2004
DOI: 10.1190/1.1707072
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Seismic low‐frequency effects in monitoring fluid‐saturated reservoirs

Abstract: There is a complex relationship between seismic attributes, including the frequency dependence of reflections and fluid saturation in a reservoir. Observations in both laboratory and field data indicate that reflections from a fluid-saturated layer have an increased amplitude and delayed traveltime at low frequencies, when compared with reflections from a gas-saturated layer. Comparison of laboratory-modeling results with a diffusive-viscous-theory model show that low (<5) values of the quality factor Q can ex… Show more

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Cited by 228 publications
(123 citation statements)
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“…The observed amplitude loss is explained by recent wave-propagation theory (Korneev et al 2004), which indicates that new frequency and angle dependent attributes are promising tools for more quantitatively imaging reservoir structure and estimating reservoir porosity and permeability.…”
Section: A351 P-wave Azimuthal Velocity and Frequency Anisotropymentioning
confidence: 99%
See 1 more Smart Citation
“…The observed amplitude loss is explained by recent wave-propagation theory (Korneev et al 2004), which indicates that new frequency and angle dependent attributes are promising tools for more quantitatively imaging reservoir structure and estimating reservoir porosity and permeability.…”
Section: A351 P-wave Azimuthal Velocity and Frequency Anisotropymentioning
confidence: 99%
“…The low value of the quality factor, Q, for the low frequency waves is a characteristic feature of permeable fluid-bearing layers (Korneev et al 2004). Goloshubin et al (2001) and Korneev et al (2004) analyzed VSP data recorded at a natural gas storage field in Indiana, where due to gas injection in the summer and withdrawal in the winter, the reservoir fluid changed seasonally.…”
Section: A351 P-wave Azimuthal Velocity and Frequency Anisotropymentioning
confidence: 99%
“…Korneev [48] successfully simulated the low frequency effects of fluid-saturated layers with the 1D diffusive-viscous wave equation theory, based on laboratory and field data. He explained that very low values of Q (quality factor) are the result of internal diffusive losses caused by fluid flow.…”
Section: Model Testmentioning
confidence: 99%
“…It is well-known that both the transmission and reflection coefficients from a fluid-saturated porous medium are functions of frequency [19,16,39,13]. Recently, low-frequency signals were successfully used in obtaining high-resolution images of oil and gas reservoirs [20,21,11] and in monitoring underground gas storage [25]. Therefore, understanding the behavior of the reflection coefficient at the low-frequency end of the seismic spectrum is of special importance.…”
Section: Introductionmentioning
confidence: 99%