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r <br /> C) <br /> FORMER AMERICAN FOREST PRODUCTS 5.0 Modeling to estimate Impact of Soil <br /> Closure Summary Report Contamination� on Groundwater{ URS Project 17322736 July 2009 <br /> Page 5-1 <br /> 5.0 MODELING TO ESTIMATE IMPACT OF SOrL CONTAMINATION ON GROUNDWATER <br /> Model simulations using VLEACH software(CH2M Hill, 1990)were used to estimate the impact of <br /> remaining soil contamination on groundwater quality "—"a-�-� p' the <br /> 1� 9 y(Dames&Moore, 1994);impact,estxmated_by <br /> ma_deiing was�negligible.VLEACH modeling was based on nn phthalene the most mobile constituent of <br /> TPHd, and conservatively neglected the effects of biodegradation. A period of 25 years using three <br /> groundwater level scenarios was modeled.Depths to groundwater of 35 feet bgs and 70 feet bgs were <br /> considered the extreme ranges, and an average depth of 54 feet bgs was considered the most likely long- j <br /> F0termaverage water level depth. The model predicted that after 25 years of water levels at an average <br /> --- depth of 35 feet bgs,the naphthalene concentration in groundwater would reach 36.5 micrograms per liter <br /> (gg/L), while at the more likely average water-level elevation of 54 feet bgs, a naphthalene concentration <br /> of 2.98 gg/L would be reached after 25 years. This concentration is below the proposed water quality goal j <br /> for the site of 20 gg/L, which is the EPA Suggested No Adverse Response Level(SNARL) for <br /> naphthalene. Based on that modeling result, soils remaining at the site would not constitute a designated <br /> waste,provided average water levels remained at an average depth of about 54 feet bgs. Water levels <br /> measured during the June 2009 groundwater monitoring event ranged from about 46 to 49 feet bgs. The j <br /> average depth to groundwater in DMW-1 for the period of record from August 1990 through June 2009 is ' <br /> r— 46 feet bgs(Figure 5). <br /> I. <br /> r <br /> b <br /> K ftrocmU273Mmericaa ForMs Closur�S�ary-Report-RevOl.doc y <br /> } <br />