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赣江三角洲形成及其演变遥感研究

Remote Sensing Research of Development and Evolution in Ganjiang Delta

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【作者】 雷天赐彭轩明陈立德祝民强

【Author】 LEI Tian-ci1,PENG Xuan-ming1,CHEN Li-de1,ZHU Min-qiang2 (1.Yichang Institute of Geology and Mineral Resources,Yichang,443003,Hubei,China;2.The Digital Land Key lab of Jiangxi Province of The East China Institute of Technology,Fuzhou,344000,Jiangxi,China)

【机构】 宜昌地质矿产研究所东华理工学院江西省数字国土重点实验室 湖北宜昌443003湖北宜昌443003江西抚州344000

【摘要】 以鄱阳湖区2个时相的M SS、TM遥感影像和1:5万地形图作为数据源,在具有最大信息量背景下,依据地物光谱、形态等影像特征对赣江河道变迁及三角洲成因进行了解译,发现河道的变迁主要表现为河流的改道和袭夺;采用人机交互式手段,利用多时相影像数据对赣江三角洲1976~1991年来演变进行了遥感动态监测,统计出15年间三角洲前缘新淤面积为37.6km2,整体淤积速度约2.5km2/a,且各部位淤积程度不一,并以中支淤积速度最快。

【Abstract】 Regarding 2-phase Remote sensing images of MSS and TM and 1:50000 relief map in Poyang Lake as data sources,the Ganjiang transition and delta evolution are interpreted in maximal information assembly based on the spectral signature and morphological character;Its was considered that river’s transition mainly manifestated its diversion and capturing stream.By the means of human-computer intesaction,making use of the remote sensing image from 1976 to 1991,the dynamic monitoring of evolution in Ganjiang Delta was carried out,the increased area in delta front was 37.6 km2 and it is pushed forward at the speed of 2.5km2/a;Each part is pushed forward at different rate and the mud filling chiefly focuses on the Ganjiang’s middle branch in delta front.

【基金】 中国地质调查局长江上游宜昌-江津段环境工程地质调查(D200602)
  • 【文献出处】 华南地质与矿产 ,Geology and Mineral Resources of South China , 编辑部邮箱 ,2007年02期
  • 【分类号】P512
  • 【被引频次】9
  • 【下载频次】370
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