38 Geoscience and Hydrogeology in the AI Era: From Predictive Models to Real-Time Applications
This session offers a unique platform to showcase advancements in Artificial Intelligence (AI), Machine Learning (ML), and physics-informed methodologies, focusing on topics in hydrogeology, subsurface flow and transport, real-time geophysical inversion, critical minerals, and energy applications.
Sunday, 19 October 2025
1:30 PM - 5:30 PM
HBGCC, 210AB
Physics-Informed Neural Network Framework for Modeling Flow in Dual-Pore Porous Media
Paper number: 38-11
Program: Technical Sessions
Time: 4:20 PM – 4:35 PM
Authors
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Kalyana NakshatralaUniversity of Houston, HOUSTON, TX
Abstract
Porous media span a remarkably diverse range of systems—including fractured carbonate reservoirs, ultra-tight shale formations, architected metallic foams, tissue-engineering scaffolds, and even plant xylem conduits. In many of these environments, flow and transport processes are governed by two hierarchically distinct but hydraulically coupled pore domains: a larger, highly permeable network that serves as the main conduit for flow, and a finer, more tortuous micro-pore network that controls storage, diffusion, and exchange dynamics. To accurately capture the resulting multiscale mass and solute transfer, the double-porosity/permeability (DPP) framework offers a powerful modeling approach. However, classical discretization methods—such as finite volume, finite difference, or finite element techniques—are often inadequate for workflows requiring rapid scenario screening, real-time data assimilation, or high-dimensional inverse analysis under sparse and noisy observations. In this talk, we introduce a physics-informed neural network (PINN) framework tailored to address these limitations. The method employs a shared neural backbone through which residual-balancing dynamically reconciles competing physical constraints. An error-guided collocation strategy further enhances accuracy by adaptively concentrating sampling points near steep pressure gradients and evolving flow fronts. Representative numerical results demonstrate that this mesh-free formulation offers multiple performance advantages: it resolves discontinuities without artificial diffusion, maintains numerical stability under extreme permeability contrasts, and avoids the spurious oscillations commonly observed in traditional mixed-element schemes.A particularly attractive feature of the proposed framework is its adaptability: the network can be incrementally retrained as new laboratory measurements, wireline logs, or in-situ sensor data become available. This enables continuously updated forecasting capabilities for critical applications such as critical-mineral extraction, tight-shale production, CO₂ and hydrogen storage integrity, and geothermal heat-exchange optimization.
Geological Society of America Abstracts with Programs. Vol. 57, No. 6
doi: 10.1130/abs/2025AM-413842
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