name: pygimli
description: |
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.
version: 1.0.0
author: Geoscience Skills
license: MIT
tags: [Geophysical Inversion, ERT, Seismic Refraction, IP, Near-Surface, FEM]
dependencies: [pygimli>=1.4.0, numpy, matplotlib]
complements: [simpeg, verde, pyvista]
workflow_role: modelling
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
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
Scripts