Laserfiche WebLink
' C-SHADRIFS.6/WPADD.12 <br /> 05/24/90 <br /> The arsenic source materials are either naturally occurring arsenic- <br /> enriched minerals or arsenic-bearing anthropogenic materials. The <br /> ' secondary minerals most likely are minerals with arsenic substitution or <br /> exchange capacity. <br /> The following statements present evaluations of the possible <br /> restrictions on the nature of the arsenic source material. <br /> ' 1. If the sources are naturally occurring arsenic-enriched <br /> minerals, the distribution might be expected to be more <br /> homogeneous rather than restricted to approximately 15 percent <br /> of the wells and only the A-zone aquifer. <br /> 2. If arsenic-bearing chemicals (anthropogenic materials such as <br /> rodenticides) are the primary source, either they were washed <br /> through the overlying sediments and are currently located <br /> within the aquifer or they are being dissolved and transported <br /> into the aquifer by infiltrating surface water. <br /> In the latter case, a secondary mineral capable of taking up the <br /> ' dissolved arsenic is required to buffer the arsenic at the observed <br /> concentrations. Identification of these solid phases requires <br /> collecting sufficient quantities of soils at the surface, the aquifer, <br /> ' the zones immediately above and below the aquifer to yield an adequate <br /> amount of arsenic-bearing material for identification. <br /> 1 To attempt to acquire these arsenic-rich source materials for positive <br /> identification, the following samples and analyses are required: <br /> 1. Ten samples of soils from drainage ways in the vicinity of <br /> well 407A; <br /> ' 2. Ten samples collected from dry well sediments in the vicinity <br /> of well 407A; <br /> ' 3. Five samples of A-zone aquifer soils in the vicinity of <br /> well 407A; <br /> 12 <br /> 1 <br />