A multiscale multi-permeability poroplasticity model linked by recursive homogenizations and deep learning
Abstract
Many geological materials, such as shale, mudstone, carbonate rock, limestone and rock salt are multi-porosity porous media in which pores of different scales may co-exist in the host matrix. When fractures propagate in these multi-porosity materials, these pores may enlarge and coalesce and therefore change the magnitude and the principal directions of the effective permeability tensors. The pore-fluid inside the cracks and the pores of host matrix may interact and exchange fluid mass, but the difference in hydraulic properties of these pores often means that a single homogenized effective permeability tensor field is insufficient to characterize the evolving hydraulic properties of these materials at smaller time scale. Furthermore, the complexity of the hydro-mechanical coupling process and the induced mechanical and hydraulic anisotropy originated from the micro-fracture and plasticity at grain scale also makes it difficult to propose, implement and validate separated macroscopic constitutive laws for numerical simulations. Here this article presents a hybrid data-driven method designed to capture the multiscale hydro-mechanical coupling effect of porous media with pores of various different sizes. At each scale, data-driven models generated from supervised machine learning are hybridized with classical constitutive laws in a directed graph that represents the numerical models. By using sub-scalemore »
- Authors:
-
- Columbia University, New York, NY (United States)
- Publication Date:
- Research Org.:
- Columbia Univ., New York, NY (United States)
- Sponsoring Org.:
- USDOE Office of Nuclear Energy (NE), Nuclear Energy University Program (NEUP); Army Research Office (ARO); US Air Force Office of Scientific Research (AFOSR); USDOE
- OSTI Identifier:
- 1538120
- Alternate Identifier(s):
- OSTI ID: 1548754
- Grant/Contract Number:
- NE0008534; W911NF-15-1-0581; FA9550-17-1-0169
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Computer Methods in Applied Mechanics and Engineering
- Additional Journal Information:
- Journal Volume: 334; Journal Issue: C; Journal ID: ISSN 0045-7825
- Publisher:
- Elsevier
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 42 ENGINEERING; dual-porosity; data-driven modeling; directed graph; embedded discontinuity; recurrent neural network; multiscale method
Citation Formats
Wang, Kun, and Sun, WaiChing. A multiscale multi-permeability poroplasticity model linked by recursive homogenizations and deep learning. United States: N. p., 2018.
Web. doi:10.1016/j.cma.2018.01.036.
Wang, Kun, & Sun, WaiChing. A multiscale multi-permeability poroplasticity model linked by recursive homogenizations and deep learning. United States. https://doi.org/10.1016/j.cma.2018.01.036
Wang, Kun, and Sun, WaiChing. Sat .
"A multiscale multi-permeability poroplasticity model linked by recursive homogenizations and deep learning". United States. https://doi.org/10.1016/j.cma.2018.01.036. https://www.osti.gov/servlets/purl/1538120.
@article{osti_1538120,
title = {A multiscale multi-permeability poroplasticity model linked by recursive homogenizations and deep learning},
author = {Wang, Kun and Sun, WaiChing},
abstractNote = {Many geological materials, such as shale, mudstone, carbonate rock, limestone and rock salt are multi-porosity porous media in which pores of different scales may co-exist in the host matrix. When fractures propagate in these multi-porosity materials, these pores may enlarge and coalesce and therefore change the magnitude and the principal directions of the effective permeability tensors. The pore-fluid inside the cracks and the pores of host matrix may interact and exchange fluid mass, but the difference in hydraulic properties of these pores often means that a single homogenized effective permeability tensor field is insufficient to characterize the evolving hydraulic properties of these materials at smaller time scale. Furthermore, the complexity of the hydro-mechanical coupling process and the induced mechanical and hydraulic anisotropy originated from the micro-fracture and plasticity at grain scale also makes it difficult to propose, implement and validate separated macroscopic constitutive laws for numerical simulations. Here this article presents a hybrid data-driven method designed to capture the multiscale hydro-mechanical coupling effect of porous media with pores of various different sizes. At each scale, data-driven models generated from supervised machine learning are hybridized with classical constitutive laws in a directed graph that represents the numerical models. By using sub-scale simulations to generate database to train material models, an offline homogenization procedure is used to replace the up-scaling procedure to generate cohesive laws for localized physical discontinuities at both grain and specimen scales. Through a proper homogenization procedure that preserves spatial length scales, the proposed method enables field-scale simulations to gather insights from meso-scale and grain-scale micro-structural attributes. This method is proven to be much more computationally efficient than the classical DEM–FEM or FEM2 approach while at the same time more robust and flexible than the classical surrogate modeling approach. Due to the usage of bridging-scale technique, the proposed model may provide multiple opportunities to incorporate different types of simulations and experimental data across different length scales for machine learning. Numerical issues will also be discussed.},
doi = {10.1016/j.cma.2018.01.036},
journal = {Computer Methods in Applied Mechanics and Engineering},
number = C,
volume = 334,
place = {United States},
year = {Sat Feb 10 00:00:00 EST 2018},
month = {Sat Feb 10 00:00:00 EST 2018}
}
Web of Science
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