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Sedimentasi Pertemuan Dua Buah Sungai pada Sungai Mangkauk dan Sungai Riam Kiwa

机译:芒考克河和里亚姆·奇瓦河上两次河果汇的沉积

摘要

Naturally river\u27s function as experienced basin to transport water from its stream area and conduct in gravitation to lower area. As water source which can be used for the irrigation of, agriculture, drinking water, industrial, energy generating, transportation. This research aim to give the analysis form and place of where there are sediment load which is there in the meeting of Riam Kiwa River and Mangkauk River which is resulted by the existence of wide difference of dimension of the river and stream speed. Method used to calculate basic speed, sediment with Van Rijn method, because entangling factor speed of the river flow and basic sediment concentration.From solution result got the following conclusion: stream speed, wide and form the river very influencing to the number of sediment which can be lifted and precipitated by current, sediment item which have diameter to smaller than 2,0 mm earn is easily brought by river stream, and form the river meeting very influencing of pattern of sediment that happened. Therefore the importance of furthermore research about sediment in the river, particularly at two river cross)
机译:河流自然是经验丰富的流域,可以从河流流域输送水,并在重力作用下流向较低区域。作为可用于农业灌溉,饮用水,工业,能源生产,运输的水源。本研究的目的是给出由于河流尺寸和水流速度差异较大而引起的里亚姆奇瓦河和芒考克河交汇处存在泥沙的分析形式和地点。由于河水流速和基本泥沙浓度的缠结因素,采用范里恩法计算基本速度,泥沙的方法。从求解结果可得出以下结论:溪流速度,河道的宽大和形成对泥沙数量的影响很大。可以通过水流将其提起并沉淀,直径小于2.0毫米的沉积物很容易被河水带走,并形成一条河流,对发生的沉积物形态产生很大的影响。因此,进一步研究河流中的沉积物(特别是两条河流跨界处)的重要性)

著录项

  • 作者

    Kurdi, Holdani;

  • 作者单位
  • 年度 2007
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  • 入库时间 2022-08-20 20:53:34

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