abinit
FreeGenerate and manage ABINIT DFT calculations. Use when the user requests ABINIT, or needs DFPT phonons, GW calculations, or BSE optical spectra.
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VASP vibrational frequency calculation. Compute ZPE and thermodynamic corrections. Handles frozen atoms for slab systems with multiple freeze modes.
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Compute vibrational frequencies using finite differences. Used for zero-point energy (ZPE), thermodynamic corrections, and checking transition states.
🔴 Must discuss with user:
🟡 Recommend confirming:
🟢 Safe defaults:
from catgo.workflow import Workflow
from catgo.workflow.builtins import geo_opt, freq, gibbs_energy
wf = Workflow("Frequency calculation")
struct = wf.add_task("structure_input", structure=optimized_json)
frq = wf.add_task(freq, structure=struct.output.structure,
system_name="CO_gas")
wf.submit()
MCP equivalent:
catgo_workflow_engine(action="create", params={"name": "Frequency calc"})
catgo_workflow_engine(action="add_task", params={
"workflow_id": "wf_xxx",
"task_type": "structure_input",
"structure": "<optimized_json>"
})
catgo_workflow_engine(action="add_task", params={
"workflow_id": "wf_xxx",
"task_type": "freq",
"software": "vasp",
"structure": "{{t_001.output.structure}}",
"system_name": "CO_gas"
})
catgo_workflow_engine(action="submit", params={"workflow_id": "wf_xxx"})
For adsorbates on surfaces, freeze the slab atoms and only compute frequencies for the adsorbate (and optionally top surface layer). This dramatically reduces cost.
| Mode | Description | Example |
|---|---|---|
"none" | All atoms vibrate (gas-phase molecules) | Small molecules |
"layers" | Freeze bottom N layers by z-coordinate | freeze_mode="layers", freeze_layers=4 |
"z_range" | Freeze atoms below a z threshold | freeze_mode="z_range", freeze_z_below=8.0 |
"element" | Freeze specific elements | freeze_mode="element", freeze_elements=["Ru", "O"] |
"indices" | Freeze specific atom indices | freeze_mode="indices", freeze_indices=[0,1,2,3] |
"manual" | Use selective_dynamics from structure | Pre-set in POSCAR |
For a typical slab with adsorbate:
opt = wf.add_task(geo_opt, structure=slab_oh_json,
ISIF=2, freeze_layers=2, system_name="*OH")
frq = wf.add_task(freq, structure=opt.output.structure,
freeze_mode="layers",
freeze_layers=4, # Freeze bottom 4 layers (all slab atoms)
system_name="*OH")
Why freeze_layers=4 for freq but freeze_layers=2 for geo_opt?
Useful when layer detection is ambiguous:
frq = wf.add_task(freq, structure=opt.output.structure,
freeze_mode="z_range",
freeze_z_below=12.5, # Angstrom
system_name="*OH")
The standard thermodynamics workflow:
wf = Workflow("OH adsorption Gibbs energy")
struct = wf.add_task("structure_input", structure=slab_oh_json)
# Step 1: Optimize geometry
opt = wf.add_task(geo_opt, structure=struct.output.structure,
ISIF=2, freeze_layers=2, system_name="*OH")
# Step 2: Frequency on optimized structure
frq = wf.add_task(freq, structure=opt.output.structure,
freeze_mode="layers", freeze_layers=4,
system_name="*OH")
# Step 3: Gibbs energy from DFT energy + frequencies
gib = wf.add_task(gibbs_energy,
energy=opt.output.energy,
frequencies=frq.output.frequencies,
phase="adsorbed", # Harmonic approximation for adsorbates
temperature=298.15, # K
freq_cutoff=50, # cm-1, replace low freqs with this value
system_name="*OH")
wf.submit()
For free molecules (H2, H2O, CO, etc.), do NOT freeze any atoms:
frq = wf.add_task(freq, structure=molecule_json,
freeze_mode="none", # All atoms vibrate
system_name="H2O_gas")
gib = wf.add_task(gibbs_energy,
energy=opt.output.energy,
frequencies=frq.output.frequencies,
phase="gas", # Ideal gas partition function
system_name="H2O_gas")
Gas vs adsorbed phase:
phase="adsorbed": harmonic approximation, frustrated translations/rotations replaced by freq_cutoffphase="gas": ideal gas approximation with translational + rotational contributions| Parameter | Default | Purpose |
|---|---|---|
| IBRION | 5 | Finite differences |
| NFREE | 2 | Central differences (2-point) |
| POTIM | 0.015 | Displacement step size (Angstrom) |
| EDIFF | 1e-6 | Tight SCF convergence (tighter than geo_opt) |
| LREAL | .FALSE. | Must be exact for frequencies |
LREAL=.FALSE. is mandatory. Real-space projection introduces noise in forces that corrupts finite-difference frequencies. The config default overrides LREAL=Auto for freq tasks.
# Check frequencies after completion
catgo_analyze(action="frequencies", params={"task_id": "t_freq"})
# Returns: list of frequencies (cm-1), ZPE, imaginary modes
# Get raw result
catgo_workflow_engine(action="get_result", params={"task_id": "t_freq"})
# Returns: {"frequencies": [...], "zpe": 0.543}
The freq task produces:
output.frequencies — list of vibrational frequencies in cm-1 (negative = imaginary)output.zpe — zero-point energy in eV| Problem | Fix |
|---|---|
| Many imaginary frequencies | Structure not converged — re-optimize with tighter EDIFFG=-0.01 |
| One imaginary frequency | Could be a transition state (expected) or shallow minimum — check mode |
| Frequencies seem wrong | Ensure LREAL=.FALSE. and EDIFF=1e-6 |
| Calculation too expensive | Freeze more atoms (increase freeze_layers) |
| Numeric noise in frequencies | Reduce POTIM to 0.01 or increase NFREE to 4 |
Frequency calculations require 6N single-point calculations where N is the number of free atoms (with NFREE=2). For a 5-atom adsorbate on a frozen slab, that is 30 SCF calculations — roughly 30x the cost of a single point.
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Generate and manage ABINIT DFT calculations. Use when the user requests ABINIT, or needs DFPT phonons, GW calculations, or BSE optical spectra.
The English summary is being prepared. Showing the original description.
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