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mining operation! A copy ofthe CDPS Industrial General Permit issued to AI with an effective date <br />of October 1, 2002 is enclosed as Attachmem 3. This permit has two outfalls and does not require <br />any water quality monitoring even though numeric standards exist for the Upper South Platte River <br />Subbasin in this area. More important was the fact that the Water Quality Control Division did not <br />review the permit application for antidegradation criteria. <br />The mining site and my property are within the historical ground water contaminant plume <br />emanating from the Rocky Mountain Arsenal (RMA) located 2.5 miles to the southeast. Weapons <br />production and industrial manufacture of pesticides and herbicides contaminated soil, sediments, and <br />water at the RMA. From 1942 through 1969, the Army manufactured weapons including nerve <br />agents at the arsenal. Shell Chemical Company leased part ofthe site from the Army and produced <br />pesticides and herbicides from 1951 until 1982. Offpost ground water contamination was not <br />identified until 1974. EPA added the arsenal to its National Priorities List (Superfund) in 1987. <br />According to the Tri-County Health Department, the majority of offpost contamination is found in <br />the shallow, unconfined aquifer (alluvial aquifer). In their overview ofthe R.Mt~ enclosed as <br />Attachment 4, Tri-County Health Department states, "The main Arsenal-related contaminants in the <br />groundwater aze: volatile organic chemicals, such as Benezene, Chloroform, Toluene, and <br />Trichloroethylene (TCE); pesticides and other related chemicals, such as Aldrin, Atrazine, <br />Chlordane, Dibromochloropropane (DBCP), Dieldrin, Enfrin, and Isodrin; Army nerve agent by- <br />products like Diisopropylmethylphosphonate (DIlvIP); and heavy metals, including Arsenic, <br />Cadmium, Chromium, Lead, and Mercury. Table SA, also included in Attachme~ 4, from the <br />Public Health Assessment dated September 30, 1996 prepared by the Agency for Toxic Substances <br />and Disease Registry lists the maximum historical detection levels and range of detections for a <br />number of these contaminants. <br />For discussion purposes, I will focus on Diisopropyl Methylphosphonate (DIMP) as it was the <br />subject of numerous investigations in this area. D1MP does not occur naturally and is created as a <br />by-product ofthe production ofthe chemical agent Sarin. Concerns regarding the toxicity to this <br />chemical prompted the Water Quality Control Commission to establish a statewide DIMP standard <br />of 8µg2 for both surface water and ground water in Colorado. In 1990, the Colorado Department <br />of Health tested my drinking water well (Arapahoe aquifer) and found 27.9 µg2 D]MP. Additional <br />sampling by Tri-County Health in 1991 produced no detectable levels. 1985 sampling of my alluvial <br />irrigation well by Tri-County Health produced a DIMP concentration of 5.2 µg/L. As a result of <br />these investigations, the residence was provided with bottled water and continues to utilize that <br />source for drinking water. During the Pre-Hearing conference, I leazned that AI has also tested for <br />D1MP in this azea and has reported concentrations above the detection limits. <br />My concern is not the contaminant concentrations in ground water today, rather the release of <br />adsorbed contaminants due to excavation mining operations. DIMP is a member of a class of semi- <br />volatileorganic compounds, though somewhat soluble, that tend to adsorb on soil particles. <br />Documerrtation of this characteristic is enclosed as Attachment 5. Adsorption is the most connmon <br />way in which contaminants are removed from the ground water as it moves through a porous <br />medium (Tchobanoglous, 1987). Adsorption occurs when a dissolved ion or molecule becomes <br />attached to the surface solid particles, sedimentary grains. The amount of a contaminant subject to <br />adsorption in a ground water aquifer is dependent upon that chemical's distribution coefficient. The <br />forces that hold the molecule to the sedimentary grains aze very weak. These adsorbed contaminants <br />are not only within the current aquifer matrix but also the zone of historical water table fluctuation as <br />