My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS_XR0004486
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
L
>
LARCH
>
425
>
2900 - Site Mitigation Program
>
PR0541913
>
ARCHIVED REPORTS_XR0004486
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
2/13/2020 4:08:03 PM
Creation date
2/13/2020 1:55:34 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004486
RECORD_ID
PR0541913
PE
2960
FACILITY_ID
FA0024043
FACILITY_NAME
FRONTIER TRANSPORTATION FACILITY
STREET_NUMBER
425
STREET_NAME
LARCH
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
21220009
CURRENT_STATUS
01
SITE_LOCATION
425 LARCH RD
P_LOCATION
03
QC Status
Approved
Scanner
SJGOV\sballwahn
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
20
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
Report of Findings <br /> • Frontier Transportation, Inc. <br />' August 31, 2005 <br /> Page 3 <br /> migration of MTBE to the west Levels of dissolved MTBE have been consistently high(above ` <br /> tMCL of 14 ug/L) in MW-1 and MW-3R Elevated levels of MTBE first appeared in MW-9 in <br /> March 2005 Shallow monitoring well MW-1q has identified dissolved MTBE during every <br /> sampling event since its installation in January 200 'v"'` -06 <br /> v <br /> 3.0) SITE GEOLOGY/HYDROGEOLOGY <br />' The site is located on the boundary of the Sacramento Valley and the San Joaquin Valley <br /> within the west-central portion of the Great Valley Geomorphic province of California The <br /> Great Valley has been filled with a sequence of older to younger alluvium of Pliocene to Holocene <br /> age which overlay sedimentary rocks of Cretaceous to Tertiary age These sedimentary units, in <br /> turn, overlay a crystalline basement of Paleozoic and Mesozoic metamorphic and igneous rocks <br />' The shallow subsurface geology in the site vicinity is a heterogeneous mix of gravel, sand, silt, and <br /> clay (Reference, Site Characterization Re ort, Twining Laboratories, October 16, 1996) <br /> BEII encountered predominantly heterogeneous clays from 0'to 30' bgs and fine-grained <br /> sands from 30' to 40' bgs,during well advancement of MW-15 through MW-18 <br /> LeFirst subsurface water was encountered at depths from 11'to 12'bgs during tank removal <br /> and monitoring well installation at this site in 1995 and 1996 Since then, shallow subsurface <br /> water has been encountered beneath the site between 6 and 10' bgs The three newly installed <br /> r shallow wells MW-19, MW-20 and MW-21 encountered groundwater at approximately 9 5' to <br /> 14' bgs during boring advancement J <br /> ' The past groundwater gradients included in quarterly groundwater monitoring reports <br /> have identified the flow of groundwater in a generally western direction beneath the site <br /> 4.0) SITE ASSESSMENT RESULTS <br /> ' On August 1, 2005 and August 2, 2005, BEA supervised the installation of groundwater <br /> monitoring wells MW-19, MW-20 and MW-21 to help define the extent of dissolved MTBE <br /> beneath the site and determine soil column contamination (See Figure 2 for well locations) <br /> Shallow monitoring wells MW-19, MW-20 and MW-21 were advanced to 20' bgs <br /> ' An 8-inch outside and 4 25-inch inside diameter hollow stem auger was used to install the <br /> monitoring wells The new groundwater monitoring wells were constructed of schedule 40 PVC <br /> casing The screen slots were sized at 0 01-inch with a size#2/16 sand annular pack The new <br /> shallow wells were screened from 5' to 20' bgs and the sand annular pack extended from 4 5' bgs <br /> • <br /> t <br /> r <br />
The URL can be used to link to this page
Your browser does not support the video tag.