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Takbiri-shale Gas AAPG

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MULTISCALE MODELING OF GAS TRANSPORT AND STORAGE IN SHALE RESOURCES Ali Takbiri-Borujeni 12/02/2014
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Page 1: Takbiri-shale Gas AAPG

MULTISCALE MODELING OF GAS TRANSPORT AND STORAGE IN

SHALE RESOURCES

Ali Takbiri-Borujeni

12/02/2014

Page 2: Takbiri-shale Gas AAPG

WHAT TO EXPECT

An introduction to gas transport modeling techniques and their complexities at different scales.

2

http://geologycafe.com/stories/frackin.html

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DIFFERENT SCALES IN SHALE GAS RECOVERY

3 1- Ruppel and Loucks (2008)

1

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FLOW REGIME CHARACTERIZATION

Gas flow regimes are characterized by the Knudsen number (Kn). Flow regimes are1:

continuum flow (0 < Kn < 10−3)

slip flow (10−3 < Kn < 10−1)

transition flow (10−1 < Kn < 10)

free molecular flow (10 < Kn < ∞)

4 1- Roy, S., R. Raju, H. F. Chuang, B. A. Cruden, and M. Meyyappan (2003). Modeling gas flow through microchannels and nanopores. Journal of applied physics 93 (8) 2- Kang, S. M., E. Fathi, R. J. Ambrose, I. Y. Akkutlu, R. F. Sigal, et al. (2011). Carbon dioxide storage capacity of organic-rich shales. Spe Journal 16 (4), 842-855

In organic nanopores in shale, Knudsen number is larger than 0.1 2.

Page 5: Takbiri-shale Gas AAPG

ORGANIC MATTER (KEROGEN)

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Knudsen number is larger than 0.1. Slip or transition flow regimes

Organic-rich shale are suitable for gas adsorption due to their large surface areas. Cause new transport effects, such as

pore-diffusion and surface-diffusion effects

Ruppel and Loucks (2008)

Page 6: Takbiri-shale Gas AAPG

EXAMPLE: REDUCED-ORDER BOLTZMANN EQUATION

Regularized 13-moment (R13) method: a set of 13 differential equations are

derived from the moments of Boltzmann equation

solutions to these equations provide fluid flow equations for Kn 1

6

Page 7: Takbiri-shale Gas AAPG

BOUNDARY CONDITIONS

Three types of gas-surface interactions1: Specular reflection tangential velocity of the molecule remains constant

normal velocity component changes its sign

Trapping molecules lose their translational energy as they

collide with the surface

molecules will stay on the surface (few picoseconds)

Sticking molecules hit the surface, lose their energy

they stay on the surface for a reasonable amount of time (few nanoseconds)

7 1- Masel, R. I. (1996). Principles of adsorption and reaction on solid surfaces, Volume 3. John Wiley & Sons.

Page 8: Takbiri-shale Gas AAPG

SORPTION MODELING

8

Langmuir isotherm

Myong, R. S. (2004). Gaseous slip models based on the Langmuir adsorption isotherm. Physics of Fluids, 16(1), 104.

Gas sorption capacity is defined by volume and pressure isotherms.

Langmuir model suggests the development of a single molecular layer of adsorption.

Page 9: Takbiri-shale Gas AAPG

VELOCITY PROFILES FOR DIFFERENT KNUDSEN NUMBERS

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Assumptions: Specular and diffusive

reflections

Slip velocity increases as Knudsen number increases

Page 10: Takbiri-shale Gas AAPG

MODEL RESULTS FOR PERMEABILITY

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PERMEABILITY IN SLIP REGIME

11

Kd vs. inverse of mean pressure for Argon at T = 338K for different channel widths

Kd vs. inverse of the mean pressure for Argon and Helium at T= 338K for channel widths of 10 and 100 nm

Page 12: Takbiri-shale Gas AAPG

IMPACT OF TEMPERATURE ON APPARENT PERMEABILITY

12

Kd vs. channel width for different temperatures at constant pressure of 0.28 MPa for Argon.

Page 13: Takbiri-shale Gas AAPG

CORE PLUG SCALE

13

A multiscale medium consisting of inorganic matrix and organic matter (kerogen).

Inorganic pores are dominantly slit-like in shape or microfracture and therefore they are stress-sensitive.

Page 14: Takbiri-shale Gas AAPG

CORE PLUG SCALE

Intrinsic permeability for conventional reservoir simulators: a property of porous media

independent of the fluid type

Due to existence of nanoscale pores in Shale, permeability is: sensitive to effective stress, pore pressure,

temperature, and the fluid type.

14

Page 15: Takbiri-shale Gas AAPG

EXPERIMENTAL MEASUREMENT

•Unsteady state methods such as GRI and pressure pulse decay are faster and can measure permeability as low as 1 nD

•Steady-state permeability measurements

15

Comparison of crushed rock permeability from different laboratories1

1- Passey, Q. R., Bohacs, K., Esch, W. L., Klimentidis, R., & Sinha, S. (2010, January 1). From Oil-Prone Source Rock to Gas-Producing Shale Reservoir - Geologic and Petrophysical Characterization of Unconventional Shale Gas Reservoirs. Society of Petroleum Engineers.

Page 16: Takbiri-shale Gas AAPG

PERMEABILITY MEASUREMENT

16

laboratory measured apparent permeability, if conducted in low pressure and temperatures, need to be extrapolated to reservoir conditions.

