Materials & chemistry

Atomistic Materials

Pretrain crystal potentials from scratch across eight physics suites.

Task & evaluation

Objective
Learn one model of atomic interactions that works across many physical settings.
Input
Elements, atomic positions and the repeating cell.
Output
Energy, forces and response to deformation.
Data
About 42 million structures labeled by quantum calculations.
Evaluation
Eight physical tests, from crystal stability to vibrations and ion migration.
Research challenge
Remain accurate when atoms move away from their resting arrangements.

Understanding the task

Follow one learned energy landscape from a stretching bond to the many physical properties it must explain.

Can one model describe many kinds of atomic motion?

Atoms in a material pull and push on one another. An interatomic potential predicts the energy of an arrangement and the forces that make it change. A fast, accurate potential can help simulate vibrations, deformation, heat transport and ion motion without repeating an expensive quantum calculation at every step.

The hard part is reliability away from familiar structures. Two models can agree near a crystal’s resting arrangement yet disagree when a bond stretches or an ion squeezes through a narrow passage. The interactive example shows how matching the bottom of an energy well can still miss the physics farther away.

INTERACTIVE · ONE LANDSCAPE, MANY PROBES

Same minimum. Different physics.

A harmonic fit and an anharmonic reference agree in energy, force and curvature at equilibrium. Move the atoms, then strain the cell to see where that agreement ends.

— Anharmonic reference┄ Candidate

1 · Distance → energy → force

Stretch a bond. The force on the right atom is F = −dE/dr; arrows point in the direction it would move.

Energy and force change with distance
Try r/r₀ = 1.60: a quadratic well keeps pulling harder, while a dissociating bond weakens. Matching local curvature can still miss higher-order physics.

2 · Cell strain → energy → stress

Change the horizontal cell length at fixed fractional coordinates. Every horizontal bond stretches together.

Strain probes the same energy landscape
Near zero strain the slopes agree. Finite deformation exposes differences. Elasticity probes stress response; MOF mechanics additionally uses evaluator-controlled volume scans and dispersion.

What this connects to in the task

Stability probes relaxed energies; phonons probe local curvature; conductivity needs higher-order force constants. Disorder, cleavage and migration visit other parts of the landscape. All eight suites reuse the same ASE calculator: total energy (eV), forces (eV/Å) and stress (eV/ų, positive tensile). The evaluator chooses the physical perturbations.

Synthetic illustration, not benchmark data or a materials simulator. Here r₀ = D = 1, Eref = (1 − exp[−2(r − 1)])² − 1 and Efit = 4(r − 1)² − 1. The cell is a 2D nearest-neighbor sketch; its dimensionless stress proxy is dEbond/dε, not a calculated 3D material stress. Controls explore a toy model, not alternative benchmark settings.

HOW THE REFERENCE MODEL WORKS

One learned energy surface, reused by every protocol

  1. 1 · StructureElements, atomic positions and repeating cell
  2. 2 · Learned representationLearn relationships between neighboring atoms
  3. 3 · Energy predictionThe energy surface determines forces and response to deformation
  4. 4 · Shared predictionsEnergy, forces and stress from one model
  5. 5 · Evaluator-controlled physicsRelaxations, displacements, strain, volume scans, surfaces and migration paths

Forces follow the slope of the energy surface. Matching a few energy values does not guarantee that its slopes and curvature are correct.

SCORING LAB · INVENTED FOUR-PATH EXAMPLE

A failed migration path still contributes error

Three ion-migration paths have absolute barrier errors of 0.10, 0.20 and 0.30 eV. Set the fourth path’s error, or mark it failed. The documented protocol caps each path’s error at 2 eV and assigns failures 2 eV.

All-path MAE = (0.10 + 0.20 + 0.30 + 0.40) / 4 = 0.25 eV

This is arithmetic teaching data, not a measured material or actual NEB run. An unconverged but finite path is separate from an exception: the evaluator additionally reports converged-only error and convergence fraction. The eight-suite task has no aggregate score.

What the model learns from

The training pool contains about 42 million atomic configurations from several quantum-calculation datasets. Some follow crystals relaxing toward equilibrium; others deliberately displace atoms or simulate their motion. Each example supplies an arrangement, its energy, forces and stress—the internal response to deforming the cell.

