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国土资源遥感  2014, Vol. 26 Issue (2): 170-176    DOI: 10.6046/gtzyyg.2014.02.27
  技术应用 本期目录 | 过刊浏览 | 高级检索 |
近30年长江中下游平原典型区耕地覆盖变化
常潇1,2, 肖鹏峰1,2, 冯学智1,2, 张学良1,2, 杨永可1,2, 冯威丁1,2
1. 南京大学地理信息科学系, 南京 210023;
2. 南京大学江苏省地理信息技术重点实验室, 南京 210023
Change of cropland in typical area of Middle-Lower Yangtze Plain over the past 30 years
CHANG Xiao1,2, XIAO Pengfeng1,2, FENG Xuezhi1,2, ZHANG Xueliang1,2, YANG Yongke1,2, FENG Weiding1,2
1. Department of Geographical Information Science, Nanjing University, Nanjing 210023, China;
2. Jiangsu Key Laboratory of Geographic Information Science and Technology, Nanjing University, Nanjing 210023, China
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摘要 以长江中下游平原苏皖边界的10个县市为研究区,利用1984,1990,1995,2000,2005和2010年6期的TM/ETM+图像提取土地覆盖信息,从时间和空间2个方面研究耕地覆盖变化。结果表明:1从时间变化来看,研究区近30 a耕地总体呈减少趋势,经历了快速减少、缓慢减少和急剧减少3个过程,1984—1990年、1990—2000年及2000—2010年耕地分别减少了374.10 km2,66.09 km2及1 724.33 km2,主要表现为城镇和水体侵占耕地,但林地开垦使耕地增加;2从空间变化上看,沿江城市周围大面积耕地转变为建设用地,以1984年的南京市区、马鞍山市区和芜湖市区为主,且城镇化速度在加快;1990年以来沿石臼湖和固城湖周边地区的部分耕地转变成养殖塘,其西部地区转换较频繁;1984—2000年耕地沿山体和耕地交界处增加,2000年之后又因实施退耕还林和营造经济林而有所减少。
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关键词 高光谱光谱解混二次散射模型填图规则矿物填图    
Abstract:In order to analyze the spatial-temporal change characteristics of the cropland in typical areas of Middle- Lower Yangtze Plains from 1984 to 2010, the authors extracted the land cover information of the study area in 1984, 1990, 1995, 2000, 2005 and 2010 from Landsat TM/ETM+ images. The results show that the amount of cropland decreased over the past 30 years. There were three stages of the cropland change: Fast reduction, slow reduction, and sharp reduction. The total area of cropland loss was 374.10 km2 from 1984 to 1990. The decrease of cropland was 66.09 km2 from 1990 to 2000, and the loss speed was relatively slow. The cropland in the study area was reduced rapidly to 1 724.33 km2 from 2000 to 2010. Most of the lost cropland was transformed into the construction land, and the cropland in cities along the Yangtze River, such as Nanjing, Maanshan, and Wuhu, was decreased more seriously than that in counties. The speed of urbanization was accelerated. Moreover, plenty of cropland was turned into ponds to breed fish and crabs around the Shijiu Lake and the Gucheng Lake, particularly in western regions where the conversion was prominently frequent from 1990. On the other hand, cropland was increased along the boundary of cropland and mountain from 1984 to 2000. After that, the cropland decreased because of the implementation of returning cropland to forest and creating economic forest.
Key wordshyperspectral imagery    spectral unmixing    secondary scattering model    mapping rules    mineral mapping
收稿日期: 2013-03-10      出版日期: 2014-03-28
:  TP79  
基金资助:国家973计划项目“全球变化研究”(编号:2011CB952001)资助。
作者简介: 常潇(1988- ),女,硕士研究生,主要从事资源遥感方面的研究。Email:ziyuanhuayu@gmail.com。
引用本文:   
常潇, 肖鹏峰, 冯学智, 张学良, 杨永可, 冯威丁. 近30年长江中下游平原典型区耕地覆盖变化[J]. 国土资源遥感, 2014, 26(2): 170-176.
CHANG Xiao, XIAO Pengfeng, FENG Xuezhi, ZHANG Xueliang, YANG Yongke, FENG Weiding. Change of cropland in typical area of Middle-Lower Yangtze Plain over the past 30 years. REMOTE SENSING FOR LAND & RESOURCES, 2014, 26(2): 170-176.
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https://www.gtzyyg.com/CN/10.6046/gtzyyg.2014.02.27      或      https://www.gtzyyg.com/CN/Y2014/V26/I2/170
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