Laserfiche WebLink
5470, and after 57 years the MTBE concentration decreases to below 5 micrograms per liter <br /> (ugR-) <br /> Summary: The model results demonstrate that the highest MTBE concentrations are observed <br /> after first year This observation corresponds reasonably well with the actual groundwater <br /> analytical data collected from well MW-1 Historical groundwater analytical data indicate that <br /> this well,which was sampled for the fust time during April 1998 containedug/L MTBE, and n 9 t; <br /> maximum concentrations were detected in October 1998 (1,800 ug/L) and October 1999 (1,640 <br /> ug/L) This tuneframe is approximately 2 to 3 years following soil sample collection Since <br /> October 1999, MTBE concentrations in well MW-1 have decreased to non-detect Ievels, winch <br /> suggests that the MTBE mass in soils near this well are no Ionger present <br /> The modelled MTBE concentrations do not agree well with actual MTBE concentrations <br /> detected in well MW-1 because the initial conditions used in the model overestimate the actual <br /> MTBE mass between the depths of 9 and 14 fbg This is also why the modeled MTBE <br /> concentrations require a longer period of time to leach from the soil profile and attenuate in <br /> groundwater A <br /> i <br /> The decline in groundwater elevations over the last several years can not be accounted for in the <br /> model However, based on MTBE's high solubility and low adsorption to soil, and the model <br /> prediction that most of the MTBE would reach groundwater in 1 year, it is unlikely that the <br /> decrease in groundwater elevation would allow for MTBE mass accumulation in soils located <br /> between depths of 15 and 25 fbg (past and present depths to groundwater, respectively) <br /> Consequently, it is our technical opinion that the majority of the MTBE mass previously <br /> identified in soils near well MW-1, appear to have leached to groundwater as demonstrated by <br /> the VLEACH model and supported by the groundwater analytical data <br /> i <br /> 0323 4 <br />