{"created":"2023-07-27T06:57:55.743674+00:00","id":55400,"links":{},"metadata":{"_buckets":{"deposit":"cd824c9a-482f-4458-952d-cd699f41ef62"},"_deposit":{"created_by":18,"id":"55400","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"55400"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00055400","sets":["934:935:937"]},"author_link":["16147","15203","15726","15234","15233","99976","60881","164","15698","99961","99963","16145","15225","134"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-07-25","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"4","bibliographicPageEnd":"214","bibliographicPageStart":"199","bibliographicVolumeNumber":"58","bibliographic_titles":[{"bibliographic_title":"地球科学"},{"bibliographic_title":"Earth Science","bibliographic_titleLang":"en"}]}]},"item_4_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Wakimoto, Rie"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Tazaki, Kazue"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"Nawatani, Naoko"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Ikeda, Yorimasa"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Imai, Shigeo"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Sato, Kazuhiro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Okuno, Masayuki"}],"nameIdentifiers":[{},{}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"大島紬は使用する泥田の状態により,染色の仕上りが異なると言われている.本研究では,現在使用中の泥田,現在は使われていない旧泥田,来期使用のために一年間休閑中の泥田の泥について鉱物学的,微生物学的特徴を検討した.3つの泥田のEh,DOは,ともに休閑中の田で最も還元状態を示した.泥の中には石英,長石類の他に鉄酸化物や鉄に富むクロライト,バーミキュライト,雲母類粘土鉱物,カオリン鉱物などの粘土鉱物が確認された.一年休閑させている泥田の泥と現在使用中の泥田の泥の総Fe量はともに多く,鉄酸化物や粘土鉱物中に含まれている.一方,有機成分は,現在使用中の泥田で最も高く,この結果は光学顕微鏡観察および偏性嫌気性細菌培養により,多種多様の微生物が観察された事と一致する.また,偏性嫌気性細菌培養結果は,特に鉄還元細菌と考えられる球菌,桿菌が多いことを示した.泥により黒く染色された絹糸部分からは,Fe,S,Ca,Al,Si,P,K,Mnが検出され,これらの元素は,泥およびテーチ木起源と考えられる.よって,大島紬を独特の深い黒色に染色する泥田の条件として,泥田の水質が還元状態である事,染色に重要な鉄は二価鉄である事,泥中には鉄還元細菌をはじめとする多種多様の微生物が存在し,鉄を二価に変えている事があげられる.","subitem_description_type":"Abstract"},{"subitem_description":"\"Dorozome\" is one of the traditional dying methods with muddy clays in Amami-Ohshima Island, Kagoshima, Japan. The brilliant black color of dyed \"Ohshima Tsumugi\" derives from muddy clays in Dorota (small ponds with muddy clays). In this paper, muddy clays for dying were mineralogically, chemically and microbiologically characterized. The muddy clays consist of Fe-rich chlorite, vermiculite, mica clay minerals, kaolin minerals as well as a large amount of iron hydroxides associated with high P2O5, N, C and S contents in the muddy field. Principally, iron is a key element which constitutes not only crystalline/amorphous hydroxides iron minerals, but also clay minerals. After one year of using the muddy clays, the Eh and DO are significantly reduced in fallow field. Various microorganisms were observed in the muddy clays, such as coccus and bacillus typed bacteria and fungi. Anaerobic bacteria may contribute for reducing condition in the muddy field. The black parts of \"Ohshima Tsumugi\" contain high concentrations of S, Ca and Fe, whereas white parts without dye contain a small amount of such elements. The heavy metals are originated from both muddy clays and Rhaphiolepis umbellata. The results suggest that specific condition of iron hydroxides is an important factor for brilliant black dye under reducing condition.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域地球社会基盤学系","subitem_description_type":"Other"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00061675","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"地学団体研究会 The Association for the Geological Collaboration in Japan"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.15080/agcjchikyukagaku.58.4_199","subitem_relation_type_select":"DOI"}}]},"item_4_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.jstage.jst.go.jp/browse/agcjchikyukagaku/-char/ja"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.jstage.jst.go.jp/browse/agcjchikyukagaku/-char/ja","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"http://www.chidanken.jp/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://www.chidanken.jp/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.chidanken.jp/08_1.html"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.chidanken.jp/08_1.html","subitem_relation_type_select":"URI"}}]},"item_4_rights_23":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright © 地学団体研究会 The Association for the Geological Collaboration in Japan"}]},"item_4_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AN00141269","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0366-6611","subitem_source_identifier_type":"ISSN"},{"subitem_source_identifier":"2189-7212","subitem_source_identifier_type":"ISSN"}]},"item_4_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"脇元, 理恵"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"田崎, 和江"}],"nameIdentifiers":[{},{},{}]},{"creatorNames":[{"creatorName":"縄谷, 奈緒子"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"池田, 頼正"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"今井, 茂雄"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"佐藤, 一博"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"奥野, 正幸"}],"nameIdentifiers":[{},{},{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2021-07-26"}],"displaytype":"detail","filename":"SC-PR-TAZAKI-K-199.pdf","filesize":[{"value":"5.4 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-TAZAKI-K-199.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/55400/files/SC-PR-TAZAKI-K-199.pdf"},"version_id":"dce56a29-4537-4c98-8905-14a886a432e8"}]},"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":"奄美大島紬を染める泥の特性","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"奄美大島紬を染める泥の特性"},{"subitem_title":"Characterization of muddy clays for \"Ohshima Tsumugi\" using traditional dye method","subitem_title_language":"en"}]},"item_type_id":"4","owner":"18","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2021-07-26"},"publish_date":"2021-07-26","publish_status":"0","recid":"55400","relation_version_is_last":true,"title":["奄美大島紬を染める泥の特性"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T15:10:22.202978+00:00"}