research communications
of iron(III) perchlorate nonahydrate
aTU Bergakademie Freiberg, Institute of Inorganic Chemistry, Leipziger Strasse 29, D-09596 Freiberg, Germany
*Correspondence e-mail: Horst.Schmidt@chemie.tu-freiberg.de
Since the discovery of perchlorate salts on Mars and the known occurrence of ferric salts in the regolith, there is a distinct possibility that the title compound could form on the surface of Mars. [Fe(H2O)6](ClO4)3·3H2O was crystallized from aqueous solutions at low temperatures according to the solid–liquid phase diagram. It consists of Fe(H2O)6 octahedra (point group symmetry -3.) and perchlorate anions (point group symmetry .2) as well as non-coordinating water molecules, as part of a second hydrogen-bonded coordination sphere around the cation. The perchlorate appears to be slightly disordered, with major–minor component occupancies of 0.773 (9):0.227 (9).
Keywords: crystal structure; low-temperature salt hydrates; perchlorate hydrates; iron perchlorate; Mars.
CCDC reference: 1032663
1. Chemical context
Since the discovery of perchlorate salts on the surface of Mars during the Phoenix expedition (Hecht et al., 2009; Davila et al., 2013; Kerr, 2013; Marion et al., 2010; Navarro-González et al., 2010), interest in the solubility and crystal structures of the perchlorate hydrate phases became more important (Chevrier, Hanley & Altheide, 2009; Catling et al., 2010). Based on the red color of the planet, one can expect different iron phases, such as perchlorate and sulfate, to be important constituents of the regolith (Chevrier, Ulrich & Altheide, 2009; Chevrier & Altheide, 2008; Hennings et al., 2013). While investigating the solubility of ferric perchlorate, we obtained the nonahydrate as a stable phase in the binary salt–water system.
2. Structural commentary
The central Fe atom is situated on a threefold inversion axis and is octahedrally coordinated by six water molecules in the first, and by six water molecules as well as six perchlorate tetrahedra in the second coordination spheres (Fig. 1). The water molecules of the second coordination sphere (O4 and symmetry equivalents) are connected to perchlorate tetrahedra (Fig. 2a) via hydrogen bonds (Table 1). Six O4-water molecules form a second, larger octahedron outside the octahedron of the first coordination shell (Fig. 2b). The perchlorate anion, situated on a twofold rotation axis, appears to be slightly disordered, with major:minor component occupancies of 0.773 (9):0.227 (9).
3. Supramolecular features
From the a), it is obvious that the O4 atoms form a secondary hydration shell around the Fe(H2O)6 units. This becomes clearer when drawing the second octahedra as water coordination polyhedra (yellow, Fig. 3b). The water molecules of the second coordination sphere are closer [4.143 (4) Å] to the Fe atom than the perchlorate tetrahedra [4.271 (4) Å].
of ferric perchlorate nonahydrate (Fig. 34. Database survey
For et al. (2012) for the Al, Ga and Sc salts and Hennings et al. (2014) for the strontium salt. For determinations of other FeIII salts with a high water content, see: Schmidt et al. (2013); Lindstrand (1936).
determination of other perchlorate nonahydrates, see: Davidian5. Synthesis and crystallization
Iron(III) perchlorate nonahydrate crystallized from an aqueous solution of 54.41 wt% Fe(ClO4)3 thermostated at 263 K after 2 d. To prepare this solution, ferric perchlorate nonahydrate (Fluka, pure) was used. The content of FeIII ions was analysed using gravimetric analysis by precipitation with ammonia. All crystals are stable in their over a period of at least four weeks.
