Restoration of the biodiversity of technogenic landscapes of anthracite deposits in Siberia

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Table 1

Calculation of the SES points of the main types of soils.

Soil type	Corg, %	Cs_C	PC, %	Cs_PC	Density, g/cm³	Cs_D	CCE, mg-equiv/100g	Cs CCE	Cs_av	SES, point
EIef	2.9	0.84	1.8	0.04	2.2	0.50	5.0	0.12	0.38	37.5
EOAef	2.4	0.69	7.5	0.18	1.7	0.65	14.0	0.33	0.46	46.3
ETef	4.6	0.62	9.5	0.23	1.5	0.73	25.0	0.60	0.54	54.2
EIeb	2.9	0.86	1.8	0.04	1.7	0.64	8.0	0.19	0.43	43.3
EOAeb	5.1	1.49	6.4	0.15	1.6	0.69	11.0	0.26	0.65	64.9
ETc	0.7	0.20	59.6	1.42	1.5	0.73	37.0	0.88	0.81	80.6
EOAc	0.3	0.10	61.0	1.45	1.3	0.85	36.0	0.85	0.81	81.3
Ch	3.4	1.00	42.0	1.00	1.1	1.00	45.0	1.00	1.00	100.0

Notes. Cs – coefficient of specificity; Corg – the content of organic carbon; PC – the content of physical clay; CCE – the capacity of cation exchange; Cs_av – average coefficient of specificity; SES – the soil-ecological state.

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