Abstract

Experimental systems demonstrate that humic acids are capable of accepting electrons from a wide spectrum of donors and transferring those electrons to a wide spectrum of acceptors, linking normally thermodynamically discrete redox couples. By functioning as a wide redox potential ‘flavoprotein’, humics encompass all the redox potentials pertinent to aquatic systems and hence determine relative electron activity, the negative log of which is pE. A chemically determined, system oxidation-reduction potential allows pE to be used along with pH in developing a biochemical framework for thermodynamically derived predictions of aquatic system behavior.

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