TY - JOUR
T1 - Physics-Informed Neural Network Method for Forward and Backward Advection-Dispersion Equations
AU - He, Qi Zhi
AU - Tartakovsky, Alexandre M.
N1 - Funding Information:
This research was partially supported by the U.S. Department of Energy (DOE) Advanced Scientific Computing (ASCR) program. Pacific Northwest National Laboratory is operated by Battelle for the DOE under Contract DE‐AC05‐76RL01830.
Publisher Copyright:
© 2021. American Geophysical Union. All Rights Reserved.
PY - 2021/7
Y1 - 2021/7
N2 - We propose a discretization-free approach based on the physics-informed neural network (PINN) method for solving the coupled advection-dispersion equation (ADE) and Darcy flow equation with space-dependent hydraulic conductivity (Formula presented.). In this approach, (Formula presented.), hydraulic head, and concentration fields are approximated with deep neural networks (DNNs). We assume that K(x) is given by its values on a grid, and we use these values to train the K DNN. The head and concentration DNNs are trained by minimizing the residuals of the flow equation and ADE and using the initial and boundary conditions as additional constraints. The PINN method is applied to one- and two-dimensional forward ADEs, where its performance for various Péclet numbers (Pe) is compared with the analytical and numerical solutions. We find that the PINN method is accurate with errors of less than 1% and outperforms some conventional discretization-based methods for large Pe. Next, we demonstrate that the PINN method remains accurate for the backward ADEs, with the relative errors in most cases staying under 5% compared to the reference concentration field. Finally, we show that when available, the concentration measurements can be easily incorporated in the PINN method and significantly improve (by more than 50% in the considered cases) the accuracy of the PINN solution of the backward ADE.
AB - We propose a discretization-free approach based on the physics-informed neural network (PINN) method for solving the coupled advection-dispersion equation (ADE) and Darcy flow equation with space-dependent hydraulic conductivity (Formula presented.). In this approach, (Formula presented.), hydraulic head, and concentration fields are approximated with deep neural networks (DNNs). We assume that K(x) is given by its values on a grid, and we use these values to train the K DNN. The head and concentration DNNs are trained by minimizing the residuals of the flow equation and ADE and using the initial and boundary conditions as additional constraints. The PINN method is applied to one- and two-dimensional forward ADEs, where its performance for various Péclet numbers (Pe) is compared with the analytical and numerical solutions. We find that the PINN method is accurate with errors of less than 1% and outperforms some conventional discretization-based methods for large Pe. Next, we demonstrate that the PINN method remains accurate for the backward ADEs, with the relative errors in most cases staying under 5% compared to the reference concentration field. Finally, we show that when available, the concentration measurements can be easily incorporated in the PINN method and significantly improve (by more than 50% in the considered cases) the accuracy of the PINN solution of the backward ADE.
KW - backward advection-dispersion equations
KW - data assimilation
KW - forward advection-dispersion equations
KW - physics-informed machine learning
KW - source identification
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U2 - 10.1029/2020WR029479
DO - 10.1029/2020WR029479
M3 - Article
AN - SCOPUS:85110073103
SN - 0043-1397
VL - 57
JO - Water Resources Research
JF - Water Resources Research
IS - 7
M1 - e2020WR029479
ER -