Explore the words cloud of the DYNAVOLC project. It provides you a very rough idea of what is the project "DYNAVOLC" about.
The following table provides information about the project.
Coordinator |
LUDWIG-MAXIMILIANS-UNIVERSITAET MUENCHEN
Organization address contact info |
Coordinator Country | Germany [DE] |
Total cost | 243˙352 € |
EC max contribution | 243˙352 € (100%) |
Programme |
1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility) |
Code Call | H2020-MSCA-IF-2017 |
Funding Scheme | MSCA-IF-GF |
Starting year | 2018 |
Duration (year-month-day) | from 2018-04-01 to 2021-06-16 |
Take a look of project's partnership.
# | ||||
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1 | LUDWIG-MAXIMILIANS-UNIVERSITAET MUENCHEN | DE (MUENCHEN) | coordinator | 243˙352.00 |
2 | ROYAL INSTITUTION FOR THE ADVANCEMENT OF LEARNING MCGILL UNIVERSITY | CA (MONTREAL) | partner | 0.00 |
The growing number of inhabitants, tourists, and economic activities near volcanoes, require adequate volcanic hazard-assessment and -mitigation plans to guide decision-making in the case of volcanic unrest. Especially the Campi flegrei caldera (Naples, Italy) is a significant threat to the EU, as a large scale eruption is foreseen within the coming century. Accurate forecasting of volcanic behaviour is hampered by a lack of understanding of the magmas transport properties. Changes in viscosity due to the interaction between primitive and evolved magmas are documented to trigger volcanic eruptions across the globe. In the past decades, two key transition zones in magma rheology were identified that separate effusive from explosive and eruptible from non-eruptible magmas: 1) solidification through crystallization and 2) fluidization through vesiculation.
Even though these transition zones are identified and the computation capacities to forecast volcanic eruptions have grown exponentially over the past decades, none of the available computer models are able to produce coherent results and no model scenario is verified in nature. This is because predictive approaches rely on accurate rheological data, which are absent to date.
Recent technological advances, in combination with a new, interdisciplinary research approach now allow us to address this knowledge gap. Measuring the evolution of magma viscosity across the two change zones is one of the most interesting challenges at the interface between geo- and material-sciences.
This project aims to develop a systematic understanding of the evolution of rheological transition zones from magma chambers to super eruptions. The results allow more precise forecasting of volcanic eruptions and may find application in the glass and ceramic industries. The proposed research and training will set me up as an independent researcher who can lead a cutting-edge research group bridging the gap between geo- and material-sciences.
year | authors and title | journal | last update |
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2019 |
S. Kolzenburg, A.G. Ryan, J.K. Russell Permeability evolution during non-isothermal compaction in volcanic conduits and tuffisite veins: Implications for pressure monitoring of volcanic edifices published pages: 115783, ISSN: 0012-821X, DOI: 10.1016/j.epsl.2019.115783 |
Earth and Planetary Science Letters 527 | 2020-01-30 |
2019 |
Amy G. Ryan, Stephan Kolzenburg, Alessandro Vona, Michael J. Heap, James K. Russell, Steven Badger A proxy for magmatic foams: FOAMGLAS®, a closed-cell glass insulation published pages: 100001, ISSN: 2590-1591, DOI: 10.1016/j.nocx.2018.100001 |
Journal of Non-Crystalline Solids: X 1 | 2020-01-30 |
2018 |
S. Kolzenburg, D. Giordano, K. U. Hess, D. B. Dingwell Shear Rate-Dependent Disequilibrium Rheology and Dynamics of Basalt Solidification published pages: , ISSN: 0094-8276, DOI: 10.1029/2018gl077799 |
Geophysical Research Letters | 2019-06-11 |
2018 |
Stephan Kolzenburg, Amy G. Ryan, and James Kelly Russell Post eruptive permeability evolution of volcanic conduits and tuffisites published pages: EGU2018-10608, ISSN: , DOI: |
Geophysical Research Abstracts Vol. 20 Vol. 20 | 2019-06-11 |
2018 |
Danilo Di Genova, Alberto Caracciolo, and Stephan Kolzenburg Measuring the degree of “nanotilisation†of volcanic glasses and theirimplications for volcanic processes published pages: , ISSN: , DOI: |
Geophysical Research Abstracts Vol. 20 | 2019-06-11 |
2018 |
Amy Ryan, Michael J. Heap, James K. Russell, Stephan Kolzenburg, and Alessandro Vona Permeability development in high porosity foams published pages: , ISSN: , DOI: |
Geophysical Research Abstracts Vol. 20 | 2019-06-11 |
2018 |
Danilo Di Genova, Alberto Caracciolo, Stephan Kolzenburg Measuring the degree of “nanotilization†of volcanic glasses: Understanding syn -eruptive processes recorded in melt inclusions published pages: , ISSN: 0024-4937, DOI: 10.1016/j.lithos.2018.08.011 |
Lithos | 2019-06-11 |
2018 |
S. Kolzenburg, J. Jaenicke, U. Münzer, D.B. Dingwell The effect of inflation on the morphology-derived rheological parameters of lava flows and its implications for interpreting remote sensing data - A case study on the 2014/2015 eruption at Holuhraun, Iceland published pages: 200-212, ISSN: 0377-0273, DOI: 10.1016/j.jvolgeores.2018.04.024 |
Journal of Volcanology and Geothermal Research 357 | 2019-06-11 |
2018 |
Stephan Kolzenburg, Daniele Giordano, Daniele Giordano, Andrea Di Muro, Andrea Di Muro, D. Dingwell, D. Dingwell Equilibrium Viscosity and Disequilibrium Rheology of a high Magnesium Basalt from Piton De La Fournaise volcano, La Reunion, Indian Ocean, France published pages: , ISSN: 1593-5213, DOI: 10.4401/ag-7839 |
Annals of Geophysics 61/Vol 61 (2018) | 2019-04-03 |
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