{"created":"2024-06-03T02:00:32.382598+00:00","id":6656,"links":{},"metadata":{"_buckets":{"deposit":"27be090e-e6c4-4a69-adb9-3c4e092006f6"},"_deposit":{"created_by":10,"id":"6656","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"6656"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00006656","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"41","bibliographicPageEnd":"1100","bibliographicPageStart":"1097","bibliographic_titles":[{"bibliographic_title":"水工学論文集","bibliographic_titleLang":"ja"},{"bibliographic_title":"PROCEEDINGS OF HYDRAULIC ENGINEERING","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The object of this study is to develop a method for estimating both the ground thermometric parameter (ρ c λ) and ground conductive heat flux (G) simultaneously by using the ground surface temperature (Ts). This method is based on the Fourier series expressions of the result of heat transfer equation. The method is tested by a field-measurement. The following results are obtained: 1) The estimated ρ c λ have a reasonable value. 2) Estimated diurnal variations of G agree very well with that observed. 3) The spatial distribution of ρ c λ is also estimated from the surface temperature distribution obtained by the thermo-graphy.","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"The object of this study is to develop a method for estimating both the ground thermometric parameter (ρ c λ) and ground conductive heat flux (G) simultaneously by using the ground surface temperature (Ts). This method is based on the Fourier series expressions of the result of heat transfer equation. The method is tested by a field-measurement. The following results are obtained: 1) The estimated ρ c λ have a reasonable value. 2) Estimated diurnal variations of G agree very well with that observed. 3) The spatial distribution of ρ c λ is also estimated from the surface temperature distribution obtained by the thermo-graphy.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"公益社団法人 土木学会","subitem_publisher_language":"ja"},{"subitem_publisher":"Japan Society of Civil Engineers","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.2208/prohe.41.1097"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0916-7374","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"森脇 亮","creatorNameLang":"ja"},{"creatorName":"MORIWAKI Ryo","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"神田 学","creatorNameLang":"ja"},{"creatorName":"KANDA Manabu","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"横山 仁","creatorNameLang":"ja"},{"creatorName":"Yokoyama Hitoshi","creatorNameLang":"en"}]}]},"item_title":"地表面温度を用いた土壌熱物性値及び地中熱流量の逆推定法の提案","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"地表面温度を用いた土壌熱物性値及び地中熱流量の逆推定法の提案","subitem_title_language":"ja"},{"subitem_title":"Direct Estimation of Ground Thermometric Parameter and Ground Conductive Heat Flux, from Ground Surface Temperature","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"10","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-06-03"},"publish_date":"2024-06-03","publish_status":"0","recid":"6656","relation_version_is_last":true,"title":["地表面温度を用いた土壌熱物性値及び地中熱流量の逆推定法の提案"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2024-06-03T02:00:34.587697+00:00"}