{"_buckets": {"deposit": "5a058131-ea09-4ef2-8e0a-498df056c65f"}, "_deposit": {"id": "7030", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "7030"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00007030", "sets": ["870"]}, "author_link": ["18927", "18928", "18929", "18930", "18931", "18932"], "item_1615768549627": {"attribute_name": "出版タイプ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_9_alternative_title_19": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Storm-runoff characteristics of the three small steep watersheds, upstream of the Tenryu river", "subitem_alternative_title_language": "en"}]}, "item_9_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1994-12", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "108", "bibliographicPageStart": "85", "bibliographicVolumeNumber": "13", "bibliographic_titles": [{"bibliographic_title": "名古屋大学農学部演習林報告", "bibliographic_titleLang": "ja"}]}]}, "item_9_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "起伏が大きく、地質の異なる３つの小流域で、流出量、電気伝導度を連続観測した。また、自動採水装置で降雨時の河川水を採取し、水質分析を行った。なお、それぞれの流域の流域面積・起伏比などの地形条件や、植生や斜面物質などの条件はほぼ等しい。1993年の観測の結果、流出率やイベントの減衰の仕方、イベント発生の敏感さなど3流域で異なる結果を得た。中古生層地域のK1流域は、流出率が大きく、減衰が遅い流出が起こる。しかし降雨量が少ないときには流出が起きなかったり、起きても流出率がほとんど0％である。また、1つのイベントに、降雨と同時に発生する極めて小さな1次ピークと、平均9時間程度遅れて発生する大きな2次ピークとが存在する。花崗岩地域のY1流域は、ピーク流量が大きく、かつ減衰が速く、降雨に対して敏感な鋭い流出が発生する。変成岩地域のO1流域は、ピーク流量が小さく、減衰が速く、流出量が小さいという、流出反応が全体的に小さい特性を持つ。ハイドログラフおよび水質の特徴から、これらの流域では、表面流は主な流出成分ではない可能性が高いことが示唆された。したがって、流出特性の違いは、地質の違いによる地中での水の挙動の違いを示唆する。", "subitem_description_language": "ja", "subitem_description_type": "Abstract"}, {"subitem_description": "Hydrological observations were conducted in the small (3.8-7.1ha) steep forested watersheds where three types of bedrocks are underlain (Paleozoic sedimentary rocks, Granite, Metamorphic rocks). A contrasting runoff response to rainfall was observed. In K1 watersheds (sedimentary rocks), runoff did not respond to each rainfall, occurring only at the high antecedent rainfall condition. Double peak hydrographs, having very low initial peak and high secondary peak, were observed. Contrary to this, in Y1 watershed (Granite), frequent runoff events with high discharge peak were observed, and the quick flow runoff ratio was proportional to the amount of rainfall. In O1 watershed (Metamorphic rocks), the runoff response is similar to Y1 watershed, but the quick flow runoff ratio was much smaller. From the above results, it is suggested that these differences were caused by different storm water flow paths due to different underlying geology.", "subitem_description_language": "en", "subitem_description_type": "Abstract"}]}, "item_9_description_5": {"attribute_name": "内容記述", "attribute_value_mlt": [{"subitem_description": "農林水産研究情報センターで作成したPDFファイルを使用している。", "subitem_description_language": "ja", "subitem_description_type": "Other"}]}, "item_9_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/8704"}]}, "item_9_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.18999/bulnuf.13.85", "subitem_identifier_reg_type": "JaLC"}]}, "item_9_publisher_32": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "名古屋大学農学部付属演習林", "subitem_publisher_language": "ja"}]}, "item_9_relation_43": {"attribute_name": "関連情報", "attribute_value_mlt": [{"subitem_relation_type": "isVersionOf", "subitem_relation_type_id": {"subitem_relation_type_id_text": "http://rms1.agsearch.agropedia.affrc.go.jp/contents/JASI/pdf/academy/56-1675.pdf", "subitem_relation_type_select": "URI"}}]}, "item_9_select_15": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_9_source_id_7": {"attribute_name": "ISSN（print）", "attribute_value_mlt": [{"subitem_source_identifier": "0469-4708", "subitem_source_identifier_type": "PISSN"}]}, "item_9_text_14": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}]}, "item_access_right": {"attribute_name": "アクセス権", "attribute_value_mlt": [{"subitem_access_right": "open access", "subitem_access_right_uri": "http://purl.org/coar/access_right/c_abf2"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "岩下, 広和", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "18927", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "IWASHITA, Hirokazu", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18928", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "恩田, 裕一", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "18929", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ONDA, Yuichi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18930", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "一柳, 錦平", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "18931", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ICHIYANAGI, Kimpei", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18932", "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": "2018-02-19"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "bulnuf_13_85.pdf", "filesize": [{"value": "3.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 3100000.0, "url": {"label": "bulnuf_13_85.pdf", "objectType": "fulltext", "url": "https://nagoya.repo.nii.ac.jp/record/7030/files/bulnuf_13_85.pdf"}, "version_id": "9d4ac22d-e710-4e9b-aa56-42a7341410d1"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "降雨流出特性", "subitem_subject_scheme": "Other"}, {"subitem_subject": "山地小流域", "subitem_subject_scheme": "Other"}, {"subitem_subject": "基盤岩", "subitem_subject_scheme": "Other"}, {"subitem_subject": "二つのピーク", "subitem_subject_scheme": "Other"}, {"subitem_subject": "降雨時河川水質", "subitem_subject_scheme": "Other"}, {"subitem_subject": "runoff characteristics", "subitem_subject_scheme": "Other"}, {"subitem_subject": "mountainous headwater catchment", "subitem_subject_scheme": "Other"}, {"subitem_subject": "bedrock", "subitem_subject_scheme": "Other"}, {"subitem_subject": "secondary peak", "subitem_subject_scheme": "Other"}, {"subitem_subject": "water qualities in event", "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": "天竜川上流域における急峻な3つの小流域の流出特性の違い", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "天竜川上流域における急峻な3つの小流域の流出特性の違い", "subitem_title_language": "ja"}]}, "item_type_id": "9", "owner": "1", "path": ["870"], "permalink_uri": "https://doi.org/10.18999/bulnuf.13.85", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2007-08-28"}, "publish_date": "2007-08-28", "publish_status": "0", "recid": "7030", "relation": {}, "relation_version_is_last": true, "title": ["天竜川上流域における急峻な3つの小流域の流出特性の違い"], "weko_shared_id": -1}