Abstract

Time-lapse seismic monitoring constitutes the foundation for most monitoring programmes involving CO2 storage. Two major sources of uncertainty in the estimation of changes in the reservoir properties like saturation and pressure, using time-lapse seismics, are the non-repeatability of the source positions and the difficulty to separate the effect of the overburden from that of the changes taking place in a CO2 reservoir. In order to address those challenges, we propose a new concept of using non-physical (ghost) reflection events retrieved by seismic interferometry. We test this concept on data of realistic numerical modelling and scaled laboratory experiments, both representing a horizontally layered subsurface. Our results demonstrate that the seismic reflection ghosts can indeed be used advantageously to monitor changes in the CO2 reservoir.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call