Journal of Mineralogical and Petrological Sciences
Online ISSN : 1349-3825
Print ISSN : 1345-6296
ISSN-L : 1345-6296
Thermal decomposition and reversible transformation of ulexite NaCaB5O6(OH)6·5H2O
Kosuke Yamaguchi Satoru OkadaHiroki HasegawaAtsushi Kyono
著者情報
ジャーナル オープンアクセス 早期公開

論文ID: 250417

詳細
抄録

Borate minerals, particularly hydrated borates, undergo structural transformations during thermal decomposition, which is an important process for understanding their thermodynamic stability and structural properties. In this study, we investigated reversible transformations of the dehydration/dehydroxylation phases of ulexite NaCaB5O6(OH)6·5H2O under high-humidity conditions. Remarkably, the dehydrated ulexite NaCaB5O6(OH)6·3H2O rapidly transformed back to ulexite after exposure to high-humidity conditions, indicating a high rehydration capacity caused by minimal structural reconfiguration. In contrast, the amorphous phase obtained at the temperature of 180–500°C exhibited multiple recrystallization pathways, forming both ulexite and borax Na2B4O5(OH)4·8H2O, likely due to dissolution–reprecipitation mechanisms. Anhydrous ulexite NaCaB5O9 formed by further heating of the amorphous phase at 600°C reversibly transformed to ulexite through progressive rehydroxylation of its fundamental building blocks (FBBs). Furthermore, we confirmed that the thermal transformation of ulexite follows the principle of FBB inheritance, where a structural unit of the FBBs persists across successive phases. Ulexite fully preserved the FBB to dehydrated ulexite, whereas dehydrated ulexite passed a partial FBB to anhydrous ulexite. Even after the phase decomposition, a part of the FBB in anhydrous ulexite was retained in CaB2O4. Dehydrated ulexite, its amorphous phase, and anhydrous ulexite produced by thermal decomposition of ulexite can revert to ulexite under high-humidity conditions. This transformation property implies that the inherited and retained FBBs are reorganized upon rehydration into the crystal structure of ulexite, which represents the thermodynamically most stable phase. This observation also indicates that reconstitution of FBBs can occur readily in water-rich environments. These insights have significant implications for the thermodynamic modeling of borate systems, geological boron cycle involving the bonding mode inheritance of FBB, and the development of borate-based functional materials.

著者関連情報
© 2025 Japan Association of Mineralogical Sciences

This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0), which permits non-commercially distribute and reproduce an unmodified in any medium, provided the original work is properly cited.
https://creativecommons.org/licenses/by-nc-nd/4.0/
次の記事
feedback
Top