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Eff ects of aff orestation on soil structure formation in two climatic regions of the Czech Republic

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Figure

Fig. 1. T-test of clay content (a), porosity (b), water-stable aggregates (c)
Table 3. Evaluation of porosity ± standard deviation, across both study areas, highland and lowland of the Czech Republic (in %)
Table 5. Chemical characteristics of soil ± standard deviation, by study area: Orlické hory Mts
Table 6. Evaluation of SOM quality ± standard deviation, across both study areas, highland and lowland of the Czech Republic

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