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长江流域植被变化影响因素与水沙关系研究OA

Study on influencing factors of vegetation change and water-sediment relationship in Yangtze River Basin

中文摘要英文摘要

[目的]系统探讨长江流域植被变化的时空特征、主导驱动因子及其与水沙过程的耦合关系,为流域生态保护与资源管理提供科学依据.[方法]基于2001-2020年长江流域归一化植被指数(Normalized Difference Vegetation Index,NDVI)、气象数据和水沙数据,采用趋势分析、相关性分析和残差分析等方法,定量评估气候因子与人类活动对植被演变的影响,并分析了NDVI与年输沙量、年径流量之间的关系.[结果]长江流域NDVI整体呈波动上升趋势,年均增长速率为0.001 7/a.其中,中上游地区NDVI上升显著(分别为0.001 7/a和0.001 9/a),而下游区域呈显著下降趋势(-0.000 9/a).温度对植被生长的促进作用最为显著,降水和太阳辐射的影响则表现出明显的区域差异.退耕还林等生态工程显著提升了中上游地区的植被覆盖度,而城市扩张导致下游地区植被退化;植被改善显著降低了中上游年输沙量并提高了年径流量,下游水沙过程则主要受水库调控影响.[结论]长江流域植被变化具有显著的时空异质性,受气候变化和人类活动的共同驱动,生态工程有效提升了流域生态质量,并通过调节水沙过程增强了生态系统调节功能,对流域可持续发展具有重要意义.

[Objective]This study systematically investigates the spatiotemporal characteristics of vegetation change in the Yangtze River Basin,its main driving factors,and the coupling relationship with water-sediment processes,providing a scientific basis for ecological protection and resource management in the river basin.[Methods]Based on normalized difference vegetation index(NDVI),meteorological data,and water-sediment data in the Yangtze River Basin from 2001 to 2020,trend analysis,correlation analysis,and residual analysis were applied to quantitatively assess the impact of climatic factors and human activities on vegetation evolution.Additionally,the relationships between NDVI,annual sediment load,and annual runoff were analyzed.[Results]The NDVI in the Yangtze River Basin showed an overall fluctuating upward trend,with an average annual growth rate of 0.001 7/a.Among them,the middle and upper reaches demonstrated significant NDVI increases(0.001 7/a and 0.001 9/a,respectively),while a notable decline(-0.000 9/a)was observed in the lower reaches.Temperature had the most significant promoting effect on vegetation growth,while the impact of precipitation and solar radiation exhibited distinct regional differences.Ecological projects such as Grain-for-Green Program significantly improved vegetation cover in the upper and middle reaches,while urban expansion led to vegetation degradation in the lower reaches.Vegetation recovery substantially reduced annual sediment load and increased runoff in the upper and middle reaches,while water-sediment processes in the lower reaches were mainly regulated by reservoirs.[Conclusion]Vegetation changes in the Yangtze River Basin show significant spatiotemporal heterogeneity and are jointly driven by climate change and human activities.Ecological projects have effectively enhanced ecological quality and ecosystem regulatory functions through water-sediment process regulation,which is crucial for sustainable development of the river basin.

刘新波;刘旭婷;韩剑桥;李雨晨;杨磊;安日辉

中国长江电力股份有限公司,武汉 430010武汉大学,武汉 430072武汉大学,武汉 430072中国长江电力股份有限公司,武汉 430010中国长江三峡集团有限公司武汉科创园,武汉 430010中国长江三峡集团有限公司武汉科创园,武汉 430010

农业科技

植被动态气候变化人类活动水沙变化长江流域

vegetation dynamicsclimate changehuman activitieswater-sediment variationsYangtze River Basin

《水土保持研究》 2026 (2)

50-57,8

中国长江电力股份有限公司"流域水体含沙量动态遥感与输沙量变化趋势分析研究"(合同编号:Z242302046)

10.13869/j.cnki.rswc.2026.02.038

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