{"_buckets": {"deposit": "93a5c5b5-dec6-4529-9274-d74cbbc306e2"}, "_deposit": {"id": "8646", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "8646"}, "status": "published"}, "_oai": {"id": "oai:kitami-it.repo.nii.ac.jp:00008646", "sets": ["1:86"]}, "author_link": ["89975", "89976", "89977", "89978", "89971", "89972", "89973", "89974"], "item_1646810750418": {"attribute_name": "\u51fa\u7248\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_3_alternative_title_198": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "FRAZIL SLUSH VARIATION IN TAKE FACILITIES ON ICE-COVERED RIVERS", "subitem_alternative_title_language": "en"}]}, "item_3_biblio_info_186": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2017", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "I_1326", "bibliographicPageStart": "I_1321", "bibliographicVolumeNumber": "73", "bibliographic_titles": [{"bibliographic_title": "\u571f\u6728\u5b66\u4f1a\u8ad6\u6587\u96c6B1(\u6c34\u5de5\u5b66)", "bibliographic_titleLang": "ja"}]}]}, "item_3_description_184": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "\u672c\u7814\u7a76\u306e\u76ee\u7684\u306f\uff0c\u53d6\u6c34\u5830\u4e0a\u6d41\u306b\u304a\u3051\u308b\u6cb3\u5ddd\u7e26\u65ad\u65b9\u5411\u306e\u6676\u6c37\u5909\u52d5\u73fe\u8c61\u306e\u89e3\u660e\u3067\u3042\u308b\uff0e\u6676\u6c37\u306e\u767a\u751f\u30fb\u8f38\u9001\u30fb\u5806\u7a4d\n\u3092\u8003\u616e\u3057\u305f\u8a08\u7b97\u30e2\u30c7\u30eb\u3092\u69cb\u7bc9\u3057\u305f\uff0e\u904e\u53bb\u306b\u51ac\u671f\u306e\u53d6\u6c34\u969c\u5bb3\u304c\u767a\u751f\u3057\u305f\u5b9f\u6cb3\u5ddd\u306b\u304a\u3044\u3066\uff0c\u6676\u6c37\u8f38\u9001\u91cf\u304a\u3088\u3073\u6c37\u677f\u30fb\n\u6676\u6c37\u65ad\u9762\u7a4d\u306e\u73fe\u5730\u89b3\u6e2c\u3092\u5b9f\u65bd\u3057\u305f\uff0e\u89b3\u6e2c\u5024\u304a\u3088\u3073\u8a08\u7b97\u5024\u306b\u57fa\u3065\u304d\uff0c\u6676\u6c37\u5909\u52d5\u73fe\u8c61\u3092\u63a8\u5b9a\u3057\u305f\uff0e\u7d50\u6c37\u306f\u53d6\u6c34\u5830\u304b\n\u3089\u59cb\u307e\u308a\uff0c\u6642\u9593\u306e\u7d4c\u904e\u3068\u3068\u3082\u306b\u4e0a\u6d41\u3078\u3068\u9032\u3080\uff0e\u6c34\u9762\u3067\u767a\u751f\u304a\u3088\u3073\u8f38\u9001\u3055\u308c\u308b\u6676\u6c37\u306f\uff0c\u4e0b\u6d41\u306e\u6c37\u677f\u4e0b\u306b\u5806\u7a4d\u3059\u308b\uff0e\n\u7d50\u6c37\u306e\u5148\u7aef\u5730\u70b9\u306e\u4e0a\u6d41\u306b\u8fd1\u3044\u307b\u3069\uff0c\u6676\u6c37\u9762\u7a4d\u306f\u65e9\u3044\u6bb5\u968e\u3067\u6025\u6fc0\u306b\u5897\u52a0\u3059\u308b\uff0e\u305d\u306e\u5f8c\uff0c\u4e0a\u6d41\u306e\u6676\u6c37\u304c\u4e0b\u6d41\u3078\u3068\u6d41\n\u308c\u3066\uff0c\u4e0b\u6d41\u306b\u304a\u3044\u3066\u6676\u6c37\u9762\u7a4d\u304c\u6025\u6fc0\u306b\u5897\u52a0\u3059\u308b\uff0e\u51ac\u671f\u306e\u53d6\u6c34\u969c\u5bb3\u306e\u5371\u967a\u6027\u304c\u9ad8\u3044\u6642\u671f\u306f\uff0c\u7d50\u6c37\u306e\u59cb\u307e\u308a\u306e\u6642\u671f\n\u3068\uff0c\u7d50\u6c37\u5f8c\u306b\u4e0a\u6d41\u304b\u3089\u6676\u6c37\u304c\u8f38\u9001\u3055\u308c\u308b\u6642\u671f\u3067\u3042\u308b\u3053\u3068\u304c\u63a8\u5bdf\u3055\u308c\u305f\uff0e", "subitem_description_type": "Abstract"}, {"subitem_description": "This study aims to clarify the frazil slush variation mechanisms associated with the water intake facilities of ice-covered rivers. A river ice calculation model was developed to determine the dynamics of frazil slush\ngeneration, transport, and accumulation. Field observations of frazil slush transport, ice sheet and frazil slush cross sections were performed. In the results, The phenomenon in which a river freezes begins from\nintake facilities, and it progresses to upstream direction. Frazil slush that is generated upstream accumulates under downstream ice sheets. Frazil slush accumulates more quickly in upstream than downstream. Then, as\nupstream frazil slush accumulation begins to flow downstream, it accumulates more quickly in downstream.", "subitem_description_type": "Abstract"}]}, "item_3_full_name_183": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "89975", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Yoshikawa, Yasuhiro", "nameLang": "en"}]}, {"nameIdentifiers": [{"nameIdentifier": "89976", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Okabe, Hirokazu", "nameLang": "en"}]}, {"nameIdentifiers": [{"nameIdentifier": "89977", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Hashiba, Masahiro", "nameLang": "en"}]}, {"nameIdentifiers": [{"nameIdentifier": "89978", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Morita, Tomotsugu", "nameLang": "en"}]}]}, "item_3_publisher_212": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u571f\u6728\u5b66\u4f1a"}]}, "item_3_rights_192": 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