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The study on dynamic changes of desertification in Ganjiahu Wetland edge

机译:甘家湖湿地边缘荒漠化动态变化研究。

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The data source of which this paper used was from MSS image in 1972, TM images in 1999, 2000 and 2008, analyzed area change of desertification types, matrix of area transfer, dynamic degree, changes of state index and so on at Ganjiahu wetland edge from 1972–2008. The results showed that: during the past 36 years, the area of desertification increased gradually; the largest area changing was water area into grassland, followed by grassland into sandy area and woodland into sandy area, It showed that the land desertification was growing; The average rate of annual change of desertification was relatively large, the growth rate of sandy area was the larges(19.4%), followed by grass growth rate 3.07%; the state index calculations of desertification types showed that the state index of sandy area and saline was positive with the trend of increasing size, the state indexes of woodland, grassland, water area were negative with the trend of downsizing size.
机译:本文使用的数据源分别来自1972年的MSS图像,1999年,2000年和2008年的TM图像,分析了甘家湖湿地边缘的荒漠化类型的面积变化,面积转移矩阵,动态度,状态指数的变化等。从1972年到2008年。结果表明:在过去的36年中,荒漠化面积逐渐增加;变化最大的区域是水域进入草地,其次是草地进入沙地,林地进入沙地,表明土地沙漠化正在加剧。荒漠化的年平均变化率比较大,沙地的增长率最大(19.4%),其次是草木的增长率3.07%。荒漠化类型的状态指数计算结果表明,沙化和盐分的状态指数呈正向,随规模增大的趋势;林地,草地,水域的状态指数呈负向,随尺寸减小的趋势。

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