Agent skill
pygimli
Multi-method geophysical modelling and inversion framework. Use when Claude needs to: (1) Perform electrical resistivity tomography (ERT) inversion, (2) Run seismic refraction tomography (SRT), (3) Model induced polarization (IP) data, (4) Simulate ground penetrating radar (GPR), (5) Create finite element meshes for geophysical problems, (6) Perform joint inversions of multiple datasets, (7) Forward model geophysical responses, (8) Analyze time-lapse monitoring data.
Install this agent skill to your Project
npx add-skill https://github.com/majiayu000/claude-skill-registry/tree/main/skills/other/other/pygimli
SKILL.md
pyGIMLi - Geophysical Inversion
Quick Reference
import pygimli as pg
from pygimli.physics import ert, srt
# Load ERT data
data = ert.load("survey.ohm")
# Invert
mgr = ert.ERTManager(data)
model = mgr.invert(lam=20, verbose=True)
# View result
mgr.showResult()
Key Classes
| Class | Purpose |
|---|---|
pg.Mesh |
Finite element meshes |
pg.DataContainer |
Survey data and geometry |
pg.Inversion |
Base inversion framework |
ert.ERTManager |
ERT processing and inversion |
srt.SRTManager |
Seismic refraction inversion |
Essential Operations
Load and View ERT Data
import pygimli as pg
from pygimli.physics import ert
data = ert.load("survey.ohm")
print(f"Measurements: {data.size()}")
ert.showData(data) # Pseudosection
ERT Inversion
from pygimli.physics import ert
mgr = ert.ERTManager(data)
model = mgr.invert(
lam=20, # Regularization
verbose=True
)
mgr.showResult()
resistivity = mgr.model
Seismic Refraction
from pygimli.physics import srt
data = srt.load("traveltimes.sgt")
mgr = srt.SRTManager(data)
model = mgr.invert(lam=30, zWeight=0.3)
mgr.showResult()
Create Custom Mesh
import pygimli as pg
from pygimli.physics import ert
data = ert.load("survey.ohm")
mesh = pg.meshtools.createParaMesh(
data.sensors(),
quality=34.0,
paraMaxCellSize=5,
boundary=2
)
pg.show(mesh)
Save and Export
# Save mesh and model
mgr.mesh.save("result_mesh.bms")
pg.save(model, "resistivity_model.vector")
# Export to VTK for ParaView
mgr.mesh.exportVTK("result", mgr.model)
Array Types
| Code | Array |
|---|---|
wa |
Wenner-alpha |
wb |
Wenner-beta |
dd |
Dipole-dipole |
pd |
Pole-dipole |
pp |
Pole-pole |
slm |
Schlumberger |
gr |
Gradient |
Data Formats
| Format | Extension | Description |
|---|---|---|
| BERT/pyGIMLi | .ohm | Unified data format |
| Syscal | .txt | IRIS export |
| Res2DInv | .dat | 2D inversion format |
| ABEM | .ohm | ABEM Terrameter |
| SRT | .sgt | Seismic traveltimes |
When to Use vs Alternatives
| Scenario | Recommendation |
|---|---|
| Standard ERT inversion with common arrays | pyGIMLi - simplest API, built-in array types |
| Seismic refraction tomography (SRT) | pyGIMLi - integrated SRT manager |
| Multi-method inversion (DC, magnetics, gravity, EM) | SimPEG - broader method coverage |
| Commercial ERT processing with reporting | Res2DInv - industry standard, GUI-based |
| Custom forward operators or research flexibility | SimPEG - more modular design |
| FEM-based geophysical modelling | pyGIMLi - native FEM mesh support |
Choose pyGIMLi when: You need near-surface geophysical inversion (ERT, SRT, IP) with
minimal code. Its manager classes (ERTManager, SRTManager) handle the full workflow
from data loading to inversion to visualization in a few lines.
Avoid pyGIMLi when: You need methods beyond near-surface (use SimPEG), or you require a commercial-grade reporting pipeline.
Common Workflows
ERT data inversion and visualization
- Load ERT data file with
ert.load("survey.ohm") - Inspect data: check measurement count with
data.size(), plot pseudosection - Remove outliers or bad data points
- Create
ERTManagerwith data - Run inversion:
mgr.invert(lam=20)(start with higher lambda) - Check chi-squared value (target ~ 1)
- Visualize result with
mgr.showResult() - Export mesh and model to VTK for ParaView:
mgr.mesh.exportVTK() - Adjust lambda and zWeight if needed, re-invert
Inversion Tips
- Start with higher lambda (50-100) and decrease
- Check data quality - remove outliers before inversion
- Use zWeight < 1 for layered structures
- Check coverage - low coverage = poorly resolved
- Chi-squared ~ 1 indicates good fit without overfitting
References
- Geophysical Methods - Supported methods and workflows
- Mesh Generation - Mesh creation and quality control
Scripts
- scripts/ert_inversion.py - Complete ERT inversion workflow
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