雅鲁藏布江中游河谷区域风沙化土地演变趋势及驱动因素

    Evolution and Causes of Aeolian Desertification of the Middle Reaches of Yarlung Zangbo River,China

    • 摘要: 以雅鲁藏布江(简称雅江)中游河谷区域为研究区,运用RS和GIS技术,对近18a(1990—2008年)来该区域风沙化土地的发展趋势进行了研究。结果表明,1990—2008年雅江中游河岸及山坡风沙化土地面积增长5267hm2,目前总面积达81842hm2,其中1990—2000年增长3085hm2,年均增长308hm2;2000—2008年增长2182hm2,年均增长273hm2,与前10a相比有所下降。风力吹蚀作用是河谷地区风沙化土地发展、蔓延的主要驱动因素。2000年以后降水量的增加以及雅江日喀则和山南段开展的大规模人工造林是风沙化土地增长速度减缓的主要原因。

       

      Abstract: A study was carried out on development of aeolian desertification in the valley of the middle reaches of Yarlung Zangbo River in the past 18 years(1990-2008) with the aid of RS and GIS technologies.It was found that the area of aeolian desertified lands in this region increased by 5 267 hm2 from 1990 to 2008,and the total area of aeolian desertified land reached to 81 842 hm2 in 2008.In the first 10 years(1990-2000),it increased by 3 085 hm2 averaging by 308 hm2 annually and in the next 8 years(2000-2008) by 2 182 hm2averaging by 273 hm2 annually.Obviously,the rate slowed down in expansion in the late years.Wind erosion is the main driving factor of aeolian desertification in this region,and increased precipitation and large scaled afforestation in Xigaze and the southern section of the mountains beginning from 2000 are the main reasons for the slowed down aeolian desertification rate.

       

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