Guérinite Ca6(HAsO4)3(AsO4)2∙10.5H2O – a revision of the mineral formula

Abstract A single crystal of guérinite from the Plaka Mine, Lavrion, Greece, was examined by X-ray diffraction. The mineral crystallizes in the monoclinic space group P 2 1 / n with unit cell parameters a = 17.628 (2), b = 6.728 (1), c = 23.384 (3) Å, β = 90.68 (1)°, V = 2773.4 (6) Å 3 . The originally reported mineral formula Ca 5 (HAsO 4 ) 2 (AsO 4 ) 2 ∙9H 2 O, Z = 5 should be revised to Ca 6 (HAsO 4 ) 3 (AsO 4 ) 2 ∙10.5H 2 O, Z = 4. Accordingly, guérinite is no longer considered a polymorph to ferrarisite. The structure is characterized by complex layers consisting of corner- and edge sharing of CaO n ( n = 7, 8) polyhedra and arsenate groups. The connection between these units is achieved exclusively via hydrogen bonding.

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Publication Details

Journal
Mineralogy and Petrology
Published
2024-10-07
DOI
https://doi.org/10.1007/s00710-024-00873-2
Primary Topic
Crystal Structures and Properties
Type
article
Field-Weighted Citation Impact
0.00

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article

Guérinite Ca6(HAsO4)3(AsO4)2∙10.5H2O – a revision of the mineral formula

Gerald Giester, Branko Rieck, Irene Liebhart
Mineralogy and Petrology
Crystal Structures and Properties
article

Guérinite Ca6(HAsO4)3(AsO4)2∙10.5H2O – a revision of the mineral formula

Gerald Giester, Branko Rieck, Irene Liebhart
article en

Abstract

Abstract A single crystal of guérinite from the Plaka Mine, Lavrion, Greece, was examined by X-ray diffraction. The mineral crystallizes in the monoclinic space group P 2 1 / n with unit cell parameters a = 17.628 (2), b = 6.728 (1), c = 23.384 (3) Å, β = 90.68 (1)°, V = 2773.4 (6) Å 3 . The originally reported mineral formula Ca 5 (HAsO 4 ) 2 (AsO 4 ) 2 ∙9H 2 O, Z = 5 should be revised to Ca 6 (HAsO 4 ) 3 (AsO 4 ) 2 ∙10.5H 2 O, Z = 4. Accordingly, guérinite is no longer considered a polymorph to ferrarisite. The structure is characterized by complex layers consisting of corner- and edge sharing of CaO n ( n = 7, 8) polyhedra and arsenate groups. The connection between these units is achieved exclusively via hydrogen bonding.

Mineralogy and PetrologyVol. 118(4)
University of Vienna (AT)
Universität Wien
Openalex Percentile: Top 90%
Crystal Structures and Properties
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