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张承水源涵养区土地利用演变及产水量的响应

Land Use Evolution and Water Yield Response in Zhangcheng Water Source Conservation Area

  • 摘要: 密云水库上游流域张承地区作为密云水库的水源涵养区,担负着向北京市提供饮用水源的重要任务,研究其水源供给服务对实现区域高质量发展和保障首都的水生态安全具有重要意义。通过遥感解译分析了张承水源涵养区2000-2019年的土地利用变化情况,在此基础上,基于InVEST产水模型,从空间上定量评估了2000-2019年研究区的产水量分布及变化情况,并借助情景分析探讨产水量变化与土地利用演变之间关系。结果表明:(1)2000-2019年,研究区土地利用整体呈现耕地面积减少,林地、草地、建设用地不断增加的特点;(2)2000年、2010年和2019年研究区的总产水量分别为2.61、3.46和2.71亿m3,不同时期的产水量表现出空间异质性,整体变化趋势为产水量由西高东低逐渐变为东高西低;(3)研究区不同土地利用类型平均产水深度从大到小依次为:建设用地、裸地、水域、耕地、林地、草地,在蒸散系数不变的情况下,土地利用由产水能力低的地类转为产水能力高的地类会造成区域产水量的增加,反之减少。

     

    Abstract: As the water source conservation area of Miyun Reservoir,Zhangcheng Area in the upper reaches of Miyun Reservoir bears the important task of providing drinking water to Beijing.The study of water supply service in Zhangcheng Water Source Conservation Area is of great significance to the high-quality development and ensuring the water ecological security of the capital. Based on the remote sensing the land use change in Zhangcheng Water Conservation Area were interpreted and analyzed from 2000 to 2019. Based on the InVEST water yield model the spatial distribution and change of water yield in the study area from 2000 to 2019 were quantitatively evaluated,and the relationship between water yield change and land use evolution was discussed by using scenario analysis.The results show that :(1) From 2000 to2019,the overall land use in the study area was characterized by the decrease in plow land,and the increase in forest land,grassland and construction land.(2)The total water yield of the study area in 2000,2010 and 2019 was 2.61,3.46 and 2.71 million m3.The water yield in different periods showed spatial heterogeneity,which changed gradually from high in the west and low in the east into high in the east and low in the west.(3) The average depth of water yield of different land use types in the study area from large to small is:construction land,bare land,water area,plow land,forest land and grass land. When the evapotranspiration coefficient remains unchanged,the change of land use from land type with low water yield capacity to land type with high water yield capacity will lead to an increase in regional water yields,and vice versa.

     

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