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The vertical distribution of soil organic matter predicted by a simple continuous model of soil organic matter transformationsNew modification of the simple continuous model of soil organic matter (SOM) transformation

An elementary multistage discrete model of soil organic matter transformations with a continuous scale of stabilityThe proposed elementary mathematical model of formation and decomposition of soil organic matter

The possibility of use research methods of soil organic matter for assess the biochar properties materials (10 samples) used the method of stepwise oxidation of soil organic matter (SOM) and methods

Some peculiarities of arable soil organic matter detection using optical remote sensing data of rainfall on the success of soil organic matter (SOM) content (% by mass) detection and mapping based

Effect of organic matter on the sorption activity of heavy loamy soils for volatile organic compounds under low moisture conditions sites on soil minerals by organic matter. At moisture contents above 5–6%, the effect of the soil

Effects of biotic and abiotic factors on soil organic matter mineralization: Experiments and structural modeling analysis
© 2017 Elsevier Masson SAS Soil organic matter (SOM) mineralization is affected by various abiotic

The possibility of use research methods of soil organic matter for assess the biochar properties materials (10 samples) used the method of stepwise oxidation of soil organic matter (SOM) and methods

Effect of plant communities on aggregate composition and organic matter stabilisation in young soils kg−1 soil). Conclusions: Particulate organic matter explains most of the differences in organic C

Perspectives in soil organic carbon storage: from a global perspective to the possibilities of landscapesThe features of the deposition of soil organic carbon on the national and regional scale

Effect of organic matter on the sorption activity of heavy loamy soils for volatile organic compounds under low moisture conditions sites on soil minerals by organic matter. At moisture contents above 5–6%, the effect of the soil

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