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ARCHIVED REPORTS_XR0005353
Environmental Health - Public
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ARCHIVED REPORTS_XR0005353
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Last modified
3/16/2020 7:20:03 PM
Creation date
3/16/2020 5:01:10 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0005353
RECORD_ID
PR0545550
PE
3528
FACILITY_ID
FA0003973
FACILITY_NAME
SHOCKEY & SONS TRUCKING
STREET_NUMBER
850
STREET_NAME
MILGEO
STREET_TYPE
RD
City
RIPON
Zip
95366
CURRENT_STATUS
02
SITE_LOCATION
850 MILGEO RD
P_LOCATION
05
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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19 February 1997 <br /> AGE-NC Project No. 95-0185 <br />' Page 2 of 4 <br /> placed in a chilled container and transported under chain-of-custody to McCampbell Analytical Inc. <br />' (MAI) in Pacheco, California. Each sample was analyzed for total petroleum hydrocarbons <br /> quantified as gasoline and diesel (TPH-g and TPH-d), and for volatile aromatic compounds <br /> (benzene, toluene, ethylbenzene and total xylene: BTE&X) in accordance with EPA methods <br /> 5030/8015m and 602, respectively. <br /> i' 3.0. FINDINGS <br />' 3.1. GROUNDWATER GRADIENT AND FLOW DIRECTION <br /> The relative elevation of ground water in each well was calculated by subtracting the ground water <br /> depth from the surveyed casing elevation (Table 1). Monitoring well casing elevations were <br /> surveyed relative to a MW-4, which was assigned an arbitrary elevation of 60 feet above sea level. <br /> Depth to ground water at the site ranged from 21.14 to 21.82 feet below surface grade (bsg). <br /> Ground water at the site has a very low gradient. At such a low gradient, normal measurement error <br /> M can equal or even surpass the differences between wells, and can greatly influence the inferred <br /> ground water flow direction determination. The ground water flow direction is generally toward the <br /> east, at a hydraulic gradient of 0.0002 ft/ft. The relative ground water elevations at the site are <br />' contoured on Figure 3 - Relative Ground Water- Elevation. Traces of free product were noted <br /> following purging of MW-1, which may effect the ground water elevation very slightly near the <br /> former USTs location. <br />' The regional ground water flow direction is generally southwest and the maPPed flow direction on <br /> the site is a variation from the regional trend. This variation may be due in part to seasonal changes <br /> in the local ground water flow patterns and to the very low gradient. <br /> ' 3.2. LABORATORYRESULTS OF GROUND WATER SAMPLES <br /> TPH-d was detected in ground water samples collected on 05 December 1996, from monitoring <br /> ' wells MW-1, MW-3 and MW-4 at concentrations of 26,000 parts per billion (ppb, reported as <br /> micrograms per liter: ,ug/l: ppb), 180 ppb and 44,000 ppb, respectively. TPH-g was detected in <br />' ground water samples from MWA and MW-4 at concentrations of 400 ppb ,and 300 ppb, <br /> respectively: BTE&X compounds were detected in sainples collected from MW-1' and MW-4 at <br /> concentrations as high as 20 ppb (xylenes, MW- 1). Benzene was detected in the water sample from <br /> MW-4, near the former UST area, at 3.8 ppb. Traces of free product were noted during purging of <br /> MW-1. The laboratory report noted an immiscible sheen in the samples collected from MWA and <br /> MW-4. Analytical results of monitoring well ground water samples are summarized in Table 2 - <br />
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