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WORK PLANS_FILE 1
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WORK PLANS_FILE 1
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Last modified
3/9/2020 11:24:52 AM
Creation date
3/9/2020 9:59:26 AM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
FileName_PostFix
FILE 1
RECORD_ID
PR0545428
PE
3528
FACILITY_ID
FA0005487
FACILITY_NAME
MARCIS DIESEL SERVICE
STREET_NUMBER
2969
STREET_NAME
LOOMIS
STREET_TYPE
RD
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
2969 LOOMIS RD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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Geological recknlcsInc. Page 3 <br /> Soil Vapor Extraction <br /> Pilot Test Work Plan <br /> Project No. 770.2 <br /> September 17,2003 <br /> 2.2 Hydrogeology <br /> L.i Table 1 includes Summary of Groundwater Elevation and Gradients- Water Table Wells, <br /> Table 2 includes Summary of Groundwater Elevation and Gradients- Deep Wells and Table <br /> 6 contains the well construction details. , <br /> The water table well groundwater elevation on June 18, 2003 averaged —38.4'5"feet mean 1- <br /> sea level (MS�) or—63 feet below grade surface (bgs). The elevation of the water table has <br /> varied from 5 65 feet bgs during the course of the investigation. <br /> CThe historical groundwater gradients are illustrated in Figures 7 & 8: Groundwater Gradient <br /> Rose Diagrams for Water Table and.Deep Wells, respectively. The site's shallow aquifer <br /> displays highly variable shifts in groundwater direction. It is noted that groundwater <br /> direction has been predominantly to'the southeast since additional wells Were installed in <br /> May 2002. The deeper aquifer flow had been consistently to the east but on April 28 and <br /> May 23, 2003 the gradient reversed,180°from an easterly direction to a westerly direction. <br /> L The direction reversed again to the east for the June 2003 sounding event. A well receptor <br /> survey was completed in January 2001 and numerous agricultural, residential and <br /> conunercial wells were identified near the site. The variability in groundwater gradients and <br /> direction may be due to pumping influences from these wells. <br /> Vertical gradients are calculated for the MW-5/105 & MW-6/106 well pairs. Table 3 shows <br /> the calculated vertical gradients for the wells with both positive and negative vertical <br /> gradients recorded. Similar to the historical lateral directions, the direction of groundwater <br /> in the vertical plane also fluctuates at the site. The magnitude of vertical groundwater flow <br /> direction ranged from—0.02 to 0.0097 for the site investigation. As stated above, the site is <br /> probably under the influence of groundwater wells operating in the area that account for the <br /> variable vertical gradients. <br /> I <br /> 2.3 Contaminant Distribution `4 <br /> 1 <br /> Tables 4 & 5 in Appendix A contain the site soil and groundwater data, respectively. <br /> Figures 4 and 6 illustrate the soil and groundwater contaminant distribution as j <br /> superimposed on the two cross-sections A - A' and B — 13% respectively. The groundwater <br /> Aie54 data from the June 18, 2003, monitoring event are presented in the diagrams adjacent to the <br /> respective well's screened interval. . <br /> In Figure 4, a column of soil contamination is present under the former UST <br /> L excavation/dispenser area. In the vicinity of MW-6/MW-106, no soil contamination was <br /> I <br /> detected and Win. Hunter & Associates stated no contamination was present in MW-3. This <br /> r suggests that the contamination migrated downward to impact the groundwater without less j <br /> L i <br />
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