Kieserite
Talla D, Wildner M
American Mineralogist 104 (2019) 1732-1749
Investigation of the kieserite-szomolnokite solid-solution series, (Mg,Fe)SO4*H2O,
with relevance to Mars: Crystal chemistry, FTIR, and Raman spectroscopy
under ambient and martian temperature conditions
Note: T = -160 C
Locality: Synthetic
_database_code_amcsd 0021014
CELL PARAMETERS: 6.8648 7.6684 7.6055 90.000 117.792 90.000
SPACE GROUP: C2/c
X-RAY WAVELENGTH: 1.541838
Cell Volume: 354.185
Density (g/cm3): 2.595
MAX. ABS. INTENSITY / VOLUME**2: 8.229166062
RIR: 1.033
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
18.48 90.52 4.8008 -1 1 1 4
18.64 4.26 4.7608 1 1 0 4
26.26 100.00 3.3935 -1 1 2 4
26.50 13.92 3.3641 0 0 2 2
26.60 55.69 3.3514 1 1 1 4
26.76 88.88 3.3312 0 2 1 4
29.01 12.89 3.0783 -2 0 2 2
29.42 53.74 3.0365 2 0 0 2
35.09 41.13 2.5572 -2 2 1 4
35.50 47.52 2.5287 0 2 2 4
37.57 2.03 2.3941 -1 1 3 4
37.79 2.97 2.3804 2 2 0 4
38.12 1.64 2.3607 -1 3 1 4
38.20 6.19 2.3559 1 3 0 4
41.63 13.34 2.1695 -3 1 2 4
41.85 1.76 2.1584 -3 1 1 4
42.69 3.04 2.1182 -1 3 2 4
42.91 13.35 2.1078 1 3 1 4
44.22 31.63 2.0483 -2 2 3 4
44.79 2.92 2.0235 2 2 1 4
46.39 12.32 1.9573 3 1 0 4
46.93 5.63 1.9359 0 2 3 4
47.42 2.01 1.9171 0 4 0 2
48.09 6.94 1.8921 -2 0 4 2
48.89 2.48 1.8630 2 0 2 2
50.51 6.77 1.8069 -1 1 4 4
50.88 1.30 1.7946 -1 3 3 4
50.96 1.36 1.7920 1 1 3 4
53.39 1.64 1.7160 -4 0 2 2
54.05 4.68 1.6968 -2 2 4 4
54.40 1.95 1.6865 3 1 1 4
54.56 1.20 1.6820 0 0 4 2
54.78 22.67 1.6757 2 2 2 4
54.85 1.74 1.6737 -2 4 1 4
55.14 10.54 1.6656 0 4 2 4
56.55 15.36 1.6273 -2 4 2 4
57.60 4.34 1.6003 -3 3 3 4
58.13 12.10 1.5869 3 3 0 4
58.97 3.27 1.5663 -4 2 2 4
60.12 11.68 1.5392 -4 0 4 2
60.48 4.83 1.5307 -4 2 3 4
60.94 2.84 1.5203 -4 2 1 4
61.03 2.10 1.5182 4 0 0 2
61.69 11.01 1.5036 -1 3 4 4
62.09 1.40 1.4950 1 3 3 4
62.15 3.60 1.4936 2 4 1 4
62.46 1.41 1.4870 1 5 0 4
63.88 5.79 1.4573 0 4 3 4
63.88 1.10 1.4572 -3 1 5 4
64.31 2.45 1.4484 -3 3 4 4
65.04 3.54 1.4339 3 1 2 4
65.33 1.06 1.4284 -4 2 4 4
65.69 3.54 1.4214 -1 5 2 4
66.10 2.21 1.4135 -2 2 5 4
66.20 1.11 1.4116 4 2 0 4
66.97 2.90 1.3972 2 2 3 4
69.84 1.10 1.3467 -2 4 4 4
70.48 2.86 1.3361 2 4 2 4
72.09 2.08 1.3101 -1 5 3 4
73.17 3.48 1.2935 -4 2 5 4
74.16 9.41 1.2786 -4 4 2 4
74.41 3.22 1.2749 4 2 1 4
74.77 2.71 1.2697 0 2 5 4
74.79 3.44 1.2694 -3 5 2 4
74.95 3.50 1.2671 -3 5 1 4
75.09 2.94 1.2650 1 3 4 4
75.14 1.34 1.2644 0 4 4 4
75.51 1.25 1.2590 -4 4 3 4
75.93 3.98 1.2532 -4 4 1 4
76.47 5.59 1.2456 2 0 4 2
77.92 2.69 1.2260 3 1 3 4
78.71 2.29 1.2157 -5 1 5 4
79.04 1.48 1.2115 -4 0 6 2
80.18 4.11 1.1971 -2 2 6 4
80.65 2.25 1.1913 -2 4 5 4
80.66 1.31 1.1912 4 0 2 2
81.68 1.07 1.1789 1 5 3 4
81.76 3.07 1.1780 2 6 0 4
82.25 1.98 1.1721 -5 3 4 4
83.73 2.57 1.1552 -4 2 6 4
86.39 2.74 1.1262 2 6 1 4
87.56 2.39 1.1142 -5 1 6 4
87.94 1.15 1.1104 0 6 3 4
88.85 1.22 1.1014 0 4 5 4
89.29 1.70 1.0970 5 3 0 4
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XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs
For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.