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 = -80 C
Locality: Synthetic
_database_code_amcsd 0021013
CELL PARAMETERS: 6.8815 7.6534 7.6172 90.000 117.884 90.000
SPACE GROUP: C2/c
X-RAY WAVELENGTH: 1.541838
Cell Volume: 354.596
Density (g/cm3): 2.592
MAX. ABS. INTENSITY / VOLUME**2: 8.319019221
RIR: 1.045
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
18.47 87.99 4.8045 -1 1 1 4
18.63 3.87 4.7618 1 1 0 4
26.23 100.00 3.3969 -1 1 2 4
26.48 13.75 3.3664 0 0 2 2
26.59 54.66 3.3520 1 1 1 4
26.80 87.44 3.3269 0 2 1 4
28.93 12.81 3.0861 -2 0 2 2
29.37 53.85 3.0413 2 0 0 2
35.08 39.85 2.5583 -2 2 1 4
35.52 45.40 2.5276 0 2 2 4
37.53 1.96 2.3965 -1 1 3 4
37.78 3.08 2.3809 2 2 0 4
38.17 1.59 2.3577 -1 3 1 4
38.26 6.06 2.3526 1 3 0 4
41.53 12.83 2.1743 -3 1 2 4
41.77 1.62 2.1623 -3 1 1 4
42.72 3.15 2.1165 -1 3 2 4
42.96 12.41 2.1055 1 3 1 4
44.17 30.53 2.0502 -2 2 3 4
44.78 3.05 2.0238 2 2 1 4
46.33 11.96 1.9599 3 1 0 4
46.93 5.66 1.9359 0 2 3 4
47.52 2.01 1.9133 0 4 0 2
48.00 7.00 1.8954 -2 0 4 2
48.85 2.38 1.8643 2 0 2 2
50.46 6.42 1.8086 -1 1 4 4
50.90 1.42 1.7940 -1 3 3 4
50.94 1.24 1.7927 1 1 3 4
53.25 1.62 1.7201 -4 0 2 2
53.99 4.72 1.6985 -2 2 4 4
54.35 2.01 1.6881 3 1 1 4
54.52 1.13 1.6832 0 0 4 2
54.77 21.88 1.6760 2 2 2 4
54.91 1.65 1.6721 -2 4 1 4
55.22 10.35 1.6634 0 4 2 4
56.60 14.70 1.6262 -2 4 2 4
57.55 4.22 1.6015 -3 3 3 4
58.11 11.62 1.5873 3 3 0 4
58.86 3.14 1.5689 -4 2 2 4
59.95 11.13 1.5431 -4 0 4 2
60.36 4.66 1.5335 -4 2 3 4
60.85 2.80 1.5224 -4 2 1 4
60.92 2.14 1.5206 4 0 0 2
61.69 10.48 1.5037 -1 3 4 4
62.11 1.21 1.4945 1 3 3 4
62.21 3.38 1.4923 2 4 1 4
62.58 1.36 1.4844 1 5 0 4
63.75 1.05 1.4598 -3 1 5 4
63.94 5.36 1.4560 0 4 3 4
64.25 2.29 1.4497 -3 3 4 4
64.99 3.41 1.4350 3 1 2 4
65.19 1.04 1.4311 -4 2 4 4
65.80 3.31 1.4193 -1 5 2 4
66.03 2.19 1.4149 -2 2 5 4
66.12 1.04 1.4131 4 2 0 4
66.96 2.81 1.3976 2 2 3 4
69.85 1.06 1.3466 -2 4 4 4
70.53 2.83 1.3353 2 4 2 4
72.18 1.97 1.3087 -1 5 3 4
73.01 3.35 1.2959 -4 2 5 4
74.12 9.23 1.2792 -4 4 2 4
74.34 3.03 1.2760 4 2 1 4
74.73 2.53 1.2702 0 2 5 4
74.84 3.08 1.2687 -3 5 2 4
75.00 3.31 1.2663 -3 5 1 4
75.10 2.84 1.2649 1 3 4 4
75.18 1.36 1.2638 0 4 4 4
75.46 1.21 1.2598 -4 4 3 4
75.90 3.62 1.2536 -4 4 1 4
76.42 5.19 1.2463 2 0 4 2
77.86 2.50 1.2268 3 1 3 4
78.48 2.13 1.2187 -5 1 5 4
78.84 1.44 1.2141 -4 0 6 2
80.09 3.91 1.1982 -2 2 6 4
80.57 1.26 1.1923 4 0 2 2
80.63 2.02 1.1915 -2 4 5 4
81.77 1.04 1.1778 1 5 3 4
81.90 2.79 1.1763 2 6 0 4
82.09 1.95 1.1740 -5 3 4 4
83.55 2.37 1.1572 -4 2 6 4
86.54 2.59 1.1248 2 6 1 4
87.31 2.27 1.1168 -5 1 6 4
88.08 1.10 1.1090 0 6 3 4
88.87 1.13 1.1012 0 4 5 4
89.19 1.57 1.0981 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.