The samples were stored in a freezer or a cryostat at low temperatures. The crystals were separated and embedded in perfluorinated ether for X-ray diffraction analysis
6. Refinement
Crystal data, data collection and structure . The H atoms were placed in the positions indicated by difference Fourier maps. No further constraints were applied.
details are summarized in Table 2
|
Supporting information
CCDC reference: 1032663
10.1107/S1600536814024295/pk2533sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: 10.1107/S1600536814024295/pk2533Isup2.hkl
Since the discovery of perchlorate salts on the surface of Mars during the Phoenix expedition (Hecht et al., 2009), interest in the solubility and crystal structures of the perchlorate hydrate phases became more important (Chevrier, Hanley & Altheide, 2009). Based on the red color of the planet, one can expect different iron phases, such as perchlorate and sulfate, to be important constituents of the regolith (Chevrier, Ulrich & Altheide, 2009; Chevrier & Altheide, 2008; Hennings et al., 2013). While investigating the solubility of ferric perchlorate, we obtained the nonahydrate as a stable phase in a binary salt–water system.
The central Fe atom is octahedrally coordinated by six water molecules in the first, and by six water molecules as well as six perchlorate tetrahedra in the second coordination spheres. The water molecules of the second coordination sphere (O4 and symmetry equivalents) are connected to perchlorate tetrahedra (Fig. 2a) via hydrogen bonds (Table 1). Six O4-water molecules form a second, larger octahedron outside the octahedron of the first coordination shell (Fig. 2b). The perchlorate anion appears to be slightly disordered, with major:minor component occupancies of 0.773 (9):0.227 (9).
From the
of ferric perchlorate nonahydrate (Fig. 3a), it is obvious that the O4 atoms form a secondary hydration shell around the Fe(H2O)6 units. This becomes clearer when drawing the second octahedra as water coordination polyhedra (yellow, Fig. 3b). The water molecules of the second coordination sphere are closer [4.143 (4) Å] to the Fe atom than the perchlorate tetrahedra [4.271 (4) Å].For
determination of other perchlorate nonahydrates, see Davidian et al. (2012) and Hennings et al. (2014). For determinations of other FeIII salts with a high water content, see Schmidt et al. (2013).Iron(III) perchlorate nonahydrate crystallized from an aqueous solution of 54.41 wt% Fe(ClO4)3 thermostated at 263 K after 2 d. To prepare this solution, ferric perchlorate nonahydrate (Fluka, pure) was used. The content of FeIII ions was analysed using gravimetric analysis by precipitation with ammonia. All crystals are stable in their
over a period of at least four weeks.The samples were stored in a freezer or a cryostat at low temperatures. The crystals were separated and embedded in perfluorinated ether for X-ray diffraction analysis
