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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:人类活动对中国西北地区河西走廊干旱区水文过程的影响,在中国西北部,在过去的50年里

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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:与中国西北部的其他干旱区一样,河西走廊的特点是交替高山和平原。山区具有丰富的降水和冰川,为平原提供表面水流,并形成众多内陆河流系统。地下水和弹簧的水文制度在很大程度上取决于表面径流。河西走廊地区的区域水文和生态系统在过去半个世纪下发生了浓烈人类活动的推动力。本文旨在展示从几个角度来看人类活动产生的水文变化的特点,例如:在山前面和溪流下游的表面径流变化,年度和年度阶段,地下水位和弹簧水量的变化,以及时间和空间水化学制度。通过石羊河东部的山脉发出的流出发布的山脉已经显着下降。从黑河和胸部河流的年山流出分别在走廊的中部和西部部分,倾向于增加。然而,河流放电在下游较低,终端湖泊正在收缩或烘干,由于扩大对水资源的大规模开采的大规模开采,水质变得更糟。从山谷流动后,许多小河很快就消失了,河流课程缩短,弹簧水量不断减少,地下水位落在中下游的大部分部分。这些水文变化加剧了供水需求悖论,并导致严重的环境问题。了解水文过程的特点和制度变化对于推动合理利用有限水资源的解决方案以及在中国西北部环境退化的限制是重要的。

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