Numerical resolution of a mono-disperse model of bubble growth in magmas

被引:10
|
作者
Forestier-Coste, L. [1 ,2 ]
Mancini, S. [1 ,2 ,3 ]
Burgisser, A. [3 ]
James, F. [1 ,2 ]
机构
[1] Univ Orleans, MAPMO UMR 7349, Federat Denis Poisson FR 2964, F-45067 Orleans, France
[2] CNRS, F-45067 Orleans, France
[3] Univ Tours, Univ Orleans, CNRS INSU, Inst Sci Terre Orleans, F-45071 Orleans 2, France
关键词
Coupled ode system and diffusion equation; Mass preserving scheme; Bubble growth; DYNAMICS; DECOMPRESSION; MELTS;
D O I
10.1016/j.apm.2012.01.031
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Growth of gas bubbles in magmas may be modeled by a system of differential equations that account for the evolution of bubble radius and internal pressure and that are coupled with an advection-diffusion equation defining the gas flux going from magma to bubble. This system of equations is characterized by two relaxation parameters linked to the viscosity of the magma and to the diffusivity of the dissolved gas, respectively. Here, we propose a numerical scheme preserving, by construction, the total mass of water of the system. We also study the asymptotic behavior of the system of equations by letting the relaxation parameters vary from 0 to infinity. and show the numerical convergence of the solutions obtained by means of the general numerical scheme to the simplified asymptotic limits. Finally, we validate and compare our numerical results with those obtained in experiments. (C) 2012 Elsevier Inc. All rights reserved.
引用
收藏
页码:5936 / 5951
页数:16
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