Laserfiche WebLink
Vadose Zone Soil Gas <br /> Second Semester Results <br /> Vadose zone soil gasses are generally measured at soil gas wells approximately 400 feet from the edge of <br /> refuse,but not from perimeter migration monitoring wells at the property boundary. Soil gasses were <br /> sampled on September 11, 2013. Samples were collected by first measuring the methane content using a <br /> CES-LANDTEC GEMTM 500 portable gas analyzer. The GEMTM 500 was operated until a steady-state gas <br /> composition indicated that the well was purged. After purging, gas samples were collected in stainless steel <br /> Summa canisters and sent to Atmospheric Analysis &Consulting, Inc. for analysis by EPA method TO-15 <br /> (Appendix H). <br /> VOCs were detected in all ten soil gas samples (Table 6). The highest concentration of any VOC was found <br /> in SG-1 which is approximately 100 feet from the edge of refuse. Freon 12 was most often reported with the <br /> highest concentration in a sample. The most VOCs (six)were reported in SG-10. The source of the VOCs <br /> in the vadose zone is likely the old unlined portion of the landfill. <br /> Methane was detected in three interior soil gas well this semester below the regulatory limit. Data from the <br /> perimeter migration monitoring wells indicates that the facility is compliant with Title 27 regulations for off- <br /> site migration. <br /> VOCs have been consistently detected in soil gas since monitoring began in October 2003; however,VOCs <br /> in groundwater is not indicated. The presence of VOCs in the soil at these concentrations is apparently not, <br /> in itself, a significant condition at this landfill. <br /> GROUNDWATER DIRECTION AND FLOW RATE <br /> Groundwater elevations were measured in monitoring wells during the third and fourth quarters. <br /> Groundwater was determined to flow towards the east-southeast(Figures 3 and 4). The calculated average <br /> linear groundwater flow velocity in the third quarter was 79.21 feet per year based on a hydraulic gradient of <br /> 0.00235 foot per foot. The calculated average linear groundwater flow velocity in the fourth quarter was <br /> 76.95 feet per year based on a hydraulic gradient of 0.002285 foot per foot (Appendix F). <br /> STANDARD OBSERVATIONS <br /> Regular site inspections were performed during the second semester of 2013. Monthly standard observations <br /> have been summarized(included in CD that accompanies report). The electronic signatures on the forms <br /> certify that all observations were performed and are accurate. <br /> RUN-OFF/RUN-ON FACILITIES <br /> The Foothill Sanitary Landfill utilizes several methods to control run-on and run-off. The natural <br /> topography of the area controls any run-on into the site. Also,the working area is a significant distance from <br /> the property boundary and at a higher elevation, so run-on from surrounding properties into refuse is not <br /> possible. <br /> To control run-off, a perimeter ditch along the north, west and east ends of the unit directs all storm water <br /> run-off into a sedimentation basin on the east side of the site. The rest of the run-off from the unit gathers <br /> into a sedimentation basin at the southeast corner of Area 1. There were no breeches to any of the run- <br /> on/run-off facilities during this monitoring period. <br /> Foothill Sanitary Landfill 9 Department of Public Works/Solid Waste <br /> 2nd Semester and Annual 2013 Groundwater Monitoring County of San Joaquin—January 31,2014 <br />