4.6 Article

Investigation of hot spring gas components and soil gas fluxes in Arxan Holocene volcanic field, Inner Mongolia, NE China

期刊

FRONTIERS IN EARTH SCIENCE
卷 11, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2023.1174315

关键词

dormant volcano monitoring; volcanic gas emissions; soil gas fluxes; hot spring gas components; Arxan volcanic field

向作者/读者索取更多资源

The latest research shows that the Arxan volcanic field has a unified magma system and heating channel, indicating the potential risk of eruption. The volcanic field exhibits strong hydrothermal activity and multiple gas emission sites. Measurements of gas composition and soil CO2 flux were conducted in this study, revealing high concentrations of CO2 and other gases. The soil CO2 flux of Arxan volcano is comparable to the emission level of the Iwojima volcano.
The latest research results show that there is a unified magma system and heating channel beneath the Arxan volcanic field, indicating a potential risk of eruption. The Arxan volcanic field features multiple gas emission sites (e.g., Jinjianggou hot springs and Yinjianggou hot springs) and exhibits strong hydrothermal activity. In this study, measurements of the hot spring gas composition and soil CO2 flux in the Arxan Holocene volcanic field were conducted, and the results were combined with previous research results to analyze the degassing characteristics of this region. The results show that the volcanic gases in the Arxan volcanic field are composed of 0.07%-1.09% CO2, 0.33-12 ppm CH4, 1.57-53 ppm H-2, 800-30,241 ppm He, and 1.14%-1.86% Ar. The He content in this area is notably higher than that in other dormant volcanoes in China. This difference is possibly caused by U-Th decay in the Mesozoic granodiorite and acidic volcanic rocks in the study area, which can produce substantial radiogenic He. The soil gas concentrations near the Jinjianggou and Yinjianggou hot springs are higher than those of two Holocene volcanoes. The peak CO2 concentration in the soil near the Jinjianggou hot spring can reach 35,161 ppm. The single-site soil microseepage CO2 flux in the Arxan volcanic field is 4.66-107.18 g m(-2) d(-1), and the estimated annual CO2 emission flux from the volcanic field to the atmosphere is 0.63 x 10(5) t, which also demonstrates that soil CO2 flux of Arxan volcano is comparable to the soil CO2 emission level of the Iwojima volcano.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据