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Quantification of the Mass Flux of H _2O Gas (Steam) at Three Active Volcanoes Using Thermal Infrared Imagery

机译:使用热红外图像定量分析三个活火山上H _2O气体(蒸汽)的质量通量

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摘要

We apply a measurement technique that utilizes thermal video of vapor-dominated volcanic plumes to estimate the H _2O gas flux at three degassing volcanoes. Results are compared with H _2O flux measurements obtained using other methods to verify the thermal camera-derived values. Our estimation of the H _2O emission rate is based on the mass and energy conservation equations. H _2O flux is quantified by extracting the temperature and width of the gas plume from the thermal images, calculating the transit velocity of the gas plume from the thermal video, and combining these results with atmospheric parameters measured on-site. These data are then input into the equations for conservation of mass and energy. Selected volcanoes for this study were Villarrica in Chile, Stromboli in Italy, and Santa Ana in El Salvador. H _2O fluxes estimated from the thermal imagery were 38-250 kg s ~(-1) at Villarrica, 4. 5-14 kg s ~(-1) for Stromboli's Central Crater, and 168-219 kg s ~(-1) at Santa Ana. These compare with H _2O flux values estimated by other methods of 73-220, 3-70 and 266 kg s ~(-1), at the three volcanoes, respectively. The good agreement between thermal image-derived results and those estimated by other methods seem to validate this method.
机译:我们应用了一种测量技术,该技术利用了以蒸气为主的火山羽的热视频来估算三个脱气火山处的H _2O气体通量。将结果与使用其他方法获得的H _2O通量测量结果进行比较,以验证热像仪得出的值。我们对H _2O排放速率的估算基于质量和能量守恒方程。通过从热图像中提取出气体羽流的温度和宽度,从热图像中计算出气体羽流的传播速度,并将这些结果与现场测量的大气参数相结合,可以对H _2O通量进行量化。然后将这些数据输入到方程中,以节省质量和能量。本研究选择的火山是智利的比利亚里卡,意大利的斯特龙博利和萨尔瓦多的圣安娜。根据热像仪估计的H _2O通量在比利亚里卡(Villarrica)为38-250 kg s〜(-1),对于斯特龙博利中央火山口为5-14 kg s〜(-1),以及168-219 kg s〜(-1)在圣安娜。这些分别与在其他三个火山处通过其他方法估算的H _2O通量值73-220、3-70和266 kg s〜(-1)比较。热图像得出的结果与其他方法估计的结果之间的良好一致性似乎证明了该方法的有效性。

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