TY - JOUR
T1 - Dispersion analysis of passive surface-wave noise generated during hydraulic-fracturing operations
AU - Forghani-Arani, Farnoush
AU - Willis, Mark
AU - Snieder, Roel
AU - Haines, Seth S.
AU - Behura, Jyoti
AU - Batzle, Mike
AU - Davidson, Michael
N1 - Publisher Copyright:
© 2014.
PY - 2014/12/1
Y1 - 2014/12/1
N2 - Surface-wave dispersion analysis is useful for estimating near-surface shear-wave velocity models, designing receiver arrays, and suppressing surface waves. Here, we analyze whether passive seismic noise generated during hydraulic-fracturing operations can be used to extract surface-wave dispersion characteristics. Applying seismic interferometry to noise measurements, we extract surface waves by cross-correlating several minutes of passive records; this approach is distinct from previous studies that used hours or days of passive records for cross-correlation. For comparison, we also perform dispersion analysis for an active-source array that has some receivers in common with the passive array. The active and passive data show good agreement in the dispersive character of the fundamental-mode surface-waves. For the higher mode surface waves, however, active and passive data resolve the dispersive properties at different frequency ranges. To demonstrate an application of dispersion analysis, we invert the observed surface-wave dispersion characteristics to determine the near-surface, one-dimensional shear-wave velocity.
AB - Surface-wave dispersion analysis is useful for estimating near-surface shear-wave velocity models, designing receiver arrays, and suppressing surface waves. Here, we analyze whether passive seismic noise generated during hydraulic-fracturing operations can be used to extract surface-wave dispersion characteristics. Applying seismic interferometry to noise measurements, we extract surface waves by cross-correlating several minutes of passive records; this approach is distinct from previous studies that used hours or days of passive records for cross-correlation. For comparison, we also perform dispersion analysis for an active-source array that has some receivers in common with the passive array. The active and passive data show good agreement in the dispersive character of the fundamental-mode surface-waves. For the higher mode surface waves, however, active and passive data resolve the dispersive properties at different frequency ranges. To demonstrate an application of dispersion analysis, we invert the observed surface-wave dispersion characteristics to determine the near-surface, one-dimensional shear-wave velocity.
KW - Dispersion
KW - Interferometry
KW - Noise
KW - Passive
KW - Surface-wave
UR - http://www.scopus.com/inward/record.url?scp=84908303656&partnerID=8YFLogxK
U2 - 10.1016/j.jappgeo.2014.09.008
DO - 10.1016/j.jappgeo.2014.09.008
M3 - Article
AN - SCOPUS:84908303656
SN - 0926-9851
VL - 111
SP - 129
EP - 134
JO - Journal of Applied Geophysics
JF - Journal of Applied Geophysics
ER -