Near-surface site investigation by seismic interferometry using urban traffic noise in Singapore

Geophysics ◽  
2019 ◽  
Vol 84 (2) ◽  
pp. B169-B180 ◽  
Author(s):  
Yunhuo Zhang ◽  
Yunyue Elita Li ◽  
Heng Zhang ◽  
Taeseo Ku

We have evaluated a field test in the city of Singapore to assess the feasibility of the passive seismic survey for bedrock depth determination and to further investigate the optimal acquisition parameters. The ambient noise field, dominated by urban traffic noise, is recorded passively for the application of seismic interferometry. Spectral analysis indicates that the traffic-induced noise by local roads is concentrated between 3 and 25 Hz. We use multiple signal classification beamforming for wavefield direction of propagation analysis. We apply seismic interferometry to retrieve the surface-wave part of the Green’s functions, based on which surface-wave dispersion relations are extracted and further inverted for 1D S-wave velocity profiles. Subsequently, we compare the inversion results from seismic interferometry with borehole logs at multiple sites in Singapore and establish that the bedrock depths are well-determined using passive seismic methods within a maximum error of 3 m. By investigating the convergence of the crosscorrelograms, we ascertain that the best compromise of cost, efficiency, and accuracy for a passive site investigation in Singapore can be achieved in 15 min in the morning of a working day using an array as short as 30 m with six vertical geophones, although these parameters should be reinvestigated at other sites and other times. The success of this case study demonstrates that accurate near-surface site investigation can be achieved with faster acquisition, fewer receivers, and a smaller acquisition footprint compared with conventional methods, all of which improve the efficiency particularly in a highly developed urban environment.

Geophysics ◽  
2010 ◽  
Vol 75 (2) ◽  
pp. SA15-SA25 ◽  
Author(s):  
David F. Halliday ◽  
Andrew Curtis ◽  
Peter Vermeer ◽  
Claudio Strobbia ◽  
Anna Glushchenko ◽  
...  

Land seismic data are contaminated by surface waves (or ground roll). These surface waves are a form of source-generated noise and can be strongly scattered by near-surface heterogeneities. The resulting scattered ground roll can be particularly difficult to separate from the desired reflection data, especially when this scattered ground roll propagates in the crossline direction. We have used seismic interferometry to estimate scattered surface waves, recorded during an exploration seismic survey, between pairs of receiver locations. Where sources and receivers coincide, these interreceiver surface-wave estimates were adaptively subtracted from the data. This predictive-subtraction process can successfully attenuate scattered surface waves while preserving the valuable reflected arrivals, forming a new method of scattered ground-roll attenuation. We refer to this as interferometric ground-roll removal.


2013 ◽  
Vol 133 (5) ◽  
pp. 3592-3592
Author(s):  
Frits Van der Eerden ◽  
Freek Graafland ◽  
Peter Wessels ◽  
Tom Basten

2013 ◽  
Vol 74 (4) ◽  
pp. 614-621 ◽  
Author(s):  
Alberto Ramírez ◽  
Efraín Domínguez

1993 ◽  
Vol 119 (5) ◽  
pp. 751-762 ◽  
Author(s):  
Parviz A. Koushki ◽  
Louis F. Cohn ◽  
Abdurrahman A. Felimban

1995 ◽  
Vol 98 (5) ◽  
pp. 2607-2612 ◽  
Author(s):  
G. Cammarata ◽  
A. Fichera ◽  
S. Graziani ◽  
L. Marletta

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