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_. <br />--; <br />each cell. This will tend to attenuate the influence of lower k/m ratios to a large <br />--- -- degree. Table l presents a-summary of the range of values utilized for the two- .-:---_- <br />pazameters in the sensitivity runs. - - <br />VL RESULTS-AND GUNCLUSIONS - - <br />The model simulation results for the north mined azea only and the combined <br />north and south mine azea configurations aze presented on Figures 4 and 5. In the <br />- - figures, the-drawdown contours reflect--the magnitude of the- impacts;. of the------ ..-. - <br />dewatering at steady-state conditions. <br />One significant test of any modeling study is an assessment of the qualitative <br />nature of the results in light of the model set-up, boundary conditions and the <br />nature of the stresses applied. In this case, the patterns of drawdowns appear <br />reasonable for the boundary conditions input. The contours exhibit the steep <br />gradient out from the dewatered areas that would be expected for a fairly <br />transmissive aquifer and also exhibit a configuration that appears correct for a <br />dewatered area adjacent to a meandering stream system. The attenuating effects <br />of the Ski Lake under both mine configurations are also cleazly exhibited in the <br />drawdown contours. <br />The magnitude of the drawdowns and the distance-drawdown patterns are seen to <br />differ only slightly from the north only mine area to the combined north-south <br />configuration. This is the duect result of the location of the stream with respect to <br />13 <br />Martin and Wood Water Consukants, Inc. <br />