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Estimation and prediction of the oscillation pattern of meandering geometry in a sub-catchment basin of Bhagirathi-Hooghly river, West Bengal, India

机译:印度孟加拉西孟加拉邦河谷盆地曲折几何振荡模式的估计与预测

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摘要

Meandering is the winding curve or bends in a river within the floodplain area. Though it is a natural process, it affects the populace by the resultant effect of lateral migration with bank erosion in the floodplain area. The present sub-catchment basin (Nabadwip-Kalyani stretch) of the Bhagirathi-Hooghly river is a vital lifeline of southern West Bengal, which offers adequate water for irrigation, industrialisation, and human habitation. This region is experiencing a favourable geomorphic change through river bank line changing with bank erosion and sinuous meandering. Illegal sand mining and monsoonal flood enhances the meandering process and triggers the reduction of settlement and cropland. The present study elaborates on the migration tendencies and meandering geometry of this zone and tries to predict the future river centerline position in a sinuous course. The study area is divided into 30 cross-sections, which reveals the increasing trend of lateral migration and erosion behaviour towards the eastward section of this region. The spatial and temporal shifting of river centerline and resultant migration observes and predicts through the migration coefficient approach by Arc GIS v 9.3.1.This model indicates the trend of channel width decreasing, with increasing near bank velocity in the crescent of meandering bend in future. The simulated and predicted centerline validates by positive linear relation ( R~2) and lowest RMSE value in few cross-sectional areas. The oscillation character of meander signifies the amount of discharge in the sub-catchment basin. The unpredictable behaviour of the migration shows a rapid change of meandering geometry through the increasing nature of bank erosion possibilities with peak discharge during monsoon. The study predicts future centerline of the meandering channel and the information on river migration, which will contribute to the plan on bank erosion and denote the vulnerable zonation.
机译:蜿蜒的是洪泛区区域内的河流曲线或弯曲。虽然它是一种自然的过程,但它通过横向迁移与洪泛区中的银行侵蚀产生效果影响民众。 Bhagirathi-Hooghly河的本集团盆地(Nabadwip-Kalyani延伸)是西孟加拉邦南部的重要生命线,为灌溉,工业化和人类居住提供了足够的水。该地区正在通过河岸线改变银行侵蚀和蜿蜒的蜿蜒态度,经历了有利的地貌变化。非法沙坑和季风洪水增强了蜿蜒的过程,并触发了沉降和农作物的减少。本研究详细阐述了该区域的迁移趋势和蜿蜒的几何形状,并试图在蜿蜒的过程中预测未来的河流中心线位置。研究区分为30个横截面,揭示了对该地区东部侧面迁移和侵蚀行为的越来越大的趋势。通过弧GIS v 9.3.1的迁移系数方法观察并预测河流中心线的空间和时间转移和预测。该模型表示通道宽度下降的趋势,随着未来的曲折弯曲的新月中的近距离速度越来越多。模拟和预测的中心线通过正线性关系(R〜2)验证,并且在很少的横截面积中的最低RMSE值。曲折的振荡特征意味着子流域盆地的放电量。迁移的不可预测的行为通过在季风期间峰值放电的峰值放电增加,蜿蜒几何形状的快速变化。该研究预测了蜿蜒的渠道的未来中心线和河流迁移的信息,这将有助于银行侵蚀的计划,并表示脆弱的区划。

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