Decomposition of Mullite by Silica Volatilization
Thermal decomposition of mullite into corundum was investigated using a high‐temperature X‐ray single‐crystal camera equipped with a gas‐flame furnace and by scanning electron microscopy and electron probe microanalysis (EPMA). When heated to ∼1750°C, mullite decomposed to corundum by the liberation...
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Veröffentlicht in: | Journal of the American Ceramic Society 1980-01, Vol.63 (1-2), p.44-46 |
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creator | IWAI, SHIN-ICHI WATANABE, TAKASHI MINATO, ICHIRO OKADA, KIYOSHI MORIKAWA, HIDEKI |
description | Thermal decomposition of mullite into corundum was investigated using a high‐temperature X‐ray single‐crystal camera equipped with a gas‐flame furnace and by scanning electron microscopy and electron probe microanalysis (EPMA). When heated to ∼1750°C, mullite decomposed to corundum by the liberation of the SiO2 component with topotaxial relations of:
1
(310)mull∥(001)cor; [001]mull∥[110]cor
2
(130)mull∥(001)cor; [001]mull∥[110]cor
3
(110)mull∥(001)cor; [001]mull∥[110]cor
Thus, it was considered that, when mullite decomposed into corundum, their oxygen close‐packed planes were almost preserved. The SEM photographs showed that the crystals of the developed corundum are prismatic and ∼5 μm wide. The EPMA showed that the phase boundary between mullite and developed corundum is discontinuous. |
doi_str_mv | 10.1111/j.1151-2916.1980.tb10647.x |
format | Article |
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1
(310)mull∥(001)cor; [001]mull∥[110]cor
2
(130)mull∥(001)cor; [001]mull∥[110]cor
3
(110)mull∥(001)cor; [001]mull∥[110]cor
Thus, it was considered that, when mullite decomposed into corundum, their oxygen close‐packed planes were almost preserved. The SEM photographs showed that the crystals of the developed corundum are prismatic and ∼5 μm wide. The EPMA showed that the phase boundary between mullite and developed corundum is discontinuous.</description><identifier>ISSN: 0002-7820</identifier><identifier>EISSN: 1551-2916</identifier><identifier>DOI: 10.1111/j.1151-2916.1980.tb10647.x</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><ispartof>Journal of the American Ceramic Society, 1980-01, Vol.63 (1-2), p.44-46</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4484-6ecd40892f437c5a86b16ef3f4dba5b319b4163d460f81dd5cd9cb802fa6bb1b3</citedby><cites>FETCH-LOGICAL-c4484-6ecd40892f437c5a86b16ef3f4dba5b319b4163d460f81dd5cd9cb802fa6bb1b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fj.1151-2916.1980.tb10647.x$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fj.1151-2916.1980.tb10647.x$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,777,781,1412,27850,27905,27906,45555,45556</link.rule.ids></links><search><creatorcontrib>IWAI, SHIN-ICHI</creatorcontrib><creatorcontrib>WATANABE, TAKASHI</creatorcontrib><creatorcontrib>MINATO, ICHIRO</creatorcontrib><creatorcontrib>OKADA, KIYOSHI</creatorcontrib><creatorcontrib>MORIKAWA, HIDEKI</creatorcontrib><title>Decomposition of Mullite by Silica Volatilization</title><title>Journal of the American Ceramic Society</title><description>Thermal decomposition of mullite into corundum was investigated using a high‐temperature X‐ray single‐crystal camera equipped with a gas‐flame furnace and by scanning electron microscopy and electron probe microanalysis (EPMA). When heated to ∼1750°C, mullite decomposed to corundum by the liberation of the SiO2 component with topotaxial relations of:
1
(310)mull∥(001)cor; [001]mull∥[110]cor
2
(130)mull∥(001)cor; [001]mull∥[110]cor
3
(110)mull∥(001)cor; [001]mull∥[110]cor
Thus, it was considered that, when mullite decomposed into corundum, their oxygen close‐packed planes were almost preserved. The SEM photographs showed that the crystals of the developed corundum are prismatic and ∼5 μm wide. The EPMA showed that the phase boundary between mullite and developed corundum is discontinuous.</description><issn>0002-7820</issn><issn>1551-2916</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1980</creationdate><recordtype>article</recordtype><sourceid>K30</sourceid><recordid>eNqVkEFPwzAMhSMEEmPwHyo4t8RNmqYckMYYG2iMAwOOUZKmUkq3jqYTG7-eVJ2444tt-b1n6UPoEnAEvq5L3xII4wxYBBnHUasAM5pGuyM0gORwOkYDjHEcpjzGp-jMudKvXk4HCO6Nrleb2tnW1uugLoLnbVXZ1gRqH7zaymoZvNeVbP34IzvNOTopZOXMxaEP0dvDZDmehfOX6eN4NA81pZyGzOicYp7FBSWpTiRnCpgpSEFzJRNFIFMUGMkpwwWHPE90nmnFcVxIphQoMkRXfe6mqb-2xrWirLfN2r8UEGeccMx56lU3vUo3tXONKcSmsSvZ7AVg0SESpegQiY6D6BCJAyKx8-bb3vxtK7P_h1M8jcYTSn1A2AdY15rdX4BsPgVLSZqIj8VUJPPZAhZ3IJbkFwlrfM4</recordid><startdate>198001</startdate><enddate>198001</enddate><creator>IWAI, SHIN-ICHI</creator><creator>WATANABE, TAKASHI</creator><creator>MINATO, ICHIRO</creator><creator>OKADA, KIYOSHI</creator><creator>MORIKAWA, HIDEKI</creator><general>Blackwell Publishing Ltd</general><general>American Ceramic