The anthropogenic evolution of zheltozems (Acrisols) in the sanatorium zone of the Sochi agglomeration is characterized by a change in the acid-base properties and humus status of soils since the late 1920s. The pHwater shifted from 5.1 to 7.4 (mean values for soil genetic horizons) and the total exchangeable bases increased 2.4 times (from 17.2 to 41.2 cmol(+)/kg) in the topsoil and 1.3 times (from 15.9 to 21.0 cmol(+)/kg) in the structural-metamorphic gleyed BMg horizon. Soil alkalization typical for urban environment resulted in the suppression of eluviation of the upper part of the BMg horizon. Humus content remained at the same level (about 6.7%) in the topsoil, but increased (to 3.6–4.3% as compared to the initial 0.5–0.8%) in the subsoil. This transformation is caused by two factors: (1) the input of technogenic salts of metals with the surface runoff and drainage water, which are alkaline and transform the acid-base soil properties; (2) cultivation of soils (filling of the humus horizon of chernozem onto the soil surface) for planting exotic plants from dendroparks in sanatoriums. The soils are qualified for dark structural-metamorphic agrozems. There are small local areas of abrazems, and soils of subordinate landscapes in the lower parts of slopes adjacent to small streams are represented by chemozems over zheltozems. On steep slopes to the Black Sea coast without sanatorium infrastructure, almost untransformed typical zheltozems are formed under natural vegetation. With an increase in pH as a result of stronger anthropogenic transformation, the base saturation of zheltozems steadily decreases.
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