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Anomalous Diffuse CO2 Emission prior to the January 2002 Short-term Unrest at San Miguel Volcano, El Salvador, Central America

机译:中美洲萨尔瓦多圣米格尔火山2002年1月短期动荡之前的异常扩散CO2排放

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On January 16, 2002, short-term unrest occurred at San Miguel volcano. A gas-and-steamash plume rose a few hundred meters above the summit crater. An anomalous microseismicity pattern, about 75 events between 7:30 and 10:30 hours, was also observed. Continuous monitoring of CO2 efflux on the volcano started on November 24, 2001, in the attempt to provide a multidisciplinary approach for its volcanic surveillance. The background mean of the diffuse CO2 emission is about 16 g m-2 d-1, but a 17- fold increase, up to 270 g m-2 d-1, was detected on January 7, nine days before the January 2002 short-term unrest at San Miguel volcano. These observed anomalous changes on diffuse CO2 degassing could be related to either a sharp increase of CO2 pressure within the volcanic-hydrothermal system or degassing from an uprising fresh gas-rich magma within the shallow plumbing system of the volcano since meteorological fluctuations cannot explain this observed increase of diffuse CO2 emission.
机译:2002年1月16日,圣米格尔火山发生了短期动乱。一股气体和蒸汽的烟柱上升到山顶火山口上方几百米处。还观察到异常的微震模式,在7:30到10:30小时之间发生了大约75次事件。 2001年11月24日开始对火山的CO2排放进行连续监测,以期为火山监测提供多学科的方法。扩散CO2 排放的背景平均值约为16 g m-2 d-1 ,但增加了17倍,达到270 g m-2 d -1 ,是在2002年1月圣米格尔火山短期动乱发生的9天前的1月7日发现的。这些在弥散的CO2 脱气中观察到的异常变化可能与火山热液系统中CO2 压力的急剧增加或从浅水管道系统中起义的富含天然气的新鲜岩浆脱气有关。火山,因为气象波动无法解释这种观测到的弥散性CO2排放增加的现象。

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