{"_buckets": {"deposit": "590e88ee-754f-4b97-90da-f48a72d2d4d7"}, "_deposit": {"id": "18708", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "18708"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00018708", "sets": ["322"]}, "author_link": ["54544", "54545", "54546", "54547", "54548"], "item_10_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2011-07", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "B7", "bibliographicPageEnd": "B07205", "bibliographicPageStart": "B07205", "bibliographicVolumeNumber": "116", "bibliographic_titles": [{"bibliographic_title": "Journal of Geophysical Research: Solid Earth", "bibliographic_titleLang": "en"}]}]}, "item_10_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "1] While iron occurs predominantly in the form of Fe^2+ in the Earth\u0027s upper mantle and transition zone, Al-bearing (Mg,Fe)SiO3 perovskite (Pv), a primary mineral in the lower mantle, contains a large proportion of ferric iron (Fe^3+). It has been demonstrated that such Fe^3+ strongly affects physical and chemical properties of Pv. On the other hand, the iron substitution mechanism and valence state of iron in postperovskite (PPv) are still unclear. Here we determined the valence state of iron in PPv with changing Al^3+ content, on the basis of electron energy-loss near-edge structure spectroscopy measurements. The results show that PPv includes a small amount of Fe^3+, which is independent from the Al3+ content. This indicates that Fe^3+ in Pv and coexisting metallic iron recombine to form Fe^2+ upon phase transition from Pv to PPv in pyrolitic mantle. Such Fe^2+ partitions preferentially into (Mg,Fe)O ferropericlase (Fp), and therefore PPv is depleted in iron compared to Pv. Such a marked change in the valence state of iron and resulting iron depletion in PPv have broad implications for seismic and transport properties in the lowermost mantle. Phase transition from Pv to Fe-poor PPv occurs in a much narrower pressure range than that for a fixed iron content.", "subitem_description_language": "en", "subitem_description_type": "Abstract"}]}, "item_10_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "DOI", "subitem_identifier_uri": "http://dx.doi.org/10.1029/2010JB008179"}, {"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/20807"}]}, "item_10_publisher_32": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "John Wiley \u0026 Sons", "subitem_publisher_language": "en"}]}, "item_10_relation_11": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isVersionOf", "subitem_relation_type_id": {"subitem_relation_type_id_text": "https://doi.org/10.1029/2010JB008179", "subitem_relation_type_select": "DOI"}}]}, "item_10_rights_12": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "Copyright 2011 by the American Geophysical Union.", "subitem_rights_language": "en"}]}, "item_10_select_15": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_10_source_id_7": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0148-0227", "subitem_source_identifier_type": "PISSN"}]}, "item_1615787544753": {"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_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": "Sinmyo, Ryosuke", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "54544", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Hirose, Kei", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "54545", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Muto, Shunsuke", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "54546", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ohishi, Yasuo", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "54547", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yasuhara, Akira", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "54548", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-21"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "jgrb16835.pdf", "filesize": [{"value": "568.2 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 568200.0, "url": {"label": "jgrb16835.pdf", "objectType": "fulltext", "url": "https://nagoya.repo.nii.ac.jp/record/18708/files/jgrb16835.pdf"}, "version_id": "105c39fb-721a-4daa-9c76-1765c834e9db"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Experimental mineralogy and petrology", "subitem_subject_scheme": "Other"}, {"subitem_subject": "High-pressure behavior", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Mineral and crystal chemistry", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Reactions and phase equilibria", "subitem_subject_scheme": "Other"}, {"subitem_subject": "X-ray, neutron, and electron spectroscopy and diffraction", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "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": "The valence state and partitioning of iron in the Earth’s lowermost mantle", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "The valence state and partitioning of iron in the Earth’s lowermost mantle", "subitem_title_language": "en"}]}, "item_type_id": "10", "owner": "1", "path": ["322"], "permalink_uri": "http://hdl.handle.net/2237/20807", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2014-11-18"}, "publish_date": "2014-11-18", "publish_status": "0", "recid": "18708", "relation": {}, "relation_version_is_last": true, "title": ["The valence state and partitioning of iron in the Earth’s lowermost mantle"], "weko_shared_id": -1}