abinit
免费Generate 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.
中文简介正在准备中。当前显示原文说明。
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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.
中文简介正在准备中。当前显示原文说明。
Use when the user asks to place an adsorbate molecule on a surface, find adsorption sites, or set up a surface+adsorbate model for DFT.
中文简介正在准备中。当前显示原文说明。
Use when the user asks for adsorption energy, binding energy, or wants to compare how strongly a molecule binds to a surface.
中文简介正在准备中。当前显示原文说明。
Use when the user asks to analyze computational results: Gibbs free energy, OER/HER/CO2RR overpotentials, adsorption energy, convergence tests, DOS/d-band analysis, or Bader charge analysis.
中文简介正在准备中。当前显示原文说明。
Use AmberTools antechamber for molecular force field parameterization. Generates GAFF/GAFF2 parameters and AM1-BCC or RESP charges for use in AMBER or LAMMPS classical MD simulations.
中文简介正在准备中。当前显示原文说明。
One-shot recipes for adding, deleting, moving, and replacing individual atoms in the active CatGo viewer structure. Use whenever the user asks to "add an atom", "delete atoms", "remove this atom", "move atom N", "replace H with Li", or any single-atom edit — including "add a hydrogen on top of atom 12" / "delete atoms 5–9" / "swap the oxygen at site 3 for fluorine". Skips the discovery loop (no need to list structure tools or check adsorption sites first); goes straight to the matching `catgo_structure` action. Triggers in Chinese on 加原子, 删原子, 减原子, 移动原子, 替换原子, 增加氢, 删除氧, 把 ... 换成 ....
中文简介正在准备中。当前显示原文说明。