Chiral edge-shared octahedral chains in liskeardite, [(Al,Fe) 32(AsO4)18(OH)42(H 2O)22]52H2O, an open framework mineral with a pharmacoalumite-related structure

Ian E Grey, W G Mumme, C. M. Macrae, T. Caradoc-Davies, J. R. Price, M. S. Rumsey, S. J. Mills

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Abstract

The type specimen of liskeardite, (Al, Fe)3AsO 4(OH)65H2O, from the Marke Valley Mine, Liskeard District, Cornwall, has been reinvestigated. The revised composition from electron microprobe analyses and structure refinement is [Al 29.2Fe2.8(AsO4)18(OH) 42(H2O)22]52H2O. The crystal structure was determined using synchrotron data collected on a 2 μm diameter fibre at 100 K. Liskeardite has monoclinic symmetry, space group I2, with the unit-cell parameters a = 24.576(5), b = 7.754(2) Å, c = 24.641(5) Å, and β = 90.19(1)°. The structure was refined to R = 0.059 for 9769 reflections with I > 3σ(I). It is of an open framework type in which intersecting polyhedral slabs parallel to (101) and (101) form 17.4 Å × 17.4 Å channels along [010], with water molecules occupying the channels. Small amounts (<1 wt.%) of Na, K and Cu are probably adsorbed at the channel walls The framework comprises columns of pharmacoalumite-type, intergrown with chiral chains of six cis edge-shared octahedra. It can be described in terms of cubic close packing, with vacancies at both the anion and cation sites. The compositional and structural relationships between liskeardite and pharmacoalumite are discussed and a possible mechanism for liskeardite formation is presented.

Original languageEnglish
Pages (from-to)3125-3135
Number of pages11
JournalMineralogical Magazine
Volume77
Issue number8
DOIs
Publication statusPublished - Dec 2013
Externally publishedYes

Keywords

  • Chiral Chain
  • Cornwall
  • Crystal Structure
  • Liskeardite
  • Pharmacoalumite-Related
  • Uk

Cite this

@article{28d427b2a3bb4c88af029da83848eed8,
title = "Chiral edge-shared octahedral chains in liskeardite, [(Al,Fe) 32(AsO4)18(OH)42(H 2O)22]52H2O, an open framework mineral with a pharmacoalumite-related structure",
abstract = "The type specimen of liskeardite, (Al, Fe)3AsO 4(OH)65H2O, from the Marke Valley Mine, Liskeard District, Cornwall, has been reinvestigated. The revised composition from electron microprobe analyses and structure refinement is [Al 29.2Fe2.8(AsO4)18(OH) 42(H2O)22]52H2O. The crystal structure was determined using synchrotron data collected on a 2 μm diameter fibre at 100 K. Liskeardite has monoclinic symmetry, space group I2, with the unit-cell parameters a = 24.576(5), b = 7.754(2) {\AA}, c = 24.641(5) {\AA}, and β = 90.19(1)°. The structure was refined to R = 0.059 for 9769 reflections with I > 3σ(I). It is of an open framework type in which intersecting polyhedral slabs parallel to (101) and (101) form 17.4 {\AA} × 17.4 {\AA} channels along [010], with water molecules occupying the channels. Small amounts (<1 wt.{\%}) of Na, K and Cu are probably adsorbed at the channel walls The framework comprises columns of pharmacoalumite-type, intergrown with chiral chains of six cis edge-shared octahedra. It can be described in terms of cubic close packing, with vacancies at both the anion and cation sites. The compositional and structural relationships between liskeardite and pharmacoalumite are discussed and a possible mechanism for liskeardite formation is presented.",
keywords = "Chiral Chain, Cornwall, Crystal Structure, Liskeardite, Pharmacoalumite-Related, Uk",
author = "Grey, {Ian E} and Mumme, {W G} and Macrae, {C. M.} and T. Caradoc-Davies and Price, {J. R.} and Rumsey, {M. S.} and Mills, {S. J.}",
year = "2013",
month = "12",
doi = "10.1180/minmag.2013.077.8.07",
language = "English",
volume = "77",
pages = "3125--3135",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
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}

Chiral edge-shared octahedral chains in liskeardite, [(Al,Fe) 32(AsO4)18(OH)42(H 2O)22]52H2O, an open framework mineral with a pharmacoalumite-related structure. / Grey, Ian E; Mumme, W G; Macrae, C. M.; Caradoc-Davies, T.; Price, J. R.; Rumsey, M. S.; Mills, S. J.

