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Monitoring methane emission of mud volcanoes by seismic tremor measurements: A pilot study

机译:通过地震颤动监测泥火山的甲烷排放:一项初步研究

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A new approach for estimating methane emission at mud volcanoes is here proposed based on measurements of the seismic tremor on their surface. Data obtained at the Dashgil mud volcano in Azerbaijan reveal the presence of energy bursts characterized by well-determined features (i.e. waveforms, spectra and polarization properties) that can be associated with bubbling at depth. Counting such events provides a possible tool for monitoring gas production in the reservoir, thus minimizing logistic troubles and representing a cheap and effective alternative to more complex approaches. Specifically, we model the energy bursts as the effect of resonant gas bubbles at depth. This modelling allows to estimate the dimension of the bubbles and, consequently, the gas outflow from the main conduit in the assumption that all emissions from depth occur by bubble uprising. The application of this model to seismic events detected at the Dashgil mud volcano during three sessions of measurements carried out in 2006 and 2007 provides gas flux estimates that are in line with those provided by independent measurements at the same structure. This encouraging result suggests that the one here proposed could be considered a new promising, cheap and easy to apply tool for gas flux measurements in bubbling gas seepage areas.
机译:在此提出了一种基于泥火山表面甲烷地震测量的估算甲烷排放的新方法。在阿塞拜疆的达什吉尔泥火山上获得的数据揭示了能量爆发的存在,这些能量爆发具有确定的特征(即波形,光谱和极化特性),这些特征可能与深度起泡有关。对此类事件进行计数为监视储层中的天然气产量提供了一种可能的工具,从而最大程度地减少了后勤问题,并为更复杂的方法提供了一种廉价而有效的替代方法。具体来说,我们将能量爆发建模为深处共振气泡的影响。该模型允许估计气泡的尺寸,并由此估计主管道中的气体流出量,前提是所有深度的排放都是通过气泡上升而产生的。将该模型应用于在2006年和2007年进行的三次测量期间在达什吉尔泥火山中检测到的地震事件,所提供的气体通量估算值与在相同结构处的独立测量结果相符。这一令人鼓舞的结果表明,这里提出的方法可以被认为是一种新的有前途的,廉价的且易于应用的工具,用于在冒泡的气体渗流区域进行气体通量测量。

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