{"_buckets": {"deposit": "2b3eecfb-bb96-4b8b-a2b7-18a691007d5c"}, "_deposit": {"id": "4156", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4156"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004156", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2006-05"}, "bibliographicIssueNumber": "6", "bibliographicPageEnd": "566", "bibliographicPageStart": "549", "bibliographicVolumeNumber": "68", "bibliographic_titles": [{"bibliographic_title": "BULLETIN OF VOLCANOLOGY", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The vesiculation of magma during the 1983 eruption of Miyakejima Volcano, Japan, is discussed based on systematic investigations of water content, vesicularity, and bubble size distribution for the products. The eruption is characterized by simultaneous lava effusion and explosive sub-plinian (\u0027dry\u0027) eruptions with phreatomagmatic (\u0027wet\u0027) explosions. The magmas are homogeneous in composition (basaltic andesite) and in initial water content (H2O = 3.9 +/- 0.9 wt%), and residual groundmass water contents for all eruption styles are low (H2O \u0026lt; 0.4 wt%) suggestive of extensive dehydration of magma.\nFor the scoria erupted during simultaneous \u0027dry\u0027 and \u0027wet\u0027 explosive eruptions, inverse correlation was observed between vesicularity and residual water content. This relation can be explained by equilibrium exsolution and expansion of ca. 0.3 wt% H2O at shallow level with different times of quenching, and suggests that each scoria with different vesicularity, which was quenched at a different time, provides a snapshot of the vesiculation process near the point of fragmentation. The bubble size distribution (BSD) varies systematically with vesicularity, and total bubble number density reaches a maximum value at vesicularity Phi similar to 5. At Phi similar to 0.5, a large number of bubbles are connected with each other, and the average thickness of bubble walls reaches the minimum value below which they would rupture. These facts suggest that vesiculation advanced by nucleation and growth of bubbles when Phi \u0026lt; 0.5, and then by expansion of large bubbles with coalescence of small ones for Phi \u0026gt; 0.5, when bubble connection becomes effective.\nLow vesicularity and low residual water content of lava and spatter (Phi \u0026lt; 0.1 H2O \u0026lt; 0.1 wt%), and systematic decrease in bubble number density from scoria through spatter to lava with decrease in vesicularity suggest that effusive eruption is a consequence of complete degassing by bubble coalescence and separation from magma at shallow levels when magma ascent rate is slow.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "SPRINGER", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1007/s00445-005-0029-2"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0258-8900", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "T Shimano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "S Nakada", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Vesiculation path of ascending magma in the 1983 and the 2000 eruptions of Miyakejima volcano, Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Vesiculation path of ascending magma in the 1983 and the 2000 eruptions of Miyakejima volcano, Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4156", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4156", "relation": {}, "relation_version_is_last": true, "title": ["Vesiculation path of ascending magma in the 1983 and the 2000 eruptions of Miyakejima volcano, Japan"], "weko_shared_id": -1}