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X-ray powder diffraction (XRD) data were used to solve the crystal structures of phases in the magnesium perchlorate hydrate system, Mg(ClO
4)
2·
nH
2O (
n = 4, 2). A heating stage and humidity generator interfaced to an environmental cell enabled
in-situ XRD analyses of dehydration reactions under controlled temperatures and partial pressures of H
2O (
P). The crystal structures were determined using an
ab initio charge-flipping method and were refined using fundamental-parameter Rietveld methods. Dehydration of magnesium perchlorate hexahydrate to tetrahydrate (348 K) results in a decrease in symmetry (space group =
C2), where isolated Mg
2+ cations are equatorially coordinated by four H
2O molecules with two [ClO
4]
− tetrahedra at the apices. Further dehydration to the dihydrate (423 K) leads to bridging of the isolated packets to form double corner-sharing chains of octahedra and polyhedra (space group =
C2/
m).
Supporting information
Crystal data top
Cl2H8MgO12 | V = 504.56 (4) Å3 |
Mr = 295.27 | Z = 2 |
Monoclinic, C2 | Cu Kα radiation, λ = 1.5418 Å |
a = 11.4806 (4) Å | T = 348 K |
b = 8.0025 (3) Å | white |
c = 5.9370 (3) Å | flat sheet, 10 × 14 mm |
β = 112.328 (3)° | |
Data collection top
Bruker D8 diffractometer | Scan method: step |
Specimen mounting: Ni-Cr plated copper front loaded sample mount | 2θmin = 10°, 2θmax = 110°, 2θstep = 0.017° |
Data collection mode: reflection | |
Refinement top
Rp = 0.074 | Profile function: PVII |
Rwp = 0.104 | 52 parameters |
Rexp = 0.006 | H-atom parameters not refined |
RBragg = 0.058 | Background function: third-order Chebyshev polynomial |
8383 data points | Preferred orientation correction: sixth-order spherical harmonics |
Excluded region(s): 89.5 to 90.5 2θ | |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Cl | 0.70333 | 1 | 0.10907 | 0.4 | |
Mg | 1 | 1 | 0.5 | 0.8 | |
O1 | 0.333333 | 0.5 | 0.166667 | 1.2 | |
O2 | 0.166667 | 0.66083 | 0.15301 | 1.2 | |
O3 | 0.833333 | 0.37593 | 0.76325 | 1.2 | |
O4 | 0.5 | 0.23849 | 0.5 | 1.2 | |
O5 | 1 | 0.27036 | 0.5 | 1.2 | |
O6 | 0.65143 | 0.97079 | 0.85351 | 1.2 | |
O7 | 0.89363 | 1.01313 | 0.72724 | 1.2 | |
H1 | 0.54733 | 0.8735 | 0.56476 | 1 | |
H2 | 0.93783 | 0.65429 | 0.43875 | 1 | |
H3 | 0.5796 | 0.50118 | 0.09709 | 1 | |
H4 | 0.30059 | 0.50382 | 0.71989 | 1 | |
Crystal data top
Cl2H4MgO10 | V = 387.89 (3) Å3 |
Mr = 259.24 | Z = 2 |
Monoclinic, C2/m | Cu Kα radiation, λ = 1.5418 Å |
a = 14.3878 (6) Å | T = 423 K |
b = 5.21861 (19) Å | white |
c = 5.4380 (3) Å | flat sheet, 10 × 14 mm |
β = 108.199 (2)° | |
Data collection top
Bruker D8 diffractometer | Scan method: step |
Specimen mounting: Ni-Cr plated copper front loaded sample mount | 2θmin = 10°, 2θmax = 110°, 2θstep = 0.017° |
Data collection mode: reflection | |
Refinement top
Rp = 0.053 | Profile function: PVII |
Rwp = 0.078 | 25 parameters |
Rexp = 0.012 | H-atom parameters not refined |
RBragg = 0.036 | Background function: third-order Chebyshev polynomial |
8383 data points | Preferred orientation correction: sixth-order spherical harmonics |
Excluded region(s): 89.5 to 90.5 2θ | |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Mg | 0 | 0 | 0.5 | 0.8 | |
Cl | 0.62578 | 1 | 0.83043 | 0.4 | |
O1 | 0.38167 | 0.5 | 0.64837 | 1.2 | |
O2 | 0.32043 | 1 | 0.89 | 1.2 | |
O3 | 0.05762 | 0.25 | 0.79317 | 1.2 | |
O4 | 0.31265 | 1 | 0.34525 | 1.2 | |
H | 0.67187 | 0.62617 | 0.43766 | 1 | |
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