{"@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/1362825894769181952.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1346/ccmn.1978.0260503"}},{"identifier":{"@type":"URI","@value":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0009860400004110"}},{"identifier":{"@type":"NAID","@value":"30003541038"}}],"dc:title":[{"@value":"Reaction Series for Dioctahedral Smectites"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Several dioctahedral clay minerals are related through reaction series. These series can be produced hydro-thermally from beidellite gel and montmorillonite by making simple changes in interlayer and solution chemistry. The series are:\n<jats:list list-type=\"simple\"><jats:list-item><jats:p>gel-K-beidellite-random illite/smectite-K-rectorite-illite</jats:p></jats:list-item><jats:list-item><jats:p>K-montmorillonite-K-rectorite-illite</jats:p></jats:list-item><jats:list-item><jats:p>Na-montmorillonite or beidellite-Na-rectorite-paragonite</jats:p></jats:list-item><jats:list-item><jats:p>Li-montmorillonite-Li-tosudite-Li-rectorite-cookeite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Mg-montmorillonite-Mg-rectorite-tosudite-sudoite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Ca-montmorillonite-Ca-rectorite-margarite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Al-Ca-montmorillonite-kaolinite/smectite-kaolinite (150°C)</jats:p></jats:list-item><jats:list-item><jats:p>Al-Ca-montmorillonite-pyrophyllite/smectite-pyrophyllite (320°C).</jats:p></jats:list-item></jats:list></jats:p><jats:p>Assuming stability for the mixed-layer phases, paragenesis is a function of P, T, and X conditions. If the phases are considered to be metastable, paragenesis is a function of the speed and path of reaction.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825894769181952","@type":"Researcher","foaf:name":[{"@value":"Dennis Eberl"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00098604"},{"@type":"EISSN","@value":"15528367"}],"prism:publicationName":[{"@value":"Clays and Clay Minerals"}],"dc:publisher":[{"@value":"Cambridge University Press (CUP)"}],"prism:publicationDate":"1978-10","prism:volume":"26","prism:number":"5","prism:startingPage":"327","prism:endingPage":"340"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"url":[{"@id":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0009860400004110"}],"createdAt":"2006-08-25","modifiedAt":"2025-08-04","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050568617200406400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Anatomy of active volcanic edifice at the Kusatsu–Shirane volcano, Japan, by magnetotellurics: hydrothermal implications for volcanic unrests"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854372807424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oscillation frequencies of long-period seismic events at Kusatsu–Shirane volcano, Japan, related to the volume of water vapour in a hydrothermal crack"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206544994176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrothermal synthesis of beidellite from aluminosilicate glass by varying water/solid ratio"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572358420854144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"高塩濃度,高アルカリ環境における粘土鉱物の生成と変化--放射性廃棄物地層処分環境におけるベントナイト緩衝材の変質に関連して"},{"@language":"ja-Kana","@value":"コウエン ノウド コウアルカリ カンキョウ ニ オケル ネンド コウブツ ノ セイセイ ト ヘンカ ホウシャセイ ハイキブツ チソウ ショブン カンキョウ ニ オケル ベントナイト カンショウザイ ノ ヘンシツ ニ カンレン シテ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1346/ccmn.1978.0260503"},{"@type":"CIA","@value":"30003541038"},{"@type":"CROSSREF","@value":"10.2465/minerj.15.300_references_DOI_W6s3bgxMoam9XQpQbKHh2CJtUQb"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01283-2_references_DOI_W6s3bgxMoam9XQpQbKHh2CJtUQb"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaf006_references_DOI_W6s3bgxMoam9XQpQbKHh2CJtUQb"}]}