One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …

Seismic fluid identification works as an effective approach to characterize the fluid feature
and distribution of the reservoir underground with seismic data. Rock physics which builds …

For electrically powered applications such as consumer electronics and especially for
electric vehicles a precise state-of-charge estimation for their lithium-ion batteries is desired …

Natural fractures in hydrocarbon reservoirs can cause significant seismic attenuation and
dispersion due to wave induced fluid flow between pores and fractures. We present two …

Although significant advancement has occurred in the interpretation of seismic amplitude-
variation-with-offset (AVO) anomalies, a theory is lacking to guide the interpretation of …

Porous rocks encountered in hydrocarbon reservoirs are often saturated with a mixture of
two or more fluids. Generation of synthetic seismograms as well as interpretation of in-situ …

Saturation of porous rocks with a mixture of two fluids (known as partial saturation) has a
substantial effect on the seismic waves propagating through these rocks. In particular, partial …

Saturation of porous rocks with a mixture of two fluids has a substantial effect on seismic‐
wave propagation. In particular, partial saturation causes significant attenuation and …

A detailed analysis of the relationship between elastic waves in inhomogeneous, porous
media and the effect of wave-induced fluid flow is presented. Based on the results of the …

Elastic upscaling of thinly layered rocks typically is performed using the established Backus
averaging technique. Its poroelastic extension applies to thinly layered fluid-saturated …