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Effect of Impurities on the Redox Properties of Goethite
Journal article   Peer reviewed

Effect of Impurities on the Redox Properties of Goethite

Drew E Latta, Sebastian T Mergelsberg, Duo Song, Eric J Bylaska, Michelle M Scherer, Bryanna Popejoy, Sarah A Saslow, Jeffrey G Catalano and Eugene S Ilton
Environmental science & technology, Vol.59(16), pp.7799-8294
04/29/2025
DOI: 10.1021/acs.est.4c13480
PMID: 40254805

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Abstract

Iron oxide minerals regulate the flux of electrons in the environment and are important hosts for trace and minor, yet critical, elements. Here, we present the first evidence of a direct link between the local coordination environments of Ni and Zn and the redox properties of their host phase goethite (α-FeOOH), the most abundant Fe(III) (oxyhydr)oxide at Earth's surface. We used aqueous redox measurements to show that the redox potential , and hence the mineral's stability, follows the order: pure goethite ≥ Zn-goethite > Ni-goethite. Parallel X-ray absorption and scattering measurements demonstrate, using quantum-informed analysis, that the local coordination environment of the smaller impurity, Ni, causes more bulk strain energy than Zn, which nearly accounts for the difference in between Ni- and Zn-goethite. Our theory-informed, experimental study reveals how two common impurities affect the stability of goethite with implications for the biogeochemical reactivity of Fe(III) (oxyhydr)oxide in mediating elemental and electron fluxes in the environment.
Zinc goethite nickel impurity incorporation lattice strain redox

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