1989—2019年新疆塔里木河流域地表−地下水变化  

Analysis of surface-groundwater changes in the Tarim River Basin of Xinjiang from 1989 to 2019

作　　者：王勇[1,2] 资锋 卢善龙[2,3,4] 李明阳 周晋峰 杨晓红 王文中 牛睿集[7] Wang Yong;Zi Feng;Lu Shanlong;Li Mingyang;Zhou Jinfeng;Yang Xiaohong;Wang Wenzhong;Niu Ruiji(Hunan University of Science and Technology,Xiangtan 411201,Hunan,China;Aerospace Information Innovation Institute,Chinese Academy of Sciences,Beijing 100101,China;International Research Center of Big Data for Sustainable Development Goals,Beijing 100094,China;University of Chinese Academy of Sciences,Beijing 100049,China;China Biodiversity Conservation and Green Development Foundation,Beijing 100035,China;Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences,Shijiazhuang 050061,Hebei,China;Kongque River Middle Reaches Management Station,Bayingoleng Administration Bureau,Tarim River Basin,Korla 841000,Xinjiang,China)

机构地区：[1]湖南科技大学地球科学与空间信息工程学院,湖南湘潭411201 [2]中国科学院空天信息创新研究院,北京100101 [3]可持续发展大数据国际研究中心,北京100094 [4]中国科学院大学,北京100049 [5]中国生物多样性保护与绿色发展基金会,北京100035 [6]中国地质科学院水文地质环境地质研究所,河北石家庄050061 [7]新疆塔里木河流域巴音郭楞管理局孔雀河中游管理站,新疆库尔勒市841000

出　　处：《地理科学》2023年第5期899-909,共11页Scientia Geographica Sinica

基　　金：中国科学院战略性先导科技专项项目(XDA19090120);第二次青藏高原综合科学考察研究项目(2019QZKK0202)资助。

摘　　要：综合利用多源遥感卫星资料,分析了1989—2019年塔里木河流域及其各水系水体面积在气候变化和生态调水影响下的年际变化趋势与各水系地表水变化对典型区域(罗布泊)地下水的影响。研究结果表明:①近30 a来,塔里木河流域地表水面积增长趋势明显;②降水是引起流域内地表水面积变化的主要气候因素,生态调水则影响着流域内地表水的空间分布格局;③流域内各水系地表水的增长变化对罗布泊地区地下水储量的恢复作用显著。对于了解塔里木河流域地表−地下水系统的长期变化规律、制定科学合理的水资源开发利用策略具有重要意义。Comprehensively using multi-source remote sensing satellite data,the interannual trends in the area of water bodies in the Tarim River Basin and its various water systems from 1989 to 2019 and the impact of surface water changes of each water system on groundwater in a typical area(Lop Nur)under the influence of climate change and ecological water diversion were analyzed.The results of the study show that:1)The surface water area of the Tarim River Basin has been increasing in a significant trend the surface water area of the Tarim River Basin has been increasing significantly in the last three decades;2)Precipitation is the main climatic factor causing changes in surface water area in the basin,while ecological water transfer affects the spatial distribution pattern of surface water in the basin;3)The changes in the growth of surface water in each water system in the basin have a significant effect on the recovery of groundwater reserves in the Lop Nor area.The research results of this paper are of great significance for understanding the long-term changes of the surface-groundwater system in the Tarim River Basin and formulating a scientific and reasonable water resources development and utilization strategy.

关 键 词：地表水 地下水 气候变化 生态调水 塔里木河流域 

分 类 号：TV213.4[水利工程—水文学及水资源]