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Mr. Mike Nakagawa - 2 - 17 February 2060- <br /> different <br /> 000different location than the other figures. Similarly, the text describes MW-9 adjacent to boring SB-3, but <br /> Figure 2 shows them 100 feet apart. Please submit a corrected Figure 2. <br /> The groundwater gradient for December 1997 is 0.01 feet/foot as noted in the text, but the gradient is <br /> 0.006 feet/foot as calculated from Figure 5, and was 0.001 feet/foot when calculated in April 1997. The <br /> groundwater contour map does not include the groundwater elevation at MW-6. When it is included, it <br /> appears that there is a groundwater mound offsite to the northwest, and MW-6 is downgradient of the <br /> facility. This finding invalidates the conclusion that the high nitrate concentration of 220 mg/1 found in <br /> MW-6 is upgradient of the formerly active portion of the site and invalidates the assessment that nitrate <br /> should not be included in a feasibility study. IT's argument that nitrate in groundwater at the Cal Farm <br /> site is attributed to an off-site upgradient source cannot be substantiated on this basis. Therefore;the <br /> feasibility study will need to address nitrate concentrations in groundwater. <br /> Second and Third Quarter 1998 Monitoring Report <br /> The figure presenting the June 1998 groundwater contour map identified the groundwater elevation as <br /> ND in MW-6 when the corresponding table identified it as—0.87 feet elevation. The figure also shows <br /> MW-4 elevation as—0.12 feet when the table shows it as +0.12 feet. The field log data agree with the <br /> table data. When the contours are redrawn, the groundwater mound observed in the northwest area of <br /> the facility in previous quarters once again is apparent. A localized groundwater mound appears at <br /> MW-8,which historically has been in the downgradient direction. <br /> The September 1998 groundwater contour incorrectly includes the data from the deep monitoring well <br /> (MW-7) with the data from the shallow monitoring wells. When the contours are redrawn, the <br /> groundwater mound in the northwest area is again apparent. <br /> The text notes that nitrate concentrations have increased considerably in both of these quarters relative to <br /> the previous one. The laboratory reported the nitrate as nitrate, and the tables presented the values as <br /> such. In previous quarters, the nitrate data was presented as nitrogen, which is 4.5 times lower than <br /> when nitrate is presented as nitrate. When the data are converted to nitrate as nitrogen, nitrate increased <br /> in MW-3, 4, 6, 7 and 9 and decreased in MW-2 and 8. The largest increases were approximately 100 <br /> mg/1 in MW-6 and MW-9 in June 1998, when the groundwater elevation was within three to five feet of <br /> the ground surface. This suggests that nitrate is present in the vadose zone at the shallow water table in <br /> these two locations, or that there was significant nitrate infiltration from surface ponding over the winter <br /> months. <br /> 1998 Annual Report and First Quarter 1999 Monitoring Report <br /> The groundwater contour map for September 1998 also incorrectly included MW-7 in the shallow <br /> groundwater contours. When the contours are redrawn, the groundwater mound is present in the <br /> northwest comer. <br /> This groundwater mound near the northwest corner of the facility disappeared in March 1999, and the <br /> gradient was in the southerly direction. A localized mound is present at MW-5, where it had appeared at <br /> the adjacent well in June 1998 (MW-8). In March 1999,nitrate concentrations in MW-6 and MW-9 <br /> decreased relative to June 1998, i.e. when groundwater elevations were similar to those found in June <br /> 1998. <br />