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Author : Owen R. Williams,Robert B. Thomas,Richard L. Daddow
Publisher : Unknown
Page : 96 pages
File Size : 50,5 Mb
Release : 1988
Category : Sediment transport
ISBN : MINN:31951D02067164A
Author : Harold P. Guy
Publisher : Unknown
Page : 72 pages
File Size : 53,9 Mb
Release : 1970
Category : Sediment transport
ISBN : IND:30000138303858
Author : Anonim
Publisher : Unknown
Page : 72 pages
File Size : 53,5 Mb
Release : 1966
Category : Hydraulic machinery
ISBN : UIUC:30112110760516
Author : Anonim
Publisher : Unknown
Page : 156 pages
File Size : 46,9 Mb
Release : 1963
Category : Sediment transport
ISBN : MINN:31951D03885869E
Author : U.s. inter-agency committee on water resources. sub-committee on sedimentation
Publisher : Unknown
Page : 0 pages
File Size : 44,9 Mb
Release : 1963
Category : Electronic
ISBN : OCLC:1417538526
Author : Marvin J. Fishman,Linda C. Friedman
Publisher : Unknown
Page : 564 pages
File Size : 50,7 Mb
Release : 1989
Category : River sediments
ISBN : UCR:31210008267658
Author : International Atomic Energy Agency
Publisher : Unknown
Page : 74 pages
File Size : 43,7 Mb
Release : 2005
Category : Science
ISBN : UOM:39015062419158
Provides guidance on selected techniques for the measurement of particles moving in the fluvial environment. The potential user is directed in the selection of an appropriate technique through the presentation of operating principles, application guidelines and estimated costs.
Author : Harold P. Guy
Publisher : Unknown
Page : 59 pages
File Size : 40,8 Mb
Release : 1970
Category : Sediment transport
ISBN : OCLC:56294546
Author : IAEA.
Publisher : Unknown
Page : 69 pages
File Size : 52,7 Mb
Release : 2005
Category : Electronic
ISBN : OCLC:1027190844
Sediment transport data are often used for the evaluation of land surface erosion, reservoir sedimentation, ecological habitat quality and coastal sediment budgets. Sediment transport by rivers is usually considered to occur in two major ways: (1) in the flow as a suspended load and (2) along the bed as a bed load. This publication provides guidance on selected techniques for the measurement of particles moving in both modes in the fluvial environment. The relative importance of the transport mode is variable and depends on the hydraulic and sedimentary conditions. The potential user is direct.
Author : J. D. Gordon,Carla A. Newland,Shane T. Gagliardi
Publisher : Unknown
Page : 152 pages
File Size : 50,8 Mb
Release : 2000
Category : Sediments (Geology)
ISBN : UOM:39015049374427
Author : Anonim
Publisher : Unknown
Page : 96 pages
File Size : 52,8 Mb
Release : 2003
Category : Hydrology
ISBN : MINN:31951D025365008
Author : Anonim
Publisher : Unknown
Page : 108 pages
File Size : 52,8 Mb
Release : 1941
Category : Sedimentation and deposition
ISBN : UCSD:31822009711516
Author : Anonim
Publisher : Unknown
Page : 32 pages
File Size : 42,5 Mb
Release : 2004
Category : Forests and forestry
ISBN : MINN:31951D03001268K
This report and associated web site files provide sediment transport and related data for coarse-bed streams and rivers to potential users. Information on bedload and suspended sediment transport, streamflow, channel geometry, channel bed material, floodplain material, and large particle transport is provided for 33 study reaches in Idaho that represent a wide range of drainage areas, average annual streamflows, channel gradients, and substrate sizes. All the study reaches have a coarser layer of surface bed material overlaying finer subsurface material. Both bedload and suspended sediment transport increase with discharge and the relationship can be reasonably represented using a log-log model. At most sites, the suspended load makes up the majority of the total sediment load. The size of the largest bedload particle in transport and usually the median size of the bedload increase with discharge. However, the median size of the bedload is much smaller than the channel surface material and sand is the primary or a large component of the bedload material. A large proportion of the annual sediment production occurs at the higher streamflows during snowmelt. On average, discharges equal to or larger than bankfull occur 3.3 percent of the time and transport 61.5 percent of the annual bedload sediment. Discharges less than the average annual discharge, on average, occur 75.0 percent of the time and transport about 3.8 percent of the annual bedload sediment.
Author : Anonim
Publisher : Unknown
Page : 92 pages
File Size : 54,6 Mb
Release : 1987
Category : Marine sediments
ISBN : UCR:31210026469831
Author : Broderick E. Davis
Publisher : Unknown
Page : 28 pages
File Size : 42,9 Mb
Release : 2005
Category : Sediment transport
ISBN : UCR:31210025015882