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Integration of the Biot-Gassmann Fluid Substitution Method and Machine Learning-Based Velocity-Stress Relationship
Ayyaz Mustafa1, Guanyi Lu1, Andrew P Bunger1,2
1Department of Civil and Environmental Engineering, University of Pittsburgh, Pittsburgh 15261, Pennsylvania, United States.
This study enhances machine/deep learning (ML/DL) models for predicting in situ stress using low-frequency acoustic velocities derived from dry rock data. The improved workflow accurately estimates subsurface stress, advancing geothermal energy exploration.
Area of Science:
- Geophysics and Rock Mechanics
- Machine Learning Applications in Earth Sciences
Background:
- Accurate in situ stress estimation is crucial for subsurface engineering, including geothermal energy extraction.
- Traditional methods often rely on saturated rock data, but low-frequency interpretations may benefit from dry rock properties.
- The impact of frequency dispersion on velocity-stress relationships for in situ stress prediction remains an open question.
Purpose of the Study:
- To enhance machine/deep learning (ML/DL) workflows for in situ stress prediction.
- To investigate the efficacy of using Biot-Gassmann-derived equivalent saturated velocities from dry rock data for ML/DL model training.
- To assess the impact of low-frequency acoustic velocities on the accuracy of in situ stress prediction.
Main Methods:
- Acquisition of true triaxial ultrasonic velocity (TUV) data from dry core samples under various stress configurations.
- Application of Biot-Gassmann fluid substitution to derive equivalent saturated velocities from dry rock ultrasonic velocities.
- Training and validation of ML/DL models using the derived low-frequency equivalent saturated velocities and TUV data from Utah FORGE site cores.
Main Results:
- ML/DL models trained with equivalent saturated velocities achieved high predictive performance for in situ stress.
- Validation/testing yielded R-squared values of 0.86, 0.971, and 0.975 for vertical, minimum horizontal, and maximum horizontal stress, respectively.
- Shapley additive explanations (SHAP) analysis confirmed model reliability and improved scientific understanding of the velocity-stress relationship.
Conclusions:
- The enhanced ML/DL workflow using low-frequency acoustic velocities from dry rock is a viable and accurate method for in situ stress prediction.
- This approach offers a reliable alternative for interpreting lower frequency measurements in subsurface geological settings.
- The study validates the use of Biot-Gassmann theory in conjunction with ML/DL for robust geophysical stress analysis.
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