Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature
The thermal conductivity of a single-phase gehlenite (2CaO Al 2 O 3 SiO 2 ) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO 2 :Al 2 O 3 = 38:28:34 (mass%), which was maintained after melting and cooling. After polish...
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description | The thermal conductivity of a single-phase gehlenite (2CaO Al
2
O
3
SiO
2
) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO
2
:Al
2
O
3
= 38:28:34 (mass%), which was maintained after melting and cooling. After polishing the samples, the size of the gehlenite crystal was sufficiently large to be measured using a thermal microscope. The value of
λ
C
ρ
, where
λ
is thermal conductivity
C
is specific heat andρis density, of the samples was measured every 10 μm to obtain its distribution. When comparing the results with the optical microscopy image of the sample, the gehlenite region showed a larger value of
λ
C
ρ
than the glassy region. Specifically, the value of
λ
C
ρ
of the gehlenite region was determined to be 2.2 ± 0.1 kJs
−0.5
·m
−2
·K
−1
, which resulted in a thermal conductivity of 2.1 ± 0.2 Wm
−1
·K
−1
. Moreover, the oxide gehlenite phase showed lower thermal conductivity than the other constituent phases, i.e., CaO, Al
2
O
3
, and SiO
2
. |
doi_str_mv | 10.1007/s10765-023-03185-3 |
format | Article |
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2
O
3
SiO
2
) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO
2
:Al
2
O
3
= 38:28:34 (mass%), which was maintained after melting and cooling. After polishing the samples, the size of the gehlenite crystal was sufficiently large to be measured using a thermal microscope. The value of
λ
C
ρ
, where
λ
is thermal conductivity
C
is specific heat andρis density, of the samples was measured every 10 μm to obtain its distribution. When comparing the results with the optical microscopy image of the sample, the gehlenite region showed a larger value of
λ
C
ρ
than the glassy region. Specifically, the value of
λ
C
ρ
of the gehlenite region was determined to be 2.2 ± 0.1 kJs
−0.5
·m
−2
·K
−1
, which resulted in a thermal conductivity of 2.1 ± 0.2 Wm
−1
·K
−1
. Moreover, the oxide gehlenite phase showed lower thermal conductivity than the other constituent phases, i.e., CaO, Al
2
O
3
, and SiO
2
.</description><identifier>ISSN: 0195-928X</identifier><identifier>EISSN: 1572-9567</identifier><identifier>DOI: 10.1007/s10765-023-03185-3</identifier><language>eng</language><publisher>New York: Springer US</publisher><subject>Aluminum oxide ; Calcium oxide ; Classical Mechanics ; Condensed Matter Physics ; Gehlenite ; Geophysics ; Heat conductivity ; Heat transfer ; Industrial Chemistry/Chemical Engineering ; Microscopy ; Optical microscopy ; Physical Chemistry ; Physics ; Physics and Astronomy ; Room temperature ; Silicon dioxide ; Thermal conductivity ; Thermal microscopy ; Thermodynamics</subject><ispartof>International journal of thermophysics, 2023-06, Vol.44 (6), Article 93</ispartof><rights>The Author(s) 2023</rights><rights>The Author(s) 2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c358t-5cd0d0477cdbafd00ae221079388f5b366ea6a6ca750e93a12489b37ff59aac43</cites><orcidid>0000-0002-4844-4159 ; 0000-0001-5449-2651</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10765-023-03185-3$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10765-023-03185-3$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Inoue, Yuta</creatorcontrib><creatorcontrib>Watanabe, Takashi</creatorcontrib><creatorcontrib>Hayashi, Miyuki</creatorcontrib><creatorcontrib>Susa, Masahiro</creatorcontrib><creatorcontrib>Endo, Rie</creatorcontrib><title>Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature</title><title>International journal of thermophysics</title><addtitle>Int J Thermophys</addtitle><description>The thermal conductivity of a single-phase gehlenite (2CaO Al
2
O
3
SiO
2
) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO
2
:Al
2
O
3
= 38:28:34 (mass%), which was maintained after melting and cooling. After polishing the samples, the size of the gehlenite crystal was sufficiently large to be measured using a thermal microscope. The value of
λ
C
ρ
, where
λ
is thermal conductivity
C
is specific heat andρis density, of the samples was measured every 10 μm to obtain its distribution. When comparing the results with the optical microscopy image of the sample, the gehlenite region showed a larger value of
λ
C
ρ
than the glassy region. Specifically, the value of
λ
C
ρ
of the gehlenite region was determined to be 2.2 ± 0.1 kJs
−0.5
·m
−2
·K
−1
, which resulted in a thermal conductivity of 2.1 ± 0.2 Wm
−1
·K
−1
. Moreover, the oxide gehlenite phase showed lower thermal conductivity than the other constituent phases, i.e., CaO, Al
2
O
3
, and SiO
2
