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ADVISORY - ACTIVE SOIL GAS INVESTIGATIONS <br />the soil gas investigation, one or more continuously cored boring(s) should be installed <br />at the first location to the proposed greatest depth of the soil gas investigation. If the soil <br />gas data are to be used for human health risk assessment, geotechnical data may be <br />needed. Geotechnical information needed for vapor intrusion risk assessment purposes <br />can be found in DTSC's Vapor Intrusion Guidance (DTSC, 2011). <br />Lithologic logs should be prepared for all borings, including soil matrix and geotechnical <br />borings. Information gathered from the continuously cored borings may include lithologic <br />descriptions, geotechnical data and contaminant data. Information collected from <br />borings should be used to update the CSM. All boring logs generated during the soil gas <br />survey should be provided to the regulating agency. <br />3.1.2 Sample Spacing <br />Sample locations may be based on historical site use and potential contaminant release <br />points. Initial spacing can be grid-based such as sampling on a 50- by 50-foot grid. <br />Alternatively, initial sampling can be based on historical or suspected site use. When <br />areas of contamination are identified, a more focused grid spacing or biased sampling <br />approach may be employed. Use a close interval grid or radial or step-out sampling <br />pattern such as 10- to 20-foot grid pattern and multi-level sampling at 5-, 10-, 15-feet <br />vertically to delineate identified contaminant areas. If historical information for the area <br />is unknown, a screening grid pattern, such as 100- by 100-foot, may be used. <br />3.1.3 Sample Depth <br />All available information such as boring logs and field instrument readings from soil <br />cuttings or cores should be used to select the correct depths to collect soil gas samples. <br />Probes should be installed at depths with elevated vapor readings. Vertical sampling <br />should continue until vapor-phase contaminants are no longer encountered. If vertical <br />characterization to groundwater is needed, the deepest soil gas sample should be <br />collected near the capillary fringe. Soil gas wells or probes should not be installed too <br />close to the water table because low flow conditions might be encountered due to the <br />high moisture content. Nested soil gas wells may be installed in the annular space of <br />groundwater monitoring wells to serve as a dual-purpose well if both vapor and <br />groundwater monitoring are required. <br />Soil gas sample depths should be chosen to minimize the effects of changes in <br />barometric pressure and temperature, breakthrough of ambient air from the surface, <br />and to ensure that representative samples are collected. Soil gas samples collected at <br />less than 5 feet below ground surface (bgs) may be subject to barometric pressure <br />effects and prone to breakthrough of ambient air through the soil column and, hence, <br />samples are not typically collected from depths of less than five feet unless site-specific <br />conditions dictate otherwise. Consideration should be given to source location, types of <br />chemicals of concern and the lithology encountered. Variation of sample depths and the <br />need for deeper sample locations should be evaluated based on site-specific <br />characteristics and DQ0s. <br />When evaluating vapor intrusion, sampling soil gas immediately adjacent to a building's <br />foundation is only appropriate if the samples are collected near the contaminant source. <br />July 2015 8