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---------------- <br /> 10 <br /> Evaluation of Natural Attenuation: 7SOO West Eleventh Street, Tracy, C.4. Page 14 <br /> not close to the bottom of the well) and approximately 2-3 gallons of water were pumped <br /> through the system before a water sample was carefully introduced into the glass testing <br /> container. Great care was taken when introducing the water to prevent entrainment of air <br /> into the sample. <br /> After sampling a well, the line filter was discarded, the peristaltic pump lines were <br /> thoroughly decontaminated and a new filter was installed before proceeding to test water <br /> for ferrous oxide in the next well. <br /> When the 1,10 phenanthroline reagent was added to the samples, the color of the water <br /> became orange only in the cases of the samples from Monitoring Well MW-7 and <br /> MWFP-l. In the sample from all other wells, the sample water remained clear. These <br /> results are documented.in Table 5 and further discussed in Section 7.0. <br /> 4.1.2 Dissolved Oxygen and Redox Potential <br /> Dissolved oxygen and redox potential was measured in the field by use of a YSI Model <br /> 556 Multiprobe System equipped with an in-line flow chamber. <br /> Groundwater was pumped from each well by the peristaltic pump and the system was <br /> i purged of entrained air in the same manner as was the case for the ferrous oxide tests <br /> discussed above. The results of the measurements are presented in Table 5 and discussed <br /> in Section 7.0. <br /> 4.1.3 Temperature, Conductivity and pH <br /> r.:.I <br /> Temperature, conductivity and pH of the groundwater were also measured using the YSI <br /> Model 556 Multiprobe System. The values of these parameters were recorded at the same <br /> time as the measurements of dissolved oxygen and redox potential. The results of the <br /> measurements are presented in Table 5 and discussed in Section 7.0. <br /> .1 4.2 Sampling and Laboratory Analyses for Natural Attenuation Parameters <br /> The peristaltic pump system (without filtration) was also used to recover samples for <br /> laboratory analyses for natural attenuation parameters. The slow discharge rate of the <br /> peristaltic pump permitted the aliquots of groundwater to be introduced into the <br /> glassware without entrainment of air. The glassware was provided by the laboratory and, <br /> where necessary, contained the appropriate pre-dispensed preservatives. <br /> -� After the caps had been placed on the glassware, the sample vials and bottles were then <br /> tightly closed, labeled for identification, entered into chain-of-custody control and packed <br /> j` on chemical ice for transport, on the same day that they were recovered, to Severn Trent <br /> Laboratories' (STL) laboratory in Pleasanton, California for analysis. <br /> E <br /> Each groundwater sample recovered was analyzed at the laboratory for the following <br /> suite of analytes. <br /> f <br /> sic <br />