{"created":"2023-07-25T08:08:23.124864+00:00","id":7757,"links":{},"metadata":{"_buckets":{"deposit":"b8857027-d4a2-4462-bd33-b0102fb3ae84"},"_deposit":{"created_by":18,"id":"7757","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"7757"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00007757","sets":["228:273:5339","35:36"]},"author_link":[],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1977-11","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"60","bibliographicPageStart":"43","bibliographicVolumeNumber":"19","bibliographic_titles":[{"bibliographic_title":"鹿児島大学工学部研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"The research reports of the Faculty of Engineering, Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1977-11","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"In the latter half of the 3rd period, which the author feels inclined to characterize as a\noverblown time, studies and reports much increased in several branches, geology, disaster science,\ncivil engineering, soil mechanics and so on. Investigation efforts increased and experiments\nwere repeated, and analysis became minute and acute.　At the same time, in some cases,\ncomplicated and rather unpractical logics appeared in their opinions. Conception high, meaning\nobscure.\nIn the geological field flow and emplacement mechanism of Ito pyroclastic flow of Aira caldera\nis reported and concerning the different pyroclastic flows in the Kokubu area and the neighbouring\nzone, some other members as S. Aramaki, R. Ota, and T. Tsuyuki publish their opinions.\nTuffaceous and pumiceous sediments in Kakuto Basin were also investigated by some persons.\nHere they suffered from considerably big earthquake disasters of seismic intensity 5-6 in Feb.\n1968. Many investigation data were obtained through these events. Formerly we had scarcely\nthe data of Shirasu behaviour in seismic shock.　These data well revealed a few secrets of\nShirasu nature.\nThe earthquake damages were found of various types as mountainside slip, crack and settlement\nof river banks, sand boiling, and destruction of structures &c. The auther picked up\nmainly Shirasu damage reports concerned. Shirasu in this environs is not original but there\nare Shirasu like sediments of tuffaceous materials and of Ito pumice flow poured into the past\nlake. They are weeker than usual Shirasu and this is the most reason that the damages,\nespecially that of the mountainside were comparativly large for the seismic intensity. Cut\ncliffs were safer to the mountainside.\nAs for the engineering department, studies on fill-up ground and reclamation works will\nbecome important, for seismic shock influece to disturbed Shirasu material is not made clear\nyet.\nThe auther's rough introduction to the reports of Shirasu studies has now come to an end.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_relation_32":{"attribute_name":"関連（relation）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/12722","subitem_relation_type_select":"HDL"}}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0451212X","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00040363","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"511","subitem_subject_scheme":"NDC"}]},"item_7_text_44":{"attribute_name":"備考","attribute_value_mlt":[{"subitem_text_value":"追補・正誤あり: http://hdl.handle.net/10232/12722"}]},"item_7_version_type_14":{"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":"上田, 通夫","creatorNameLang":"ja"},{"creatorName":"UEDA, Michio","creatorNameLang":"en"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-28"}],"displaytype":"detail","filename":"AN00040363_v19_p43-60.pdf","filesize":[{"value":"40.0 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"AN00040363_v19_p43-60.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/7757/files/AN00040363_v19_p43-60.pdf"},"version_id":"5bf93596-8119-4751-b94d-e769ccb5f638"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"シラスの土質力学的特性とその原因 : シラス防災の研究　第一部　その5","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"シラスの土質力学的特性とその原因 : シラス防災の研究　第一部　その5","subitem_title_language":"ja"},{"subitem_title":"MECHANICAL PROPERTIES OF　\"SHIRASU\" AND THE CAUSES : Research on \"SHIRASU\" Disaster Prevention Part I No. 5","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["36","5339"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-06-17"},"publish_date":"2015-06-17","publish_status":"0","recid":"7757","relation_version_is_last":true,"title":["シラスの土質力学的特性とその原因 : シラス防災の研究　第一部　その5"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-02-20T04:59:37.059696+00:00"}