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The Channel Characteristics Analysis of Two River Types in Lee's Ferry Area

The Channel Characteristics Analysis of Two River Types in Lee's Ferry Area
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摘要 Discovery showed that some of the rivers in Lee's Ferry area run on bedrocks while some are on the alluvium,based on geomorphology,the different kinds of channel characteristics can influence whether these rivers run on bed rock or alluvium. By analyzing the velocity,discharge,width and depth,hydraulic radius and comparing the different channel characteristics of rivers in other areas with Lee's Ferry,it is observed that the channel discharge,velocity and the hydraulic radius play an important role in controlling the transport-limited river and these factors can be inferred to be correct even for all the river channels in Arizona. Discovery showed that some of the rivers in Lee's Ferry area run on bedrocks while some are on the alluvium,based on geomorphology,the different kinds of channel characteristics can influence whether these rivers run on bed rock or alluvium. By analyzing the velocity,discharge,width and depth,hydraulic radius and comparing the different channel characteristics of rivers in other areas with Lee's Ferry,it is observed that the channel discharge,velocity and the hydraulic radius play an important role in controlling the transport-limited river and these factors can be inferred to be correct even for all the river channels in Arizona.
出处 《Meteorological and Environmental Research》 CAS 2016年第2期52-54,57,共4页 气象与环境研究(英文版)
基金 Supported by the(2012)Sino-American 121 Program,Sino-American Cooperation on Higher Education and Professional Development,CCIEE
关键词 Channel characteristic Lee's Ferry Controlling factor Channel characteristic Lee's Ferry Controlling factor
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参考文献7

  • 1JEFFREY WJ. Rivers, major world~ MI. NY: Macmillan Library Ref- erence, 1994.
  • 2PHOENIX DA. Geology of the Lees Ferry area, Coconino County, Arizona. U.S. [ RI. Geological Survey Bulletin, 1963.. 1137.
  • 3DADE WB, FRIEND PF. Grain-size, sediment-transport regime, and channel slope in alluvial rivers[ J ~. Journal of Geology, 1998, 106(6) = 661 -675.
  • 4COLLINS BD, MONTGOMERY DR, The legacy of Pleistocene glac-iation and the organization of lowland alluvial process domains in the Puget Sound regionIJl. Geomorphology, 2011,126(1 -2): 174 - 185.
  • 5DIETRICH WE, SMITH JD, DUNNE T. Flow and sediment transport in a sand bedded meander~J~. Journal of Geology, 1979, 67(3) : 305 -315.
  • 6DIETRICH WE. Mechanics of flow and sediment transport in river bends. In River Channels= environment and processE RI. Edited by K. Richards, The Institute of British Geographers, Blackwell, Ox- ford, 1987:179-227.
  • 7BRARDINONI F, HASSAN MA. Glacial erosion, evolution of river long profiles, and the organization of process domains in mountain drainage basins of coastal British Columbia[ Jl. Journal of Geo- physical Research, 2006, 111 (F1) :347 -360.

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