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A novel and inexpensive method for measuring volcanic plume water fluxes at high temporal resolution

机译:一种用于在高时间分辨率下测量火山岩羽流水通量的新颖且廉价的方法

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摘要

© 2017 by the authors.Water vapour (H2O) is the dominant species in volcanic gas plumes. Therefore,measurements of H2O fluxes could provide valuable constraints on subsurface degassing and magmatic processes. However, due to the large and variable concentration of this species in the background atmosphere, little attention has been devoted to monitoring the emission rates of this species from volcanoes. Instead, the focus has been placed on remote measurements of SO2, which is present in far lower abundances in plumes, and therefore provides poorer single flux proxies for overall degassing conditions. Here, we present a new technique for the measurement of H2O emissions at degassing volcanoes at high temporal resolution (≈1 Hz), via remote sensing with low cost digital cameras. This approach is analogous to the use of dual band ultraviolet (UV) cameras for measurements of volcanic SO2 release, but is focused on near infrared absorption by H2O. We report on the field deployment of these devices on La Fossa crater, Vulcano Island, and the North East Crater of Mt. Etna, during which in-plume calibration was performed using a humidity sensor, resulting in estimated mean H2O fluxes of ≈15 kg·s-1 and ≈34 kg·s-1, respectively, in accordance with previously reported literature values. By combining the Etna data with parallel UV camera and Multi-GAS observations, we also derived, for the first time, a combined record of 1 Hz gas fluxes for the three most abundant volcanic gas species: H2O, CO2, and SO2. Spectral analysis of the Etna data revealed oscillations in the passive emissions of all three species, with periods spanning ≈40-175 s, and a strong degree of correlation between the periodicity manifested in the SO2 and H2O data, potentially related to the similar exsolution depths of these two gases. In contrast, there was a poorer linkage between oscillations in these species and those of CO2, possibly due to the deeper exsolution of carbon dioxide, giving rise to distinct periodic degassing behaviour.
机译:©2017作者,水蒸气(H2O)是火山气柱中的主要物种。因此,H2O通量的测量可以为地下脱气和岩浆过程提供有价值的约束。但是,由于该物种在背景大气中的浓度较大且变化不定,因此很少关注监测火山中该物种的排放速率。取而代之的是,重点放在了SO2的远程测量上,SO2的烟气丰度低得多,因此对于整体脱气条件而言,它提供的单通量代理更差。在这里,我们介绍了一种新技术,该技术可通过低成本数码相机进行遥感,以高时间分辨率(≈1Hz)在脱气火山上测量H2O排放。此方法类似于使用双波段紫外线(UV)相机测量火山中SO2的释放,但重点在于H2O吸收近红外光。我们报告了在La Fossa火山口,Vulcano岛和Mt东北火山口上这些设备的现场部署情况。根据先前报道的文献资料,Etna使用湿度传感器进行了内部校准,导致估计的平均H2O通量分别约为≈15kg·s-1和≈34kg·s-1。通过将Etna数据与平行UV相机和Multi-GAS观测值相结合,我们还首次得出了三种最丰富的火山气体:H2O,CO2和SO2的1 Hz气体通量的组合记录。 Etna数据的频谱分析显示,所有这三种物种的被动发射均发生振荡,周期约≈40-175 s,并且SO2和H2O数据中显示的周期性之间具有很强的相关性,可能与相似的析出深度有关这两种气体中的一种。相反,这些物种的振荡与CO2的振荡之间的联系较差,这可能是由于二氧化碳的更深层释放所致,从而产生了独特的周期性脱气行为。

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