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坡面侵蚀土壤化学性质对磁化率影响机理的研究
  • 期刊名称:《水土保持学报》,2008,22(2):51-53.
  • 时间:0
  • 分类:S157.1[农业科学—土壤学;农业科学—农业基础科学]
  • 作者机构:[1]山东农业大学资源与环境学院,山东泰安271018, [2]莱阳农学院资源与环境学院,山东青岛266109
  • 相关基金:国家自然科学基金(40701094);山东省教育厅科技计划项目(J07YF10).山东农业大学青年科技创新基金(23457)
  • 相关项目:土壤侵蚀磁性示踪剂的研制及其应用方法研究
中文摘要:

研究了不同侵蚀强度下土壤磁化率及其与土壤化学性质的关系,结果表明:土壤pH、有机质含量和各形态氧化铁含量均与磁化率呈正相关,且氧化铁含量与磁化率呈极显著正相关,表明土壤不同形态氧化铁含量的多少是影响坡面土壤磁化率变化的关键因素。土壤侵蚀导致坡面物质的再分布,从而使土壤pH、有机质、氧化铁含量等土壤化学性质随之发生变化,这些因素随着侵蚀的强弱而发生变化,是影响坡面侵蚀土壤磁性变化的根源。

英文摘要:

The relationship between soil susceptibility and the soil chemical characters were studied, and find out the mechanism of soil susceptibility variation with soil erosion intensity. The soil susceptibility increases with the soil erosion decreasing, and at the same time, the content of organic materials and magnetism mineral content are adding. In this study, we find the content of free ferric oxide is main reason of causing the soil susceptibility variation. The mechanism of soil susceptibility variation is that soil erosion make the soil redistribution in the slope, and the soil chemical characters changed too, at the same time and then the soil susceptibility changed too.

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