PNNL

Abstract

Our understanding of how Fe(II) reacts with Fe(III) oxides has evolved significantly based on evidence for electron transfer at the oxide-water interface and Fe(II)-catalyzed recrystallization. Recent experiments, as well as computational calculations, further suggest that defects at oxide surfaces can facilitate electron transfer. There is, however, some evidence that these processes cease after continued contact with Fe(II). Here, we explore the sustainability of these processes over longer time frames by measuring whether exposure to Fe(II) inhibits Fe(II)-goethite electron transfer, and whether this inhibition is reversible. To quantify the extent of electron transfer, we used selective isotope labeling with 57Fe Mössbauer spectroscopy. The results revealed that pre-reacting goethite with Fe(II) decreases the extent of electron transfer during subsequent exposures, and that less electron transfer occurs with increasing reaction time. Similarly, X-ray absorption spectroscopy and magnetic circular dichroism suggest that reaction with Fe(II) consumes surface defects and forms a passivation layer, making goethite less susceptible to electron transfer. When Fe(II) is removed by either wet chemical extraction or oxidation, electron transfer is mostly restored, suggesting that inhibition of electron transfer is reversible. Our results show that in environmental systems, which are commonly subjected to transient geochemical fluctuations, electron transfer between Fe(II) and Fe oxides, and processes linked to it, are likely to be relevant beyond just short time scales.