Transition Metal Ions in The Processes Of Acid Rain Formation

摘要

Redox dissolution of a nuclei of which a part is insoluble Fe_2O_3 favors sulfite oxidation in the atmosphere from a thermodynamic and kinetic point of view. Coupled with UV light absorption, the uptake of HO_2 radicals from the gas through the reaction FeOH~(2+) + O_2 and the presence in the droplets of manganese ions, the redox dissolution results in a non-linear rise of the dynamics of the redox cycling of iron and faster removal of SO_2 from the gas.