Seminar talk, 1 March 2017: Difference between revisions

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<math>u_t=2uu_x+u_{xxx}+\varepsilon\chi_{a,b}u_{xx}</math>,
<math>u_t=2uu_x+u_{xxx}+\varepsilon\chi_{a,b}u_{xx}</math>,


where <math>\chi_{a,b}</math> is the characteristic function of the interval <math>[a,b]</math>, then the soliton <math>6a^2\mathrm{ch}^{-2}(4a^3t+ax)</math> arrived from the right partially reflects at viscous barrier <math>x\in[a,b]</math> and partially passes through in the form of soliton of smaller velocity and amplitude.  The process in some degree is described by the so-called balance laws, which are the evolution of conservation laws for KdV.
where <math>\chi_{a,b}</math> is the characteristic function of the interval <math>[a,b]</math>, then the soliton <math>6a^2\mathrm{ch}^{-2}(4a^3t+ax)</math> arrived from the right partially reflects at viscous barrier <math>x\in[a,b]</math> and partially passes through in the form of a soliton of smaller velocity and amplitude.  The process in some degree is described by the so-called balance laws, which are the evolution of conservation laws for KdV.
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Latest revision as of 23:28, 22 February 2017

Speaker: Alexey Samokhin

Title: Reflections of soliton on viscous barrier and the degradation of conserved quantities for the KdV

Abstract:
If waves are described by the equation

,

where is the characteristic function of the interval , then the soliton arrived from the right partially reflects at viscous barrier and partially passes through in the form of a soliton of smaller velocity and amplitude. The process in some degree is described by the so-called balance laws, which are the evolution of conservation laws for KdV.

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