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 12
      Locality: oxalic renal stones of St. Petersburg citizens aged 24-65 years
      _database_code_amcsd 0020082

      CELL PARAMETERS:   12.3567  12.3567   7.3573   90.000   90.000   90.000
      SPACE GROUP: I4/m      
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:   1123.372
      Density (g/cm3):      2.001
      MAX. ABS. INTENSITY / VOLUME**2:      8.697495545    
      RIR:      1.415
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                10.12          9.75        8.7375    1   1   0         4
                14.01          2.88        6.3216    1   0   1         8
                14.34        100.00        6.1783    2   0   0         4
                20.10         32.33        4.4185    1   2   1         8
                20.33          1.43        4.3688    2   2   0         4
                22.76         11.88        3.9075    1   3   0         4
                24.19          8.32        3.6786    0   0   2         2
                24.77          1.91        3.5940    3   0   1         8
                26.29          2.31        3.3904    1   1   2         8
                28.23          4.20        3.1608    2   0   2         8
                28.74          1.22        3.1066    3   2   1         8
                28.90         14.35        3.0892    4   0   0         4
                31.80         14.55        2.8139    2   2   2         8
                32.25         89.74        2.7755    1   4   1         8
                32.40          2.31        2.7630    4   2   0         4
                37.10         11.69        2.4233    1   5   0         4
                37.38         12.85        2.4055    1   0   3         8
                38.04          2.55        2.3657    4   0   2         8
                38.42          2.71        2.3427    4   3   1         8
                38.42          4.18        2.3427    3   4   1         8
                39.46          1.84        2.2835    3   3   2         8
                40.23         27.19        2.2416    2   1   3         8
                40.85          1.33        2.2093    4   2   2         8
                40.85          8.21        2.2093    2   4   2         8
                42.67         10.52        2.1192    3   5   0         4
                42.67          4.50        2.1192    5   3   0         4
                44.78          7.29        2.0237    5   1   2         8
                45.48          3.77        1.9944    2   3   3         8
                46.37          4.47        1.9582    6   1   1         8
                46.37         11.59        1.9582    1   6   1         8
                46.48          1.48        1.9538    6   2   0         4
                46.48          1.82        1.9538    2   6   0         4
                47.93         12.60        1.8980    4   1   3         8
                47.93          7.06        1.8980    1   4   3         8
                49.56          1.39        1.8393    0   0   4         2
                49.65         14.56        1.8363    5   3   2         8
                49.65          1.78        1.8363    3   5   2         8
                50.81          1.50        1.7970    6   0   2         8
                51.12          2.32        1.7869    6   3   1         8
                51.12          1.70        1.7869    3   6   1         8
                51.86          1.45        1.7629    2   0   4         8
                52.36          1.16        1.7475    5   5   0         4
                52.36          1.95        1.7475    1   7   0         4
                52.57          4.87        1.7408    3   4   3         8
                52.57          1.92        1.7408    4   3   3         8
                54.10          4.20        1.6952    2   2   4         8
                55.57          1.30        1.6539    2   7   1         8
                56.74          1.80        1.6225    7   3   0         4
                58.47          1.71        1.5785    5   5   2         8
                59.05          3.32        1.5644    6   1   3         8
                61.83          2.08        1.5004    7   4   1         8
                61.92          1.80        1.4985    2   8   0         4
                61.92          1.44        1.4985    8   2   0         4
                62.57          1.75        1.4845    7   3   2         8
                62.57          1.46        1.4845    3   7   2         8
                64.92          1.68        1.4364    7   5   0         4
                65.55          1.51        1.4241    8   0   2         8
                67.42          1.36        1.3891    5   3   4         8
                67.42          3.01        1.3891    3   5   4         8
                67.49          1.17        1.3878    2   8   2         8
                70.36          1.64        1.3380    5   7   2         8
                71.42          1.32        1.3208    1   4   5         8
                71.56          1.34        1.3186    9   2   1         8
                72.76          1.15        1.2997    8   1   3         8
                77.91          1.02        1.2262    0   0   6         2
                80.62          2.12        1.1917    1   6   5         8
                80.62          1.75        1.1917    6   1   5         8
                82.32          1.72        1.1714   10   0   2         8
                84.22          1.08        1.1497    3   6   5         8
                89.72          1.23        1.0930    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.