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Impact of missing flow on active inundation areas and transformation of parafluvial wetlands in Punarbhaba-Tangon river basin of Indo-Bangladesh

机译:缺失流动对南京南京北京汤塘河盆地的活跃淹没地区的影响和转型湿地

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摘要

Punarbhaba river of Indo-Bangladesh has experienced hydro-ecological alteration after installation of Komardanga dam in 1992 and consequently wetland and inundation areas have undergone into transformation. The present work intends to explore the impact of flow attenuation on contemporary and upcoming flood extent and flood plain wetlands. In post-dam condition, average and maximum flows are attenuated by 36 and 41%, respectively, and as a result the active flood prone area is squeezed considerably by 39.72%. Average flood water depth is also reduced by 37.87% (4.45metre) after flow modification. Due to shrinkages of flood prone areas, wetland area is also reduced from 215.70 to 90.40 km(2) and larger part of the present wetland area is under stress and critical state. Predicted flood prone areas in next 25 years will be 328.91 km(2) and consequently 65.63 km(2) wetland areas may further be under hydro-ecological threats. Release of ecological flow is essential to restore and preserve the wetland.
机译:1992年在电科帕冈大坝安装后经历了水力生态改变,因此湿地和淹没地区经历了转型。本工作旨在探讨流动衰减对现代,即将泛滥的洪水范围和洪水平原湿地的影响。在后坝后状态下,平均和最大流量分别衰减36和41%,因此主动洪水易于区域被大幅挤压39.72%。平均洪水深度在流动修改后也减少了37.87%(4.45morre)。由于洪水易发的地区的收缩,湿地面积从215.70降至90.40 km(2),并且当前湿地区域的较大部分处于应力和临界状态。预计25年的洪水普遍区域将是328.91 km(2),因此65.63公里(2)湿地区域可能进一步受水电生态威胁。生态流动释放对于恢复和保留湿地至关重要。

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