{"created":"2021-03-01T06:00:36.922006+00:00","id":8156,"links":{},"metadata":{"_buckets":{"deposit":"abec1d01-488e-4bb1-97a2-762d5109f218"},"_deposit":{"id":"8156","owners":[],"pid":{"revision_id":0,"type":"depid","value":"8156"},"status":"published"},"_oai":{"id":"oai:kitami-it.repo.nii.ac.jp:00008156","sets":["1:86"]},"author_link":["42699","42700","42701","42702","42695","44835","42697","42698"],"item_1646810750418":{"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_3_alternative_title_198":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Change of moisture content of unsuitable soil through freezing and thawing process appeared in natural cold climate"}]},"item_3_biblio_info_186":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2009","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"214","bibliographicPageStart":"205","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"地盤工学ジャーナル"}]}]},"item_3_description_184":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"地盤が地表面から冷やされて凍結が下方に進行していくとき，未凍土中の水分は凍結面すなわち上部に移動していく。この現象によって，凍結した部分は移動してきた水分により高含水状態になるが，水分が移動した未凍結部分は低含水比となる。この原理を利用して高含水比土の水分を低下させることができれば，低コストの土質改良が可能となる。本研究では，屋外凍結実験土槽を用いて，地盤中の温度と含水比分布，さらに冬期間の凍結性状の計測を2年間に渡って継続した。その結果，未凍結期における乾燥とそれに続く凍結期における水分移動の特性を明らかにすることができた。さらに，屋外土槽に投入した網走湖浚渫底質の含水比低下は，凍結期を挟んだ1年でその大部分が発生し，含水比は300%から150%程度にまで低下するなどの結果が得られた。\nGround freezes from the surface downward, and during this process soil moisture is drawn upward. The moisture content of soil that has frozen is high, whereas the moisture content of non-frozen soil below that is low, because water is drawn upward toward the soil that has frozen. If high-moisture soil can be improved to yield low-moisture soil using this phenomenon, low-cost improvement will be possible. Moisture can be reduced by repeated freezing and thawing, changes in soil temperature, then, soil moisture change through winter were monitored in outdoor experiments. It was shown that unsuitable soil could be improved by repeated freezing and thawing, that the decrease in moisture content was finished within one season.","subitem_description_type":"Abstract"}]},"item_3_full_name_183":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"42699","nameIdentifierScheme":"WEKO"}],"names":[{"name":"SATO, Atsuko","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"42700","nameIdentifierScheme":"WEKO"}],"names":[{"name":"NAKAMURA, Dai","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"42701","nameIdentifierScheme":"WEKO"}],"names":[{"name":"SUZUKI, Teruyuki","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"42702","nameIdentifierScheme":"WEKO"}],"names":[{"name":"NISHIMOTO, Satoshi","nameLang":"en"}]}]},"item_3_publisher_212":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"公益社団法人　地盤工学会"}]},"item_3_relation_191":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://doi.org/10.3208/jgs.4.205","subitem_relation_type_select":"DOI"}}]},"item_3_rights_192":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"c2009 公益社団法人　地盤工学会"}]},"item_3_select_195":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"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":"佐藤, 厚子","creatorNameLang":"ja"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"中村, 大","creatorNameLang":"ja"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"鈴木, 輝之","creatorNameLang":"ja"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"西本, 聡","creatorNameLang":"ja"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-11-22"}],"displaytype":"detail","filename":"2009_自然寒冷下での凍結融解過程における高含水比土の水分挙動.pdf","filesize":[{"value":"1.5 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"2009_自然寒冷下での凍結融解過程における高含水比土の水分挙動.pdf","url":"https://kitami-it.repo.nii.ac.jp/record/8156/files/2009_自然寒冷下での凍結融解過程における高含水比土の水分挙動.pdf"},"version_id":"fbb41aab-df88-4ffd-b901-79d521fa439e"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"frost heave","subitem_subject_scheme":"Other"},{"subitem_subject":"freeze-dry","subitem_subject_scheme":"Other"},{"subitem_subject":"high water content","subitem_subject_scheme":"Other"},{"subitem_subject":"improving","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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"自然寒冷下での凍結融解過程における高含水比土の水分挙動","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"自然寒冷下での凍結融解過程における高含水比土の水分挙動","subitem_title_language":"ja"},{"subitem_title":"Change of moisture content of unsuitable soil through freezing and thawing process appeared in natural cold climate","subitem_title_language":"en"}]},"item_type_id":"3","owner":"1","path":["86"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2016-04-04"},"publish_date":"2016-04-04","publish_status":"0","recid":"8156","relation_version_is_last":true,"title":["自然寒冷下での凍結融解過程における高含水比土の水分挙動"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-13T02:21:43.158648+00:00"}