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Energy Description for Immiscible Two-Fluid Flow in Porous Media by Integral Geometry and Thermodynamics H. H. Khanamiri 1 , C. F. Berg 1 , P. A. Slotte 1 , S. Schlüter 2 , O. Torsæter 1 1 Department of Geoscience and Petroleum, PoreLab, Norwegian University of Science and Technology (NTNU), Trondheim, 2 Department of Soil System Sciences, Helmholtz-Centre for Environmental Research UFZ, Halle Full text article available at https://doi.org/10.1029/2018WR023619

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Page 1: Energy Description for Immiscible Two-Fluid Flow in Porous ... · Energy Description for Immiscible Two-Fluid Flow in Porous Media by Integral Geometry and Thermodynamics H. H. Khanamiri

Energy Description for Immiscible Two-Fluid

Flow in Porous Media by Integral Geometry

and Thermodynamics

H. H. Khanamiri1, C. F. Berg1, P. A. Slotte1, S. Schlüter2, O. Torsæter1

1Department of Geoscience and Petroleum, PoreLab, Norwegian University of

Science and Technology (NTNU), Trondheim,2Department of Soil System Sciences, Helmholtz-Centre for Environmental

Research – UFZ, Halle

Full text article available at https://doi.org/10.1029/2018WR023619

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2

Two-fluid flow in porous media

• In a common approach, we use 𝑘𝑟𝛼 𝑆𝛼 and macroscopic 𝑃𝑐 𝑆𝑤 .

𝑣𝛼 = −𝑘𝑟𝛼 𝑆𝛼 𝑘

𝜇𝛼𝛻𝑝𝛼, 𝛼 = 𝑤, 𝑛

𝑃𝑐 𝑆𝑤 = 𝑃𝑛 − 𝑃𝑤

• Pore scale phenomena affect the 𝑘𝑟 and macroscopic flow.

• However, they are not well represented in the common approach (for ex. dependency of 𝑘𝑟on microscopic flow regimes).

Ref. PetroWiki

Darcy (1856), Wycoff & Botset (1936), Leverett (1941), Avraam and Payatakes (1995)

Ref. PetroWiki

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3

Recent advances in imaging

• From black-box coreflooding to fast X-ray micro-tomography

core sample

injection production

pressure measurement

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4

Intrinsic volumes in integral geometry

• For a 3D set of objects 𝐾, 𝑉0 K − 𝑉3 K denote the intrinsic volumes.

• Example of 𝐾: an assembly of fluid clusters

• 𝑉0 K = 𝑉 K

• 𝑉1 K = 𝐴 K = ∫𝛿𝐾𝑑𝐴

• 𝑉2 K = 𝐻 K =1

2∫𝛿𝐾 𝜅1 + 𝜅2 𝑑𝐴

• 𝑉3 K =1

4𝜋χ K =

1

4𝜋∫𝛿𝐾𝜅1𝜅2𝑑𝐴

𝐾

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5

Characterization theorem in integral geometry

• Under certain conditions, a function 𝜇 on 𝐾 can be

written as a linear combination of intrinsic volumes of 𝐾(Hadwiger 1975).

µ K =

𝑖=0

𝑛

𝑐𝑖𝑉𝑖 K

𝐾

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6

Free energy (F) of a fluid

• F of a fluid confined by a complex boundary fulfills the

requirements of the Hadwiger theorem.

• Therefore, F can be described by a linear combination

of intrinsic volumes (Mecke & Arns 2005).

Mecke & Arns 2005

𝐹 K =

𝑖=0

𝑛

𝑐𝑖𝑉𝑖 K

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7

Free energy of a 2-fluid flow system

(by integral geometry)

bulks (α, β, s) interfaces (αβ, αs, βs) contact lines (αβs)

Interfaces and lines

have volume.

