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Article
Water-Extractable Organic Matter of the Soils with Different Degrees of Erosion and Sedimentation in a Small Catchment in the Central Forest-Steppe of the Central Russian Upland: Soil Sediments on the Dry Valley Bottom
The composition of the water-extractable organic matter (WEOM) of sedimented soils, namely, dark-humus water-accumulative stratozems (Fluvic Chernic Phaeozems (Loamic, Pachic)) in the nonplowed bottom of a dry...
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Article
Water-Extractable Organic Matter of Soils with Different Degrees of Erosion-Induced Degradation and Sedimentation in a Small Catchment in the Central Forest-Steppe Part of the Central Russian Upland: Tilled Soils
Dissolved organic matter is the most mobile part of soil organic matter; however, its change and transformation occurring during soil erosion are insufficiently studied. We assess the optical properties of wat...
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Article
Dissolved Organic Matter of Chernozems of Different Use: the Relationship of Structural Features and Mineral Composition
Structural peculiarities of the organic component of dissolved organic matter (DOM) of typical chernozems (Protocalcic Chernozem), differing in the principal direction of soil organic matter transformation (ac...
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Article
Effect of Polyelectrolytes on Soil Organic Matter in Model Experiments
The influence of polyelectrolyte-based soil conditioners on the qualitative and quantitative composition of soil organic matter (SOM) was studied for two soils: sandy Dystric Arenosol (Aric) with 1% of C and s...
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Article
Heterogeneity of Organic Matter of Aggregates of Protocalcic Chernozems
Layers were step-by-step removed from macroaggregates (2–1 mm in diameter) of Protocalcic Chernozems via successive abrasion in a revolving rotator during 5, 10, 15, and 39 h. During processing, the aggregates...