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[OLD] Fe oxides


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From: T.C. Onstott

Subject: Fe oxides

I was reproducing some figures in a paper by Potsma and Jakobsen (1996) who used Phreeqe to model Hematite and Goethite reduction of sulfide and I noticed that the GWB data seems to differ from the Phreeqe data base with respect to the log K of these two minerals. Is this true or am I missing something here?

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