{"_buckets": {"deposit": "189aa8b1-539c-4666-87d4-ec7231d8401f"}, "_deposit": {"id": "11699", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11699"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00011699"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Highly precise AMS radiocarbon dating of woods buried by the 10th century eruption of Baitoushan volcano(Proceedings of the 15^\u003cth\u003e Symposium on Researches Using the Tandetron AMS System at Nagoya University in 2002)"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2003-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "65", "bibliographicPageStart": "58", "bibliographicVolumeNumber": "14", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u52a0\u901f\u5668\u8cea\u91cf\u5206\u6790\u8a08\u696d\u7e3e\u5831\u544a\u66f8"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The eruption age can be determined by radiocarbon dating of wood samples that had been blighted by the volcanic eruption. The wood samples were collected from the sediment layers of the pyroclastic flow or mudflow deposits that were produced by the 10th century eruption of Baitoushan in China. The ash is referred to as the B-Tm (Baitoushan-Tomakomai) tephra, which is often found at the archaeological excavation sites in northern Japan. However, the precise age of the eruption has not been determined yet. A sample with 102 annual rings and barks was divided year by year. 35 annual rings out of the divided ones were selected for ^\u003c14\u003eC dating. This amounts to a selection of annual rings of almost every 3 years. The ^\u003c14\u003eC ages were obtained by using AMS. The ^\u003c14\u003eC ages were calibrated to calendar year by wiggle matching. The calibrated age of the outermost annual ring was 936^\u003c+8\u003e_\u003c-6\u003e cal AD. 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