石灰性土壤有机矿质复合体及其团聚性研究
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STUDIES ON PROPERTIES OF ORGANO-MINERAL COMPLEX AND AGGREGATE IN CALCAREOUS SOILS
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    摘要:

    土壤有机矿质复合体是形成土壤微团聚体的基础.由于各类复合体与团聚体在土中相互掺杂,给研究分析造成极大困难,长期以来这方面的研究还处于探索阶段.本文对黄土区石灰性土壤中有机矿质复合体和团聚体的形成提出一些初步的看法,以供商榷.

    Abstract:

    Four group of water-stable microaggregate were separated from calcareous soils by means of three colloidal-dispersing methods.They are the group dispersed by sodium (GI1),the group dispersed by decalcification (GI2),the group dispersed by grinding (GII) and the group dispersed by water.The contents of humus,fulvic acid and clay mineral in these four groups showed a tendency as follows:GII>GI2>GI1Go.The content of microaggregate<10 μ in four groups is positively correlated with the contents of particles<10 μ,CaCO3 and in soil.

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杨彭年.石灰性土壤有机矿质复合体及其团聚性研究[J].土壤学报,1984,21(2):144-152. Yang Pengnian. STUDIES ON PROPERTIES OF ORGANO-MINERAL COMPLEX AND AGGREGATE IN CALCAREOUS SOILS[J]. Acta Pedologica Sinica,1984,21(2):144-152.

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  • 在线发布日期: 2013-02-25
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