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ARCHIVED REPORTS_XR0002382
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545195
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ARCHIVED REPORTS_XR0002382
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Last modified
1/23/2020 3:23:40 PM
Creation date
1/23/2020 2:59:56 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0002382
RECORD_ID
PR0545195
PE
3528
FACILITY_ID
FA0002915
FACILITY_NAME
TRACY MARKET INC
STREET_NUMBER
15
Direction
E
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
21435004
CURRENT_STATUS
02
SITE_LOCATION
15 E GRANT LINE RD
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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Project 113-26-04, 05, Page 7 <br /> November 17,1995 <br /> Undisturbed soil samples were procured at five foot intervals during monitoring <br /> well drilling. Brass sampler liners were cleaned with a TSP solution and rinsed in <br /> tap water prior to insertion into the sampler, a California modified split barrel The <br /> sampler was then inserted through the augers to the boring bottom The sampler <br /> was advanced by successive blows from a 140 pound hammer utilizing about a 30 <br /> inch drop BIow counts per six inch interval were recorded when using the 140# <br /> hammer The sampler was extracted from the boring and the liners removed The <br /> samples were utilized for logging of soil characteristics, and possibly selected for <br /> chemical analysis Only completely full sampler liners representing the lower foot of <br /> the sampled interval were selected for analysis <br /> At the soil boring locations a small slide hammer with a sampling shoe containing a <br /> single brass sample tube was used to obtain undisturbed samples Sample retention <br /> within the sample tube was about 75% at most locations <br /> Selected soil samples were sealed at each end with teflon sheets or aluminum foil <br /> and plastic caps The samples were then labeled and placed into a cooler with ice and <br /> chain of custody documentation and procedures were initiated (Appendix B <br /> Sampling Documentation) At the lab, the selected soil samples were analyzed for <br /> TPH as gasoline and BTEX <br /> It was apparent during drilling and sampling that gasoline contaminated soil was <br /> present beneath much of the investigated area between about 5 5 and 7 feet depth <br /> BGS, which likely represents the capillary fringe of the water bearing zone and/or <br /> the highest seasonal groundwater level The exceptions were all of the down <br /> gradient data points B-14, MW-6, MW-7, and B-20 (B-20 may be cross gradient to off <br /> site plume axis), as well as the cross gradient point B-21 Petroleum odors and soil <br /> discoloration were not noted during drilling and soil and groundwater samples <br /> from these locations did not appear to contain gasoline <br /> Site Geology <br /> Soils encountered during drilling were continuously logged by a geologist using the <br /> Unified Soil Classification System (USCS)(Appendix C Boring & Well Completion <br /> Logs) The monitor well drilling and installation was performed under the <br /> supervision of a State Certified Engineering Geologist The soils encountered during <br /> drilling were found to be similar at the eighteen locations <br /> Each location had asphalt or concrete at the surface From beneath the pavement <br /> down to about 1 foot depth was base rock or sand fill. Beneath that the native soil <br /> consisted primarily of silty clay or clayey silt, (CL) which was olive brown to light <br /> yellowish brown, silty 20-30%, sandy very fine grained <10%, damp, and stiff <br /> Between about 5.5 and 7 feet depth BGS, the soil was silty sand, (SM, ML), colored <br /> light yellowish brown to brown-olive brown Where impacted by gasoline these <br /> soils were green-gray to blue-gray These sands were generally very fine to fine <br /> grained, and contained up to 30-40% silt CIay was minor within these soils First <br /> Parker Environmental Services, 190 East 7th Street, Pittsburg, CA 94565-2317 <br /> Phone (510) 439-1024 Fax (510) 439-2566 <br />
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