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

Lecture 10: Oxidation-Reduction Equilibria

Overview

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.

Objectives

You should be able to:

Lecture Notes

Homework and Self-Assessment

Supplemental Reading

Back to Geochemistry course homepage.
There have been 1,592 visits to this page. Last Modified on December 6, 2011 at 16:06.