The ecological potential of the soils of natural old-growth forests is analyzed. It has been found that the upper horizon of brown mountain-forest soils is characterized by excellent indicators of total porosity (63,63 %), soil water permeability (3,08 cm⸱min-¹), soil bulk density (0,88 g⸱cm-³) and catalase enzyme activity (4,9 cm3 O2 per 1 g of soil per 1 min). The results indicate excellent ecological potential of the soils, which allows using their indicators as a reference for restoring soil cover under the forest ecosystems of the Skole Beskydy. The recreational and agrogenic impact on soils in the mountainous region was also analyzed. It was found that the upper humus-accumulative horizon suffers the most from plowing, trampling by livestock, and damage by erosion processes caused by prolonged recreational use. While cattle grazing is seasonal, the impact of recreationists is increasing and corresponds to stages II and IV of recreational degradation, soils under arable land are subject to the greatest anthropogenic impact in terms of time interval due to the transfer of the upper horizons downwards, and vice versa. The processes of soil recovery under pasture, after the removal of agrogenic load, are much faster than under plowed areas. Arable land undergoes several successive stages of recovery (arable land → fallow land → shrub vegetation → woody vegetation I (mainly gray alder and birch-aspen stands) → woody vegetation II (indigenous forest-forming species of the region), where the process itself takes 150-200 years. Третє місце серед досліджуваних ділянок посідають туристичні шляхи. Зазначимо, що само відновлення стежок відбувається здебільшого на початку ІІ стадії дегресії, ІV стадія потребує реконструкції, а період відновлення сягає кілька десятків років. The analysis of water-physical properties under old-growth natural stands as a benchmark shows that the density of soil structure increases by 1,2 times on the category II trail and 1.5 times on the category IV trail Based on the results of the analysis of data made within the soil profile, it was found that under pasture the soil is compacted to a depth of 10 cm, under arable land - to the depth of plowing, and on trails the compaction is 5-10 cm in the initial stages and reaches 30 cm to the depth of the parent rock at the IV stage of recreational degradation. Systematic monitoring of the tourist routes and ecological trails of the Skole Beskydy National Park will help prevent degradation processes in a timely manner. In the areas with low recreational load, it is proposed to mark the tourist trails, and for safety and convenience, to install bridges with handrails over mountain streams. On the trails of the IV category, it is necessary to mark the routes, limit the access of recreationists in bad weather to the outstanding attractions. Key words: еcological potential of soils; old-growth natural forests; trail; land use; brown mountain-forest soils; forest floor; mountainous region.
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