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Record Search Query:
[Personnel: Last_Name='MASTIN', Middle_Name='G.', First_Name='LARRY']
Conflow: A numerical program for conduit flow and thermodynamics
Entry ID: USGS_CONFLOW
Summary
Abstract:
Conflow is a model that calculates flow properties (pressure, vesicularity, and
some 35 other parameters) as a function of vertical position within a volcanic conduit during a steady-state eruption. The model idealizes the magma-gas mixture as a single homogeneous fluid and calculates gas exsolution under the assumption of equilibrium conditions. These are the same assumptions on which classic conduit models (e.g. Wilson and Head, 1981) have been based. They are most appropriate when applied to eruptions of rapidly ascending magma (basaltic lava-fountain eruptions, and Plinian or sub-Plinian eruptions of intermediate or silicic magmas) that contains abundant nucleation sites (microlites, for example) for bubble growth. The program runs on Windows-based PCs running Windows 95 or later.
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Service Citation
Service Keywords
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Use Constraints
Please cite service providers, Larry G. Mastin (USGS) and Mark S. Ghiorso
(University of Washington).
Ancillary Keywords
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Distribution Media
Personnel
Publications/References
Mastin, L. G. and M. S. Ghiorso, 2000, A Numerical Program for Steady-State
Flow of Magma-Gas Mixtures Through Vertical Eruptive Conduits: U.S. Geological Survey Open-File Report 00209, &http://vulcan.wr.usgs.gov/Projects/Mastin/Publications/OFR00-209/fr... l&.
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