{"created":"2021-03-01T06:50:41.122406+00:00","id":32055,"links":{},"metadata":{"_buckets":{"deposit":"a8686d2b-92d8-4edb-a6e9-aa10c8054948"},"_deposit":{"id":"32055","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32055"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032055","sets":["80:4411:4415","9:504:4413:4416"]},"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Temperature Distribution in a Vault for Crustal Movement Observation"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1974-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"42","bibliographicPageStart":"33","bibliographicVolumeNumber":"13","bibliographic_titles":[{"bibliographic_title":"地震研究所研究速報"}]}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Temperature measurement in a vault is a standard job at a crustal movement observatory. A precise mercury thermometer (0.1°C/div.) has been used conventjonally for this purpose. Recent progress in an observational system has needed more precjse knowledge about the temperature changes in a vault for satisfactory correction of the data. Basically, a vault is subject to temperature changes by two principal causes, heat conduction from the surface and the air flow through the entrance. In the first case, the underground temperature is a function of the depth from the ground surface. In a vault which is excavated in a mountain slope, therefore, the temperature is not uniform to all its extension, being subject to relatively large seasonal changes in a shallower part. The second type disturbance will affect the vault in a more complicated way.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"71119","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Yamada, Juhei"}]},{"nameIdentifiers":[{"nameIdentifier":"71120","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Yanagisawa, Michio"}]},{"nameIdentifiers":[{"nameIdentifier":"71121","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Shimazu, Takashi"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00032046","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10165194","subitem_source_identifier_type":"NCID"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"051.1","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"山田, 重平"}],"nameIdentifiers":[{"nameIdentifier":"71116","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"柳沢, 道夫"}],"nameIdentifiers":[{"nameIdentifier":"71117","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"島津, 孝"}],"nameIdentifiers":[{"nameIdentifier":"71118","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-12"}],"displaytype":"detail","filename":"jis0130004.pdf","filesize":[{"value":"516.9 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jis0130004.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32055/files/jis0130004.pdf"},"version_id":"4c1ed658-782e-401c-a29b-8de61f752701"}]},"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":"地殻変動観測坑の温度分布","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"地殻変動観測坑の温度分布"}]},"item_type_id":"4","owner":"1","path":["4415","4416"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-12-22"},"publish_date":"2010-12-22","publish_status":"0","recid":"32055","relation_version_is_last":true,"title":["地殻変動観測坑の温度分布"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:08:23.716315+00:00"}