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I ~.o ) I t'- CJ ';:'.J i:;) I I I I I I I I I I I I I I I I I Results of the aquifer testing of the Carroll Well and the Owens Well are thought to be representitive of HSU-2 and the upper several hundred feet of HSU-3. This is expected due to confirmation by geophysical logging of the depths from which water is produced in the 2620-foot deep Carroll Well. Since water from the Owens Well and the Carroll Well flow at the same temperature and at nearly the same specific conductance, it is likely that they produce water from almost the same portions of HSU-2 and HSU-3, Figure 2.5 is a graph of normalized time versus flow-rate data collected during the flow test of the Carroll Well. Based upon the best-fit (linear regression) line through these data, the transmissivity was calculated to be approximately 13,900 gpd/ft for HSU-2 and the upper several hundred feet of HSU-3 (Appendix A). The straight-line approximation time versus head-recovery plot for the one-hour recovery period at the Carroll Well (Figure 2.6) indicates a transmissivity of approximately 4900 gpd/ft (Appendix A). A graph of residual drawdown versus time (Figure 2.7) indicates a transmissivity of approximately 4500 gpd/ft (Appendix A). The values of T for HSU-2 calculated from the Carroll Well test are a factor of approximately 10 to 20 less than expected (Emery et al, 1973). The reason for this may be that the Carroll Well casing slots are partially plugged due to corrosion or encrustation, or possibly that the well had never been developed (cleaned) adequately after it was drilled. 2.3 GEOPHYSICAL LOGGING 2.3.1 Hooper Pool Well Logging An attempt was made to run borehole temperature and fluid-resistivity logs in the Hooper Pool Well on August 25, 1986. The purpose of the logging was to characterize the water quality of HSU-2 and HSU-3 in the Hooper area. At a depth of approximately 165 feet, a casing restriction was noted due to 2-4