| CHARACTERISTICS OF SEDIMENT TRANSPORT AND CHANNEL FORMATION BY FLOODS AT HYPERCONCENTRATIONS OF SEDIMENT IN THE YELLOW RIVER |
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| 引用本文： | QI Pu and ZHAO Yean Engineer,Institute of Hydraulic Research,Yellow River Conservancy Commission Engineer,Institute of Hydraulic Research,Yellow River Conservancy Commission. CHARACTERISTICS OF SEDIMENT TRANSPORT AND CHANNEL FORMATION BY FLOODS AT HYPERCONCENTRATIONS OF SEDIMENT IN THE YELLOW RIVER[J]. 国际泥沙研究, 1993, 0(1) |
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| 作者姓名： | QI Pu and ZHAO Yean Engineer Institute of Hydraulic Research Yellow River Conservancy Commission Engineer Institute of Hydraulic Research Yellow River Conservancy Commission |
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| 作者单位： | QI Pu and ZHAO Yean Engineer，Institute of Hydraulic Research，Yellow River Conservancy Commission Engineer，Institute of Hydraulic Research，Yellow River Conservancy Commission |
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| 摘 要： | 1. INTRODUCTIONThe Yellow River is a heavily sediment--laden river. Floods at Hyperconcentrationso f sediment (hereinafter simply referred to as hyperconcentrated flood) frequently occurring in the main river and its tributaries possess different characteristics of sedimenttransport. Sometimes they cause severe deposition whereas at other times they are capable of carrying substantial amount of sediment over long distances. The study on the lawof sediment transport is of significance to …
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CHARACTERISTICS OF SEDIMENT TRANSPORT AND CHANNEL FORMATION BY FLOODS AT HYPERCONCENTRATIONS OF SEDIMENT IN THE YELLOW RIVER |
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| QI Pu and ZHAO Yean Engineer. CHARACTERISTICS OF SEDIMENT TRANSPORT AND CHANNEL FORMATION BY FLOODS AT HYPERCONCENTRATIONS OF SEDIMENT IN THE YELLOW RIVER[J]. International Journal of Sediment Research, 1993, 0(1) |
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| Authors: | QI Pu and ZHAO Yean Engineer |
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| Affiliation: | QI Pu and ZHAO Yean Engineer,Institute of Hydraulic Research,Yellow River Conservancy Commission Engineer,Institute of Hydraulic Research,Yellow River Conservancy Commission |
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| Abstract: | This paper deals with sediment transport at hyperconcentrations in the Yellow River and its tributaries in channel of different patterns (braided and meandering). Such kind of sediment transport has significant effects on the formation and stability of a deep and narrow channel best suited to the conveyance of hyperconcentrated flood. The anomalies occurring with such flow are also discussed. |
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| Keywords: | Hyperconcentrated flood Channel patterns Braided Meandering Morphology Bingham model Yield stress Deposition Scouring. |
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