1. 中国科学院新疆生态与地理研究所,新疆,乌鲁木齐,830011
2. 中国科学院大学,北京,100049
纸质出版:2013
移动端阅览
闫俊杰, 乔木, 田长彦, 等. 新疆典型绿洲阜康地区土地利用/覆被及景观格局变化分析[J]. 水土保持通报, 2013,32(1):139-145.
YAN Jun-jie, QIAO Mu, TIAN Chang-yan, et al. Changes of Land Use/Cover and Landscape Pattern in Typical Oasis of Fukang Area in Xinjiang Wei Autonomous Region[J]. Bulletin of Soiland Water Conservation, 2013, 32(1): 139-145.
闫俊杰, 乔木, 田长彦, 等. 新疆典型绿洲阜康地区土地利用/覆被及景观格局变化分析[J]. 水土保持通报, 2013,32(1):139-145. DOI:
YAN Jun-jie, QIAO Mu, TIAN Chang-yan, et al. Changes of Land Use/Cover and Landscape Pattern in Typical Oasis of Fukang Area in Xinjiang Wei Autonomous Region[J]. Bulletin of Soiland Water Conservation, 2013, 32(1): 139-145. DOI:
利用1977
1990和2006年的3期遥感影像
将GIS及景观生态学的分析方法相结合
对新疆阜康地区1977—2006年土地利用/覆被和景观格局变化进行了分析。结果表明:(1)研究区土地利用/覆被变化显著
耕地和建设用地持续增加
林地、草地、水域、盐碱和未利用土地逐步减少
且有明显加快的趋势;耕地增加主要来源于草地和盐碱地
建设用地主要来源于耕地、草地及未利用土地。(2)在类型水平上
耕地、建设用地和未利用土地连通性增强
优势度增加;林地、水域和盐碱地斑块趋于均匀而分离
破碎度增加
连通性降低;草地形状趋于规则
破碎度增加
但连通性变化不大;沙地几乎没有变化。在景观水平上
景观整体异质性增强
表现出多样化和均匀化的发展趋势。(3)驱动力分析表明
气温对水域
降水对草地影响较大
但人为因素是主要驱动因素
其中人口增加是直接动力
政策环境的改善及产业结构的调整加快了土地利用的变化速度。
Using remote sensing data collected in the years of 1977
1999and 2007
and integrating GIS with analytical methods of landscape ecology
research on changes of land use/cover and landscape pattern of Fukang area in Xinjiang Wei Autonomous Region from 1977to 2006was conducted.The results indicate that:(1)Significant changesin land use/cover have taken place in Fukang area from 1977to 2006.Farmland and construction land increased continually
while the area of forestland
grassland
water land
and salinized land decreased accordingly
and stillthe rate was accelerating.Increase in farmland was mainly from grass land and salinized land
while increasein construction land was mainly from farmland
grass land and unused land.(2)At the class level
spatialconnectedness and landscape dominance of farmland
construction land and unused land increased gradually.Patches of forest
water land and salinized land became more separated
broken and evenly distributed thanbefore and their spatial connectedness decreased.Patches of grassland tended to be more regular and fragmented
but its spatial connectedness hardly changed.Patches of sandlot hardly changed.At the landscapelevel
the heterogeneity of the whole landscape increased in general
and the landscape was evolving in the direction of diversity and evenness.(3)The analysis of driving forces show that:though temperature and precipitation has comparatively large impact upon water land and grassland respectively
anthropogenic factorswere the main driving forces
among which
increase in population was the direct driving force
and improveson policies and industrial structure accelerated the rate of changes of the land use.
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