Society</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>HDMVH</scope><scope>K30</scope><scope>PAAUG</scope><scope>PAWHS</scope><scope>PAWZZ</scope><scope>PAXOH</scope><scope>PBHAV</scope><scope>PBQSW</scope><scope>PBYQZ</scope><scope>PCIWU</scope><scope>PCMID</scope><scope>PCZJX</scope><scope>PDGRG</scope><scope>PDWWI</scope><scope>PETMR</scope><scope>PFVGT</scope><scope>PGXDX</scope><scope>PIHIL</scope><scope>PISVA</scope><scope>PJCTQ</scope><scope>PJTMS</scope><scope>PLCHJ</scope><scope>PMHAD</scope><scope>PNQDJ</scope><scope>POUND</scope><scope>PPLAD</scope><scope>PQAPC</scope><scope>PQCAN</scope><scope>PQCMW</scope><scope>PQEME</scope><scope>PQHKH</scope><scope>PQMID</scope><scope>PQNCT</scope><scope>PQNET</scope><scope>PQSCT</scope><scope>PQSET</scope><scope>PSVJG</scope><scope>PVMQY</scope><scope>PZGFC</scope></search><sort><creationdate>198001</creationdate><title>Decomposition of Mullite by Silica Volatilization</title><author>IWAI, SHIN-ICHI ; WATANABE, TAKASHI ; MINATO, ICHIRO ; OKADA, KIYOSHI ; MORIKAWA, HIDEKI</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4484-6ecd40892f437c5a86b16ef3f4dba5b319b4163d460f81dd5cd9cb802fa6bb1b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1980</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>IWAI, SHIN-ICHI</creatorcontrib><creatorcontrib>WATANABE, TAKASHI</creatorcontrib><creatorcontrib>MINATO, ICHIRO</creatorcontrib><creatorcontrib>OKADA, KIYOSHI</creatorcontrib><creatorcontrib>MORIKAWA, HIDEKI</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Periodicals Index Online Segment 15</collection><collection>Periodicals Index Online</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - West</collection><collection>Primary Sources Access (Plan D) - International</collection><collection>Primary Sources Access & Build (Plan A) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Midwest</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Northeast</collection><collection>Primary Sources Access (Plan D) - Southeast</collection><collection>Primary Sources Access (Plan D) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Southeast</collection><collection>Primary Sources Access (Plan D) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - UK / I</collection><collection>Primary Sources Access (Plan D) - Canada</collection><collection>Primary Sources Access (Plan D) - EMEALA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - International</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - International</collection><collection>Primary Sources Access (Plan D) - West</collection><collection>Periodicals Index Online Segments 1-50</collection><collection>Primary Sources Access (Plan D) - APAC</collection><collection>Primary Sources Access (Plan D) - Midwest</collection><collection>Primary Sources Access (Plan D) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Canada</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - EMEALA</collection><collection>Primary Sources Access & Build (Plan A) - APAC</collection><collection>Primary Sources Access & Build (Plan A) - Canada</collection><collection>Primary Sources Access & Build (Plan A) - West</collection><collection>Primary Sources Access & Build (Plan A) - EMEALA</collection><collection>Primary Sources Access (Plan D) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - Midwest</collection><collection>Primary Sources Access & Build (Plan A) - North Central</collection><collection>Primary Sources Access & Build (Plan A) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - Southeast</collection><collection>Primary Sources Access (Plan D) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - APAC</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - MEA</collection><jtitle>Journal of the American Ceramic Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>IWAI, SHIN-ICHI</au><au>WATANABE, TAKASHI</au><au>MINATO, ICHIRO</au><au>OKADA, KIYOSHI</au><au>MORIKAWA, HIDEKI</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Decomposition of Mullite by Silica Volatilization</atitle><jtitle>Journal of the American Ceramic Society</jtitle><date>1980-01</date><risdate>1980</risdate><volume>63</volume><issue>1-2</issue><spage>44</spage><epage>46</epage><pages>44-46</pages><issn>0002-7820</issn><eissn>1551-2916</eissn><abstract>Thermal decomposition of mullite into corundum was investigated using a high‐temperature X‐ray single‐crystal camera equipped with a gas‐flame furnace and by scanning electron microscopy and electron probe microanalysis (EPMA). When heated to ∼1750°C, mullite decomposed to corundum by the liberation of the SiO2 component with topotaxial relations of:
1
(310)mull∥(001)cor; [001]mull∥[110]cor
2
(130)mull∥(001)cor; [001]mull∥[110]cor
3
(110)mull∥(001)cor; [001]mull∥[110]cor
Thus, it was considered that, when mullite decomposed into corundum, their oxygen close‐packed planes were almost preserved. The SEM photographs showed that the crystals of the developed corundum are prismatic and ∼5 μm wide. The EPMA showed that the phase boundary between mullite and developed corundum is discontinuous.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1151-2916.1980.tb10647.x</doi><tpages>3</tpages></addata></record> |
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title | Decomposition of Mullite by Silica Volatilization |
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