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作 者:窦苗[1,2,3,4] 孙建国[1,2] 陈海鹏[1,2,3,4] DOU Miao SUN Jian-guo CHIEN Hai-peng(Faculty of Geomatics, Lanzhou Jiaotong University, Lanzhou, Gansu 730070 Gansu Provincial Engineering Laboratory for National Geographic State Monitoring, Lanzhou, Gansu 730070 Institute of Geographic Sciences and Natural Resources Research, CAS,Beijing 100101 Key Laboratory of Land Surface Pattern and Simulation, Chinese Academy of Sciences, Beijing 100101)
机构地区:[1]兰州交通大学测绘与地理信息学院,甘肃兰州730070 [2]甘肃省地理国情检测工程实验室,甘肃兰州730070 [3]中国科学院地理科学与资源研究所,北京100101 [4]中国科学院陆地表层格局与模拟重点实验室,北京100101
出 处:《安徽农业科学》2017年第21期54-58,共5页Journal of Anhui Agricultural Sciences
基 金:国家重点基础研究发展计划(973计划)(2015CB452702)
摘 要:[目的]掌握横断山区产水量及水源分布空间。[方法]利用In VEST模型评估计算2005—2014年横断山区年均产水量,分析产水量的空间分布特征及其原因。[结果]横断山区年均产水量为1 723.3亿m3,与自然径流量较为接近;产水量的空间分布总体呈现出自西北向东南递增的趋势;年均产水量及其空间分布特征与研究区土地利用/覆被类型、土壤深度、地势等因素存在密切关系。[结论]该研究可为横断山区水文过程进一步研究提供基础资料,同时为区域水资源管理提供科学依据。[ Objective ] To master water production and water distribution in Hengduan Mountains. [ Method ] Using INVEST model, the average annual water yield of Hengduan Mountains between 2005 - 2014 was evaluated and analyzed, and the spatial distribution characteristics of water production and their causes were analyzed. [ Result] The results showed that the annual average water yield was 172.33 billion m3 , which was relatively close to natural runoff. The spatial distribution of water yield showed a trend of increase from northwest to southeast in general. The annual average water yield and its spatial distribution was closely related to land use/cover type, soil depth, topography and so on. [ Conclusion ] The study can provide basic data for further study of hydrological processes in Hengduan Mountains, and provide scientific basis for regional water resources management.
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