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Last modified
7/14/2009 5:02:33 PM
Creation date
5/22/2009 7:40:02 PM
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UCREFRP
UCREFRP Catalog Number
8170
Author
Trammell, M. A., K. D. Christopherson, C. L. Rakowski, J. C. Schmidt, K. S. Day, C. Crosby and T. E. Chart.
Title
Flaming Gorge Studies
USFW Year
1999.
USFW - Doc Type
Assessment of Colorado Pikeminnow Nursery Habitat in the Green River.
Copyright Material
NO
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<br />were also applied to the int reted video. General habitat es defined for the <br />~P tYP <br />biological surveys were classified into nine types. Six types were encountered during <br />this study; Scour Channel, Migrating Sandwaves, Horseshoe Vortex, Flooded Tributary <br />mouths, Shoreline Eddy, and Shoreline. <br />Not all general types were needed for the study bar, and two categories were further '~ <br />divided and defined. Scour Channel was divided into either upstream or downstream <br />facing habitats, and Migratory Sandwave into four types which all share the <br />characteristics of being shallow and transient. Isolated pools were included as a <br />separate category. Flooded Tributary and Shoreline Eddy and Shoreline were lumped <br />into "other" or not used. Specific types are described in Table 5, Chapterl. <br />3) Describe the relationship between geomorphological processes of sediment transport and <br />nursery habitat formation and maintenance in the Green River. <br />- Flood magnitudes are divided into three categories: less than bar top, less than bankfull, <br />and greater than baukfull. Antecedent bar top elevation can be high or low. The <br />combined effects on nursery habitat availability of the antecedent condition of bar top <br />elevation and flood magnitude are described in a 2 by 3 matrix (Table 11 in Chapter 1). <br />The relatively infrequent high peaks increase bar elevation. The thalweg scours on the <br />ascending limb of the hydrograph and quickly rebuilds to near previous levels as flows <br />peak and recede. The maximum height of the bar tops build to just under the surface <br />level of the water at peak flow. <br />- The more frequent low peaks and subsequent flows erode and sculpt sand bars. Small <br />migrating dunes and bars can be superimposed on stable bar edges, increasing <br />complexity. <br />- Secondary channels behind large compound bars provide the majority of total and <br />quality habitat. They are generally stable in location from year to year. These channels <br />scour during high peaks, and fill during lower peaks. The area of available habitat in <br />each such channel is a function of bar top elevation (to block throughflow), minimum <br />elevation at the downstream channel mouth, and flow stage, all of which are dependent <br />on antecedent conditions. <br />4) Describe the relationship between nursery habitat types available to and selected by <br />Colorado pikeminnow. <br />- Colorado pikeminnow selected for secondary (scour) channel habitats over all other <br />types of habitat in numbers and area. These were the only type of habitat in which the <br />observed use by pikeminnow was consistently greater than the expected use, although <br />all types of habitats were used to some extent. <br />xv <br /> <br />
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