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Z <br />w Z <br />O <br />w Q <br />CO <br />I 1--. <br />Z <br />w w <br />? U <br />Z Z <br />w O <br />d U <br />U) <br />U) <br />w <br />0 <br />(Y <br />Q <br />2 <br />x C) <br />_U) <br />0 <br />} <br />_J <br />Q <br />0 <br />TIME <br />I ? <br />00 <br />w 0- <br />00 <br />Z Z <br />W Q <br />LL w <br />U) Q <br />Z <br />} w <br />J <br />Q ? <br />0 w <br />CO <br />TIME <br />Figure 18.--Procedure used to model suspended-sediment transport-rate graphs. <br />N <br />W <br />1`- <br />lr <br />O <br />11 <br />zQ <br />Q ? <br />X <br />r ? <br />w <br />I- a <br />z <br />w (0 <br />?z <br />?O <br />w <br />cn Z <br />1- <br />0 <br />W <br />o? <br />zQ <br />w? <br />a <br />0 <br />CO <br />,30 <br />Breaks indicate no data <br />for these months <br />20 <br />10 <br />0 <br />1971 1972 1973 1974 1975 1976 <br />WATER YEAR <br />Figure 19. --Monthly mean suspended-sediment transport rate at streamflow-gaging station 09212500, <br />Big Sandy River at Leckie Ranch, near Big Sandy. <br />DISCHARGE