{"created":"2023-07-25T10:29:43.503049+00:00","id":422,"links":{},"metadata":{"_buckets":{"deposit":"f3941504-1c3c-44c8-a1c2-8964cdead98e"},"_deposit":{"created_by":3,"id":"422","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"422"},"status":"published"},"_oai":{"id":"oai:shizuoka.repo.nii.ac.jp:00000422","sets":["8:87:111"]},"author_link":["355","334"],"item_25_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Analytical method of ^<32>P in atmospheric aerosol"}]},"item_25_biblio_info_5":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-07","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"86","bibliographicPageStart":"79","bibliographicVolumeNumber":"24","bibliographic_titles":[{"bibliographic_title":"静岡大学地球科学研究報告"}]}]},"item_25_description_30":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_25_description_9":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Cosmic ray produced ^<32>P(t_<1/2>=14.3days;E_<max>=1.71MeV) is a powerful tracer of physical and biological processes and the short time scales of atmospheric and upper ocean P cycling. In spite of their tremendous potential for tracing processes involving phosphorus in the environment, the very low activities in nature have impeded their use in biogeochemistry. In order to determine the low-level beta activities of ^<32>P in nature, sample concentration and/or extraction from large volumes of samples are required with a low-level β counting in the field. Preconcentration of the activity in aerosol is achieved here by various concentrating methods. Low-level β counting is achieved by liquid scintillation counting and low background counting. The result of measurement of the activity in aerosol by liquid scintillation counting at Shizuoka University (34°58'N, 138°24'E) ranged from 0.0010±0.0002 to 0.003l±0.0002dpm / m^3 (dpm : disintegrations per minute). Decay-curve in low background counting confirms the existence of ^<33>P(t_<l/2> = 25.3days;E_<max> = 0.25MeV).","subitem_description_type":"Abstract"}]},"item_25_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.14945/00000349","subitem_identifier_reg_type":"JaLC"}]},"item_25_publisher_6":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"静岡大学地球科学教室"}]},"item_25_relation_22":{"attribute_name":"NII論文ID","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"110000413381","subitem_relation_type_select":"NAID"}}]},"item_25_source_id_19":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03886298","subitem_source_identifier_type":"ISSN"}]},"item_25_source_id_23":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00103190","subitem_source_identifier_type":"NCID"}]},"item_25_subject_8":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_25_version_type_32":{"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":"栗本, 卓"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"鈴木, 款"}],"nameIdentifiers":[{},{},{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-12-14"}],"displaytype":"detail","filename":"KJ00000102421.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00000102421.pdf","url":"https://shizuoka.repo.nii.ac.jp/record/422/files/KJ00000102421.pdf"},"version_id":"71932e39-07c3-42ef-a596-8afe33d8c8be"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"^<32>P","subitem_subject_scheme":"Other"},{"subitem_subject":"aerosol","subitem_subject_scheme":"Other"},{"subitem_subject":"liquid scintillation counting","subitem_subject_scheme":"Other"},{"subitem_subject":"lowbackground counting","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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"大気エアロゾル中の^<32>Pの測定法の検討","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"大気エアロゾル中の^<32>Pの測定法の検討"}]},"item_type_id":"25","owner":"3","path":["111"],"pubdate":{"attribute_name":"公開日","attribute_value":"2008-01-25"},"publish_date":"2008-01-25","publish_status":"0","recid":"422","relation_version_is_last":true,"title":["大気エアロゾル中の^<32>Pの測定法の検討"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2024-02-19T05:39:41.777937+00:00"}