Morphology and roughness in the hydraulics of large bed element channels
The evolution of natural steep channels is a function of two factors in accordance with the principle of least action: flow distribution in the channel and terrain geomorphology. Large bed elements (LBE) occurring in the stream bed act on both factors. Stream flow in steep natural terrain occurs in...
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| Format: | conferenceObject |
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1996
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| Online Access: | http://hdl.handle.net/10725/7242 http://libraries.lau.edu.lb/research/laur/terms-of-use/articles.php http://cedb.asce.org/CEDBsearch/record.jsp?dockey=0066610 |
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