{"created":"2022-01-27T08:17:31.056124+00:00","id":2004843,"links":{},"metadata":{"_buckets":{"deposit":"b3e2d1bf-746b-41e3-8702-2a7da3d5326e"},"_deposit":{"id":"2004843","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"2004843"},"status":"published"},"_oai":{"id":"oai:u-ryukyu.repo.nii.ac.jp:02004843","sets":["1642837622505:1642837957109:1642837963990","1642838403551:1642838406414"]},"author_link":[],"item_1617186331708":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_1551255647225":"\u7af9\u5bcc\u5cf6\u6d77\u5e95\u6e29\u6cc9\u306e\u8caf\u7559\u5c64\u306b\u3064\u3044\u3066\u306e\u4e00\u8003\u5bdf","subitem_1551255648112":"ja"},{"subitem_1551255647225":"Geothermal reservoir of the Taketomi-jima submarine hot spring in Okinawa, Japan","subitem_1551255648112":"en"}]},"item_1617186419668":{"attribute_name":"Creator","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"\u6728\u6751, \u653f\u662d","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"\u6797, \u6b63\u96c4","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"\u5927\u68ee, \u4fdd","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"Kimura, Masaaki","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hayashi, Masao","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Oomori, Tamotsu","creatorNameLang":"en"}]}]},"item_1617186476635":{"attribute_name":"Access Rights","attribute_value_mlt":[{"subitem_1522299639480":"open access","subitem_1600958577026":"http://purl.org/coar/access_right/c_abf2"}]},"item_1617186626617":{"attribute_name":"Description","attribute_value_mlt":[{"subitem_description":"A geochemical study on hot spring gush out of the sea bottom of 22 meters deep off Taketomi-jima reveals that the spring water at well mouth is 17.8-18.1 % of chlorinity and 37.5\u2103 in temperature which is considerably higher than the temperature of the water column in the vicinity (about 25\u2103). Based upon the result of the simple mixing  ratios between sea water and fresh spring water, temperature and depth of the subground water reservoir could be \\nestimated as 191\u2103 and 130 m beneath sea level. This is thought to be active thermal source which gives good cause for hope.","subitem_description_type":"Other"},{"subitem_description":"\u7d00\u8981\u8ad6\u6587","subitem_description_type":"Other"}]},"item_1617186643794":{"attribute_name":"Publisher","attribute_value_mlt":[{"subitem_1522300295150":"ja","subitem_1522300316516":"\u7409\u7403\u5927\u5b66\u7406\u5b66\u90e8"}]},"item_1617186702042":{"attribute_name":"Language","attribute_value_mlt":[{"subitem_1551255818386":"jpn"}]},"item_1617186783814":{"attribute_name":"Identifier","attribute_value_mlt":[{"subitem_identifier_type":"HDL","subitem_identifier_uri":"http://hdl.handle.net/20.500.12000/12168"}]},"item_1617186920753":{"attribute_name":"Source Identifier","attribute_value_mlt":[{"subitem_1522646500366":"ISSN","subitem_1522646572813":"0286-9640"},{"subitem_1522646500366":"NCID","subitem_1522646572813":"AN00250774"}]},"item_1617186941041":{"attribute_name":"Source Title","attribute_value_mlt":[{"subitem_1522650068558":"ja","subitem_1522650091861":"\u7409\u7403\u5927\u5b66\u7406\u5b66\u90e8\u7d00\u8981"},{"subitem_1522650068558":"en","subitem_1522650091861":"Bulletin of the College of Science. University of the Ryukyus"}]},"item_1617187056579":{"attribute_name":"Bibliographic Information","attribute_value_mlt":[{"bibliographicIssueNumber":"40","bibliographicPageEnd":"144","bibliographicPageStart":"137"}]},"item_1617258105262":{"attribute_name":"Resource Type","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_1617265215918":{"attribute_name":"Version Type","attribute_value_mlt":[{"subitem_1522305645492":"VoR","subitem_1600292170262":"http://purl.org/coar/version/c_970fb48d4fbd8a85"}]},"item_1617605131499":{"attribute_name":"File","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","filename":"No40p137.pdf","mimetype":"application/pdf","url":{"objectType":"fulltext","url":"https://u-ryukyu.repo.nii.ac.jp/record/2004843/files/No40p137.pdf"},"version_id":"90d50417-ad1c-456c-9896-f6d011cc3858"}]},"item_title":"\u7af9\u5bcc\u5cf6\u6d77\u5e95\u6e29\u6cc9\u306e\u8caf\u7559\u5c64\u306b\u3064\u3044\u3066\u306e\u4e00\u8003\u5bdf","item_type_id":"15","owner":"1","path":["1642837963990","1642838406414"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2009-08-28"},"publish_date":"2009-08-28","publish_status":"0","recid":"2004843","relation_version_is_last":true,"title":["\u7af9\u5bcc\u5cf6\u6d77\u5e95\u6e29\u6cc9\u306e\u8caf\u7559\u5c64\u306b\u3064\u3044\u3066\u306e\u4e00\u8003\u5bdf"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-02-15T03:58:14.923660+00:00"}