Abstract
Brucite [Mg(OH)2] is a promising sorbent for carbon dioxide removal (CDR) due to its availability and low calcination temperatures. However, natural and synthetic brucites tend to contain metal impurities, such as iron or manganese, and how these impurities affect the interfacial chemical reactivity is uncertain. Here, the impact of low concentrations of iron and manganese impurities on the carbonation efficiency of Mg(OH)2 was examined. Mg(OH)2 with small amounts (1–5 mol %) of Fe and Mn was synthesized. The increasing substitution of Fe into Mg(OH)2 was accompanied by the oxidation of Fe. The phase transformation sequence during the carbonation was found to be brucite [Mg(OH)2] → amorphous magnesium carbonate (MgCO3·nH2O) → nesquehonite (MgCO3·3H2O), regardless of impurity concentration. Both the Fe- and Mn-doped Mg(OH)2 samples were more reactive than endmember Mg(OH)2, possibly due to their higher surface areas and lower stabilities. During carbonation, 3 mol % Fe- and Mn-doped Mg(OH)2 showed the highest reactivity. The variance in reactivity for Mn-doped Mg(OH)2 was less than that of Fe-doped Mg(OH)2. These results suggest that natural or industrial waste Mg(OH)2 with less than 5 mol % Fe and Mn impurities may be targeted as more effective CDR sorbents than endmember Mg(OH)2.
| Original language | English |
|---|---|
| Pages (from-to) | 2160-2170 |
| Number of pages | 11 |
| Journal | Journal of Physical Chemistry C |
| Volume | 130 |
| Issue number | 6 |
| DOIs | |
| State | Published - Feb 12 2026 |
Funding
This article is based on Chapter 3 of Dong Youn Chung̀s PhD thesis.(102)This work was mainly supported by the U.S. Department of Energy (DOE), Office of Science, Basic Energy Sciences (BES), Materials Sciences and Engineering Division. TEM and SEM 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. The synchrotron XRD measurements were performed at GeoSoilEnviroCARS (The University of Chicago, Sector 13), Advanced Photon Source (APS), Argonne National Laboratory (ANL). GeoSoilEnviroCARS was supported by the National Science Foundation─Earth Sciences (EAR-1634415). This research used resources of the APS, a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by ANL under Contract No. DE-AC02-06CH11357. Synchrotron-XRD measurements were funded by U.S. National Science Foundation (NSF) grant EAR-1925903, American Chemical Society Petroleum Research Fund (ACS PRF), and the Pennsylvania State University.
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