摘要
以达拉特旗中部沙丘为研究区域,在3S技术支持下解译达拉特旗1987,1995,2000和2003年4期遥感影像,获得4个年份的沙漠化动态数据,运用滑动平均法探讨了沙漠化发展演变的动力机制。结果表明,该地区近20a来,沙漠化土地处于逆转—发展—逆转的过程中。1995—2000年间,是该地区沙漠化动态变化最大的时期,沙漠化驱动力的累加效应表明,人口数量与牲畜量对沙漠化的累加效应均很明显,且人口数量对沙漠化的累加效应要高于牲畜量;年均风速对沙漠化的累加效应在各个时间尺度均很显著,年均温在大于2a的时间尺度上对沙漠化的累加效应最明显。
The study area is located in the center of Dalate County. Based on 35 techniques and combined with ground investigation, the Land-sat TM images of 1987, 1995, 2000 and 2003 were interpreted. The changes of sandy land were analyzed by using the database of desertification dynamics from 1987 to 2003. RS and GIS softwares, such as Erdas 8.6, ArcView 3.3 and ArcInfo 7.1 were used as an interpretation tool. The cumulative impact analysis was used to find the reasons of desertification. Results showed that in the past 20 years, the desertifled lands were in the status of the reverse-development-reverse. The degree of dynamic desertification was the highest from 1995 to 2000. The analyses of natural elements and human activities with sliding average indicated that the cumulative impacts of population and livestock on desertification were significant, and the effect of population was stronger than livestock, the cumulative impacts of annual mean wind were always significant in all temporal scales. The effect of annual mean temperature was significant （at 0.01 scale ） over two years.
出处
《水土保持通报》
CSCD
北大核心
2007年第2期112-118,共7页
Bulletin of Soil and Water Conservation
基金
国家"十五"攻关项目(2002BA517A-09-05)
鲁东大学校基金(YD05008)
鲁东大学研究生创新基金(Ycx0607)
关键词
动态变化
累加效应
沙漠化
dynamic change
cumulative impact
desertification
