Chalconatronite Mosset A, Bonnet J J, Galy J Zeitschrift fur Kristallographie 148 (1978) 165-177 Structure cristalline de la chalconatronite synthetique: Na2Cu(CO3)2*3H2O Locality: synthetic _database_code_amcsd 0010801 CELL PARAMETERS: 9.6960 6.1010 13.7790 90.000 91.830 90.000 SPACE GROUP: P2_1/n X-RAY WAVELENGTH: 1.541838 Cell Volume: 814.685 Density (g/cm3): 2.279 MAX. ABS. INTENSITY / VOLUME**2: 9.736109778 RIR: 1.391 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 10.99 1.21 8.0474 -1 0 1 2 11.33 26.81 7.8090 1 0 1 2 12.86 100.00 6.8860 0 0 2 2 15.89 4.77 5.5781 0 1 1 4 17.17 42.41 5.1631 1 1 0 4 18.31 2.63 4.8455 2 0 0 2 18.45 1.99 4.8077 1 1 1 4 19.44 6.18 4.5665 0 1 2 4 21.15 8.34 4.2010 -1 0 3 2 21.33 63.14 4.1650 -1 1 2 4 21.68 14.05 4.0984 1 0 3 2 21.69 8.97 4.0975 1 1 2 4 22.09 1.44 4.0237 -2 0 2 2 22.78 4.81 3.9045 2 0 2 2 23.45 2.54 3.7944 2 1 0 4 24.17 17.33 3.6817 -2 1 1 4 24.26 38.48 3.6682 0 1 3 4 24.49 5.99 3.6349 2 1 1 4 25.88 10.72 3.4430 0 0 4 2 26.19 3.26 3.4021 1 1 3 4 26.54 6.17 3.3590 -2 1 2 4 28.58 5.66 3.1229 3 0 1 2 29.80 14.32 2.9985 0 1 4 4 30.00 2.89 2.9783 0 2 1 4 30.73 6.59 2.9098 1 2 0 4 30.95 3.73 2.8894 2 1 3 4 30.97 15.06 2.8873 -1 1 4 4 31.33 4.03 2.8549 3 1 0 4 31.36 18.93 2.8524 -1 2 1 4 31.48 9.45 2.8423 1 1 4 4 31.49 1.58 2.8414 1 2 1 4 32.20 2.47 2.7799 3 1 1 4 33.40 3.74 2.6825 -3 0 3 2 33.54 7.04 2.6720 -1 0 5 2 33.55 2.02 2.6711 1 2 2 4 33.64 1.43 2.6639 -3 1 2 4 34.12 1.94 2.6275 1 0 5 2 34.34 7.89 2.6113 3 1 2 4 34.45 7.20 2.6030 3 0 3 2 34.74 1.07 2.5821 -2 1 4 4 35.49 8.13 2.5296 2 2 1 4 35.77 12.05 2.5104 0 1 5 4 36.59 5.07 2.4556 -3 1 3 4 36.73 2.00 2.4471 1 2 3 4 36.98 16.52 2.4309 -2 2 2 4 37.11 8.38 2.4228 4 0 0 2 37.41 2.86 2.4038 2 2 2 4 37.57 3.88 2.3942 3 1 3 4 39.47 1.17 2.2832 0 2 4 4 39.84 7.84 2.2629 4 0 2 2 39.96 6.58 2.2560 -2 1 5 4 40.47 2.36 2.2288 -3 1 4 4 40.79 2.78 2.2120 1 2 4 4 41.08 2.16 2.1972 -3 2 1 4 41.66 1.54 2.1678 3 1 4 4 42.44 4.96 2.1298 -3 0 5 2 43.45 22.41 2.0825 -2 2 4 4 43.87 12.33 2.0636 3 0 5 2 44.21 3.17 2.0488 2 2 4 4 44.28 2.88 2.0458 -4 1 3 4 45.00 4.49 2.0144 -3 2 3 4 45.11 15.05 2.0100 -1 2 5 4 45.39 3.67 1.9983 4 1 3 4 45.58 8.32 1.9903 1 3 0 4 46.12 1.07 1.9680 1 3 1 4 47.47 7.35 1.9154 -1 3 2 4 47.95 7.03 1.8972 4 2 0 4 48.99 2.98 1.8594 0 3 3 4 49.28 1.21 1.8490 -1 1 7 4 49.33 9.70 1.8472 5 1 0 4 49.59 1.09 1.8382 -5 1 1 4 50.30 1.09 1.8140 -3 1 6 4 50.78 3.39 1.7979 -5 1 2 4 51.66 1.68 1.7692 -4 1 5 4 51.78 2.24 1.7655 5 0 3 2 51.81 6.40 1.7647 -2 1 7 4 52.48 3.58 1.7435 -2 3 3 4 52.86 1.39 1.7321 -5 1 3 4 52.93 2.14 1.7300 -2 2 6 4 52.96 5.92 1.7290 2 1 7 4 53.21 2.15 1.7215 0 0 8 2 53.22 1.30 1.7210 3 3 0 4 53.31 5.49 1.7185 4 1 5 4 53.55 1.48 1.7113 -3 3 1 4 53.62 1.23 1.7093 3 2 5 4 53.77 2.58 1.7047 -3 0 7 2 53.90 1.37 1.7010 2 2 6 4 55.23 2.93 1.6630 3 3 2 4 55.92 1.69 1.6443 4 2 4 4 56.02 1.29 1.6415 -1 1 8 4 56.19 2.08 1.6371 -1 2 7 4 56.23 2.07 1.6360 0 3 5 4 56.47 1.10 1.6297 -5 2 1 4 56.73 3.18 1.6226 1 2 7 4 56.86 3.31 1.6194 5 2 1 4 57.24 1.23 1.6095 -5 0 5 2 57.29 1.11 1.6082 1 3 5 4 57.32 5.22 1.6075 5 1 4 4 59.36 1.96 1.5568 -6 1 1 4 59.47 1.03 1.5543 -5 2 3 4 60.03 1.29 1.5412 2 3 5 4 60.60 1.03 1.5280 5 2 3 4 60.72 1.81 1.5252 0 4 0 2 61.99 2.28 1.4970 1 4 1 4 62.40 2.25 1.4881 -3 2 7 4 62.41 1.15 1.4879 -1 2 8 4 62.76 1.27 1.4806 -6 0 4 2 63.46 1.43 1.4659 4 3 3 4 63.94 2.33 1.4560 3 2 7 4 65.27 1.36 1.4295 1 4 3 4 65.50 1.37 1.4250 -4 0 8 2 65.58 1.06 1.4235 -5 2 5 4 65.73 2.15 1.4207 2 4 2 4 66.45 1.18 1.4070 2 1 9 4 66.52 3.39 1.4056 -6 2 2 4 66.81 1.66 1.4003 -3 0 9 2 67.37 1.24 1.3899 6 2 2 4 68.60 1.21 1.3679 -4 3 5 4 68.72 2.46 1.3659 -2 3 7 4 69.70 1.15 1.3491 2 3 7 4 69.70 2.02 1.3490 1 2 9 4 70.00 1.38 1.3441 4 3 5 4 71.18 1.07 1.3246 -1 4 5 4 72.88 1.03 1.2978 1 3 8 4 75.11 1.33 1.2648 4 4 2 4 75.28 1.06 1.2624 -6 3 1 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.