My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS XR0005966
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
C
>
COUNTRY CLUB
>
2081
>
3500 - Local Oversight Program
>
PR0544590
>
ARCHIVED REPORTS XR0005966
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/21/2019 2:12:54 PM
Creation date
6/21/2019 11:10:49 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0005966
RECORD_ID
PR0544590
PE
3528
FACILITY_ID
FA0003932
FACILITY_NAME
KWIKEE FOODS
STREET_NUMBER
2081
STREET_NAME
COUNTRY CLUB
STREET_TYPE
BLVD
City
STOCKTON
Zip
95204
APN
12315225
CURRENT_STATUS
02
SITE_LOCATION
2081 COUNTRY CLUB BLVD
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.
/
21
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
FIRST QUARTER REPORT <br /> KWIKEE FOODS <br /> 2081 Country Club Boulevard <br /> Stockton, California <br /> February 26, 1999 <br /> EXECU'T`IVE SUMMARY <br /> Groundwater monitoring at the Kwikee Food site took place on January 28, 1999. The depth to <br /> groundwater in the three monitoring wells was measured with a Solinst water level meter, and a <br /> battery-operated purge pump was used to purge the wells of standing water. Fourty-five gallons of <br /> water were removed from the wells and stored in a DOT-approved drum on site. After purging, <br /> water samples were collected in glass vials and transported to the laboratory and were analyzed for <br /> Total Petroleum Hydrocarbons as gasoline and BTEX_ <br /> As in May 1998, the present groundwater gradient is southwest, at 0.025 ft/ft. This is in contrast <br /> to an east or northeast gradient, which is the more typical pattern. The present gradient <br /> demonstrates that the southwest gradient in May 1998 was not a fluke, but was due to Subsurface <br /> conditions that apparently prevail only during part of the year. This alternating southwest and <br /> northeast flow presumably creates a "sloshing" effect on gasoline hydrocarbons in the aquifer, <br /> preventing the contaminants from consistently migrating in one direction away from the. site. <br /> As in the past, hydrocarbons were detected in all wells, but at concentrations similar to Vose in the <br /> past two monitoring events rather than at the much higher concentrations that were commonplace <br /> prior to 1998. This sharp decline in concentrations may be the result of the removal in March 1998 <br /> of the two USTs that were formerly present, but it is also possible that the reduction is Niue to the <br /> exceptionally high water table that has existed for over a year. Because of the high wate'- table, the <br /> screened interval in all three wells is several feet below the soil-groundwater inteiface. It is <br /> therefore too early to conclude that the decrease in concentrations is real; additional monitoring, <br /> probably supplemented with additional monitoring wells, will be required before a clear picture of <br /> contaminant behavior can be developed at this site. <br /> f <br />
The URL can be used to link to this page
Your browser does not support the video tag.