energy materials
The crystal structure of the higher manganese silicide MnSi1.7 (known in the literature as HMS) is investigated in samples with different compositions obtained by different techniques at temperatures not higher than 1273 K. Powder X-ray diffraction was applied. The crystal structure is described as incommensurate composite. In addition to the ordered model already known in the literature, the partial disorder in the silicon substructure was detected and described introducing an additional atomic site with a different modulation function.
Keywords: higher magnesium silicide; non-commensurate composite crystal structure; disorder; powder X-ray diffraction.
Supporting information
Crystallographic Information File (CIF) https://doi.org/10.1107/S2052520615019757/kc5025sup1.cif | |
Rietveld powder data file (CIF format) https://doi.org/10.1107/S2052520615019757/kc5025Isup2.rtv |
B-IncStrDB reference: 11402EFCaNO
CCDC reference: 1432489
Computing details top
Cell refinement: WinCSD; data reduction: WinCSD; program(s) used to solve structure: WinCSD; program(s) used to refine structure: WinCSD; software used to prepare material for publication: WinCSD (Akselrud et al., 1993).
(I) top
Crystal data top
Mn2Si3.5 | Z = 2 |
Tetragonal, I41/amd(00p)00ss† | F(000) = 198.7 |
q1 = 1.7374c*; q2 = 0.5756c* | Dx = 5.213 Mg m−3 |
a = 5.5235 (3) Å | Cu Kα1 radiation, λ = 1.54061 Å |
c = 4.3634 (3) Å | T = 295 K |
V = 133.13 (2) Å3 | 25 × 25 mm |
† Symmetry operations: (1) +x1, +x2, +x3, +x4; (2) −x1, +x2, +x3, 1/2+x4; (3) 3/4+x2, 3/4−x1, 1/4+x3, +x4; (4) 1/2+x1, −x2, 1/2+x3, 1/2+x4; (5) 1/4−x2, 3/4−x1, 1/4+x3, 1/2+x4; (6) 1/2−x1, −x2, 1/2+x3, +x4; (7) 1/4+x2, 1/4+x1, 3/4+x3, 1/2+x4; (8) 3/4−x2, 1/4+x1, 3/4+x3, +x4; (9) −x1, −x2, −x3, −x4; (10) +x1, −x2, −x3, −1/2−x4; (11) −3/4−x2, −3/4+x1, −1/4−x3, −x4; (12) −1/2−x1, +x2, −1/2−x3, −1/2−x4; (13) −1/4+x2, −3/4+x1, −1/4−x3, −1/2−x4; (14) −1/2+x1, +x2, −1/2−x3, −x4; (15) −1/4−x2, −1/4−x1, −3/4−x3, −1/2−x4; (16) −3/4+x2, −1/4−x1, −3/4−x3, −x4; (17) 1/2+x1, 1/2+x2, 1/2+x3, +x4; (18) 1/2−x1, 1/2+x2, 1/2+x3, 1/2+x4; (19) 1/4+x2, 1/4−x1, 3/4+x3, +x4; (20) +x1, 1/2−x2, +x3, 1/2+x4; (21) 3/4−x2, 1/4−x1, 3/4+x3, 1/2+x4; (22) −x1, 1/2−x2, +x3, +x4; (23) 3/4+x2, 3/4+x1, 1/4+x3, 1/2+x4; (24) 1/4−x2, 3/4+x1, 1/4+x3, +x4; (25) −1/2−x1, −1/2−x2, −1/2−x3, −x4; (26) −1/2+x1, −1/2−x2, −1/2−x3, −1/2−x4; (27) −1/4−x2, −1/4+x1, −3/4−x3, −x4; (28) −x1, −1/2+x2, −x3, −1/2−x4; (29) −3/4+x2, −1/4+x1, −3/4−x3, −1/2−x4; (30) +x1, −1/2+x2, −x3, −x4; (31) −3/4−x2, −3/4−x1, −1/4−x3, −1/2−x4; (32) −1/4+x2, −3/4−x1, −1/4−x3, −x4. |
Data collection top
Huber Guinier G670 diffractometer | Scan method: step |
Radiation source: sealed X-ray tube, GE ID-3003 | 2θmin = 15.0°, 2θmax = 100.3°, 2θstep = 0.005° |
Specimen mounting: packed powder pellet |
Refinement top
Least-squares matrix: full with fixed elements per cycle | 0 parameters |
Rp = 0.112 | 1/sqrt[Yi] |
Rwp = 0.087 | (Δ/σ)max = 0.032 |
Profile function: pseudo-Voit |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
x | y | z | Biso*/Beq | Occ. (<1) | |
Mn | 0 | 0.25 | 0.375 | 0.70 (6)* | 0.850 (4) |
Si1 | 0.181 (2) | 0.379 (2) | 0.825 (3) | 0.8 (2)* | 0.106 (3) |
Mn1 | 0.181 (2) | 0.379 (2) | 0.825 (3) | 0.8 (2)* | 0.019 (3) |
Si2 | 0.25 | 0 | 0.75 | 0.9 (6)* | 0.52 (5) |