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首页> 外文期刊>Journal of Geology & Geophysics >Meandering Bend Development Process at Mawa Reach of the Padma River
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Meandering Bend Development Process at Mawa Reach of the Padma River

机译:帕德玛河Mawa河段弯弯曲曲发展过程

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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.
机译:帕德玛河在蜿蜒的台地阶段,在Mawa河段右岸(2号河段)形成了一条蜿蜒的弯道。弯道发展过程始于1992年,并一直持续到2000年。在1995-96年间,最大横向延伸量为780 m / yr,平均横向延伸量为450 m / yr。在弯道开发过程中,Padma在弯道处侵蚀了超过12,500公顷的陆地。高度易腐蚀的河岸材料和河流特征使该位置形成弯头。在不同时间的大量样本测量表明,河流的曲折波长在30至40 km之间变化。 2000年,河段的曲折宽度约为17公里。该弯道仅维持了8年(1992-2000年),虽然没有那么凹,但对像帕德玛河大桥一样的河道治理工作具有重要意义。开发了CEGIS的卫星图像和弯曲弯道的几种定义图模型,以解释弯道的形成过程和弯曲特性。

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