{"created":"2021-03-01T06:33:52.838424+00:00","id":28108,"links":{},"metadata":{"_buckets":{"deposit":"09af846c-5181-4406-860e-e99dcf2b18c8"},"_deposit":{"id":"28108","owners":[],"pid":{"revision_id":0,"type":"depid","value":"28108"},"status":"published"},"_oai":{"id":"oai:niigata-u.repo.nii.ac.jp:00028108","sets":["453:456","503:836:1555:1572"]},"item_7_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Tritium Level of Spring and River Waters in the Changjiang (Yantse) Valley"}]},"item_7_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1989-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"57","bibliographicPageStart":"49","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"新潟大学積雪地域災害研究センター研究年報"},{"bibliographic_title":"新潟大学積雪地域災害研究センター研究年報","bibliographic_titleLang":"en"}]}]},"item_7_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Some spring water (50 samples) was collected from the landslide areas in the Chanjiang (Yantse) valley, and river water was sampled from the Chanjiang river and its branches. Two rain water samples (Nov. 2, 1987) were collected in Huepai district. The conventional measurements of low level tritium were carried out by using liquid scintillation counting. Spring water varied from 0.22 to 6.73 Bq/l (mean value 3.09+1.18 Bq/l). and the Changjiang river water varies from 3.40 to 3.81 (Mean value 3.7+0.81 Bq/l).The rain water was 0.63 and 1.78 Bq/l. Water source of the rain water in this season was estimated as sea water after consideration of climatic conditions and the tritium concentration of sea water. Some ground water having high tritium concentrations was affected by precipitation contaminated by atmospheric nuclear explosion tests and a few low tritium concentration water was surely recharged before the artificial tritium addition. We concluded that the conventional measurements of low level tritium concentrations is very useful to estimate the ground water flow in the landslides in China.","subitem_description_type":"Abstract"}]},"item_7_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"161525","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Sato, Osamu"}]},{"nameIdentifiers":[{"nameIdentifier":"161526","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Aoki, Shigeru"}]},{"nameIdentifiers":[{"nameIdentifier":"161527","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Suzuki, Koji"}]},{"nameIdentifiers":[{"nameIdentifier":"161528","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakagawa, Takao"}]},{"nameIdentifiers":[{"nameIdentifier":"161529","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Hashimoto, Tetsuo"}]}]},"item_7_publisher_7":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"新潟大学積雪地域災害研究センター"}]},"item_7_select_19":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_7_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00183327","subitem_source_identifier_type":"NCID"}]},"item_7_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03877892","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"佐藤, 修"}],"nameIdentifiers":[{"nameIdentifier":"161520","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"青木, 滋"}],"nameIdentifiers":[{"nameIdentifier":"161521","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"鈴木, 幸治"}],"nameIdentifiers":[{"nameIdentifier":"161522","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"仲川, 隆夫"}],"nameIdentifiers":[{"nameIdentifier":"161523","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"橋本, 哲夫"}],"nameIdentifiers":[{"nameIdentifier":"161524","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":"2019-08-20"}],"displaytype":"detail","filename":"11_49-57.pdf","filesize":[{"value":"438.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"11_49-57.pdf","url":"https://niigata-u.repo.nii.ac.jp/record/28108/files/11_49-57.pdf"},"version_id":"4b7481a1-c8dc-41a6-b4b1-270b6a08e5a2"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Tritium","subitem_subject_scheme":"Other"},{"subitem_subject":"Changjiang","subitem_subject_scheme":"Other"},{"subitem_subject":"Landslide","subitem_subject_scheme":"Other"},{"subitem_subject":"Ground water","subitem_subject_scheme":"Other"},{"subitem_subject":"River water","subitem_subject_scheme":"Other"},{"subitem_subject":"トリチウム","subitem_subject_scheme":"Other"},{"subitem_subject":"長江","subitem_subject_scheme":"Other"},{"subitem_subject":"地すべり","subitem_subject_scheme":"Other"},{"subitem_subject":"地下水","subitem_subject_scheme":"Other"},{"subitem_subject":"河川水","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":"長江(揚子江)流域の地すべり地の湧水・河川水のトリチウム濃度 (故大草重康教授追悼号）","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"長江(揚子江)流域の地すべり地の湧水・河川水のトリチウム濃度 (故大草重康教授追悼号）"},{"subitem_title":"長江(揚子江)流域の地すべり地の湧水・河川水のトリチウム濃度 (故大草重康教授追悼号）","subitem_title_language":"en"}]},"item_type_id":"7","owner":"1","path":["456","1572"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-03-04"},"publish_date":"2016-03-04","publish_status":"0","recid":"28108","relation_version_is_last":true,"title":["長江(揚子江)流域の地すべり地の湧水・河川水のトリチウム濃度 (故大草重康教授追悼号）"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-15T03:58:05.043608+00:00"}