{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362825895375657216.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1151-2916.1961.tb15355.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1151-2916.1961.tb15355.x"}},{"identifier":{"@type":"URI","@value":"https://ceramics.onlinelibrary.wiley.com/doi/pdf/10.1111/j.1151-2916.1961.tb15355.x"}},{"identifier":{"@type":"NAID","@value":"30015554981"}}],"dc:title":[{"@value":"Conversion of Quartz to Tridymite"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n                    The conditions under which tridymite becomes a stable phase have been reinvestigated. When quartz was heated with 2% alkali oxide, tridymite formed directly at 872° to 898°C. with Na\n                    <jats:sub>2</jats:sub>\n                    O, at 883° to 902°C. with K\n                    <jats:sub>2</jats:sub>\n                    O, and above 1005°C. with Li\n                    <jats:sub>2</jats:sub>\n                    O. Cristobalite occurred as an intermediate phase above 893°C. with Li\n                    <jats:sub>2</jats:sub>\n                    O, above 898°C. with Na\n                    <jats:sub>2</jats:sub>\n                    O, and above 902°C. with K\n                    <jats:sub>2</jats:sub>\n                    O. When quartz plus sodium chloride was heated in vacuum, tridymite did not form but cristobalite started to appear at 1050°C. The results showed that the formation of tridymite can be strictly a solid‐state process. New schematic tentative diagrams for the high‐silica region of binary systems are suggested. Quartz and cristobalite are regarded as the only stable crystalline phases of pure silica. Tridymite is pictured as a binary incongruently melting phase.\n                  </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1582543023916281216","@type":"Researcher","foaf:name":[{"@value":"S. B. HOLMQUIST"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00027820"},{"@type":"EISSN","@value":"15512916"}],"prism:publicationName":[{"@value":"Journal of the American Ceramic Society"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1961-02","prism:volume":"44","prism:number":"2","prism:startingPage":"82","prism:endingPage":"86"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1151-2916.1961.tb15355.x"},{"@id":"https://ceramics.onlinelibrary.wiley.com/doi/pdf/10.1111/j.1151-2916.1961.tb15355.x"}],"createdAt":"2006-06-07","modifiedAt":"2025-11-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004233964326912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First evidence for silica condensation within the solar protoplanetary disk"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025430626339072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental evidence of phase transition of silica polymorphs in basaltic eucrites: implications for thermal history of protoplanetary crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680129472640","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ファイヤライト (Fe<SUB>2</SUB>SiO<SUB>4</SUB>) の生成と還元反応について"},{"@language":"en","@value":"A Study on the Formation and Reduction of Fayalite (Fe<SUB>2</SUB>SiO<SUB>4</SUB>)"},{"@value":"ファイヤライト(Fe2SiO4)の生成と還元反応について"},{"@language":"ja-Kana","@value":"ファイヤライト Fe2SiO4 ノ セイセイ ト カンゲン ハンノウ ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135650127368960","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of Mineralizers on the Phase Transitions and Sintering Behavior of Silica Bricks"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1151-2916.1961.tb15355.x"},{"@type":"CIA","@value":"30015554981"},{"@type":"CROSSREF","@value":"10.1073/pnas.1722265115_references_DOI_SgCodoe2ahQpO9ta6CBROqDTDJ8"},{"@type":"CROSSREF","@value":"10.1038/s41598-024-77544-x_references_DOI_SgCodoe2ahQpO9ta6CBROqDTDJ8"},{"@type":"CROSSREF","@value":"10.2355/tetsutohagane1955.54.12_1203_references_DOI_SgCodoe2ahQpO9ta6CBROqDTDJ8"}]}