383 <br /> Page 3 of 6 <br /> ©2004 Kleinfelder,Inc. <br />
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