<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-05-27T05:32:14Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/9784" metadataPrefix="marc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/9784</identifier><datestamp>2026-02-03T10:52:44Z</datestamp><setSpec>com_10630_2254</setSpec><setSpec>col_10630_37953</setSpec></header><metadata><record xmlns="http://www.loc.gov/MARC21/slim" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Cuesta-García, Ana María</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">García-Aranda, Miguel Ángel</subfield>
      <subfield code="e">author</subfield>
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Sanz, Jesús</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Gómez-de-la-Torre, María de los  Ángeles</subfield>
      <subfield code="e">author</subfield>
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Losilla, Enrique R.</subfield>
      <subfield code="e">author</subfield>
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   <datafield ind2=" " ind1=" " tag="260">
      <subfield code="c">2013-11-11</subfield>
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      <subfield code="a">Stoichiometric dicalcium silicate, Ca2SiO4, displays a well-known polymorphism with temperature. When&#xd;
this phase is doped by a range of elements, belite, one of the main phases of cements, is generated. Here,&#xd;
we thoroughly study the aluminum doping of dicalcium silicate. This type of study is important for&#xd;
cement characterization and also from a basic point of view. Ca2Si1−2xAl2xO4−x□x (x = 0, 0.010, 0.014,&#xd;
0.03) has been prepared and studied by X-ray powder diffraction and the Rietveld method. The limiting&#xd;
composition has been established as Ca2Si0.972Al0.028O3.986□0.014. The 27Al MAS NMR band located close&#xd;
to ∼−70 ppm is ascribed to tetrahedral environments, in agreement with the proposed aliovalent Si/Al&#xd;
atomic substitution mechanism. Thermal analysis measurements under a wet atmosphere indirectly&#xd;
confirm the increase of oxygen vacancies as the amount of incorporated protons increases with the&#xd;
aluminium content. A thorough electrical characterization has been carried out including overall conductivity&#xd;
measurements under wet and dry atmospheres and conductivity as a function of the oxygen&#xd;
partial pressure. The samples show oxide anion conductivity with a small p-type electronic contribution&#xd;
under oxidizing conditions. These compounds display a very important proton contribution to the overall&#xd;
conductivities under humidified atmospheres.</subfield>
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   <datafield ind1="8" ind2=" " tag="024">
      <subfield code="a">1477-9226</subfield>
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      <subfield code="a">http://hdl.handle.net/10630/9784</subfield>
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   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Químina inorgánica</subfield>
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   <datafield ind2="0" ind1="0" tag="245">
      <subfield code="a">Mechanism of stabilization of dicalcium silicate solid solution with aluminium</subfield>
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