このアイテムのアクセス数: 243

このアイテムのファイル:
ファイル 記述 サイズフォーマット 
s11440-020-00939-3.pdf2.88 MBAdobe PDF見る/開く
完全メタデータレコード
DCフィールド言語
dc.contributor.authorKido, Ryunosukeen
dc.contributor.authorHigo, Yosukeen
dc.contributor.authorTakamura, Fukushien
dc.contributor.authorMorishita, Ryoichien
dc.contributor.authorKhaddour, Ghonwaen
dc.contributor.authorSalager, Simonen
dc.contributor.alternative木戸, 隆之祐ja
dc.contributor.alternative肥後, 陽介ja
dc.contributor.alternative高村, 福志ja
dc.date.accessioned2020-02-25T03:44:18Z-
dc.date.available2020-02-25T03:44:18Z-
dc.date.issued2020-07-
dc.identifier.issn1861-1125-
dc.identifier.issn1861-1133-
dc.identifier.urihttp://hdl.handle.net/2433/245800-
dc.description.abstractWater retention characteristics are important for modeling the mechanical and hydraulic behavior of partially saturated sand. It is well known that the soil water characteristic curve shows hysteresis during drying and wetting processes. For a better understanding of the water retention characteristics of partially saturated soil, a microscopic investigation of the morphological transitions for the pore water phase and the pore air phase, such as volume distribution, spatial distribution and continuity during drying and wetting processes, is crucial. In the present study, different water retention states of a partially saturated sand were visualized during water retention tests using microfocus X-ray computed tomography (CT). The CT images obtained from the tests were segmented into the soil particle phase, the pore water phase and the pore air phase. Then, a series of image processing, erosion, dilation and cluster labeling was applied to the images in this order to quantify the cluster volume distributions, the number of clusters and the continuity of both the pore water phase and the pore air phase. The morphological transitions for the pore air phase and the pore water phase, subjected to decreasing and increasing degrees of saturation, were revealed using the results of the image processing, and then, the water retention states were characterized based on the morphologies for the two phases. The influence of the morphologies on the hysteresis was discussed.en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherSpringer Natureen
dc.rightsThis is a post-peer-review, pre-copyedit version of an article published in 'Acta Geotechnica'. The final authenticated version is available online at: https://doi.org/10.1007/s11440-020-00939-3en
dc.rightsThe full-text file will be made open to the public on 19 February 2021 in accordance with publisher's 'Terms and Conditions for Self-Archiving'.en
dc.rightsThis is not the published version. Please cite only the published version.en
dc.rightsこの論文は出版社版でありません。引用の際には出版社版をご確認ご利用ください。ja
dc.subjectImage processingen
dc.subjectMicrofocus X-ray CTen
dc.subjectMorphologyen
dc.subjectPartially saturated sanden
dc.subjectWater retention stateen
dc.subjectWater retention testen
dc.titleMorphological transitions for pore water and pore air during drying and wetting processes in partially saturated sanden
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.jtitleActa Geotechnicaen
dc.identifier.volume15-
dc.identifier.issue7-
dc.identifier.spage1745-
dc.identifier.epage1761-
dc.relation.doi10.1007/s11440-020-00939-3-
dc.textversionauthor-
dc.addressDepartment of Civil and Earth Resources Engineering, Kyoto Universityen
dc.addressDepartment of Urban Management, Kyoto Universityen
dc.addressDepartment of Urban Management, Kyoto Universityen
dc.addressJapan Oil, Gas and Metals National Corporationen
dc.addressCNRS, Grenoble-INP, 3SR, Université Grenoble Alpesen
dc.addressCNRS, Grenoble-INP, 3SR, Université Grenoble Alpesen
dcterms.accessRightsopen access-
datacite.date.available2021-02-19-
datacite.awardNumber17J06250-
dc.identifier.pissn1861-1125-
dc.identifier.eissn1861-1133-
jpcoar.funderName日本学術振興会ja
jpcoar.funderName.alternativeJapan Society for the Promotion of Science (JSPS)en
出現コレクション:学術雑誌掲載論文等

アイテムの簡略レコードを表示する

Export to RefWorks


出力フォーマット 


このリポジトリに保管されているアイテムはすべて著作権により保護されています。