In: Mineralogical Magazine, Vol. 77, No. 8, 12.2013, p. 3125-3135.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - Chiral edge-shared octahedral chains in liskeardite, [(Al,Fe) 32(AsO4)18(OH)42(H 2O)22]52H2O, an open framework mineral with a pharmacoalumite-related structure

AU - Grey, Ian E

AU - Mumme, W G

AU - Macrae, C. M.

AU - Caradoc-Davies, T.

AU - Price, J. R.

AU - Rumsey, M. S.

AU - Mills, S. J.

PY - 2013/12

Y1 - 2013/12

N2 - The type specimen of liskeardite, (Al, Fe)3AsO 4(OH)65H2O, from the Marke Valley Mine, Liskeard District, Cornwall, has been reinvestigated. The revised composition from electron microprobe analyses and structure refinement is [Al 29.2Fe2.8(AsO4)18(OH) 42(H2O)22]52H2O. The crystal structure was determined using synchrotron data collected on a 2 μm diameter fibre at 100 K. Liskeardite has monoclinic symmetry, space group I2, with the unit-cell parameters a = 24.576(5), b = 7.754(2) Å, c = 24.641(5) Å, and β = 90.19(1)°. The structure was refined to R = 0.059 for 9769 reflections with I > 3σ(I). It is of an open framework type in which intersecting polyhedral slabs parallel to (101) and (101) form 17.4 Å × 17.4 Å channels along [010], with water molecules occupying the channels. Small amounts (<1 wt.%) of Na, K and Cu are probably adsorbed at the channel walls The framework comprises columns of pharmacoalumite-type, intergrown with chiral chains of six cis edge-shared octahedra. It can be described in terms of cubic close packing, with vacancies at both the anion and cation sites. The compositional and structural relationships between liskeardite and pharmacoalumite are discussed and a possible mechanism for liskeardite formation is presented.

AB - The type specimen of liskeardite, (Al, Fe)3AsO 4(OH)65H2O, from the Marke Valley Mine, Liskeard District, Cornwall, has been reinvestigated. The revised composition from electron microprobe analyses and structure refinement is [Al 29.2Fe2.8(AsO4)18(OH) 42(H2O)22]52H2O. The crystal structure was determined using synchrotron data collected on a 2 μm diameter fibre at 100 K. Liskeardite has monoclinic symmetry, space group I2, with the unit-cell parameters a = 24.576(5), b = 7.754(2) Å, c = 24.641(5) Å, and β = 90.19(1)°. The structure was refined to R = 0.059 for 9769 reflections with I > 3σ(I). It is of an open framework type in which intersecting polyhedral slabs parallel to (101) and (101) form 17.4 Å × 17.4 Å channels along [010], with water molecules occupying the channels. Small amounts (<1 wt.%) of Na, K and Cu are probably adsorbed at the channel walls The framework comprises columns of pharmacoalumite-type, intergrown with chiral chains of six cis edge-shared octahedra. It can be described in terms of cubic close packing, with vacancies at both the anion and cation sites. The compositional and structural relationships between liskeardite and pharmacoalumite are discussed and a possible mechanism for liskeardite formation is presented.

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KW - Cornwall

KW - Crystal Structure

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KW - Pharmacoalumite-Related

KW - Uk

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U2 - 10.1180/minmag.2013.077.8.07

DO - 10.1180/minmag.2013.077.8.07

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