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Last modified
7/14/2009 5:02:37 PM
Creation date
5/20/2009 3:06:25 PM
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UCREFRP
UCREFRP Catalog Number
9671
Author
Rees, D. E., W. J. Miller and J. A. Ptacek.
Title
Volume 1 Draft Final Report - Ecological and Physical Processes During Spring Peak Flow and Summer Base Flows in the Colorado River.
USFW Year
2003.
USFW - Doc Type
Fort Collins, CO.
Copyright Material
NO
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<br />. The range of flows required to deposit and remove fine sediment from the bed of the <br />channel. <br /> <br />Provided that fine sediment producing events have occurred in the upstream tributaries, <br />fine sediment (mud) is deposited at various locations within the Clifton site where the <br />velocity is less than 2.5 ft/s or shear stress is less than 0.03 lb/ft2. Mud is re-entrained <br />from these locations when the identified velocities of shear stress thresholds are <br />exceeded. The results of the 2-D modeling of the Clifton site indicate that at a flow of <br />800 cfs (equaled or exceeded 92 percent of the time), about 35 percent of the site is <br />relatively mud-free. At flows of 1,100 cfs and 1,400 cfs (equaled or exceeded about 80 <br />percent of the time), about 47 to 54 percent of the site is relatively mud-free. At a flow of <br />2,000 cfs (equaled or exceeded 45 percent of the time), about 67 percent of the site is <br />mud-free. About 85 percent of the site is mud-free at a flow of 4,800 cfs (equaled or <br />exceeded 16 percent of the time). <br /> <br />· Whether it is necessary to mobilize the underlying coarse-grained bed material for <br />flushing of accumulated fine sediment. <br /> <br />Flushing of fine sediments from the gravels and cobbles that make up the bed of the river <br />in the riffles and runs at the Clifton site occurs at flows in excess of 4,800 cfs and 13- <br />15,000 cfs, respectively when the critical discharge is exceeded, and this is described by <br />the framework response of the process-response model. However, the results of the 2-D <br />modeling show that the surficial fine sediments can be re-mobilized and flushed byless <br />than the critical flows for the underlying bed material throughout the Clifton site. This is <br />described by the transient response portion of the process-response model. <br /> <br />Biological Investigations <br /> <br />The biological portion of this study was developed to provide specific and detailed information <br />describing the relationship between physical processes (including peak flows) and periphyton <br />and macro invertebrate communities. This approach provided an opportunity to assess the <br />influence of peak flows and other physical processes that may affect periphyton and <br />macro invertebrate communities during summer and fall seasons. <br /> <br />The objective for the biological investigations was to quantify the primary and secondary <br />production, and then determine if the present fish biomass appeared to be limited by the available <br />productivity. Specific objectives and conclusions from the biological portion of this study are as <br />follows: <br /> <br />· Are primary and secondary productivity and standing crop dependant on magnitude of <br />peak flow? <br /> <br />Magnitude of annual peak flow had little or no measurable effect on most of the variation <br />observed in periphytonand macroinvertebrate communities in the l5-MR during this <br />study. <br /> <br />Draft Final Report - 15 Mile Reach Studies <br />Miller Ecological Consultants, Inc. <br /> <br />Page ES-4 <br />October 24, 2003 <br />
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