Page 17: Takbiri-shale Gas AAPG

EXPERIMENTAL RESULTS-STEADY STATE

A new steady-state permeability measurement technique

17

Permeability measurement using steady-state method1

1- Zamirian, M., Aminian, K. K., Fathi, E., & Ameri, S. (2014, October 21). A Fast and Robust Technique for Accurate Measurement of the Organic-rich Shales Characteristics under Steady-State Conditions. Society of Petroleum Engineers. doi:10.2118/171018-MS

Page 18: Takbiri-shale Gas AAPG

CYLINDRICAL BUNDLE

For a known pore size distribution, permeability of the core can be calculated from:

φ/T: porosity-tortuosity ratio

18

Page 19: Takbiri-shale Gas AAPG

EXAMPLE

Pore-size distribution obtained by Nitrogen adsorption method at 77K1.

19 1- Zamirian, M., Aminian, K. K., Fathi, E., & Ameri, S. (2014, October 21). A Fast and Robust Technique for Accurate Measurement of the Organic-rich Shales Characteristics under Steady-State Conditions. Society of Petroleum Engineers. doi:10.2118/171018-MS

Page 20: Takbiri-shale Gas AAPG

MULTICONTINUUM APPROACH

•The governing equations are based on the principle of conservation of mass.

•Fluid transport and storage of each continuum can be governed by different physics.

•Spatial coordinates of each continuum are not explicitly defined.

20 1- Akkutlu, I.Y., and Fathi, E. (2012). Multiscale gas transport in shales with local Kerogen heterogeneities. SPE Journal, Volume 17, Number 4. 2- Azom, P. N. and Javadpour, F. (2012, January 1). Dual-Continuum Modeling of Shale and Tight Gas Reservoirs. Society of Petroleum Engineers. doi:10.2118/159584-MS

Multicontinuum approach for shale gas transport1 Organic pores inorganic pores fractures

Page 21: Takbiri-shale Gas AAPG

FLOW IN FRACTURED POROUS MEDIA

21

Fluid transport is governed by Darcy equation. Different measurement techniques exist: Flow experiments Correlations Numerical techniques

Page 22: Takbiri-shale Gas AAPG

IMAGE-BASED NUMERICAL MODELING

22

Chukwudozie C. Pore-scale lattice Boltzmann simulations of inertial flows in realistic porous media: a first principle analysis of the Forchheimer relationship. Master’s thesis, Louisiana State University; 2011.

SEM image of the rock Constructed 3D gray scale image Flow simulation results

Page 23: Takbiri-shale Gas AAPG

FLOW IN PROPPED FRACTURES

23 Takbiri Borujeni, A. (2013). Multi-scale modeling of inertial flows through propped fractures. PhD dissertation, Louisiana State University.

Page 24: Takbiri-shale Gas AAPG

RESERVOIR SIMULATION

24

Page 25: Takbiri-shale Gas AAPG

INERTIAL FLOWS AT PROPPANT-RESERVOIR INTERFACE

25

Inertial flows can not be upscaled

Page 26: Takbiri-shale Gas AAPG

DISCRETE MODELS

In discrete models, fractures are discretely within the reservoir

26

http://en.wikipedia.org/wiki/User:Jpvandijk/TaskForceMajella#CITEREFvan_Dijk2002.2C_b

Page 27: Takbiri-shale Gas AAPG

MULTICONTINUUM APPROACH FOR FRACTURED FORMATIONS

27

Principle of multicontinuum approach for fractured formations1

1- Dietrich, P., R. Helmig, M. Sauter, H. Htzl, J. Kngeter, and G. Teutsch (2005). Flow and Transport in Fractured Porous Media. Springer.

Page 28: Takbiri-shale Gas AAPG

CONCLUSION

• Klinkenberg equation might not be sufficient to determine permeability.

• Apparent permeability is stress-dependent.

• Multicontinuum approaches can be used.

• Knudsen number is larger than 0.1.

• Continuum assumptions are no longer valid.

• Sorption and slippage phenomena comes into the picture.

• Continuum assumptions are valid • Inertial flows come to the picture • Two modeling approaches: discrete and

multicontinuum

28

Page 29: Takbiri-shale Gas AAPG

APPENDIX

29

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MOLECULAR DYNAMICS

30

Lennard-Jones Plot of Carbon, Methane, and CO21

1- Wilcox, Jennifer, Carbon Capture, Springer New York Dordrecht Heidelberg London, 2012

Page 31: Takbiri-shale Gas AAPG

MODELING OF FLUID FLOW IN KEROGEN

Classical continuum-based gas flow equations cannot be used1.

Modeling approaches: Molecular Dynamics Direct Simulation Monte Carlo Burnett equation Reduced-order Boltzmann equations

31

Configuration of molecules and channel in molecular dynamic simulator.

Javadpour, F. 2009. Nanopores and Apparent Permeability of Gas Flow in Mudrocks (Shales and Siltstone). J. Cdn. Pet. Tech. 48 (8): 16–21.

Page 32: Takbiri-shale Gas AAPG

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The International Union of Pure and Applied Chemistry (IUPAC) pore size classifications

Page 34: Takbiri-shale Gas AAPG

BOLTZMANN EQUATION

34

Page 35: Takbiri-shale Gas AAPG

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Page 37: Takbiri-shale Gas AAPG

IMAGE-BASED PORE-SCALE MODELING

Velocity field at the pore space

Image from

XCT

Segmented Image Pore-scale Flow Simulation

(Lattice Boltzmann)(Sukop et al., 2007)

Reservoir Simulation Impacts on productivity indices

Berea Core Sample (Petroleum Cores)

Proppants (CARBO Ceramics)


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