1. 南京大学地理与海洋科学学院,江苏,南京,210093
2. 福建师范大学地理科学学院,福建,福州,350007
纸质出版:2015
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杨柳, 陈兴伟, 许有鹏, 等. 东南沿海地区小流域土地利用/覆被变化的水文效应[J]. 水土保持通报, 2015,35(2):70-75.
YANG Liu, CHEN Xingwei, XU Youpeng, et al. Hydrological Responses to Land Use and Cover Change in a Small Watershed of Southeast China Coast Area[J]. Bulletin of Soiland Water Conservation, 2015, 35(2): 70-75.
杨柳, 陈兴伟, 许有鹏, 等. 东南沿海地区小流域土地利用/覆被变化的水文效应[J]. 水土保持通报, 2015,35(2):70-75. DOI: 10.13961/j.cnki.stbctb.2015.02.014.
YANG Liu, CHEN Xingwei, XU Youpeng, et al. Hydrological Responses to Land Use and Cover Change in a Small Watershed of Southeast China Coast Area[J]. Bulletin of Soiland Water Conservation, 2015, 35(2): 70-75. DOI: 10.13961/j.cnki.stbctb.2015.02.014.
[目的] 研究我国东南沿海小流域土地利用/覆被变化的水文效应
为该区水土资源合理配置和可持续发展提供科学依据。[方法] 以东南沿海福建省晋江山美水库集水区为例
运用SWAT水文模型。[结果] (1)研究区土地利用变化表现为林地转向园地和建设用地、耕地转向建设用地的特征。(2)固定其他条件
将构建的模型2006年土地利用数据替换为1995年
对比分析发现2000-2010年全流域和典型子流域的年径流深增加
洪水期平均径流增加
枯水期径流基本减少。(3)从全流域空间角度看
径流量均增大
特别是研究区西部地区和东南部地区;同时径流量变率增大
稳性减小。(4)园地、林地、建设用地和水田是驱动区内水文变化的主要因子。[结论] 研究区土地利用与覆被变化导致"洪水量更大
枯水量更小"的径流变化趋势。河川径流的变化受各地类变化的组合叠加效应影响
这种叠加效应还须进一步研究。
[Objective] Studying the hydrological responses to land use and cover change of Southeast China coast in a small watershed
in order to provide references for the rational allocation and sustainable development of water and soil resources.[Methods] The confluence catchment of Jinjiang Shanmei Reservoir in Fujian Province of China
a place located at the southeast coast of China
was selected to illustrate the effects of land use and cover change(LUCC) on hydrological processes by SWAT model.[Results] (1) From 1995 to 2006
the forest land was mainly converted to garden land and construction land
while farm land was mainly transformed to construction land; (2) In the model
if other conditions were fixed
only data of land use in 2006 was replaced with the corresponding input variable in 1995
the runoff could be outputted as contrast:from 2000 to 2010
the annual runoffs in the whole watershed and also in the tributary drainage area consequently increased; and the averaged runoff during flooding increased
while the runoff during rainless period decreased; (3) The runoff volume in the whole watershed increased with an increased variation as contrast with the previous corresponding value; (4) Garden land
forest land
construction land and paddy field were the main driving factors that caused the regional hydrological changes.[Conclusion] Land use and cover change in the study area were found to result in a runoff trend that are "the flood volume is larger
the runoff yield is smaller". The changes of river runoff was resulted from the combined effects of all types of land use change. This combination effects need to be further studied.
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