2022
DOI: 10.1134/s1064229322070031
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Organic Matter and Physical Properties of Postagrogenic Eroded Soddy-Podzolic Soil and Arable Soddy-Podzolic Soil

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Cited by 6 publications
(6 citation statements)
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“…Indicators of the intensity of processes of mineralization of nitrogen compounds, soil organic matter, humus, probability of bacterial colony formation (PCF) were calculated as described earlier (Malynovska et al, 2023). For a general assessment of the biological state of the soil, the indicator of total biological activity (TBA) was calculated using the method of relative values (Rusakova, 2013). The content of humus in the soil was determined according to (DSTU 4289:2004).…”
Section: Methodsmentioning
confidence: 99%
“…Indicators of the intensity of processes of mineralization of nitrogen compounds, soil organic matter, humus, probability of bacterial colony formation (PCF) were calculated as described earlier (Malynovska et al, 2023). For a general assessment of the biological state of the soil, the indicator of total biological activity (TBA) was calculated using the method of relative values (Rusakova, 2013). The content of humus in the soil was determined according to (DSTU 4289:2004).…”
Section: Methodsmentioning
confidence: 99%
“…Indicators of the intensity of processes of mineralization of nitrogen compounds, soil organic matter, humus, probability of bacterial colony formation (PCF) were calculated as described earlier (Malynovska et al, 2023). For a general assessment of the biological state of the soil, the indicator of total biological activity (TBA) was calculated using the method of relative values (Rusakova, 2013). The content of humus in the soil was determined according to (DSTU 4289:2004).…”
Section: Methodsmentioning
confidence: 99%
“…The positive correlation of Gm and TP with K and Mg highlights crucial aspects in soil dynamics, as under adequate moisture conditions, these nutrients mobilize in the soil and are incorporated into the pro le through pores, becoming accessible for root absorption by plants. In this regard, attention is drawn to soil decompaction before liming, as it assists in the process of water in ltration and percolation, reducing surface runoff and consequently, the transport of particles and nutrients in erosive processes (Borisov et al, 2022), which can contaminate downstream water bodies (Zhu et al, 2020).…”
Section: Soil Physical Attributesmentioning
confidence: 99%