Yugawaralite
Artioli G, Stahl K, Cruciani G, Gualtieri A, Hanson J C
American Mineralogist 86 (2001) 185-192
In situ dehydration of yugawaralite
Sample: at T = 581 K
_database_code_amcsd 0002629
CELL PARAMETERS: 6.7836 13.9842 10.0736 90.000 111.443 90.000
SPACE GROUP: Pc
X-RAY WAVELENGTH: 1.541838
Cell Volume: 889.468
Density (g/cm3): 2.119
MAX. ABS. INTENSITY / VOLUME**2: 6.089507012
RIR: 0.936
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
6.32 2.48 13.9842 0 1 0 2
11.36 12.94 7.7878 0 1 1 2
12.66 38.10 6.9921 0 2 0 2
14.03 6.35 6.3141 1 0 0 1
15.15 100.00 5.8499 -1 1 1 2
15.81 2.38 5.6052 0 2 1 2
18.93 46.49 4.6882 0 0 2 1
18.94 58.06 4.6861 1 2 0 2
19.01 83.22 4.6685 -1 0 2 1
19.04 4.96 4.6614 0 3 0 2
19.98 5.64 4.4450 0 1 2 2
20.05 11.59 4.4283 -1 1 2 2
20.62 52.90 4.3065 1 1 1 2
21.29 15.17 4.1740 0 3 1 2
22.84 6.34 3.8939 0 2 2 2
22.91 3.40 3.8826 -1 2 2 2
23.56 17.02 3.7761 -1 3 1 2
23.73 1.51 3.7501 1 3 0 2
26.97 1.54 3.3055 0 3 2 2
27.06 6.28 3.2947 -2 1 1 2
27.47 5.69 3.2473 1 3 1 2
27.53 24.91 3.2396 1 0 2 1
27.57 14.69 3.2356 -1 1 3 2
27.70 4.65 3.2203 -2 0 2 1
28.27 4.16 3.1570 2 0 0 1
28.44 2.05 3.1381 -2 1 2 2
29.20 78.35 3.0585 1 4 0 2
29.28 6.39 3.0502 0 1 3 2
29.75 1.88 3.0034 -1 2 3 2
30.41 17.90 2.9395 1 2 2 2
30.56 23.33 2.9250 -2 2 2 2
31.08 2.79 2.8773 2 2 0 2
31.93 1.40 2.8026 0 4 2 2
32.36 7.63 2.7669 1 4 1 2
32.75 15.90 2.7347 -2 1 3 2
33.09 2.62 2.7074 -1 3 3 2
33.43 15.66 2.6801 0 5 1 2
33.69 1.71 2.6603 1 3 2 2
33.72 10.09 2.6582 2 1 1 2
33.83 2.67 2.6495 -2 3 2 2
34.55 2.06 2.5959 0 3 3 2
34.63 2.00 2.5901 -2 2 3 2
35.65 3.69 2.5184 -1 0 4 1
36.24 2.69 2.4785 -1 1 4 2
36.93 1.37 2.4338 -2 4 1 2
37.02 4.58 2.4281 1 1 3 2
37.44 1.65 2.4019 0 5 2 2
37.86 3.04 2.3763 1 4 2 2
37.98 4.07 2.3694 -1 2 4 2
38.40 3.95 2.3441 0 0 4 1
38.42 1.16 2.3431 2 4 0 2
38.45 1.02 2.3413 2 3 1 2
38.57 1.65 2.3343 -2 0 4 1
40.72 1.71 2.2157 -1 3 4 2
40.75 1.56 2.2141 -2 2 4 2
41.19 1.74 2.1916 -1 6 1 2
41.43 2.51 2.1794 1 3 3 2
41.87 6.69 2.1574 -2 5 1 2
42.22 1.97 2.1407 2 4 1 2
42.22 1.18 2.1406 -1 5 3 2
42.97 5.42 2.1047 3 0 0 1
43.42 1.28 2.0842 0 5 3 2
44.33 1.39 2.0434 -1 4 4 2
44.97 3.83 2.0158 -3 3 1 2
45.61 1.49 1.9888 -1 1 5 2
45.96 4.53 1.9746 1 0 4 1
46.25 3.86 1.9629 -3 0 4 1
46.48 2.29 1.9539 0 7 1 2
46.73 3.68 1.9438 -3 1 4 2
46.89 1.84 1.9378 -2 1 5 2
47.06 1.46 1.9311 -1 2 5 2
47.64 2.07 1.9087 -1 6 3 2
47.87 1.20 1.9003 1 2 4 2
47.88 9.49 1.8999 2 4 2 2
48.06 2.16 1.8933 -3 4 2 2
48.08 1.32 1.8922 3 1 1 2
48.30 1.23 1.8843 -2 2 5 2
48.55 1.99 1.8751 2 6 0 2
49.39 1.24 1.8452 -1 3 5 2
50.59 1.15 1.8042 -2 3 5 2
51.07 1.12 1.7883 -2 6 3 2
52.34 3.45 1.7480 0 8 0 2
52.57 2.26 1.7408 -3 1 5 2
53.22 2.02 1.7211 -2 7 1 2
53.28 1.10 1.7193 1 4 4 2
53.31 3.27 1.7184 0 8 1 2
53.68 1.01 1.7074 -2 4 5 2
53.83 5.24 1.7030 -3 5 3 2
54.10 1.38 1.6951 -4 0 2 1
54.47 1.10 1.6847 1 8 0 2
54.99 1.23 1.6699 2 4 3 2
55.14 1.49 1.6656 -1 0 6 1
55.73 2.07 1.6493 -2 6 4 2
56.16 1.10 1.6379 0 8 2 2
56.69 1.97 1.6237 2 6 2 2
56.85 2.12 1.6196 -3 6 2 2
58.49 2.37 1.5780 2 2 4 2
58.52 2.66 1.5772 3 5 1 2
58.97 2.20 1.5663 -2 3 6 2
59.12 2.26 1.5627 0 0 6 1
59.15 1.28 1.5620 3 6 0 2
59.39 1.15 1.5562 -3 0 6 1
59.52 1.73 1.5531 0 1 6 2
59.80 2.95 1.5466 -3 1 6 2
60.87 2.23 1.5219 -4 3 4 2
60.93 1.01 1.5205 0 7 4 2
61.38 1.99 1.5105 -1 9 1 2
61.78 1.40 1.5017 -2 4 6 2
63.06 1.75 1.4743 -1 9 2 2
63.27 3.33 1.4697 2 4 4 2
63.60 1.64 1.4630 4 1 1 2
63.62 1.96 1.4625 -4 4 4 2
64.80 3.32 1.4387 4 4 0 2
67.14 1.31 1.3941 2 9 0 2
69.22 1.51 1.3573 -2 9 3 2
69.79 2.14 1.3477 2 9 1 2
69.96 1.66 1.3447 3 8 0 2
70.17 1.95 1.3412 3 0 4 1
70.94 1.28 1.3286 -4 5 5 2
70.98 1.08 1.3279 3 5 3 2
71.81 1.63 1.3145 1 9 3 2
73.06 1.61 1.2951 -4 4 6 2
74.00 1.08 1.2810 2 9 2 2
75.52 1.81 1.2590 -5 4 2 2
75.86 1.29 1.2541 -2 1 8 2
77.80 1.42 1.2277 -3 7 6 2
79.14 1.03 1.2102 -4 8 3 2
80.35 1.02 1.1950 -1 3 8 2
80.70 1.09 1.1907 5 1 1 2
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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.