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The Link between Brushite and Gypsum: Miscibility, Dehydration, and Crystallochemical Behavior in the CaHPO4·2H2O−CaSO4·2H2O System

dc.contributor.authorPinto, André Filipe Jorge 
dc.contributor.authorCarneiro, Joana
dc.contributor.authorKatsikopoulos, Dionysios 
dc.contributor.authorJiménez Bautista, Amalia 
dc.contributor.authorPrieto Rubio, Manuel 
dc.date.accessioned2016-04-08T07:40:53Z
dc.date.available2016-04-08T07:40:53Z
dc.date.issued2012
dc.identifier.citationCrystal Growth & Design ,12 (1), p. 445–455 (2012); doi:10.1021/cg2012815
dc.identifier.issn1528-7483
dc.identifier.issn1528-7505
dc.identifier.urihttp://hdl.handle.net/10651/36371
dc.description.abstractThe present study explores the mixing properties of the Ca(SO4,HPO4)·2H2O solid solution and the role of the “double-salt” Ca2SO4HPO4·4H2O (ardealite) by means of precipitation experiments carried out in a solution calorimeter at 25 °C. Moreover, the dehydration behavior of a number of solids with different compositions is studied by thermogravimetry and thermoX-ray diffraction. The experimental results indicate the existence of two (sulfate-rich and phosphate-rich) ranges of solid solution that are separated by two miscibility gaps from a range around the midpoint 50% molar) composition in which ardealite forms. On the phosphate-rich miscibility range, the structural (020) layers contract with the sulfate content, whereas the interlayer spacing expands. This contraction is consistent with the negative enthalpy of mixing determined from the calorimetric data. For the ardealite range of compositions, the strong contraction of the (020) layers resolves in a different stacking sequence (with double b-axis and (040) as elementary stacking layers). Therefore, ardealite is demonstrated to be not a member of the Ca(SO4,HPO4)·2H2O solid solution but a nearly stoichiometric compound with specific structural features. The thermogravimetric study indicates a specific dehydration behavior for ardealite, which again supports the idea that this phase is not a member of the solid solution.eng
dc.description.sponsorshipThis research was supported by the Marie Curie European Network “Mineral Nucleation and Growth Kinetics” (European Commission Grant UE-MRTN-CT- 2006- 035488) and by the Spanish Ministry of Education and Science (Grant CGL2010- 20134-CO2-02)eng
dc.format.extentp. 445 - 455spa
dc.language.isoengspa
dc.publisherAmerican Chemical Societyeng
dc.relation.ispartofCrystal Growth & Design, 12(1)spa
dc.rights© American Chemical Society 2011
dc.subjectbrusitespa
dc.subjectgypsumspa
dc.subjectmiscibilityspa
dc.subjectdehydrationspa
dc.subjectCrystallochemicalspa
dc.titleThe Link between Brushite and Gypsum: Miscibility, Dehydration, and Crystallochemical Behavior in the CaHPO4·2H2O−CaSO4·2H2O Systemeng
dc.typeinfo:eu-repo/semantics/articlespa
dc.identifier.doi10.1021/cg2012815
dc.type.dcmitextspa
dc.relation.projectIDCGL2010-20134-CO2-02 (European Commission grant UE-MRTN-CT- 2006- 035488)eng
dc.relation.projectIDMINECO/CGL2010-20134-CO2-02
dc.relation.projectIDUE/MRTN-CT- 2006- 035488
dc.relation.publisherversionhttp://dx.doi.org/10.1021/cg2012815eng
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessspa


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