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Pits: Es1b, Es2b, Es3b Es4b 0.0 1.0 2.0 3.0 % Es5m 0 a 10 10 Ahkb AhBkb 30 Ahkb + AhBkb Ahk + AhBk 50 70 90 110 Blkb Blkb Blk 130 B2kb B2kb 0 B2k 150 170 BCkb BCkb BCk 190 フ CM 123456 20 20 Depth, cm 40 40 60 60 80 100 120 140 160 180 Organic carbon 0 20 20 40 60 1 - carbonate pseudomycelium, 2 - white soft carbonate spots, 3 - carbonate impregnation, 4- gypsum veins, 5 – animal holes, 6 – the depth of appearance of carbonate pedofeatures 0.0 1.0 2.0 3.0 % 1.2% b a Carbonate 1.0 carbon 0.8 SO4 of gypsum 0.6 80 0.4 100 120 20 0.2 140 0.0 16660 180 200 100-120 120-140 140-160 160-180 | 180-200 100-120 | 120-140 140-160 160-180 180-200 100-120 120-140 100-120 120-140 140-160 160-180 80-200 12 100-120 120-140 140-160 160-180 | 180-200 3 - 200 4-5 During the interval of kurgan construction, the morphological and physicochemical properties of soils changed. There is a decrease in intensity of the black color of the humus horizon and the content of organic carbon within the first 50 cm of profile, an increase in the content of gypsum, carbon of carbonates, a shift of the area of their accumulation up the profile, and transformation of the forms of carbonate pedofeatures. 5 Soil pits: 1 – Es1b, 2 – Es2b, 3 – Es3b, 4 - Es4b, 5 – Es5m CC BY Depth, cm
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