Studies of the fusibility of coal ash
To establish a means for predicting the melting temperature of coal ash, the chemical composition, mineral matter content and melting temperature were investigated for 24 coal ash samples. The fusibility of coal ash was studied from the view point of the mineral matter. The melting temperatures of t...
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Veröffentlicht in: | Fuel (Guildford) 1986-11, Vol.65 (11), p.1505-1510 |
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creator | Unuma, Hidero Takeda, Shohei Tsurue, Takashi Ito, Saburo Sayama, Sogo |
description | To establish a means for predicting the melting temperature of coal ash, the chemical composition, mineral matter content and melting temperature were investigated for 24 coal ash samples. The fusibility of coal ash was studied from the view point of the mineral matter. The melting temperatures of these samples ranged from 1285
to > 1500 °
C. A conventional acid-base index did not show a good correlation with melting temperature for these coal ash samples (correlation coefficient = −0.67) and the reason for this is discussed. An empirical index, which is derived from the correlation between mineral composition and melting temperature, is proposed. It was linearly proportional to melting temperature for the coal ash samples (correlation coefficient = 0.85) and furthermore, the applicability of the index to abitrary coal ash was demonstrated. |
doi_str_mv | 10.1016/0016-2361(86)90325-X |
format | Article |
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to > 1500 °
C. A conventional acid-base index did not show a good correlation with melting temperature for these coal ash samples (correlation coefficient = −0.67) and the reason for this is discussed. An empirical index, which is derived from the correlation between mineral composition and melting temperature, is proposed. It was linearly proportional to melting temperature for the coal ash samples (correlation coefficient = 0.85) and furthermore, the applicability of the index to abitrary coal ash was demonstrated.</description><identifier>ISSN: 0016-2361</identifier><identifier>EISSN: 1873-7153</identifier><identifier>DOI: 10.1016/0016-2361(86)90325-X</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Applied sciences ; Coal and derived products ; coal ash ; Energy ; Exact sciences and technology ; Fuels ; fusibility ; mineral matter ; Structure, chemical and physical properties</subject><ispartof>Fuel (Guildford), 1986-11, Vol.65 (11), p.1505-1510</ispartof><rights>1986</rights><rights>1987 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c364t-131da2a0909b90f8ad02bb87b8be2dfd86b84be9a467273fc6da117b888348e53</citedby><cites>FETCH-LOGICAL-c364t-131da2a0909b90f8ad02bb87b8be2dfd86b84be9a467273fc6da117b888348e53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/0016-2361(86)90325-X$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3549,27923,27924,45994</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=8253322$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Unuma, Hidero</creatorcontrib><creatorcontrib>Takeda, Shohei</creatorcontrib><creatorcontrib>Tsurue, Takashi</creatorcontrib><creatorcontrib>Ito, Saburo</creatorcontrib><creatorcontrib>Sayama, Sogo</creatorcontrib><title>Studies of the fusibility of coal ash</title><title>Fuel (Guildford)</title><description>To establish a means for predicting the melting temperature of coal ash, the chemical composition, mineral matter content and melting temperature were investigated for 24 coal ash samples. The fusibility of coal ash was studied from the view point of the mineral matter. The melting temperatures of these samples ranged from 1285
to > 1500 °
