2017 年 IAVCEI CCVG 第 13 次火山气体研讨会的二氧化碳扩散脱气调查结果:厄瓜多尔普卢拉华圆顶复合体

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of Volcanology and Geothermal Research Pub Date : 2024-07-29 DOI:10.1016/j.jvolgeores.2024.108145
M.C. Lamberti , D. Sierra , C. Cardellini , F. Viveiros , A. Vásconez Müller , F.J. Vasconez , D.F. Narváez , C. Silva , G. Melián , S. Caliro , B.M. Kis , A. Ionescu , S. Hidalgo
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引用次数: 0

摘要

Pululahua 是一个潜在的活跃安山岩和英安岩熔岩穹丘群。本文介绍了在 2017 年国际火山学和地球内部化学协会(IAVCEI)火山气体化学委员会(CCVG)第 13 届气体研讨会期间,对 Pululahua 的二氧化碳(CO)扩散脱气进行重点调查的结果。我们的目标是采用测量一氧化碳通量和温度以及数据处理的标准方法,对一氧化碳扩散脱气进行全面调查。这些方法用于绘制测量参数的空间分布图、调查一氧化碳的来源以及量化普卢拉瓦火山勘测区域内的一氧化碳产出。我们共进行了 350 次土壤一氧化碳通量测量和 329 次土壤温度测量,并采集了 12 个气体样本进行碳同位素组成分析,这些样本围绕着建筑群中最年轻的三个圆顶。此外,还对一个热水池进行了 17 次一氧化碳通量测量。我们的研究结果表明,普卢拉华火山口底部的弥散排放物既有生物源二氧化碳,也有火山源二氧化碳。每种来源的通量大小相似,约 90% 的测量结果属于中间通量范围。碳同位素组成证实了火山二氧化碳排放的存在。弥散脱气分布凸显了环形山内较年轻圆顶周围的二氧化碳异常。我们使用统计和地质统计方法估算了 3.36 千米范围内的一氧化碳扩散排放量,得出的数值分别为 154.2 吨 d 和 126.2 吨 d。根据对土壤脱气产生的一氧化碳排放总量的地质统计量化,普卢拉华火山口的火山一氧化碳排放量估计在 59 到 97 t d 之间。
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Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador

Pululahua is a potentially active andesite and dacite lava dome complex. This paper presents the results of a survey focused on carbon dioxide (CO2) diffuse degassing at Pululahua, which was conducted during the 2017 International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) Commission of the Chemistry of Volcanic Gases (CCVG) 13th Gas Workshop. Our objective was to conduct a comprehensive investigation of CO2 diffuse degassing by employing standard methods for measuring CO2 flux and temperature, and data processing. These methods were applied to map the spatial distribution of the measured parameters, investigate the origin of CO2, and quantify the volcanic CO2 output within the surveyed area of Pululahua. We carried out a total of 350 soil CO2 flux and 329 soil temperature measurements and collected 12 gas samples for carbon isotopic composition analysis, surrounding the three youngest domes in the complex. In addition, seventeen CO2 flux measurements over a thermal water pool were performed. Our findings indicate that the diffuse emission at Pululahua's crater floor is fed by both biogenic and volcanic CO2. Fluxes from each source are similar in magnitude, with approximately 90% of the measurements falling into an intermediate flux range. The occurrence of volcanic CO2 emissions is supported by the carbon isotopic composition. Diffuse degassing distribution highlights a CO2 anomaly surrounding the younger domes within the crater. We estimated the CO2 diffuse emission using both statistical and geostatistical approaches over area of 3.36 km2, resulting in values of 154.2 t d−1 and 126.2 t d−1 respectively. Based on the geostatistical quantification of the total CO2 emission from soil degassing, Pululahua's crater volcanic CO2 contribution is estimated between 59 and 97 t d−1. Finally, the potential hazards associated with the release of cold CO2 at Pululahua's crater are also discussed.

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来源期刊
CiteScore
5.90
自引率
13.80%
发文量
183
审稿时长
19.7 weeks
期刊介绍: An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society. Submission of papers covering the following aspects of volcanology and geothermal research are encouraged: (1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations. (2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis. (3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization. (4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing. (5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts. (6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact.
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