A higher-order finite element reactive transport model for unstructured and fractured grids
Abstract
Abstract This work presents a new reactive transport framework that combines a powerful geochemistry engine with advanced numerical methods for flow and transport in subsurface fractured porous media. Specifically, the PhreeqcRM interface (developed by the USGS) is used to take advantage of a large library of equilibrium and kinetic aqueous and fluid-rock reactions, which has been validated by numerous experiments and benchmark studies. Fluid flow is modeled by the Mixed Hybrid Finite Element (FE) method, which provides smooth velocity fields even in highly heterogenous formations with discrete fractures. A multilinear Discontinuous Galerkin FE method is used to solve the multicomponent transport problem. This method is locally mass conserving and its second order convergence significantly reduces numerical dispersion. In terms of thermodynamics, the aqueous phase is considered as a compressible fluid and its properties are derived from a Cubic Plus Association (CPA) equation of state. The new simulator is validated against several benchmark problems (involving, e.g., Fickian and Nernst-Planck diffusion, isotope fractionation, advection-dispersion transport, and rock-fluid reactions) before demonstrating the expanded capabilities offered by the underlying FE foundation, such as high computational efficiency, parallelizability, low numerical dispersion, unstructured 3D gridding, and discrete fraction modeling.
- Authors:
- Publication Date:
- Research Org.:
- The Ohio State Univ., Columbus, OH (United States)
- Sponsoring Org.:
- USDOE; USDOE Office of Fossil Energy (FE)
- OSTI Identifier:
- 1664561
- Alternate Identifier(s):
- OSTI ID: 1816368
- Grant/Contract Number:
- FEAA-045; AC05-00OR22725
- Resource Type:
- Published Article
- Journal Name:
- Scientific Reports
- Additional Journal Information:
- Journal Name: Scientific Reports Journal Volume: 10 Journal Issue: 1; Journal ID: ISSN 2045-2322
- Publisher:
- Nature Publishing Group
- Country of Publication:
- United Kingdom
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Moortgat, Joachim, Li, Mengnan, Amooie, Mohammad Amin, and Zhu, Di. A higher-order finite element reactive transport model for unstructured and fractured grids. United Kingdom: N. p., 2020.
Web. doi:10.1038/s41598-020-72354-3.
Moortgat, Joachim, Li, Mengnan, Amooie, Mohammad Amin, & Zhu, Di. A higher-order finite element reactive transport model for unstructured and fractured grids. United Kingdom. https://doi.org/10.1038/s41598-020-72354-3
Moortgat, Joachim, Li, Mengnan, Amooie, Mohammad Amin, and Zhu, Di. Wed .
"A higher-order finite element reactive transport model for unstructured and fractured grids". United Kingdom. https://doi.org/10.1038/s41598-020-72354-3.
@article{osti_1664561,
title = {A higher-order finite element reactive transport model for unstructured and fractured grids},
author = {Moortgat, Joachim and Li, Mengnan and Amooie, Mohammad Amin and Zhu, Di},
abstractNote = {Abstract This work presents a new reactive transport framework that combines a powerful geochemistry engine with advanced numerical methods for flow and transport in subsurface fractured porous media. Specifically, the PhreeqcRM interface (developed by the USGS) is used to take advantage of a large library of equilibrium and kinetic aqueous and fluid-rock reactions, which has been validated by numerous experiments and benchmark studies. Fluid flow is modeled by the Mixed Hybrid Finite Element (FE) method, which provides smooth velocity fields even in highly heterogenous formations with discrete fractures. A multilinear Discontinuous Galerkin FE method is used to solve the multicomponent transport problem. This method is locally mass conserving and its second order convergence significantly reduces numerical dispersion. In terms of thermodynamics, the aqueous phase is considered as a compressible fluid and its properties are derived from a Cubic Plus Association (CPA) equation of state. The new simulator is validated against several benchmark problems (involving, e.g., Fickian and Nernst-Planck diffusion, isotope fractionation, advection-dispersion transport, and rock-fluid reactions) before demonstrating the expanded capabilities offered by the underlying FE foundation, such as high computational efficiency, parallelizability, low numerical dispersion, unstructured 3D gridding, and discrete fraction modeling.},
doi = {10.1038/s41598-020-72354-3},
journal = {Scientific Reports},
number = 1,
volume = 10,
place = {United Kingdom},
year = {Wed Sep 23 00:00:00 EDT 2020},
month = {Wed Sep 23 00:00:00 EDT 2020}
}
https://doi.org/10.1038/s41598-020-72354-3
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