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<br /> <br />TABLE 33 <br />Sediment Balance of Reduced Peak Flows Without Redistributing <br />---------- <br />Percent ------------- <br />Mean Annual --------------------- <br />Annual Sediment Load ---------------- <br />. Million Tons -------------- <br />Years Balance <br />Remaining <br />---- <br />--- Flow, cfs Deerlodge Park <br />----- Mathers Hole <br />--------------- Set to Zero <br />--------------- <br />-- <br />- <br />90% ------------- <br />1976 ---------------- <br />2.327 2.472 32 <br />80% 1810 2.059 2.141 25 <br />70% 1643 1.800 1.827 10 <br />65% 1560 1.674 1.676 2 <br />64% <br />---------- 1543 <br />------------- 1.649 <br />--------------------- 1.647 <br />--------------- 0 <br />---------------- <br />Again, as the daily flow pattern changes such that the peaks are reduced, the <br />days in which the balance is set to zero declines. Only the high flow years of <br />1983-1985 are able to effectively reduce the balance as peaks are reduced <br />further and further. Total transport at Mathers Hole is again greater than at <br />Deerlodge Park, but as the flow distribution changes and is reduced, the <br />balance is not set to zero as often and the loads at both locations approach <br />being approximately equal. <br />DISCUSSION OF RESULTS <br />The total sediment balance for the Deerlodge Park to Mathers Hole reach shows <br />the same general seasonal trend throughout the years. Sediment tends to <br />accumulate during the baseflow months while the majority of annual load is <br />transported during the peak flow periods and the balance is set to zero. If <br />the timing or magnitude of peak discharges are significantly altered, sand <br />deposited on banks and bars from late summer through winter may not be swept <br />away seasonally (Elliott,1984). The sediment budget program tends to confirm <br />this statement. <br />,-Again, this budget must be viewed in terms of trends. The accuracy of the <br />results are only as accurate as the rating curves developed from measured flow <br />and sediment values, the manner in which the distribution of flow values are <br />changed, and the other assumptions presented earlier. <br />The 'minimum monthly hydrographs' for the three scenarios are compared to the <br />'historic' hydrograph at Deerlodge Park in Figure 6 and listed in Table 34. <br />Tables 35 through 38 show the mean monthly flows for the period of record for <br />the four hydrographs.