Mapping reservoir characteristics using earth's nonlinearity as a seismic attribute
AssigneeNonlinear Seismic Imaging, Inc.
InventorTawassul Ali Khan
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AssigneeNonlinear Seismic Imaging, Inc.
InventorTawassul Ali Khan
Estimating the term…
This invention relates to mapping the hydrocarbon reservoir characteristics by mapping the reservoir formations that display dynamic elastic nonlinearity responses to the seismic signals. The main reason of this nonlinear behavior in the reservoir rocks is their bulk rock property: the porosity, fractures, differential pressure and pore saturation. To map these bulk rock properties, the interaction of the two seismic waves as they propagate through elastically nonlinear rocks is recorded. Two compressional seismic signals are transmitted from the surface. Seismic reflection data using surface or borehole detectors are recorded. One of the transmitted signals is a conventional swept frequency and the other is a mono-frequency signal. During the propagation of these two signals through the elastically nonlinear reservoir rocks, there is an interaction between the two signals. The sum and difference frequencies of the two primary seismic signals that were transmitted from the surface are created. These new frequencies constitute an ‘interaction’ wave that travels along with the two primary waves. In this invention, the ‘interaction’ signal created by the two seismic waves as they propagate through the reservoir rocks is separated from the primary signals and used to map the reservoir rocks that exhibit elastic nonlinearity due their bulk rock properties. The cross-correlation of the recorded data with the swept frequency signal provides a conventional seismic data set that is used for normal 2-D or 3-D seismic processing. The cross-correlation of the recorded data with the summed and differenced signals provides two sets of data that represent the seismic reflected image from the subsurface nonlinear formations.
A method of mapping the reservoir rocks that exhibit elastic nonlinearity due to their porosity, fracturing, heterogeneity and pore fluids and distinguishing them from the rocks that are relatively linear due to lack of porosity, homogeneous rock structure and lower fluid content;
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