“…On map V, an increase in the content of mobile phosphorus was found in soil layers from 0 to 80 m −1 , which can be explained in the absence of fertilizers by its biogenic accumulation, since phosphorus, as shown in the studies of T. Kulakovskaya et al, has an extremely weak migration ability, and no more than 3-5% of its total reserves is washed out [7,8,18,19]. In addition, it was shown that in shallow, weakand medium-azole peat bogs, with commercial water regime and high groundwater aquifer, they can penetrate into the subsoil and underlying layers [5,6,19], which our observations also showed.…”