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- W2189310464 abstract "considered. There are four possible axi-symmetric patterns of the motion depending on the location of lighter fluid and the retraction of either light or heavy magmas. It is possible that light magma ascends in the middle or in the peripheral part of the conduit and the opposite ‐ heavy magma sinks in the peripheral or central part of the conduit. Light magma can carry upwards some part of heavy magma or heavy magma can bring downward some light magma. In the first case all gas will be transported to the surface, in the second case some gas will be recycled. The model based on mass conservation and Navier-Stokes equations was simplified to a system of two transcendent equations, relating the radius of the fluids contact and pressure gradient via the density ratio of the fluids. We aimed to figure out the dependence of chamber pressure and magma discharge for a fixed length of the conduit. The obtained solutions are non-unique and refer to different possible states of the flow." @default.
- W2189310464 created "2016-06-24" @default.
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- W2189310464 date "2011-01-01" @default.
- W2189310464 modified "2023-09-27" @default.
- W2189310464 title "Magmatic convection in a volcano conduit." @default.
- W2189310464 hasPublicationYear "2011" @default.
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