Laserfiche WebLink
Soil Boring Results and VEG/ISCO Work Plan <br />Field Maintenance Shop #24, Stockton, California October 2016 <br />indicate groundwater typically flows to the north-northeast, exhibiting small, possibly seasonal <br />fluctuations within that range. The groundwater gradient is generally very flat, with an average of <br />approximately 0.0010 feet/foot according to data collected in the second quarter 2016. <br />In April 2013, specific capacity testing data was acquired from two site monitoring wells located <br />inside the source zone area (FMS-MW6 and FMS-MW7) and one site monitoring well outside the <br />source zone area (FMS-MW2). Testing results (OTIE, 2013) showed hydraulic conductivity (Ksat) <br />values are highest in the soils outside the source zone area (between 70.4 and 103 gallons per <br />day per square foot (gpd/ft2) and lowest in the soils inside the source zone area (between 0.4 and <br />11.16 gpd/ft2). The Ksat value range of the source zone area soils is generally consistent with silty <br />clays (Shevnin V. et al., 2006). <br />2.0 SOIL CHARACTERIZATION STUDY <br />A Soil Characterization Study was conducted to provide additional data for optimizing remedial <br />actions at the site including VEG for treatment of petroleum compounds in the soil and ISCO for <br />reducing petroleum contaminants in groundwater. The scope of the Soil Characterization Study <br />included performing three (3) soil borings in the source area in the vicinity of FMS-MW6 to a depth <br />of approximately 40 feet and the collection of 15 soil samples for environmental and geotechnical <br />analysis at multiple depths. <br />ECM installed three (3) borings (SB-4, SB-5, and SB-6) on July 20 and 21, 2016 to the west, north <br />and northwest of monitoring well FMS-MW6, respectively (Figure 5). Borings SB-5 and SB-6 were <br />advanced within the footprint of the UST concrete pad. Samples were collected from the borings <br />ranging from 9 to 39 feet bgs at 5 samples per boring. Sample locations were selected based on <br />different lithology, elevated PID readings, and general distribution in the vadose zone. The <br />deepest sample from each boring was collected 1-2 feet below the water table to analyze soil <br />samples to support ISCO injections. Field documentation and boring logs are provided in <br />Appendix A. <br />Soil samples were submitted to BC Laboratories, Inc. (BC Labs) in Bakersfield, California for <br />Environmental and geotechnical analytical laboratory analyses which included the following: <br />Volatile organic compounds (VOCs) by U.S. Environmental Protection Agency (EPA) <br />method 8260B; <br />Total petroleum hydrocarbons as gasoline (TPH-g) by EPA method 8260B <br />Total petroleum hydrocarbons as diesel TPH-d by EPA method 8015B; <br />Soil moisture content by ASTM method D-2216 <br />Soil grain size and distribution by ASTM method D4464(M); and <br />Total organic carbon (TOC) by EPA method 9060A. <br />Investigation derived waste (IDW) including any soil cuttings and equipment decontamination <br />fluids were containerized in DOT-approved, steel, 55-gallon drums. IDW from the soil borings was <br />transported offsite on August 10, 2016. A waste manifest is provided in Appendix B. <br />2.1. Soil Sample Results <br />A summary of soil sample analytical results is provided in Table 1 and geotechnical data collected <br />from selected samples is provided in Table 2. Laboratory analytical reports are provided in <br />Appendix C. A summary of analytical results is provided below for each soil boring, reporting <br />only the samples within the unsaturated portion of the vadose zone. <br />Page 3 •