On the labyrinthine crystal-chemistry of boleite, a Pb-Ag-Cu hydroxyhalide

Abstract The chemical composition and crystal structure of boleite from the Amelia Mine (Boléo District, Mexico) were investigated by a series of chemical analytical techniques and single-crystal X-ray (data collected at 293 K) and neutron diffraction (at 20 K). The concentrations of more than 60 elements were measured. The empirical formula of boleite, based on the multi-analytical approach, is: (K0.390Ca0.165Na0.095Rb0.075Cd0.040Cs0.035Tl0.002)Σ0.80Pb26.05Ag8.93Cu23.91Cl61.64(OH)48.39, of which the simplified formula should be given as (K,Ca,Na,Rb,Cd,Cs)Pb26Ag9Cu24Cl62(OH)48. However, as Cd can also be considered as a potential substituent for Ag or Cu, the simplified formula transforms to (K,Ca,Na,Rb,Cs)Pb26Ag9Cu24Cl62(OH)48. This finding indicates a more complex scenario with respect to the previous formula reported in the literature, i.e., KPb26Ag9Cu24Cl62(OH)48. Chemical data obtained in this study show no significant evidence of potential substituents of Pb, Ag, and Cu; the concentrations of REE, PGE, and other industrially relevant elements are insignificant. Despite a lack of crystallographic evidence, chemical data appear to suggest that partial Cl− vs. OH− substitution can occur. Other potential substituents of Cl−, such as F−, have not been detected at a significant level. X-ray and neutron diffraction data confirm the previously reported general structural model of boleite but consistently show that a substitutional disorder affects the K site, manifested by a large and unusual displacement parameter. The magnitude of the displacement parameter reflects static disorder, in the form of substitutional disorder, due to differences in the local bonding topology among K, Ca, Na, Rb, (Cd), and Cs statistically populating the same site. The H-bonding network in the structure of boleite is now unambiguously described on the basis of the neutron structural model, with two energetically favorable bonds, both having an Odonor-H···Clacceptor configuration. The structure of boleite does not contain H2O molecules but, instead, only two crystallographically independent hydroxyl groups.

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Publication Details

Journal
American Mineralogist
Published
2025-03-06
DOI
https://doi.org/10.2138/am-2024-9721
Primary Topic
Crystallization and Solubility Studies
Type
article
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article

On the labyrinthine crystal-chemistry of boleite, a Pb-Ag-Cu hydroxyhalide

Óscar Fabelo, Marco Merlini, Tommaso Battiston, Geoffrey Bromiley et al.
American Mineralogist
Crystallization and Solubility Studies
article

On the labyrinthine crystal-chemistry of boleite, a Pb-Ag-Cu hydroxyhalide

Óscar Fabelo, Marco Merlini, Tommaso Battiston, Geoffrey Bromiley, Giorgio Guastella, G. Diego Gatta, Pierino Malizia
article en

Abstract

Abstract The chemical composition and crystal structure of boleite from the Amelia Mine (Boléo District, Mexico) were investigated by a series of chemical analytical techniques and single-crystal X-ray (data collected at 293 K) and neutron diffraction (at 20 K). The concentrations of more than 60 elements were measured. The empirical formula of boleite, based on the multi-analytical approach, is: (K0.390Ca0.165Na0.095Rb0.075Cd0.040Cs0.035Tl0.002)Σ0.80Pb26.05Ag8.93Cu23.91Cl61.64(OH)48.39, of which the simplified formula should be given as (K,Ca,Na,Rb,Cd,Cs)Pb26Ag9Cu24Cl62(OH)48. However, as Cd can also be considered as a potential substituent for Ag or Cu, the simplified formula transforms to (K,Ca,Na,Rb,Cs)Pb26Ag9Cu24Cl62(OH)48. This finding indicates a more complex scenario with respect to the previous formula reported in the literature, i.e., KPb26Ag9Cu24Cl62(OH)48. Chemical data obtained in this study show no significant evidence of potential substituents of Pb, Ag, and Cu; the concentrations of REE, PGE, and other industrially relevant elements are insignificant. Despite a lack of crystallographic evidence, chemical data appear to suggest that partial Cl− vs. OH− substitution can occur. Other potential substituents of Cl−, such as F−, have not been detected at a significant level. X-ray and neutron diffraction data confirm the previously reported general structural model of boleite but consistently show that a substitutional disorder affects the K site, manifested by a large and unusual displacement parameter. The magnitude of the displacement parameter reflects static disorder, in the form of substitutional disorder, due to differences in the local bonding topology among K, Ca, Na, Rb, (Cd), and Cs statistically populating the same site. The H-bonding network in the structure of boleite is now unambiguously described on the basis of the neutron structural model, with two energetically favorable bonds, both having an Odonor-H···Clacceptor configuration. The structure of boleite does not contain H2O molecules but, instead, only two crystallographically independent hydroxyl groups.

American MineralogistVol. 110(10)
University of Milan (IT), Institut Laue-Langevin (FR), Lombardia Informatica (Italy) (IT), University of Edinburgh (GB)
Openalex Percentile: Top 97%
Crystallization and Solubility Studies
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