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i <br />1D <br />~~ <br />It is determined by subtracting the measured Dry Fork flow (MD) from the <br />t measured hlinnesota Creek flow (MM) which is then adjusted for Beaver <br />Reservoir (TSB), upstream diversions (D) and return flow (R ), the <br />' resultant number represents the flow without Dry Fork input or any unnatural <br />control. The expected flow in Dry Fork is then added back into the <br />' Minnesota Creek flow by dividing the resultant flow from above by one minus <br />the Ury Fork contribution factor (Dx) for the applicable month. See <br />' Table 2 for contribution factors Dx and Lx. <br />' The expected flow at the Minnesota Creek gage during retreat mining <br />operations under both Dry Fork and Lick Creek will be determined by the <br />following equation: <br />1 <br />Eli = (hiM-Mp-ML+L~SB+D-R)/(1-Dx-Lx) <br />' The logic is the same as for Ury Fork except that measured flow for Lick <br />Creek (14L) is also subtracted from measured Minnesota Creek flow and then <br />'-' expected Lick Creek flow is added using the appropriate contribution factor <br />' (Lx) from Tab]e 2. <br />EXFECTEU FLOW IN DRY FORK AND LICK CREEK <br />The expected flow in Dry Fork (ED) or Lick Creek (EL) at any given time <br />will be determined by multipling the expected flow in Minnesota Creek (EM) <br />by the appropriate monthly contribution factor (Dx or Lx).. The <br />equations are: <br />Expected Dry Fork Flow ED = EM Dx <br />Expected Lick Creek Flow EL = EM Lx <br />• <br />