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Spatial distribution of sandy desertification change in the west of Jilin Province

机译:吉林省西部沙质荒漠化变化的空间分布

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The sandy land of the western part of Jilin Province is located in the ecotone of semi-humid and semi-arid area in the temperate zone of China. The sandy desertification has widely spread in the region because of the vulnerable natural conditions and the unreasonable human activity; as a result of this, the precious land resources and the economic development in the area have been seriously impacted. In this paper, the sandy land ecologic environment geographic information system is established based on the multi-spectral, multi-temporal Landsat TM images and field investigation. The comprehensive indexes of sandy desertification extent assessment which include vegetation degradation, wind erosion extent and soil depth are presented to classify the sandy land in western Jilin into three levels--slight, moderate and severe sandy desertification with the support of GIS platform. The results demonstrate that the sandy desertification has been partly controlled in the past twenty years, except some small sites. However, this doesn't necessarily mean that there is nothing for more concern. The two main causes of sandy desertification have not been eliminated yet, one is its natural factor, especially the physical and chemical characters of sandy soil and dry climate; another is the immoderate economic activity of human being that has highly accelerated the sandy desertification process.
机译:吉林省西部的沙地位于中国温带半湿半干旱的过渡带。由于脆弱的自然条件和不合理的人类活动,沙质荒漠化在该地区广泛传播;结果,该地区的宝贵土地资源和经济发展受到严重影响。本文基于多光谱,多时间的Landsat TM影像和野外调查,建立了沙地生态环境地理信息系统。提出了包括植被退化,风蚀程度和土壤深度在内的沙质荒漠化程度综合评价指标,在GIS平台的支持下,将吉林西部的沙地分为轻度,中度和重度沙化三个等级。结果表明,在过去的20年中,除一些小地方外,沙质荒漠化得到了部分控制。但是,这并不一定意味着没有什么需要更多关注的了。沙质荒漠化的两个主要原因尚未消除,其一是其自然因素,特别是沙质土壤的理化特性和干旱气候;其二是沙漠化的自然原因。另一个是人类不适当的经济活动,极大地加速了沙漠化的沙化过程。

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