Modelling two-phase flow and transport in industrial porous …Modelling two-phase flow and...
Transcript of Modelling two-phase flow and transport in industrial porous …Modelling two-phase flow and...
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Modelling two-phase flow and transport in industrial porous media
S Majid HassanizadehS. Majid HassanizadehDepartment of Earth Sciences
Ut ht U i itUtrecht UniversityThe Netherlands
C ll bCollaborators: Simona Bottero; Utrecht University, The NetherlandsJenny Niessner; Utrecht University The NetherlandsJenny Niessner; Utrecht University, The NetherlandsVahid Joekar-Niasar; Utrecht University, The NetherlandsCas Berentsen; Delft University of Tech., The NetherlandsRainer Helmig; University of Stuttgart, GermanyMichael A. Celia; Princeton University, USAH l K D hl U i it f B NHelge K. Dahle; University of Bergen, Norway
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Outline of presentationp
Introduction: Darcy’s law for two-phase flow in porous mediaCapillary pressure in porous mediaShortcomings of standard capillary pressure theory
Experimental evidencesExperimental evidences New theory of capillaritySignificance of new theoryNew theories of two-phase flow ConclusionsConclusions
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INTRODUCTIONINTRODUCTION
Theories of (multiphase) flow in porous media have been too empirical in nature.
They have been developed through “extensions” f i l l ti hi i d h f hiof simple relationships in ad-hoc fashion.
They are not necessarily valid for complexThey are not necessarily valid for complex systems we are considering today.
Take Darcy’s law.
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DARCY TESTED HIS FORMULA ON A COLUMN OF SAND IN A LABORATORY AND DETERMINED THESAND IN A LABORATORY AND DETERMINED THE VALUE OF CONDUCTIVITY (K):
hΔLhKAQ Δ=
L
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Simple System Complex System
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METAMORPHOSIS OF DARCY’S LAW
It is now used in the f f th
Darcy’s law was d f same form for three-
dimensional unsteady proposed for one-dimensional steady-
flow of two or more compressible fluids,
state flow of almost pure incompressible co p ess b e u ds,
with lots of dissolved matter in anisotropic
pure incompressible water in saturated homogeneous matter, in anisotropic
heterogeneous homogeneous isotropic rigid sandy
deformable porous media under non-
soil under constant temperature
isothermal conditions p
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METAMORPHOSIS OFDARCY’S LAW
q = Q/AWrite the formula in terms of velocity
hΔhK Δq KL
=qL
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METAMORPHOSIS OFDARCY’S LAW
FOR ONE-DIMENSIONAL FLOW, Change tod hd x
−hL
Δd xL
dhhΔdhK hq K Δ=q Kd
= −q KL
qdxLdx
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METAMORPHOSIS OFDARCY’S LAW
For unsteady state conditions: ( , )h h x t=
h∂dhKhK ∂dhq K
d= −q K= −
∂q
dxq
x∂x∂
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METAMORPHOSIS OFDARCY’S LAW
FOR THREE-DIMENSIONAL FLOW
h∂h∂hK ∂hq K ∂=q K= −∂iq K= −∂x∂ ix∂ i
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METAMORPHOSIS OFDARCY’S LAW
FOR ANISOTROPIC MEDIA, REPLACE K BY Kij
h∂h∂hK ∂hq K ∂iq K= −
∂i ijq K= −
∂ii
qx∂
jjx∂ij
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METAMORPHOSIS OFDARCY’S LAW
FOR HETEROGENEOUS MEDIA
KijKijjis assumed to be a function
of position
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METAMORPHOSIS OFDARCY’S LAW
FOR FLOW IN UNSATURATED ZONE:
h∂hKq ∂−= iji xKq
∂−=
jx∂ j
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METAMORPHOSIS OFDARCY’S LAW
FOR FLOW IN UNSATURATED ZONE:
K is assumed to be Kij a function of t t t
ijθwater content θ
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METAMORPHOSIS OFDARCY’S LAW
FOR TWO-PHASE FLOW (say WATER AND OIL):
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METAMORPHOSIS OFDARCY’S LAW
FOR TWO-PHASE FLOW (say WATER AND OIL):
∂ ww w hK ∂
∂w wi ij
hq = - Kx∂ jx
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METAMORPHOSIS OFDARCY’S LAW
FOR TWO-PHASE FLOW (SAY WATER AND OIL):
∂ ww w hK ∂
∂w wi ij
hq = - Kx∂ jx
∂ oo o hK
∂o oi ij
j
q = - Kx∂ jx
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METAMORPHOSIS OFDARCY’S LAW
FOR TWO-PHASE FLOW (say WATER AND OIL):
kw wrkw w
ij ijK = K
ko oK = Krkij ijK K
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Capillary Pressure-saturation relationshipp y p
( )c wp S ρ⎛ ⎞ ( )( ) 1o w wo o
p Sh h z hg
ρρ ρ
⎛ ⎞− = + − −⎜ ⎟
⎝ ⎠gρ ρ⎝ ⎠
The form of Darcy’s Law remains unchanged:∂
y g αα α ∂
∂i ijhq = - K
∂i ijjx
W ddi b ll d hi tl t i l f lWe are adding bells and whistles to a simple formula to make it valid for much more complicated situations!
