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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
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
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
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
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
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
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
Application of Avizo Fire filters for reconstructed slice of sand sample




                                                                       Schlumberger Public
                             Experimental data
           Non-Local Means                          Edge-Preserving
  8 / 13                            SMR
Image segmentation using Avizo Fire




                                                        Schlumberger Public
         Non-Local Means              Edge-preserving




9 / 13                     SMR
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
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
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
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

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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