Normal oscillations of ideal stratified fluid with a free surface completely covered with the elastic ice
Taurida Journal of Computer Science Theory and Mathematics, no. 3 (2017), pp. 79-93

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Let a rigid immovable vessel be partially filled with an ideal incompressible stratified fluid. We assume that in an equilibrium state the density of a fluid is a function of the vertical variable $x_3,$ i.e., $\rho_0=\rho_0(x_3).$ In this case the gravitational field with constant acceleration $\vec g=-g\vec e_3$ acts on the fluid, here $g>0$ and $\vec e_3$ is unit vector of the vertical axis $Ox_3,$ which is directed opposite to $\vec g.$ Let $\Omega$ be the domain filled with a fluid in equilibrium state, $S$ be rigid wall of the vessel adherent to the fluid, $\Gamma$ be a free surface completely covered with the elastic ice. Let us consider the basic case of stable stratification of the fluid on density: \begin{equation*} \begin{split} 0{min}^{2} \leq N^{2}(x_3) \leq N_{max}^{2} =: N_0^2 \infty, \\ ^2(x_3) := - \frac{ g\rho_0'(x_3) }{ \rho_0(x_3)},\quad\rho_0(0)>0, \end{split} \end{equation*} where $N^{2}(x_3)$ is square frequency of buoyancy. The initial boundary value problem is reduced to a Cauchy problem \begin{equation*} \begin{split} \mathcal A \frac{d^2x}{dt^2} + \mathcal C x = f(t), \quad x(0)=x^0, \quad x^{'}(0)=x^1, \\ 0 \mathcal A= \mathcal A^{*} \in \mathcal L(\mathcal H), \quad \mathcal C = \mathcal C^{*} \geq 0. \end{split} \end{equation*} in some Hilbert space $\mathcal H$. The spectrum of normal oscillations, basic properties of eigenfunctions and other questions are studied. Let us consider the basic case of stable stratification of the fluid on density: \begin{equation*} \begin{split} 0{min}^{2} \leq N^{2}(x_3) \leq N_{max}^{2} =: N_0^2 \infty, \\ ^2(x_3) := - \frac{ g\rho_0'(x_3) }{ \rho_0(x_3)},\quad\rho_0(0)>0, \end{split} \end{equation*} where $N^{2}(x_3)$ is square frequency of buoyancy. The initial boundary value problem is reduced to a Cauchy problem \begin{equation*} \begin{split} \mathcal A \frac{d^2x}{dt^2} + \mathcal C x = f(t), \quad x(0)=x^0, \quad x^{'}(0)=x^1, \\ 0 \mathcal A= \mathcal A^{*} \in \mathcal L(\mathcal H), \quad \mathcal C = \mathcal C^{*} \geq 0. \end{split} \end{equation*} in some Hilbert space $\mathcal H$. The spectrum of normal oscillations, basic properties of eigenfunctions and other questions are studied. Let us consider the basic case of stable stratification of the fluid on density: \begin{equation*} \begin{split} 0{min}^{2} \leq N^{2}(x_3) \leq N_{max}^{2} =: N_0^2 \infty, \\ ^2(x_3) := - \frac{ g\rho_0'(x_3) }{ \rho_0(x_3)},\quad\rho_0(0)>0, \end{split} \end{equation*} where $N^{2}(x_3)$ is square frequency of buoyancy. The initial boundary value problem is reduced to a Cauchy problem \begin{equation*} \begin{split} \mathcal A \frac{d^2x}{dt^2} + \mathcal C x = f(t), \quad x(0)=x^0, \quad x^{'}(0)=x^1, \\ 0 \mathcal A= \mathcal A^{*} \in \mathcal L(\mathcal H), \quad \mathcal C = \mathcal C^{*} \geq 0. \end{split} \end{equation*} in some Hilbert space $\mathcal H$. The spectrum of normal oscillations, basic properties of eigenfunctions and other questions are studied.
Keywords: stratification effect in ideal fluids, differential equation in Hilbert space, spectral problem, eigenvalues, Riesz basis.
Mots-clés : normal oscillations
@article{TVIM_2017_3_a4,
     author = {D. O. Tsvetkov},
     title = {Normal oscillations of ideal stratified fluid with a free surface completely covered with the elastic ice},
     journal = {Taurida Journal of Computer Science Theory and Mathematics},
     pages = {79--93},
     publisher = {mathdoc},
     number = {3},
     year = {2017},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/TVIM_2017_3_a4/}
}
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D. O. Tsvetkov. Normal oscillations of ideal stratified fluid with a free surface completely covered with the elastic ice. Taurida Journal of Computer Science Theory and Mathematics, no. 3 (2017), pp. 79-93. http://geodesic.mathdoc.fr/item/TVIM_2017_3_a4/