Kαβ

interfacial

thickness (𝜀)

𝐹 = 𝐹𝑠 + 𝐹𝛼 + 𝐹𝛽 − 𝐹𝛼𝛽 − 𝐹𝛼𝑠 − 𝐹𝛽𝑠 + 𝐹𝛼𝛽𝑠

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Dependencies of intrinsic volumes

set intrinsic volumes

𝑲𝜶 𝑉𝛼, 𝐴𝛼, 𝐻𝛼 and χ𝛼

𝑲𝜷 𝑉𝛽, 𝐴𝛽, 𝐻𝛽 and χ𝛽

𝑲𝒔 𝑉𝑠, 𝐴𝑠, 𝐻𝑠 and χ𝑠

𝑲𝜶𝜷 𝑉𝛼𝛽, 𝐴𝛼𝛽, 𝐻𝛼𝛽 and χ𝛼𝛽

𝑲𝜶𝒔 𝑉𝛼𝛽 , 𝐴𝛼𝑠, 𝐻𝛼𝑠 and χ𝛼𝑠

𝑲𝜷𝒔 𝑉𝛽𝑠, 𝐴𝛽𝑠, 𝐻𝛽𝑠 and χ𝛽𝑠

𝑲𝜶𝜷𝒔 𝑉𝛼𝛽s, 𝐴𝛼𝛽s, 𝐻𝛼𝛽s and χ𝛼𝛽s

𝐹

= 𝐹𝑠 + 𝑖=0

3

𝑐𝑖𝛼𝑉𝑖𝛼 + 𝑖=0

3

𝑐𝑖𝛽𝑉𝑖𝛽

− 𝑖=0

3

𝑐𝑖𝛼𝛽𝑉𝑖𝛼𝛽 − 𝑖=0

3

𝑐𝑖𝛼𝑠𝑉𝑖𝛼𝑠

− 𝑖=0

3

𝑐𝑖𝛽𝑠𝑉𝑖𝛽𝑠 + 𝑖=0

3

𝑐𝑖𝛼𝛽𝑠𝑉𝑖𝛼𝛽𝑠

𝐹 = 𝐹𝑠 + 𝐹𝛼 + 𝐹𝛽 − 𝐹𝛼𝛽 − 𝐹𝛼𝑠 − 𝐹𝛽𝑠 + 𝐹𝛼𝛽𝑠

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Dependencies of intrinsic volumes

• Simplifications (area)

• Only 2 of (𝐴𝛼, 𝐴𝛽, 𝐴𝛼𝑠, 𝐴𝛽𝑠, 𝐴𝛼𝛽) are independent.

𝐴𝛼 − 𝐴𝛽 + 𝐴𝑠 = 𝐴𝛼𝑠

𝐴𝛽 − 𝐴𝛼 + 𝐴𝑠 = 𝐴𝛽𝑠

𝐴𝛼 + 𝐴𝛽 − 𝐴𝑠 = 𝐴𝛼𝛽

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Simplifications (interfaces)

𝑉0𝛼𝛽 = 𝒪 𝜀 , 𝜀 → 0

𝑉1𝛼𝛽 = 𝐴𝛼𝛽

𝑽𝟐𝜶𝜷 = 𝑉2𝛼𝛽,𝑙𝑒𝑓𝑡 + 𝑉2𝛼𝛽,𝑟𝑖𝑔ℎ𝑡 + 𝑉2𝛼𝛽,𝑙𝑖𝑛𝑒 = +1

4𝜋2 ∫𝛿𝐾𝛼𝛽𝑠

1

𝑅1+

1

𝑅2→∞𝑑𝐴 =

1

4𝜋2 ∫𝛿𝐾𝛼𝛽𝑠

𝑑𝐴

𝑅1=

1

4𝜋2 ∫𝐿𝛼𝛽𝑠

𝜋𝜀

2𝑑𝐿𝜀

2

=𝟏

𝟒𝝅𝑳𝜶𝜷𝒔

𝑉3𝛼𝛽 = χ𝛼𝛽

Kαβ

interfacial thickness (𝜀)

Dependencies of intrinsic volumes

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Simplifications (contact lines)

