Isotope Channelomics of Chemoautotroph as the Predictor and Regulator of the Metal Deposit formation and the Weathering Factor by Gradov OV MAOPS- LupinePublishers
Chemoautotrophic and lithotrophic microorganisms are known to
participate in the deposit formation and the rock weathering, but the
results of such chemoautotroph-mediated biogeochemical activity and mass
transfer strongly differ depending on the ionic composition of the
medium, the salt conductivity effects and the Pourbaix diagrams of their
medium, as well as on some other physico-chemical parameters which are
often not considered as the active external factors for the sake of
simplicity. The early biogeochemical considerations underlying the
models and kinetic approaches to the analysis of such processes are
mostly phenomenological and empirical and do not disclose the essence of
the processes occurring at the boundary between the medium processed by
the microorganisms and their active surface.
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