Spelling suggestions: "subject:"waves -- amathematical models"" "subject:"waves -- dmathematical models""
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Precise measurements of coda buildup and decay rates of western Pacific P, P₀ and S₀ phases and their relevance to lithospheric scatteringBrandsdottir, Bryndis 03 October 1986 (has links)
Graduation date: 1987 / Best scan available for figures.
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Fractal solutions to the long wave equationsAjiwibowo, Harman 13 September 2002 (has links)
The fractal dimension of measured ocean wave profiles is found to be in the
range of 1.5-1.8. This non-integer dimension indicates the fractal nature of the
waves. Standard formulations to analyze waves are based on a differential
approach. Since fractals are non-differentiable, this formulation fails for waves with
fractal characteristics. Integral solutions for long waves that are valid for a non-differentiable
fractal surfaces are developed. Field observations show a positive
correlation between the fractal dimension and the degree of nonlinearity of the
waves, wave steepness, and breaking waves. Solutions are developed for a variety
of linear cases. As waves propagate shoreward and become more nonlinear, the
fractal dimension increases. The linear solutions are unable to reproduce the change
in fractal dimension evident in the ocean data. However, the linear solutions do
demonstrate a finite speed of propagation.
The correlation of the fractal dimension with the nonlinearity of the waves
suggests using a nonlinear wave equation. We first confirm the nonlinear behavior
of the waves using the finite difference method with continuous function as the
initial condition. Next, we solve the system using a Runge-Kutta method to
integrate the characteristics of the nonlinear wave equation. For small times, the
finite difference and Runge-Kutta solutions are similar. At longer times, however,
the Runge-Kutta solution shows the leading edge of the wave extending beyond the
base of the wave corresponding to over-steepening and breaking.
A simple long wave solution on multi-step bottom is developed in order to
calculate the reflection coefficient for a sloping beach. Multiple reflections and
transmissions are allowed at each step, and the resulting reflection coefficient is
calculated. The reflection coefficient is also calculated for model with thousands of
small steps where the waves are reflected and transmitted once over each step. The
effect of depth-limited breaking waves is also considered. / Graduation date: 2003
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Chaos in a long rectangular wave channelBowline, Cynthia M. 24 November 1993 (has links)
The Melnikov method is applied to a model of parametrically generated cross-waves in a long rectangular channel in order to determine if these cross-waves are chaotic. A great deal of preparation is involved in order to obtain a suitable form for the application of the Melnikov method. The Lagrangian for water waves, which consists of the volume integrals of the kinetic energy density, potential energy density, and a dynamic pressure
component, is transformed to surface integrals in order to avoid constant conjugate momenta. The Lagrangian is simplified by subtracting the zero variation integrals and written in terms of generalized coordinates, the time dependent components of the crosswave and progressive wave velocity potentials. The conjugate momenta are calculated after expanding the Lagrangian in a Taylor series. The Hamiltonian is then determined by a
Legendre transformation of the Lagrangian.
Ordinarily, the first order evolution equations obtained from derivatives of the Hamiltonian are suitable for applications of the Melnikov method. However, the crosswave model results in extremely complicated evolution equations which must be simplified before a Melnikov analysis is possible. A sequence of seven canonical transformations are applied and yield a final set of evolution equations in fairly simple form. The unperturbed system is analyzed to determine hyperbolic fixed points and the equations describing the heteroclinic orbits for near resonance cases. The Melnikov function is calculated for the perturbed system which must also satisfy KAM conditions.
The Melnikov results indicate the system is chaotic near resonance. Furthermore, the heteroclinic orbits, about which chaotic motions occur, are transformed back to the original set of variables and found to be extremely complicated; this orbit would be impossible to determine analytically without the canonical transformations.
