张哲寰, 马宏伟, 刘强, 朱巍, 张廷秀. 松嫩平原近20年土壤盐渍化动态变化及驱动力分析[J]. 地质与资源, 2007, 16(2): 120-124. DOI: 10.13686/j.cnki.dzyzy.2007.02.016
    引用本文: 张哲寰, 马宏伟, 刘强, 朱巍, 张廷秀. 松嫩平原近20年土壤盐渍化动态变化及驱动力分析[J]. 地质与资源, 2007, 16(2): 120-124. DOI: 10.13686/j.cnki.dzyzy.2007.02.016
    ZHANG Zhe-huan, MA Hong-wei, LIU Qiang, ZHU Wei, ZHANG Ting-xiu. DEVELOPMENT AND DRIVES OF LAND SALINIZATION IN SONGNEN PLAIN[J]. Geology and Resources, 2007, 16(2): 120-124. DOI: 10.13686/j.cnki.dzyzy.2007.02.016
    Citation: ZHANG Zhe-huan, MA Hong-wei, LIU Qiang, ZHU Wei, ZHANG Ting-xiu. DEVELOPMENT AND DRIVES OF LAND SALINIZATION IN SONGNEN PLAIN[J]. Geology and Resources, 2007, 16(2): 120-124. DOI: 10.13686/j.cnki.dzyzy.2007.02.016

    松嫩平原近20年土壤盐渍化动态变化及驱动力分析

    DEVELOPMENT AND DRIVES OF LAND SALINIZATION IN SONGNEN PLAIN

    • 摘要: 利用1986年(TM)和2001年(ETM)卫星遥感影像数据和RS-GIS集成技术,对松嫩平原盐渍化土地的现状、程度和发展趋势进行了量化分析.结果表明,这15年中,松嫩平原盐碱地面积增加了21.7112×104 hm2,每年增加1.45×104 hm2,年平均增长率为1.4%.其中轻度盐渍化土地增加8812 hm2,年平均增长0.16%;中度盐渍化土地增加3.8306×104 hm2,年平均增长0.64%;重度盐渍化土地面积增加了16.9994×104 hm2,年平均增长了4.2%.气候变暖,降水减少,人为活动增强是盐渍化程度加重的主要驱动力.

       

      Abstract: Landsat TM (ETM) images acquired in 1986 and 2001 and the RS-GIS integrated technique are adopted to quantitatively analyze the present situation, degrees and developing trend of salinized-alkalized land in Songnen plain. It is concluded that, during the 15 years, the area of salinized land has increased 21.7112×104 hm2, averagety 1.45×104 hm2 per annum, with average annual increase rate of 1.4%. Among them, the salinized areas in light-degree, mediate-degree and heavy-degree have increased respectively by 0.8812×104 hm2, 3.8306×104 hm2 and 16.9994×104 hm2, with average annual increase rate of 0.16%, 0.64% and 4.2% respectively. The main drives for the increase of salinization are the warming climate, reduced precipitation and increased human activities.

       

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