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ARCHIVED REPORTS_XR0004040
Environmental Health - Public
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EHD Program Facility Records by Street Name
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3500 - Local Oversight Program
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PR0545387
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ARCHIVED REPORTS_XR0004040
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Entry Properties
Last modified
3/5/2020 8:55:12 AM
Creation date
3/5/2020 8:22:14 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004040
RECORD_ID
PR0545387
PE
3528
FACILITY_ID
FA0005718
FACILITY_NAME
SINCLAIR TRUCKING
STREET_NUMBER
3780
Direction
W
STREET_NAME
LINNE
STREET_TYPE
RD
City
TRACY
Zip
95376
CURRENT_STATUS
02
SITE_LOCATION
3780 W LINNE RD
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\sballwahn
Tags
EHD - Public
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clakgiul Technicsinc. Page 2 <br /> Sinclair Trucking <br /> Project No.: 1030.2 <br /> November 1,2005 <br /> C <br /> buildings are covered in compacted base rock material or native soil. As of January 20, 2005, <br /> groundwater bearing and gradient have historically averaged N49°E and 0.0037 ft/ft, <br /> respectively(Table 1 of Appendix A). <br /> f ST is located in the southeast quarter of the northwest quarter of Section 7, T3S, R6E, related <br /> IL to the Mount Diablo B&M, on the United States Geological Survey (USGS) topographic <br /> map, Vernalis Quadrangle, California, 7.5 minutes series. A review of the USGS <br /> Topographic Map reveals that the elevation of this site is approximately 75 feet above mean <br /> sea level (AMSL). <br /> The site is located on the gradually sloped floor of the northern San Joaquin Valley. The <br /> geologic composition of the area is characterized as fluvial deposits of the San Joaquin - <br /> Sacramento River delta system that overlay continental rocks and deposits derived from <br /> erosion of the Sierra Nevada Mountain Range located approximately 50 miles northeast of <br /> Modesto. <br /> The southwest tilting Sierra Nevada fault block underlies the northern San Joaquin Valley <br /> area. Overlying the consolidated rocks are unconsolidated sediments. The lower <br /> consolidated batholithic and metamorphic rocks are poorly transmissive, however the <br /> overlying sedimentary layers are often quite permeable. These unconsolidated layers include <br /> j f Pliocene/Pleistocene age continental deposits, Pleistocene age lacustrine and marsh deposits, <br /> and Holocene older and younger alluviums and flood-basin deposits. <br /> 1.2 Site Background <br /> On March 31, 1989, one steel 250-gallon underground storage tank (UST), used to supply <br /> leaded gasoline, was removed from the site. The SJCEHD inspection report indicated that <br /> corrosion was present on the UST and a petroleum odor was noticeable in the area of the tank <br /> removal. Subsequent laboratory soil analyses indicated the presence of petroleum <br /> hydrocarbons at the site. A limited over excavation to a depth of 18-feet bgs was conducted <br /> in the general area of the UST and was backfilled with native soil. <br /> fOn June 14, 1995, Geological Technics Inc. (GTI) installed three monitoring wells and <br /> advanced one soil boring in order to evaluate the vertical and lateral extent of gasoline range <br /> petroleum hydrocarbons. <br /> On February 16, 1999, GTI personnel supervised the installation of one groundwater <br /> monitoring well down gradient of the former UST to further define the lateral extent of <br /> - - =gasoline contamination in the soil and groundwater. This well showed low levels of gasoline - --- <br /> range hydrocarbons. <br /> In response to a request by Mr. Ron Rowe of SJCEHD,GTI prepared a work plan on January <br /> 18, 2000, to define the lateral extent of the soil and groundwater contamination at the site. <br /> On April 20, 2000, Ms Lori Duncan, SJCEHD, issued a letter denying the approval of the <br /> work plan. During phone conversations in May of 2000, Ms Duncan requested that a work <br />
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