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Dependence of the aggregate swelling parameters in soddy-podzolic soils on their properties.

机译:坡沙质土壤中总溶胀参数对其性能的依赖。

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The degree and rate of the aggregate swelling in loamy sandy, loamy, and clayey soddy-podzolic soils of northwestern Russia have been measured using the methods of image analysis. The results of the study have shown that the degree of swelling of the soil aggregates depended on the proportions of the fine (0.005 mm) and sandy fractions, and the rate of the swelling depended on the density of the soil solid phase. A reliable effect of the soil organic matter content on the swelling rate of the studied objects has been established. The aggregates of the arable soddy-podzolic soils with the highest content of organic matter, as well as the aggregates of the native soils, have been characterized by the lowest swelling rates. A method has been developed for the determination of the swelling rate of soil aggregates that has enabled the assessment of the soil structure. The regression dependences of the degree and rate of the aggregate swelling on the properties and composition of soddy-podzolic soils have been plotted.Notes Translated from Pochvovedenie (2013) 5, 603-611 (Ru).
机译:使用图像分析方法测量了俄罗斯西北部的壤质沙质,壤质和粘质的坡积土中聚集体的溶胀程度和速率。研究结果表明,土壤团聚体的溶胀程度取决于细颗粒(0.005 mm)和沙质部分的比例,溶胀速率取决于土壤固相的密度。建立了土壤有机质含量对研究对象溶胀率的可靠影响。具有最高有机质含量的可耕田土壤土壤的团聚体和天然土壤的团聚体具有最低的溶胀率。已经开发出一种用于确定土壤团聚体的溶胀率的方法,该方法使得能够评估土壤结构。绘制了骨料膨胀程度和速率对泥质-坡地土壤性质和组成的回归依赖关系。注释译自Pochvovedenie(2013)5,5,603-611(Ru)。

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