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Part 1: Document Description
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Citation |
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Title: |
Replication data for: Experimental analysis of bubble-driven magma motion in the conduit, for persistently active, open-vent volcanoes |
Identification Number: |
doi:10.21979/N9/Q9HFBE |
Distributor: |
DR-NTU (Data) |
Date of Distribution: |
2019-06-24 |
Version: |
1 |
Bibliographic Citation: |
Pansino, Stephen Gregory, 2019, "Replication data for: Experimental analysis of bubble-driven magma motion in the conduit, for persistently active, open-vent volcanoes", https://doi.org/10.21979/N9/Q9HFBE, DR-NTU (Data), V1 |
Citation |
|
Title: |
Replication data for: Experimental analysis of bubble-driven magma motion in the conduit, for persistently active, open-vent volcanoes |
Identification Number: |
doi:10.21979/N9/Q9HFBE |
Authoring Entity: |
Pansino, Stephen Gregory (Nanyang Technological University) |
Software used in Production: |
none |
Grant Number: |
Supported by US Department of Education–Fund for the Improvement of Postsecondary Education, ATLANTIS program |
Grant Number: |
Contribution number 337 |
Distributor: |
DR-NTU (Data) |
Access Authority: |
Pansino Stephen Gregory |
Depositor: |
Pansino Stephen Gregory |
Date of Deposit: |
2018-11-26 |
Holdings Information: |
https://doi.org/10.21979/N9/Q9HFBE |
Study Scope |
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Keywords: |
Earth and Environmental Sciences, Earth and Environmental Sciences, bubble-driven liquid motion, persistent degassing, lava lakes |
Abstract: |
These are the video files for analogue experiments of bubble-driven magma motion, for persistently degassing lava lakes. In the videos, gas is fluxed up through a tube of initially stagnant liquid. The video files have the naming convention of gas flux (mL/min) followed by liquid viscosity (mPa*s). At the beginning of each experiment, I placed food dye at the top surface of the liquid, which acted as a tracer for liquid motion. I measured the dye return flow velocity, as well as the gas fraction in the tube, and bubble size and velocities. In some videos (with dark golden syrup as the liquid), the dye is difficult to see; however, the dye was more evident in person. These experiments are used to deduce how fast magma convects in a confined conduit, depending on the gas flux and magma rheology. |
Kind of Data: |
videos (.wmv) |
Methodology and Processing |
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Sources Statement |
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Data Access |
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Other Study Description Materials |
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Related Publications |
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Citation |
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Identification Number: |
10.1007/s00445-019-1339-0 |
Bibliographic Citation: |
Pansino, S., Calder, E. S., & Menand, T. (2019). Experimental analysis of bubble-driven magma motion in the conduit, for persistently active, open-vent volcanoes. Bulletin of Volcanology, 81(12), 75. |
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1800mLmin 1mPas 2.wmv |
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2300mLmin 180mPas.wmv |
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3400mLmin 180mPas.wmv |
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3500mLmin 1mPas 1.wmv |
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4500mLmin 180mPas.wmv |
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800mLmin 180mPas.wmv |
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800mLmin 1mPas 1.wmv |
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