Polarity reversals in geodynamo simulations are triggered when stable stratification at the top of the core weakens subsurface upwellings, a kinematic control that decouples reversals from the interior force balance.
Accelerating Finite-temperature Kohn-Sham Density Functional Theory with Deep Neural Networks
1 Pith paper cite this work. Polarity classification is still indexing.
abstract
We present a numerical modeling workflow based on machine learning (ML) which reproduces the the total energies produced by Kohn-Sham density functional theory (DFT) at finite electronic temperature to within chemical accuracy at negligible computational cost. Based on deep neural networks, our workflow yields the local density of states (LDOS) for a given atomic configuration. From the LDOS, spatially-resolved, energy-resolved, and integrated quantities can be calculated, including the DFT total free energy, which serves as the Born-Oppenheimer potential energy surface for the atoms. We demonstrate the efficacy of this approach for both solid and liquid metals and compare results between independent and unified machine-learning models for solid and liquid aluminum. Our machine-learning density functional theory framework opens up the path towards multiscale materials modeling for matter under ambient and extreme conditions at a computational scale and cost that is unattainable with current algorithms.
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physics.geo-ph 1years
2025 1verdicts
CONDITIONAL 1representative citing papers
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Core-surface kinematic control of polarity reversals in advanced geodynamo simulations
Polarity reversals in geodynamo simulations are triggered when stable stratification at the top of the core weakens subsurface upwellings, a kinematic control that decouples reversals from the interior force balance.