𝑉0𝛼𝛽𝑠 = 𝒪 𝜀2 , 𝜀 → 0

𝑉1𝛼𝛽𝑠 = 𝒪 𝜀 , 𝜀 → 0

𝑉2𝛼𝛽𝑠 =1

4𝜋2 ∫𝛿𝐾𝛼𝛽𝑠

1

𝑅1+

1

𝑅2→∞𝑑𝐴 =

1

4𝜋2 ∫𝛿𝐾𝛼𝛽𝑠

𝑑𝐴

𝑅1=

1

4𝜋2 ∫𝐿𝛼𝛽𝑠

2𝜋𝜀

2𝑑𝐿

𝜀

2

=1

2𝜋𝑳𝜶𝜷𝒔

𝑉3𝛼𝛽𝑠 = ∫𝛿𝐾𝛼𝛽𝑠

1

𝑅1 𝑅2→∞𝑑𝐴 = 0

line thickness (𝜀)

Dependencies of intrinsic volumes

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12

Dependencies of intrinsic volumes

• F is a function of 7 intrinsic volumes:

• Under extreme wetting conditions:

𝐹 = 𝐹0 + 𝑐0𝑆𝛼 + 𝑐1𝛼 𝐴𝛼 + 𝑐2𝛼

𝐻𝛼 + 𝑐3𝛼 χ𝛼 + 𝑐1𝛽 𝐴𝛽 + 𝑐3𝛽 χ𝛽 + 𝑐3𝛼𝛽𝑠

𝐿𝛼𝛽𝑠

𝐹 = 𝐹0 + 𝑐0𝑆𝑛 + 𝑐1𝑛 𝐴𝑛 + 𝑐2𝑛

𝐻𝑛 + 𝑐3𝑛 χ𝑛

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Free energy (F) of a 2-fluid flow system

(by thermodynamics)

𝑑𝑉𝑤 = −𝑑𝑉𝑛

𝑑𝑊𝑒𝑥𝑡𝑒𝑟𝑛𝑎𝑙 = 𝑃𝑤𝑑𝑉𝑤 + 𝑃𝑛𝑑𝑉𝑛 = 𝑃𝑤 − 𝑃𝑛 𝑑𝑉𝑛 = 𝑃𝑐𝑑𝑉𝑛 = 𝜙𝑉𝑃𝑐𝑑𝑆𝑛

𝑑𝑊𝑒𝑥𝑡𝑒𝑟𝑛𝑎𝑙 = 𝑑𝐹 + 𝑑𝐸𝑑𝑖𝑠𝑠𝑖𝑝𝑎𝑡𝑒𝑑

∆𝐹 = 𝜙𝑉 𝑃𝑐𝑑𝑆𝑛 + 𝐸𝑑𝑖𝑠𝑠𝑖𝑝𝑎𝑡𝑒𝑑

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Efficiency (E)

Imbibition 𝐸𝐼 = −𝑑𝑊

𝑑𝐹= 𝜙𝑉𝑃𝑐

𝑑𝑆𝑤

𝑑𝐹

Drainage 𝐸𝐷 =𝑑𝐹

𝑑𝑊= −

1

𝜙𝑉𝑃𝑐

𝑑𝐹

𝑑𝑆𝑤

Imbibition

Drainage

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15

Efficiency (E)

• According to Morrow (1970), the

imbibition had an efficiency of

92.5%, whereas the drainage had

a lower efficiency.

Imbibition

Drainage

∆ 𝐹 ≃ −0.925 𝑃𝑐𝑑𝑆𝑤

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Free energy (F) for spontaneous

imbibition (SI)

𝑅2 = 0.993• Linear regression of 330 data

points for five SI with

macroscopic capillary number

of 10-10 showed a good fit.

• Efficiency of 1 had similar

results.

• ∆ 𝐹 𝑆𝑛 = 0.925 ∫𝑆𝑖

𝑆𝑛 𝑃𝑐𝑑𝑆𝑛

• ∆ 𝐹 𝑆𝑛 = 𝑐0𝑆𝑛 + 𝑐1𝑛 𝐴𝑛 + 𝑐2𝑛

𝐻𝑛 + 𝑐3𝑛 χ𝑛 + 𝑐1𝑤 𝐴𝑤 + 𝑐3𝑤 χ𝑤 + 𝑐3𝑛𝑤𝑠

𝐿𝑤𝑛𝑠 − 𝐹𝑖

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17

Efficiency for a PD-MI-MD experiment

• 1-1 lines represent no dissipation.

