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<br />Recommendations for Streamflows <br /> <br />Most methodologies for determining streamflow requirements of fish <br /> <br />are intended for the preservation or maintenance of sport fisheries <br /> <br />(Stalnaker and Arnette, 1976). However, the streamflow requirements or <br /> <br />55 <br /> <br />. <br /> <br />preferences of other key fish species such as game fish and the threat- <br /> <br />. <br /> <br />5 <br /> <br />1967). Streamflow requirements are least known for endemic fish inhabit- <br /> <br />45 <br />I&J <br />..I <br />i40 <br />II..I&J <br />II..D: <br />~:5!5 <br />;:)0 <br />D:CIl <br />..I :5!Q <br />ct~ <br />~I- <br />~t:j2 <br />II.. <br />I&J <br />520 <br />ct <br /> <br />Y. 0.681 X - 8037 <br />r . 0.86.. <br />,2e 0.74 <br /> <br /> <br />. <br /> <br />ened and endangered endemic fish are not fully known (Orsborn and Allman, <br /> <br />ing the main stem of the Upper Colorado River, In areas where there are <br /> <br />great expanses of bare soil, as in the Intermountain West, the runoff <br /> <br />would be expected to be high and to result in high peak flows (Branson <br /> <br />and Owen, 1970; figure 7). Land use practices such as grazing can greatly <br /> <br />change the natural runoff and accompanying sedtment load, For example, <br /> <br />. <br /> <br />o 'eired _e..lled' <br />. Wot.rohed, 9 thru 17 <br /> <br />a ten-year study near Grand Junction, Colorado, demonstrated that ungrazed <br /> <br />15 <br /> <br />watersheds had 30 percent less runoff and 45 percent less sedtment yield <br /> <br />o <br />o <br /> <br />30 35 40 45 50 55 60 65 70 75 80 85 <br />PERCENT 8ARE SOIL <br /> <br />~ <br />.., <br />.., <br />0<0 <br />.. <br /> <br />< <br /> <br />than grazed watersheds (Lusby, 1970), The extent to which peak flows are <br /> <br />~ <br /><. <br />.. <br />.. <br />.. <br /> <br />necessary for flushing action in the main stem streams to produce or main- <br /> <br />tain backwater areas for the young of endemic species is not known, Peak <br /> <br />~ <br />" <br />.. <br />.. <br />': <br /> <br />flows in the higher mountain streams during floods could cause high mor- <br /> <br />tality to young trout such as reported by Seegrist and Gard (1972) and <br /> <br />Figure 7, Relation Between the Percentage of Bare Soil and <br />Average Annual Runoff for Seventeen Watersheds <br /> <br />, <br />, <br />.. <br />... <br /> <br />Hoopes (1975). In high mountain streams, reduced streamflows could re- <br /> <br />--- <br /> <br />suIt in the formation of more anchor and frazil ice that could be detri- <br /> <br />mental to the bottom organisms and force young fish from their micro- <br /> <br />Source: F, A. Branson and J, E, Owen, "Plant Cover, Runoff and <br />Sediment Yield Relationships on Mancos Shale in Western Colorado," <br />Water Resources Research vol, 6, no. 3, 1970, <br /> <br />habitats, thereby increasing mortality. The microhabitat available in <br /> <br />the stream depends to a large extent on the flow. For example, reduc- <br /> <br />tion in streamflow could increase the area of the slow-shallow or deep- <br /> <br />slow portions of the stream (Hill, 1965; figure 8). Also, a reduction <br /> <br />. <br /> <br />