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The exploration application of MIKE SHE model in Qingtongxia irrigation area water recycle

机译:迈克的探讨在青通峡灌区水循环中的应用

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The water diversion-transportation-drainage-return had become the dominant regional hydrological processes in Qingtongxia irrigation area. For the reason of systematically mastering water cycle rules of Qingtongxia irrigation area, this study chose MIKE SHE distributed hydrological model with physical basis to build water-cycle model of Qingtongxia irrigation area, calculated the parameters with data of underground water level and drainage flow from 2007 to 2009, and validated the parameters with same data from 2010 to 2012. Using this model, this study simulated and analyzed the conversion relationship of different water cycle factors in Qingtongxia irrigation area. The results shown that annual average evapotranspiration was 3.537 billion m~3, total drainage ditches flow was about 2.832 billion m~3, and the groundwater runoff into Yellow River was about 55 million m~3. This study firstly quantitative clarified the relationship between recharge and discharge of Qingtongxia irrigation area and the Yellow River. These will lay the foundation for studying the water circulation evolution mechanism and water resources efficient utilization under changing environment.
机译:水转流量 - 运输排水返回已成为青通峡灌区的主导地区水文过程。出于系统地掌握青通峡灌区的水循环规则,本研究选择了迈克希海分布式水文模型与物理基础,以建立青通峡灌区水循环模型,计算了2007年地下水位数据和排水流量的参数。致2009年,并从2010年到2012年验证了具有相同数据的参数。使用该模型,本研究模拟并分析了青通峡灌区不同水循环因子的转换关系。结果表明,年平均蒸散量为35.37亿m〜3,排水总排水沟率约为28.32亿毫米,地下水径流为黄河约5500万米〜3。本研究首先定量澄清了青通峡灌区和黄河的充电和排放之间的关系。这些将奠定基础,用于研究改变环境下的水循环演化机制和水资源有效利用的基础。

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