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ARCHIVED REPORTS_XR0003161
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0540782
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ARCHIVED REPORTS_XR0003161
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Last modified
2/6/2020 10:52:45 AM
Creation date
2/6/2020 9:58:25 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003161
RECORD_ID
PR0540782
PE
2960
FACILITY_ID
FA0023314
FACILITY_NAME
RMB GARAGE
STREET_NUMBER
715
Direction
N
STREET_NAME
HUNTER
STREET_TYPE
ST
City
STOCKTON
Zip
95202
APN
13905409
CURRENT_STATUS
01
SITE_LOCATION
715 N HUNTER ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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t <br /> Site Background Information <br /> R.M.B. GARAGE (ERARDI VENTURES) <br /> 715 North Hunter Street, Stockton, California <br /> REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is located within the southern San Joaquin Valley which comprisesp art of the Great Valley <br /> geomorphic province of California The San Joaquin Valley is formed by the Great Valley <br /> geosynclme, which is a large, elongate, northwest-trending asymmetrical structural trough(basin) <br /> It is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade Range to the <br /> north, and the Sierra Nevada to the east This trough has been filled with sediments derived from <br /> both marine and continental sources Thickness of the sedimentary fill ranges from thin veneers <br /> along the valley edges to more than 20,000 feet in the south central portion of the valley The <br /> sedimentary formations range in age with the older deposits being primarily marine in origin and the <br /> younger deposits being primarily continental Continental-derived sediments were primarily <br /> deposited in lacustrine,fluvial,and alluvial environments with sediment sources being the mountain <br />' ranges surrounding the valley(Olmsted and Davis, 1961) The site is located on unconsolidated and <br /> semi-consolidated alluvium,lake,playa and terrace deposits of Quaternary age(California Division <br /> of Mines and Geology, 1977) <br /> The Modesto, Riverbank and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> .� Water Basin (Basin 5-22) Based on information obtained during drilling, ground water depth <br /> beneath the site is approximately 25 to 30 feet below surface grade (bsg) Based on information <br /> obtained from a nearby site(706 North El Dorado Street)the prevailing ground water flow direction <br />' in the vicinity of the site is inferred to be toward the northeast However, flow direction maybe both <br /> locally and seasonably variable <br /> SITE ASSESSMENT ACTIVITIES <br /> IOn 04 January 2002, four soil borings were advanced by Advanced GeoEnvironmental, Inc(AGE) <br /> at the site as part of the assessment related to the former USTs Soil probe borings B1 through B4 <br />' were advanced vertically to depths of 40 feet bsg <br /> TPH-g, TPH-d and TPH-mo were detected in the soil samples collected from borings B1 through <br /> B4 at concentrations ranging from 0 38 (milligrams per kilogram) mg/kg to 8,100 mg/kg TPH-g, <br /> 400 mg/kg to 5,500 mg/kg TPH-d and 200 mg/kg to 9,200 mg/kg TPH-mo TRPH was detected in <br /> the soil samples collected from borings B 1 through B4 at concentrations as high as 36,000 mg/kg <br /> (B4-30) One or more BTEX compounds were detected in the samples collected from borings B 1 <br /> through B4,with the exception of the 15-foot soil sample from B3, at concentrations as high as 45 <br /> mg/kg benzene, 630 mg/kg toluene, 150 mg/kg ethylbenzene and 760 mg/kg total xylenes(134-30) <br /> Seven additional volatile organic compounds were detected in the soil samples at concentrations <br /> ranging from 0 010 mg/kg to 440 mg/kg Fuel additives were not detected at or above laboratory <br /> • reporting limits in the soil samples <br /> Advanced GevEnvzronmental,Inc <br />
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