Estimating permeability of 3D micro-CT images by physics-informed CNNs
based on DNS
- URL: http://arxiv.org/abs/2109.01818v1
- Date: Sat, 4 Sep 2021 08:43:19 GMT
- Title: Estimating permeability of 3D micro-CT images by physics-informed CNNs
based on DNS
- Authors: Stephan G\"arttner and Faruk O. Alpak and Andreas Meier and Nadja Ray
and Florian Frank
- Abstract summary: This paper presents a novel methodology for permeability prediction from micro-CT scans of geological rock samples.
The training data set for CNNs dedicated to permeability prediction consists of permeability labels that are typically generated by classical lattice Boltzmann methods (LBM)
We instead perform direct numerical simulation (DNS) by solving the stationary Stokes equation in an efficient and distributed-parallel manner.
- Score: 1.6274397329511197
- License: http://creativecommons.org/licenses/by-sa/4.0/
- Abstract: In recent years, convolutional neural networks (CNNs) have experienced an
increasing interest for their ability to perform fast approximation of
effective hydrodynamic parameters in porous media research and applications.
This paper presents a novel methodology for permeability prediction from
micro-CT scans of geological rock samples. The training data set for CNNs
dedicated to permeability prediction consists of permeability labels that are
typically generated by classical lattice Boltzmann methods (LBM) that simulate
the flow through the pore space of the segmented image data. We instead perform
direct numerical simulation (DNS) by solving the stationary Stokes equation in
an efficient and distributed-parallel manner. As such, we circumvent the
convergence issues of LBM that frequently are observed on complex pore
geometries, and therefore, improve on the generality and accuracy of our
training data set. Using the DNS-computed permeabilities, a physics-informed
CNN PhyCNN) is trained by additionally providing a tailored characteristic
quantity of the pore space. More precisely, by exploiting the connection to
flow problems on a graph representation of the pore space, additional
information about confined structures is provided to the network in terms of
the maximum flow value, which is the key innovative component of our workflow.
As a result, unprecedented prediction accuracy and robustness are observed for
a variety of sandstone samples from archetypal rock formations.
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