Modeling the evolution of three-layered stokes flow and some geophysical applications

Автор: Park Vladimir Vasilyevich

Журнал: Вычислительная механика сплошных сред @journal-icmm

Статья в выпуске: 3 т.11, 2018 года.

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Analytical investigation and numerical modeling have been fulfilled to study the evolution of Stokes flow in a computational domain that consists of thick viscous layer overlaid by a thin multi-layered viscous sheet. We obtain an analytical solution and explore the short- and long-time evolution of the velocity field and layer boundaries. Linear analysis of small perturbations reveals the evolution of the flow to be multistage. It consists of several stages with typical time scales. During the evolution the inversion of layer boundary relief and transformation of the velocity field from one-layered to three-layered structure happen. These time scales are evaluated with respect to geometrical and physical parameters of layers. We fulfill numerical modeling of the evolution of the velocity field and layer boundaries. For this purpose we apply the two-dimensional coupled model that consists of the Stokes equations describing the flow in the layer and the Reynolds equations describing the flow in the sheet...

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Coupled model, stokes equations, reynolds equations, small parameter method, finite element method, lithosphere thinning

Короткий адрес: https://sciup.org/143166058

IDR: 143166058   |   DOI: 10.7242/1999-6691/2018.11.3.21

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