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GROWING OF MULLITE FROM CALCINATION OF CLAY", "subitem_title_language": "en"}]}, "item_type_id": "7", "owner": "3", "path": ["36", "5298"], "permalink_uri": "http://hdl.handle.net/10232/10740", "pubdate": {"attribute_name": "公開日", "attribute_value": "2011-03-18"}, "publish_date": "2011-03-18", "publish_status": "0", "recid": "2126", "relation": {}, "relation_version_is_last": true, "title": ["南九州産白色粘土の研究 : 第12報 粘土の加熱によるムライト生成"], "weko_shared_id": 3}
南九州産白色粘土の研究 : 第12報 粘土の加熱によるムライト生成
http://hdl.handle.net/10232/10740
http://hdl.handle.net/10232/10740918f40d6-570c-4ffd-b2ad-6fd0663044bc
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2011-03-18 | |||||
タイトル | ||||||
タイトル | 南九州産白色粘土の研究 : 第12報 粘土の加熱によるムライト生成 | |||||
タイトル | ||||||
タイトル言語 | en | |||||
タイトル | STUDIES OF THE WHITE CLAY IN THE SOUTH KYUSHU : REPORT 12. GROWING OF MULLITE FROM CALCINATION OF CLAY | |||||
タイトルよみ | ||||||
タイトルよみ | ミナミキュウシュウサン ハクショク ネンド ノ ケンキュウ : ダイ12ホウ ネンド ノ カネツ ニヨル ムライト セイセイ | |||||
著者 |
小牧, 高志
× 小牧, 高志 |
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著者よみ | ||||||
姓名 | コマキ, タカシ | |||||
別言語の著者 | ||||||
姓名 | KOMAKI, Takashi | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
要約(Abstract) | ||||||
内容記述タイプ | Other | |||||
内容記述 | GROWING OF MULLITE FROM CALCINATION OF CLAY. Clay mineral becomes Mullite when calcinated, but this formation varies which the kinds of clay. The author studied on the formation of mullite by calcinating white clay in the South Kyushu, Ibusuki clay and Aira Fukugano clay as kaolinite, Okuchi clay and Iriki clay as hydrohalloysite, Yoshinoyama clay as montmorillonite, each up to 1000°C, 1200°C and 1500°C. there were not apper the peak of mullite by X-ray diffration in calcinate clay at 1000°C, but the peak of cristobalite is observed in Iriki clay and Yoshinoyama clay. Calcinating kaolinite and hydrohalloysite at l200°C, observed much mullite, but in montmorillonite observed cristobalite instead of mullite. at 1500°C, except montmorillonite, much more mullite was observed and in case of Okuchi cristobalite is developed, too. In Okuchi clay 80% of the clay became mullite in Ibusuki clay 67% and in Yoshinoyama clay only 13%. |
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収録雑誌名 |
鹿児島大学工学部研究報告 巻 3, p. 49-59 |
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作成日 | ||||||
日付 | 1963-10-20 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
ISSN | 0451212X | |||||
NII書誌ID(雑誌) | ||||||
収録物識別子タイプ | NCID | |||||
NC ID | AN00040363 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
NDC | ||||||
主題Scheme | NDC | |||||
主題 | 458 | |||||
公開者・出版者 | ||||||
出版者 | 鹿児島大学 | |||||
公開者よみ | ||||||
公開者よみ | カゴシマ ダイガク | |||||
公開者別名 | ||||||
公開者別名 | Kagoshima University |