Aircraft System Noise Shielding Prediction with a Kirchhoff Integral Method

Author(s):  
Yueping Guo ◽  
Dennis S. Pope ◽  
Casey L. Burley ◽  
Russell H. Thomas
2014 ◽  
Vol 27 (4) ◽  
pp. 391-399 ◽  
Author(s):  
Nathalie Favretto-Cristini ◽  
Anastasiya Tantsereva ◽  
Paul Cristini ◽  
Bjørn Ursin ◽  
Dimitri Komatitsch ◽  
...  

2021 ◽  
pp. 1-15
Author(s):  
Ian A. Clark ◽  
Russell H. Thomas ◽  
Yueping Guo
Keyword(s):  

2017 ◽  
Vol 25 (03) ◽  
pp. 1750023 ◽  
Author(s):  
Nathalie Favretto-Cristini ◽  
Arkady M. Aizenberg ◽  
Bjørn Ursin ◽  
Paul Cristini ◽  
Anastasiya Tantsereva

The Discretized Kirchhoff Integral method has been recently tested against laboratory experiments using a model with surface curvatures and sharp edges generating wave diffraction effects. Comparisons between numerical and laboratory data have exhibited a good quantitative fit in terms of time arrivals and amplitudes, except in the vicinity of secondary shadow boundaries created by the interaction of the edges of some topographical structures. Following this work, the effect of multiple scattering and the surface curvatures on the wavefield is studied here, using the so-called diffraction attenuation coefficient, in order to define the cases where these effects may be neglected in the numerical modeling without loss of accuracy.


2019 ◽  
Vol 56 (2) ◽  
pp. 529-544 ◽  
Author(s):  
Lothar Bertsch ◽  
Beat Schäffer ◽  
Sébastien Guérin

Geophysics ◽  
2014 ◽  
Vol 79 (2) ◽  
pp. T77-T90 ◽  
Author(s):  
Anastasiya Tantsereva ◽  
Bjørn Ursin ◽  
Nathalie Favretto-Cristini ◽  
Paul Cristini ◽  
Arkady M. Aizenberg

Accurate simulation of seismic wave propagation in complex geologic structures is of particular interest nowadays. However, difficulties arise for complex geologic structures with great and rapid structural changes, due, for instance, to the presence of shadow zones, head waves, diffractions and/or edge effects. Different methods have thus been developed and are typically tested on synthetic configurations against analytical solutions for simple canonical problems, reference methods, or via direct comparison with real data acquired in situ. Such approaches have limitations, especially if the propagation occurs in a complex environment with strong-contrast reflectors and surface irregularities because it can be difficult to determine the method that gives the best approximation of the “real” solution or to interpret the results obtained without an a priori knowledge of the geologic environment. An alternative approach for seismics consists in comparing the synthetic data with data obtained in laboratory experiments. In contrast to in situ experiments, high-quality data are collected under controlled conditions for a known configuration. In contrast with numerical experiments, laboratory data possess many of the characteristics of field data because real waves propagate through models with no numerical approximations. Our main purpose was to test the approach of using laboratory data as reference data for benchmarking 3D numerical methods and techniques using the setup that we have designed for this study. We performed laboratory-scaled measurements of zero-offset reflection of broadband pulses from a strong topographic environment immersed in a water tank. We compared these measurements with numerical data simulated by means of a discretized Kirchhoff integral method. The comparisons of synthetic and laboratory data indicated a good quantitative fit in terms of time arrivals and acceptable fit in amplitudes. Thus, the first step of the approach was successfully applied.


Sign in / Sign up

Export Citation Format

Share Document