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Geomorphic diversity as a river management tool and its application to the Ganga River, India

机译:地貌多样性作为河流管理工具及其在印度恒河中的应用

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Understanding of geomorphic processes and the determination of geomorphic diversity in catchments are prerequisites for the sustainable rehabilitation of river systems and for reach-scale assessment of river health. The Ganga River system in India is a large, complex system consisting of several long tributaries, some >1,000km, originating from 2 distinct hinterlandsthe Himalaya to the north and the cratons to the south. Traversing through a diverse climatic regime across the Plain and through precipitation zones ranging from 600mm/year near Delhi to 1,200mm/year in the eastern plains, the Ganga River system has formed very diverse landform assemblages in 3 major geomorphic domains. We have recognized 10 different river classes for the trunk river from Gangotri (source) to Farakka (upstream of its confluence with the Brahmaputra) based on (a) landscape setting, (b) channel and active floodplain properties, and (c) channel planform parameters. The mountainous stretch is characterized by steep valleys and bedrock channels and is dominated by large-scale sediment production and transport through hill slope processes. The alluvial part of the river is characterized by 8 different river classes of varying reach lengths (60-300km) many of which show sharp transitions in landscape setting. We have highlighted the application of this approach for the assessment of habitat suitability, environmental flows, and flood risk all of which have been significantly modified during the last few decades due to large-scale anthropogenic disturbances. We suggest that the diversity embedded in this geomorphic framework can be useful for developing a sustainable river management programme to work with the contemporary character and behaviour of rivers.
机译:了解流域的地貌过程和确定地貌多样性是河流系统可持续恢复和河流健康可达性评估的前提。印度的恒河系统是一个庞大而复杂的系统,由几个长支流组成,长约1000公里,发源于北部两个不同的腹地喜马拉雅山和南部克拉通。遍及整个平原的不同气候系统以及从德里附近的600mm /年到东部平原的1200mm /年的降水带,恒河系统已经在3个主要地貌域中形成了非常多样化的地貌组合。我们已根据(a)景观环境,(b)航道和活跃洪泛区特性以及(c)航道平面图,识别了从Gangotri(源头)到Farakka(与Brahmaputra汇合处的上游)的干线河的10种不同的河类。参数。多山地带的特点是陡峭的山谷和基岩河道,并以大规模的沉积物生产和通过山坡过程的运输为主导。河流冲积部分的特征是8种不同的河段,河段的长度各不相同(60-300公里),其中许多河段在景观环境中表现出明显的过渡。我们强调了这种方法在评估栖息地的适宜性,环境流量和洪水风险方面的应用,在过去的几十年中,由于大规模的人为干扰,所有这些因素都得到了重大修改。我们认为,嵌入到该地貌框架中的多样性对于开发可持续的河流管理计划以与河流的现代特征和行为一起工作可能是有用的。

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