乌鲁木齐河流域地下水循环机理及其水资源调控响应研究

地下水循环 地表水 转化机制 调控 耦合模型
殷秀兰 2014-01 项目
Based on the construction of regional aquifer system model and analysis on problems of water resources exploitation, discharge of different sections will be measured regularly along upstream of Urumuqi river; groundwater flow system will be measurd in three dimensions with high frequency in the regions highly impacted by surface water; regional evaporation will be studied quantativly based on remote sensing and isotopic methods. Then the key phases of the exchange process of surface water and groundwater in Urumuqi River Basin will be researched through the above studies. By systematically analyzing the changes of water environment, river infiltration, groundwater discharge and groundwater flow field during the exploitation of water resources, the coupled surface water-groundwater numerical model calibrated with multi-source information will be established. The processes of recharge from mountainous areas and the changes of water environment, interaction between surface water and groundwater, groundwater flow field, salt accumulation and the responses of ecoystem which are driven by the exploitation of water resources in the past 50 years will be reproduced. The relations, mechanisms and controlling factors of those processes will be revealed. In the end, the results from this research project will provide basis for studies on joint control of regional surface water and groundwater, optimized allocation of water resources, and ecological environment construction.
在对乌鲁木齐河流域历年的调查资料和研究成果进行收集分析的基础上,对乌鲁木齐河流域上游天然河道与引水干渠流量进行定期监测,并对流域尺度遥感和同位素技术的蒸发量进行量化研究,系统地揭示流域地下水动态特征,构建含水层系统结构,并对流域水资源的利用现状及存在问题进行分析,深化对流域地下水与地表水相互作用机理的认识。进而系统分析流域水资源开发利用过程导致的地下水相关地质环境问题,构建基于多元信息校正的地表水与地下水耦合数值模型,重塑流域山区来水与水资源开发利用驱动的水环境变迁、地表水地下水相互作用、生态响应等过程,揭示它们之间的依存关系、作用机制及主控因素,提出流域地下水地表水联合调控、水资源优化配置的方案。