Meandering Bend Development Process at Mawa Reach of the Padma River

Muhammad Muzibur Rahman, M. NazrulIslam
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引用次数: 1

Abstract

The river Padma developed a meandering bend at the right bank of Mawa reach (reach 2) in meandering platform stage. The bend development process started in 1992 and continued in full form up to 2000. Maximum lateral extension occurred 780 m/yr in 1995-96 and average lateral extension was 450 m/yr. During the bend development process the Padma eroded more than 12,500 ha landmass at the bend location. The highly erodible bank materials and river characteristics allowed the bend formation at this location. A good number of samples measurement of different time indicated that the meandering wavelength of the river reach varied from 30 to 40 km. The meandering width of the river reach was about 17 km in 2000. The bend sustained only for 8 years (1992-2000) and was not so concave but the bend has great significance upon the river training work like the constricting Padma River Bridge. Satellite images of CEGIS and several definition diagram models of meandering bend have been developed to explain the bend formation process and bend characteristics.
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帕德玛河玛瓦河段蜿蜒弯道的开发过程
帕德玛河在曲流台地阶段在玛瓦河段(河段2)右岸形成曲流弯道。弯管的开发过程始于1992年,一直持续到2000年。1995-96年最大侧向扩展量为780 m/yr,平均侧向扩展量为450 m/yr。在弯曲的发展过程中,帕德玛河在弯曲的位置侵蚀了超过12500公顷的陆地。河岸物质的高度可蚀性和河流的特征使得这里形成了弯曲。大量不同时间的样品测量表明,河段的蜿蜒波长在30 ~ 40 km之间。2000年,这条河流蜿蜒的宽度约为17公里。这个弯道只持续了8年(1992-2000),并没有那么凹,但它对河流治理工作有重要意义,比如收缩的帕德玛河大桥。为了解释弯曲的形成过程和弯曲的特征,建立了CEGIS卫星图像和几种曲流弯曲的定义图模型。
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