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 11
      Locality: oxalic renal stones of St. Petersburg citizens aged 24-65 years
      _database_code_amcsd 0020081

      CELL PARAMETERS:   12.3576  12.3576   7.3578   90.000   90.000   90.000
      SPACE GROUP: I4/m      
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:   1123.612
      Density (g/cm3):      2.002
      MAX. ABS. INTENSITY / VOLUME**2:      8.669153371    
      RIR:      1.410
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                10.12          9.23        8.7381    1   1   0         4
                14.01          2.93        6.3220    1   0   1         8
                14.33        100.00        6.1788    2   0   0         4
                20.09         32.61        4.4188    2   1   1         8
                20.33          1.45        4.3691    2   2   0         4
                22.76         12.14        3.9078    3   1   0         4
                24.19          8.36        3.6789    0   0   2         2
                24.77          1.89        3.5943    3   0   1         8
                26.28          2.35        3.3906    1   1   2         8
                28.23          4.23        3.1610    2   0   2         8
                28.73          1.26        3.1068    2   3   1         8
                28.90         14.37        3.0894    4   0   0         4
                31.80         14.54        2.8141    2   2   2         8
                32.25         90.01        2.7757    4   1   1         8
                32.40          2.34        2.7632    2   4   0         4
                37.10         11.67        2.4235    5   1   0         4
                37.38         12.88        2.4057    1   0   3         8
                38.03          2.56        2.3658    4   0   2         8
                38.42          4.23        2.3429    4   3   1         8
                38.42          2.74        2.3429    3   4   1         8
                39.46          1.85        2.2836    3   3   2         8
                40.23         27.29        2.2418    1   2   3         8
                40.84          8.24        2.2094    4   2   2         8
                40.84          1.35        2.2094    2   4   2         8
                42.66          4.52        2.1193    3   5   0         4
                42.66         10.56        2.1193    5   3   0         4
                44.78          7.34        2.0238    1   5   2         8
                45.48          3.73        1.9945    3   2   3         8
                46.37         11.69        1.9583    6   1   1         8
                46.37          4.48        1.9583    1   6   1         8
                46.48          1.83        1.9539    6   2   0         4
                46.48          1.48        1.9539    2   6   0         4
                47.93          7.07        1.8981    4   1   3         8
                47.93         12.65        1.8981    1   4   3         8
                49.56          1.39        1.8395    0   0   4         2
                49.64          1.78        1.8364    5   3   2         8
                49.64         14.54        1.8364    3   5   2         8
                50.80          1.49        1.7971    6   0   2         8
                51.11          1.70        1.7870    6   3   1         8
                51.11          2.35        1.7870    3   6   1         8
                51.86          1.45        1.7630    2   0   4         8
                52.35          1.15        1.7476    5   5   0         4
                52.35          1.94        1.7476    7   1   0         4
                52.57          4.86        1.7409    4   3   3         8
                52.57          1.94        1.7409    3   4   3         8
                54.10          4.25        1.6953    2   2   4         8
                55.56          1.30        1.6540    7   2   1         8
                56.73          1.83        1.6226    3   7   0         4
                58.47          1.72        1.5786    5   5   2         8
                59.04          3.34        1.5645    1   6   3         8
                61.83          2.07        1.5006    4   7   1         8
                61.92          1.45        1.4986    2   8   0         4
                61.92          1.80        1.4986    8   2   0         4
                62.57          1.46        1.4846    7   3   2         8
                62.57          1.75        1.4846    3   7   2         8
                64.91          1.69        1.4365    5   7   0         4
                65.54          1.53        1.4242    8   0   2         8
                67.41          3.01        1.3892    5   3   4         8
                67.41          1.37        1.3892    3   5   4         8
                67.49          1.17        1.3879    8   2   2         8
                70.35          1.66        1.3381    7   5   2         8
                71.41          1.31        1.3209    4   1   5         8
                71.55          1.34        1.3187    2   9   1         8
                72.75          1.16        1.2998    1   8   3         8
                77.90          1.02        1.2263    0   0   6         2
                80.61          2.13        1.1918    6   1   5         8
                80.61          1.75        1.1918    1   6   5         8
                82.31          1.72        1.1714   10   0   2         8
                84.21          1.08        1.1498    6   3   5         8
                89.71          1.23        1.0930   11   2   1         8
================================================================================
       XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs
  For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.