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ARCHIVED REPORTS_XR0004840
Environmental Health - Public
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EHD Program Facility Records by Street Name
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MACARTHUR
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24500
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2900 - Site Mitigation Program
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PR0505329
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ARCHIVED REPORTS_XR0004840
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Last modified
3/4/2020 9:26:58 AM
Creation date
3/4/2020 8:45:09 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004840
RECORD_ID
PR0505329
PE
2950
FACILITY_ID
FA0006715
FACILITY_NAME
TRACY COLD STORAGE INC
STREET_NUMBER
24500
Direction
S
STREET_NAME
MACARTHUR
STREET_TYPE
DR
City
TRACY
Zip
953780420
APN
25024001
CURRENT_STATUS
02
SITE_LOCATION
24500 S MACARTHUR DR
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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' 3-2 <br /> encountered in other areas of the site, except for Boring MW-4 winch contained approxi- <br /> mately two feet of loose gravel from a former railroad spur that has been removed <br /> I <br /> In areas where fill is not present, a dark brown silt was encountered from the ground surface <br /> �r to 2 ft-bgs The silt was generally dry and contained organic material <br /> Underlying the fill and/or silt units and typically to the bottom of the borings (16 to 18 <br /> ft-bgs), a dark brown to brown silty clay was encountered In the vicinity of the former <br /> UFT, the silty clay was believed to be stamed by gasoline constituents and appeared gray to <br /> greenish-gray in color, and often had a petroleum odor associated with the staining Gener- <br /> ally, the silty clay unit contained trace amounts of fine sand at depths of 12 to 18 ft-bgs <br /> The moisture content generally increased with depth and the silty clay unit often became <br /> saturated near the bottom of the borings at depths from 12 to 16 feet <br /> 312 Hydmgeology <br /> The site is located in the Central Valley portion of California The unconsolidated sediments <br /> comprising the aquifer system include gravel, sand, silt, and clay and are of both marine and <br /> non-marine origin Ground water occurs under both confined and water table conditions <br /> Ground water at the site was typically encountered at a depth of 12 to 14 ft-bgs and in some <br /> instances static water levels were recorded at higher elevations in the completed monitoring <br /> wells, suggesting locally confined or semi-confined conditions A potentnometrnc surface <br /> map was prepared based on water levels obtained on August 26, 1994 (Table 4) The poten- <br /> tiometric surface, depicted in Figure 4, shows shallow ground water generally flowing to the <br /> north-northwest with a hydraulic gradient of approximately 0 004 foot per foot (ft/ft) <br /> There is an indication that the two supply wells may be affecting the shallow water-bearing <br /> zone (Figure 4) The ground water flow direction appears to change to a more northwesterly <br /> direction in the vicinity of the supply wells (Figure 4) Remcor has not been able to obtain <br /> detailed information concerning, construction (total depth, screened interval, cased inter- <br /> val[s]), lnthologic boring logs, water levels, or pumping rates of these two supply wells, this <br /> 29025 <br /> ' "REALISTIC SOLUTIONS FOR HAZARDOUS WASTE PROBLEMS" <br />
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