Novel Use of P-wave and S-wave Seismic Attenuation for Deep Natural Gas Exploration and Development
To develop and test a new methodology for using seismic attenuation(Q) attributes, from multi-component P-wave and S-wave seismic data, for assessing the presence of high oil or natural gas saturations, and estimating reservoir properties (in particular, gas saturation, lithology, and porosity).
Deeply buried gas reservoirs along the Gulf of Mexico shelf are an important future energy resource for the U.S. One of the greatest problems encountered by operators in this area is identifying commercially viable targets for drilling. Standard 3D seismic methods for direct hydrocarbon indication, such as amplitude versus offset (AVO), have proven unreliable for detecting deep gas targets below 15,000 feet or so.
This study combines three elements: (1) a synthesis of the latest rock physics understanding of how rock P-wave and S-wave inelasticity is related to rock type, pore fluid types, and pore microstructure, (2) synthetic seismic modeling that will help identify the relative contributions of scattering and intrinsic inelasticity to apparent attenuation (Q) attributes, and (3) robust algorithms that extract relative P- and S- wave attenuation attributes from seismic data. Recognizing the pitfalls of measuring attenuation in-situ, RSI will implement procedures that emphasize relative attenuation anomalies that are calibrated to well log information, and that incorporate empirical and theoretical constraints from rock physics.
After developing the necessary methodologies for computing Q from downhole measurements and reflection seismic data, RSI will employ Artificial Neural Network and other methods to link the well-derived reservoir properties to the seismic attenuation attributes. This will provide a quantitative means to interpret Qp and Qs in terms of oil and gas saturation, lithology, porosity, and possibly permeability. This will be the ultimate accomplishment of this project. The developed methods will be tested using actual field data to be supplied by U.S.-based oil and gas companies. The data will be analyzed for indications of hydrocarbon accumulation and the results will be compared to data from “blind” wells that will be withheld from the original analysis.
Rock Solid Images (RDSPI, LP)
Houston, Texas 77063
RSI plans to develop and test a new methodology for extracting seismic attenuation attributes from multi-component P-wave and S-wave seismic data, and relating these to the presence of natural gas occurrences in deep reservoirs (over 15,000 feet). The methodology will make use of existing seismic data already in the libraries of U.S. operators. Therefore, it will be much more economically viable than methods requiring special and additional seismic data acquisition. The results will make drilling for deep gas less risky and will encourage more rapid development of deep, higher risk, domestic, natural gas resources.
This project is complete. The final report is listed below under "Additional Information".
In September 2005, the performer completed the project’s first milestone, final development of equations for computing seismic wave attenuation from digital well log data. This represents a significant accomplishment, as there is currently no commercial tool to measure attenuation in the borehole, and it is known to contain useful information about critical reservoir properties, including gas charge.
During December 2005, the project performer loaded Seitel Eugene Island GOM ocean-bottom-cable seismic data along with the accompanying velocity data. These data were used to test the validity of the equations developed during the first year of the project for relating p- and s-wave attenuation attributes to gas saturation, porosity, and lithology.
During January 2006, the project performer completed development of a qualitative method for registering multicomponent seismic data, based on the nature and similarity of particular PS and PP reflections. The performer consulted with UT BEG on their methodologies for co-registering PP and PS seismic displays. The co-registration is one step in interpreting the Seitel Eugene Island, Gulf of Mexico dataset.
Through July 2006, the project performer has validated the reliability of their equations using the Eugene Island ocean-bottom-cable data set.
Rock physics modeling is key to realistically assessing P- and S- wave attenuation. The new rock physics model, developed as part of this study, links attenuation and velocity dispersion that occurs in partially saturated reservoirs as well as in non-reservoir rock. This new model estimates Qp (P-wave attenuation) and Qs (S-wave attenuation) from basic elastic variables such as, porosity, lithology, fluid, and pressure. Thus far, the results of this modeling effort have been consistent with experimentally-measured values.
A large potential of this model is that it allows for consistent forward modeling of attenuation depending on the properties and conditions in the subsurface to supplement and extend the existing real data. Such rock-physics-based “what-if” forward modeling is a powerful tool of seismic interpretation and has been extensively used with the elastic properties. This new theoretical development will help extend this approach into the inelastic domain.
Attenuation can be used in exploration and development only if it can be extracted from real seismic data. To test whether such extraction is viable researchers, as part of this study, created synthetic seismic traces for P-to-P and P-to-S amplitude using their rock physics predictions. In this synthetic modeling they used a new raytracer tool designed specifically for this task. The results prove that the amplitude is indeed affected by attenuation and, by inference, that the seismic P- and S-wave attenuation can be measured in the field and eventually used for the purpose of rock diagnostics.
Current Status and Remaining Tasks:
Early results indicated that the P-wave attenuation is noticeably affected by the presence of hydrocarbons, but the S-wave attenuation is not. The model predicts that the ratio of these attenuation values can be used as a hydrocarbon indicator. The project team has completed the final report that summarizes the results of the validation of the model with real seismic and well log data from a survey in the deep Gulf of Mexico. The final report is listed below under "Additional Information".
Project Start Date: September 29, 2004
Project End Date: September 30, 2006
DOE Contribution: $776,321
Performer Contribution: $332,709
NETL – Fran Toro (firstname.lastname@example.org or 304-285-4107)
RSI – Joel Walls (email@example.com or 713-783-5593 )
Project Final Report [PDF-8.21MB] - December, 2006
The following papers were presented at the 2005, Society of Exploration Geophysics meeting:
A Rock Physics and Attenuation Analysis of a Well from the Gulf of Mexico [PDF-190KB]
Gary Mavko, Stanford University, Jack Dvorkin*, Stanford University and Rock Solid Images, Joel Walls, Rock Solid Images
A Theoretical Estimate of S-Wave Attenuation in Sediment [PDF-70KB]
Gary. Mavko*, Stanford University, Jack Dvorkin, Stanford University and Rock Solid Images, Joel Walls, Rock Solid Images
Evaluation of an Inelastic (Q) Synthetic Seismic Generator [PDF-275KB]
Scott Singleton*, Rock Solid Images, and Jack Dvorkin, Stanford University and Rock Solid Images
Effects of pore fluid properties at high pressure and temperature on seismic response [PDF-238KB]
Joel Walls*, Rock Solid Images and Jack Dvorkin, Rock Solid Images and Stanford University
Well 2700 and PP seismic volume from Seitel
Well 2700 and PS seismic volume from Seitel