Calculate equilibrium phases, their molar fractions, and compositions from a local thermodynamic database using pycalphad. Compare temperatures, check material balance and sampling stability, and export results with recorded conditions and database identifiers.
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Computes finite-temperature CALPHAD equilibria, phase fractions, and phase compositions from thermodynamic TDB databases using pycalphad. Use for alloy phase stability, equilibrium temperature sweeps, tie lines, lever-rule checks, or reproducible phase-fraction calculations with explicit components and mole-fraction conditions.
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Use for equilibrium phase fractions and compositions at a fixed bulk elemental mole composition, specified pressure, and a list of finite temperatures. The bundled helper executes real pycalphad equilibria, checks mass balance, repeats at greater sampling density, and exports each stable composition set separately.
Equilibrium is constrained by the selected database, components, phases, and conditions. It does not predict precipitation rates, retained metastable microstructures, or properties of phases missing from the database. Successful numerical checks do not establish the database's experimental accuracy.
VA where required by sublattice models. Vacancies are not an independent bulk
mole fraction. Keep coupled order/disorder definitions in the TDB, but do not select
both partners as separate candidates when the ordered model already includes the
disordered contribution; the helper rejects such filtered candidate lists.1 - sum(independent fractions); fractions are not silently normalized. Set K and Pa.
Convert weight percentages or mass fractions before using this helper.database_temperature_range_k to null if unknown. This is user-supplied evidence,
not a range automatically inferred from every TDB function. Requests outside a declared
interval fail. Check pressure and composition validity separately.pdens (phase-constitution
sampling density). Near transitions, refine temperatures and sampling density further.Read references/model-and-validation.md for the analytic example, basis conversion, native Model/Workspace/property/plot contracts, miscibility-gap handling, and convergence limits.
From the collection root:
uv run --no-project --python 3.12 --with pycalphad==0.11.2 --with numpy==2.5.3 \
python skills/pycalphad/scripts/equilibrate.py \
skills/pycalphad/assets/ideal-cu-ni.tdb \
skills/pycalphad/assets/equilibrium.json equilibrium-result
Tested on Python 3.12, pycalphad 0.11.2, and NumPy 2.5.3. Use a new output directory. All thermodynamic calculations are local; the script does not upload a TDB.
For the supplied hypothetical model at X(Ni)=0.5 and 101325 Pa:
| Temperature | Equilibrium result |
|---|---|
| 900 K | FCC_A1 only |
| 1100 K | 0.5 FCC_A1 + 0.5 LIQUID; X(Ni) approximately 0.527307 and 0.472693 respectively |
| 1300 K | LIQUID only |
The suite verifies analytic common-tangent compositions, a noncentral lever-rule case, Gibbs energy, mass balance, both single-phase limits, and actual same-phase miscibility gap vertices. These validate the computational workflow, not real Cu-Ni metallurgy.
report.json: settings and versions, TDB/settings SHA-256, excluded database phases,
requested, solver-imposed, and reconstructed bulk compositions, per-temperature
baseline/refined results, and checks. Experimental validity is not evaluated by the helper.phase-equilibria.csv: one row per stable vertex per temperature and sampling run,
including phase name, molar phase fraction, and elemental mole fractions. Its Gibbs
energy column is the whole-system molar Gibbs energy, repeated for each vertex;
it is not the individual phase energy.Unused pycalphad vertices have blank names and NaN values; those are omitted. Named vertices with invalid values cause failure. Multiple vertices with the same phase name are retained because a miscibility gap can contain two composition sets of one phase. Vertex indices do not track the same physical phase continuously across temperatures.
In stable 0.11.2, pycalphad clips independent mole fractions to [1e-10, 1-1e-10].
Each result records solver_bulk_mole_fractions and the largest absolute difference
from the requested bulk in composition_condition_adjustment_absolute_error.
Mass-balance checks still compare against the requested composition; a tighter
tolerance can therefore fail at an endpoint. Do not claim exact pure-component or
ultratrace results from a clipped multicomponent calculation.
all_checks_passed requires each run's phase-sum and bulk-composition residuals within
mass_balance_tolerance, phase totals stable within phase_fraction_tolerance, and
system Gibbs energy stable within gibbs_energy_tolerance_j_per_mol when pdens doubles.
This comparison does not certify the global minimum or track individual composition-set
movement within a same-phase miscibility gap; inspect their exported compositions too.
Failed checks remain visible in the report rather than being relabeled as convergence.
The helper handles elemental mole fractions, one composition, one pressure, and up to 1000 explicit positive temperatures. It validates selected phases through pycalphad's phase-compatibility rules; incompatible or automatically filtered order/disorder phase sets produce an explicit error. It does not silently remove requested phases.
Charged-species constraints, externally imposed chemical potentials, custom models, activity reference-state changes, and database optimization require additional modeling and are outside this helper's tested scope. Do not extrapolate the pedagogical asset to real material selection or heat-treatment decisions.
Upstream latest documentation currently describes 0.11.3 development builds. The
bundled helper and the reference's native examples were exercised against stable
0.11.2 on 2026-10-01; the release's source was checked against the installed wheel.
No remote thermodynamic calculation or database-fetch API is used. Database loads a
local path, file-like object, or TDB text; a URL is not a supported download shortcut.
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