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Quantification of eroded and deposited riverbanks and monitoring river's channel using RS and GIS

机译:使用RS和GIS量化侵蚀和沉积的河岸和监测河道的监测河道

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The Padma and the Jamuna are the two of three major rivers those flow within few meters of height in Bangladesh. These rivers are very important in context of water navigation, irrigation, fishing and fresh water for down stream. On the other side, those are the rivers of erosion of riverbanks and deposition of sandbanks. The main objective of this study is to estimate the eroded and deposited banks of the Padma and the Jamuna and to visualize movement of their channels from 1977 to 2000. Three dates of Landsat images were acquired in 1977 (MSS), 1989 (TM) and 2000 (ETM+) over the study area. Processing of Landsat images was performed by PCI Geomatics and ArcGIS 9.2 was used for quantification of eroded and deposited land covers. Subset the data was performed as preprocessing of image. Seven types of land covers of level I were decided for imagery classification where settlement areas were separated using mask. Supervised classification method was applied using 200 pixels for each class as test set other than training area for accuracy assessment where average accuracies of 85.64%, 89.14% and 90.07% were achieved in 1977 (MSS), 1989 (TM) and 2000 (ETM+) respectively. ArcGIS 9.2 was used to transfer the classified images to GIS layer for quantification. Eroded and deposited areas of the Padma and the Jamuna between the years were calculated by superimposition and pair-wise comparison of river layers in 1977–89 and 1989–2000. From 1977 to 1989 and 1989 to 2000, estimated average erosion was 5436 and 2954 hectares/year and deposition was 773 and 1954 hectares/year correspondingly. In 1977, 1989 and 2000, estimated rivers area in the study area were 2789, 3348, 3458 sq km. During this period, there was more erosion than deposition which indicates that rivers were getting wider. The confluence point of the Padma and the Jamuna was migrated toward southeast and their channels were moved by erosion and deposition following their direction. General trend of - channel movement of the Padma was toward south but for the Jamuna, it was quite irregular.
机译:Padma和Jamuna是三大河流中的两种,在孟加拉国的距离几米之内。这些河流在水导航,灌溉,捕鱼和淡水中的背景下非常重要。在另一边,这些是河岸侵蚀的河流和沙洲的沉积。本研究的主要目标是估计帕尔马和贾马纳的侵蚀和存放的银行,并从1977年到2000年可视化他们的渠道的移动。1977年(MSS),1989(TM)获得了三个Landsat图像的日期2000年(ETM +)在研究区。通过PCI地理学和ArcGIS 9.2进行覆盖物图像的处理用于定量侵蚀和沉积的陆地覆盖物。子集数据被执行作为图像预处理。七种类型的级别我被决定用于图像分类,其中使用面膜分离沉降区域。使用200个像素的监督分类方法,每个班级的测试设置为比训练区域以外的准确度评估,1977年(MSS),1989(TM)和2000(ETM +)实现了85.64%,89.14%和90.07%的平均精度分别。 ArcGIS 9.2用于将分类的图像传送到GIS层进行量化。通过1977 - 89和1989-2000的河流层的叠加和成对比较来计算帕尔马和朱梅纳之间的侵蚀和沉积的区域。从1977年到1989年到1989年至2000年至2000年,估计的平均侵蚀是5436,2954公顷/年,沉积为773和1954公顷/年。 1977年,1989年和2000年,研究区的估计河区是2789,3348,3458平方公里。在此期间,侵蚀比沉积更多,表明河流越来越宽。 PADMA和Jamuna的汇合点迁移到东南,其渠道在其方向后被侵蚀和沉积移动。帕尔玛的渠道运动的一般趋势是南方,而是为jamuna来说,它是非常不规则的。

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