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Self organisation in braided systems : DEM analysis of the River Feshie, ScotlandLangham, Joseph Anthony January 2004 (has links)
No description available.
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Controls on channel form and floodplain character along the Bulstrode River, southern Quebec, CanadaSavanhu, G. M. (George Mutangamberi) January 1993 (has links)
The hydraulic dimensions and planform character of a river channel are very much affected by the channel gradient and the calibre of the bed materials. One of the two major objectives of this study is to analyze these effects on selected reaches along the Bulstrode River, near Victoriaville. / The second objective is to relate the variations in gradient, sediment calibre and channel geometry to the changes in floodplain character along the river valley. / The river is about 85 km long and flows across the Appalachian highlands and foothills in southern Quebec. This study focuses on six alluvial reaches along the river, ranging from 0.7 to 1.5 km in length. The channel gradient ranges from 0.0036 to 0.0001. The decline in gradient is associated with rapid downstream fining from small cobble and gravel-bed in the 'upvalley reaches' to a sand-bedded channel in the 'downvalley' reaches. / The discharge remains fairly constant over the river length, averaging about 140 m$ sp3$/sec. Channel depth, particularly the thalweg depth, increases appreciably in the downstream direction. The channel width decreases appreciably in the downstream direction. The channel capacity varies significantly without a clear pattern in the steeper cobble-gravel bed reaches and generally declines in the more hydraulically efficient, gentler and more hydraulically efficient fine gravel-sand bed downstream reaches. / This study finds that floodplain characteristics vary with specific stream power and within-channel processes, but not in the same manner as suggested in the Nanson and Croke (1992) model. (Abstract shortened by UMI.)
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River channel adjustment to hydrologic changeTilleard, John W. Unknown Date (has links) (PDF)
The size of an alluvial river channel can adjust in response to changes in the pattern of flows that it carries. An important case of such channel change occurs downstream of dams or water diversions where flow regulation has been observed to cause morphological and ecological impacts. (For complete abstract open document)
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Channel changes of the San Xavier Reach of the Santa Cruz River, Tucson, Arizona 1971-1988Guber, Albert L. January 1988 (has links) (PDF)
Thesis (M.A. - Geography and Regional Development)--University of Arizona, 1988. / Includes bibliographical references (leaves 116-119).
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Channel change in the Rillito Creek system, southeastern Arizona : implications for floodplain management /Pearthree, Marie Slezak. January 1982 (has links) (PDF)
Thesis (M.S. - Geosciences) - University of Arizona. / Includes bibliographical references (leaves 125-130).
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The influence of fine sediment introduced to an armored bed downstream from a damPritchard, Mary Katharin. January 1900 (has links)
Thesis (M.S.)--Texas State University-San Marcos, 2007. / Vita. Appendix: leaves 65-67. Includes bibliographical references (leaves 68-75).
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Soil quality and stream channel characteristics of montane and subalpine riparian meadows, Sierra Nevada, CaliforniaJungst, Laura J. January 2008 (has links)
Thesis (M.S.)--University of Wyoming, 2008. / Title from PDF title page (viewed on Mar. 22, 2010). Includes bibliographical references.
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Historical change in channel form and riparian vegetation of the McKenzie River, Oregon /Minear, Paula J. January 1994 (has links)
Thesis (M.S.)--Oregon State University, 1995. / Typescript (photocopy). Includes bibliographical references (leaves 24-102). Also available on the World Wide Web.
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Investigating the riffle-pool/meander link : a comparative analysis of horizontal and vertical undulations in stream channel morphology /Lofthouse, Caroline J. January 2007 (has links)
Thesis (M.Sc.)--York University, 2007. Graduate Programme in Geography. / Typescript. Includes bibliographical references (leaves 80-82). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:MR29578
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Characterizing ancient avulsion stratigraphy and its significanceJones, Heather L. January 2007 (has links)
Thesis (Ph. D.)--University of Wyoming, 2007. / Title from PDF title page (viewed on Dec. 9, 2008). Includes bibliographical references (p. 145-160).
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