{"created":"2023-05-15T15:27:44.758303+00:00","id":16674,"links":{},"metadata":{"_buckets":{"deposit":"bc80667b-cdf3-4308-8a8a-c95c1663c5ca"},"_deposit":{"created_by":3,"id":"16674","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"16674"},"status":"published"},"_oai":{"id":"oai:sucra.repo.nii.ac.jp:00016674","sets":["95:239:635"]},"author_link":["16684"],"item_120_alternative_title_1":{"attribute_name":"タイトル（別言語）","attribute_value_mlt":[{"subitem_alternative_title":"Soil Water Dynamics in a Hilly Soil on a Landslide Site under Natural Precipitation"}]},"item_120_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"84","bibliographicPageStart":"79","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"埼玉大学地域共同研究センター紀要"},{"bibliographic_title":"Report of Cooperative Research Center, Saitama University","bibliographic_titleLang":"en"}]}]},"item_120_date_31":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2009-06-18","subitem_date_issued_type":"Created"}]},"item_120_description_19":{"attribute_name":"概要","attribute_value_mlt":[{"subitem_description":"Soil water content and water pressure were monitored in a test pit excavated in a forested hilly soil during Dec. 2001 to Nov. 2002. The present monitoring system worked well, and provided us useful information successively on soil water dynamics. Rapid drainage of rainwater occurs not only in a heavy rainfall but also in a small amount of rainfall, suggesting that preferential flow is generated as soon as a rainfall starts. This occurs because a soil matrix is fully saturated with water under the soil moisture condition throughout the monitoring period. Field-measured hydraulic conductivities are larger than those that are laboratory-measured. The reason is explained as follows: that macropores are well connected in macro-scale so that preferential flow paths are easily formed in the field. In a small sample, however, macropores are not fully connected to make preferential flow paths through them.","subitem_description_type":"Other"}]},"item_120_description_29":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"subitem_description":"text","subitem_description_type":"Other"}]},"item_120_description_30":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_120_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24561/00016668","subitem_identifier_reg_type":"JaLC"}]},"item_120_publisher_11":{"attribute_name":"出版者名","attribute_value_mlt":[{"subitem_publisher":"埼玉大学地域共同研究センター"}]},"item_120_source_id_14":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13474758","subitem_source_identifier_type":"ISSN"}]},"item_120_text_3":{"attribute_name":"著者 ローマ字","attribute_value_mlt":[{"subitem_text_value":"Ken Kawamoto"}]},"item_120_text_32":{"attribute_name":"アイテムID","attribute_value_mlt":[{"subitem_text_value":"KY-AA11808968-03-30"}]},"item_120_text_4":{"attribute_name":"著者 所属","attribute_value_mlt":[{"subitem_text_value":"埼玉大学工学部建設工学科"}]},"item_120_text_5":{"attribute_name":"著者 所属(別言語)","attribute_value_mlt":[{"subitem_text_value":"Department of Civil and Environmental Engineering, Faculty of Engineering, Saitama University"}]},"item_120_text_9":{"attribute_name":"年月次","attribute_value_mlt":[{"subitem_text_value":"2002"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"川本, 健"}],"nameIdentifiers":[{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2018-01-24"}],"displaytype":"detail","filename":"KY-AA11808968-03-30.pdf","filesize":[{"value":"264.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KY-AA11808968-03-30.pdf","url":"https://sucra.repo.nii.ac.jp/record/16674/files/KY-AA11808968-03-30.pdf"},"version_id":"a429e9f7-8a27-413c-98b3-f7e313fd769a"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Soil Water Dynamics","subitem_subject_scheme":"Other"},{"subitem_subject":"Field Monitoring","subitem_subject_scheme":"Other"},{"subitem_subject":"Macropore","subitem_subject_scheme":"Other"},{"subitem_subject":"Preferential Flow","subitem_subject_scheme":"Other"},{"subitem_subject":"hilly Soil","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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"斜面崩壊丘陵地における自然降雨下での土壌水分動態の把握","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"斜面崩壊丘陵地における自然降雨下での土壌水分動態の把握"}]},"item_type_id":"120","owner":"3","path":["635"],"pubdate":{"attribute_name":"公開日","attribute_value":"2009-05-21"},"publish_date":"2009-05-21","publish_status":"0","recid":"16674","relation_version_is_last":true,"title":["斜面崩壊丘陵地における自然降雨下での土壌水分動態の把握"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-05-15T18:14:39.055899+00:00"}