{"created":"2023-05-15T12:20:39.187633+00:00","id":11294,"links":{},"metadata":{"_buckets":{"deposit":"4435a760-5d6e-4bc5-b556-426e2adee0e4"},"_deposit":{"created_by":1,"id":"11294","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"11294"},"status":"published"},"_oai":{"id":"oai:kansai-u.repo.nii.ac.jp:00011294","sets":["528:1588:1592:1594"]},"author_link":["34799","25275","25276","25278","25279"],"control_number":"11294","item_9_alternative_title_20":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Relationship between Apparent Electric Resistivity and Rain Fall in Fracture Zone of Rock Slope by Continious Measurment","subitem_alternative_title_language":"en"}]},"item_9_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-06-10","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"82","bibliographicPageStart":"74","bibliographicVolumeNumber":"38","bibliographic_titles":[{"bibliographic_title":"応用地質"}]}]},"item_9_description_4":{"attribute_name":"概要","attribute_value_mlt":[{"subitem_description":"岩盤斜面内の地下水は,主に亀裂,断層や不連続面内を流れることはよく知られている。本論文では,ダイポール・ダイポール電気探査法を用いて,5つの降雨パターンで,ある岩盤斜面で連続的に見かけ比抵抗を測定した。そのときの側線は,1つの破砕帯を横切って設けている。そして,比抵抗の変化と降雨との関係について考察した。その結果,破砕帝部分とほかの岩盤内とでは,比抵抗の変化特性は全く異なっており,とくに,比抵抗の変化と降雨とは1つの指数関数に近似できることが認められた。そして,この指数関数の係数を用いて,降雨浸透に伴う岩盤斜面の状態変化のモニタリングが可能であることを示した。\n\\nIt is well known that the groundwater in rock slope mainly flow joint, fracture zone, fault and discontinuity plane. In this paper, using Dipole-Dipole electric resistivity method, the electric resistivities are continuously measured in a rock slope during five rain fall patterns with the measuring line crossing a fracture zone, and the relationship between the change of apparent electric resistivity and the rain fall are discussed. As the results, making a comparison between fracture zones and the other rock mass, the characteristics of the change of apparent electric resistivity is quite diffferent, and especially, it is recognized that the relationship between the change of apparent electric resistivity and rain fall can be approximated with an exponential function.","subitem_description_type":"Other"}]},"item_9_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"25278","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakamura, Makoto"}]},{"nameIdentifiers":[{"nameIdentifier":"25279","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nishida, Kazuhiko"}]}]},"item_9_publisher_34":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本応用地質学会"}]},"item_9_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"02867737","subitem_source_identifier_type":"PISSN"}]},"item_9_version_type_17":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"楠見, 晴重","creatorNameLang":"ja"},{"creatorName":"Kusumi, Harushige","creatorNameLang":"en"}],"familyNames":[{"familyName":"楠見","familyNameLang":"ja"},{"familyName":"Kusumi","familyNameLang":"en"}],"givenNames":[{"givenName":"晴重","givenNameLang":"ja"},{"givenName":"Harushige","givenNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"34799","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"70158880","nameIdentifierScheme":"e-Rad","nameIdentifierURI":"https://nrid.nii.ac.jp/ja/nrid/1000070158880"}]},{"creatorNames":[{"creatorName":"中村, 真","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"25275","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"西田, 一彦","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"25276","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"20067581","nameIdentifierScheme":"e-Rad","nameIdentifierURI":"https://nrid.nii.ac.jp/ja/nrid/1000020067581"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2019-05-23"}],"displaytype":"detail","filename":"KU-1100OB-19970610-00.pdf","filesize":[{"value":"1.2 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KU-1100OB-19970610-00.pdf","url":"https://kansai-u.repo.nii.ac.jp/record/11294/files/KU-1100OB-19970610-00.pdf"},"version_id":"327f26db-4e19-40fb-aec9-6742a3cc09c3"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"岩盤斜面","subitem_subject_scheme":"Other"},{"subitem_subject":"rock slope","subitem_subject_scheme":"Other"},{"subitem_subject":"破砕帯部","subitem_subject_scheme":"Other"},{"subitem_subject":"fracture zone","subitem_subject_scheme":"Other"},{"subitem_subject":"見かけ比抵抗","subitem_subject_scheme":"Other"},{"subitem_subject":"apparent electric resistivity","subitem_subject_scheme":"Other"},{"subitem_subject":"連続計測","subitem_subject_scheme":"Other"},{"subitem_subject":"continious measurment","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"連続計測による岩盤斜面の破砕帯部における見かけ比抵抗と降雨との関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"連続計測による岩盤斜面の破砕帯部における見かけ比抵抗と降雨との関係","subitem_title_language":"ja"}]},"item_type_id":"9","owner":"1","path":["1594"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2010-07-14"},"publish_date":"2010-07-14","publish_status":"0","recid":"11294","relation_version_is_last":true,"title":["連続計測による岩盤斜面の破砕帯部における見かけ比抵抗と降雨との関係"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2024-01-15T05:01:18.071881+00:00"}