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2.4 Well Construction <br /> Vadose zone observation wells were planned at the site, however the desired drill depths <br /> could not be attained, therefore, no wells were constructed <br /> 2.5 Disposal of Contaminated Materials <br /> Drill cuttings (if any) from the boreholes, are currently stored in 55-gallon drums located at <br /> the site Decontamination liquids were contained in 55-gallon drums, as they were produced, <br /> and stored on-site. Stockpiled cuttings and water are currently being profiled and scheduled <br /> for disposal at appropriate facilities <br /> 3.0 Results <br /> 3.1 Site Geology <br /> During drilling activities conducted in the facility basement, approximately 4.5 feet of <br /> foundation fill material was encountered, which consisted of gravels and assorted debris <br /> (rebar, bricks, etc ) with intermittent concrete layers Native soils were encountered at <br /> approximately 4.5 feet below the basement floor. <br /> A particle size analysis, using the hydrometer method, was conducted on a native soil sample <br /> collected from borehole VW-1. Results indicated the sample was composed of 26% fines and <br /> 74% coarse grained material, which can be described as brown silty sand with gravel using <br /> the Unified Soil Classification System (USCS) <br /> Identification of soil stratigraphy underlying the abandoned tanks was not possible due to <br /> auger refusal, however, review of boring logs for wells located surrounding the site indicates <br /> that the site is underlain by unconsolidated fluvial sediments consisting of layers of lean clay <br /> and sand with varying amounts and sand and fines respectively (Figures 4 and 5). Copies of <br /> the IT Corporation boring logs for wells MW-1, MW-2, and MW-3 are included as Appendix <br /> C of this report. <br /> 3.2 Site Hydrogeology <br /> No groundwater was encountered during this investigation, however, groundwater is known to <br /> exist at the site at a depth of approximately 41 feet below grade Groundwater flow vanes <br /> from east to northeast under a shallow gradient. <br /> MZ/09-06-94/UST/940138 mer 6 <br />