Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O
A wide compositional range, covering about 90% of an expected erythrite-köttigite substitutional solid solution with extreme compositions of (Co<sub>2.84</sub>Mg<sub>0.14</sub>Zn<sub>0.02</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2&...
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doaj-680c321eec904956bd6a673200a1be072020-11-25T04:02:41ZengMDPI AGMinerals2075-163X2020-06-011054854810.3390/min10060548Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>OJustyna Ciesielczuk0Mateusz Dulski1Janusz Janeczek2Tomasz Krzykawski3Joachim Kusz4Eligiusz Szełęg5Institute of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, PolandInstitute of Materials Engineering, University of Silesia, 75 Pułku Piechoty 1a, 41-500 Chorzów, PolandInstitute of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, PolandInstitute of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, PolandInstitute of Physics, University of Silesia, 75 Pułku Piechoty 1, 41-500 Chorzów, PolandInstitute of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, PolandA wide compositional range, covering about 90% of an expected erythrite-köttigite substitutional solid solution with extreme compositions of (Co<sub>2.84</sub>Mg<sub>0.14</sub>Zn<sub>0.02</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O and (Zn<sub>2.74</sub>Co<sub>0.27</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O, was revealed in a suite of samples from a polymetallic ore deposit in Miedzianka, SW Poland. Members of the solid solution series were examined by means of Electron Probe Microanalysis (EPMA), Scanning Electron Microscopy (SEM)/Energy-Dispersive Spectrometer (EDS), X-ray single-crystal and powder diffraction, and Raman spectroscopy. Metal cations were randomly distributed between two special octahedral sites in the erythrite–köttigite structure. In response to Co ↔ Zn substitutions, small but significant changes in bond distances (particularly in [AsO<sub>4</sub>] tetrahedra), rotation, and distortion of co-ordination polyhedra were observed. Two sub-series of dominant cationic substitutions (Co-Mg-Ni and Co-Fe-Zn) were noted within the arsenate series of vivianite-group minerals linked by erythrite. The paragenetic sequence erythrite → Zn-rich erythrite → Co-rich köttigite → köttigite reflects the evolution of the solution’s pH towards increased acidity and a relative increase in the concentration of Zn ions following precipitation of erythrite.https://www.mdpi.com/2075-163X/10/6/548erythriteköttigitesolid solutionarsenate seriesvivianite-group mineralsstructure refinement |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Justyna Ciesielczuk Mateusz Dulski Janusz Janeczek Tomasz Krzykawski Joachim Kusz Eligiusz Szełęg |
spellingShingle |
Justyna Ciesielczuk Mateusz Dulski Janusz Janeczek Tomasz Krzykawski Joachim Kusz Eligiusz Szełęg Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O Minerals erythrite köttigite solid solution arsenate series vivianite-group minerals structure refinement |
author_facet |
Justyna Ciesielczuk Mateusz Dulski Janusz Janeczek Tomasz Krzykawski Joachim Kusz Eligiusz Szełęg |
author_sort |
Justyna Ciesielczuk |
title |
Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O |
title_short |
Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O |
title_full |
Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O |
title_fullStr |
Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O |
title_full_unstemmed |
Crystal Chemistry of an Erythrite-Köttigite Solid Solution (Co<sub>3–x</sub>Zn<sub>x</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O |
title_sort |
crystal chemistry of an erythrite-köttigite solid solution (co<sub>3–x</sub>zn<sub>x</sub>) (aso<sub>4</sub>)<sub>2</sub>·8h<sub>2</sub>o |
publisher |
MDPI AG |
series |
Minerals |
issn |
2075-163X |
publishDate |
2020-06-01 |
description |
A wide compositional range, covering about 90% of an expected erythrite-köttigite substitutional solid solution with extreme compositions of (Co<sub>2.84</sub>Mg<sub>0.14</sub>Zn<sub>0.02</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O and (Zn<sub>2.74</sub>Co<sub>0.27</sub>) (AsO<sub>4</sub>)<sub>2</sub>·8H<sub>2</sub>O, was revealed in a suite of samples from a polymetallic ore deposit in Miedzianka, SW Poland. Members of the solid solution series were examined by means of Electron Probe Microanalysis (EPMA), Scanning Electron Microscopy (SEM)/Energy-Dispersive Spectrometer (EDS), X-ray single-crystal and powder diffraction, and Raman spectroscopy. Metal cations were randomly distributed between two special octahedral sites in the erythrite–köttigite structure. In response to Co ↔ Zn substitutions, small but significant changes in bond distances (particularly in [AsO<sub>4</sub>] tetrahedra), rotation, and distortion of co-ordination polyhedra were observed. Two sub-series of dominant cationic substitutions (Co-Mg-Ni and Co-Fe-Zn) were noted within the arsenate series of vivianite-group minerals linked by erythrite. The paragenetic sequence erythrite → Zn-rich erythrite → Co-rich köttigite → köttigite reflects the evolution of the solution’s pH towards increased acidity and a relative increase in the concentration of Zn ions following precipitation of erythrite. |
topic |
erythrite köttigite solid solution arsenate series vivianite-group minerals structure refinement |
url |
https://www.mdpi.com/2075-163X/10/6/548 |
work_keys_str_mv |
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