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机构地区:[1]西南农业大学土化系
出 处:《土壤学报》1996年第1期70-77,共8页Acta Pedologica Sinica
摘 要:紫色水稻土的原土复合量(重组腐殖质)为中性土>钙质土>酸性土,同一土壤剖面中其含量是随土层深度下降;而有机无机复合度为钙质土>中性、酸性土,在土壤剖面中是随土层深度增加。<0.01mm土粒团聚量和<0.01mm土粒团聚度为钙质土>中性土>酸性土。原土复合量和有机质含量,物理性粘粒含量、铁氧化物含量与<0.01mm土粒团聚量呈显著正相关;而有机无机复合度与有机质含量呈显著负相关,与腐殖质结合状态,物理性粘粒含量和<0.01mm土粒团聚度间无显著相关性。土壤有机质在上粒团聚中,是与矿物质呈复合状态的腐殖质(原土复合量)起作用,而原上复合量的多少很大程度上决定了<0.01mm土粒团聚量。有机无机复合和土粒团聚的关系是通过原土复合量和<0.01mm土粒团聚量间的关系来体现的。The content of soil complexing in paddy soils developed from purple soils appears in the sequence of neutral soils>calcareous soils>acid soils and decreases with depth of soil layer,while the degree of organo-mineral complexing is in the order of calcareous soils>neutral and acid soils and increases with the depth of soil layer.content and degree of <0.01mm soil particle aggregation are in the sequence of calcareous soil > neutral soils>acid soils.The content of soil complexing is positively related with the contents of organic matter,physical clay,Fe oxide and <0.01mm soil particle aggregation.But the degree of organo-mineral complexing is negatively related to content of organic matter,but insigificantly related to the combined forms of humus,the content of physical clay and the degree of<0.01mm soil particle aggregation.The complexing humus with mineral(content of soil complexing) in soil organic matter plays an important role.in soil particle aggregation.The content of<0.01mm soil particle aggregation depends on the content of soil complexing to a great extent. The relationship between complexing of organo-mineral and aggregation of soil particle is reflected by the relationship between the content of soil complexing and the content of <0.01mm soil particle aggregation.
分 类 号:S152.482[农业科学—土壤学] S155.32[农业科学—农业基础科学]
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