3 edition of Bed-material entrainment potential, Roaring Fork River at Basalt, Colorado found in the catalog.
Bed-material entrainment potential, Roaring Fork River at Basalt, Colorado
Elliott, John G.
by U.S. Dept. of the Interior, U.S. Geological Survey, U.S. Geological Survey, Information Services [distributor] in Denver, Colo
Written in English
|Other titles||Bed material entrainment potential, Roaring Fork River at Basalt, Colorado|
|Statement||by John G. Elliott ; prepared in cooperation with the Town of Basalt, Colorado|
|Series||Water-resources investigations report -- 02-4223|
|Contributions||Geological Survey (U.S.), Basalt (Colo.)|
|The Physical Object|
|Pagination||iv, 33 p. :|
|Number of Pages||33|
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2 Bed-Material Entrainment Potential, Roaring Fork River at Basalt, Colorado situation resulting in sediment deposition and possibly progressive Bed-material entrainment potential and loss of channel conveyance.
Little or no sediment in the d size range is likely to be entrained or transported through much of the study reach by the bar-inundating stream-flow. Bed-Material Entrainment Potential, Roaring Fork River at Basalt, Colorado by John G.
Elliott Available from the U.S. Geological Survey, Branch of Information Services, BoxDenver Federal Center, Denver, COUSGS Water-Resources Investigations Report33 p., 7 figs. Get this from a library.
Bed-material entrainment potential, Roaring Fork River at Basalt, Colorado. [John G Elliott; Geological Survey (U.S.); Basalt (Colo.)].
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Consequently, transport of bed-material particles is a relatively frequent occurrence. Large bed-material transport rates, however, are extremely rare.
Empirical evidence obtained at these and other streams indicates that a stable, self-formed gravel-bed channel cannot be maintained at a dimensionless shear stress greater than about Cited by: Sponsor a Book.
Stream channelization Bed-material entrainment potential, Roaring Fork River at Basalt, Colo Elliott, John G. Read. The National Flood-Frequency Program--methods for estimating flood mag Robert R.
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Sediment-Transport Investigations of the Upper Yellowstone River, Montana, through Data Collection, Analysis, and Simulation of Sediment Transport Article January with 5 Reads. 2) initial work on modeling the potential shear stress on existing river-bounding berms and on the future berms under a scenario of fully repaired berms.
The module was. the Colorado River Basin have affected the sediment transport flow regime within the basin, concepts of fluvial geomorphology followed by a review of the Colorado River Basin, and the effects of dams as well as climate change within the basin are Size: KB.
Based on the measured bed material d 50 of mm and d 84 of mm, the τ c for initiation of motion is estimated to be about N/m² (Van Rijn ; Julien ). Sediment mobility only determines whether a given particle size has the potential to be mobile, and is Author: Rochelle A.
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Free essays, homework help, flashcards, research papers, book reports, term papers, history, science, politics.The equilibrium concept of streams discussed above can also be described by various qualitative relationships.
One of the most widely used relationships is the one proposed by Lane () which states that: QS % QsD50 where Q is the water discharge, S is the slope, Qs is the bed material load, and D50 is the median size of the bed : Samir Haddad.A Bibliography of Aeolian (Eolian) Sand Dunes and Related.