2006
DOI: 10.1190/1.2159053
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Fluid mobility and frequency-dependent seismic velocity — Direct measurements

Abstract: The influence of fluid mobility on seismic velocity dispersion is directly observed in laboratory measurements from seismic to ultrasonic frequencies. A forceddeformation system is used in conjunction with pulse transmission to obtain elastic properties at seismic strain amplitude (10 −7 ) from 5 Hz to 800 kHz. Varying fluid types and saturations document the influence of pore-fluids. The ratio of rock permeability to fluid viscosity defines mobility, which largely controls pore-fluid motion and pore pressure … Show more

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Cited by 479 publications
(374 citation statements)
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References 42 publications
(44 reference statements)
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“…This indicates that increasing the viscosity of the pore fluid moves the dispersion effects to occur at lower seismic frequencies. This agrees well with the concept of fluid mobility, defined as the ratio between permeability and viscosity by Batzle et al (2006). Overall, the maximum P-and S-wave attenuation values are larger for brine than for the other two fluids.…”
Section: The Fluid Effectsupporting
confidence: 78%
“…This indicates that increasing the viscosity of the pore fluid moves the dispersion effects to occur at lower seismic frequencies. This agrees well with the concept of fluid mobility, defined as the ratio between permeability and viscosity by Batzle et al (2006). Overall, the maximum P-and S-wave attenuation values are larger for brine than for the other two fluids.…”
Section: The Fluid Effectsupporting
confidence: 78%
“…Corresponding laboratory experiments are already conducted for seismic purposes [e.g., Batzle et al, 2006] and could be extended to seismoelectric measurements. Although our analysis was performed considering laboratory-size samples, the results of this study also have corresponding implications for seismoelectric conversions at the field scale.…”
Section: Discussionmentioning
confidence: 99%
“…Examples include the phenomena encountered in rock physics, where ultrasound up to 1 GHz has been deployed on small samples at both elevated temperature and pressure. 63,64,65 These methods are also being used to measure properties such as density, viscosity, and particle size in process industries and at the DOE Hanford Waste Treatment Plant (WTP). Such methods are being considered for various applications in fuel reprocessing facilities.…”
Section: Ultrasonic Transducersmentioning
confidence: 99%