{"created":"2023-07-25T08:09:08.562598+00:00","id":8651,"links":{},"metadata":{"_buckets":{"deposit":"c851a2ac-9fdb-470d-a731-412298620c3c"},"_deposit":{"created_by":18,"id":"8651","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"8651"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00008651","sets":["54:79"]},"author_link":["5739"],"item_8_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2013-03-31","subitem_date_issued_type":"Collected"}]},"item_8_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"2011-2012年度科学研究費助成事業(科学研究費補助金(若手研究(B))研究成果報告書　課題番号：23760466　研究代表者：齋田倫範(鹿児島大学・大学院理工学研究科・助教)","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"本研究では，九州南部の川内川上流域を対象とし，細粒土砂生産特性の把握を目的とした浮遊砂輸送量に関する現地観測，ならびに主要な細粒土砂生産地域の特定を目的とした元素組成に基づく土壌特性のマッピングを行った．その結果，支川である羽月川流域で細粒土砂生産能が相対的に高いことや大口盆地南部では平常時に細粒土砂が堆積する傾向にあることが確認された．さらに，原位置元素組成調査によって，土壌の化学的特性に基づく小流域スケールでの地域区分の可能性が示された．","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"In this study, field observations on suspended sediment transport were carried out to evaluate fine sediment production rates in upstream sites of the Sendai River basin. And mapping of soil characteristics in the Kakuto Basin were carried out to detect dominant producing areas of fine sediments. As a result of these observations,\nIt is clarified that the Hatsuki River basin, the most major branch of the upper Sendai River, is an area of a relatively high sediment production rate and that the southern part of Okuchi baisn is on a depositional trend. In addition, a possibility of area classification on the space scale comparable to small watersheds based on elementary composition of soil is indicated.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_8_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_8_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"510","subitem_subject_scheme":"NDC"}]},"item_8_text_41":{"attribute_name":"科研費番号 ","attribute_value_mlt":[{"subitem_text_value":"23760466"}]},"item_8_version_type_14":{"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":"齋田, 倫範","creatorNameLang":"ja"},{"creatorName":"SAITA, Tomonori","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"5739","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000080432863","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-28"}],"displaytype":"detail","filename":"23760466.pdf","filesize":[{"value":"515.9 kB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"23760466.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/8651/files/23760466.pdf"},"version_id":"58c2bd6a-1de8-47a0-a4cd-3c6967ce6201"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"水工水理学","subitem_subject_language":"ja","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":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"山地流域の地形・地質・土壌分類に基づく粒度別土砂生産ポテンシャルの空間的評価","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"山地流域の地形・地質・土壌分類に基づく粒度別土砂生産ポテンシャルの空間的評価","subitem_title_language":"ja"},{"subitem_title":"Spatial evaluation of sediment production rates by grain size based on topographical, geological and soil features in mountainous watersheds","subitem_title_language":"en"}]},"item_type_id":"8","owner":"18","path":["79"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2013-10-01"},"publish_date":"2013-10-01","publish_status":"0","recid":"8651","relation_version_is_last":true,"title":["山地流域の地形・地質・土壌分類に基づく粒度別土砂生産ポテンシャルの空間的評価"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-05-23T02:18:09.957161+00:00"}