Permeability Models for Magma Flow through the Earth's Mantle: A Lie Group Analysis
Keyword(s):
The migration of melt through the mantle of the Earth is governed by a third-order nonlinear partial differential equation for the voidage or volume fraction of melt. The partial differential equation depends on the permeability of the medium which is assumed to be a function of the voidage. It is shown that the partial differential equation admits, as well as translations in time and space, other Lie point symmetries provided the permeability is either a power law or an exponential law of the voidage or is a constant. A rarefactive solitary wave solution of the partial differential equation is derived in the form of a quadrature for the exponential law for the permeability.
2010 ◽
Vol 12
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pp. 125-131
2020 ◽
Vol 5
(1)
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pp. 1-7
2013 ◽
Vol 5
(04)
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pp. 407-422
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2014 ◽
Vol 9
(8)
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pp. 238-248
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1999 ◽
Vol 169
(1-2)
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pp. 81-88
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