Abstract
Despite extensive research on MgO’s reactivity in the presence of CO2 under various conditions, little is known about whether impurities incorporated into the solid, such as iron, enhance or impede hydroxylation and carbonation reactions. The purity of the MgO required for the successful implementation of MgO looping as a direct air capture technology affects the deployment costs. With this motivation, we tested how incorporated iron impacts MgO (100) reactivity and passivation layer formation under ambient conditions by using atomic force microscopy, electron microscopy, and synchrotron-based X-ray scattering. Based on electron microprobe analysis, our MgO samples were 0.5 wt % iron, and Mössbauer spectroscopy results indicated that 70% of the iron is present as Fe(II). We find that even these low levels of iron dopants impeded both the hydroxylation at various relative humidities (10%, 33%, 75%, and >95%) and carbonation in CO2 (33%, 75%, and >95%) on the (100) surface. Crystalline reaction products were formed. Reaction layers on the sample were easily removed by exposing the sample to deionized water for 2 min. Overall, our findings demonstrate that the presence of iron dopants slows the reaction rate of MgO, indicating that MgO without incorporated iron is preferable for mineral looping applications.
| Original language | English |
|---|---|
| Pages (from-to) | 3457-3468 |
| Number of pages | 12 |
| Journal | Journal of Physical Chemistry C |
| Volume | 129 |
| Issue number | 7 |
| DOIs | |
| State | Published - Feb 20 2025 |
Funding
This work was supported by the U.S. Department of Energy, Office of Science, Basic Energy Sciences, Materials Sciences and Engineering Division. TEM characterization was conducted as part of a user project at the Center for Nanophase Materials Sciences (CNMS), which is a U.S. Department of Energy, Office of Science User Facility at Oak Ridge National Laboratory. We would like to thank James Kolopus for providing the MgO and (Mg,Fe)O samples used in this study. Jeffrey Baxter is acknowledged for FIB sample preparation. We acknowledge Allan Patchen for the microprobe characterization. XRR and GIXRD measurements were conducted at GeoSoilEnviroCARS (The University of Chicago, Beamline 13-ID-C), Advanced Photon Source (APS), Argonne National Laboratory. GeoSoilEnviroCARS is supported by the National Science Foundation-Earth Sciences (EAR-1634415). J.E.S., A.K.W., and P.J.E. received further support from the Department of Energy-GeoScience (DE-SC0019108). This research used resources of the Advanced Photon Source, a U.S. Department of Energy Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract DE-AC02-06CH11357.