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The Syabru-Bensi hydrothermal system (SBHS), located in the Nepal Himalayas, is characterized by numerous hot (>30°C) springs and the release of dry, cold (<35°C) CO 2 associated with radon-222, detailed in the companion paper. In the SBHS, CO 2 and radon fluxes on the ground vary over 5-6 orders of magnitude, reaching exceptional mean values of 100 kg m À2 d À1 and 12 Bq m À2 s À1 , respectively. This paper extends the companion paper by developing three quantitative models for the radon signature of CO 2 based on measurements of radon and radium concentrations in the spring waters and effective radium concentration of rocks and soils. The first model considers near-surface radon and CO 2 degassing from water, considered unlikely unless there exist currently unidentified large discharges of hydrothermal water. The second model considers CO 2 , arising from deeper hydrothermal sources, incorporating radon from shallow radium sources as it percolates upward toward the surface, considered more likely as a percolation depth of 100 m is sufficient to account for the observed radon discharge. The third model considers the observed peak radon concentrations in the gas zones and assumes that gaseous CO 2 can be transported from kilometer-scale depths through a fault network connected to the zones. This latter model affords the possibility that variations of physical parameters at depths associated with earthquake nucleation might be detectable at the surface. Gas-dominated transport might operate in other locations in Himalayas and elsewhere and may be an important aspect of the coupled mechanisms associated with seismically active orogens.
The Syabru-Bensi hydrothermal system (SBHS), located in the Nepal Himalayas, is characterized by numerous hot (>30°C) springs and the release of dry, cold (<35°C) CO 2 associated with radon-222, detailed in the companion paper. In the SBHS, CO 2 and radon fluxes on the ground vary over 5-6 orders of magnitude, reaching exceptional mean values of 100 kg m À2 d À1 and 12 Bq m À2 s À1 , respectively. This paper extends the companion paper by developing three quantitative models for the radon signature of CO 2 based on measurements of radon and radium concentrations in the spring waters and effective radium concentration of rocks and soils. The first model considers near-surface radon and CO 2 degassing from water, considered unlikely unless there exist currently unidentified large discharges of hydrothermal water. The second model considers CO 2 , arising from deeper hydrothermal sources, incorporating radon from shallow radium sources as it percolates upward toward the surface, considered more likely as a percolation depth of 100 m is sufficient to account for the observed radon discharge. The third model considers the observed peak radon concentrations in the gas zones and assumes that gaseous CO 2 can be transported from kilometer-scale depths through a fault network connected to the zones. This latter model affords the possibility that variations of physical parameters at depths associated with earthquake nucleation might be detectable at the surface. Gas-dominated transport might operate in other locations in Himalayas and elsewhere and may be an important aspect of the coupled mechanisms associated with seismically active orogens.
Geology is about more than just rocks and other hard objects. Fluids play a major role in shaping the surface of not just Earth but other planets and moons as well. In fact, according to Michael Manga, a geologist at the University of California, Berkeley, just about everything in Earth can be viewed as a fluid. "The atmosphere and the oceans are fluids," he explains. "Volcanoes erupt magma, which is a fluid. Water flowing through the Earth's crust-groundwater-is a fluid. Earth's mantle can be viewed as a fluid on geological timescales, even though it's a solid material." Throughout his career, Manga, who was elected to the National Academy of Sciences in 2018, has applied principles of fluid dynamics to help answer a wide range of questions in earth science: What makes volcanoes erupt explosively, how can earthquakes trigger distant volcanic eruptions, how do groundwater flows and earthquakes interact, and what goes on beneath the icy surface of moons in the outer Solar System. Finding GeophysicsAchievement runs in Manga's family. His father grew up in South Africa, the son of fruit sellers, and after immigrating to Canada and working in a steel mill, he eventually became a professor of health economics at the University of Ottawa. Manga's mother took care of the family while Manga and his brothers were growing up, but later went back to school and earned a doctorate in linguistics. Growing up in Ottawa, Ontario, Manga developed an interest in science in elementary school, when he joined the Macoun Field Naturalist Club. This club for children and teenagers meets on weekends at what is now the Canadian Museum of Nature, where adult volunteers introduce facets of nature and natural history. The club also organizes camping trips where members can study various species in the field and become comfortable in the outdoors. Manga participated in the club through high school.Perhaps due to the influence of the Macoun Club, Manga intended to study entomology when he entered McGill University in Montreal. Those plans changed following his exposure to introductory courses in his first year. Manga chose to major in the subject that he least understood: physics.
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