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首页> 外文期刊>Moscow University Soil Science Bulletin >PHYSICS OF SOILSPHYSICAL PROPERTIES OF SODDY-PODZOLIC SOIL IN THE PROCESS OF ITS CULTIVATION
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PHYSICS OF SOILSPHYSICAL PROPERTIES OF SODDY-PODZOLIC SOIL IN THE PROCESS OF ITS CULTIVATION

机译:耕作过程中土壤-土壤的土壤物理性质

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摘要

Liming and liberal application of mineral fertilizers aimed at improving soil fertility change the chemical, physicochemical, and biological processes in soils. Cations and anions applied with fertilizers primarily affect the composition of soil solution, interact with the surface of soil particles, and thus change the composition and properties of the soil exchange complex SEC. Liming not only neutralizes acids, but also increases the content of calcium an essential nutrient and colloid coagulator in soil solution. All these changes occurring at the molecular-ionic level affect the composition and properties of the solid soil phase at the levels of elementary soil particles and soil aggregates [1-4].The aim of this work was to study the effectof liming and mineral fertilization on the structure and related physical and water-physical properties of soddy-podzolic soil and to monitor changes in the physical properties of soddy-podzolic soil after the cessation of liming and fertilization.
机译:旨在提高土壤肥力的石灰和自由施用矿物肥料会改变土壤中的化学,物理化学和生物过程。施用肥料的阳离子和阴离子主要影响土壤溶液的组成,与土壤颗粒的表面相互作用,从而改变土壤交换复合物SEC的组成和性质。石灰化不仅可以中和酸,还可以增加土壤溶液中必需营养物和胶体凝结剂钙的含量。在分子离子水平上发生的所有这些变化都会在基本土壤颗粒和土壤团聚体水平上影响固相的组成和性质[1-4]。这项工作的目的是研究石灰和矿物肥料的作用。研究了土壤肥沃土壤的结构及相关的物理和水物理性质,并监测了停止施肥和施肥后土壤肥沃土壤的物理性质的变化。

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