Fe(II) interaction with cement phases: Method development, wet chemical studies and X-ray absorption spectroscopy

Fe(II) interaction with cement phases was studied by means of co-precipitation and sorption experiments in combination with X-ray absorption fine structure (XAFS) spectroscopy. Oxidation of Fe(II) was fast in alkaline conditions and therefore, a methodology was developed which allowed Fe(II) to be stabilised in the sorption experiments and to prepare samples for spectroscopy. X-ray diffraction (XRD) of the co-precipitation samples showed uptake of a small portion of Fe(II) by calcium-silicate-hydrates (C-S-H) in the interlayer indicated by an increase in the interlayer spacing. Fe(II) incorporation by AFm phases was not indicated. Wet chemical experiments using Fe-55 radiotracer revealed linear sorption of Fe(II) irrespective of the Ca/Si ratio of C-S-H and equilibrium pH. The K-d values for Fe(II) sorption on C-S-H are more than three orders of magnitude lower as compared to Fe(III), while they are comparable to those of other bivalent metal cations. XAFS spectroscopy showed Fe(II) binding by C-S-H in an octahedral coordination environment. The large number of neighbouring atoms rules out the formation of a single surface-bound Fe(II) species. Instead the data suggest presence of Fe(II) in a structurally bound entity. The data from XRD and XAFS spectroscopy suggests the presence of both surface- and interlayer-bound Fe(II) species. (C) 2020 The Author(s). Published by Elsevier Inc.

Automated summary

The study found that Fe(II) oxidation rate is fast under alkaline conditions, and a methodology was developed to stabilize Fe(II) for sorption experiments and spectroscopy analysis. Results showed that C-S-H can uptake a small portion of Fe(II), while Fe(II) incorporation by AFm phases was not indicated. XAFS spectroscopy revealed Fe(II) binding in an octahedral coordination environment with C-S-H.