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首页> 外文期刊>Natural Hazards >River bank erosion hazard study of river Ganga, upstream of Farakka barrage using remote sensing and GIS
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River bank erosion hazard study of river Ganga, upstream of Farakka barrage using remote sensing and GIS

机译:基于遥感和GIS的法拉卡卡河上游恒河河岸侵蚀危害研究

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摘要

This study has been carried out to analyze and report the river bank erosion hazard due to morphometric change of the Ganga River (also called Ganges in English) in the upstream of Farakka Barrage up to Rajmahal. Morphometric parameters, such as, Sinuosity, Braidedness Index, and percentage of the island area to the total river reach area were measured for the year of 1955, 1977, 1990, 2001, 2003, and 2005 from LANDSAT and IRS satellite images. The analysis shows that there is a drastic increase in all of those parameters over the period of time. This study has found that bank failure is because of certain factors like soil stratification of the river bank, presence of hard rocky area (Rajmahal), high load of sediment and difficulty of dredging and construction of Farakka Barrage as an obstruction to the natural river flow. For the increasing sinuosity, the river has been engulfing the large areas of left bank every year. The victims are mostly Manikchak and Kaliachak-II blocks of Malda district, with a loss of around 1,670 ha agricultural land since 1977. Temporal shift measurements for the river reach between Farakka and Rajmahal has been done with help of 22 cross-sections in this reach. Erosion impact area has also been estimated to emphasize the devastating nature of the hazard.
机译:这项研究已经进行了分析并报告了由于法拉卡河上游至拉贾马哈尔上游的恒河(英语中也称为恒河)的形态变化而引起的河岸侵蚀危害。根据LANDSAT和IRS卫星图像,分别测量了1955、1977、1990、2001、2003和2005年的形态参数,如细度,辫度指数以及岛屿面积占河流总面积的百分比。分析表明,随着时间的推移,所有这些参数都急剧增加。这项研究发现,河岸破坏是由于某些因素造成的,例如河岸的土壤分层,坚硬的岩石区(Rajmahal)的存在,沉积物的高负荷以及法拉卡卡拦河坝的疏and和施工作为阻碍自然河水流动的障碍。 。由于不断增加的弯曲度,河流每年都在吞没左岸的大片地区。受害者主要是马尔达(Malda)地区的Manikchak和Kaliachak-II街区,自1977年以来损失了约1,670公顷的农业用地。在该河段的22个断面的帮助下,对法拉卡(Farakka)和拉贾马哈尔(Rajmahal)之间的河段进行了时移测量。 。还估计了侵蚀影响区域,以强调危害的破坏性。

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