Identification of prime factors of active river bank erosion in the lower course of Ganga Bhagirathi River: a study

Pub Date : 2022-12-21 DOI:10.12775/bgeo-2022-0011
D. Ghosh
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Abstract

The present study aims to identify prime factors of active and continuous riverbank erosion. Field visits were conducted from 2015 to 2019. To fulfil the objective of the study, 21 study units prone to bank erosion were selected along the banks of Ganga-Bhagirathi at Jangipur sub-division. Remote sensing and geographic information system were used to measure the area under erosion and deposition from the 1985 to 2015 at five-year intervals. Bank height, bank angle, length of fracture from bank line, river velocity, and channel depth were measured for each study unit using different instruments like cup-type water current meter, clinometers, and measuring tape. Soil samples were collected for textural analysis. Factor analysis was performed to find out prime responsible factors for active riverbank erosion. The result of the study shows that bank height, bank angle, channel width, and fracture length together comprise the first component, which explains 29.48 percent of variance. Riverbank erosion happens due to physical and manmade factors in the lower plain area of the Ganga-Bhagirathi River.
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恒河巴吉拉蒂河下游河岸活跃侵蚀的主要因素识别研究
本研究旨在找出河堤主动和持续侵蚀的主要因素。2015年至2019年进行了实地考察。为了实现研究的目标,在江吉布尔的恒河-巴吉拉蒂河沿岸选择了21个容易发生河岸侵蚀的研究单位。利用遥感和地理信息系统对1985 - 2015年的侵蚀沉积面积进行了每5年一次的测量。利用杯式水流计、测斜仪、卷尺等不同仪器测量了各研究单元的岸高、岸角、断裂带离岸线的长度、流速和河道深度。采集土壤样品进行质地分析。通过因子分析,找出河堤主动侵蚀的主要原因。研究结果表明,岸高、岸角、河道宽度和裂缝长度共同构成了第一个分量,解释了29.48%的方差。恒河-巴吉拉蒂河下游平原地区的河岸侵蚀是由自然和人为因素造成的。
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