My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FIELD DOCUMENTS
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
C
>
CHARTER
>
1821
>
3500 - Local Oversight Program
>
PR0544468
>
FIELD DOCUMENTS
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/16/2019 4:31:25 PM
Creation date
5/16/2019 4:22:35 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0544468
PE
3528
FACILITY_ID
FA0025278
FACILITY_NAME
RENTAL MACHINERY COMPANY
STREET_NUMBER
1821
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
1821 E CHARTER WAY
P_LOCATION
01
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.
/
33
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
23 June 1998 - <br /> AGE-NC Project No. 97-0349 <br /> Page 2 of 5 <br /> valley is a nearly flat,elongate trough trending northwest and southeast for approximately 450.miles. <br /> e,. The valley is enclosed by the granitic Sierra Nevada on the east and the sedimentary and <br /> metamorphic Coast Ranges on the west. The nearly flat-laying surficial and upper several hundred <br /> feet of subsurface layers consist primarily of unconsolidated alluvial and floodplain deposits <br /> (predominantly sand, silt, and clay) of Quaternary age,which'were derived frgm the mountains of <br /> the Sierra Nevada. Beneath the upper'sedimentary deposits lie a thick sequence of marine deposits <br /> of Mesozoic age,which in turn are underlain by a pre-Jurassic complex of igneous and metamorphic <br /> `y basement rock. ' <br /> `y 2.4. GROUND WATER DEPTH AND FLOW DIRECTION <br /> The estimated depth to ground water at the site is 50 feet below surface grade (bsg) based on. <br /> information from Lines of Equal Depth of Water Wells Fall 1993, published by the San Joaquin <br /> County Flood .Control District -.and Water Conservation District and ground water depth <br /> �., measurements in monitoring wells located approxim_ately.400 feet north and'200 feet south of the <br /> site (Re-Manufacturing). <br /> Ground water flow direction, as determined from the Re-Manufacturing site, is south-southeast. . <br /> However, due to local seasonal variations flow direction may vary. The uppermost ground water <br /> flows in an unconfined aquifer..With increasing depth, the aquifer becomes semi_confined, due to <br /> the presence of fine of sediments: <br /> 3.0. PROCEDURES <br /> 3.1. PROBING AND SAMPLING <br /> LM <br /> s One soil probe boring (PB 1)was advanced at the site, under the observation of a representative of <br /> �. the PHS-EHD..On 21 August.1997,probe boring PB 1 was advanced in the former UST area to a <br /> depth of 65 feet bsg. Location of the soil probe boring is illustrated on-Figure 2. <br /> Soil samples were collected from each boring at five-foot intervals, beginning at a depth of 5 feet <br /> bsg and continuing to a depth'of 50 feet bsg, using a Geoprobe soil sampling assembly and four <br /> brass sleeves. Samples were collected using a 2.15-inch diameter,two-foot long;piston-type sampler <br /> `y loaded with four pre-cleaned 1.375-inch by 6-inch brass sleeves.'The sampling equipment was <br /> washed in an Alconox solution and rinsed with water prior.to,each sampling run to prevent cross- <br /> contamination.After collection,the ends of the second brass sleeve were covered with Teflon sheets, <br /> capped and sealed with tape. Samples were placed in a chilled container under ice and transported <br /> to McCampbell Analytical, Inc, (MAI)under chain-of-custody. <br /> Advanced GeoEnvironmental,Inc. <br />
The URL can be used to link to this page
Your browser does not support the video tag.