Composition and hydrophobic properties of organic matter in the densimetric fractions of soils from the Subpolar Urals
Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools...
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Published in | Eurasian soil science Vol. 48; no. 11; pp. 1212 - 1221 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
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Pleiades Publishing
01.11.2015
Springer Springer Nature B.V |
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Abstract | Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HF₁ characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88° among the soil horizons and from 22 to 137° among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. |
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AbstractList | Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HF
1
characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88° among the soil horizons and from 22 to 137° among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HFi characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88[degrees] among the soil horizons and from 22 to 137[degrees] among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. Keywords: mountain soils, Yugyd Va, organic carbon, contact wetting angle, WRB DOI: 10.1134/S1064229315110058 Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HF₁ characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88° among the soil horizons and from 22 to 137° among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HF sub(1) characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88 degree among the soil horizons and from 22 to 137 degree among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. Organic matter features in the upper mineral horizons have been studied for four soils in the Subpolar Urals: humus-illuvial podbur (Entic Podzol), gleyic humus-illuvial podbur (Stagnic Entic Podzol), iron-illuvial podzol (Albic Podzol), and eluviated burozem (Leptic Cambisol). Organic matter pools have been separated by densimetric fractionation. The concentrations of carbon and nitrogen and the relative contributions of separate densimetric fractions to the total content of elements in the upper soil horizons reflect the genetic features of formation of the studied soils. The saturation of organic matter with nitrogen increases with increasing density of the fractions. The proportion of heavy fraction HF^sub 1^ characterized by a high content of fine silt particles increases in the upper horizons of podburs (Entic Podzol, Stagnic Entic Podzol) and burozem (Leptic Cambisol). The contact wetting angles, which characterize the hydrophobic properties of soils, have been determined for the densimetric fractions and horizons of gleyic humus-illuvial podbur (Stagnic Entic Podzol) and iron-illuvial podzol (Albic Podzol). These values vary from 60 to 88° among the soil horizons and from 22 to 137° among the densimetric fractions. It has been found that the hydrophobic properties of the studied soil horizons are largely determined by the contents of free and occluded organic matter fractions. |
Audience | Academic |
Author | Dymov, A. A Milanovskii, E. Yu Kholodov, V. A |
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CitedBy_id | crossref_primary_10_1016_j_geoderma_2019_114006 crossref_primary_10_19047_0136_1694_2021_106_49_76 crossref_primary_10_1515_johh_2017_0058 crossref_primary_10_1016_j_still_2024_106141 crossref_primary_10_1134_S1064229322030152 crossref_primary_10_1134_S1064229323601154 crossref_primary_10_1134_S1064229320100129 crossref_primary_10_1134_S1064229323700229 crossref_primary_10_1134_S1064229319040136 crossref_primary_10_1134_S1064229317070080 crossref_primary_10_1134_S1064229323603669 |
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SubjectTerms | Analysis Cambisols carbon contact angle Decomposing organic matter Earth and Environmental Science Earth Sciences Fractionation Geotechnical Engineering & Applied Earth Sciences Humus hydrophobicity Matter & antimatter Nitrogen Organic chemicals organic matter particles Podzols silt Soil Chemistry Soil horizons Soil properties Soils |
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Title | Composition and hydrophobic properties of organic matter in the densimetric fractions of soils from the Subpolar Urals |
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