2019 Pacific South Honorary Lecturer Seismic attenuation, dispersion, and anisotropy in porous rocks: Mechanisms and Models

2019 Pacific South Honorary Lecturer Seismic attenuation, dispersion, and anisotropy in porous rocks: Mechanisms and Models

By ASEG Victoria

Date and time

Thu, 21 Mar 2019 6:00 PM - 8:00 PM AEDT

Location

The Kelvin Club

14-30 Melbourne Place Melbourne, VIC 3000 Australia

Description

Dear member,

Please join us on the 21st of march 2019 at 6 pm, to listen to this year Asia Pacific SEG honorary lecturer.

We will have the pleasure to welcome Pr Boris Gurevitch from curtin University, who will present on the his work on Seismic attenuation, dispersion, and anisotropy in porous rocks: Mechanisms and Models.

Please register on Eventbrite before the 18/03/2019 COB, and email catering requirement to vicpresident@aseg.org.au.

Abstract

Understanding and modeling of attenuation of elastic waves in fluidsaturated rocks is important for a range of geophysical technologies that utilize seismic, acoustic, or ultrasonic amplitudes. A major cause of elastic wave attenuation is viscous dissipation due to the flow of the pore fluid induced by the passing wave. Wave-induced fluid flow occurs as a passing wave creates local pressure gradients within the fluid phase and the resulting fluid flow is accompanied with internal friction until the pore pressure is equilibrated. The fluid flow can take place on various length scales: for example, from compliant fractures into the equant pores (so-called squirt flow), or between mesoscopic heterogeneities like fluid patches in partially saturated rocks. A common feature of these mechanisms is heterogeneity of the pore space, such as fractures, compliant grain contacts, or fluid patches. Using theoretical calculations and experimental data, we will explore how this heterogeneity affects attenuation, dispersion, and anisotropy of porous rocks. I will outline a consistent theoretical approach that quantifies these phenomena and discuss rigorous bounds for attenuation and dispersion.


Biography:

Boris Gurevich has an MSc in geophysics from Moscow State University (1976) and a PhD from Institute of Geosystems, Moscow, Russia (1988), where he began his research career (1981–1994). In 1995–2000 he was a research scientist at the Geophysical Institute of Israel, where he focused mainly on diffraction imaging problems. Since 2001, he has been a professor of geophysics at Curtin University and advisor to CSIRO (Perth, Western Australia). At Curtin he has served as Head of Department of Exploration Geophysics (2010–2015) and since 2004 as director of the Curtin Reservoir Geophysics Consortium. He has served on editorial boards of Geophysics, Journal of Seismic Exploration, and Wave Motion. He is a Fellow of the Institute of Physics and has more than 100 journal publications in the areas of rock physics, poroelasticity, seismic theory, modeling, imaging, and monitoring of CO2 geosequestration. His research achievements include development of advanced theoretical models of seismic attenuation and dispersion in heterogeneous porous rocks.

Sponsored by Shell


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