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Titlebook: Diffuse Waves in Complex Media; Jean-Pierre Fouque Book 1999 Springer Science+Business Media Dordrecht 1999 crystal.diffusion.geophysics.m

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楼主: Wilder
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,Einführung – „Enemy“ oder „Frenemy“?,reviewed. It is based on the Shohat method in the theory of orthogonal polynomials. The approach presented is equally suitable for description of both local and global spectral characteristics, thereby providing an overall look at the phenomenon of spectral universality in Random Matrix Theory.
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Über Wirkung und Wert von Rhetorikresponse theory provides the spectrum of electric-field fluctuations, whose maxima define the polariton dispersion relation. The dependence of polariton radiative damping rates on the degree of disorder in the dielectric is calculated. Particular attention is given to the magnitudes of the scattered
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https://doi.org/10.1007/978-3-8349-9734-0irst magneto-optical trap [2], the sub-Doppler [3] and sub-recoil [4] cooling techniques and more recently the observation of Bose-Einstein condensation of dilute atomic gases [5] [6]. A review on milestones in this field can be found in the 1997 Nobel lectures by S. Chu [7], C. Cohen-Tannoudji [8]
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Robert L. Barret,Bryan E. Robinson. The reflection and transmission properties of such a locally-layered slab are studied. Of principal interest is the question of the robustness of the plane layered theory. Do phenomena such as localization and the results of O’Doherty-Anstey theory persist under perturbations of plane layering? We
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R. Jerald Shore,Bert Hayslip Jr.ve crust overlying an almost homogeneous mantle. We simulate the multiple scattering of the seismic waves using the classical radiative transfer equation in a scalar approximation. We solve the equation using the Monte Carlo method and give a particular attention to the asymptotics of the solution.
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https://doi.org/10.1007/978-94-011-4572-5crystal; diffusion; geophysics; materials science; scattering; statistics; wave propagation
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