My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0007980 SSNL
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
G
>
GAWNE
>
23004
>
2600 - Land Use Program
>
PA-0900272
>
SU0007980 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/7/2020 11:33:19 AM
Creation date
9/5/2019 10:40:47 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0007980
PE
2622
FACILITY_NAME
PA-0900272
STREET_NUMBER
23004
Direction
E
STREET_NAME
GAWNE
STREET_TYPE
RD
City
STOCKTON
APN
18708004
ENTERED_DATE
11/16/2009 12:00:00 AM
SITE_LOCATION
23004 E GAWNE RD
RECEIVED_DATE
11/13/2009 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\G\GAWNE\23004\PA-0900272\SU0007980\SS STUDY.PDF
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
41
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
Ground Water Information <br /> Depth and Gradient <br /> Live Oak reviewed ground water elevation information available from the San Joaquin <br /> County Flood Control and Water Conservation District to determine the ground water <br /> levels near the Site. Data from spring and fall of 2009 were the most recent available <br /> from this source. According to an analysis of these maps (Plates 5 and 6), ground <br /> water elevation is 0 to 15 feet below mean sea level; ground water flows down to the <br /> northwest at a rate of 7.7 to 14.2 feet per mile in the vicinity of the Site. <br /> Given that the ground elevation of the Site is approximately 90 feet, the depth to water <br /> below the Site is estimated to range between 90 to 105 feet, depending on the season. <br /> Potential Ground Water Contamination Issues <br /> The Soil Suitability Study isC not intended to be an investigation into ground-water <br /> contamination sources, and s- ch investigation was conducted. Many sources can <br /> contribute to ground water contamination, including leaking underground storage tanks, <br /> agricultural activities, dairies, septic systems, and storm water infiltration. Agricultural <br /> activities and the use of septic systems in the area are known ground water <br /> contamination sources with the potential to impact the Site. <br /> n-Site Wells <br /> Nowells exist on the Site. No well permits for the Site were identified at the San/ <br /> Joaquin ounty Environmental Health Department. <br /> Water Sample <br /> (N�o ter sample was collected from the Site. <br /> .Soil Profile and Geologic Information <br /> The Site can be found on the Geologic Map of Califomia, San Jose sheet (Rogers, <br /> 1966). It is depicted within map units of Pleistocene nonmarine deposits and stream <br /> channel deposits (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the USDA Web <br /> Soil Survey to be composed of Madera sandy loam and Madera-Alamo complex, with a <br /> small area of Galt clay north of the canal (Plate 8) (USDA, 2009). The table below <br /> presents some selected properties of these soils: <br /> LOGE1018 Page 3 <br />
The URL can be used to link to this page
Your browser does not support the video tag.