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On the development of water waves generated by a submerged moving bodyin a two-layer fluid systemYang, Jiazhen, 楊嘉楨. January 2008 (has links)
published_or_final_version / Mechanical Engineering / Master / Master of Philosophy
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Correlation of P-wave velocity and weatheredLam, Wan, 林蘊 January 2004 (has links)
published_or_final_version / Applied Geosciences / Master / Master of Science
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Stability and interaction of waves in coupled nonlinear Schrödinger type systemsChiu, Hok-shun., 趙鶴淳. January 2009 (has links)
published_or_final_version / Mechanical Engineering / Master / Master of Philosophy
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Shear wave attenuation in unconsolidated laboratory sedimentsBrunson, Burlie A. 23 June 1983 (has links)
Shear wave attenuation measurements were made
using ceramic bimorph transducers to excite transverse
vibrations in a cylindrical column of unconsolidated
sediment. Three different water-saturated
sediments were used in an attempt to determine the
effects of grain shape and sorting on the frequency
dependence of attenuation. The mean grain size of the
sediments was held constant while the grain shape and
size distributions were varied. The sediment assemblages
used in the attenuation measurements included
a moderately-sorted angular quartz sand, a well-sorted
angular quartz sand, and well-sorted spherical
glass beads. The moderately-sorted sand showed the
greatest attenuation over the measurement frequency
range of 1 to 20 kHz. The well-sorted sand and the
glass beads showed generally lower attenuation with
the beads being the least lossy propagation medium.
All three sediments showed evidence of viscous attenuation
due to fluid-to-grain relative motion. This
mechanism leads to a non-linear relationship between
attenuation and frequency.
Sediment physical properties were measured for
use as inputs to a theoretical attenuation model based
on the Biot theory of propagation of waves in porous
media. The model allowed attenuation versus frequency
predictions to be made for each of the three sediment
assemblages. The resultant comparisons between the
measured and predicted attenuations demonstrated the
importance of using measured model inputs obtained
under controlled laboratory conditions when theoretical
model capabilities are being evaluated. The model
comparison shed significant light on the ability of
this particular model to predict shear wave attenuation
in non-ideal sediments. / Graduation date: 1984
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Waves and balanced mean flows in the atmosphereBuehler, Oliver January 1996 (has links)
No description available.
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The investigation of signal processing techniques when applied to visually evoked potential propagation path analysisHeneidy, Hamdy Soliman January 1991 (has links)
No description available.
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The higher order dynamics of progressive wavesSwan, Christopher January 1987 (has links)
No description available.
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Bent-ray travel-time tomography and migration without ray tracingEcoublet, Philippe January 1995 (has links)
No description available.
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Theory of multiwave mixing in two- and three-level media.An, Sunghyuck. January 1988 (has links)
This dissertation presents theories of multiwave mixing in two- and three-level media. The first part of the dissertation treats the semiclassical theories in two-level media. Chapter 2 gives the simple semiclassical theory of four-wave mixing when the two pump frequences differ by more than the reciprocal of the population-difference lifetime. This difference washes out the pump spatial holes as well as one of the two reflection gratings. We compare the results to the degenerate treatment of Abrams and Lind and find significant differences in the reflection coefficient spectra. Chapter 3 presents the semiclassical theory of multiwave in a squeezed vacuum characterized by unequal in-phase and in-quadrature dipole decay times. For a highly squeezed vacuum, we find sharp resonances in both probe absorption and reflection coefficients, which provide sensitive ways to measure the amount of squeezing in the vacuum. The second part of the dissertation treats the quantum theories in two- and three-level media. Chapter 4 develops the fourth-order quantum theory of multiwave mixing to describe the effects of sidemode saturation in two-level media. We derive explicit formulas for the fourth-order quantum coefficients and show that the fourth-order quantum theory reproduces the third-order semiclassical coefficient obtained by truncating a continued fraction. We apply the results to cavity problems and find significant differences in the sideband spectra given by the second- and fourth-order treatments, particularly as the sidemode approaches the laser threshold. The final chapter presents a quantum theory of multiwave mixing in three-level cascades with a two-photon pump. The explicit formulas for the resonance fluorescence spectrum and the quantum combination-tone source term are derived. The theory is applied to the generation of squeezed states of light. We find almost perfect squeezing for some strong pump intensities and good broad-band squeezing for low pump intensities.
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A theoretical study of nonlinear guided wavesGubbels, Monica Ann, 1964- January 1988 (has links)
The effect of linear absorption on TE0 nonlinear guided waves and the effect of linear absorption, input-beam misalignment and nonlinear saturation on soliton emission from a nonlinear waveguide have been numerically investigated using the beam propagation method. In the first case the distribution of the absorption is found to have a dramatic effect on the propagation of the nonlinear guided waves. In the second case results reminiscent of the lossless case are found to survive in the presence of these complications.
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