2018
DOI: 10.2478/ssa-2018-0008
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Sequestration of organic carbon in rendzinas – a review

Abstract: The article refers to the stock and sequestration of organic carbon in soils rich in carbonates, particularly in rendzinas. It presents factors determining sequestration of organic carbon in rendzinas in comparison to other soils, and describes the mechanisms of accumulation of organic matter in these soils. Attention was paid to the atypical morphology of organic and humus horizons occurring in soils rich in carbonates, with specificity related to biological processes.

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Cited by 3 publications
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“…An important factor forming the sequestration of carbon in calcareous soils is the type of parent rock, which determines the content of calcium and magnesium and the amount and type of clay minerals. All the processes described above lead to the creation of specific morphological properties of Rendzinas with a deep black surface horizon, as well as certain conditions -and specific feature of organic compounds (Wasak et al, 2018). The type of humus is fulvic-humic to humic, the ratio Ch/Cf is from 0.6 to 3.75 (Figure 4).…”
Section: Resultsmentioning
confidence: 99%
“…An important factor forming the sequestration of carbon in calcareous soils is the type of parent rock, which determines the content of calcium and magnesium and the amount and type of clay minerals. All the processes described above lead to the creation of specific morphological properties of Rendzinas with a deep black surface horizon, as well as certain conditions -and specific feature of organic compounds (Wasak et al, 2018). The type of humus is fulvic-humic to humic, the ratio Ch/Cf is from 0.6 to 3.75 (Figure 4).…”
Section: Resultsmentioning
confidence: 99%