Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling
Volcanic eruptions are among Earth's most perilous and influential natural occurrences. However, volcanic activity remains difficult to predict and, by extension, prepare against. Volcanism and its associated hazards are heavily influenced by the behavior of volatile compounds, such as carbon d...
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sg-ntu-dr.10356-1748142024-04-15T15:31:47Z Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling Yeo, Jeanne Simon Anthony Turner Redfern Asian School of the Environment Petrology and Fluid Processes, RWTH Aachen University Ying-Jui Hsu simon.redfern@ntu.edu.sg, ying-jui.hsu@pfp.rwth-aachen.de Earth and Environmental Sciences Volcanic degassing Volatiles Plumbing systems Magma ascent Rruptions High pressure High temperature Pinatubo Piton de la Fournaise Volcanic eruptions are among Earth's most perilous and influential natural occurrences. However, volcanic activity remains difficult to predict and, by extension, prepare against. Volcanism and its associated hazards are heavily influenced by the behavior of volatile compounds, such as carbon dioxide (CO2), water vapor (H2O), and sulfur (S), during degassing. Volcanic degassing is the process where these volatiles escape from the magmatic system into the atmosphere, significantly guiding eruption dynamics and are key to understand in improving future volcanic prediction models. Despite their importance, volcanic degassing is still poorly understood, with existing models producing conflicting results. This paper thus examines novel and lesser-studied volcanic degassing models, Sulfur_X and D-Compress, and their efficacy in explaining volatile behavior within various volcanic systems, particularly in subduction zones and mantle hot spots. Focusing on historical eruptions of Mt. Pinatubo (arc) and Piton de la Fournaise (hot spot), we analyze the volatiles' behavior using an array of published and experimental data, with an emphasis on magma ascent phases. By simulating and comparing these findings with actual eruption conditions, we aim to provide insights into the factors influencing volatile degassing during these volcanic eruptions, while validating and testing the applicability of various existing models and data sets. Bachelor's degree 2024-04-12T00:17:41Z 2024-04-12T00:17:41Z 2024 Final Year Project (FYP) Yeo, J. (2024). Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling. Final Year Project (FYP), Nanyang Technological University, Singapore. https://hdl.handle.net/10356/174814 https://hdl.handle.net/10356/174814 en application/pdf Nanyang Technological University |
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Earth and Environmental Sciences Volcanic degassing Volatiles Plumbing systems Magma ascent Rruptions High pressure High temperature Pinatubo Piton de la Fournaise Yeo, Jeanne Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
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Volcanic eruptions are among Earth's most perilous and influential natural occurrences. However, volcanic activity remains difficult to predict and, by extension, prepare against. Volcanism and its associated hazards are heavily influenced by the behavior of volatile compounds, such as carbon dioxide (CO2), water vapor (H2O), and sulfur (S), during degassing. Volcanic degassing is the process where these volatiles escape from the magmatic system into the atmosphere, significantly guiding eruption dynamics and are key to understand in improving future volcanic prediction models. Despite their importance, volcanic degassing is still poorly understood, with existing models producing conflicting results. This paper thus examines novel and lesser-studied volcanic degassing models, Sulfur_X and D-Compress, and their efficacy in explaining volatile behavior within various volcanic systems, particularly in subduction zones and mantle hot spots. Focusing on historical eruptions of Mt. Pinatubo (arc) and Piton de la Fournaise (hot spot), we analyze the volatiles' behavior using an array of published and experimental data, with an emphasis on magma ascent phases. By simulating and comparing these findings with actual eruption conditions, we aim to provide insights into the factors influencing volatile degassing during these volcanic eruptions, while validating and testing the applicability of various existing models and data sets. |
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Simon Anthony Turner Redfern |
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Simon Anthony Turner Redfern Yeo, Jeanne |
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Final Year Project |
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Yeo, Jeanne |
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Yeo, Jeanne |
title |
Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
title_short |
Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
title_full |
Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
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Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
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Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
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rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling |
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Nanyang Technological University |
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2024 |
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https://hdl.handle.net/10356/174814 |
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