МАТЕМАТИЧНА МОДЕЛЬ ГІДРОФІЗИЧНИХ ПРОЦЕСІВ В ЛІСОВИХ БОЛОТНИХ ЕКОЦЕНОЗАХ ЖИТОМИРСЬКОГО ПОЛІССЯ

Using the results of hydrological monitoring of the bog ecosystems of Zhytomyr Polissya, the mathematical modeling of the main hydrophysical processes in forest-bog ecological systems was analyzed and carried out. In conducting studies on the study of swamp forest feeds of the type C 5 , B 5 , D 5 , the first tested methods for determining the hydrodynamic regime in swamps were taken as the basis, which today is very relevant due to the change in the moisture supply of forest edible species. It is proved that forest marsh ecosystems, especially those formed in forest edapops C 4-5 , D 4-5 , are characterized by a rather high hydrostatic dynamism. This factor, in turn, affects both the degree of their wateriness and the ability to retain moisture. The hydrodynamics of the marsh edomoles of Zhytomyr Polissya consists in the formation of special hydrostatic conditions in which all the physical bodies that fall into them are in a semi-immersed state. Therefore, most of the Polissya forest swamps formed in forest types B 5 , C 5 , D 5 are regulators of subsoil drainage in catchment areas and in turn determine the supply of small rivers of Zhytomyr region. Key words: peat bogs, mountain bogs, hydrophysics, physico-mathematical model, lowland swamps, eutrophic bog, peat peat, alloy, peat development, energy conservation, resource conservation.