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The subsurface investigation performed in the immediate vicinity <br /> of the existing on-site UST' s, and the subsequent analytical <br /> testing, did not reveal evidence for leakage from the tanks. <br /> The shallow subsurface assessment of the gravel-surface storage <br /> area did not reveal the presence of the compounds tested for. <br /> The two shallow exploratory borings were advanced in areas <br /> that were observed to have collected water or runoff. <br /> Chemical releases to the soil and groundwater have been <br /> documented at facilities located within 2000 feet of the project <br /> site, but not within the site itself. The extent of these <br /> chemical releases, and direction of chemical movement, have not <br /> been determined or verified by local or state regulatory <br /> agencies. <br /> Numerous sites in the immediate vicinity of the subject property <br /> have or have had problems associated with underground tank leaks; <br /> therefore, it is .apparent that groundwater migration of nearby <br /> chemical releases is the most significant potential pathway for <br /> chemical occurrences on the project site. <br /> The direction of groundwater flow beneath the project site is a <br /> significant factor in evaluating the potential site impacts from <br /> the Kearney-KPF, American Moulding and Millwork, or other <br /> possible contributor properties. The proximity of the reported <br /> contaminant releases with respect to the project site is <br /> sufficient to warrant further investigation effort at the site. <br /> Groundwater monitoring wells could be installed along the north <br /> and eastern property boundaries to assess the current groundwater <br /> conditions and to allow for early detection of possible off-site <br /> migration of contaminants into the project site. An additional <br /> monitoring well could be installed along the southeast portion of <br /> the boundary to monitor the existing underground storage tanks <br /> and to allow for determination of the groundwater flow direction <br /> and gradient in the shallow aquifer. <br /> LIMITATIONS <br /> The findings and conclusions presented in this report are based <br /> on a preliminary field reconnaissance, data obtained from the <br /> literature research, a limited subsurface investigation, and <br /> analytical testing. Collection of groundwater samples for <br /> analytical testing was not performed. <br /> This report has been prepared in accordance with generally <br /> accepted methodologies and standards of practice of the area. <br /> No warranty, expressed or implied, is made as to the findings, <br /> conclusions and recommendations included in the report. <br /> BSI <br /> 8 &/�SSOCIlI('S <br />