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ARCHIVED REPORTS 2nd QUARTER 2011 QUARTERLY REPORT
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2900 - Site Mitigation Program
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PR0518132
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ARCHIVED REPORTS 2nd QUARTER 2011 QUARTERLY REPORT
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Last modified
7/10/2019 2:44:31 PM
Creation date
7/10/2019 11:42:03 AM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2nd QUARTER 2011 QUARTERLY REPORT
RECORD_ID
PR0518132
PE
2960
FACILITY_ID
FA0013716
FACILITY_NAME
H & H MARINA
STREET_NUMBER
15135
STREET_NAME
EIGHT MILE
STREET_TYPE
RD
City
STOCKTON
Zip
95219
APN
06908021
CURRENT_STATUS
01
SITE_LOCATION
15135 EIGHT MILE RD
P_LOCATION
01
QC Status
Approved
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EHD - Public
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Site Background Information: Herman and Helens Marina <br /> Page 4 of 13 <br /> to lean clay near the top of HU3 is classified as HU313. The overall unit is characterized by <br /> fluctuating pore pressures ranging from low in silty clays and clayey silts to high in the silts. <br /> A pore-pressure dissipation test in clayey silt/silt at 43 feet bsg in CPT-4 showed a steep <br /> decrease in pore pressure within 400 seconds (t50 = 1.7 min), corresponding to low <br /> hydraulic conductivities ranging between 5x10"5 to 10-7 cm/sec, which are values that are <br /> typical of silt mixtures and very stiff, fine-grained soil (Robertson and others, 1986). <br /> Hydrostratigraphic Units 4 (HU4), 6 (HU6) and 8 (HU8) extend from approximately 70 to <br /> 83 feet, 93 to 95 feet and below 102 feet bmsg, respectively, and consist mainly of fine-to <br /> medium-grained, poorly-graded sand. Pore pressureswithin these intervals are consistently <br /> low. <br /> Hydrostratigraphic Units 5 (HU5) and 7 (HU7) extend from 80 to 90 feet and 96 to 102 feet <br /> bmsg, are composed mainly of silts. These intervals are characterized by uniformly high <br /> pore pressures; a pore-pressure dissipation test in the silt at 70 feet bsg in CPT-4 showed <br /> a slow decrease in pore pressure over approximately 3,000 seconds (t50 = 8.3 min), <br /> corresponding to very low hydraulic conductivities ranging between 5x10 to 2x10.8 <br /> cm/sec, which are values that are typical of silty clay and clay, and very stiff, fine-grained <br /> soil (Robertson and others, 1986). <br /> SITE ASSESSMENT ACTIVITIES <br /> On 22 August 1995, three hydropunch soil borings (HP-1, HP-2 and HP-3)were advanced <br /> at the site. TPH-g and BTEX were detected in soil and ground water samples collected <br /> from each boring, at maximum concentrations of 300 mg/kg TPH-g, 190 mg/kg TPH-d, 1.2 <br /> kg/mg benzene, 3.1 mg/kg toluene, 5.5 mg/kg ethylbenzene and 22 mg/kg in soil sample <br /> HP-1-11', and 1.0 micrograms/liter (Ng/1) TPH-g, 0.24 pg/I TPH-d, 260 pg/I benzene, 8.4 <br /> pg/I ethylbenzene and 36 pg/I xylenes in water sample HP-1). <br /> On 29 August 1996, five probe borings were advanced at the site. TPH-g, BTEX and <br /> methyl-tertiary butyl ether (MTBE) were detected in the soil and ground water samples <br /> collected from the borings advanced in the northern portion of the site. <br /> On 10 September 1997,fourground water monitoring wells(MW-1, MW-2, MW-3 and MW- <br /> 4)were installed at the site to investigate and monitor the lateral extent of impacted ground <br /> water. TPH-g, BTEX, and MTBE were detected in the soil samples from borings MW-2 and <br /> MW-4. TPH-g, BTEX, MTBE, tertiary amyl methyl ether(TAME) and tertiary butanol (TBA) <br /> were detected in the ground water samples collected from the wells on 18 September 1997. <br /> Ground water elevation data at the site indicated that the ground water was being <br /> controlled by the active island drainage pumping system adjacent to the site. <br /> Advanced GeoEnvironmentnl,Inc. <br />
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