A review of laboratory and numerical modelling in volcanology
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Published:2018-04-27
Issue:2
Volume:9
Page:531-571
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ISSN:1869-9529
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Container-title:Solid Earth
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language:en
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Short-container-title:Solid Earth
Author:
Kavanagh Janine L., Engwell Samantha L., Martin Simon A.ORCID
Abstract
Abstract. Modelling has been used in the study of volcanic systems for more than 100 years, building upon the approach first applied by Sir James Hall in 1815. Informed by observations of volcanological phenomena in nature, including eye-witness accounts of eruptions, geophysical or geodetic monitoring of active volcanoes, and geological analysis of ancient deposits, laboratory and numerical models have been used to describe and quantify volcanic and magmatic processes that span orders of magnitudes of time and space. We review the use of laboratory and numerical modelling in volcanological research, focussing on sub-surface and eruptive processes including the accretion and evolution of magma chambers, the propagation of sheet intrusions, the development of volcanic flows (lava flows, pyroclastic density currents, and lahars), volcanic plume formation, and ash dispersal. When first introduced into volcanology, laboratory experiments and numerical simulations marked a transition in approach from broadly qualitative to increasingly quantitative research. These methods are now widely used in volcanology to describe the physical and chemical behaviours that govern volcanic and magmatic systems. Creating simplified models of highly dynamical systems enables volcanologists to simulate and potentially predict the nature and impact of future eruptions. These tools have provided significant insights into many aspects of the volcanic plumbing system and eruptive processes. The largest scientific advances in volcanology have come from a multidisciplinary approach, applying developments in diverse fields such as engineering and computer science to study magmatic and volcanic phenomena. A global effort in the integration of laboratory and numerical volcano modelling is now required to tackle key problems in volcanology and points towards the importance of benchmarking exercises and the need for protocols to be developed so that models are routinely tested against real world data.
Publisher
Copernicus GmbH
Subject
Paleontology,Stratigraphy,Earth-Surface Processes,Geochemistry and Petrology,Geology,Geophysics,Soil Science
Reference292 articles.
1. Abdelmalak, M. M., Mourgues, R., Galland, O., and Bureau, D.: Fracture mode analysis and related surface deformation during dyke intrusion: Results from 2D experimental modelling, Earth Planet. Sc. Lett., 359–360, 93–105, https://doi.org/10.1016/j.epsl.2012.10.008, 2012. 2. Abdelmalak, M. M., Bulois, C., Mourgues, R., Galland, O., Legland, J. B., and Gruber, C.: Description of new dry granular materials of variable cohesion and friction coefficient: Implications for laboratory modeling of the brittle crust, Tectonophysics, 684, 39–51, https://doi.org/10.1016/j.tecto.2016.03.003, 2016. 3. Ampferer, O.: Uber das bewegungsbild von falten-gebirgen, Jahrb. der Geol. Reichsanstalt, 56, 539–662, 1906. 4. Andrews, B. J. and Manga, M.: Effects of topography on pyroclastic density current runout and formation of coignimbrites, Geology, 39, 1099–1102, https://doi.org/10.1130/G32226.1, 2011. 5. Andrews, B. J. and Manga, M.: Experimental study of turbulence, sedimentation, and coignimbrite mass partitioning in dilute pyroclastic density currents, J. Volcanol. Geoth. Res., 225–226, 30–44, https://doi.org/10.1016/j.jvolgeores.2012.02.011, 2012.
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