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PR0508319
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Last modified
2/1/2019 5:15:32 PM
Creation date
2/1/2019 4:25:06 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0508319
PE
2950
FACILITY_ID
FA0008031
FACILITY_NAME
FORTIFIBER
STREET_NUMBER
501
Direction
E
STREET_NAME
ACACIA
STREET_TYPE
ST
City
STOCKTON
Zip
95202
CURRENT_STATUS
01
SITE_LOCATION
501 E ACACIA ST
P_LOCATION
01
QC Status
Approved
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EHD - Public
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CJeologicaC7eckrcics inc, • • Page 3 <br /> Fonzia <br /> SGWI Report <br /> Project No.: 774.2 <br /> June 10, 1999 <br /> ' 1.0 SCOPE OF INVESTIGATION <br /> GTI advanced 4 additional boreholes utili ing the GeoProbe® direct-push method to further <br /> define the lateral and vertical extent of petroleum hydrocarbon-impacted soil and <br /> groundwater beneath the site. <br /> 1.1 Borehole Drilling & Soil Sample Collection <br /> On May 24 & 25, 1999, GTI conducted' additional site characterization. Four GeoProbe <br /> boreholes (GP-14 through GP-17)were advanced at the locations indicated on Figure 2. The <br /> I boreholes were drilled with a GeoProbe® drilling rig owned and operated by V&W Drilling <br /> of Rio Vista, CA (C57# 720904). The Ge Probe®rig advances a continuous coring tool with <br /> a pneumatic hammer to a selected depth. The soil sample enters an acetate cylinder <br /> ' contained in the coring tool. Upon filling, the coring tool is pulled from the borehole and the <br /> soil cylinder is removed. A selected interval(s) was cut from the cylinder and preserved for <br /> laboratory analysis. The remainder of th soil sample was used for geologic logging and <br /> ' subjectively field-screened with an organic vapor meter (OVM). The OVM is a portable <br /> photo-ionization detector that uses a 10.0 eV lamp to detect compounds with ionization <br /> potentials below 10.0 eV (hydrocarbon range). All collected soil samples were sealed with <br /> plastic end caps, labeled, and placed in a cooler chilled to 4° Celsius for transport to the <br /> ' laboratory following Chain of Custody (COC)protocol. <br /> The sediments were logged by a GTI geologist under the supervision of Ray Kablanow, a <br /> I California registered geologist. The soils were logged according to the Unified Soil <br /> Classification System (USCS) and recorded with field observations on borehole logs <br /> (Appendix C). <br /> Soil samples were collected at depths pre-approved by the SJC PHS/EHD for each boring: <br /> • Boring GP-14 was drilled to approximately 37 feet bgs, and soil samples were <br /> collected at 12, 19, 28, and 33 feet bgs. <br /> • Boring GP-15 was drilled to approximately 11.5 feet bgs and soil samples were <br /> collected at 9 and 11 feet bgs. <br /> • Boring GP-16 was drilled to approximately 12 feet bgs. A soil sample was collected <br /> ' at 12 feet bgs. <br /> • Boring GP-17 was drilled to approximately 12 feet bgs. Soil samples were collected <br /> from 9 and 12 feet bgs. <br /> ' The soil samples were submitted for the rc quested analyses to the State-certified laboratory, <br /> BSK Analytical Laboratories (BSK) in Fre no, California under COC protocol. <br /> ' 1.2 Groundwater Sample Collection <br /> Groundwater samples were collected with a HydroPunch®-type sampler at depths pre- <br /> approved by the SJC PHS/EHD for each boring. The groundwater samples were gently <br /> transferred into 1-liter amber glass bottles pd Y2-liter poly bottles. The bottles were labeled <br /> and placed in a cooler at 4° Celsius for transport to the laboratory following COC protocol. <br /> ' Clean surgical gloves are worn at all times in handling of the sample and sampling <br /> equipment. All down-hole equipment was cleaned with an Alconox solution and pressure <br /> washed between each sampling interval. The joints in the drill rods were additionally sealed <br /> with factory o-rings and teflon tape to prevent cross-contamination. <br /> 1 <br />
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