Department of Earth Sciences, University of Bristol
Chemistry for Earth Sciences
Prof. D.M. Sherman

Lecture 10: Oxidation-Reduction Equilibria


Several geochemically important elements (S, O, C, N, Fe, Mn) can exist in more than one oxidation state over the range of conditions in the Earth's crust. Oxidation-reduction equilibria are the primary means by which biological processes interact with geochemistry.


You should be able to:

Lecture Notes

Homework and Self-Assessment

Supplemental Reading

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