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ARCHIVED REPORTS_XR0011731
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0541344
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ARCHIVED REPORTS_XR0011731
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Last modified
12/13/2019 1:26:39 PM
Creation date
12/13/2019 11:33:36 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011731
RECORD_ID
PR0541344
PE
2960
FACILITY_ID
FA0023692
FACILITY_NAME
GUARDINO & CRAWFORD
STREET_NUMBER
517
Direction
W
STREET_NAME
FREMONT
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
13721410
CURRENT_STATUS
01
SITE_LOCATION
517 W FREMONT ST
P_LOCATION
01
QC Status
Approved
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EHD - Public
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' 24 October 2005 <br /> . AGE-NC Project No 95-0167 <br />' Page 7 of 10 <br /> to gravelly sand below This zone is characterized by low pore pressures and may be considered a <br /> flow unit <br />' HU2-HU2 extends from approximately 33 feet to 43 feet bsg This zone consists primarily of clay, <br /> clayey silt, and silty clay This zone is characterized by generally low pore pressure, except for a <br /> high-pressure peak at the bottom of the unit associated with very fine sands or less permeable clayey <br /> material <br /> HU3 - Extending from 43 feet to approximately 55 feet bsg, HU3 is composed primarily of layers <br />' of sandy material (sand and fine- to coarse-grained sand) This zone exhibits uniformly low pore <br /> pressures and may be considered a flow unit <br />' HU4 - Extending from 55 feet to approximately 70 feet bsg, HU4 is composed primarily of thin, <br /> alternating layers of silty material (silt, and silt with clay) <br /> HU5 - Extending from 70 feet to approximately 80 feet bsg, HU5 is composed primarily of layers <br /> of sandy material (silty sand, sand, and fine-to coarse-grained sand) This zone exhibits uniformly <br /> low pore pressures and may be considered a flow unit <br /> 3 3 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> On 24 September 2004, depths to ground water ranged from 16 13 feet to 16 94 feet below the tops <br /> ' of the well casings Groundwater elevations at the site averaged approximately 5 15 feet below mean <br /> sea level (MSL) Ground water was within the screened interval of each well, thus producing an <br /> accurate sampling of the first encountered ground water <br /> ' The ground water flow direction was determined by plotting and contouring the ground water <br /> elevation data The shape of the water table at the time of the September 2004 monitoring event was <br /> ' in the form of a mound centered over monitoring well MW-2,with a trough immediately to the west <br /> Ground water at the site was determined to be flowing radially outward from the mound under an <br /> average hydraulic gradient of approximately 0 012 foot/foot(ft/ft) Figure 5 illustrates the contoured <br /> ' ground water elevations as measured on 24 September 2004 <br /> 3 4 ANALYTICAL RESULTS OF SOIL SAMPLES _ <br /> A total of seven soil samples were collected from pilot borings MW-7 and MW-8 and analyzed for <br /> ' the constituents listed in section 2 1 1 , no petroleum hydrocarbon constituents were detected at or <br /> • above laboratory reporting limits in the soil samples analyzed <br /> Advanced GeoEnvironmentsl,Inc <br />
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