• Early PD and MD have less dissipation (fewer irreversible processes, e.g. Haines jumps).

• Late PD and MD show a decrease in F when external work is applied.

𝑊 = 𝑆𝑖

𝑆𝑛

𝑃𝑐𝑑𝑆𝑛

𝐹 𝑆𝑛 = 𝑐0𝑆𝑛 + 𝑐1𝑛 𝐴𝑛 + 𝑐2𝑛

𝐻𝑛 + 𝑐3𝑛 χ𝑛 + 𝑐1𝑤 𝐴𝑤 + 𝑐3𝑤 χ𝑤 + 𝑐3𝑛𝑤𝑠

𝐿𝑤𝑛𝑠 − 𝐹𝑖

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Work in progress…

• The coefficients from regression were correlated:– Limited temporal

resolution or limitednumber of data points might not cover the possible nonlinear behavior.

• Possible non-geometric dependencies are not identified.

PD-MI-MD experiment

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Conclusions

• Free energy is a function of 7 geometrically independent variables (𝑆𝑛, 𝐴𝑛, 𝐴𝑤 , 𝐻𝑛, χ𝑛, χ𝑤 , 𝐿𝑤𝑛𝑠).

• The independent variables in extreme wetting conditions are (𝑆𝑛, 𝐴𝑛, 𝐻𝑛, χ𝑛).

• Dissipation of the processes can be calculated by combining integral geometry and thermodynamics.

• Possible non-geometric dependencies have yet to be found by further experimental and theoretical work.

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Thank You

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Integral geometry and 2-fluid flow

• Steiner formula is a relation between volume and other

intrinsic volumes when the structure changes.

• Based on simulated non-wetting fluid configurations

– 𝐻𝑤𝑛 𝑆𝑛, 𝐴𝑤𝑛, χ𝑛 is valid as a state function.

– 𝐻𝑤𝑛 𝑆𝑛 , 𝐻𝑤𝑛 𝑆𝑛, 𝐴𝑤𝑛 are non-unique.

McClure et al. 2018

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References*

• Darcy, H. (1856). Les Fontaines Publiques de la Ville de Dijon. Paris: Dalmont. • Wyckoff, R. D., & Botset, H. G. (1936). The flow of gas‐liquid mixtures through unconsolidated sands. Journal of Applied

Physics, 7, 325.• Leverett, M. C. (1941). Capillary behavior in porous solids. Society of Petroleum Engineers, 142( 01), 152– 169.

https://doi.org/10.2118/941152‐G• Avraam, D. G., & Payatakes, A. C. (1995). Flow regimes and relative permeabilities during steady‐state two‐phase flow in

porous media. Journal of Fluid Mechanics, 293, 207– 236. https://doi.org/10.1017/S0022112095001698• McClure, J. E., Armstrong, R. T., Berrill, M. A., Schlüter, S., Berg, S., Gray, W. G., & Miller, C. T. (2018). Geometric state

function for two-fluid flow in porous media. Physical Review Fluids, 3, 084306. https://doi.org/10.1103/PhysRevFluids.3.084306

• Hadwiger, H. (1957). Vorlesungen über Inhalt, Oberfläche und Isoperimetrie (Lecture on Content, Surface and Isoperimetry) (p. 312). Berlin‐Heidelberg: Springer‐Verlag. https://doi.org/10.1007/978‐3‐642‐94702‐5

• Morrow, N. R. (1970). Physics and thermodynamics of capillary action in porous media. Industrial and Engineering Chemistry, 62( 6), 32– 56. https://doi.org/10.1021/ie50726a006

• Mecke, K., & Arns, C. H. (2005). Fluids in porous media: A morphometric approach. Journal of Physics. Condensed Matter, 17( 9), S503– S534. https://doi.org/10.1088/0953‐8984/17/9/014

* Check the fulltext article at https://doi.org/10.1029/2018WR023619 for details of this work and a complete list of

references.