Weddellite
      Izatulina A, Gurzhiy V, Frank-Kamenetskaya O
      American Mineralogist 99 (2014) 2-7
      Weddellite from renal stones: Structure refinement and dependence of
      crystal chemical features on H2O content.
      Note: Sample 8
      Locality: oxalic renal stones of St. Petersburg citizens aged 24-65 years
      _database_code_amcsd 0020078

      CELL PARAMETERS:   12.3443  12.3443   7.3599   90.000   90.000   90.000
      SPACE GROUP: I4/m      
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:   1121.514
      Density (g/cm3):      1.995
      MAX. ABS. INTENSITY / VOLUME**2:      9.073503987    
      RIR:      1.481
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                10.13         11.29        8.7287    1   1   0         4
                14.01          2.42        6.3216    1   0   1         8
                14.35        100.00        6.1722    2   0   0         4
                20.11         32.38        4.4163    1   2   1         8
                20.35          1.60        4.3644    2   2   0         4
                22.78         10.69        3.9036    1   3   0         4
                24.19          8.98        3.6799    0   0   2         2
                24.79          1.82        3.5916    3   0   1         8
                26.28          2.18        3.3909    1   1   2         8
                28.23          3.57        3.1608    2   0   2         8
                28.76          1.37        3.1043    3   2   1         8
                28.93         13.16        3.0861    4   0   0         4
                31.81         14.60        2.8133    2   2   2         8
                32.28         86.12        2.7733    1   4   1         8
                32.44          2.16        2.7603    4   2   0         4
                37.14         11.59        2.4209    1   5   0         4
                37.37         12.52        2.4062    1   0   3         8
                38.05          2.38        2.3646    4   0   2         8
                38.46          2.60        2.3407    4   3   1         8
                38.46          4.31        2.3407    3   4   1         8
                39.48          1.64        2.2824    3   3   2         8
                40.23         27.00        2.2419    2   1   3         8
                40.87          1.23        2.2081    4   2   2         8
                40.87          7.80        2.2081    2   4   2         8
                42.71         10.07        2.1170    3   5   0         4
                42.71          4.20        2.1170    5   3   0         4
                44.81          6.92        2.0225    5   1   2         8
                45.48          3.61        1.9942    2   3   3         8
                46.41          4.32        1.9564    6   1   1         8
                46.41         11.41        1.9564    1   6   1         8
                46.53          1.52        1.9518    6   2   0         4
                46.53          1.89        1.9518    2   6   0         4
                47.94         12.06        1.8976    4   1   3         8
                47.94          7.16        1.8976    1   4   3         8
                49.54          1.36        1.8400    0   0   4         2
                49.68         14.35        1.8350    5   3   2         8
                49.68          1.87        1.8350    3   5   2         8
                50.85          1.49        1.7958    6   0   2         8
                51.17          2.31        1.7852    6   3   1         8
                51.17          1.64        1.7852    3   6   1         8
                51.85          1.39        1.7633    2   0   4         8
                52.41          1.19        1.7457    5   5   0         4
                52.41          1.88        1.7457    1   7   0         4
                52.59          1.93        1.7402    4   3   3         8
                52.59          4.66        1.7402    3   4   3         8
                54.09          4.22        1.6955    2   2   4         8
                55.62          1.24        1.6523    2   7   1         8
                56.80          1.85        1.6209    7   3   0         4
                58.52          1.63        1.5773    5   5   2         8
                59.08          3.39        1.5637    6   1   3         8
                61.90          2.02        1.4990    7   4   1         8
                61.99          1.69        1.4970    2   8   0         4
                61.99          1.40        1.4970    8   2   0         4
                62.63          1.70        1.4834    7   3   2         8
                62.63          1.40        1.4834    3   7   2         8
                64.99          1.59        1.4350    7   5   0         4
                65.61          1.46        1.4230    8   0   2         8
                67.44          1.37        1.3888    5   3   4         8
                67.44          3.00        1.3888    3   5   4         8
                67.55          1.20        1.3866    2   8   2         8
                70.43          1.65        1.3369    5   7   2         8
                71.41          1.32        1.3210    1   4   5         8
                71.64          1.32        1.3173    9   2   1         8
                72.81          1.15        1.2989    8   1   3         8
                77.88          1.02        1.2266    0   0   6         2
                80.63          2.10        1.1915    1   6   5         8
                80.63          1.77        1.1915    6   1   5         8
                82.40          1.74        1.1703   10   0   2         8
                84.24          1.10        1.1495    3   6   5         8
                89.83          1.23        1.0919    2  11   1         8
================================================================================
       XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs
  For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.