More data does not automatically mean better supervision. Different calculations can use different energy references and approximations. The task separates evaluation materials from training, with structure-level separation for several amorphous systems whose compositions remain represented.

The results below concern pretrained UMA models and subsequent adaptation. They illustrate physical tradeoffs but do not establish performance under the newer requirement to learn from scratch.

Technical details
Training pool in the documented release; counts are after filtering, not the fine-tuning sample
SourceFramesPhysical coverage and label caveat
MPtrj1,065,435Crystal relaxation trajectories; MP PBE/PBE+U, 520 eV
sAlex9,434,535Alexandria subsample; MP-compatible PBE/PBE+U
MatPES-PBE 2025.1193,171DIRECT-sampled MD, 85 elements; PBE without +U, 680 eV
OMat2431,716,685Rattled, rattled-relax and AIMD; different pseudopotentials and energy offsets
Total42,409,82691 GB; a shared pool, not a requirement to train on every frame

Eight views of the same landscape

Stability screening asks which structures resist decomposition. Vibrations probe local curvature; elasticity probes response to strain. Heat conductivity depends on more complex interactions between vibrations. Flexible frameworks, disordered solids, cleaved surfaces and ion migration explore still other regions of the energy landscape.

The task reports fifteen physical metrics rather than averaging incompatible units into one score. A model can improve discovery accuracy while making dynamics worse. Failed calculations also matter: an accurate answer on the easy cases is insufficient if difficult simulations break.

Technical details
What each suite measures
SuiteValidation / testWhat is measured
Stability screening1,000 / 5,000Stable/unstable F1; hull-distance MAE (meV/atom)
Phonons300 / 500Maximum and mean frequency (K); entropy/heat capacity (J/K/mol); free energy (kJ/mol)
Elasticity300 / 500Bulk and shear modulus MAE (GPa)
Thermal conductivity40 / 63Conductivity SRME at 300 K
MOF mechanics40 / 60Bulk-modulus MAPE; evaluator adds D3(BJ)
Amorphous solids376 / 558 structuresEnergy and force relative RMSE, averaged over five systems
Surfaces2,000 / 2,000 slabsCleavage relative MAE; disjoint bulk materials
Ion migration256 / 390 pathsBarrier MAE (eV); all paths, converged paths and convergence fraction

Learning an energy landscape

The reference model learns an energy surface over atomic arrangements. Its slope gives forces: atoms tend to move downhill. How that slope changes determines vibrations and other responses. Accurate energies at a few points therefore do not guarantee accurate motion between them.

One experiment adapts the model to Materials Project data near familiar crystals. Another replaces half the training examples with displaced structures from OMat24. For those additional examples it learns from forces and stress, avoiding incompatible energy references. The idea is to retain knowledge of configurations that atoms visit away from equilibrium.

Every evaluation uses the same potential. Researchers cannot choose a different model for each physical property, making this a test of broad reliability.

A clear tradeoff, not a universal improvement

Adapting UMA to Materials Project data raises stability-screening F1—a combined measure of finding stable materials and avoiding false alarms—from 0.54 to 0.86, but increases several physical errors. Adding displaced structures partly repairs heat-conductivity and framework-mechanics performance. It does not solve the whole problem.

For example, the mixed-data model lowers conductivity error by about 11% relative to the Materials Project adaptation, while increasing the maximum-vibration-frequency error by about 18%. Better performance in one part of the landscape can coexist with worse local curvature elsewhere.

The original Materials Project adaptation included a small overlap with later evaluation materials: about 0.2% of training frames. Treat it as a historical diagnostic, not a clean current-protocol baseline. Multiple training seeds and a from-scratch comparison are still missing.

Detailed physical results
Historical test references; lower is better except F1
MetricOriginal UMACrystal-focused trainingMixed-data training
Discovery F10.540.860.86
Phonon max-frequency MAE, K7.947.155.5
Conductivity SRME0.280.440.39
MOF modulus MAPE25.2%25.0%21.4%
AM26 force relative RMSE11.8%14.7%14.1%
NEB barrier MAE, eV0.1260.1260.134

Compute and resources

Materials adaptation

Reported measurement

≈18.1 GPU-h
Time
2 h 16 min
Hardware
8 × H100
GPU allocation
≈18.1 GPU-h

Training on material configurations.

