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Few comments on top of my head.
Did you look at the first gradient to see roughly what it's trying to update? |
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@mloubout It seems I do something incorrect. If you have ideas... The gradient at any iteration looks like in picture below: Calculating single shot at position 5712m with 119 receivers [2500, 5450] gives the following image with the same velocity model and same 16 Hrz Ricker source wavelet: Also at each iteration I set gradient in water to 0: water_depth = Int(350) # meters
gradient[:, 1:Int(water_depth/d[2])] .= 0f0 Model grid spacings 6.25 |
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Hi,
I'm trying to obtain FWI results from Viking Graben line 12.
The problem is that the solution doesn't converge.
I would appreciate any help.
My setup: Ubuntu 20.04, 8 threads, 20 Gb RAM, Seismic Unix, OpenSeaSeis, Petrel.
link to processed data
Data description (geometry):
water depth about 330 m
number of samples in raw data: 1500 (in FWI I use only 3600 ms to fit in RAM)
sampling interval: 4 ms
each shot contains 119-120 receivers
about 1000 shots overall (in FWI I use records from SP 300 to SP 700)
SRC spacing = 25 m
GRP spacing = 25 m
distance from source to first receiver = 262 m
The processing:
tpow=2
f=1,5,70,80
,amps=0,1,1,0
The result (wells converted to time domain using VSP data, without doing Well-Tie: thus wells were transformed to time domain unreliably):

Then using prepared Vnmo, picked horizons, Dix formula and smooth filter I compute starting velocity model (Vinterval):

I cut the model up to about 4 km depth with spacings 12.5 m (equal to CDP step) with 8 Hrz signal or 6.25 m with about 16 Hrz signal to fit in my RAM and I use SEGY records up to 3600 ms.
To compute FWI I use the code:
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