.</description><subject>Aluminum oxide</subject><subject>Calcium oxide</subject><subject>Classical Mechanics</subject><subject>Condensed Matter Physics</subject><subject>Gehlenite</subject><subject>Geophysics</subject><subject>Heat conductivity</subject><subject>Heat transfer</subject><subject>Industrial Chemistry/Chemical Engineering</subject><subject>Microscopy</subject><subject>Optical microscopy</subject><subject>Physical Chemistry</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Room temperature</subject><subject>Silicon dioxide</subject><subject>Thermal conductivity</subject><subject>Thermal microscopy</subject><subject>Thermodynamics</subject><issn>0195-928X</issn><issn>1572-9567</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kEFLxDAQhYMouK7-AU8Bz9Fpsmmao6y6CiuCrCB4CGma7la2TU2yQv-9WSt6kzkMA997M_MQOs_gMgMQVyEDkXMClBFgWcEJO0CTjAtKJM_FIZpAJjmRtHg9RichvAOAFJJN0NuNjda3Tdd0axw3Fq82adRbPHddtTOx-WzigF2NF3aztV0TLS6HX-ixMd4F4_oB64ifnWvxyra99TruvD1FR7XeBnv206fo5e52Nb8ny6fFw_x6SQzjRSTcVFDBTAhTlbquALSlNP0jWVHUvGR5bnWuc6MFByuZzuiskCUTdc2l1mbGpuhi9O29-9jZENW72_kurVS0gJyDSJUoOlL7k4O3tep902o_qAzUPkQ1hqhSiOo7RMWSiI2ikOBubf2f9T-qL6PMdas</recordid><startdate>20230601</startdate><enddate>20230601</enddate><creator>Inoue, Yuta</creator><creator>Watanabe, Takashi</creator><creator>Hayashi, Miyuki</creator><creator>Susa, Masahiro</creator><creator>Endo, Rie</creator><general>Springer US</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><orcidid>https://orcid.org/0000-0002-4844-4159</orcidid><orcidid>https://orcid.org/0000-0001-5449-2651</orcidid></search><sort><creationdate>20230601</creationdate><title>Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature</title><author>Inoue, Yuta ; Watanabe, Takashi ; Hayashi, Miyuki ; Susa, Masahiro ; Endo, Rie</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c358t-5cd0d0477cdbafd00ae221079388f5b366ea6a6ca750e93a12489b37ff59aac43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Aluminum oxide</topic><topic>Calcium oxide</topic><topic>Classical Mechanics</topic><topic>Condensed Matter Physics</topic><topic>Gehlenite</topic><topic>Geophysics</topic><topic>Heat conductivity</topic><topic>Heat transfer</topic><topic>Industrial Chemistry/Chemical Engineering</topic><topic>Microscopy</topic><topic>Optical microscopy</topic><topic>Physical Chemistry</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Room temperature</topic><topic>Silicon dioxide</topic><topic>Thermal conductivity</topic><topic>Thermal microscopy</topic><topic>Thermodynamics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Inoue, Yuta</creatorcontrib><creatorcontrib>Watanabe, Takashi</creatorcontrib><creatorcontrib>Hayashi, Miyuki</creatorcontrib><creatorcontrib>Susa, Masahiro</creatorcontrib><creatorcontrib>Endo, Rie</creatorcontrib><collection>SpringerOpen</collection><collection>CrossRef</collection><jtitle>International journal of thermophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Inoue, Yuta</au><au>Watanabe, Takashi</au><au>Hayashi, Miyuki</au><au>Susa, Masahiro</au><au>Endo, Rie</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature</atitle><jtitle>International journal of thermophysics</jtitle><stitle>Int J Thermophys</stitle><date>2023-06-01</date><risdate>2023</risdate><volume>44</volume><issue>6</issue><artnum>93</artnum><issn>0195-928X</issn><eissn>1572-9567</eissn><abstract>The thermal conductivity of a single-phase gehlenite (2CaO Al
2
O
3
SiO
2
) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO
2
:Al
2
O
3
= 38:28:34 (mass%), which was maintained after melting and cooling. After polishing the samples, the size of the gehlenite crystal was sufficiently large to be measured using a thermal microscope. The value of
λ
C
ρ
, where
λ
is thermal conductivity
C
is specific heat andρis density, of the samples was measured every 10 μm to obtain its distribution. When comparing the results with the optical microscopy image of the sample, the gehlenite region showed a larger value of
λ
C
ρ
than the glassy region. Specifically, the value of
λ
C
ρ
of the gehlenite region was determined to be 2.2 ± 0.1 kJs
−0.5
·m
−2
·K
−1
, which resulted in a thermal conductivity of 2.1 ± 0.2 Wm
−1
·K
−1
. Moreover, the oxide gehlenite phase showed lower thermal conductivity than the other constituent phases, i.e., CaO, Al
2
O
3
, and SiO
2
.</abstract><cop>New York</cop><pub>Springer US</pub><doi>10.1007/s10765-023-03185-3</doi><orcidid>https://orcid.org/0000-0002-4844-4159</orcidid><orcidid>https://orcid.org/0000-0001-5449-2651</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Aluminum oxide Calcium oxide Classical Mechanics Condensed Matter Physics Gehlenite Geophysics Heat conductivity Heat transfer Industrial Chemistry/Chemical Engineering Microscopy Optical microscopy Physical Chemistry Physics Physics and Astronomy Room temperature Silicon dioxide Thermal conductivity Thermal microscopy Thermodynamics |
title | Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature |
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