Asphalt internal structure characterization with X-Ray computed tomography
Application of Avizo Fire image processing for substances investigation inside porous medium
1. Application of Avizo Fire image
processing for substances investigation
Schlumberger Public
inside porous medium
A. Nadeev, I. Yakimchuk, D. Mikhailov, E. Chuvilin, D. Koroteev,
D. Korobkov, V. Shako
Schlumberger Moscow Research
1 / 13 SMR
2. X-ray attenuation bases
The value of linear attenuation coefficient (LAC) of every substance depends
on chemical composition, material density and X-ray radiation energy:
m (E)
Schlumberger Public
μm – mass attenuation coefficient at given X-ray radiation (E) energy (cm2/g),
ρ – material density (g/cm3)
I I 0e l
I – X-ray radiation intensity after l length propagation, I0 – initial X-ray radiation intensity,
μ – linear attenuation coefficient (cm-1), l – length of radiation propagation (cm)
The best solutions is application of X-ray contrast agents –
chemical composition change!
2 / 13 SMR
3. Aims
Exciting micro-CT images Additional/new measurements
• X-ray micro-CT based approach development for investigation of
Schlumberger Public
phases distribution inside porous space of rock samples
• identification of possible ways to improve X-ray contrast of phases (ice,
gas hydrate, clays and etc.) in porous medium:
to avoid disturbance of distribution or phases properties change
• application of X-ray contrast agents for distribution analysis of phases in 2D
and 3D micro-CT images using Avizo Fire software
3 / 13 SMR
4. Micro-CT experiment
• SkyScan-1172 (Bruker micro-CT, Belgium) micro-CT
scanner
• Parameters of our experiments:
• Source: 100 kV &100 A
• Filter: built-in Al+Cu
Sample
Schlumberger Public
• Pixel size resolution: 3.0-3.5 m
• 1200-1800 angular projections (3600)
• Modified Feldkamp reconstruction algorithm (Nrecon with
InstaRecon engine, GPU base reconstruction)
• Image processing and visualization: Avizo Fire 7.0.0, CTAn,
CTVox
• Special stages: SkyScan micro-CT cooling stage to
investigate ice saturated samples SkyScan-1172 micro-CT scanner equipped by
cooling stage
• Artificial and natural sandstones:
• Samples contains ice and/or clay phases
4 / 13 SMR
5. Method for contrast improvement: ice saturation with ions of
heavy metal
Cooling chamber, T = - 6oC
Sample
Diffusion coefficient of
Schlumberger Public
Pb(NO3)2 in ice is
0.2×10-5 cm2/sec-1
(Fick’s Law) Ice which contains
ions of heavy metal
1% Pb(NO3)2
Appropriate time for saturation of frozen sample with Pb2+ ions is about 1 week
5 / 13 SMR
6. Influence of heavy metal ions on ice visualization
spatial
resolution
is 3.2
Schlumberger Public
m/pixel
average
grain size
is 300 m
Micro-CT images of ice contained sand samples without contrast agent
(a) and saturated with lead ions (b)
6 / 13 SMR
7. Influence of heavy elements on clay visualization
a b
Schlumberger Public
A+B- +C+D-
ToC
spatial resolution is
A+1-xC+xB- 3.2 m/pixel
A+B- – clay and C+D- – contrast
agent compounds 5% water based clay
solution
Distribution of modified clay in dried (a) and wet sample (b)
7 / 13 SMR
8. Application of Avizo Fire filters for reconstructed slice of sand sample
Schlumberger Public
Experimental data
Non-Local Means Edge-Preserving
8 / 13 SMR
9. Image segmentation using Avizo Fire
Schlumberger Public
Non-Local Means Edge-preserving
9 / 13 SMR
10. Avizo Fire permeability calculation (XLab Hydro application)
“Experimental” permeability
in z direction for the model
400x400x200 voxels:
Schlumberger Public
Permeability of rock is
667 mD
Permeability of ice
saturated rock is 83 mD
10 / 13 SMR
11. Ice distribution analysis
Cutting from 3D image of sample
Schlumberger Public
Sample length, µm
Pore size distribution for two cases (15% of
humidity): rock matrix porosity and remain porosity
Ice content, % taking into account the pore ice
Cylinder height = 6 mm,
diameter = 3 mm
11 / 13 SMR
12. Clay distribution analysis
1 23 4 1 23 4
0.12 1
0.9
Concetration of clay
0.1
3 0.8
Void fraction, %
0.08 0.7
0.6
0.06 0.5
0.4
0.04
0.3
Schlumberger Public
0.02 0.2
0.1
0 0
0 1 2 3 4 5 6 0 1 2 3 4 5 6
Length of sample, mm Length from inlet, mm
1 2 3 4
Spatial resolution is 3.2 m/pixel There is a damage in sample inlet
12 / 13 SMR
13. Summary
• Special approaches for improvement X-ray contrast of phases inside rock porous medium
were developed: clay contrasting is based on ions interchange/ adsorption reactions, for ice
visualization is applied ions solid state diffusion
Bruker micro-CT scanner SkyScan 1172 equipped with cooling stage can be used for
Schlumberger Public
•
investigation unconsolidated or low consolidated reservoir rock, where ice in porous medium
plays role of natural cement
• Unconsolidated rock properties such as: porosity, pore size distribution, residual water
saturation and, finally, building adequate 3D digital model can be achieved in case of correct
matrix-ice segmentation due to Avizo Fire software application
• XLab Hydro extension of Avizo Fire 7.0.0 can be applied for permeability calculation of
phases invaded rock
13 / 13 SMR