Combined model of conduit flow and eruption cloud for prediction of transition of eruption style
| Project/Area Number |
21340123
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Solid earth and planetary physics
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| Research Institution | The University of Tokyo |
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Principal Investigator |
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| Co-Investigator(Renkei-kenkyūsha) |
SUZUKI Yujiro 東京大学, 地震研究所, 助教 (30392939)
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| Project Period (FY) |
2009 – 2011
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| Project Status |
Completed (Fiscal Year 2011)
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| Budget Amount *help |
¥14,040,000 (Direct Cost: ¥10,800,000、Indirect Cost: ¥3,240,000)
Fiscal Year 2011: ¥5,330,000 (Direct Cost: ¥4,100,000、Indirect Cost: ¥1,230,000)
Fiscal Year 2010: ¥5,330,000 (Direct Cost: ¥4,100,000、Indirect Cost: ¥1,230,000)
Fiscal Year 2009: ¥3,380,000 (Direct Cost: ¥2,600,000、Indirect Cost: ¥780,000)
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| Keywords | 火山現象 / 火山 / 流体 / 計算物理 / 噴火推移予測 / 減災 / 火山物理 / マグマ上昇 / 数値計算 / 火山噴煙 |
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| Research Abstract |
We have developed a 1-dimensional(1D) 2-phase conduit flow model and analyzed the stability of steady lava dome eruptions. Through this analysis, we have revealed the transition conditions from lava dome eruptions to explosive eruptions in response to pressure change at magma chamber. We have also investigated how the eruption conditions(pressure and velocity) at the vent depend on the crater shape during explosive eruptions on the basis of the quasi-1D conduit flow model. These results of eruption conditions at the vent based on the quasi-1D conduit flow model have been used as the vent conditions for the 3-dimensional eruption cloud model. As a result we have succeeded in predicting the condition for pyroclastic flow to generate(i. e., column collapse condition) during explosive eruptions.
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Report
(4 results)
Research Products
(54 results)
