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ARCHIVED REPORTS_XR0003664
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0505553
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ARCHIVED REPORTS_XR0003664
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Last modified
7/23/2020 5:09:56 PM
Creation date
7/23/2020 4:04:13 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003664
RECORD_ID
PR0505553
PE
2960
FACILITY_ID
FA0006856
FACILITY_NAME
FRANKS FOOD MART
STREET_NUMBER
2072
Direction
W
STREET_NAME
YOSEMITE
STREET_TYPE
AVE
City
MANTECA
Zip
94336
APN
22202001
CURRENT_STATUS
01
SITE_LOCATION
2072 W YOSEMITE AVE
P_LOCATION
04
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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2 . 0 GROUNDWATER FLOW DIRECTION AND GRADIENT <br /> On December 18, 2000, ASE measured the depth to water in each site <br /> groundwater monitoring well using an electric water level sounder The <br /> surface of the groundwater was also checked for the presence of free- <br /> floating hydrocarbons or sheen using an oil/water interface probe and a <br /> product thickness bailer Monitoring well MW-5 contained 002-feet of <br /> free-floating hydrocarbons The free-floating hydrocarbons are believed <br /> to be gasoline A hydrocarbon sheen was present on the groundwater <br /> surface in monitoring well MW-6 No free-floating hydrocarbons or sheen <br /> were observed in any other site monitoring well Groundwater elevation <br /> data is presented as Table One <br /> Groundwater elevation (potentiometric surface) contours are plotted on <br /> Figures 2, 3 and 4 Groundwater in the shallow zone (less than 20-feet <br /> bgs) has historically shown a northern flow ASE installed a "pump and <br /> treat" interim remediation system in September 2000 to influence the <br /> offsite downgradient flow pattern in the shallow zone Based on t h e <br /> groundwater elevations taken on December 18, 2000, there appears to b e <br /> a "coning effect" occurring in the northern portion of the site Although <br /> . the historic gradient has been to the north, groundwater now appears t o <br /> be flowing toward the recovery wells <br /> Groundwater in the middle zone (55-70-feet bgs) appeared to flow to t h e <br /> south with a gradient of approximately 0 0016-feet/foot, which is <br /> consistent with previous findings The groundwater flow in the deep zone <br /> (greater than 100-feet) appeared to flow to the northeast at a very flat <br /> gradient of approximately 0 0001-feet/foot Potentiometric surface <br /> differences in wells adjacent to each other but screened in different zones <br /> (such as monitoring wells MW-6, MW-7 and MW-8) show a decreasing <br /> hydraulic head with depth, suggesting the potential for downward <br /> groundwater flow <br /> 3 . 0 GROUNDWATER SAMPLE COLLECTION <br /> On December 18 and 19, 2000, ASE collected groundwater samples from <br /> the site wells for analysis Monitoring well MW-5 was not sampled due to <br /> the free-floating hydrocarbons present in that well Prior to sampling, t h e <br /> site monitoring wells were purged of four well casing volumes of <br /> groundwater using pumps and/or dedicated bailers The pH, temperature <br /> and conductivity of the purge water were monitored during evacuation, <br /> . and samples were not collected until these parameters stabilized <br /> Samples were collected from the wells using pre-cleaned dedicated <br /> Frank's One Stop Quarterly Report — December 2000 Sampling <br /> -2- <br />
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