Examination of the thermal and metallographic characteristics at high temperatures of natural stones (andesite) extracted from different elevations

MakaleAçık ErişimScopus SJRQ2

Özet

This study examines the high‑temperature thermal response of andesite stones extracted from two different elevations of Mount Ağrı (Türkiye) in order to improve material selection strategies for engineering applications. Thermal conductivity and density values of the samples were first measured under laboratory conditions. The specimens were then heated to 850 °C and cooled by natural convection while surface temperatures were recorded at fixed time intervals using a thermal camera. Based on these measurements, convective heat transfer coefficients were determined, and the time‑dependent thermal diffusivity and Biot numbers were subsequently calculated using the first-term approximation of the Fourier series. Metallographic examinations were conducted to correlate the thermal behavior with microstructural characteristics. Results indicate a pronounced effect of elevation on thermal performance. The sample obtained from the higher elevation exhibited substantially greater thermal diffusivity, reaching 2.93 × 10⁻5 m2 s−1 at 360 s and decreasing to 8.96 × 10⁻6 m2 s−1 at 1300 s. In contrast, the lower‑elevation andesite showed lower diffusivity values (1.83 × 10⁻5 m2 s−1 at 360 s and 5.9 × 10⁻6 m2 s−1 at 1300 s). Conversely, Biot numbers were consistently higher for the lower‑elevation sample, decreasing from 0.60 to 0.29 during the cooling process, whereas the high‑elevation sample displayed values from 0.314 to 0.165. Metallographic analysis confirmed that variations in microstructure—linked to different geological formation conditions—directly influenced these thermophysical properties. Overall, the findings demonstrate that andesite sourced at higher elevations possesses superior thermal diffusivity and more favorable heat‑transfer characteristics at elevated temperatures. These results highlight the importance of geological origin in the design, assessment, and selection of natural stone materials for high‑temperature engineering applications.

Anahtar Kelimeler

RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/munzur/1247Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.1007/s10973-026-15650-wYayıncı resmi DOI adresi
İndeks kayıtları
Kaydın indeks veri tabanlarındaki sayfası (aktarımda alınan kayıt numarasıyla). Erişim, indeksin kendi koşullarına bağlıdır.
Atıflar
Scopus
0
WoS
0
OpenAlex
0
Her kaynağın kendi saydığı toplam atıf; aktarım ve zenginleştirme sırasında alındı.
Tam Kayıt
AlanDeğerDil
dc.contributor.authorIşık, Erdem
dc.contributor.authorKahraman, Gökhan
dc.contributor.authorAtalar, Aydın
dc.date.accessioned2026-10-28T14:54:01.543060092Z
dc.date.available2026-10-28T14:54:01.543060092Z
dc.date.issued2026
dc.description.abstractThis study examines the high‑temperature thermal response of andesite stones extracted from two different elevations of Mount Ağrı (Türkiye) in order to improve material selection strategies for engineering applications. Thermal conductivity and density values of the samples were first measured under laboratory conditions. The specimens were then heated to 850 °C and cooled by natural convection while surface temperatures were recorded at fixed time intervals using a thermal camera. Based on these measurements, convective heat transfer coefficients were determined, and the time‑dependent thermal diffusivity and Biot numbers were subsequently calculated using the first-term approximation of the Fourier series. Metallographic examinations were conducted to correlate the thermal behavior with microstructural characteristics. Results indicate a pronounced effect of elevation on thermal performance. The sample obtained from the higher elevation exhibited substantially greater thermal diffusivity, reaching 2.93 × 10⁻5 m2 s−1 at 360 s and decreasing to 8.96 × 10⁻6 m2 s−1 at 1300 s. In contrast, the lower‑elevation andesite showed lower diffusivity values (1.83 × 10⁻5 m2 s−1 at 360 s and 5.9 × 10⁻6 m2 s−1 at 1300 s). Conversely, Biot numbers were consistently higher for the lower‑elevation sample, decreasing from 0.60 to 0.29 during the cooling process, whereas the high‑elevation sample displayed values from 0.314 to 0.165. Metallographic analysis confirmed that variations in microstructure—linked to different geological formation conditions—directly influenced these thermophysical properties. Overall, the findings demonstrate that andesite sourced at higher elevations possesses superior thermal diffusivity and more favorable heat‑transfer characteristics at elevated temperatures. These results highlight the importance of geological origin in the design, assessment, and selection of natural stone materials for high‑temperature engineering applications.
dc.description.sponsorshipTürkiye Bilimsel ve Teknolojik Araştırma Kurumu, TUBITAK
dc.identifier.doi10.1007/s10973-026-15650-w
dc.identifier.eissn1588-2926
dc.identifier.endpage8347
dc.identifier.issn1388-6150
dc.identifier.issue10
dc.identifier.scopus2-s2.0-105039941316
dc.identifier.startpage8335
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/munzur/1247
dc.identifier.volume151
dc.identifier.wosWOS:001775443600001
dc.language.isoen
dc.publisherSpringer Science and Business Media B.V.
dc.relation.ispartofJournal of Thermal Analysis and Calorimetry
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectEnergy
dc.subjectNatural convection
dc.subjectNatural stones
dc.subjectTime-dependent heat transfer
dc.subject.classificationThermodynamics
dc.subject.classificationChemistry, Analytical
dc.subject.classificationChemistry, Physical
dc.subject.classificationChemistry
dc.subject.otherGeology
dc.subject.otherHeat convection
dc.subject.otherHeat transfer coefficients
dc.subject.otherHigh temperature applications
dc.subject.otherHigh temperature engineering
dc.subject.otherMetallography
dc.subject.otherThermal conductivity
dc.subject.otherThermal diffusivity
dc.subject.otherThermal Engineering
dc.subject.otherBiot number
dc.subject.otherEnergy
dc.subject.otherEngineering applications
dc.subject.otherHigh elevation
dc.subject.otherHighest temperature
dc.subject.otherMaterials selection
dc.subject.otherNatural stones
dc.subject.otherThermal
dc.subject.otherThermal response
dc.subject.otherTime-dependent heat transfer
dc.subject.otherFourier series
dc.titleExamination of the thermal and metallographic characteristics at high temperatures of natural stones (andesite) extracted from different elevations
dc.typeArticle
rdl.citation.openalex0
rdl.citation.scopus0
rdl.citation.wos0
rdl.oa.statushybrid
rdl.oa.urlhttps://link.springer.com/content/pdf/10.1007/s10973-026-15650-w.pdf
rdl.scopus.quartileQ2
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)