{"created":"2021-03-01T06:17:02.289188+00:00","id":497,"links":{},"metadata":{"_buckets":{"deposit":"8f4073f6-a056-4c46-b72c-a83f985a29f0"},"_deposit":{"id":"497","owners":[],"pid":{"revision_id":0,"type":"depid","value":"497"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00000497","sets":["27:28:37","9:10:11"]},"item_2_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"The Influence of Edaphic Factors to Sand Dune Remobilization in the Sandy Grassland in Inner Mongolia, China"}]},"item_2_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1998","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"5","bibliographicPageEnd":"584","bibliographicPageStart":"581","bibliographicVolumeNumber":"61","bibliographic_titles":[{"bibliographic_title":"ランドスケープ研究"}]}]},"item_2_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"旧日本軍が作成した1930年代の地形図と中国科学院が作成した1980年代の砂漠化類型園を比べた結果,中国内蒙古自治区奈量旗でも,周辺で報告された結果にほぼ一致する約1.8倍の流動砂丘の拡大がみられた｡ 1980年代における砂漠化程度は,地形では砂丘,低位段丘,氾濫原の順に大きく,土壌では風積砂土が湿草地を上回った｡大半のカテゴリでは, 1930年代に砂漠化地域だったところのほうがそうでなかったところより1980年代の砂漠化の度合いが大きかったか,例外的に逆の結果になるものもあった｡","subitem_description_type":"Abstract"}]},"item_2_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"1705","nameIdentifierScheme":"WEKO"}],"names":[{"name":"TACHIIRI, Kaoru"}]},{"nameIdentifiers":[{"nameIdentifier":"1706","nameIdentifierScheme":"WEKO"}],"names":[{"name":"TAKEUCHI, Kazuhiko"}]}]},"item_2_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本造園学会"}]},"item_2_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10455955","subitem_source_identifier_type":"NCID"}]},"item_2_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13408984","subitem_source_identifier_type":"ISSN"}]},"item_2_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"629","subitem_subject_scheme":"NDC"},{"subitem_subject":"290.13","subitem_subject_scheme":"NDC"}]},"item_2_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"東京大学大学院農学生命科学研究科"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"立入, 郁"}],"nameIdentifiers":[{"nameIdentifier":"1703","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"武内, 和彦"}],"nameIdentifiers":[{"nameIdentifier":"1704","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":"2017-05-30"}],"displaytype":"detail","filename":"LRJ_61_50_581.pdf","filesize":[{"value":"807.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"LRJ_61_50_581.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/497/files/LRJ_61_50_581.pdf"},"version_id":"5c04b064-a2d2-43a2-8725-a2ddfae30ab2"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"中国内蒙古・砂地草原における土地的要因が流動砂丘の拡大に及ぼす影響","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"中国内蒙古・砂地草原における土地的要因が流動砂丘の拡大に及ぼす影響"}]},"item_type_id":"2","owner":"1","path":["11","37"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-06-30"},"publish_date":"2010-06-30","publish_status":"0","recid":"497","relation_version_is_last":true,"title":["中国内蒙古・砂地草原における土地的要因が流動砂丘の拡大に及ぼす影響"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T03:41:28.513913+00:00"}