{"created":"2023-05-15T14:59:04.454841+00:00","id":80146,"links":{},"metadata":{"_buckets":{"deposit":"7c2d1b26-a498-4d2d-b311-0408ecb9ec42"},"_deposit":{"created_by":1,"id":"80146","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"80146"},"status":"published"},"_oai":{"id":"oai:repo.qst.go.jp:00080146","sets":["1"]},"author_link":["879537","879533","879536","879534","879535"],"item_8_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2020-03","bibliographicIssueDateType":"Issued"},"bibliographicVolumeNumber":"15","bibliographic_titles":[{"bibliographic_title":"Journal of Instrumentation"}]}]},"item_8_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Starting in 1996, the coordinates of the accelerator components on the SPring-8 storage ring were continuously surveyed for over two decades. The dispersion of the elevation changes of the ground motion lang dz2rang analyzed from the aspect of the empirical ATL-law which has been intensively researched since 1990s. With the ATL-law, lang dz2rang can be expressed as products of a ground diffusion coefficient A, temporal survey spans T, and spatial scales L. The coefficient A is well known to depend on the local geology and is evaluated as (7.6 ± 1.4) × 10−6 μm2/s/m for the SPring-8 storage ring. In this paper, a transition of survey methods in the SPring-8 storage ring is reviewd and survey results both in horizontal and vertical directions are presented. Furthermore, the relevance of the ATL-law approach for the ground elevation dispersion are discussed.","subitem_description_type":"Abstract"}]},"item_8_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1088/1748-0221/15/03/P03033","subitem_relation_type_select":"DOI"}}]},"item_8_relation_17":{"attribute_name":"関連サイト","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://iopscience.iop.org/article/10.1088/1748-0221/15/03/P03033/meta","subitem_relation_type_select":"URI"}}]},"item_8_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1748-0221","subitem_source_identifier_type":"ISSN"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Okayasu, Y."}],"nameIdentifiers":[{"nameIdentifier":"879533","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Matsui, S."}],"nameIdentifiers":[{"nameIdentifier":"879534","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Zhang, C."}],"nameIdentifiers":[{"nameIdentifier":"879535","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kimura, Hiroaki"}],"nameIdentifiers":[{"nameIdentifier":"879536","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kimura, Hiroaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"879537","nameIdentifierScheme":"WEKO"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"An interpretation of SPring-8 ground elevation by the empirical AT L-law approach","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"An interpretation of SPring-8 ground elevation by the empirical AT L-law approach"}]},"item_type_id":"8","owner":"1","path":["1"],"pubdate":{"attribute_name":"公開日","attribute_value":"2020-07-01"},"publish_date":"2020-07-01","publish_status":"0","recid":"80146","relation_version_is_last":true,"title":["An interpretation of SPring-8 ground elevation by the empirical AT L-law approach"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-05-15T21:42:08.007570+00:00"}