基于InVEST模型的白龙江流域水源供给服务时空分异
甘肃白龙江流域是我国嘉陵江上游水资源重要的补给地之一,对其开展流域生态系统水源供给服务功能空间定量评估研究,有利于水源区保护规划的制定和生态补偿机制的建立。论文基于研究区土地利用数据、气象、土壤和野外观测数据等,应用InVEST模型水源供给模块估算白龙江流域生态系统的水源供给量,并定量分析流域水源供给服务的空间分布特征及不同地形因子的影响。结果表明:白龙江流域生态系统水源平均供给量约在388 mm左右,且存在一定的空间异质性;中部干热河谷区域水源供给量相对较小,东南部山地林区降雨量大,水源供给量较高,林地(如云冷杉类、针叶林类等)和农田水源供给量较高。流域内水源供给量随海拔高度和坡度的增加呈现...
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| Published in | 自然资源学报 Vol. 32; no. 8; pp. 1337 - 1347 |
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| Main Author | |
| Format | Journal Article |
| Language | Chinese |
| Published |
广西师范学院北部湾环境演变与资源利用教育部重点实验室,南宁530001
2017
广西师范学院广西地表过程与智能模拟重点实验室,南宁530001 兰州大学资源环境学院西部环境教育部重点实验室,兰州730000%兰州大学资源环境学院西部环境教育部重点实验室,兰州,730000%广西师范学院北部湾环境演变与资源利用教育部重点实验室,南宁530001 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1000-3037 |
| DOI | 10.11849/zrzyxb.20160799 |
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| Summary: | 甘肃白龙江流域是我国嘉陵江上游水资源重要的补给地之一,对其开展流域生态系统水源供给服务功能空间定量评估研究,有利于水源区保护规划的制定和生态补偿机制的建立。论文基于研究区土地利用数据、气象、土壤和野外观测数据等,应用InVEST模型水源供给模块估算白龙江流域生态系统的水源供给量,并定量分析流域水源供给服务的空间分布特征及不同地形因子的影响。结果表明:白龙江流域生态系统水源平均供给量约在388 mm左右,且存在一定的空间异质性;中部干热河谷区域水源供给量相对较小,东南部山地林区降雨量大,水源供给量较高,林地(如云冷杉类、针叶林类等)和农田水源供给量较高。流域内水源供给量随海拔高度和坡度的增加呈现先增加后减小的趋势,其高值区主要分布在1 500~3 500 m和15°~40°区段;阴坡区域水源供给量大于阳坡区域。 |
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| Bibliography: | Water supply service is not only an essential ecosystem service for supporting human well-being, but also a hot topic in ecology and hydrology. The quantitative assessment and mapping of spatiotemporal variation of water supply service have important significance for water conservation planning, water management and establishment of ecological compensation mechanism in the water source areas. Bailong River Watershed(BRW), a vital ecological function region of water supply and conservation in the upper Yangtze River, locates in the transitional ecotone of the Loess Plateau, Qinba Mountains and Tibet Plateau. Based on In VEST model simulations, RS, GIS spatial analysis, field observation and survey, BRW was selected as a case to estimate water supply service and analyze the impact of vegetation types,elevation, slope, slope direction on the spatiotemporal pattern of water supply service.Moreover, the reference factors and data, such as land use, meteorology(eg. precipitation,evapotranspiration), soil and the DE |
| ISSN: | 1000-3037 |
| DOI: | 10.11849/zrzyxb.20160799 |