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REMOVAL_1995
Environmental Health - Public
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PR0505718
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REMOVAL_1995
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Entry Properties
Last modified
4/1/2020 11:52:50 AM
Creation date
11/2/2018 5:26:28 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2300 - Underground Storage Tank Program
File Section
REMOVAL
FileName_PostFix
1995
RECORD_ID
PR0505718
PE
2381
FACILITY_ID
FA0003299
FACILITY_NAME
Tracy Golf And Country Club
STREET_NUMBER
35200
Direction
S
STREET_NAME
CHRISMAN
STREET_TYPE
Rd
City
Tracy
Zip
95377
APN
25327019
CURRENT_STATUS
02
SITE_LOCATION
35200 S Chrisman Rd
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
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\MIGRATIONS\C\CHRISMAN\35200\PR0505718\REMOVAL 1995.PDF
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EHD - Public
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19 September 1995 <br /> AGE-NC Project No. 95-0183 <br /> Page 2 of 4 <br /> approximately 450 miles. The valley is enclosed by the igneous Sierra Nevada to the east and the <br /> sedimentary and metamorphic Coast Ranges to the west. The surficial and upper several hundred feet <br /> of subsurface layers consists of a great thickness of predominantly unconsolidated alluvial and <br /> floodplain deposits(dominantly sands, silts, and clays) of Quaternary age, which are derived from the <br /> predominantly granitic mountains of the Sierra Nevada. Beneath the upper sedimentary deposits lie <br /> a thick sequence of marine deposits of Mesozoic age. These units are further underlain by a pre- <br /> Jurassic complex of igneous and metamorphic basement rock. <br /> 2.3. GROUND WATER DEPTH <br /> The water-table surface beneath.the site occurs at a depth of approximately 85 feet below site grade <br /> (BSG). The uppermost ground water flows in an unconfined aquifer. With depth, the aquifer <br /> becomes more confined due to the presence of mixed heterogeneous layers of sediments. The <br /> regional direction of ground water flow in the upper aquifer is generally toward the northeast. <br /> 3.0. SCOPE OF WORK <br /> The scope of work for the proposed investigation includes advancing five soil borings to a maximum <br /> depth of 25 feet. Borings will be advanced using a Geoprobe 5400, utilizing direct push technology. <br /> Soil will be continuously cored and selected soil samples will be preserved. Upon completion of the <br /> investigation, a report of the findings will be prepared and will include recommendations for further <br /> investigation, if necessary. Drilling for this investigation is to be performed by Advanced <br /> GeoEnvironmental Inc. Laboratory analyses will be performed by McCampbell Analytical, Inc., a <br /> State-certified laboratory located in Pacheco, California. <br /> 3.1. EQUIPMENT DECONTAMINATION <br /> All sampling tools and brass sleeves used for sample collection will be thoroughly rinsed with clean <br /> water after washing with a solution of Alconox. All probe rods are cleaned prior to advancement in <br /> each borehole. <br /> 3.2. LABORATORY ANALYSIS <br /> Selected soil samples will be analyzed for the following constituents: total petroleum hydrocarbons <br /> quantified as gasoline(TPH-g);benzene, toluene, ethylbenzene, and xylenes (BTEJQ; and total lead. <br /> A minimum of one soil sample will be analyzed from each probing. Laboratory reports of soil <br /> analyses, testing methods, laboratory quality assurance/quality control (QA/QC) reports, and soil <br />
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