Abstract
A model of distribution of inorganic substances in the polluted waters of an oligotrophic bog has been developed and geomigratory calculations have been carried out on the example of Vasyugan Bog. It is shown that the most significant changes of mineralization of bog waters caused by the inflow of industrial waste waters from oil and gas production enterprises are referred to the high layer with a thickness of approximately 0.5–1.0 m. The creation of loam as an insulating barrier in the active layer of the bog helps reduce the negative impact on the waters, but does not preserve their baseline state on the lower layer.
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