Analysis of strong scattering at the micro-scale

被引:29
作者
van Wijk, K [1 ]
Komatitsch, D
Scales, JA
Tromp, J
机构
[1] Colorado Sch Mines, Dept Geophys, Phys Acoust Lab, Dept Geophys, Golden, CO 80401 USA
[2] Seismol Lab, Pasadena, CA 91125 USA
关键词
D O I
10.1121/1.1647480
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
Exploiting the fine structure of strongly scattered waves could provide a wealth of new information in seismology, ultrasonics, acoustics, and other fields that study wave propagation in heterogeneous media. Therefore, noncontacting laser-based measurements of ultrasonic surface waves propagating in a strongly disordered medium are performed in which the ratio of the dominant surface wavelength to the size of a scatterer is large, and waves that propagate through many scatterers are recorded. This allows analysis of scattering-induced dispersion and attenuation, as well as the transition from ballistic to diffusive propagation. Despite the relatively small size of the scatterers, multiple scattering strikingly amplifies small perturbations, making changes even in a single scatterer visible in the later-arriving waveforms. To understand the complexity of the measured waveforms, elastic spectral-element numerical simulations are performed. The multiple-scattering sensitivity requires precise gridding of the actual model, but once this has been accomplished, we obtain good agreement between the measured and simulated waveforms. In fact, the simulations are invaluable in analyzing subtle effects in the data such as weak precursory body-wave diffractions. The flexibility of the spectral-element method in handling media with sharp boundaries makes it a powerful tool to study surface-wave propagation in the multiple-scattering regime. (C) 2004 Acoustical Society of America.
引用
收藏
页码:1006 / 1011
页数:6
相关论文
共 30 条
[1]   ORIGIN OF CODA WAVES - SOURCE, ATTENUATION, AND SCATTERING EFFECTS [J].
AKI, K ;
CHOUET, B .
JOURNAL OF GEOPHYSICAL RESEARCH, 1975, 80 (23) :3322-3342
[2]   Scattering of elastic waves in 2-D composite media .1. Theory and test [J].
Benites, RA ;
Roberts, PM ;
Yomogida, K ;
Fehler, M .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1997, 104 (1-3) :161-173
[3]   Long-range correlations in the diffuse seismic coda [J].
Campillo, M ;
Paul, A .
SCIENCE, 2003, 299 (5606) :547-549
[4]   ENERGY-SPECTRA AND LEVEL STATISTICS OF FIBONACCI AND THUE-MORSE CHAINS [J].
CARPENA, P ;
GASPARIAN, V ;
ORTUNO, M .
PHYSICAL REVIEW B, 1995, 51 (18) :12813-12816
[5]   SCATTERED PKKP - FURTHER EVIDENCE FOR SCATTERING AT A ROUGH CORE-MANTLE BOUNDARY [J].
CHANG, AC ;
CLEARY, JR .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1981, 24 (01) :15-29
[6]  
CHANG AC, 1978, B SEISMOL SOC AM, V68, P1059
[7]   Diffusing acoustic wave spectroscopy [J].
Cowan, ML ;
Jones, IP ;
Page, JH ;
Weitz, DA .
PHYSICAL REVIEW E, 2002, 65 (06) :1-066605
[8]   Light transport through the band-edge states of Fibonacci quasicrystals [J].
Dal Negro, L ;
Oton, CJ ;
Gaburro, Z ;
Pavesi, L ;
Johnson, P ;
Lagendijk, A ;
Righini, R ;
Colocci, M ;
Wiersma, DS .
PHYSICAL REVIEW LETTERS, 2003, 90 (05) :4-055501
[9]   Observations of PKKP precursors used to estimate small-scale topography on the core-mantle boundary [J].
Earle, PS ;
Shearer, PM .
SCIENCE, 1997, 277 (5326) :667-670
[10]   2D and 3D elastic wave propagation by a pseudo-spectral domain decomposition method [J].
Faccioli, E ;
Maggio, F ;
Paolucci, R ;
Quarteroni, A .
JOURNAL OF SEISMOLOGY, 1997, 1 (03) :237-251