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4 Constitutive Assumptions

[page 145, §1]   
[145.1.1] The porous medium is assumed to be macroscopically homogeneous

ϕx=ϕ=const(12)

although this assumption rarely holds in practice [26]. [145.1.2] Let us further assume that the fluids are incompressible so that

ϱ1x,t=ϱW(13a)
ϱ2x,t=ϱW(13b)
ϱ3x,t=ϱO(13c)
ϱ4x,t=ϱO(13d)

where the constants ϱW,ϱO are independent of x and t.

[145.2.1] Flows through porous media often have low Reynolds numbers. [145.2.2] Thus accelerations and the inertial term

DiDtvi=0(14)

can be neglected in the momentum balance equation (10).

[145.3.1] The momentum transfer into phase i from all the other phases is assumed to arise from viscous drag,

mi=j=15Rijvj-vi(15)

with resistance coefficients Rij quantifying the loss due to viscous friction between phase i and j. [145.3.2] The matrix is assumed to be rigid so that v5=0. [145.3.3] Hence -Ri5vi is the momentum transfer from the wall into phase i. [145.3.4] Then

m1=R13v3-v1+R14v4-v1-R15v1(16a)
m2=R23v3-v2+R24v4-v2-R25v2(16b)
m3=R31v1-v3+R32v2-v3-R35v3(16c)
m4=R41v1-v4+R42v2-v4-R45v4(16d)

where R12=0 and R34=0 was used because there is no common interface and hence no direct viscous interaction between these phase pairs. [145.3.5] The viscous resistance coefficients Rij may be rewritten in term of dimensionless coefficients rij as

Rij=μWk-1rij,i=1,2(17a)
Rij=μOk-1rij,i=3,4(17b)

where μW,μO are the viscosities of water and oil, k is the absolute permeability tensor of the medium, and rij are dimensionless viscous drag coefficients. [145.3.6] Each Rij is a 3×3-matrix. [145.3.7] In practice viscous coupling terms between the two fluid phases are often neglected.

[page 146, §1]    [146.1.1] The stress tensor is written as a pressure term plus a capillary correction term. [146.1.2] The reference pressure for the nonpercolating phases is the pressure of the surrounding percolating phase [24]. [146.1.3] Thus

Σ1=-PW1+Σc1(18a)
Σ2=-PO1+Σc2(18b)
Σ3=-PO1+Σc3(18c)
Σ4=-PW1+Σc4,(18d)

where Σci are capillary stresses resulting from the presence of fluid-fluid and fluid-matrix interfaces.

[146.2.1] Similarly, the body forces are augmented with capillary body forces as

Fi=ϱig+Fci(19)

with i=1,2,3,4. [146.2.2] The capillary body forces Fci are responsible for keeping the trapped fluids inside the medium. [146.2.3] They are assumed to be potential forces

Fci=-Πci(20)

where Πci are the capillary potentials.

[146.3.1] One has considerable freedom to specify the capillary stresses Σci and potentials Πci. [146.3.2] General thermodynamic considerations suggest ideas to restrict this freedom. [146.3.3] Let F denote the total Helmholtz free energy of the system with and oil-water interface, and let FW and FO denote the individual Helmholtz free energies of bulk water and bulk oil. [146.3.4] Then [27, 28]

dF=-PWdVW-POdVO+σWOdA~WO+σWMdA~WM+σOMdA~OM(21)

where PW,PO are the oil and water pressure, VW,VO are the volumes of oil and water, and A~WO,A~WM,A~OM are the total interfacial areas between oil and water, water and matrix, resp. oil and matrix. [146.3.5] The oil-water surface tension σWO and the fluid-matrix interfacial tensions σWM,σOM are related by Youngs equation

σOM=σWM+σWOcosϑ(22)

where ϑ is the contact angle of water. [146.3.6] The interfacial areas obey

A~WO=A~31+A~32+A~41+A~42(23)
A~PM=A~WM+A~OM(24)
A~WM=A~15+A~25(25)
A~OM=A~35+A~45(26)

where A~ij is the total interfacial area between phase i and j, and the volumes are related by eqs. (5b) and (5c).

[page 147, §1]    [147.1.1] In equilibrium dF=0 holds. [147.1.2] Also, sample volume and internal surface are constant because the porous medium is rigid. [147.1.3] This implies dV=0 and dA~PM=0. [147.1.4] Using eq. (5c) one arrives at

0=PO-PW+σWOA~WOVW-cosϑA~WMVW(27)

where Youngs equation (22) was also used.

