The role of chemoautotrophs / lithotrophs in the formation of
deposits and weathering is almost universally known, however, the
results of this biogeochemical activity and mass transfer mediated
by chemoautotrophs are radically different depending on the ionic
composition of the medium, the salt conductivity effects and the
Purbe diagram of the corresponding conditions of this activity,
as well as a number of other physico-chemical Characteristics
often not considered as impact factors (for simplifying models).