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“Extended” Darcy’s Lawy
hK Δq Kx
=Δ
The “extended” Darcy’s Law remains unchanged:α
α α ∂∂i ijhq = - K
∂i ijj
qx
We have added bells and whistles to a simple formula to make it valid for much more complicated situations!
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Comparison of theories of Aristotle and Galileo for free fall of objects with hypothetical measurements (after French, 1990)
GALILEO
objects with hypothetical measurements (after French, 1990)
tyl V
eloc
it
ARISTOTLE
erm
inal
DATA POINTS
Te
Time
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PhD RESEARCH PROJECTHypothetical plot of terminal velocity
R d h d
Hypothetical plot of terminal velocity as a function of mass density for various shapes
Rod shaped
Roundty Round
PyramidDiskoc
itl V
eloc
it
Disk
min
al V
elo
erm
inal
Term T
e
Mass Density
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How many relative permeability-saturation curves have been measured during the past few decades!?have been measured during the past few decades!?
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How many capillary pressure-saturation curves have been measured during the past few decades!?
Imbibitionscanning
Drainage scanning
been measured during the past few decades!?
scanning curves
scanning curves
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Relative permeability is supposed to be less than 1.
Water and oil relative permeabilities in 43 sandstone reservoirs plotted as a function of water saturation
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Problems with current theories of multiphase flowProblems with current theories of multiphase flow
P di t d it d t b th lPressure gradient and gravity are assumed to be the only driving forces. Effects of all other forces are lumped into coefficients.
In particular, interfacial forces and interfacial energies are not explicitly taken into account. This is unacceptable.not explicitly taken into account. This is unacceptable.
There is discrepancy between the theory and measurement.
Capillary pressure curves are measured under equilibrium conditions and then used under non-equilibrium (flow)
diticonditions.
Capillary pressure is believed to go to infinity. Nonsense!
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Forces acting within interfaces control fluid di t ib ti ithi th didistribution within the porous medium.
2c σ2c
M
pRσ=
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Mass transfer among phases occurs through interfaces.
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Where are interfaces in porous media theories!?
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Problems with current theories of multiphase flowProblems with current theories of multiphase flow
P di t d it d t b th lPressure gradient and gravity are assumed to be the only driving forces. Effects of all other forces are lumped into coefficients.
In particular, interfacial forces and interfacial energies are not explicitly taken into account. This is unacceptable.not explicitly taken into account. This is unacceptable.
There is discrepancy between the theory and measurement.
Capillary pressure curves are measured under equilibrium conditions and then used under non-equilibrium (flow)
diticonditions.
Capillary pressure is believed to go to infinity. Nonsense!
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Measurement of Capillary Pressure-Saturation Curvesp y
Capillary pressure-saturation curves for a given medium are obtained by measurement of saturation inside and fluidobtained by measurement of saturation inside and fluid pressures outside the porous medium under quasi-equilibrium conditions. Time to equilibrium can be 24 hours to 7 days.Hydrophobic and hydrophilic membranes affect the resultsHydrophobic and hydrophilic membranes affect the results.
Air chamberapcp =
Porous Medium
*
pa
pp p−
Medium
P Pl tWater reservoir
***
****
Drying curvepScanning drying curve
*
Porous Plate(impermeable to air)*
*
Wetting curve
*Scanning drying curve
S**
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Industrial Porous MediaIndustrial Porous Media
M i d t i l i l di flMany industrial processes involve porous media flows.
Some examples are processes in fuel cells, paper-pulp drying, food production and safety, filtration, concrete, ceramics, moisture absorbents, textiles, paint drying, polymer composites and detergent tabletspolymer composites, and detergent tablets
There is clear difference between industrial porous media and soils:and soils:- fast flow- significant mass transfer across fluid-fluid interfaces- significant deformations- wettability changes- high porsosityhigh porsosity
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Dewatering of paper pulp
press nips The paper pulp layer is transported through the press aperture on a felt. The paper-felt sandwich is thus compressed, so that the water is pressed out of the paper, is absorbed by the felt, and then flows laterally away from the nips.
