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The research of groundwater flow model in Ejina Basin, Northwestern China

机译:西北额济纳盆地地下水流模型研究

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Water resources is a primary controlling factor for economical development and ecological environmental protection in the inland river basins of arid western China. Groundwater, as the important component of total water resources, plays a dominant role in the development of western China. In recent years, with the utilization ratio of surface water raised, the groundwater recharge rate has been reduced by surface water, and groundwater was exploited on a large-scale. This has led to the decline of groundwater levels and the degradation of eco-environments in the lower reaches of Heihe watershed, especially. Therefore, the study on the groundwater-level change in recent years, as well as simulating and predicting groundwater levels changes in the future is very significant to improve the ecological environment of the Heihe River Basin, coordinate the water contradiction, and allocate the water resources. The purpose of this study is to analyze the groundwater-level variations of the Ejina region basin on a large-scale, to develop and evaluate a conceptual groundwater model in Ejina Basin; according to the experimental observation data, to establish the groundwater flow model combining MODFLOW and GIS Software; simulated the regional hydrologic regime in recent 10 years and compared with various delivery scenarios from midstream; determined which one would be the best plan for maintaining and recovering the groundwater levels and increasing the area of Ejina Oasis. Finally, this paper discusses the possible vegetation changes of Ejina Basin in the future.
机译:水资源是中国西部内陆河流域经济发展和生态环境保护的主要控制因素。地下水作为水资源总量的重要组成部分,在西部大开发中起着主导作用。近年来,随着地表水利用率的提高,地表水降低了地下水的补给率,大规模地开采了地下水。这尤其导致了黑河流域下游的地下水位下降和生态环境恶化。因此,近年来对地下水位变化的研究,以及对未来地下水位变化的模拟和预测,对于改善黑河流域的生态环境,协调水资源矛盾,调配水资源具有十分重要的意义。 。这项研究的目的是大规模分析额济纳地区盆地的地下水位变化,以开发和评估额济纳盆地的概念性地下水模型。根据实验观测数据,结合MODFLOW和GIS软件建立地下水流模型。模拟了近十年来的区域水文状况,并与中游的各种输水方案进行了比较;确定哪种方案是维持和恢复地下水位并增加额济纳绿洲面积的最佳方案。最后,本文讨论了额济纳盆地未来可能发生的植被变化。

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