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- W2285107665 abstract "Miyake volcano began to erupt on 8 July 2000. Its SO2 emission amounted to a maximum 6×10 4 ton per day, which is equivalent to the total anthropogenic emission in northeast Asia and is 20 times larger than that of Japan. It has then decreased gradually but remains at a level of 10 4 ton per day even now. Here airborne volatile-component partitioning among gas, aerosols and raindrops caused by the volcanic effluents and evidence of its change were investigated by continuous observation of aerosols, together with gas and precipitation measurements, on a prominent mountain ridge and from analysis based on a multicomponent thermodynamic equilibrium model. The volcanic SO2 is converted to sulphate aerosols in the atmospheric reactions, and both cause environmental acidification. On the other hand, the abundant sulphate changes the thermodynamic equilibrium of volatile NO3 - , Cl - , NH4 + components between" @default.
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- W2285107665 date "2004-06-04" @default.
- W2285107665 modified "2023-09-28" @default.
- W2285107665 title "Change Of Aerosol And Precipitation In TheMid Troposphere Over Central Japan Caused ByMiyake Volcano Effluents" @default.
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- W2285107665 doi "https://doi.org/10.2495/air040151" @default.
- W2285107665 hasPublicationYear "2004" @default.
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