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...
محفوظ في:
| المؤلف الرئيسي: | |
|---|---|
| التنسيق: | conferenceObject |
| منشور في: |
1996
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| الموضوعات: | |
| الوصول للمادة أونلاين: | 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 |
| الوسوم: |
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