Edingtonite Stahl K, Hanson J C European Journal of Mineralogy 10 (1998) 221-228 An in situ study of the edingtonite dehydration process from X-ray synchrotron powder diffraction Sample: 310 K _database_code_amcsd 0006714 CELL PARAMETERS: 9.5374 9.6127 6.5233 90.000 90.000 90.000 SPACE GROUP: P2_12_12 X-RAY WAVELENGTH: 1.541838 Cell Volume: 598.057 Density (g/cm3): 2.709 MAX. ABS. INTENSITY / VOLUME**2: 8.823600966 RIR: 1.060 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 13.57 100.00 6.5233 0 0 1 2 16.42 36.80 5.3978 0 1 1 4 16.46 44.20 5.3843 1 0 1 4 18.46 49.66 4.8064 0 2 0 2 18.61 51.49 4.7687 2 0 0 2 18.89 74.99 4.6976 1 1 1 4 20.69 9.85 4.2921 1 2 0 4 20.79 3.39 4.2719 2 1 0 4 22.98 3.54 3.8695 0 2 1 4 24.83 90.56 3.5856 1 2 1 4 24.91 88.60 3.5738 2 1 1 4 26.33 20.45 3.3852 2 2 0 4 27.34 12.38 3.2617 0 0 2 2 28.91 11.46 3.0887 0 1 2 4 28.93 11.02 3.0862 1 0 2 4 29.41 23.45 3.0374 1 3 0 4 29.60 29.12 3.0183 3 1 0 4 29.73 23.80 3.0047 2 2 1 4 30.42 34.10 2.9384 1 1 2 4 32.52 80.04 2.7535 1 3 1 4 32.69 88.84 2.7393 3 1 1 4 33.70 4.94 2.6596 2 3 0 4 33.80 7.08 2.6516 3 2 0 4 34.54 37.85 2.5969 1 2 2 4 34.60 44.35 2.5924 2 1 2 4 36.48 5.14 2.4628 2 3 1 4 36.58 6.54 2.4564 3 2 1 4 38.32 2.03 2.3488 2 2 2 4 39.42 33.11 2.2858 0 3 2 4 39.59 28.56 2.2766 3 0 2 4 39.95 34.30 2.2568 3 3 0 4 39.98 4.21 2.2550 0 4 1 4 40.27 2.08 2.2394 4 0 1 4 40.59 2.04 2.2228 1 3 2 4 40.73 1.73 2.2153 3 1 2 4 41.13 17.33 2.1945 1 4 1 4 41.40 15.49 2.1810 4 1 1 4 41.53 3.55 2.1744 0 0 3 2 42.11 9.37 2.1461 2 4 0 4 42.31 10.35 2.1360 4 2 0 4 42.38 10.06 2.1328 3 3 1 4 42.63 3.02 2.1209 0 1 3 4 42.65 2.04 2.1200 1 0 3 4 43.72 16.08 2.0703 1 1 3 4 43.93 5.90 2.0612 2 3 2 4 44.01 6.40 2.0575 3 2 2 4 44.44 6.28 2.0386 2 4 1 4 44.64 4.45 2.0299 4 2 1 4 45.80 3.25 1.9811 0 2 3 4 45.87 4.82 1.9785 2 0 3 4 46.84 6.05 1.9397 1 2 3 4 46.88 8.01 1.9378 2 1 3 4 47.53 1.97 1.9129 4 3 0 4 47.98 6.91 1.8961 1 4 2 4 48.22 6.60 1.8874 4 1 2 4 48.29 1.55 1.8846 1 5 0 4 48.67 1.10 1.8710 5 1 0 4 49.09 1.40 1.8559 3 3 2 4 49.42 4.44 1.8441 0 5 1 4 49.56 10.31 1.8393 3 4 1 4 49.67 9.98 1.8356 4 3 1 4 49.81 4.20 1.8308 5 0 1 4 49.84 16.60 1.8295 2 2 3 4 50.40 4.64 1.8106 1 5 1 4 50.76 5.57 1.7985 5 1 1 4 51.23 1.86 1.7831 2 5 0 4 51.55 2.45 1.7730 5 2 0 4 51.70 4.64 1.7681 1 3 3 4 51.82 3.23 1.7643 3 1 3 4 53.26 1.85 1.7200 2 5 1 4 53.56 2.26 1.7109 5 2 1 4 54.19 7.24 1.6926 4 4 0 4 54.51 1.47 1.6834 2 3 3 4 54.58 3.82 1.6814 3 2 3 4 55.48 7.16 1.6562 0 5 2 4 55.61 7.33 1.6527 