Lame's problem of gravitational viscoelasticity - The isochemical, incompressible planet

Physics

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Viscoelasticity, Gravitational Effects, Planetary Structure, Incompressible Fluids, Hydrostatics, Elastic Deformation, Geophysical Fluids, Perturbation, Green'S Functions, Load Distribution (Forces)

Scientific paper

We consider a spherical, isochemical, incompressible, nonrotating fluid planet and study infinitesimal, quasi-static, gravitational-viscoelastic perturbations, induced by surface loads, of a hydrostatic initial state. The analytic solution to the incremental field equations and interface conditions governing the problem is derived using a formulation in terms of the isopotential incremental pressure measuring the increment of the hydrostatic initial pressure with respect to a particular level surface of the gravitational potential. This admits the decoupling of the incremental equilibrium equation from the incremental potential equation. As result, two mutually independent (4 x 4) and (2 x 2) first-order ordinary differential systems in terms of the mechanical and gravitational quantities, respectively, are obtained, whose integration is algebraically easier than that of the conventional (6 x 6) differential system. In support of various types of application, we provide transfer functions, impulse-response functions and Green's functions for the full range of incremental field quantities of interest in studies of planetary deformations.

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