2017
DOI: 10.1002/zaac.201700342
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Oxocentered Units in Three Novel Rb‐Containing Copper Compounds Prepared by CVT Reaction Method

Abstract: Three novel copper compounds, Rb 4 Cu 4 OCl 10 (I), Rb[Cu 3 O](SeO 3 ) 2 Cl (II), and RbCu 3 (OH)(SeO 3 )Cl 4 (H 2 O) 3 (III) were prepared by chemical vapor transport (CVT) reactions method from mixtures of CuO, SeO 2 , RbCl, and CuCl 2 . The crystal structures of the three compounds were determined by direct methods. Compound I is a Rb analogue of ponomarevite, K 4 Cu 4 OCl 10 . Its crystal structure contains {[OCu 4 ]Cl 10 } 4clusters with oxocentered [OCu 4 ] 6+ tetrahedra as * Prof. Dr. S. V. Krivovichev … Show more

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“…Kondinski clusters (M = Fe 3+ , Ti 4+ ) in arsmirandite and lehmannite found in Tolbachik fumaroles provides a useful clue for the targeted synthesis of their analogues under laboratory conditions. As it has been demonstrated previously [49][50][51] , fumarolic minerals with oxocentered cores can be conveniently synthesized using chemical vapor transport techniques. The occurrence of the [M⊂Cu 12 O 8 (AsO 4 ) 8 ] q− nanoclusters in Tolbachik fumaroles testifies that they are stable under high temperatures (500-700 °C) at least in the gaseous and crystalline phases and may as well possess interesting physical and chemical properties.…”
Section: Discussionmentioning
confidence: 99%
“…Kondinski clusters (M = Fe 3+ , Ti 4+ ) in arsmirandite and lehmannite found in Tolbachik fumaroles provides a useful clue for the targeted synthesis of their analogues under laboratory conditions. As it has been demonstrated previously [49][50][51] , fumarolic minerals with oxocentered cores can be conveniently synthesized using chemical vapor transport techniques. The occurrence of the [M⊂Cu 12 O 8 (AsO 4 ) 8 ] q− nanoclusters in Tolbachik fumaroles testifies that they are stable under high temperatures (500-700 °C) at least in the gaseous and crystalline phases and may as well possess interesting physical and chemical properties.…”
Section: Discussionmentioning
confidence: 99%