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Curtin Department of Exploration Geophysics
Curtin Home > Faculties > Science and Engineering > WASM > Department of Exploration Geophysics

Seismic Processing
 

Seismic Signatures of Patchy Saturation


Another major effort of the group is focused on the study of the effects of patchy saturation on seismic signatures. The main objective is to quantify the effect of random spatial distribution of fluid patches. The approach is based on the general theory of heterogeneous poroelasticity developed in 2003-2005. The aim of the current effort is to build a general model for elastic properties of partially saturated rock with a given statistical distribution of fractures and with arbitrary contrast between the properties of the two fluids (e.g., gas and liquid).

Future work will also involve analysis of the effect of self-similar distribution of fluid patches. We are also developing a series of fluid injection experiments with X-ray and ultrasonic control to validate theoretical findings. This research is partially funded by the ARC Discovery Project Seismic response of partially saturated petroleum reservoir zones: towards quantitative recovery monitoring.

Research Leader: Prof Boris Gurevich (
B.Gurevich@curtin.edu.au).


Velocity-Stress Relationships (for time-lapse seismic)
 

One of the major issues in planning and quantitative interpretation of time-lapse seismic data is quantification of the pressure and stress effects on seismic velocities. To this end we are developing theoretical models of rock deformation. In particular, we have developed a method to assess the effect of rock heterogeneity on effective stress coefficients and showed that the addition of a tiny amount of very soft material may significantly affect effective stress coefficients. This has been demonstrated for an idealised concentric spherical geometry. Currently we are examining the magnitude of this effect for more realistic geometries.

A related effort is to assess the effect of core damage of velocity-stress relationships measured in the laboratory. To study this effect we are developing a method to compare laboratory measured velocities with sonic log measurements for different types of rocks.

Research Leader: Prof Boris Gurevich (B.Gurevich@curtin.edu.au).