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Chevron Pipeline Co.,Dividend Prope,�.y -2- 7 March 1996 <br /> bioremediation is only one of many remedial methods that may be appropriate for a given site. <br /> Passive-bioremediation is not a"do nothing" alternative. Proper site characterization and <br /> monitoring are needed to clearly demonstrate the applicability and progress of this remedial <br /> metho(i. <br /> 6) A mass balance of initially-released material (the mass of hydrocarbons that existed at the <br /> site during initial investigations and at present) would add to'the discharger's assessment of <br /> the success of the passive bioremediation method. How long ago did the leak occur? <br /> 7) Is passive bioremediation the best method for hydrocarbon removal at this site? Why? What <br /> of her methods are available and how would their success be compared with the method <br /> chosen? Summarize what other remedial actions have been taken since the discovery of <br /> contamination at the site (e.g., soil removal, free product skimming, ground water pumping) <br /> and the rationale for not following the active measures proposed in November 1993. <br /> 8) How does the monitoring performed at the site to date demonstrate the success of the chosen <br /> rc medial method in capturing the entire plume? Are some data missing (e.g., down-gradient <br /> o:'MW-13)? <br /> 9) Background levels have not yet been achieved at the site. How long is it expected to take for <br /> tle chosen remedial method to reach beneficial use protective water quality limits? How <br /> long to reach background levels? How do these times compare with existing and potential <br /> future beneficial use patterns in the area affected by the release? <br /> 10) Geomatrix'response to this item indicates that they consider this to be a"low-risk soil case." <br /> I 3o not agree. Since pollutants at this site have been detected and continue to exist in waters <br /> o;`the State at levels that would impair beneficial uses of these waters, the case is not "soil <br /> oily." The site may be "low-risk"; however, documentation of the risk to existing and <br /> probable beneficial uses of waters of the State has not been clearly nor completely <br /> di;monstrated in a manner consistent with that required by this agency for other similar sites <br /> (i.e., leaking underground tanks per the Tri-Regional Recommendations, Appendix B). The <br /> ir:formation requested in our 1 February 1996 letter should clarify the extent of risk to water. <br /> Well Logs and Geologic Cross Section <br /> Several monitoring well logs were not submitted. The logs submitted for monitoring wells MW-8, <br /> -11, -1:!, -13, -14,-15, -16, -17, -18 and-19, prepared in August 1991, are rudimentary and <br /> incomplete. Lithologic information is incomplete. Well screen intervals and other drilling and <br /> well construction details are missing, as is information on initial and static water levels. <br /> The geologic cross section is helpful in demonstrating what is known about the site's lithology <br /> from monitoring well logs. Sandy zones are interbedded with the more prevalent clayey soils. <br /> Information about the interconnectedness of these more permeable zones is apparently <br /> unavailable. By indicating only a single ground water table level, the diagram gives the <br /> impression that water levels have not changed over the period of site investigation. Showing the <br /> range in water levels over the years that the site has been monitored would be more realistic. Also <br /> useful would be indications of the extent of contaminants in soil and water at the site, as shown in <br /> the cross section contained in Geomatrix' 26 October 1995 report. <br />