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Gary A. Reents -6- 24 February 1989 <br /> 2. H&A proposes to construct three (3) monitoring wells within the 100-foot sand <br /> layer. The sand layer varies in thickness from 5 feet at borehole 6-x <br /> (Southwest corner of south yard) to 30 feet at borehole 7-x (approximately <br /> 3600 feet downgradient). <br /> H&A proposes to construct two (2) monitoring wells for lateral plume <br /> definition along the transect C-C' (near Horner Avenue) , where the thickness <br /> of the 100-foot sand should be sufficient for screening . This transect <br /> approximates the known longitudinal limit of the chromium plume within the <br /> intermediate zone. Also, a Phase IV well (MW-423), installed in the merged <br /> 100-foot sand and intermediate zone, and located near the center of this <br /> transect, had a chromium concentration of 0.08 mg/l . The locations of these <br /> Stage 1 monitoring wells for lateral definition of the plume, within the <br /> 100-foot sand, are appropriate. <br /> In addition, H&A proposes to construct a monitoring well , within the 100-foot <br /> sand, approximately 1200 feet downgradient of the C-C' transect. The location <br /> of this well also is appropriate. <br /> 3. Within the intermediate zone the two (2 ) wells proposed along East Main <br /> Street, to define the plume' s lateral extent, are sufficient. However, the <br /> four (4) wells proposed for downgradient control are on the opposite side of <br /> Mormon Slough. This spacing (approx. 1400 ft) is consistent with the off-site <br /> spacing previously employed . However, the Mormon Slough and a public water <br /> supply well (CWS52) located at the northern bank of Mormon Slough and Oro <br /> Avnue, could significantly affect water levels and flow patterns. The four <br /> (4) monitoring wells proposed for downgradient definition could determine, <br /> based upon current data ( i .e. , potentiometric map and chromium isoconcen- <br /> tration maps) , the longitudinal limit of the plume. However, the hydraulic <br /> influence of Mormon Slough and/or CWS52 (or CWS62 to the east) could signifi- <br /> cantly alter the existing plume migration trend. Therefore, it would be <br /> prudent to locate potential State 2 monitoring well north of Mormon Slough and <br /> west of CWS 52, along the northern bank of Mormon Slough. <br /> 4. Two (2) deep wells are proposed along East Main Street to determine <br /> the downgradient extent of the chromium migration. The farthest existing <br /> downgradient deep well is MW-461, at the corner of Horner and Sinclair. This <br /> well had a chromium concentration of 0.02 mg/l . Monitoring well MW-420 <br /> located adjacent to the public supply well (CWS20-01), had less than 0.01 mg/1 <br /> of chromium. The proposed locations of the deep wells, for downgradient <br /> definition of the plume, appear appropriate. <br /> In addition, a deep well is proposed near the corner of Gertrude Avenue and <br /> Horner Avenue, to determine the lateral extent of chromium migration, and <br /> two(2) deep wells are proposed at Franklin High School at the corner of Dawes <br /> and Washington, per a request by the Department of Health Services. The <br /> well at the corner of Gertrude and Horner is adjacent to two(2) intermediate <br /> wells that have an average chromium concentration of 0.10 mg/1 . This well <br /> location appears appropriate. <br />