Data collection: X-AREA (Stoe & Cie, 2009); cell
X-AREA (Stoe & Cie, 2009); data reduction: X-RED (Stoe & Cie, 2009); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL2012 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).The molecular unit (a) and second coordination sphere (b) of ferric perchlorate nonahydrate. Dashed lines indicate hydrogen bonds. Displacement ellipsoids are drawn at the 50% probability limit. The minor disorder component has been omitted. [Symmetry codes: (i) x-y, -y, 1/2 - z; (ii) -y, x-y, z; (iii) x, x-y, 1/2 + z.] The connection scheme of water molecules of the second coordination sphere by hydrogen bonds (a) and the formation of a secondary hydration shell (yellow) around the cations (b). The minor disorder component has been omitted for clarity. Dashed lines indicate hydrogen bonds. The of iron(III) perchlorate nonahydrate with coordination polyhedra of the first (a) and second (b) coordination sphere. The minor disorder component has been omitted for clarity. Dashed lines indicate hydrogen bonds. |
[Fe(H2O)6](ClO4)3·3H2O | Dx = 2.015 Mg m−3 |
Mr = 516.34 | Mo Kα radiation, λ = 0.71073 Å |
Trigonal, R3c:H | Cell parameters from 47287 reflections |
a = 16.1930 (15) Å | θ = 7.0–29.7° |
c = 11.2421 (11) Å | µ = 1.46 mm−1 |
V = 2552.9 (5) Å3 | T = 100 K |
Z = 6 | Needle, colorless |
F(000) = 1578 | 0.54 × 0.37 × 0.19 mm |
STOE IPDS 2T diffractometer | 659 independent reflections |
Radiation source: fine-focus sealed tube | 641 reflections with I > 2σ(I) |
Detector resolution: 6.67 pixels mm-1 | Rint = 0.075 |
rotation method scans | θmax = 27.5°, θmin = 2.5° |
Absorption correction: integration (Coppens, 1970) | h = −20→20 |
Tmin = 0.531, Tmax = 0.755 | k = −20→20 |
8865 measured reflections | l = −14→14 |
Refinement on F2 | 0 restraints |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.041 | All H-atom parameters refined |
wR(F2) = 0.092 | w = 1/[σ2(Fo2) + (0.0269P)2 + 23.9134P] where P = (Fo2 + 2Fc2)/3 |
S = 1.11 | (Δ/σ)max < 0.001 |
658 reflections | Δρmax = 0.64 e Å−3 |
60 parameters | Δρmin = −0.80 e Å−3 |
[Fe(H2O)6](ClO4)3·3H2O | Z = 6 |
Mr = 516.34 | Mo Kα radiation |
Trigonal, R3c:H | µ = 1.46 mm−1 |
a = 16.1930 (15) Å | T = 100 K |
c = 11.2421 (11) Å | 0.54 × 0.37 × 0.19 mm |
V = 2552.9 (5) Å3 |
STOE IPDS 2T diffractometer | 659 independent reflections |
Absorption correction: integration (Coppens, 1970) | 641 reflections with I > 2σ(I) |
Tmin = 0.531, Tmax = 0.755 | Rint = 0.075 |
8865 measured reflections |
R[F2 > 2σ(F2)] = 0.041 | 0 restraints |
wR(F2) = 0.092 | All H-atom parameters refined |
S = 1.11 | w = 1/[σ2(Fo2) + (0.0269P)2 + 23.9134P] where P = (Fo2 + 2Fc2)/3 |
658 reflections | Δρmax = 0.64 e Å−3 |
60 parameters | Δρmin = −0.80 e Å−3 |
