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Stream Channel Parameters <br />• Exhibit 55A and Changes Due to Mining-Induced Subsidence Page 10 <br />CHANGES IN SEDIMENT YIELD <br />The mean annual sediment yield for each of the 12 basins will not change except for minor <br />chammel cutting and channel filling extending over a 3- to 5-year period resulting from the <br />geomorphological tendency for the existing channels to either be cut or filled. Overall, there will <br />be a tendency for these changes in sediment production to balance out within the basins. <br />Referring to Table 2, it is noted that the mean annual sediment yield for the subject basins ranges <br />from approximately 6 to 220 cubic yazds per year. These sediment yields are not expected to <br />change (i.e., increase or decrease) by more than about 5 percent due to any change in hydraulic <br />chazacteristics resulting from the increase in slope as identified in Table 4. <br />SUMMARY <br />Stream channel chazacteristics will change as a result of subsidence. This analysis of stream <br />• channels was undertaken to determine the magnitude of change resulting from the change in <br />chammel slope. The changes to stream channel parameters were analyzed using standard <br />procedures of the sedimentation and geomorphic engineering professions based on the effects of <br />thalweg slope changes (either increase or decrease) due to mining-induced subsidence. The <br />results aze summarized in Table 5. <br />• <br />The maximum estimated change in channel width is seven feet, and the maximum change in <br />channel depth is 0.4 feet. Changes in new regime width and depths occur in a slow process that <br />may take from three to five years or more. The likely change in sediment yield is not expected to <br />be more than 5 percent from the values given in Table 2. <br />The mining-induced subsidence impacts on existing stream channel pazameters and basin <br />sediment yield aze not significant. Any changes in channel characteristics will occur gradually <br />and reach the new regime over a period of several years. Maximum channel geometry changes <br />will most likely be localized rather than reach wide. Monitoring of any channel morphology and <br />geometry changes will allow for site-specific prescriptive mitigation as deemed necessary. <br />831-032.620 Wright Water Engineers, Inc. <br />