C. A conventional acid-base index did not show a good correlation with melting temperature for these coal ash samples (correlation coefficient = −0.67) and the reason for this is discussed. An empirical index, which is derived from the correlation between mineral composition and melting temperature, is proposed. It was linearly proportional to melting temperature for the coal ash samples (correlation coefficient = 0.85) and furthermore, the applicability of the index to abitrary coal ash was demonstrated.</description><subject>Applied sciences</subject><subject>Coal and derived products</subject><subject>coal ash</subject><subject>Energy</subject><subject>Exact sciences and technology</subject><subject>Fuels</subject><subject>fusibility</subject><subject>mineral matter</subject><subject>Structure, chemical and physical properties</subject><issn>0016-2361</issn><issn>1873-7153</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1986</creationdate><recordtype>article</recordtype><recordid>eNp9kE1Lw0AQhhdRMFb_gYccVPQQ3a9sNhdBil9Q8KBCb8t-zNKVtKm7idB_b2JLj15mYOZ5Z3hfhM4JviWYiDs8lIIyQa6luKkxo2UxP0AZkRUrKlKyQ5TtkWN0ktIXxriSJc_Q5XvXuwApb33eLSD3fQomNKHbjBPb6ibXaXGKjrxuEpzt-gR9Pj1-TF-K2dvz6_RhVlgmeFcQRpymGte4NjX2UjtMjZGVkQao804KI7mBWnNR0Yp5K5wmZFhLybiEkk3Q1fbuOrbfPaROLUOy0DR6BW2fFOW04iUeQb4FbWxTiuDVOoaljhtFsBozUaNhNRpWUqi_TNR8kF3s7utkdeOjXtmQ9lpJS8YoHbD7LQaD158AUSUbYGXBhQi2U64N___5BT39c3k</recordid><startdate>19861101</startdate><enddate>19861101</enddate><creator>Unuma, Hidero</creator><creator>Takeda, Shohei</creator><creator>Tsurue, Takashi</creator><creator>Ito, Saburo</creator><creator>Sayama, Sogo</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>F28</scope><scope>FR3</scope></search><sort><creationdate>19861101</creationdate><title>Studies of the fusibility of coal ash</title><author>Unuma, Hidero ; Takeda, Shohei ; Tsurue, Takashi ; Ito, Saburo ; Sayama, Sogo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c364t-131da2a0909b90f8ad02bb87b8be2dfd86b84be9a467273fc6da117b888348e53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1986</creationdate><topic>Applied sciences</topic><topic>Coal and derived products</topic><topic>coal ash</topic><topic>Energy</topic><topic>Exact sciences and technology</topic><topic>Fuels</topic><topic>fusibility</topic><topic>mineral matter</topic><topic>Structure, chemical and physical properties</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Unuma, Hidero</creatorcontrib><creatorcontrib>Takeda, Shohei</creatorcontrib><creatorcontrib>Tsurue, Takashi</creatorcontrib><creatorcontrib>Ito, Saburo</creatorcontrib><creatorcontrib>Sayama, Sogo</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>ANTE: Abstracts in New Technology & Engineering</collection><collection>Engineering Research Database</collection><jtitle>Fuel (Guildford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Unuma, Hidero</au><au>Takeda, Shohei</au><au>Tsurue, Takashi</au><au>Ito, Saburo</au><au>Sayama, Sogo</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Studies of the fusibility of coal ash</atitle><jtitle>Fuel (Guildford)</jtitle><date>1986-11-01</date><risdate>1986</risdate><volume>65</volume><issue>11</issue><spage>1505</spage><epage>1510</epage><pages>1505-1510</pages><issn>0016-2361</issn><eissn>1873-7153</eissn><abstract>To establish a means for predicting the melting temperature of coal ash, the chemical composition, mineral matter content and melting temperature were investigated for 24 coal ash samples. The fusibility of coal ash was studied from the view point of the mineral matter. The melting temperatures of these samples ranged from 1285
to > 1500 °
C. A conventional acid-base index did not show a good correlation with melting temperature for these coal ash samples (correlation coefficient = −0.67) and the reason for this is discussed. An empirical index, which is derived from the correlation between mineral composition and melting temperature, is proposed. It was linearly proportional to melting temperature for the coal ash samples (correlation coefficient = 0.85) and furthermore, the applicability of the index to abitrary coal ash was demonstrated.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/0016-2361(86)90325-X</doi><tpages>6</tpages></addata></record> |
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source | ScienceDirect Journals (5 years ago - present) |
subjects | Applied sciences Coal and derived products coal ash Energy Exact sciences and technology Fuels fusibility mineral matter Structure, chemical and physical properties |
title | Studies of the fusibility of coal ash |
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