{"created":"2022-01-27T02:39:17.354557+00:00","id":2002803,"links":{},"metadata":{"_buckets":{"deposit":"73b0c781-5c71-4775-9bce-5615179b779f"},"_deposit":{"id":"2002803","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"2002803"},"status":"published"},"_oai":{"id":"oai:u-ryukyu.repo.nii.ac.jp:02002803","sets":["1642837622505:1642837905044:1642837918880","1642838403551:1642838407312"]},"author_link":[],"item_1617186331708":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_1551255647225":"国頭マージの浸入特性に関する研究 : 土壌侵食に関連して(生産環境学科)","subitem_1551255648112":"ja"},{"subitem_1551255647225":"Infiltration Characteristics of Kunigami Maaji : In Relation to Soil Erosion (Department of Enviromental Sciences and Technology)","subitem_1551255648112":"en"}]},"item_1617186419668":{"attribute_name":"Creator","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"翁長, 謙良","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"吉永, 安俊","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"志茂, 守信","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"Onaga, Kenryo","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Yoshinaga, Anshun","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Shimo, Morinobu","creatorNameLang":"en"}]}]},"item_1617186476635":{"attribute_name":"Access Rights","attribute_value_mlt":[{"subitem_1522299639480":"open access","subitem_1600958577026":"http://purl.org/coar/access_right/c_abf2"}]},"item_1617186609386":{"attribute_name":"Subject","attribute_value_mlt":[{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"国頭マージ"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"浸入能"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"土壌侵食"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"濁度"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Knigami maaji soil"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Intake rate"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Soil erosion"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Turbidity"}]},"item_1617186626617":{"attribute_name":"Description","attribute_value_mlt":[{"subitem_description":"この研究は国頭マージ地帯における土壌侵食の土壌要因の1つである浸入のメカニズムの解明を目的としたもので, 主として散水浸入量と湛水浸入量についての実験的研究である。結果及び考察は以下の通りである。(1)散水浸入において, 湛水後の積算浸入量と時間の関係はKostiakov型の式D=CT^n(ここでD=積算浸入量, T=時間, C・n=定数)によく適合した。(2)散水浸入において, 積算浸入量は初期含水比及び降雨強度に関係なく, 60分間で約10mmであった。(3)散水浸入強度は, 試験開始後60分において, 湛水浸入強度の1/5∿1/8であった。(4)国頭マージ地帯における土壌侵食の最も大きな土壌要因は浸入特性であり, 降雨時における土壌表面でのクラスト形成が浸入量の激減に関与していることが考察された。","subitem_description_type":"Other"},{"subitem_description":"The purpose of this study is to clear the fundamental cause of soil erosion of Kunigami Maaji Soil. Rainfall infilration and ponded infiltration of Kunigami Maaji Soil were measured. The result obtained are as follows. (1) In rainfall infiltration, the relationship between cumulative infiltration after ponding and time could be expressed by the Kostiakov's type of equation (D=CTn). (2) In rainfall infiltration, cumulative infiltration was sbout 10mm after 60 minute regardless of initial water content and rainfal intensity. (3) After 60 minute rainfall infiltration rate was 1/5 to 1/8 rate that of ponded infiltration rate. (4) It was found that on Kunigami Maaji regions, the most fundamental cause of soil erosion problem is decrease of infiltration rate by crust formation on the soil surface by raindrop impact.","subitem_description_type":"Other"},{"subitem_description":"紀要論文","subitem_description_type":"Other"}]},"item_1617186643794":{"attribute_name":"Publisher","attribute_value_mlt":[{"subitem_1522300295150":"ja","subitem_1522300316516":"琉球大学農学部"}]},"item_1617186702042":{"attribute_name":"Language","attribute_value_mlt":[{"subitem_1551255818386":"jpn"}]},"item_1617186783814":{"attribute_name":"Identifier","attribute_value_mlt":[{"subitem_identifier_type":"HDL","subitem_identifier_uri":"http://hdl.handle.net/20.500.12000/3774"}]},"item_1617186920753":{"attribute_name":"Source Identifier","attribute_value_mlt":[{"subitem_1522646500366":"ISSN","subitem_1522646572813":"0370-4246"},{"subitem_1522646500366":"NCID","subitem_1522646572813":"AN00250548"}]},"item_1617186941041":{"attribute_name":"Source Title","attribute_value_mlt":[{"subitem_1522650068558":"ja","subitem_1522650091861":"琉球大学農学部学術報告"},{"subitem_1522650068558":"en","subitem_1522650091861":"The Science Bulletin of the Faculty of Agriculture. University of the Ryukyus"}]},"item_1617187056579":{"attribute_name":"Bibliographic Information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1994-12-01","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"41","bibliographicPageEnd":"277","bibliographicPageStart":"269"}]},"item_1617258105262":{"attribute_name":"Resource Type","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_1617265215918":{"attribute_name":"Version Type","attribute_value_mlt":[{"subitem_1522305645492":"VoR","subitem_1600292170262":"http://purl.org/coar/version/c_970fb48d4fbd8a85"}]},"item_1617605131499":{"attribute_name":"File","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","filename":"KJ00000161754.pdf","mimetype":"application/pdf","url":{"objectType":"fulltext","url":"https://u-ryukyu.repo.nii.ac.jp/record/2002803/files/KJ00000161754.pdf"},"version_id":"1e2c20f1-6e4d-4517-a316-c2ce35d83bca"}]},"item_title":"国頭マージの浸入特性に関する研究 : 土壌侵食に関連して(生産環境学科)","item_type_id":"15","owner":"1","path":["1642837918880","1642838407312"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-02-14"},"publish_date":"2008-02-14","publish_status":"0","recid":"2002803","relation_version_is_last":true,"title":["国頭マージの浸入特性に関する研究 : 土壌侵食に関連して(生産環境学科)"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-10-31T01:09:17.689001+00:00"}