Crystal structures of the double salt dihydrates K<sub>2</sub>Cd(SeO<sub>4</sub>)<sub>2</sub>·2H<sub>2</sub>O, K<sub>2</sub>Mn(SO<sub>4</sub>)<sub>2</sub>·2H<sub>2</sub>O, (NH<sub>4</sub>)<sub>2</sub>Cu(SeO<sub>4</sub>)<sub>2</sub>·2H<sub>2</sub>O and KFeH(SO<sub>4</sub>)<sub>2</sub>·2H<sub>2</sub>O

Autor(en)
Michel Fleck, Uwe Kolitsch, Birgit Hertweck, Gerald Giester, Manfred Wildner, Markus Prem, Astrid Wohlschläger
Abstrakt

The crystal structures of the four synthetic double salt compounds K2Mn(SO4)2·2H2O (space group P1̅, no. 2, Z = 2, a = 6.574(1), b = 7.332(1), c = 10.700(1) Å, α = 72.89(1), β = 73.91(1), γ = 69.77(1)°, V = 453.6(1) Å3) and K2Cd(SeO4)2·2H2O(space group P1̅, no. 2, Z = 2, a = 6.625(1), b = 7.542(1), c = 11.349(1) Å, α = 72.17(1), β = 74.55(1), γ = 70.13(1)°, V = 499.3(1) Å3) as well as (NH4)2Cu(SeO4)2·2H2O (space group P1̅, no. 2, Z = 1, a = 5.784(1) Å, b = 7.107(1) Å, c = 7.371(1) Å, α = 104.21(2)°, β = 93.04(2)°, γ = 112.27(2)°, V = 268.19(7) Å3), and KFeH(SO4)2·2H2O(space group P1̅, no. 2, Z = 1, a = 4.626(1), b = 5.820(1), c = 8.265(1) Å, α = 103.86(1), β = 99.77(1), γ = 95.66(1)°, V = 210.64(2) Å3) have been determined from single-crystal X-ray diffraction data collected with a CCD area detector at 293 K, and were refined to R(F) = 0.0231, 0.0251, 0.0230 and 0.0194, respectively. The first two compounds are isostructural. The atomic arrangements are described, with a focus on the hydrogen bonding. All compounds contain kröhnkite [Na2Cu(SO4)2·2H2O]-type tetrahedral-octahedral chains but show different topological arrangements of these chains. A classification is proposed in an accompanying paper. A particular feature of KFeH(SO4)2·2H2O is a disordered H atom involved in a short hydrogen bond, which shows no ordering down to 110 K.

Organisation(en)
Institut für Mineralogie und Kristallographie
Journal
Zeitschrift für Kristallographie : international journal for structural, physical, and chemical aspects of crystalline materials
Band
217
Seiten
242-248
Anzahl der Seiten
7
ISSN
0044-2968
DOI
https://doi.org/10.1524/zkri.217.6.242.22812
Publikationsdatum
2002
Peer-reviewed
Ja
ÖFOS 2012
1051 Geologie, Mineralogie
Link zum Portal
https://ucrisportal.univie.ac.at/de/publications/59c2422f-9cc2-4471-a316-cb55683570c6