General study on the eruption at Shinmoedake volcano, Kirishima, in 2011
2011年雾岛新茂岳火山喷发综合研究
基本信息
- 批准号:22900001
- 负责人:
- 金额:--
- 依托单位:
- 依托单位国家:日本
- 项目类别:
- 财政年份:2010
- 资助国家:日本
- 起止时间:2010 至 2011
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
A magmatic eruption event took place at Shinmoedake (Kirishima) Volcano in January 2011, leaving about 300 years of hiatus. Three subplinian explosions occurred on 26 and 27 January, which were followed by 4-day accumulation of lava at the summit crater. Vulcanican explosions were repeated from February to April, and a series of eruptions ended with phreatic explosions which occurred in June and September 2011. This eruption event was preceded by both phreatic explosions in 2008 and 2010 and elevated seismic activity in the regions surrounding Kirishima. GPS observation indicated that significant swelling of the magma chamber which located about 6 km NW of the Shinmoedake crater had continued since the end of 2009. Deflation of the magma chamber accompanied clearly subplinian explosions and the lava accumulation in the crater. The strain-meter observation showed small increases in pressure several tens of minutes prior to the subplinian explosions. Seismic array-observation during a se … More ries of vulcanian explosions showed that volcanic tremors occurred beneath the summit crater and between it and the magma chamber, supporting magma's migration from the magma chamber to the crater. The latter was confirmed by the absolute gravity measurement at the place just above the magma chamber. Inflation of the summit area, ncrease in the shallow earthquakes and decrease in the volcanic gas emitted from the crater were observed prior to the vulcanian explosions, strongly implying sealing of the conduit top preceding the explosions. It is considered that magma mixing occurred just before the eruption event because the products of the earliest stage consisted of two magmas with different compositions. The total volume of magma erupted in this event is estimated about 25 million m3, which is about 1/3 volume of the eruption 300 years ago.During this study, we tried two times to make the eruption scenario in which sequences of eruptions are indicated, based on records of eruptions of this volcano 300 years ago and of analogous volcanoes in and outside Japan. No significant mudflows occurred in this eruption event. It is considered that the reason is that the eruption products were mainly of pumice which has high permeability of rain water. Inflation of magma chamber resumed soon after the eruptions in January 2011 and continued by the end of 2011, reaching the same level before the eruption event. It almost stopped in the beginning of 2012, suggesting a halt of the magma supply from depth. Less
