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      The crystal structure of caratiite

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      Mineralogical Magazine
      Mineralogical Society

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          Abstract

          The crystal structure of caratiite, K 4Cu 4O 2 (SO 4) 4 MeCl ( a 13.60(2), c 4.98(1) Å, Z = 2) was solved in space group I4 from single crystal data, and refined to R = 0.035 for 654F o > 6 σ(F o). The atomic arrangement is characterized by Cu 2O(SO 4) 2 chains parallel to [001], with Cu in (4 + 1) co-ordination and O surrounded tetrahedrally by four Cu atoms. These chains are interconnected by K atoms to a framework, the channels of which house the Me and Cl atoms. The nature of the Me atoms is not completely clear; most probably the position is half occupied by Cu, fully occupied by Na, or occupied by a mixture of the two.

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          Most cited references9

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          A general theory of X-ray diffraction in crystals

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            On the crystal chemistry of salt hydrates. IV. The refinement of the crystal structure of MgSO4.7H2O (epsomite)

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              The crystal structure of atacamite and the crystal chemistry of cupric compounds

              A Wells (1949)
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                Author and article information

                Journal
                Mineralogical Magazine
                Mineral. mag.
                Mineralogical Society
                0026-461X
                1471-8022
                December 1984
                July 05 2018
                December 1984
                : 48
                : 349
                : 541-546
                Article
                10.1180/minmag.1984.048.349.10
                c6ddd965-19e5-454d-bada-7c95fe96b10f
                © 1984

                https://www.cambridge.org/core/terms

                History

                Biochemistry,Animal science & Zoology
                Biochemistry, Animal science & Zoology

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