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Spatial and Temporal Analysis of Temperature and Gaseous Emission Inside a Gallery in An Active Volcanic Island (Tenerife, Canary Islands)

机译:活跃火山岛(TEGERIFE,GINARY ISLANDS)中的温度和气态排放的空间和时间分析

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摘要

In Tenerife there are a vast number of sub-horizontal blind water mines, called "galleries". Seven air and soil temperatures and CO2 concentration profiles in air were carried out inside the Rio de Guia gallery (hereinafter RdG). An anomalous stable maximum temperature point (hereinafter MTP) was found around 2000 m from the entrance. During the warm period, a clear CO2 stagnation was detected before MTP, showing concentrations up to 14,000 ppm. In order to study gas emission and its dynamics inside the gallery, four stations were deployed around MTP. All stations recorded air and soil temperatures, and CO2 and Rn concentration in air from November 2009 to January 2011. After analyzing this dataset, it was possible to characterize the influence of MTP. This thermal anomaly divided the gallery into two sections. In the cold period, the outer section located outwards from MTP became colder while the inner section warmed up owing to a less heat transfer into the deepest part of the gallery. There were several short periods when variations in barometric pressure created an advection movement that was able to temporally change the gas behavior inside the gallery. Two soil gas samples were taken around MTP and their delta C-13 (CO2) ratios suggested a magmatic origin. All data were combined to create a model for the gas and thermal dynamics inside the gallery. This model, together with identification of background levels in each parameter, allows to identify any anomalous signal that could be elated with changes in volcanic activity.
机译:在特内里费岛上有大量的潜水盲水地,称为“画廊”。在Rio de Guia Gallery(下文中的RDG)内进行空气中的七个空气和土壤温度和CO2浓度谱。距入口处约2000米的异常稳定的最大温度点(下文称为MTP)。在温暖时期,在MTP之前检测到明确的CO2停滞,显示出高达14,000ppm的浓度。为了在画廊内研究气体排放及其动力学,在MTP周围部署了四个站点。从2009年11月到2011年1月,所有工作台录制了空气和土壤温度,CO2和RN浓度。在分析了这个数据集后,可以表征MTP的影响。该热异常将图库分为两部分。在寒冷的时期,从MTP向外的外部部分变得更冷,而内部部分由于进入画廊最深部分的热传递而被加热。当气压的变化产生了一个流动的平流运动时,有几个短时间内,能够在空间上改变画廊内的气体行为。在MTP周围拍摄了两种土壤气体样品,其Delta C-13(CO 2)比率提出了岩石突发。组合所有数据以创建库内的气体和热动力学模型。该模型以及每个参数中的背景水平的识别,允许识别可以在火山活动的变化中亮起的任何异常信号。

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