Elapsed time by stage

Materials adaptation
136 min

No finer stage timing is reported for this workload. Separate cards describe separate measurements, not parts of one total.

Original pretraining is excluded.

Mixed-data adaptation

Reported measurement

≈18.3 GPU-h
Time
2 h 17 min
Hardware
8 × H100
GPU allocation
≈18.3 GPU-h

Training with a broader mixture of atomic environments.

Elapsed time by stage

Mixed-data adaptation
137 min

No finer stage timing is reported for this workload. Separate cards describe separate measurements, not parts of one total.

A separate alternative run, not an additional stage.

Mixed-data preparation

Reported measurement

16 min
Time
16 min
Hardware
96 workers
GPU allocation
Not applicable (CPU stage)

Preparing the broader training mixture.

Elapsed time by stage

Data preparation
16 min

No finer stage timing is reported for this workload. Separate cards describe separate measurements, not parts of one total.

Full physical evaluation

Reported measurement

6 h 18 min
Time
6 h 18 min
Hardware
8 × H100, shared with three other evaluation jobs
GPU allocation
Not established (shared GPUs)

All eight test suites for the mixed-data model.

Elapsed time by stage

MOF
159 min
Physical tests
104 min
NEB
85 min
Conductivity
28 min

The bar covers the four timed major suites (6 h 16 min). The reported full evaluation is 6 h 18 min; minor suites and rounding are not assigned invented durations. GPUs were shared.

Shared hardware: this timing is not an exclusive GPU-hours measurement. Largest components: MOF 2 h 39 min, physical tests 1 h 44 min, NEB 1 h 25 min and conductivity 28 min.

Learning from the failures

The next question is which atomic arrangements are missing from training. Sampling more distorted structures may help bond breaking and migration, while examples chosen to reveal curvature may help vibrations. Controlled comparisons should check all physical suites: improving force error alone is not enough to claim a better universal potential.

References and provenance

UMA: A Family of Universal Models for Atoms

Introduces the model family used to predict atomic energies and forces across different kinds of matter.

Task definition and experimental evidence

Documents the mixed training data and physical tests used here. These measurements use a different protocol from the public paper results.

Task description and code

Code links require access to the project’s GitHub repository.

Leaderboard

Simulated

Design preview · leaderboard values and research histories are simulated.

Agent search and reference methods ranked together by Discovery F1.
#MethodTypeDiscovery F1 ↑Force MAE ↓Energy MAE ↓Research timeRun
1Agent search0.66050.54050.699176 h
2Agent search0.65730.54310.702560 h
3UMA-S-1.1 (MP + OMat24 mixed replay)Reference0.65500.54500.7050——
4UMA-S-1.1 (zero-shot)Reference0.53710.66460.8598——
How to read these leaderboard metrics

These leaderboard values and research histories are simulated design examples. The leaderboard is ranked by Discovery F1. The research curves show relative improvement in this metric over UMA-S-1.1 (MP + OMat24 mixed replay); only accepted new-best results update the retained trajectory. A positive gain means a better result, with the sign adjusted for metrics where lower is better. The task protocol is described in Task & evaluation above. These preview columns and trajectories are not measured benchmark results and must not be compared with the recorded experiments. The leaderboard and agent-search curves are simulated UI examples, not measured benchmark runs. Its three columns do not represent the documented 15-metric, eight-suite protocol, which has no aggregate score. Historical measured results, units, training eligibility caveats and failure handling appear in Understanding the task; leaderboard baseline labels must not be read as those measurements.

Discovery F1Primary metric · Higher is better
Balances precision and recall when identifying stable candidate materials. A high score requires finding useful candidates while limiting false positives.
Force MAELower is better
Mean absolute difference between predicted and reference atomic forces. It measures local force accuracy rather than material-discovery performance.
Energy MAELower is better
Mean absolute difference between predicted and reference energies. Interpret values using the units and normalization in the task protocol.