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Impacts of environmental flow controls on the water table and groundwater chemistry in the Ejina Delta, northwestern China

机译:西北额济纳三角洲环境流量控制对地下水位和地下水化学的影响

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摘要

The impacts of environmental flow controls on the water table and chemistry of groundwater in the Ejina Delta, an arid inland river basin in northwest China, were investigated with field observations in 2001 and 2009. The results indicate that the shallow groundwater level rose by 0-2 m in the upper reaches of the east tributary of the Heihe River and in the areas of Saihantaolai—Dalaikubu during the period of environmental flow controls. The chemical constituents of the groundwater show a distinct spatial heterogeneity with the total dissolved solids (TDS) in the groundwater increasing from the periphery towards the depocenter of the Ejina Basin. In addition, the rate of groundwater cycling in the south of the Ejina Delta increased, and the mineralization of groundwater declined, while the overall mineralization and salinity increased in the northern regions, especially in the depocenter of the Ejina Basin. Since shallow groundwater is important to the ecology of arid regions, and because understanding the changes in the shallow groundwater environment (groundwater level and hydrochemistry) in response to environmental flow controls is essential for the sustainable improvement of the ecological environment, the results of this paper can be used as a reference for watershed water resources planning and management to help maintain the health and proper function of rivers in arid regions.
机译:通过对2001年和2009年的野外观测,研究了环境流量控制对西北干旱内陆河流域额济纳三角洲的地下水位和地下水化学的影响。结果表明,浅层地下水位上升了0-在环境流量控制期间,黑河流域东支流上游和赛汉陶莱—达莱库布地区2 m。地下水的化学成分表现出明显的空间异质性,地下水中的总溶解固体(TDS)从额济纳盆地的外围向沉积中心增加。此外,额济纳三角洲南部的地下水循环速率增加,地下水的矿化度下降,而北部地区,特别是额济纳盆地的沉积中心地区的总矿化度和盐度增加。由于浅层地下水对于干旱地区的生态至关重要,并且因为了解浅层地下水环境(地下水位和水化学)对环境流量控制的响应对于生态环境的可持续改善至关重要,因此本文的结果可作为流域水资源规划和管理的参考,以帮助维持干旱地区河流的健康和正常运行。

著录项

  • 来源
    《Environmental Geology》 |2011年第1期|p.15-24|共10页
  • 作者单位

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences,11A, Datun Road, Chaoyang District, Beijing 100101,People's Republic of China;

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences,11A, Datun Road, Chaoyang District, Beijing 100101,People's Republic of China;

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences,11A, Datun Road, Chaoyang District, Beijing 100101,People's Republic of China;

    Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences,11A, Datun Road, Chaoyang District, Beijing 100101,People's Republic of China;

    Graduate University of the Chinese Academy of Sciences,19A Yuquan Road, Beijing 100049, People's Republic of China;

    Graduate University of the Chinese Academy of Sciences,19A Yuquan Road, Beijing 100049, People's Republic of China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    environmental flow controls; groundwater environment; groundwater level; hydrochemistry; ejina delta; heihe river basin;

    机译:环境流量控制;地下水环境;地下水位;水化学额济纳三角洲黑河流域;

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