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Last modified
1/26/2010 2:53:49 PM
Creation date
10/12/2006 3:39:06 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.10.D
Description
Glen Canyon Dam/Lake Powell
State
AZ
Basin
Colorado Mainstem
Date
5/24/2000
Author
Hazel et al.
Title
Sand Deposition in the Colorado River Ecosystem from Flooding of the Paria River and the Effects of the Nov 1997 Glen Canyon Dam Test Flow
Water Supply Pro - Doc Type
Report/Study
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<br />I <br />., <br />f <br />'. <br /> <br />NAU Sand Bar Studies <br /> <br />Final Report <br /> <br />., <br />~ <br />" <br /> <br />1997 ranked among the top 20% during the 75 years of gage record on the Paria River (Topping et ai" <br />2000b), This new sediment was the first significant input from the Paria River since the winter of <br />1995, and the largest since 1980, It is important to note that Paria River floods generally do not have a <br />significant effect on mainstem river stage because the water volumes are small relative to those in the <br />main stem and the duration of peak discharge is short, on the order of hours, <br /> <br />THE 1997 TEST FLOW <br /> <br />The 1997 Test Flow was the first attempt by the adaptive management program to implement a <br />flow release strategy for sediment redistribution following a tributary flood, The hydrograph of the test <br />flow, beginning on November 3, consisted of a rapid increase in discharge from 479 m3/s (16,909 fe/s) <br />to a steady flow of 878 m3/s (31,000 fels) for 48 hours, followed by a slow decrease to 480 m3/s on <br />November 6 (Fig, 2b), The maximum rate of up ramp was 68 m3/s (2,400 fe/s) per hour and the <br />maximum downramp rate was 39 m3/s (1,377 fe/s) per hour. Similar to the hydrograph for the 1996 <br />Controlled Flood, the slower rate of downramp was designed to reduce erosion caused by dewatering <br />- <br />of bank stored water in sand bars and to avoid stranding of trout in the tailwaters fishery upstream <br />from Lees Ferry, The release was approximately 93% of maximum power plant capacity, <br /> <br />e. <br />.,: <br /> <br />!~ <br />, <br />:;. <br /> <br />'" <br />, <br />~ <br />< <br />~ <br />. <br />~ <br />.~ <br /> <br />" <br /> <br />1"- <br />r-' <br /> <br />,. <br /> <br />STUDY AREAS AND METHODS <br /> <br />Modeling Tributary Sand Inputs <br /> <br />A flow and sediment transport model for the Paria River was previously developed by Topping <br /> <br /> <br />(1997), The outputs from this model are the wetted reach-averaged cross-section geometry, the <br /> <br /> <br />discharge of water, the sand transport rate (in 10 size classes), and the silt and clay transport rate, The <br /> <br /> <br />model provides excellent agreement with the historical record for discharges, suspended-sediment <br /> <br /> <br />concentrations and hydraulic geometries for previous floods, In the future. model estimates may <br /> <br /> <br />provide cost-effective, real-time predictive capabilities for suspended-sediment yields to the Colorado <br /> <br /> <br />River, <br /> <br />To examine the rate at which sand inputs from the Paria River were transported downstream, we <br /> <br /> <br />compared model predicted sand loads (0,0625-2,0 mm) to measured bed changes below the mouth of <br /> <br /> <br />the Paria River (described below), Model loads were compared to deposit volume changes by <br /> <br /> <br />assuming a porosity of 35% for sand-sized sediment on the bed and 20% uncertainties associated with <br /> <br /> <br />the suspended-sand measurements [see Appendix B in Topping et ai, (2000a)], <br /> <br />., <br />...~ <br /> <br />;.l <br />:~ <br />~ <br />'. <br />.~ <br />',: <br />~ <br />~ <br />r:; <br />~ <br />:..1' <br />t <br /> <br />~.., <br />:\. <br /> <br />II <br />
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