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Nonlinear Wave Motion in Viscoelasticity and Free Surface FlowsUssembayev, Nail 24 July 2020 (has links)
This dissertation revolves around various mathematical aspects of nonlinear wave motion
in viscoelasticity and free surface flows.
The introduction is devoted to the physical derivation of the stress-strain constitutive
relations from the first principles of Newtonian mechanics and is accessible to a broad
audience. This derivation is not necessary for the analysis carried out in the rest of the
thesis, however, is very useful to connect the different-looking partial differential equations
(PDEs) investigated in each subsequent chapter.
In the second chapter we investigate a multi-dimensional scalar wave equation with
memory for the motion of a viscoelastic material described by the most general linear
constitutive law between the stress, strain and their rates of change. The model equation is
rewritten as a system of first-order linear PDEs with relaxation and the well-posedness of
the Cauchy problem is established.
In the third chapter we consider the Euler equations describing the evolution of a perfect,
incompressible, irrotational fluid with a free surface. We focus on the Hamiltonian
description of surface waves and obtain a recursion relation which allows to expand the
Hamiltonian in powers of wave steepness valid to arbitrary order and in any dimension. In
the case of pure gravity waves in a two-dimensional flow there exists a symplectic coordinate
transformation that eliminates all cubic terms and puts the Hamiltonian in a Birkhoff
normal form up to order four due to the unexpected cancellation of the coefficients of all
fourth order non-generic resonant terms. We explain how to obtain higher-order vanishing
coefficients.
Finally, using the properties of the expansion kernels we derive a set of nonlinear evolution
equations for unidirectional gravity waves propagating on the surface of an ideal fluid
of infinite depth and show that they admit an exact traveling wave solution expressed in
terms of Lambert’s W-function. The only other known deep fluid surface waves are the
Gerstner and Stokes waves, with the former being exact but rotational whereas the latter
being approximate and irrotational. Our results yield a wave that is both exact and irrotational,
however, unlike Gerstner and Stokes waves, it is complex-valued.
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