{"_buckets": {"deposit": "e49170a3-38eb-4b46-8702-8ea1f6405ded"}, "_deposit": {"created_by": 16, "id": "2001450", "owners": [16], "pid": {"revision_id": 0, "type": "depid", "value": "2001450"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:02001450", "sets": ["1684378320437"]}, "author_link": [], "item_1628147817048": {"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_6_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2021-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "27", "bibliographicPageStart": "12", "bibliographicVolumeNumber": "43", "bibliographic_titles": [{"bibliographic_title": "環境科学年報"}]}]}, "item_6_description_20": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "2020年8月5日の諏訪湖では，SS，Chl-a，IL，Trans.は2003年以降の同時期の平均的な状況よ りも改善されていた。表層から下層の水温はいずれも同時期平均より低く，特にW.T.2m～W.T.5m はこれまでの16観測日中で最も低温であった。表層から下層のDO は同時期平均よりも高く，特 にDO0m～DO3m は15 観測日中で最も高かった。下層の貧酸素状態は同時期よりも改善されてい た。 2020年8月5日の表層4水質要素の主成分分析により主要な分布パターンを抽出した。第1主 成分は，SS，Chl-a の変動とW.T.0m の変動の一部を説明し，第2主成分はTrans.の変動を説明する パターンである。 2020年夏季の諏訪湖湖心における水深0.5mと水深1.5mの水温ピークは，8月21日（水深0.5m 27.8℃ ），8月22日（水深1.5m27.4℃）とほぼ同時期に出現した。水深3m，4m，5m の水温ピーク は，水深0.5mと水深1.5mの水温ピークよりも遅れて9月2日（水深3m25.4℃），9月3日（水深 4m25.0℃），9月7日（水深5m24.5℃）に出現した。", "subitem_description_type": "Abstract"}]}, "item_6_description_30": {"attribute_name": "資源タイプ（コンテンツの種類）", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_6_description_5": {"attribute_name": "引用", "attribute_value_mlt": [{"subitem_description": "環境科学年報 43 : 12-27, (2021)", "subitem_description_type": "Other"}]}, "item_6_link_3": {"attribute_name": "信州大学研究者総覧へのリンク", "attribute_value_mlt": [{"subitem_link_text": "柳町, 晴美", 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