首页> 外文会议>Symposium on Water Resources Systems - Water Availability and Global Change; Jun 30-Jul 11, 2003; Sapporo, Japan >The impacts of human activity on hydrological processes in the arid zones of the Hexi Corridor, northwest China, in the past 50 years
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The impacts of human activity on hydrological processes in the arid zones of the Hexi Corridor, northwest China, in the past 50 years

机译:近50年来人类活动对河西走廊干旱区水文过程的影响

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The Hexi Corridor, like other arid zones in northwest China, is characterized by alternating high mountains and plains. The mountain areas have abundant precipitation and glaciers that provide surface water flow to the plains and form numerous inland river systems. The hydrological regimes of the groundwater and springs, to a large extent, depend on the surface runoff. The regional hydrology and ecosystems of the Hexi Corridor region have changed over the last half century under the driving force of intense human activity. This paper aims to show the characteristics of hydrological changes resulting from human activities in the last 50 years from several points of view, such as: surface runoff changes at the mountain front and in the lower reaches of streams, both annual and inter-annual, the changes of the groundwater table and spring water volume, and temporal and spatial hydro-chemical regimes. Streamflow issuing from mountains in the eastern section of the Corridor by way of the Shiyang River has decreased significantly. Annual mountain outflow from the Heihe and Shule rivers in the central and western portions of the Corridor, respectively, have tended to increase. However, river discharge in the lower reaches is decreasing, terminal lakes are contracting or drying up and water quality is getting worse due to expanding large-scale exploitation of water resources. Many small rivers disappear soon after flowing from mountain valleys, river courses are shortening, the spring water volume is continually reducing, and the groundwater table is falling in most parts of the middle and lower reaches. These hydrological changes exacerbate the water supply-demand paradox, and result in serious environmental problems. Understanding the characteristics of hydrological processes and regime change is important for driving the solutions to rational use of the limited water resources and the limiting of environmental degradation in the northwest China.
机译:与中国西北地区的其他干旱地区一样,河西走廊的特点是高山和平原交错。山区有丰富的降水和冰川,可为平原提供地表水流,并形成许多内陆河系。地下水和泉水的水文状况在很大程度上取决于地表径流。在过去的半个世纪中,在人类活动的推动下,河西走廊地区的区域水文学和生态系统发生了变化。本文旨在从多个角度展示过去50年中人类活动导致的水文变化特征,例如:山区前沿和河流下游以及每年和年际的地表径流变化,地下水位和泉水量的变化,以及时空的水化学状态。从走廊东部的山区通过石羊河流出的水流量已大大减少。走廊中部和西部地区的黑河和疏勒河每年的山区流出量都有增加的趋势。但是,由于扩大了对水资源的大规模开发,下游的河流流量正在减少,终端湖泊正在收缩或枯竭,水质日益恶化。许多小河从山谷流出后不久就消失了,河道正在缩短,泉水量不断减少,中下游大部分地区的地下水位正在下降。这些水文变化加剧了水供需矛盾,并导致严重的环境问题。了解水文过程和政权变化的特征对于推动合理利用有限的水资源和限制西北地区环境退化的解决方案至关重要。

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