# Peregrine Soliton with Controllable Center in the Causal Interpretation of Quantum Mechanics

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The standard "self-focusing" nonlinear Schrödinger equation, also known as the Gross–Pitaevskii equation, appears in wave propagation through nonlinear media such as signal transmission in optical fibers, Bose–Einstein condensation, and surface waves over sufficiently deep water. This Demonstration studies a spatially localized algebraic breather solution (Peregrine soliton), where the maximum of the squared wavefunction varies by initial conditions. The causal interpretation of quantum theory developed by Louis de Broglie and David Bohm introduced trajectories that are guided by a quantum potential. The velocities of single particles, following the trajectories, are determined by the phase of the wavefunction. The system is time reversible.

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Contributed by: Klaus von Bloh (November 2011)

Open content licensed under CC BY-NC-SA

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## Details

The nonlinear Schrödinger equation is , with , and so on, where is a complex function and is its complex conjugate. Here the common standard notation is used, where is the temporal and is the spatial coordinate. The maximum of the original Peregrine soliton is located at the fixed point [1]. Wang, He, and Li find in [2] a rational-like solution with a controllable center, which has the same structure as the original Peregrine breather solution.

In the eikonal representation of the wave, , the gradient of the phase is the particle velocity . In this interpretation, the origin of the motion of the particle is the potential , given by , plus an additional term . The latter may be interpreted alternatively as a kind of fluid pressure or quantum potential.

For the complex-valued wavefunction,

,

there is an analytic solution for the quantum motion, where the squared modulus of the wavefunction is interpreted as the wave density. The phase function for the breather is defined as

,

from which the equation of motion is derived by solving:

The analytical solution is given, where is an integration constant. The initial position is estimated by solving the equation numerically. Real-valued trajectories are obtained for several 's. The starting positions of the particles are linearly distributed around the peak of the wave at and . You can control the paths together with the starting points by changing the initial conditions and . The path together with the starting point leads to a trajectory in space.

References

[1] D. H. Peregrine, "Water Waves, Nonlinear Schrödinger Equations and Their Solutions,"* Journal of the Australian Mathematical Society, Series B*,* *25(1),* *1983 pp. 16–43. journals.cambridge.org/action/displayAbstract?fromPage=online&aid=3968224.

[2] X.-C. Wang, J.-S. He, and Y.-S. Li, "Rogue Wave with a Controllable Center of Nonlinear Schrödinger Equation," *Communications in Theoretical Physics*, 56(4), 2011 pp. 631–637. ctp.itp.ac.cn/EN/volumn/volumn_1277.shtml.

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