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Climate Change 2016

October 27-29, 2016

Volume 7, Issue 9(Suppl)

J Earth Sci Clim Change

ISSN: 2157-7617 JESCC, an open access journal

conferenceseries

.com

October 24-26, 2016 Valencia, Spain

World Conference on

Climate Change

Laboratory scale monitoring of CO

2

sequestration using complex electrical conductivity and seismic

property changes derived by seismic interferometry

Ranajit Ghose, Deyan Draganov, Alex Kirichek

and

Karel Heller

Delft University of Technology, The Netherlands

I

n order to realize and maintain a successful CO

2

storage endeavor, a program of careful monitoring of the changes in

reservoir properties is necessary. The way the reservoir properties change is generally case-specific, as such modifications

are principally related to the distribution of pores, fluid composition, and the thermodynamic conditions. Of the various

geophysical methods, so far seismic and electrical methods have been primarily used with varying success to monitor

remotely the changes in a carbon capture and storage (CCS) reservoir. However, a quantitative characterization of the dynamic

reservoir properties has remained difficult mainly due to three reasons. First, laboratory calibration of rock-physical models

used to extract the reservoir properties from geophysical data is challenging. Second, quantitative and integrated geophysical

approaches that are specifically sensitive to changes in fluid (supercritical CO

2

and brine) saturation, salinity and pressure are

yet to be developed. Third, the difficulty to capture reliably in surface measurements the seismic signature of the changes in a

CCS reservoir without the unwanted effects of overburden changes has been an obstacle. In order to address these issues, we

have developed a laboratory facility where simultaneous seismic and electrical measurements can be performed on a reservoir

rock under realistic pressure and temperature conditions. Changing saturation and salinity could be quantified on dynamic

measurements of complex electrical conductivity. Application of seismic interferometry could resolve changes in seismic

velocity in the reservoir due to fluid substitution. The approach of joint inversion of these two data types can be applicable to

realistic, quantitative field-monitoring.

Biography

Ranajit Ghose is an Associate Professor at Delft University of Technology, The Netherlands. His areas of research interest are high-resolution seismic with focus

on shear wave, near-surface and geotechnical geophysics, quantitative integrated approaches in geophysics, seismic attenuation, poro-elasticity and property

estimation, seismic wave propagation in fractured media and anisotropy and monitoring CO

2

sequestration. He is presently the Editor-in-Chief of the journal “Near

Surface Geophysics”.

r.ghose@tudelft.nl

Ranajit Ghose et al., J Earth Sci Clim Change 2016, 7:9(Suppl)

http://dx.doi.org/10.4172/2157-7617.C1.027