{"created":"2023-03-31T02:38:52.762530+00:00","id":5678,"links":{},"metadata":{"_buckets":{"deposit":"3fc9251b-5062-4781-8808-149bc94dba8b"},"_deposit":{"id":"5678","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"5678"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00005678","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2019-09","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"特別号","bibliographicPageEnd":"79","bibliographicPageStart":"57","bibliographicVolumeNumber":"38","bibliographic_titles":[{"bibliographic_title":"自然災害科学","bibliographic_titleLang":"ja"},{"bibliographic_title":"Japan Society for Natural Disaster Science","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"2014（平成26）年8月20日に広島県広島市で発生した土石流災害について，無人航空機（UAV）撮影とSfM写真測量により土砂堆積量を計測し，地質による被害特性の差異を明らかにした。人的被害は，谷出口から平均132 mの範囲で発生し，これは建物被害域よりも小さかった。建物被害域は，ホルンフェルス地域よりも花崗岩地域のほうが範囲が大きかった。また，ホルンフェルス地域では，建物が土石流を停止させる働きを示したが，花崗岩地域では，細粒な土砂が建物の間を通って，より遠方まで到達した。これらの結果は，このイベントにおける土石流の到達範囲が，沖積錐の地形発達範囲と同等か，それよりも小さいことを示している。","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"The debris flow disasters in Hiroshima City on 20 August 2014 were surveyed via Unmanned Aerial Vehicle photography (UAV) and Structure from Motion photogrammetry (SfM) to measure sediment deposition volume and to reveal the characteristics of damage to buildings and of geology. The average flow path in areas of human casualties was smaller than that in areas of building damage. Most casualties were concentrated within an average of 132m from the fan apex of each debris flow. The average flow path in areas of building damage was much longer on granite area than on hornfels area. On hornfels area, buildings stopped debris flow, but on granite area, fine particles continued downstream through gaps in buildings. These results show that the reach of debris flow in this event was the same as or less than the topographical development range of the alluvial cone.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本自然災害学会","subitem_publisher_language":"ja"},{"subitem_publisher":"Japan Society for Natural Disaster Science","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.24762/jndsj.38.S06_57"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0286-6021","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"内山 庄一郎","creatorNameLang":"ja"},{"creatorName":"Uchiyama Shoichiro","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"須貝 俊彦","creatorNameLang":"ja"},{"creatorName":"Toshihiko Sugai","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_title":"平成26年8月豪雨による広島市土石流災害の被害の特徴","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"平成26年8月豪雨による広島市土石流災害の被害の特徴","subitem_title_language":"ja"},{"subitem_title":"Damage characteristics of debris flow disasters caused by heavy rain in Hiroshima City in August 2014","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-05-24"},"publish_date":"2023-05-24","publish_status":"0","recid":"5678","relation_version_is_last":true,"title":["平成26年8月豪雨による広島市土石流災害の被害の特徴"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-05-24T02:50:32.444747+00:00"}