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ARCHIVED REPORTS_XR0011498
Environmental Health - Public
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EHD Program Facility Records by Street Name
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STOCKTON
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2900 - Site Mitigation Program
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PR0535812
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ARCHIVED REPORTS_XR0011498
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Last modified
5/18/2020 9:35:04 AM
Creation date
5/18/2020 9:27:29 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011498
RECORD_ID
PR0535812
PE
2959
FACILITY_ID
FA0020626
FACILITY_NAME
COLBERG BOAT WORKS
STREET_NUMBER
401
Direction
N
STREET_NAME
STOCKTON
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
13546010
CURRENT_STATUS
01
SITE_LOCATION
401 N STOCKTON ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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I <br /> Sediments encountered in the Stockton area consist of recent fill mate-nal, which vanes according <br /> to construction activities, older Pleistocene, Holocene and Recent Quaternary sediments which are <br />' approximately 200 feet duck in this area, and deeper continental deposits of Pliocene and <br /> Pleistocene age <br /> Locally, the site is underlain by the Riverbank Formation which consists of a brown to red-gray <br /> locally pebbly sand with minor silt and clay Overlying the Riverbank Formation is a thin layer of <br /> recent alluvial deposits chiefly composed of tan to brown silty sand with local zones of gravel and <br />' clay <br /> .5 Hydrogeology_ <br /> Stockton is located in the San Joaquin Groundwater Basin as defined in Depdrtment of Water <br /> Resources Bulletin 118-80 (January, 1990) The upper 700 to 800 feet of the unconsolidated <br /> sediments in the San Joaquin Basin contains a number of water-beanng zones The distribution of <br /> water-bearing zones is directly related to the subsurface geology in any particular area. For the <br /> most part, groundwater occurs in unconfined conditions, however, due to distribution of clay <br /> lenses in the sediments, groundwater can occur in semi-confined conditions as well <br /> For the most part, groundwater movement is southwesterly toward the valley trough,in the case of <br /> unconfined aquifers Locally, surface drainage and irrigation pumping can affect both groundwater <br /> flow directions and water table elevations <br /> Groundwater at the site varies from 15 to 30 feet below surface (bs) Water was encountered at 18 <br /> feet bs during the overexcavation of the gasoline UST basin on the property <br /> .0 CURRENT INVESTIGATION <br /> ' 3.1 Probe Investigatign <br /> Apex personnel supervised the dulling of eleven probe holes (P-I through P-11) on December 12 <br /> and 13, 1994, at the locations indicated on Figure 2 The probe sampling was conducted by <br /> ' Environmental Control Associates of Aptos, California, to depths of up to 30 feet bs, using 3/4- <br /> inch <br /> 14inch I D galvanized steel probe pipe The probe work was conducted according to the Apex <br /> standard operating procedures (SOP) included as Attachment A <br /> The probe process does not produce any cuttings, so cuttings disposition was not a factor in this <br /> investigation <br /> ' .2 Soil Sampling & Anall5is <br /> Soil samples were collected from the probe holes for field screening, classification and selection <br /> for laboratory analysis of hydrocarbons Two soil samples were collected from probe holes P-6, <br /> P-7 and P-8 and one soil sample was collected from P-1 through P-5 and P-9 through P-11 The <br /> soil samples were submitted under chain-of-custody, to Excelchem Environmental Labs of <br /> Sacramento, Cahfornia, a state-certified analytical laboratory Soil samples from P-1 through P-5, <br /> ' P-9 and P-10 were analyzed for total petroleum hydrocarbons, as gasoline (TPHg), TPH, as diesel <br /> (TPHd), benzene, toluene, ethylbenzene, and total xylenes (BTEX) by modified EPA Method <br /> 8015 and 8020, respectively Soil samples from P-4, P-5, P-9, P-10 were also analyzed for TPH, <br /> Phase II Site Assessment Report <br /> COLOI 001 <br /> January 23, 1995 Page 3 <br />
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