2011年1月,新竹(雾岛)火山发生了岩浆喷发事件,造成了大约300年的间歇。1月26日和27日发生了三次地下爆炸,随后在山顶火山口积聚了4天的熔岩。从2月到4月,火山爆发反复发生,2011年6月和9月,一系列火山爆发以潜水式爆炸结束。在这次喷发事件之前,2008年和2010年的两次潜水爆炸以及雾岛周围地区的地震活动加剧。GPS观测显示,位于Shinmoedake陨石坑西北约6公里处的岩浆库自2009年底以来一直在持续显著膨胀。岩浆房的收缩伴随着明显的俯冲爆炸和火山口的熔岩堆积。应变计观测显示,在次平面爆炸前几十分钟,压力有小幅上升。更多的火山爆发表明,火山震动发生在山顶火山口下方及其与岩浆库之间,支持岩浆从岩浆库向火山口的迁移。后者是由岩浆房上方的绝对重力测量证实的。火山喷发前观察到峰顶区域的膨胀、浅层地震的增加和火山口喷出的火山气体的减少,这强烈暗示了火山喷发前管道顶部的密封。由于最早阶段的产物由两种不同成分的岩浆组成,因此认为岩浆混合发生在喷发事件发生之前。这次喷发的岩浆总量估计约为2500万立方米,约为300年前那次喷发的1/3。在本研究中,我们根据300年前这座火山的喷发记录以及日本国内外类似火山的喷发记录,两次尝试制作喷发场景,其中显示了喷发顺序。这次喷发没有发生明显的泥石流。认为喷发产物主要为浮石,具有较高的雨水渗透性。2011年1月火山喷发后,岩浆库的膨胀很快恢复,并持续到2011年底,达到喷发前的水平。2012年初,它几乎停止了喷发,这表明岩浆供应已经停止。少
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
霧島新燃岳2011年1月26日噴火前後の地殻変動
2011年1月26日雾岛新茂岳喷发前后的地壳运动
- DOI:
- 发表时间:2011
- 期刊:
- 影响因子:0
- 作者:中尾茂・森田裕一・後藤和彦;八木原寛・平野舟一郎;ほか
- 通讯作者:ほか
新燃岳・享保噴火における被災状況について
关于新茂岳/巨峰喷发造成的损失
- DOI:
- 发表时间:2011
- 期刊:
- 影响因子:0
- 作者:Fujii;Y.;K. Satake;S. Sakai;M. Shinohara;and T. Kanazawa;岡崎康浩;筒井正明・小林哲夫
- 通讯作者:筒井正明・小林哲夫
MT連続観測による霧島硫黄山北の比抵抗変化
通过连续 MT 观测观察雾岛 Ioyama 北部电阻率的变化
- DOI:
- 发表时间:2011
- 期刊:
- 影响因子:0
- 作者:鈴木由希・中田節也・他;板倉陽子;相澤広記・上嶋誠・橋本武志・神田径・他
- 通讯作者:相澤広記・上嶋誠・橋本武志・神田径・他
新燃岳の噴火シナリオ(2)
新茂岳喷发情景(2)
- DOI:
- 发表时间:2011
- 期刊:
- 影响因子:0
- 作者:Shinohara;M.;T. Yamada;K. Nakahigashi;S. Sakai;K. Mochizuki;K. Uehira;Y. Ito;R. Azuma;Y. Kaiho;T. No;H. Shiobara;R. Hino;Y. Murai;H. Yakiwara;T. Sato;Y. Machida;T. Shinbo;T. Isse;H. Miyamachi;K Obana;N. Takahashi;S. Kodaira;Y. Kaned;植木貞人・大久保修平・大島弘光・他;中田節也
- 通讯作者:中田節也
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NAKADA Setsuya其他文献
NAKADA Setsuya的其他文献
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{{ truncateString('NAKADA Setsuya', 18)}}的其他基金
RESEARCH ON VOLCANIC ACTIVITY IN THE NORTHERN MARIANAS
北马里亚纳群岛火山活动研究
- 批准号:
19403003 - 财政年份:2007
- 资助金额:
-- - 项目类别:
Grant-in-Aid for Scientific Research (B)
Geological and petrological study on phreatomagmatic explosions of the Miyakejima eruption in 2000
2000年三宅岛喷发的岩浆爆发地质和岩石学研究
- 批准号:
16340166 - 财政年份:2004
- 资助金额:
-- - 项目类别:
Grant-in-Aid for Scientific Research (B)
Petrological research on magma behavior during volcanic eruptions
火山喷发过程中岩浆行为的岩石学研究
- 批准号:
12304033 - 财政年份:2000
- 资助金额:
-- - 项目类别:
Grant-in-Aid for Scientific Research (A)
PETROLOGICAL STUDY ON MAGMA STORAGE AND MOVEMENT IN THE UPPER CRUST
上地壳岩浆储存和运动的岩石学研究
- 批准号:
09640565 - 财政年份:1997
- 资助金额:
-- - 项目类别:
Grant-in-Aid for Scientific Research (C)
Origin of phenocrysts and eruption mechanism -in case of Unzen Volcano-.
斑晶的起源和喷发机制-以云仙火山为例-。
- 批准号:
07454134 - 财政年份:1995
- 资助金额:
-- - 项目类别:
Grant-in-Aid for Scientific Research (B)
Research on eruption phenomena of dacite magma
英安岩浆喷发现象研究
- 批准号:
04452083 - 财政年份:1992
- 资助金额:
-- - 项目类别:
Grant-in-Aid for General Scientific Research (B)
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