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Riverbank erosion rates prediction incorporating soil erodibility and soil properties relationship: Bernam River, Malaysia case study

机译:河岸侵蚀利率预测土壤易蚀和土壤性质关系:伯恩河,马来西亚案例研究

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Riverbank erosion and lateral migration changes are very complex and complicated processes. Although it is obvious that all rivers will experience these phenomena, it may be less obvious that there are consistent underlying relationships between different riverbank erosion and lateral migration with parameters such as hydraulic and hydrodynamic characteristics, river bank geometry, soil properties, grain or flow resistance, channel characteristics and others such as vegetation condition. Relationship between soil erodibility and the riverbank erosion rates is considered as one of the primary processes concerned in the development of channel migration. This research investigates riverbank erosion in the Bernam River, Malaysia. Field monitoring data was collected to obtain sufficient amount of information for variables of riverbank erosion factors i.e. channel geometry, hydraulics characteristics and erodibility in order to explain the controls on temporal changes in riverbank erosion rates.
机译:Riverbank侵蚀和横向迁移变化是非常复杂和复杂的过程。虽然很明显,所有河流都会体验这些现象,但这可能不太明显,不同的河岸侵蚀和横向迁移之间存在一致的潜在关系,液压和流体动力学特性,河岸几何形状,土壤性质,谷物或流动阻力等参数之间存在一致的潜在关系,沟道特征和其他植被状况等其他特征。土壤蚀和河岸侵蚀率之间的关系被认为是有关渠道迁移发展的主要过程之一。本研究调查了马来西亚河马河流的河岸侵蚀。收集现场监测数据,以获得足够量的河岸侵蚀因素的变量信息,即通道几何形状,液压特性和蚀力,以解释河岸侵蚀率的时间变化的控制。

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