Pictures courtesy of Oleg Iliev of ITWM, Kaiserslautern
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Simulation of dewatering of paper pulpg p p p p
Capillary pressure curves are measured for feltCapillary pressure curves are measured for felt under quasi-static conditions. It takes around 24 hours to obtain them.24 hours to obtain them.
They are then used to model a process thatThey are then used to model a process that takes only seconds!
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Air and oil flow in oil filters
Pictures courtesy of Oleg Iliev of ITWM, Kaiserslautern
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Proton Exchange Membrane (PEM) Fuel Cells
Pc-Sw measurement of hydrophobic y pgas diffusion layer of a PEM fuel cell
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Unsaturated flow in thin fibrous materials
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Unsaturated flow in thin fibers
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Unsaturated flow in pampers
Measurement of capillaryMeasurement of capillary pressure curves takes about 12 hours.
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Unsaturated flow in pampers
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Capillary pressure-saturation experiments (PCE and Water)(PCE and Water)
Experiments carried out at GeoDelft; Soil sample: 3 cm high and 6cm in dia. Fluids: PCE and water;Fluids: PCE and water; Primary drainage, Main drainage, Main imbibition; Quasi-static and dynamic experiments
PCE
Air chamber
PPT NW back
3 cmsand
water PCE reservoir
PPT NW back
PPT W frontwater
Water
Soil sample
Water
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10 0
12.5
Pc [(in sand]
Pc [in fluids]Pc-S curves based on
d
7.5
10.0 [ ] pressures measured inside the soil sample.
5.0
c [k
Pa] Capillary pressure
DOES NOT go to
2.5
Pc
ginfinity!
A th th0.0
Are these the curves we should use in our i l t ?
-2.50.0 20.0 40.0 60.0 80.0 100.0
Water saturation
simulators?
Water saturation
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Measurement of “Dynamic Pressure Difference” CurvesDynamic Pressure Difference Curves
n wP Pn wP PP
− =Δ
10
]
dynPΔ8
ure
[kPa
]
4
6
ry P
ress
u
cP2C
apilla
D ynam ic Prim ary drainage-1
0.2 0.4 0.6 0.8 10W ater Saturation [-]
S tatic prim ary drainage
Hassanizadeh et al., 2004
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Two-phase flow dynamic experiments (PCE and Water)
10.0prim drain PN~16kPa
Dyn.P.D.
)
8.0
pprim drain PN~20kPaprim drain PN~25kPamain imb PW~0kPamain imb PW~5kPamain imb PW~8kPa
S.P.D.S M D
Dyn.M.D.
w(k
Pa)
6.0
main imb PW 8kPamain imb PW~10kPamain imb PW~0kPa lastmain drain PN~16kPamain drain PN~20kPamain drain PN~25kPaS.M.D.
S.M.I.Pn-P
w
4.0
main drain PN~25kPamain drain PN~30kPaStatic Pc inside
Dyn.M.I.2.0
-2 0
0
Saturation, S0 0.20 0.40 0.60 0.80 1.00
2.0
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Experiments on the uniqueness of curves(drainage experiments by Topp Klute and Peters 1967)
cp S−(drainage experiments by Topp, Klute, and Peters , 1967)
These are all drainage curves
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There is no unique pc-S curve.
Main Scanning Drainage Curves
Dynamic Drainage Curves
c P i D i C
Main Drainage CurvesSecundary Scanning Drainage Curves
ssur
e pc Primary Drainage Curve
ary
pres
Cap
illa
Primary Imbibition CurveM i I bibiti CMain Imbibition Curve
Main Scanning Imbibition Curves
Secundary Scanning Imbibition Curves
Saturation, S
Dynamic Imbibition Curves
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There is no unique pc-S curve.
Main Scanning Drainage Curves
Dynamic Drainage Curves
Main Drainage Curves
g g
Secundary Scanning Drainage Curves
Primary Drainage Curve
re p
cpr
essu
r
Primary Imbibition Curve
apill
ary
Main Imbibition Curve
Main Scanning Imbibition Curves
Secundary Scanning Imbibition Curves
Ca
Secundary Scanning Imbibition CurvesDynamic Imbibition Curves
Saturation, S
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A New Theory of yCapillarity in Porous Media
1 Difference in fluids’ pressures are equal1. Difference in fluids pressures are equal to capillary pressure but only at equilibrium.
2. Capillary pressure is not only a function p y p yof saturation but also of interfacial area
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Forces acting within interfaces control fluid di t ib ti ithi th didistribution within the porous medium.
