Unveiling the Amphoteric Surface Reactivity of Montebrasite using Spectroscopic and First-Principles Methods

The amblygonite-montebrasite group of minerals is the most abundant lithium (Li)-bearing phosphate found in phosphorus-rich Li pegmatites. The separation of montebrasite from spodumene─the primary Li ore mineral─commonly by flotation, is necessary for effective downstream Li extraction. Understanding how water molecules interact with the montebrasite surface is necessary to understand its separation from other minerals by flotation. This study examined the interaction between water and montebrasite using dissolution tests, surface charge analysis, and various spectroscopic techniques (UV, FTIR, XPS, and XANES), all supported by density functional theory calculations. We found evidence of amphoteric properties, with mineral surface protonation and hydroxylation resulting in water (de)protonation. Chemical reactivity involved acid–base reactions, F/OH ion exchange (−142.61 kcal/mol), nonstoichiometric dissolution (F > Li > Al > P), and dissociative chemisorption (−187.06 kcal/mol) at the mineral–water interface. This surface reactivity could impact solution chemistry and influence collector adsorption on the mineral surface during flotation. Surface dissolution and ion exchange may lead to the release of Li to industrial process water, in addition to F, potentially forming LiF in solution. These findings are significant in the froth flotation field because the change in solution pH caused by substantial amounts of amphoteric minerals, such as montebrasite, can affect flotation results, leading to unstable flotation circuits since flotation performance depends on pH. However, this issue may be managed by achieving and/or maintaining an equilibrium pH through an appropriate conditioning stage. This work builds important knowledge of montebrasite surface properties and the montebrasite–water interface, essential to understanding many natural phenomena and engineering processes. Accordingly, we discussed the implications for montebrasite froth flotation, mineral alteration, environmental impact, and its potential as a promising functional material for heterogeneous catalysis and Li-ion batteries.

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Journal
The Journal of Physical Chemistry C
Published
2025-09-19
DOI
https://doi.org/10.1021/acs.jpcc.5c04541
Primary Topic
Mineralogy and Gemology Studies
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article
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article

Unveiling the Amphoteric Surface Reactivity of Montebrasite using Spectroscopic and First-Principles Methods

Espoir M. Murhula, Charlotte E. Gibson, Lucia Zuin, Gideon Lambiv Dzemua et al.
The Journal of Physical Chemistry C
Mineralogy and Gemology Studies
article

Unveiling the Amphoteric Surface Reactivity of Montebrasite using Spectroscopic and First-Principles Methods

Espoir M. Murhula, Charlotte E. Gibson, Lucia Zuin, Gideon Lambiv Dzemua, Wennie Wang, G. Schatte, Suk Gyu Lim
article en

Abstract

The amblygonite-montebrasite group of minerals is the most abundant lithium (Li)-bearing phosphate found in phosphorus-rich Li pegmatites. The separation of montebrasite from spodumene─the primary Li ore mineral─commonly by flotation, is necessary for effective downstream Li extraction. Understanding how water molecules interact with the montebrasite surface is necessary to understand its separation from other minerals by flotation. This study examined the interaction between water and montebrasite using dissolution tests, surface charge analysis, and various spectroscopic techniques (UV, FTIR, XPS, and XANES), all supported by density functional theory calculations. We found evidence of amphoteric properties, with mineral surface protonation and hydroxylation resulting in water (de)protonation. Chemical reactivity involved acid–base reactions, F/OH ion exchange (−142.61 kcal/mol), nonstoichiometric dissolution (F > Li > Al > P), and dissociative chemisorption (−187.06 kcal/mol) at the mineral–water interface. This surface reactivity could impact solution chemistry and influence collector adsorption on the mineral surface during flotation. Surface dissolution and ion exchange may lead to the release of Li to industrial process water, in addition to F, potentially forming LiF in solution. These findings are significant in the froth flotation field because the change in solution pH caused by substantial amounts of amphoteric minerals, such as montebrasite, can affect flotation results, leading to unstable flotation circuits since flotation performance depends on pH. However, this issue may be managed by achieving and/or maintaining an equilibrium pH through an appropriate conditioning stage. This work builds important knowledge of montebrasite surface properties and the montebrasite–water interface, essential to understanding many natural phenomena and engineering processes. Accordingly, we discussed the implications for montebrasite froth flotation, mineral alteration, environmental impact, and its potential as a promising functional material for heterogeneous catalysis and Li-ion batteries.

The Journal of Physical Chemistry C
United States Geological Survey (US), Queen's University (CA), Government of Northwest Territories (CA), Canadian Light Source (Canada) (CA), The University of Texas at Austin (US)
Openalex Percentile: Top 79%
Mineralogy and Gemology Studies
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