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Anhydrite crystal structure

The supersaturation is too low in all experiments to be measured accurately, but it seems reasonable to assume that the effect of residence time is imposed through the kinetics. Another observation is that the D-value for cadmium uptake in anhydrite is about ten times higher than in HH or DH. An explanation for this higher D seems to be related to the crystal structures of the calcium sulfates. Only the AH structure matches with an anhydrous CdSO phase, while no hemi- or dihydrate phase of CdS04 exists. [Pg.390]

Other inorganic crystals studied by Mark and his collaborators, sometimes leading to complete structure determinations, include strontium chloride, zinc hydroxide, tin tetraiodide, potassium chlorate, potassium permanganage, and ammonium ferrocyanide. Minerals investigated by them include CaSO (anhydrite), BaSO (barite), PbSO, Fe2TiO[j (pseudobrookite), and three forms of Al2Si05 (cyanite, andalusite, and sillimanite). [Pg.95]

After the induction period (initial solution of hemihydrate t>r anhydrite), nuclcation of dihydrale occurs. Further crystal growth leads to a close-grained structure of dihydratc crystals which accounts for the rigidity of plaster Excess water is rcmove<.l by drying... [Pg.423]


See other pages where Anhydrite crystal structure is mentioned: [Pg.328]    [Pg.186]    [Pg.257]    [Pg.253]    [Pg.470]    [Pg.113]    [Pg.192]    [Pg.740]    [Pg.740]    [Pg.154]    [Pg.117]    [Pg.340]    [Pg.134]    [Pg.36]    [Pg.361]   
See also in sourсe #XX -- [ Pg.157 ]




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