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Damming effects on the degree of hydrological alteration and stability of wetland in lower Atreyee River basin

机译:坝上河流域湿地水文改变与稳定性的渔裂效果

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Numerous studies have discovered damming effect on downstream river eco-hydrological state but little is thought about its consequences on eco-hydrology of riparian wetlands. Hydrological data scarcity at a spatial scale is one of the major constraints. The present study intends to explore the damming effect on eco-hydrological components like wetland depth, consistency in water appearance, hydrological stability, eco-hydrological failure and eco-deficit using spectral indices from remote sensing data taking Atreyee river basin as a case. Time series Normalized differences water index and Modified normalized differences water index are taken as the database. Range of variability approach and flow duration curve methods are adopted for the computing failure rate of ecological water appearance and eco-deficit in the wetland. The result shows a statistically acceptable positive relation (0.76 to 0.89) between normalized differences water index and modified normalized differences water index value and depth of water in wetland inferring the substitutability of spectral values to depth data. In the post-dam phase (2012 onward) about 82% and 96% wetland area in pre-monsoon and post-monsoon season has turned into a hydrologically unstable state leading to a growing failure rate for attaining ecologically essential water volume and eco-hydro deficit state of wetland. Damming has converted only 100% wetland area into the eco-deficit zone which is ecologically not viable. Based on the findings study recommends that for the survival of the river and wetland ecological flow is required to release from the dam.
机译:众多研究发现了对下游河生态水文州的渔裂效应,但对河岸湿地生态水文的影响很少。空间尺度的水文数据是主要限制之一。本研究打算探讨湿地深度等生态水文组分的坝体效果,水外观的一致性,水文稳定性,生态水文失败和生态缺陷,使用来自遥感数据的光谱指标,以atreyee河流域为例。时间序列归一化差异水指数和修改的归一化差异水指数作为数据库。可变性方法和流动持续时间曲线方法采用了湿地生态水景的计算失败率和生态赤字。结果表明,常规化差异水指数和改性标准化差异水指数值和水深在湿地推动光谱值的可替代性以深度数据之间的差异常规差异水指数值和深度之间的统计学上可接受的阳性关系(0.76至0.89)。在后大坝阶段(2012年上行)在季风普通话和季风季节的约82%和96%的湿地地区变成了一种水文不稳定的状态,导致生态基本水量和生态水力的失败率不断增长的失败率赤字湿地。该渔村已将100%湿地区域转换为生态赤字区,这是生态上不可行的。根据研究结果,研究建议在河流的生存和湿地生态流动需要从大坝释放。

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