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ARCHIVED REPORTS XR0004973
Environmental Health - Public
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EHD Program Facility Records by Street Name
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M
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MUNFORD
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3730
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3500 - Local Oversight Program
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PR0544305
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ARCHIVED REPORTS XR0004973
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Entry Properties
Last modified
4/3/2019 2:51:15 PM
Creation date
4/3/2019 2:49:41 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004973
RECORD_ID
PR0544305
PE
3528
FACILITY_ID
FA0003736
FACILITY_NAME
CLIPPER GROUP
STREET_NUMBER
3730
Direction
E
STREET_NAME
MUNFORD
STREET_TYPE
AVE
City
STOCKTON
Zip
95205
APN
17956010
CURRENT_STATUS
02
SITE_LOCATION
3730 E MUNFORD AVE
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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development of this soil has occurred also The development is a tight clay subsoil and is the <br /> result of transport and re-deposition of very fine particles from the top of the soil profile to the <br /> subsoil, resulting in a high colloidal clay content and impervious structure in the subsoil <br /> Deeper lithology and site geology is related to the surface soils The site is mapped by the U S <br /> ' Geological Survey as "basin deposits " Basin deposits have hthologic profiles dominated by <br /> fine textured materials However, intercalating layers of coarser textured materials are common <br /> and usually capable of freely releasing water Municipal water wells drilled in the general area <br /> penetrate through alternating clays and sands to a depth of 250 feet or more before intentionally <br /> extracting water <br /> The closest surface water to the site is Duck Creek, approximately 115 of a mile to the north <br /> Mormon Slough is approximately 1 5 miles north of this site The piezometric level of <br /> groundwater has been reported to be between 70 and 80 feet below the surface at the site (San <br /> Joaquin County Flood Control and Water Conservation District, 1992 data) Municipal wells <br /> IPseal off the first 250 feet because the upper zones of saturation do not meet quality standards or <br /> do not provide sufficient quantity to be developed (Bulletin 146, California Department of Water <br /> Resources, 1967) Therefore, it is highly unlikely the fuel components at this site have affected <br /> or will affect drinking water supplies <br /> 1 <br /> Groundwater flow beneath the site is expected to be in the north-northeastern direction toward <br /> ' a groundwater pumping depression located northeast of Stockton (San Joaquin County Flood <br /> Control and Water Conservation District, Spring 1992) <br /> 1 <br /> 3.0 PROPOSED FIELD WORK - METHODS AND PROCEDURES <br /> ' A subsurface site investigation will be performed to characterize current soil and groundwater <br /> conditions beneath the site The investigation will consist of drilling and sampling three soil <br /> ' borings, and conversion of the soil borings to groundwater monitoring wells <br /> WP-0393 FNL 3 <br />
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