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<dc:title>Atmosphere-controlled thermal processing enables tunable optical properties via iron-oxide phase engineering in natural silicate materials</dc:title>
<dc:creator>Urbaneja Miguel, Álvaro</dc:creator>
<dc:creator>Torija López, Alba</dc:creator>
<dc:creator>Carrancho Alonso, Ángel</dc:creator>
<dc:creator>Iriarte Avilés, Eneko</dc:creator>
<dc:creator>González Moreno, Sara</dc:creator>
<dc:creator>González Martín, José Manuel</dc:creator>
<dc:creator>Trigo López, Miriam</dc:creator>
<dc:creator>Vallejos Calzada, Saúl</dc:creator>
<dc:subject>Iron-oxide phase equilibria</dc:subject>
<dc:subject>Redox-controlled thermal processing</dc:subject>
<dc:subject>Process–structure–property relationship</dc:subject>
<dc:subject>Magnetite–hematite transformation</dc:subject>
<dc:subject>Atmosphere-controlled heat treatment</dc:subject>
<dc:subject>Functional optical materials</dc:subject>
<dc:description>Controlled-atmosphere thermal processing was investigated as a method to engineer iron-oxide phase assemblages in iron-bearing silicate materials. Natural sandstone was heated between 200 and 1000 °C under air, N2 and CO2 atmospheres to evaluate how oxygen partial pressure governs redox transformations and the resulting macroscopic optical behaviour.&#xd;
The treatments produced a wide and reproducible range of optical responses from a single starting material. Colour evolution, quantified in the CIELAB space, correlates with bulk mineral transformations. Oxidizing conditions stabilize hematite-dominated assemblages and generate red hues, whereas reduced-oxygen atmospheres promote magnetite formation and progressive darkening. Rock-magnetic measurements identify atmosphere-dependent phase assemblages, including a high-coercivity iron oxide under strongly oxidizing conditions. The magnetic response mirrors the optical evolution, indicating that colour development originates from internal phase transformations.&#xd;
Compressive strength remained within the same order of magnitude as the untreated material across the studied conditions, indicating no catastrophic mechanical degradation.&#xd;
These results show that oxygen availability acts as a key processing variable controlling iron-oxide stability and optical response. The study establishes a process-based approach for tuning optical properties in mineral materials through atmosphere-controlled thermal processing without chemical additives. Unlike previous studies focused on temperature-driven effects or isolated observations, this work demonstrates a reproducible process-based approach to tune optical properties in natural silicate materials through controlled atmosphere engineering.</dc:description>
<dc:date>2026-08-27T11:52:34Z</dc:date>
<dc:date>2026-08-27T11:52:34Z</dc:date>
<dc:date>2026-05-29</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:identifier>2238-7854</dc:identifier>
<dc:identifier>https://hdl.handle.net/10259/11978</dc:identifier>
<dc:identifier>10.1016/j.jmrt.2026.05.175</dc:identifier>
<dc:language>eng</dc:language>
<dc:relation>Journal of Materials Research and Technology. 2026, V. 42, p. 10750-10759</dc:relation>
<dc:relation>https://doi.org/10.1016/j.jmrt.2026.05.175</dc:relation>
<dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
<dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
<dc:rights>Atribución 4.0 Internacional</dc:rights>
<dc:publisher>Elsevier</dc:publisher>
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