Geometry. All esds (except the esd in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell esds are taken into account individually in the estimation of esds in distances, angles and torsion angles; correlations between esds in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell esds is used for estimating esds involving l.s. planes. |
x | y | z | Uiso*/Ueq | Occ. (<1) | |
Fe1 | 0.0000 | 0.0000 | 0.5000 | 0.0188 (3) | |
O1 | 0.07420 (15) | 0.11666 (15) | 0.3991 (2) | 0.0252 (5) | |
O4 | 0.3333 | 0.47858 (17) | 0.4167 | 0.0247 (6) | |
Cl1 | 0.3333 | 0.2540 (19) | 0.4167 | 0.0329 (3) | 0.773 (9) |
O2 | 0.4134 (3) | 0.3438 (3) | 0.3808 (4) | 0.0342 (8) | 0.773 (9) |
O3 | 0.3070 (3) | 0.1914 (3) | 0.3110 (4) | 0.0481 (12) | 0.773 (9) |
Cl1' | 0.3333 | 0.254 (7) | 0.4167 | 0.0329 (3) | 0.227 (9) |
O2' | 0.3946 (11) | 0.3499 (13) | 0.3527 (16) | 0.0342 (8) | 0.227 (9) |
O3' | 0.2699 (12) | 0.1716 (10) | 0.3602 (15) | 0.0481 (12) | 0.227 (9) |
H1A | 0.129 (3) | 0.158 (3) | 0.417 (4) | 0.047 (12)* | |
H1B | 0.048 (3) | 0.138 (3) | 0.357 (4) | 0.051 (13)* | |
H4 | 0.375 (3) | 0.468 (3) | 0.388 (4) | 0.054 (13)* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Fe1 | 0.0157 (3) | 0.0157 (3) | 0.0251 (5) | 0.00784 (15) | 0.000 | 0.000 |
O1 | 0.0165 (10) | 0.0195 (10) | 0.0341 (11) | 0.0050 (8) | −0.0004 (8) | 0.0045 (8) |
O4 | 0.0269 (15) | 0.0164 (9) | 0.0344 (16) | 0.0135 (8) | 0.0102 (12) | 0.0051 (6) |
Cl1 | 0.0221 (5) | 0.0137 (4) | 0.0659 (8) | 0.0110 (2) | −0.0180 (5) | −0.0090 (2) |
O2 | 0.0180 (19) | 0.0381 (15) | 0.051 (2) | 0.0174 (13) | −0.0027 (15) | 0.0098 (16) |
O3 | 0.045 (3) | 0.0345 (19) | 0.067 (3) | 0.0210 (19) | −0.0055 (19) | −0.0276 (19) |
Cl1' | 0.0221 (5) | 0.0137 (4) | 0.0659 (8) | 0.0110 (2) | −0.0180 (5) | −0.0090 (2) |
O2' | 0.0180 (19) | 0.0381 (15) | 0.051 (2) | 0.0174 (13) | −0.0027 (15) | 0.0098 (16) |
O3' | 0.045 (3) | 0.0345 (19) | 0.067 (3) | 0.0210 (19) | −0.0055 (19) | −0.0276 (19) |
Fe1—O1i | 2.007 (2) | Cl1—O2 | 1.439 (18) |
Fe1—O1ii | 2.007 (2) | Cl1—O3vi | 1.479 (17) |
Fe1—O1iii | 2.007 (2) | Cl1—O3 | 1.479 (17) |
Fe1—O1iv | 2.007 (2) | Cl1'—O3'vi | 1.37 (6) |
Fe1—O1v | 2.007 (2) | Cl1'—O3' | 1.37 (6) |
Fe1—O1 | 2.007 (2) | Cl1'—O2'vi | 1.54 (7) |
Cl1—O2vi | 1.439 (18) | Cl1'—O2' | 1.54 (7) |
O1i—Fe1—O1ii | 180.00 (9) | O1v—Fe1—O1 | 180.00 (10) |
O1i—Fe1—O1iii | 91.19 (9) | O2vi—Cl1—O2 | 112 (2) |
O1ii—Fe1—O1iii | 88.81 (9) | O2vi—Cl1—O3vi | 105.8 (3) |
O1i—Fe1—O1iv | 88.81 (9) | O2—Cl1—O3vi | 109.42 (19) |
O1ii—Fe1—O1iv | 91.19 (9) | O2vi—Cl1—O3 | 109.42 (19) |
O1iii—Fe1—O1iv | 180.00 (10) | O2—Cl1—O3 | 105.8 (3) |
O1i—Fe1—O1v | 91.19 (9) | O3vi—Cl1—O3 | 114 (2) |
O1ii—Fe1—O1v | 88.81 (9) | O3'vi—Cl1'—O3' | 106 (7) |
O1iii—Fe1—O1v | 91.19 (9) | O3'vi—Cl1'—O2'vi | 124.0 (13) |
O1iv—Fe1—O1v | 88.81 (9) | O3'—Cl1'—O2'vi | 105.4 (10) |