The theoretical results were verified by experiments. Poincare maps obtained from measurements of the free surface displacement indicate both quasi-periodic and chaotic motions of the water surface. Power spectra and time series of the water surface displacement are also analyzed for chaotic behavior, with less conclusive results. Stability diagrams of cross-wave generation confirm behavior consistent with parametric excitation. / Graduation date: 1994
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Flexible membrane wave barrierThompson, Gary O. 02 May 1991 (has links)
This report details the derivation of an analytical model for a flexible membrane
wave barrier. The wave barrier consists of a thin flexible membrane suspended in the
water column by a moored cylindrical buoy on the free surface and fixed to a hinge at
the seafloor.
The analytical model combines the three-degree of freedom rigid body motion
of the cylindrical buoy with the two-dimensional analog of a vibrating string for the
response of the flexible membrane. Theoretical results for reflection and transmission
coefficients, dynamic mooring line tension, horizontal hinge force, horizontal and
vertical displacements and rotation of the cylindrical buoy are compared with measured
results presented by Bender(1989).
In general, the theoretical results compare favorably with measured results for
moored systems. However, additional studies are required to more precisely quantify
the added mass and radiation damping properties of flexible membranes in oscillating
flows. / Graduation date: 1991
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Convolutional perfectly matched layers for finite element modeling of wave propagation in unbounded domainsXu, Boqing, 許博卿 January 2014 (has links)
A general convolutional version of perfectly matched layer (PML) formulation for second-order wave equations with displacement as the only unknown based on the coordinate stretching is proposed in this study, which overcomes the limitation of classical PML in splitting the displacement field and requires only minor modifications to existing finite element programs.
The first contribution concerns the development of a robust and efficient finite element program QUAD-CPML based on QUAD4M capable of simulating wave propagation in an unbounded domain. The more efficient hybrid-stress finite element was incorporated into the program to reduce the number of iterations for the equivalent linear dynamic analysis and the total time for the direct time integration. The incorporation of new element types was verified with the QUAD4M solutions to problems of dynamic soil response and the efficiency of hybrid-stress finite element was demonstrated compared to the classical finite elements.
The second development involves the implementation of a general convolutional perfectly matched layer (CPML) as an absorbing boundary condition for the modeling of the radiation of wave energy in an unbounded domain. The proposed non-split CPML formulation is displacement-based, which shows great compatibility with the direct time integration. This CPML formulation treats the convolutional terms as external forces and includes an updating scheme to calculate the temporal convolution terms arising from the Fourier transform. In addition, the performance of the CPML has been examined by various problems including a parametric study on a number of key coefficients that control the absorbing ability of the CPML boundary.
The final task of this thesis is to apply the developed CPML models to the dynamic analyses of soil-structure interaction (SSI) problems. Typical loading conditions including external load on the structure and underground wave excitation on the medium has been considered. Practical applications of CPML models include the numerical study on the effectiveness of the rubber-soil mixture (RSM) as an earthquake protection material and the report of vibrations induced by the passage of a high-speed train. The former investigates the effectiveness of the CPML models for the evaluation of the performance of RSM subject to seismic excitation and the latter tests the boundary effects on the accuracy of the results for train induced vibrations. Both studies show that CPML as an absorbing boundary condition is theoretically sound and effective for the analysis of soil-structure dynamic response. / published_or_final_version / Civil Engineering / Doctoral / Doctor of Philosophy
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Seismic data processing in transversely isotropic media: a plane wave approachMukherjee, Anubrati 28 August 2008 (has links)
Not available / text
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A computational procedure for three-dimensional simulation of nonlinear gravity wave propagation and response of floating structuresHardjanto, Fauzi Adi 16 May 2011 (has links)
Not available / text
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The propagation of nonlinear waves in layered and stratified fluidsLai, Wing-chiu, Derek., 黎永釗. January 2001 (has links)
published_or_final_version / abstract / toc / Mechanical Engineering / Doctoral / Doctor of Philosophy
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Effect of submerged vertical structures on ship waves繆泉明, Miao, Quanming. January 2001 (has links)
published_or_final_version / abstract / toc / Mechanical Engineering / Doctoral / Doctor of Philosophy
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Probabilistic analysis of harmonics in railway traction system阮國豪, Yuen, Kwok-hoo. January 2000 (has links)
published_or_final_version / Electrical and Electronic Engineering / Master / Master of Philosophy
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