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应用生态学报 ›› 2025, Vol. 36 ›› Issue (7): 2114-2120.doi: 10.13287/j.1001-9332.202507.024

• 研究论文 • 上一篇    下一篇

长江中下游干流安庆至芜湖河段洲滩湿地植被覆盖度变化

赵朵朵, 杨中华*, 张鹏   

  1. 武汉大学水资源工程与调度全国重点实验室, 武汉 430072
  • 收稿日期:2024-12-10 接受日期:2025-05-10 出版日期:2025-07-18 发布日期:2026-01-18
  • 通讯作者: *E-mail: yzh@whu.edu.cn
  • 作者简介:赵朵朵, 女, 2002年生, 硕士研究生。主要从事河湖生态保护研究。E-mail: zhaoduoduo@whu.edu.cn
  • 基金资助:
    国家自然科学基金项目(U2340216,52020105006)和湖北省科技创新计划重点研发专项(2023BCB110)

Changes in fractional vegetation coverage of floodplain wetlands in the Anqing-Wuhu mainstem segment of the middle and lower reaches of the Yangtze River

ZHAO Duoduo, YANG Zhonghua*, ZHANG Peng   

  1. State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China
  • Received:2024-12-10 Accepted:2025-05-10 Online:2025-07-18 Published:2026-01-18

摘要: 长江中下游安庆至芜湖干流河段是多种生物的重要栖息地,洲滩湿地的生态质量直接影响整个生态系统的稳定性。本研究基于1994—2022年间Landsat系列30 m遥感影像数据,对长江中下游安庆至芜湖干流河段洲滩湿地植被覆盖度(FVC)进行分类,通过动态度及转移矩阵方法,量化不同等级植被覆盖度的转移状况,分析其时空格局。结果表明: 研究期间,洲滩植被覆盖度以高及中高等级FVC为主,研究区FVC年均值为0.6188,年均FVC呈现先上升后下降再上升的变化趋势。1994—2004年间,高FVC区域面积下降25.7 km2,中、中低FVC分别以3.0%·a-1和2.7%·a-1的增速扩张。三峡水库运行后(2004—2015年),洲滩湿地以水体的转出、高及中高FVC转入为主,FVC综合动态度及低FVC单一动态度达到最高水平。2015—2022年间,洲滩FVC逐渐增加,以中高FVC转为高FVC为主,占总转移面积的15%。引起研究区FVC变化的主要因素包括人为开垦利用、三峡调度、长江防浪林建设和长江大保护战略实施。

关键词: 改进归一化水指数, Landsat影像, 三峡工程, 转移矩阵

Abstract: The Anqing-Wuhu mainstem segment in the middle and lower reaches of the Yangtze River serves as a critical habitat for diverse species, where the ecological quality of floodplain wetlands directly governs the stability of the entire ecosystem. Utilizing 30-meter resolution Landsat satellite imagery from 1994 to 2022, we classified the floodplain wetlands in the Anqing-Wuhu mainstem segment in the middle and lower reaches of the Yangtze River using fractional vegetation coverage (FVC). Through dynamic degree analysis and transition matrices method, we quantified vegetation cover transitions across different FVC tiers and analyzed their spatiotemporal variations. The results showed that vegetation coverage of the floodplain was mainly at high and medium-high levels of FVC, with an average annual FVC value of 0.6188. The average annual FVC showed an “increase-decrease-increase” trend. During 1994-2004, high-FVC areas decreased by 25.7 km2, while medium and medium-low FVC zones expanded at annual rates of 3.0%·a-1 and 2.7%·a-1, respectively. After the operation of the Three Gorges Reservoir (2004-2015), floodplain dynamics were dominated by the outflow of water, as well as the inflow of high and medium-high FVC, with both comprehensive FVC dynamic degree and single dynamic degree of low FVC reaching peak during this period. During 2015-2022, FVC exhibited gradual recovery, primarily through medium-high to high FVC transitions, accounting for 15% of total transferred areas. Key drivers of FVC change in the study area included anthropogenic reclamation, Three Gorges flow regulation, riparian shelterbelt construction of Yangtze River, and implementation of the Yangtze River conservation strategy.

Key words: modified normalized difference water index, Landsat image, Three Gorges Project, transition matrix