O1i—Fe1—O1 | 88.81 (9) | O3'vi—Cl1'—O2' | 105.4 (10) |
O1ii—Fe1—O1 | 91.19 (9) | O3'—Cl1'—O2' | 124.0 (13) |
O1iii—Fe1—O1 | 88.81 (9) | O2'vi—Cl1'—O2' | 94 (6) |
O1iv—Fe1—O1 | 91.19 (9) |
Symmetry codes: (i) y, −x+y, −z+1; (ii) −y, x−y, z; (iii) x−y, x, −z+1; (iv) −x+y, −x, z; (v) −x, −y, −z+1; (vi) −x+2/3, −x+y+1/3, −z+5/6. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1A···Cl1 | 0.83 (5) | 2.86 (5) | 3.642 (2) | 157 (4) |
O1—H1A···O2vi | 0.83 (5) | 1.92 (5) | 2.745 (5) | 174 (4) |
O1—H1A···O2′vi | 0.83 (5) | 2.33 (5) | 3.153 (14) | 170 (4) |
O1—H1A···O3′ | 0.83 (5) | 2.27 (5) | 2.864 (17) | 129 (4) |
O1—H1B···O4vii | 0.82 (5) | 1.83 (5) | 2.642 (3) | 173 (4) |
O4—H4···O2 | 0.84 (4) | 2.39 (4) | 3.073 (5) | 139 (4) |
O4—H4···O3viii | 0.84 (4) | 2.13 (4) | 2.796 (4) | 136 (4) |
O4—H4···O2′ | 0.84 (4) | 2.13 (5) | 2.812 (17) | 138 (4) |
O4—H4···O3′viii | 0.84 (4) | 2.12 (4) | 2.708 (12) | 127 (4) |
Symmetry codes: (vi) −x+2/3, −x+y+1/3, −z+5/6; (vii) −x+1/3, −y+2/3, −z+2/3; (viii) y+1/3, −x+y+2/3, −z+2/3. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1A···Cl1 | 0.83 (5) | 2.86 (5) | 3.642 (2) | 157 (4) |
O1—H1A···O2i | 0.83 (5) | 1.92 (5) | 2.745 (5) | 174 (4) |
O1—H1A···O2'i | 0.83 (5) | 2.33 (5) | 3.153 (14) | 170 (4) |
O1—H1A···O3' | 0.83 (5) | 2.27 (5) | 2.864 (17) | 129 (4) |
O1—H1B···O4ii | 0.82 (5) | 1.83 (5) | 2.642 (3) | 173 (4) |
O4—H4···O2 | 0.84 (4) | 2.39 (4) | 3.073 (5) | 139 (4) |
O4—H4···O3iii | 0.84 (4) | 2.13 (4) | 2.796 (4) | 136 (4) |
O4—H4···O2' | 0.84 (4) | 2.13 (5) | 2.812 (17) | 138 (4) |
O4—H4···O3'iii | 0.84 (4) | 2.12 (4) | 2.708 (12) | 127 (4) |
Symmetry codes: (i) −x+2/3, −x+y+1/3, −z+5/6; (ii) −x+1/3, −y+2/3, −z+2/3; (iii) y+1/3, −x+y+2/3, −z+2/3. |
Experimental details
Crystal data | |
Chemical formula | [Fe(H2O)6](ClO4)3·3H2O |
Mr | 516.34 |
Crystal system, space group | Trigonal, R3c:H |
Temperature (K) | 100 |
a, c (Å) | 16.1930 (15), 11.2421 (11) |
V (Å3) | 2552.9 (5) |
Z | 6 |
Radiation type | Mo Kα |
µ (mm−1) | 1.46 |
Crystal size (mm) | 0.54 × 0.37 × 0.19 |
Data collection | |
Diffractometer | STOE IPDS 2T diffractometer |
Absorption correction | Integration (Coppens, 1970) |
Tmin, Tmax | 0.531, 0.755 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 8865, 659, 641 |
Rint | 0.075 |
(sin θ/λ)max (Å−1) | 0.650 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.041, 0.092, 1.11 |
No. of reflections | 658 |
No. of parameters | 60 |
H-atom treatment | All H-atom parameters refined |
w = 1/[σ2(Fo2) + (0.0269P)2 + 23.9134P] where P = (Fo2 + 2Fc2)/3 | |
Δρmax, Δρmin (e Å−3) | 0.64, −0.80 |
Computer programs: X-AREA (Stoe & Cie, 2009), X-RED (Stoe & Cie, 2009), SHELXS97 (Sheldrick, 2008), SHELXL2012 (Sheldrick, 2008), DIAMOND (Brandenburg, 2006), publCIF (Westrip, 2010).
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