Qing-Chun Jiang

Effects of multiscale wave-induced fluid flow on seismic wave dispersion and attenuation in partially saturated porous rocks

Wave-induced fluid flow (WIFF) across multiple scales causes significant seismic wave dispersion and attenuation over a broad frequency range in partially saturated rocks. Accurately characterizing these effects is crucial for improving hydrocarbon reservoir detection. In this study, we develop a model that integrate...