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农田沙漠化演变中土壤性状特征及其空间变异性分析
引用本文:苏永中,赵哈林,崔建垣.农田沙漠化演变中土壤性状特征及其空间变异性分析[J].土壤学报,2004,41(2):210-217.
作者姓名:苏永中  赵哈林  崔建垣
作者单位:中国科学院寒区旱区环境与工程研究所,兰州,730000
基金项目:国家重大基础研究发展规划项目“中国北方沙漠化过程及其防治研究”(G2 0 0 0 0 4870 4)资助
摘    要:应用经典统计分析和地统计学的方法 ,研究了科尔沁沙地旱作农田 30 0m× 90m尺度下 0~10cm土层土壤理化性状的沙漠化演变及其空间变异性特征。结果表明 ,表层土壤的粗粒化、持水性能和孔隙分布的恶化、以及土壤养分的贫瘠化演变表征了农田沙漠化的发生和发展。在农田沙漠化演变中 ,土壤性状的变异增大 ,变异系数在 5 .9%~ 5 0 .7% ,其空间分布在研究的尺度上有明显的规律性 ,存在明显的空间异质性和格局。变异函数很好地反映了沙漠化演变的趋势、程度和尺度。在研究区域 ,沙漠化发生发展的尺度在南北两个方向从农田边缘到农田中部约 10 0m处。土壤性状之间及其各因子的空间异质性有密切的关系。沙漠化对土壤有机碳和氮磷养分影响显著 ,对pH影响相对较小

关 键 词:土壤性状  空间异质性  半方差函数  旱作农田  沙漠化
收稿时间:2002/8/24 0:00:00
修稿时间:2003/3/20 0:00:00

SPATIAL HETEROGENEITY OF SOIL PROPERTIES IN THE DESERTIFICATION PROCESS OF RAINFED FARMLAND IN HORQIN SANDY LAND
Su Yongzhong,Zhao Halin and Cui Jianyuan.SPATIAL HETEROGENEITY OF SOIL PROPERTIES IN THE DESERTIFICATION PROCESS OF RAINFED FARMLAND IN HORQIN SANDY LAND[J].Acta Pedologica Sinica,2004,41(2):210-217.
Authors:Su Yongzhong  Zhao Halin and Cui Jianyuan
Affiliation:Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Abstract:This study was carried out to examine the changes of soil physical and chemical properties and their spatial he-t erogeneity on the rainfed farmland of Horqin Sandy Land in the desertification process using methods of classical stat istics and geostatistics. Sixty soil samples of 0~10 cm layer were taken on the 300 m×90 m scale. The data were analyzed geostatist ically to determine the degree and nature of spatial heterogeneity. The results showed that soil part icle size distribution develop towards being coarse, soil waterholding capacity and porosity distribution deteriorated, and soil organic C and N, P nutrients depleted in the desertification process. The variability of soil parameters increased and the coefficient of variation ranged from 5.9% (bulk density) to 50.7% (organic carbon). Geostatistical analysis revealed that there are clearly regular changes in the pattern of distribution and high degree of spat ial variability in soil properties in the desertification of the farmland. Semivariograms and its model well reflected the degree and spatial scale of the development of desertification. In the studied area, the strip of land, where desertification developed inside the edges of the farmland along the longitudinal direction was about 100 m wide. There were close relationships between soil properties and between semivariograms of soil properties, except for pH. Desertification had very significant effect on soil organic carbon and nutrients, whereas, its effect on soil pH was relatively small.
Keywords:Soil properties  Spatial heterogeneity  Semivariogram  Rainfed farmland  Desertification process
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