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Preliminary discussion of water and sediment variation mode in the middle Yellow River

机译:中黄河中水和沉积物变化模式的初步探讨

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The Yellow River is a river that has relatively less runoff but with much sediment discharge, of which the water mainly come from the upstream while the sediment from the middle reaches, and they are imbalanced in the transporting process. The amount of water and sediment change greatly and the duration of their coming centralized exceedingly, they are complex and polytropic. The mode of water and sediment variation in the middle Yellow River is mostly concerned in its management. For the specificity of the Yellow River in water and sediment, sedimentation is very serious, which severely affected the channel. In this paper, according to former research, data referred to flood and sediment were collected and arranged, the mode of water and sediment variation in the middle Yellow River was preliminarily analyzed and discussed. The results showed that the most important two modes were the Rich Water Rich Sediment mode and the Low Water Low Sediment mode.
机译:黄河是一条相对较少的径流,但具有很多沉积物的河流,其中水主要来自上游的沉积物,它们在运输过程中不平衡。 水和沉积物的数量大大变化,它们的集中持续时间非常复杂和多细胞。 中黄河中的水和沉积物变化主要涉及其管理。 对于黄河在水和沉积物中的特异性,沉淀非常严重,这严重影响了渠道。 本文根据前述研究,收集和安排了洪水和沉积物的数据,初步分析并讨论了中黄河中的水和沉积物变化。 结果表明,最重要的两种模式是富含水富沉积物模式和低水量低沉积物模式。

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