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WSP07478
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Last modified
1/26/2010 2:27:31 PM
Creation date
10/12/2006 2:25:27 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8272.600.60
Description
Colorado River Basin Salinity Control Program - Basin Member State Info - Utah
Basin
Colorado Mainstem
Water Division
5
Date
3/1/1982
Title
Salt Uptake in Natural Channels Traversing Mancos Shales in the Price River Basin - Utah
Water Supply Pro - Doc Type
Report/Study
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<br />Table 6,2, <br /> <br />N <br />f-- <br />o <br />f-4 <br /> <br />Subbasin <br />Number <br /> <br />1 <br />2 <br />3 <br />4 <br />5 <br />6 <br />7 <br />8 <br />9 <br /> <br />Subbasin characteristics. <br /> <br />Area <br /> <br />(km2) <br /> <br />2.823 <br />6,035 <br />7.122 <br />3.937 <br />4.869 <br />14.711 <br />3.263 <br />8.366 <br />4.455 <br /> <br />Overland <br />Flow <br />Routing <br />Coefficient <br /> <br />(min,) <br /> <br />11. <br />11. <br />11. <br />11. <br />11. <br />11. <br />11. <br />11. <br />11. <br /> <br />Tributary <br />Flow <br />Routing <br />Coefficient <br /> <br />application of tbe second salt loading <br />coefficient, and 2) the value of the second <br />coefficient. However, data were not available <br />for model validation. <br /> <br />(min.) <br /> <br />47. <br />57, <br />57. <br />15. <br />62. <br />)2, <br />21. <br />62. <br />31. <br /> <br />Simulation Results <br /> <br />Estimated salt output <br />from Coal Creek <br /> <br />The model was run utilizing generated <br />precipitation data for a 3-year period. The <br />simulated annual and average salt loads by <br />source are given in Table 6.4. The average <br />estimated salt load from the natural channels <br />and overland flow is 121 x 107 gms per year. <br /> <br />Table 6,3, Channel and salt loading characteristics. <br /> Mean Mean Wetted Perimeter Salt Pickup Rates <br />Stream Length Dens i ? Coefficients Initial K K after lO,OO~ min. <br />Order (gm/m2_minO.5) <br /> (m) km/km A .B (gm/m2~min .5) <br />1 45, 57.10 2.33 0.245 0.233 0.120 <br />2 404. 12,80 2.24 0.29 0,233 0.120 <br />3 3211. 2.86 2.14 0.34 0,233 0,120 <br />4 32110. 0.57 2,10 0.40 0,233 0.120 <br /> <br />400 <br /> <br />300 <br /> <br />c <br />'S <br />..... <br />... <br />E <br /> <br />200 <br /> <br /> <br />/~\ ____ FLOW <br />I ,...- <br />, I <br />I I <br />I I <br />I I <br />I I <br />I \ <br />I I <br />I \ <br />f \ <br />, I <br />" I \ <br />I 1/ \ <br />, I' \ <br />, \ <br />, \ <br />, \ <br />I \ <br />\ <br />\ <br />I \ <br />I \ <br />, <br />I <br />I <br /> <br />5 <br /> <br />2500 <br /> <br />~ <br /> <br />2000 <br /> <br />..... <br />CI <br />E <br /> <br />~ <br /> <br />3= <br />o <br />-l <br />lJ.. <br /> <br />100 <br /> <br />~ <br /> <br />/CONCENTRATION <br /> <br />2 <br />o <br />I- <br />et <br />II:: <br />I- <br />2 <br />W <br />U <br />2 <br />o <br />U <br /> <br />o <br />o <br /> <br />1500 <br /> <br /> <br />1000 <br /> <br />500 <br />30 <br /> <br />10 15 20 <br /> <br />TIM E (hours) <br /> <br />25 <br /> <br />Figure 6.3. Model response to 0.2 rom of surface runoff (lower Coal Creek site). <br /> <br />59 <br /> <br />
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