My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS_1989
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
C
>
CORRAL HOLLOW
>
31130
>
4400 - Solid Waste Program
>
PR0440003
>
Archived Reports
>
ARCHIVED REPORTS_1989
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/17/2020 3:52:44 PM
Creation date
7/3/2020 11:04:13 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1989
RECORD_ID
PR0440003
PE
4434
FACILITY_ID
FA0003698
FACILITY_NAME
CORRAL HOLLOW LANDFILL
STREET_NUMBER
31130
STREET_NAME
CORRAL HOLLOW
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
25303010
CURRENT_STATUS
01
SITE_LOCATION
31130 CORRAL HOLLOW RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4434_PR0440003_31130 CORRAL HOLLOW_1989.tif
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
64
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
probably indicates groundwater mounding to the north and east in the <br /> area of the California aqueduct/Delta Mendota canal complex (3). <br /> Shallow perched groundwater beneath the landfill flows to the northeast <br /> toward the San Joaquin River. This perched water appears to be confined <br /> to the eastern half otthe landfill. In addition, the shallow aquifer <br /> in the vicinity of CHSL also deviates slightly from the regional norm by <br /> flowing to the northwest and the southeast, a probable result of <br /> groundwater mounding. The shallow perched aquifer in the vicinity of <br /> the landfill does not contain reliable quantities of drinking water and, <br /> consequently, is not used as a drinking water source (3). <br /> Recharge to the upper water-bearing zones occurs primarily by direct <br /> infiltration of water from precipitation, irrigation, and seepage from <br /> canals and streams. The deep regional aquifer is overlain by <br /> approximately 200 feet of unsaturated, low permeability sediments that <br /> would restrict vertical infiltration of groundwater from the shallow <br /> perched aquifer to the usable deep aquifer. More permeable sections, <br /> however, may occur between the two aquifers (3). <br /> The deep regional aquifer (254 feet below ground surface at CHSL) is a <br /> principal source of drinking water for the City of Tracy and its <br /> environs. The City of Tracy operates a municipal well approximately 1.5 <br /> miles northeast of CHSL. The water from this well is blended through <br /> the municipal water system, which serves a population of approximately <br /> 29,000. The closest well to the site is a domestic well at the Carnegie <br /> Truck Stop, located approximately 2000 feet north of the site on Corral <br /> Hollow Road. This well is screened from 306 to 365 feet in the lower <br /> aquifer. There are an additional 60 private domestic wells within a <br /> 3-mile radius of the facility. The net annual precipitation for the <br /> Tracy area is 8.1 inches (14). <br /> 3.4 SURFACE WATER <br /> The closest surface water to the landfill is Corral Hollow Creek, an <br /> ephemeral stream that runs parallel to the site's southeastern boundary <br /> and lies within 200 feet of the site. Although the facility is located <br /> 3-9 <br /> sa/tm/chl/si <br />
The URL can be used to link to this page
Your browser does not support the video tag.