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C A M B R i A Mr Jeffrey Wong <br /> . February 15, 2006 <br /> Well Construction The wells were constructed using 4-mch diameter Schedule 40 <br /> PVC casing Wells MW-5 and MW-6 were screened from 60 to <br /> 75 fbg and MW-7 was screened from 90 to 95 fbg using 0 010- <br /> inch machine slotted screen The wells were completed by <br /> placing a filter pack of Monterey #2/12 sand from the bottom of <br /> the well casing to approximately 2 feet above the top of the <br /> screened casing Approximately 2 feet of bentonite were placed <br /> above the filter pack Neat Portland cement was placed in the <br /> annular space between the boring wall and the PVC casing from <br /> the top of the bentonite seal to approximately I fbg A flush- <br /> mounted, traffic-rated well box was installed to protect and <br /> finish each well to grade Cambria presents monitoring well <br /> construction details in Table 1 and on the boring logs <br /> (Attachment D) Department of Water Resources well driller's <br /> completion reports are included as Attachment G <br /> Well Development/Sampling Blaine gauged and sampled wells MW-1 through MW-4 on <br /> December 19, 2005 Blaine developed and purged newly- <br /> installed wells MW-5, MW-6, and MW-7 on December 22, 2005 <br /> and gauged and sampled the new wells on December 29, 2005 <br /> Blaine developed the wells using surge block agitation and pump <br /> evacuation Blaine's groundwater monitoring and well <br /> development report, which includes field sheets, is presented as <br /> Appendix C <br /> Wellhead Survey Virgil Chavez Land Surveying (licensed land surveyor <br /> No 6323) of Vallejo, California surveyed the top of casing <br /> elevations for wells MW-5, MW-6, and MW-7 relative to mean <br /> sea level and surveyed the wells' longitudes and latitudes on <br /> January 25, 2006 The survey report is included as <br /> Attachment H <br /> Groundwater Flow Direction Cambria evaluated water-level measurement data from <br /> December 19, 2005 and prepared a groundwater elevation <br /> contour map (Figure 3) Groundwater flow direction is northerly <br /> with an approximate hydraulic gradient of 0 003 <br /> 6 <br />