Effect of the Size of Elementary Soil Particles on the Soil Moisture Characteristic Curveстатья
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Дата последнего поиска статьи во внешних источниках: 19 сентября 2015 г.
Аннотация:Statistical analysis of water vapor sorption by light clayey brown forest soil and its elementary particles of different diameters has revealed relatively close correlations and linear relationships between the logarithm of total soil water potential (pressure) and the water contents in the separated particlesize fractions (due to the hydration of exchangeable cations in the diffuse layer near the surface of soil solid phase), as well as between the water content of particlesize fractions and the logarithm of their diameter (due to the differ
ences in the specific surface area and mineralogy of these particles).