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Trajectory propagation methods evaluation

The quasiclassical amplitude in the momentum representation does not suffer from this feature, because boundary conditions Pz h) = Pu> Pzitz) = P2z determine the unique classical trajectory for the typical scattering potentials. Such amplitude cannot be obtained as a Fourier transform of the quasiclassical propagator in coordinate representation. So it is necessary to modify the stationary phase method for the evaluation of the path integral in momentmn representation. [Pg.10]

See other pages where Trajectory propagation methods evaluation is mentioned: [Pg.187]    [Pg.192]    [Pg.187]    [Pg.192]    [Pg.187]    [Pg.192]    [Pg.462]    [Pg.246]    [Pg.249]    [Pg.203]    [Pg.203]    [Pg.119]    [Pg.597]    [Pg.5]    [Pg.233]    [Pg.622]    [Pg.654]    [Pg.677]    [Pg.203]    [Pg.24]    [Pg.1358]    [Pg.112]   
See also in sourсe #XX -- [ Pg.208 ]



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