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Field data inversion (“Koenigsee”)#
This minimalistic example shows how to use the Refraction Manager to invert a field data set. Here, we consider the Koenigsee data set, which represents classical refraction seismics data set with slightly heterogeneous overburden and some high-velocity bedrock. The data file can be found in the pyGIMLi example data repository.
# We import pyGIMLi and the traveltime module.
import matplotlib.pyplot as plt
import pygimli as pg
import pygimli.physics.traveltime as tt
The helper function pg.getExampleData downloads the data set to a temporary location and loads it. Printing the data reveals that there are 714 data points using 63 sensors (shots and geophones) with the data columns s (shot), g (geophone), and t (traveltime). By default, there is also a validity flag.
data = pg.getExampleData("traveltime/koenigsee.sgt", verbose=True)
print(data)
[::::::::::::::::::::::::::::::::::::: 83% ::::::::::::::::::::::: ] 8193 of 9844 complete
[:::::::::::::::::::::::::::::::::::: 100% ::::::::::::::::::::::::::::::::::::] 9844 of 9844 complete
md5: 641890bb17cb2bdf052cbc348669dfd0
Data: Sensors: 63 data: 714, nonzero entries: ['g', 's', 't', 'valid']
Let’s have a look at the data in the form of traveltime curves.
fig, ax = plt.subplots()
lines = tt.drawFirstPicks(ax, data)
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We initialize the refraction manager.
mgr = tt.TravelTimeManager(data)
# Alternatively, one can plot a matrix plot of apparent velocities which is the
# more general function also making sense for crosshole data.
ax, cbar = mgr.showData()
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Finally, we call the invert method and plot the result.The mesh is created based on the sensor positions on-the-fly.
mgr.invert(secNodes=3, paraMaxCellSize=5.0,
zWeight=0.2, vTop=500, vBottom=5000, verbose=1)
fop: <pygimli.physics.traveltime.modelling.TravelTimeDijkstraModelling object at 0x7f0d12180f40>
Data transformation: Identity transform
Model transformation (cumulative):
0 Logarithmic LU transform, lower bound 0.0, upper bound 0.0
min/max (data): 3.5e-04/0.03
min/max (error): 3%/3%
min/max (start model): 2.0e-04/0.002
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inv.iter 0 ... chi² = 156.33
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inv.iter 1 ... chi² = 12.31 (dPhi = 91.50%) lam: 20.0
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inv.iter 2 ... chi² = 8.91 (dPhi = 27.37%) lam: 20.0
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inv.iter 3 ... chi² = 6.65 (dPhi = 24.90%) lam: 20.0
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inv.iter 4 ... chi² = 5.97 (dPhi = 9.74%) lam: 20.0
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inv.iter 5 ... chi² = 5.77 (dPhi = 3.11%) lam: 20.0
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inv.iter 6 ... chi² = 5.61 (dPhi = 2.58%) lam: 20.0
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inv.iter 7 ... chi² = 4.68 (dPhi = 15.28%) lam: 20.0
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inv.iter 8 ... chi² = 4.24 (dPhi = 8.77%) lam: 20.0
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inv.iter 9 ... chi² = 3.95 (dPhi = 6.13%) lam: 20.0
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inv.iter 10 ... chi² = 3.77 (dPhi = 4.11%) lam: 20.0
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inv.iter 11 ... chi² = 3.69 (dPhi = 1.82%) lam: 20.0
################################################################################
# Abort criterion reached: dPhi = 1.82 (< 2.0%) #
################################################################################
1090 [863.9110357958974,...,2658.608027494803]
Look at the fit between measured (crosses) and modelled (lines) traveltimes.
mgr.showFit(firstPicks=True)
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You can plot only the model and customize with a bunch of keywords
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You can play around with the gradient starting model (vTop and vBottom arguments) and the regularization strength lam and customize the mesh.
Total running time of the script: (0 minutes 20.662 seconds)