MR011
Damage Evolution in Rock: Validation data sets and computational challenges

Session ID#: 76061

Session Description:
Machine learning (ML) is instrumental in the detection of anomalous and event signals from the evolution of fault/fractured systems caused by natural and engineered processes in the subsurface. Critical to emerging ML methods is linking these signatures to the underlying physics of damage to determine if failure is imminent. This requires the integration of diverse datasets and robust computational methods to identify and capture the measurable signatures and physics of failure. Few computational approaches for simulating damage have been verified against readily available experimental data, or have been validated via blind predictions of data sets ahead of data acquisition. This session will highlight: (1) experimental and field data related to damage evolution (acoustic emission, microseismicity, displacements, fluid pressure, flow, geochemical signatures); (2) comparison of computational models and experimental/borehole/field data that highlight model strengths and weaknesses; and (3) announcement of a damage mechanics computational challenge on damage evolution in brittle-ductile materials.
Index Terms:

3999 General or miscellaneous [MINERAL PHYSICS]
8010 Fractures and faults [STRUCTURAL GEOLOGY]
8020 Mechanics, theory, and modeling [STRUCTURAL GEOLOGY]
8164 Stresses: crust and lithosphere [TECTONOPHYSICS]


Primary Convener:  Laura J Pyrak-Nolte, Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States
Conveners:  Hongkyu Yoon, Sandia National Laboratories, Department of Geomechanics, Albuquerque, NM, United States, Joseph Morris, Lawrence Livermore National Laboratory, Livermore, CA, United States and Antonio Bobet, Purdue University, Lyles School of Civil Engineering, West Lafayette, IN, United States
Primary Liaison:  Laura J Pyrak-Nolte, Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States
 
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Liyang Jiang1, Hongkyu Yoon2, Antonio Bobet3 and Laura J Pyrak-Nolte1,3, (1)Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States, (2)Sandia National Laboratories, Department of Geomechanics, Albuquerque, NM, United States, (3)Purdue University, Lyles School of Civil Engineering, West Lafayette, IN, United States
 
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Benedikt Ahrens1, Mandy Duda2 and Erik H Saenger1,2, (1)Bochum University of Applied Sciences, International Geothermal Centre, Bochum, Germany, (2)Ruhr-University Bochum, Institute of Geology, Mineralogy, and Geophysics, Bochum, Germany
 
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Antonio Bobet, Purdue University, Lyles School of Civil Engineering, West Lafayette, IN, United States, Joseph Morris, Lawrence Livermore National Laboratory, Livermore, CA, United States, Hongkyu Yoon, Sandia National Laboratories, Department of Geomechanics, Albuquerque, NM, United States and Laura J Pyrak-Nolte, Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States
 
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Adriana Paluszny1, Robin Nicholas Thomas2 and Robert W. Zimmerman1, (1)Imperial College London, London, SW7, United Kingdom, (2)Imperial College London, London, United Kingdom
 
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Chven A Mitchell, Purdue University, Earth, Atmospheric and Planetary sciences, West Lafayette, IN, United States and Laura J Pyrak-Nolte, Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States
 
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Daniel Lizama1,2, Hongkyu Yoon3, Liyang Jiang4 and Laura J Pyrak-Nolte4, (1)University of Puerto Rico Mayaguez, Mayaguez, PR, United States, (2)Sandia National Laboratories, Geomechanics, Albuquerque, NM, United States, (3)Sandia National Laboratories, Department of Geomechanics, Albuquerque, NM, United States, (4)Purdue University, Department of Physics and Astronomy, West Lafayette, IN, United States
 
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