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近百年鄱阳湖湿地格局演变研究
引用本文:李冰,万荣荣,杨桂山,谭志强,王殿常,吴兴华.近百年鄱阳湖湿地格局演变研究[J].湖泊科学,2022,34(3):1018-1029.
作者姓名:李冰  万荣荣  杨桂山  谭志强  王殿常  吴兴华
作者单位:中国科学院南京地理与湖泊研究所,中国科学院流域地理学实验室,南京210008;中国科学院大学,北京100049,中国长江三峡集团有限公司,北京100038
基金项目:国家自然科学基金项目(42071146,U2240219,41801092)和中国长江三峡集团有限公司项目(201903144)联合资助.
摘    要:鄱阳湖是我国最大淡水湖和长江中游仅存的两个通江湖泊之一,重建其近百年自然通江的湖泊湿地演变过程,对于鄱阳湖湿地生态修复与保护具有重要意义.本研究基于两期历史时期地形图和遥感产品,构建了 1930s、1970s、1990s、2000s和2010s鄱阳湖湿地格局变化数据集,探究了土地利用方式改变和水文连通变化对鄱阳湖湿地变...

关 键 词:鄱阳湖  湖泊湿地  近百年  格局变化  水文连通性
收稿时间:2021/8/9 0:00:00
修稿时间:2021/9/22 0:00:00

Investigating spatiotemporal dynamics of Lake Poyang wetland for the recent century
Li Bing,Wan Rongrong,Yang Guishan,Tan Zhiqiang,Wang Dianchang,Wu Xinghua.Investigating spatiotemporal dynamics of Lake Poyang wetland for the recent century[J].Journal of Lake Science,2022,34(3):1018-1029.
Authors:Li Bing  Wan Rongrong  Yang Guishan  Tan Zhiqiang  Wang Dianchang  Wu Xinghua
Institution:Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, P. R. China;University of Chinese Academy of Sciences, Beijing 100049, P. R. China;China Three Gorges Corporation, Beijing 100038, P. R. China
Abstract:Lake Poyang is the largest freshwater lake in China and one of the two remaining lakes freely connected with the Yangtze River in the middle reaches of the Yangtze River. Reconstruction of the spatiotemporal dynamics of the lake-wetland that are freely connected with the Yangtze River for the recent century is of great significance for Lake Poyang wetland restoration and protection and ecosystem services promotion. The present study used two periods of historic topographic maps and remote sensing products to reconstruct the Yangtze connected lake-wetland dynamics database covering the 1930s, 1970s, 1990s, 2000s and 2010s. Impacts of land use changes as well as hydrological connectivity changes on lake-wetland dynamics were explored. Results showed that Lake Poyang wetland area decreased from 5024.3 km2 in the 1930s to 3232.7 km2 in the 2010s, with a loss rate of 35.7%, of which most of the loss occurred between the 1930s and 1970s, with a loss rate of 33.2%. The lake-wetland loss is mainly distributed in the tail of Gan and Rao Rivers and the Kangshan polder. Moreover, a total of 1149.6 km2 of lake-wetland has been converted into cultivated land due to reclamation since the 1930s, which is the main land use change type of lake-wetland. In addition, compared with the 1930s, a total of 683.4 km2 lake-wetland was separated from the main lake, from which the hydrological rhythm was independent since then. The geostatistical hydrological connectivity curve of different historic periods also indicated that both the horizontal and longitudinal hydrological connectivity decreased for certain extent for the past century and remained relative stable since the 1990s. This study could provide reference states and data basis for the ecological restoration and ecosystem service promotion of Lake Poyang and even for the middle reaches of the Yangtze River.
Keywords:Lake Poyang|lake-wetland|recent century|spatiotemporal dynamics|hydrological connectivity
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