Abstract Water and carbon dioxide are the most abundant volatile components in terrestrial magmas. As they exsolve into magmatic vapour, they promote magma buoyancy, accelerating ascent and modulating eruptive dynamics. It is commonly thought that an increase in pre-eruptive volatile content produces an increase in eruption intensity. Using a conduit model for basaltic eruptions, covering the upper 6 km of conduit, we show that for the same chamber conditions mass eruption rate is not affected by CO2content, whereas an increase in H2O up to 10 wt.% produces an increase in eruption rate of an order of magnitude. It is only when CO2is injected in the magma reservoir from an external source that the resulting pressurisation will generate a strong increase in eruption rate. Results also show that ascent velocity and fragmentation depth are strongly affected by pre-eruptive volatile contents demonstrating a link between volatile content and eruptive style. 
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                            Explosive 2018 eruptions at Kīlauea driven by a collapse-induced stomp-rocket mechanism
                        
                    
    
            Article Published: 27 May 2024 Explosive 2018 eruptions at Kīlauea driven by a collapse-induced stomp-rocket mechanism Josh Crozier, Josef Dufek, Leif Karlstrom, Kyle R. Anderson, Ryan Cahalan, Weston Thelen, Mary Benage & Chao Liang Nature Geoscience volume 17, pages572–578 (2024)Cite this article 1357 Accesses 430 Altmetric Metricsdetails Abstract Explosive volcanic eruptions produce hazardous atmospheric plumes composed of tephra particles, hot gas and entrained air. Such eruptions are generally driven by magmatic fragmentation or steam expansion. However, an eruption mechanism outside this phreatic–magmatic spectrum was suggested by a sequence of 12 explosive eruptions in May 2018 at Kīlauea, Hawaii, that occurred during the early stages of caldera collapse and produced atmospheric plumes reaching 8 km above the vent. Here we use seismic inversions for reservoir pressure as a source condition for three-dimensional simulations of transient multiphase eruptive plume ascent through a conduit and stratified atmosphere. We compare the simulations with conduit ascent times inferred from seismic and infrasound data, and with plume heights from radar data. We find that the plumes are consistent with eruptions caused by a stomp-rocket mechanism involving the abrupt subsidence of reservoir roof rock that increased pressure in the underlying magma reservoir. In our model, the reservoir was overlain by a pocket of accumulated high-temperature magmatic gas and lithic debris, which were driven through a conduit approximately 600 m long to erupt particles at rates of around 3,000 m3 s−1. Our results reveal a distinct collapse-driven type of eruption and provide a framework for integrating diverse geophysical and atmospheric data with simulations to gain a better understanding of unsteady explosive eruptions. 
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                            - PAR ID:
- 10529472
- Editor(s):
- Bahadori, Alireza
- Publisher / Repository:
- Nature Geoscience
- Date Published:
- Journal Name:
- Nature Geoscience
- Edition / Version:
- 1
- Volume:
- 17
- Issue:
- 6
- ISSN:
- 1752-0894
- Page Range / eLocation ID:
- 572 to 578
- Subject(s) / Keyword(s):
- plume dynamics geophysics eruption physics multiphase turbulence
- Format(s):
- Medium: X Size: 8.1 MB Other: pdf
- Size(s):
- 8.1 MB
- Sponsoring Org:
- National Science Foundation
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