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Interactions between dam-regulated river flow and riparian groundwater: a case study from the Yellow River, China (pages 1552–1560)

机译:大坝调节的河流流量与河岸地下水之间的相互作用:以中国黄河为例(第1552–1560页)

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The Xiaolangdi Dam, completed in 2000, is second in scale in China to the Three Gorges Project. It has generated remarkableneconomic and social benefits but with profound impacts to the riverine and regional environments. This paper reports fieldnmonitoring of riparian groundwater in the Kouma section of the Yellow River to illustrate the interactions between damregulatednriver flow and riparian groundwater. The results show that the hydrological condition in riparian zones downstreamnfrom the dam has changed from a typical wet–dry cycle to a condition of semi-permanent dryness, resulting in degradation of thentypical attributes and functions of the wetland ecosystem. Hydrological processes in the riparian zone have changed from ancomplex multiple flooding regime to a simple regime of dominant groundwater drainage towards the river, which only reversesntemporarily during the water and sediment regulation period of the dam. Data on groundwater level and groundwater qualitynshow that there are two key points, at ca 200 and 400m from the river bank, which distinguish zones with different sensitivity tonchanges of river flow and indicate different interactions between river water and groundwater. The shallow groundwater qualitynalso is negatively affected by the intensive agricultural development that has occurred since the dam was completed. Ecologicalnrestoration needs to be carried out to construct a protective natural riparian zone within ca 200m from the river, this being annecotone, which is key to the protection of both riparian groundwater and the river. The riparian zone from 200 to 400m alsonshould be treated as a transitional zone. In addition, ecologically sensitive agriculture and ecotourism organized by localncommunities would be beneficial in the area beyond 400 m. Copyright © 2011 John Wiley & Sons, Ltd.
机译:小浪底水坝于2000年完工,是中国三峡工程规模第二大的水坝。它产生了显着的经济和社会效益,但对河流和区域环境产生了深远的影响。本文报道了黄河口阿马河段河岸地下水的现场监测,以说明水流调节河床与河岸地下水之间的相互作用。结果表明,大坝下游河岸带的水文条件已经从典型的干湿循环转变为半永久性干旱,导致湿地生态系统的典型属性和功能退化。河岸带的水文过程已经从复杂的多次洪水状态转变为简单的向河流排泄主要地下水的状态,这仅在大坝的水和泥沙调节时期暂时逆转。地下水水位和地下水水质的数据表明,在距河岸约200和400m处有两个关键点,它们区分了河水流量敏感度变化不同的区域,并指出了河水与地下水之间的不同相互作用。自大坝建成以来,密集的农业发展也对地下水的浅层质量产生了负面影响。需要进行生态修​​复,以在距河约200m的范围内建立一个保护性的天然河岸带,这就是安妮酮,这是保护河岸地下水和河道的关键。 200至400m的河岸带也应视为过渡带。此外,当地社区组织的对生态敏感的农业和生态旅游将在400 m以上的区域受益。版权所有©2011 John Wiley&Sons,Ltd.

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