Morphodynamic Changes of Bhagirathi River at Murshidabad District Using Geoinformatics

Surajit Panda, Jatisankar Bandyopadhyay
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引用次数: 17

Abstract

The channel of Bhagirathi River is the branches off from the Ganga at Nurpur (lower course of the Ganga). Bhagirathi River is one of the main rivers in Murshidabad district. Analyzing the image of the Bhagirathi River in Murshidabad district through the year 1970, 1977, 1990, 2000 and 2006, it is found that significant changed has been occurred in souththern part of the river and less change is found in the middle part which is close to the Berhampore town. Toposheet of the year 1970 is also compared with the image data to observe the change. Water discharge, soil types and transportation of sediment is the major contributing factor of morphological changes like bar or shoal, ox-bow Lake, meander etc. Maximum erosion takes place at Dear Balagachi and after Baidyanathpur. A cut-off has take place at Baidyanathpur in 1984 [1]. It is found from the study that there is a possibility of natural meander cut-off at Dear Balagachi and near Majayampur. The traditional bank protection works, concrete walls, cemented stone and brick, play a significant role in the modification of the hydraulic aspect of the discharge values and in the interference in the water dynamics of erosive and depositional phenomena both upstream and downstream.
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基于地理信息学的Murshidabad地区Bhagirathi河形态动力学变化
巴吉拉蒂河的河道是恒河在努尔普尔(恒河下游)的支流。巴吉拉蒂河是穆尔西达巴德地区的主要河流之一。分析Murshidabad地区的Bhagirathi河1970、1977、1990、2000和2006年的图像,发现河的南部发生了显著的变化,而靠近Berhampore镇的中部变化较小。并将1970年的Toposheet与图像数据进行对比,观察其变化。径流量、土壤类型和泥沙运移是造成沙洲、浅滩、牛轭湖、曲流等地貌变化的主要因素。最大的侵蚀发生在Dear Balagachi和Baidyanathpur之后。1984年,Baidyanathpur发生了一次切断[1]。从研究中发现,在Dear Balagachi和Majayampur附近存在自然曲流切断的可能性。传统的护岸工程,混凝土墙,胶结石和砖,在改变水力方面的流量值和干扰上游和下游的侵蚀和沉积现象的水动力学方面发挥了重要作用。
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