WEKO3
インデックスリンク
アイテム
モンモリロナイト系粘上の物理化学的および工学的特性に及ぼすカリウム固定の影響
https://fukuyama-u.repo.nii.ac.jp/records/7598
https://fukuyama-u.repo.nii.ac.jp/records/759899297282-404b-4832-acc7-802a427a7c33
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(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1979-01-01 | |||||
タイトル | ||||||
タイトル | モンモリロナイト系粘上の物理化学的および工学的特性に及ぼすカリウム固定の影響 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | The Effect of Potassium Fixation on Physico-Chemical and Engineering Properties of Montmorillonite | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(日) | ||||||
値 | 論文 | |||||
著者名(日) |
富田, 武満
× 富田, 武満 |
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著者名よみ | ||||||
識別子Scheme | WEKO | |||||
識別子 | 41279 | |||||
姓名 | トミタ, タケミツ | |||||
著者名(英) | ||||||
識別子Scheme | WEKO | |||||
識別子 | 41280 | |||||
姓名 | Tomita, Takemitsu | |||||
言語 | en | |||||
著者所属(日) | ||||||
値 | 福山大学工学部土木工学科 | |||||
著者所属(英) | ||||||
言語 | en | |||||
値 | Faculty of Engineering, Fukuyama University | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Cation-fixation in soil occurs when exchangeable or watersoluble cation in soil are converted into the form that cannot be readily extracted with a solution of neutral salt. That is, exchangeable ions are changed to the .nonreplaciable state. Potassium ions are known to be the primary one involved in such a reaction. In the field of pedology, the study of K-fixation has been performed actively, but from the viewpoint of soil mechanics, especially soil stabilization, it has been hardly done. The present study was undertaken to clarify the physico-chemical change of clay minerals and the change of the engineering properties due to K-fixation. From the results of X-ray diffraction and differential analysis, it was found that K-fixed soil has the structure similar to illitic clay. The engineering properties of montmorillonite is also stabilized. It is considered that this stabilization is due to the formation of aggregate of clay caused by the de crease in potential energy between clay particles and by the fixation of K ions between the internal layers of clay. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00217655 | |||||
書誌情報 |
福山大学工学部紀要 巻 1, p. 61-70, 発行日 1979 |