My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS_XR0011476
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
F
>
FREMONT
>
3246
>
3500 - Local Oversight Program
>
PR0545174
>
ARCHIVED REPORTS_XR0011476
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/13/2020 3:24:25 PM
Creation date
1/13/2020 2:35:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011476
RECORD_ID
PR0545174
PE
3528
FACILITY_ID
FA0004965
FACILITY_NAME
CHEVRON USA (INACT)
STREET_NUMBER
3246
Direction
E
STREET_NAME
FREMONT
STREET_TYPE
ST
City
STOCKTON
Zip
95205
APN
14341001
CURRENT_STATUS
02
SITE_LOCATION
3246 E FREMONT ST
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
Scanner
SJGOV\wng
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
29
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
December 20, 1591 <br /> Chevron U.S.A., Inc. Pape 3 <br /> ' 02320 1883 <br /> hydrocarbons as gasoline (TPH-G) by U.S. Environmental Protection Agency (EPA)-approved methods ; <br /> 5030!8020!8015. One soil sample was analyzed for total lead by SW-846 method 6010. <br /> 4.0 SITE CONDITIONS <br /> 4.1 HVDROGEOLOGY <br /> The site is located in the northern part of the San Joaquin Valley at an elevation of <br /> approximately 25 feet. The valley fill consists of late Mesozoic through Eocene dominantly marine <br /> deposits overlain by late Tertiary and Quaternary dominantly non-marine deposits which usually contain <br /> fresh water. In Stockton area, the late Cenozoic deposits are approximately 3,000 feet thick and <br /> generally consist of alluvial gravel, sand, silt, and clay. Groundwater in these alluvial deposits is <br /> usually unconfined to semiconfined. Extensive Plio-Pleistocene lacustrine deposits, including the <br /> diatomaceous Corcoran Clay, occur in San Joaquin Valley, south of Stockton. The water beneath the <br /> clay bed is usually confined. <br /> The materials penetrated to a depth of 70 feet during drilling at the site are dominantly clays <br /> roxirr ately 30.feet.oyer a period Of three' <br /> with lenses of sand and silt The Water,tble ha �delirted app;., <br /> years fvom: ppio)<it>�at6N,:40,jaet t610406ttieloW 9tad8.. <br /> 4.2 RESULTS OF SOIL ANALYSES <br /> Trace concentrations of petroleum hydrocarbons were detected in only one of the eleven <br /> samples submitted for analyses (Table 1, Appendix C). Sample SBI-K collected at a depth of 70 feet <br /> revealed xylene concentrations of 0.013 parts per million (ppm). Lead was not datected in sample <br /> SBI-K. The laboratory reports for the soil boring samples are enclosed in Appendix D. <br /> Results of laboratory analyses of soil samples recorded during the previous and current <br /> investigations indicate that, except for the trace levels of xylene detected in S91-K, no BTEX <br /> components have been detected in any of the soil samples collected from the soil borings drilled at the <br /> site. <br /> --j , GROUNDWATER <br /> TFfiNNOLOC1:INC. <br /> veeaMwt.rwr <br />
The URL can be used to link to this page
Your browser does not support the video tag.