3 4 2 4 55.71 5.87 1.6500 4 3 2 4 55.83 7.49 1.6466 5 0 2 4 56.14 3.75 1.6384 4 4 1 4 56.38 3.64 1.6318 1 5 2 4 56.42 5.50 1.6308 0 0 4 2 56.72 4.03 1.6229 5 1 2 4 57.35 1.17 1.6067 4 0 3 4 57.53 4.90 1.6021 0 6 0 2 58.01 3.45 1.5898 1 4 3 4 58.02 4.02 1.5896 6 0 0 2 58.19 2.24 1.5855 1 1 4 4 58.22 2.80 1.5847 4 1 3 4 59.04 5.55 1.5646 2 5 2 4 59.33 5.53 1.5577 5 2 2 4 60.27 1.71 1.5356 1 6 1 4 60.63 6.55 1.5274 2 4 3 4 60.74 1.68 1.5248 6 1 1 4 60.75 2.32 1.5245 1 2 4 4 60.79 7.47 1.5238 4 2 3 4 60.79 2.59 1.5236 2 1 4 4 61.01 4.98 1.5187 2 6 0 4 61.44 5.88 1.5092 6 2 0 4 61.75 5.76 1.5024 4 4 2 4 62.82 1.87 1.4791 2 6 1 4 63.24 3.09 1.4703 6 2 1 4 63.30 3.18 1.4692 2 2 4 4 63.81 1.31 1.4587 4 5 1 4 64.72 1.25 1.4403 0 5 3 4 64.84 4.48 1.4380 3 4 3 4 64.90 8.53 1.4368 1 3 4 4 64.93 1.91 1.4362 4 3 3 4 65.00 6.20 1.4348 3 1 4 4 65.04 1.17 1.4339 5 0 3 4 65.55 1.02 1.4242 1 5 3 4 66.96 2.95 1.3975 3 6 1 4 67.30 3.19 1.3912 6 3 1 4 67.42 1.05 1.3891 3 2 4 4 69.05 1.54 1.3603 4 5 2 4 69.41 3.58 1.3541 5 5 0 4 70.02 2.03 1.3438 0 7 1 4 70.51 7.58 1.3357 4 4 3 4 70.62 1.74 1.3337 7 0 1 4 70.81 2.52 1.3306 1 7 1 4 70.86 1.04 1.3298 4 6 0 4 71.11 3.52 1.3258 5 5 1 4 71.11 1.44 1.3258 6 4 0 4 71.36 4.80 1.3218 3 3 4 4 71.40 3.07 1.3211 7 1 1 4 71.49 1.22 1.3196 2 7 0 4 72.05 1.07 1.3108 7 2 0 4 72.09 8.49 1.3102 3 6 2 4 72.42 9.06 1.3050 6 3 2 4 72.44 1.19 1.3047 0 0 5 2 72.84 1.16 1.2985 2 4 4 4 72.99 1.23 1.2962 4 2 4 4 73.17 2.26 1.2934 2 7 1 4 73.72 1.85 1.2851 7 2 1 4 75.05 1.27 1.2656 0 7 2 4 76.28 3.13 1.2483 1 2 5 4 76.32 3.04 1.2478 2 1 5 4 76.51 2.66 1.2451 2 6 3 4 76.90 1.91 1.2398 6 2 3 4 77.05 2.09 1.2378 3 7 1 4 77.38 4.80 1.2332 1 5 4 4 77.53 1.10 1.2313 7 3 1 4 77.67 3.67 1.2294 5 1 4 4 78.13 1.24 1.2233 2 7 2 4 78.58 1.48 1.2174 2 2 5 4 78.67 1.02 1.2163 7 2 2 4 79.50 1.13 1.2057 5 6 1 4 79.63 1.15 1.2040 6 5 1 4 79.68 2.07 1.2034 2 5 4 4 79.92 2.16 1.2003 5 2 4 4 80.33 1.79 1.1952 3 6 3 4 80.65 1.74 1.1913 6 3 3 4 82.20 1.46 1.1727 1 8 1 4 82.32 1.03 1.1713 2 3 5 4 82.85 1.22 1.1652 2 8 0 4 82.94 1.16 1.1641 8 1 1 4 83.56 1.30 1.1571 8 2 0 4 84.24 1.29 1.1494 5 5 3 4 84.48 1.28 1.1468 6 5 2 4 85.25 1.77 1.1384 1 4 5 4 85.43 1.74 1.1365 4 1 5 4 85.85 1.15 1.1320 6 4 3 4 86.21 1.19 1.1281 2 7 3 4 86.74 1.23 1.1226 7 2 3 4 87.02 2.54 1.1197 1 8 2 4 87.50 1.15 1.1148 2 4 5 4 87.76 2.39 1.1122 8 1 2 4 87.84 1.15 1.1114 2 6 4 4 89.14 1.81 1.0986 5 7 1 4 89.42 1.80 1.0958 7 5 1 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.