[147.2.1] These considerations suggest one particular way to specify the capillary stresses and potentials. [147.2.2] Following earlier ideas [24] the capillary stresses are specified as

Σc1=0(28a)
Σc2=-σWOϕAWOSW(28b)
Σc3=0(28c)
Σc4=-Σc2(28d)

where local equilibrium was assumed and intensive quantities (per unit volume of porous medium) were introduced. [147.2.3] The capillary potentials may be associated with the last term in eq. (27). [147.2.4] They are specified as

Πc1=0(29a)
Πc2=σWOϕcosϑAWMSW(29b)
Πc3=0(29c)
Πc4=-Πc2(29d)

in analogy with [23, 24].

[147.3.1] The mass transfer rates are Mi=j=15Mij where Mij is the mass transfer rate from phase j into phase i. [147.3.2] Neglecting chemical reactions one assumes Mij=0 for all pairs i,j except the pairs 1,2,2,1,3,4,4,3. [147.3.3] These remaining transfer rates are assumed to be given as

M12=-M21=ϕϱWb11-S2-b2S2ΘW*+η2S2-S2*SW*-SWSWt(30a)
M34=-M43=ϕϱOb31-S4-b4S4ΘO*+η4S4-S4*SO*-SOSOt(30b)

[page 148, §0]    with

SW*=ΘτWSWt+S2*-S4*(31a)
SO*=1-SW*(31b)
S2*=minSW,SWi1-ΘτWSWt(31c)
S4*=minSO,SOrΘτWSWt(31d)

as in [22, 23, 24]. [148.0.1] The limiting saturations for S2,S4, called irreducible water resp. residual oil saturation,

SWi=SWi(v1,v3)=b1v1,v3b1v1,v3+b2v1,v3(32a)
SOr=SOr(v1,v3)=b3v1,v3b3v1,v3+b4v1,v3(32b)

are velocity dependent, because they depend on the velocity dependent “reaction rates” biv1,v3,i=1,2,3,4. [148.0.2] The relation between residual oil saturation SOr and flow velocity is also known as capillary correlation or capillary desaturation curve [29, 30, 31]. [148.0.3] The factors ΘW*,ΘO* are defined as

ΘW*=Θcosϑ+1-ΘcosϑΘS2-SWi0(33a)
ΘO*=ΘcosϑΘS4-SOr0+1-Θcosϑ(33b)

where ϑ denotes the contact angle of water,

SWi0=limv0SWiv,v(34a)
SOr0=limv0SOrv,v.(34b)

are the low velocity limits of SWi,SOr, and

Θx=1,x>00,x0(35)

denotes the Heaviside unit step function. [148.0.4] The velocity dependent “reaction rates” bi are chosen such that they vanish for vanishing velocities. [148.0.5] In this paper it will be assumed that [page 149, §0]   

b1=b1(v1,v3)=τW3A4v12v32(36a)
b2=b2(v1,v3)=τW3A4v34(1-SWi0SWi0)(36b)
b3=b3(v1,v3)=τO3A4v12v32(36c)
b4=b4(v1,v3)=τO3A4v14(1-SOr0SOr0)(36d)

consistent with eq. (34). [149.0.1] The parameters τW,τO are time scales, and η2,η4,bij are dimensionless constants.

[149.1.1] The first terms in the curly brackets of (30) model an equilibrium reaction between nonpercolating and percolating fluids. [149.1.2] The reaction, i.e. breakup and coalescence, takes only place when both percolating phases move, i.e. have nonvanishing velocity. [149.1.3] The prefactors ΘW*,ΘO* reproduce the experimental observation that nonpercolating nonwetting fluid phases show little breakup or coalescence below the low velocity limit of the residual nonwetting saturation. [149.1.4] The prefactors also ensure that sign and dimensions are correct.

[149.2.1] The specific internal surfaces AWO,AWM depend on saturation. [149.2.2] Here it is assumed that

AWM=APMSW.(37)

[149.2.3] The dependence of AWOS1,S2,S3,S4 is suggested by inverting the classic hydraulic radius theory

k=C1S13A12=C3S33A32(38)

where A1=A31+A41+A51 and A3=A31+A32+A35.

[149.3.1] Finally, the system is closed selfconsistently using the condition

0=R13ϕ1+R14ϕ1+R15ϕ1+R31ϕ3-R41ϕ4+M1ϕ1v1+ϱ1D1Dtv1
+-R23ϕ2-R24ϕ2-R25ϕ2+R32ϕ3-R42ϕ4+M1ϕ2v2-ϱ2D2Dtv2
+-R13ϕ1+R23ϕ2-R31ϕ3-R32ϕ3-R35ϕ3-M3ϕ3v3-ϱ3D3Dtv3
+-R14ϕ1+R24ϕ2+R41ϕ4+R42ϕ4+R45ϕ4-M3ϕ4v4+ϱ4D4Dtv4(39)

written here in its most general form. [149.3.2] It is obtained by demanding that the closure condition should be consistent with the capillary pressure saturation relation obtained in the residual decoupling limit (see [22, 23, 24]).