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 1
      Locality: oxalic renal stones of St. Petersburg citizens aged 24-65 years
      _database_code_amcsd 0020071

      CELL PARAMETERS:   12.3363  12.3363   7.3448   90.000   90.000   90.000
      SPACE GROUP: I4/m      
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:   1117.763
      Density (g/cm3):      1.983
      MAX. ABS. INTENSITY / VOLUME**2:      9.926274521    
      RIR:      1.630
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                10.14         13.73        8.7231    1   1   0         4
                14.03          1.69        6.3109    1   0   1         8
                14.36        100.00        6.1681    2   0   0         4
                20.13         30.46        4.4112    2   1   1         8
                20.36          2.23        4.3615    2   2   0         4
                22.80          1.08        3.9011    1   3   0         4
                22.80          8.66        3.9011    3   1   0         4
                24.24          8.51        3.6724    0   0   2         2
                24.81          1.37        3.5880    3   0   1         8
                26.33          1.52        3.3847    1   1   2         8
                28.28          2.87        3.1555    2   0   2         8
                28.79          1.29        3.1015    2   3   1         8
                28.95         11.45        3.0841    4   0   0         4
                31.86         14.11        2.8092    2   2   2         8
                32.31         78.03        2.7709    4   1   1         8
                32.46          1.65        2.7585    2   4   0         4
                37.16         11.21        2.4193    5   1   0         4
                37.45         11.01        2.4014    1   0   3         8
                38.10          1.98        2.3617    4   0   2         8
                38.49          4.12        2.3388    4   3   1         8
                38.49          2.31        2.3388    3   4   1         8
                39.53          1.30        2.2797    3   3   2         8
                40.30         25.27        2.2378    1   2   3         8
                40.92          6.83        2.2056    4   2   2         8
                40.92          1.09        2.2056    2   4   2         8
                42.74          3.62        2.1157    3   5   0         4
                42.74          9.16        2.1157    5   3   0         4
                44.86          6.23        2.0203    1   5   2         8
                45.56          3.12        1.9910    3   2   3         8
                46.45         10.60        1.9549    6   1   1         8
                46.45          3.86        1.9549    1   6   1         8
                46.56          1.82        1.9505    6   2   0         4
                46.56          1.53        1.9505    2   6   0         4
                48.02          6.87        1.8948    4   1   3         8
                48.02         10.87        1.8948    1   4   3         8
                49.65          1.27        1.8362    0   0   4         2
                49.74          1.79        1.8332    5   3   2         8
                49.74         13.56        1.8332    3   5   2         8
                50.90          1.44        1.7940    6   0   2         8
                51.21          1.45        1.7839    6   3   1         8
                51.21          2.25        1.7839    3   6   1         8
                51.96          1.29        1.7599    2   0   4         8
                52.45          1.13        1.7446    5   5   0         4
                52.45          1.61        1.7446    7   1   0         4
                52.67          1.88        1.7379    3   4   3         8
                52.67          4.19        1.7379    4   3   3         8
                54.20          3.85        1.6923    2   2   4         8
                55.67          1.13        1.6511    7   2   1         8
                56.84          1.77        1.6198    3   7   0         4
                58.58          1.44        1.5758    5   5   2         8
                59.16          3.24        1.5618    1   6   3         8
                61.95          1.86        1.4980    4   7   1         8
                62.04          1.32        1.4960    2   8   0         4
                62.04          1.53        1.4960    8   2   0         4
                62.69          1.26        1.4821    7   3   2         8
                62.69          1.53        1.4821    3   7   2         8
                65.04          1.44        1.4341    5   7   0         4
                65.67          1.28        1.4218    8   0   2         8
                67.55          2.78        1.3867    5   3   4         8
                67.55          1.27        1.3867    3   5   4         8
                67.62          1.13        1.3855    8   2   2         8
                70.49          1.59        1.3358    7   5   2         8
                71.56          1.22        1.3186    4   1   5         8
                71.69          1.22        1.3164    2   9   1         8
                72.90          1.09        1.2976    1   8   3         8
                80.78          1.96        1.1897    6   1   5         8
                80.78          1.63        1.1897    1   6   5         8
                82.48          1.66        1.1694   10   0   2         8
                84.39          1.02        1.1477    6   3   5         8
                89.91          1.15        1.0911   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.