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   <dc:title>Structure, Atomistic Simulations, and Phase Transition of Stoichiometric Yeelimite</dc:title>
   <dc:creator>Cuesta-García, Ana María</dc:creator>
   <dc:creator>Gómez-de-la-Torre, María de los  Ángeles</dc:creator>
   <dc:creator>Losilla, Enrique R.</dc:creator>
   <dc:creator>Peterson, Vanessa K.</dc:creator>
   <dc:creator>Rejmak, Pawel</dc:creator>
   <dc:creator>Ayuela, Andrés</dc:creator>
   <dc:creator>Frontera, Carlos</dc:creator>
   <dc:creator>García-Aranda, Miguel Ángel</dc:creator>
   <dc:subject>Cemento</dc:subject>
   <dcterms:abstract>ABSTRACT: Yeelimite, Ca4[Al6O12]SO4, is outstanding as an aluminate&#xd;
sodalite, being the framework of these type of materials flexible and dependent&#xd;
on ion sizes and anion ordering/disordering. On the other hand, yeelimite is also&#xd;
important from an applied perspective as it is the most important phase in&#xd;
calcium sulfoaluminate cements. However, its crystal structure is not well&#xd;
studied. Here, we characterize the room temperature crystal structure of&#xd;
stoichiometric yeelimite through joint Rietveld refinement using neutron and Xray&#xd;
powder diffraction data coupled with chemical soft-constraints. Our structural&#xd;
study shows that yeelimite has a lower symmetry than that of the previously&#xd;
reported tetragonal system, which we establish to likely be the acentric&#xd;
orthorhombic space group Pcc2, with a √2a × √2a × a superstructure based on&#xd;
the cubic sodalite structure. Final unit cell values were a = 13.0356(7) Å, b =&#xd;
13.0350(7) Å, and c = 9.1677(2) Å. We determine several structures using&#xd;
density functional theory calculations, with the lowest energy structure being Pcc2 in agreement with our experimental result.&#xd;
Yeelimite undergoes a reversible phase transition to a higher-symmetry phase which has been characterized to occur at 470 °C by&#xd;
thermodiffractometry. The higher-symmetry phase is likely cubic or pseudocubic possessing an incommensurate superstructure,&#xd;
as suggested by our theoretical calculations which show a phase transition from an orthorhombic to a tetragonal structure. Our&#xd;
theoretical study also predicts a pressure-induced phase transition to a cubic structure of space group I43m. Finally, we show that&#xd;
our reported crystal structure of yeelimite enables better mineralogical phase analysis of commercial calcium sulfoaluminate&#xd;
cements, as shown by RF values for this phase, 6.9% and 4.8% for the previously published orthorhombic structure and for the&#xd;
one reported in this study, respectively.</dcterms:abstract>
   <dcterms:dateAccepted>2017-06-28T07:16:13Z</dcterms:dateAccepted>
   <dcterms:available>2017-06-28T07:16:13Z</dcterms:available>
   <dcterms:created>2017-06-28T07:16:13Z</dcterms:created>
   <dcterms:issued>2013</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>Chem. Mater. 2013, 25, 1680−1687</dc:identifier>
   <dc:identifier>0897-4756</dc:identifier>
   <dc:identifier>http://hdl.handle.net/10630/14020</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:rights>by-nc-nd</dc:rights>
   <dc:publisher>ACS publications</dc:publisher>
</qdc:qualifieddc>
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