Abstract
Water extracts from the organic horizons of southern-tundra loamy permafrost-affected soils (a surface-gleyed tundra soil, a surface-gleyed soddy tundra soil (Haplic Stagnosols (Gelic)), and a peaty tundra soil (Histic Cryosol (Reductaquic)) and their undecomposed moss layers have been analyzed. The total weight concentration of the cations (Ca2+, Mg2+, K+, and Na+) determined by the atomic absorption method reaches 20 mg/dm3 in the organic horizons and 40–90 mg/dm3 in the undecomposed moss layers. Potassium and calcium ions dominate in all the organic horizons (80–90% of the total weight); potassium ions prevail in the mosses (about 70%). The weight concentration of carbon in the water-soluble organic compounds is 0.04–0.07 g/dm3 in the organic horizons and 0.20–0.40 g/dm3 in the undecomposed moss layers. The content of low-molecular-weight organic compounds (alcohols, carbohydrates, and acids) identified by gas chromatography and chromatomass spectrometry is 1–30 mg/dm3 in the organic horizons of the soils and 80–180 mg/dm3 in the mosses, which does not exceed 26% of the total organic carbon in the extracts.
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Original Russian Text © E.V. Shamrikova, O.S. Kubik, V.V. Punegov, I.V. Gruzdev, 2014, published in Pochvovedenie, 2014, No. 3, pp. 295–303.
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Shamrikova, E.V., Kubik, O.S., Punegov, V.V. et al. Effect of the biota diversity on the composition of low-molecular-weight water-soluble organic compounds in southern tundra soils. Eurasian Soil Sc. 47, 173–181 (2014). https://doi.org/10.1134/S1064229314030077
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DOI: https://doi.org/10.1134/S1064229314030077