耕层土壤颗粒表面的分形维数及其与主要土壤特性的关系
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FRACTAL DIMENSIONS OF PARTICLE SURFACE IN THE PLOWED LAYERS AND THEIR RELATIONSHIPS WITH MAIN SOIL PROPERTIES
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    摘要:

    四川16个耕地表层的土壤颗粒表面分形维数D为2805~2942,其中砂土2821、壤土2870、粘壤土2916和粘土2939.统计分析表明D分别与国际制粗砂粒和细砂粒含量呈极显著负相关,与粉粒和粘粒含量呈极显著正相关;它与粉粒、粘粒和有机质含量的偏相关关系达极显著水平,与容重的偏相关关系达显著水平.

    Abstract:

    Fractal dimensions of particle surface were 2.805~2.942 in the plowed layers of 16 crop fields in Sichuan. Among them, sand soil was 2.821, loam soil 2.807, clay loam soil 2.916, and clay soil 2.939. Statistic analysis indicated that fractal dimensions were in highly significant negative correlation with the contents of coarse sand and fine sand, and in very significant positive correlation with the contents of silt and clay. In addition, in the partial correlation with the contents of silt, clay, organic matter and bulk density of soil was highly significant or significant.

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张世熔,邓良基,周倩,伍国锋.耕层土壤颗粒表面的分形维数及其与主要土壤特性的关系[J].土壤学报,2002,39(2):221-226. DOI:10.11766/trxb200006060211 Zhang Shi-rong, Deng Liang-ji, Zhou Qian, Wu Guo-feng. FRACTAL DIMENSIONS OF PARTICLE SURFACE IN THE PLOWED LAYERS AND THEIR RELATIONSHIPS WITH MAIN SOIL PROPERTIES[J]. Acta Pedologica Sinica,2002,39(2):221-226.

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  • 收稿日期:2000-06-06
  • 最后修改日期:2000-09-08
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  • 在线发布日期: 2013-02-25
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