{"created":"2023-07-25T08:01:01.909066+00:00","id":9818,"links":{},"metadata":{"_buckets":{"deposit":"f842a234-f574-438d-b7a1-89b96915050c"},"_deposit":{"created_by":1,"id":"9818","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"9818"},"status":"published"},"_oai":{"id":"oai:rissho.repo.nii.ac.jp:00009818","sets":["11:743:823:870"]},"author_link":["11006","11005","11008","11007"],"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-03-20","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"20","bibliographicPageStart":"9","bibliographicVolumeNumber":"37","bibliographic_titles":[{"bibliographic_title":"地域研究"},{"bibliographic_title":"REGIONAL STUDIES","bibliographic_titleLang":"en"}]}]},"item_4_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"三重県の北部を流れる員弁川の上流部は，員弁川と河内谷川という2つの小さな支流に分かれている．両支流域は隣接し，その流域面積はほぼ同じである．しかも，地形，地質，気候，植生，土壌など河川の流出に影響を与える条件もほとんど同じである．しかし，古くから員弁川の水の一部が地下を通って河内谷川に入るため，両支流の河川流出量には大きな差があると言われてきた．そこで筆者らは，河川流出量，水温，水質などを調査することによってこの言い伝えを検証するとともに，当地域の水の交流と流出の機構を解明しようとした．その結果，河内谷川の水には員弁川流域から地下を通ってきた地下水が含まれていることが確かめられた．両支流域を含む鈴鹿山脈一帯には石灰岩が広く分布し，多数の石灰洞が確認されており，それらの一部が水の移動経路になっていると考えられる．","subitem_description_type":"Abstract"},{"subitem_description":"The upper Inabe River flowing in the north of Mie Prefecture consists of two small branch rivers, the Inabe and the Kochidani. The drainage basins of the two branch rivers are neighboring, and their drainage areas are almost equal. Landform, geology, climate, vegetation and soil of two basins, which have some effects on river runoff, are very similar. But it has been said that the river discharge of the two branch rivers is different, because some part of water of the Inabe River flows into the Kochidani basin through under-ground route. So by surveying river discharge, water temperature and water quality, the authors tried to verify this assumption and to make clear the system of interchange of water and runoff in this study area. As the result, it has been confirmed that water of the Kochidani Basin including groundwater flowing from the Inabe Basin through underground route. Limestone is widely distributed in the Suzuka Mountains including the two river basins. Many limestone caves are found in the region, therefore some of them are considered to be the route of water flow.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"論説","subitem_description_type":"Other"},{"subitem_description":"ARTICLES","subitem_description_type":"Other"}]},"item_4_publisher_35":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"立正地理学会"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03896641","subitem_source_identifier_type":"ISSN"}]},"item_4_text_8":{"attribute_name":"通巻号","attribute_value_mlt":[{"subitem_text_value":"65"}]},"item_4_version_type_18":{"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":"溝口, 晃之"}],"nameIdentifiers":[{"nameIdentifier":"11005","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"原, 昭宏"}],"nameIdentifiers":[{"nameIdentifier":"11006","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"MIZOGUCHI, Teruyuki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"11007","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"HARA, Akihiro","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"11008","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":"2022-02-22"}],"displaytype":"detail","filename":"RS037-2.9-20.三重県員弁川上流域における隣接した2支流間の水の交流.pdf","filesize":[{"value":"6.4 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"RS037-2.9-20.三重県員弁川上流域における隣接した2支流間の水の交流.pdf","url":"https://rissho.repo.nii.ac.jp/record/9818/files/RS037-2.9-20.三重県員弁川上流域における隣接した2支流間の水の交流.pdf"},"version_id":"89c1b530-0194-47c8-9386-10bf7252f16e"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"三重県","subitem_subject_scheme":"Other"},{"subitem_subject":"水の交流","subitem_subject_scheme":"Other"},{"subitem_subject":"流出","subitem_subject_scheme":"Other"},{"subitem_subject":"石灰洞","subitem_subject_scheme":"Other"},{"subitem_subject":"Mie Prefecture","subitem_subject_scheme":"Other"},{"subitem_subject":"interchange of water","subitem_subject_scheme":"Other"},{"subitem_subject":"runoff","subitem_subject_scheme":"Other"},{"subitem_subject":"limestone cave","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":"三重県員弁川上流域における隣接した2支流間の水の交流","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"三重県員弁川上流域における隣接した2支流間の水の交流"},{"subitem_title":"Interchange of Water between Two Neighboring Branch Rivers in the Upper Inabe Basin, Mie Prefecture","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["870"],"pubdate":{"attribute_name":"公開日","attribute_value":"2022-02-22"},"publish_date":"2022-02-22","publish_status":"0","recid":"9818","relation_version_is_last":true,"title":["三重県員弁川上流域における隣接した2支流間の水の交流"],"weko_creator_id":"1","weko_shared_id":1},"updated":"2023-07-25T11:58:37.602275+00:00"}