2σ2cp σ=M
pR
=MR
n w cp p p=p p p− =
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Microscale Dynamic EffectsConsider two-phase flow in a single tube:
A⎛ ⎞
2
2 An w
M
qp p BR r
γ μ⎛ ⎞− = + ⎜ ⎟⎝ ⎠
Nonwetting phaseWetting phase
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NONEQUILIBRIUM CAPILLARY EFFECTLi hLinear theory
Equilibrium capillary theory:Equilibrium capillary theory:
( )n w cp p p S− =Under non-equilibrium conditions:
( ), /n w cp p p f S S t− = + ∂ ∂
Linear approx.:S∂( )n w c Sp p p St
τ ∂− = −∂
where τ is a damping coefficient.
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Dynamic capillary pressure curvesDynamic capillary pressure curves
( ) S∂cp = ( ) ( )a w c Sp p p St
τ ∂− − = −∂
Thi ti t th b h in wp p−Dynamic drying curve c Sp τ ΔΔ = −
This equation captures the behavior observed in the experiments
Drying curve cpΔp
tτΔ
Δ
Wetting curve
Dynamic wetting curve
SCurves measured in the labCurves measured in the lab can be used to evaluate τ
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Two-phase flow dynamic experiments (PCE and Water)
dS/dt vs. S - all curves4.0E-02
3.0E-02
1.0E-02
2.0E-02
[s-1
]
0.0E+00
(-)d
s/d
t
-2.0E-02
-1.0E-02
-3.0E-020.00 0.20 0.40 0.60 0.80 1.00
saturation
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Two-phase flow dynamic experiments (PCE and Water)
Determination of τPrimary drainage; S=70%Primary drainage; S=70%
2 .5
y = 6 1 .4 x + 0 .7y = 5 4 .0 x + 1 .22
kPa]
y = 5 0 .0 x + 0 .41
1 .5
) - P
c(st
at)
[k
0 .5
1
Pc(
dyn)
P a ir = 1 6 k P a
00 .0 0 0 0 .0 0 5 0 .0 1 0 0 .0 1 5 0 .0 2 0 0 .0 2 5 0 .0 3 0
P a ir = 2 0 k P a
P a ir = 2 5 k P a
0 .0 0 0 0 .0 0 5 0 .0 1 0 0 .0 1 5 0 .0 2 0 0 .0 2 5 0 .0 3 0(- )d S /d t [s -1 ]
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TWO PHASE FLOW EXPERIMENTSUtrecht University
TWO- PHASE FLOW EXPERIMENTSDynamic coefficient, τ
5x 107
4
5x 10
3
4
a.s]
S [ ]2ta
u [P
a Sw [-] τ [Pa.s]
0.80 9.83 * 104
1
0.80 9.83 100.70 1.06* 105
0.60 1.33* 105
0 50 2 61 * 106
0.4 0.5 0.6 0.7 0.80Sw [-]
0.50 2.61 106
0.40 3.62 * 107
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Estimation of τ from literature data((Hassanizadeh, Celia, and Dahle, Vadose Zone Journal, 2002)
Soil Type of Value of τReference
Soil Type
Type of experiment
Value of τ(kg/m.s)
For Air-Water Systems:For Air-Water Systems:Topp et al. (1967)Smiles et al (1971)
SandSand
DrainageDrainage
2*107
5*107Smiles et al. (1971)Stauffer (1978) Nützmann et al (1994)
SandSandSand
DrainageDrainageDrainage
5 103*104
2*106Nützmann et al. (1994)Hollenbeck & Jensen(1998)
SandSand
DrainageDrainage
2*106
2 to 12*106
For Oil Water S stems: S d tFor Oil-Water Systems:Kalaydjian (1992b)
Sandst./limest. Imbibition 2*106
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Significance of new theory for unsaturated flow:Development of vertical wetting fingers in dry soilDevelopment of vertical wetting fingers in dry soil
Experiments by Rezanejad et al., 2002
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Consequences of new theory for unsaturated flow:Development of vertical wetting fingers in dry soilDevelopment of vertical wetting fingers in dry soil
David A. DiCarlo, “Experimental measurements of saturation overshoot on infiltration” VOL. 40, 2004
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Consequences of new theory for unsaturated flow:Development of vertical wetting fingers in dry soilDevelopment of vertical wetting fingers in dry soil
David A. DiCarlo, “Experimental measurements of saturation overshoot on infiltration” VOL. 40, 2004
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Classical unsaturated flow equationqFlow equation:
⎛ ⎞⎛ ⎞( )k wrS k S pn g
t z zρ
μ⎛ ⎞⎛ ⎞∂ ∂ ∂= +⎜ ⎟⎜ ⎟∂ ∂ ∂⎝ ⎠⎝ ⎠
Capillary pressure-saturation relationship:
( )
⎝ ⎠
( )a w cp p p S− =
Richards equation:S S∂ ∂ ⎛ ∂ ⎞⎛ ⎞S Sn D gt z z
ρ∂ ∂ ⎛ ∂ ⎞⎛ ⎞= +⎜ ⎟⎜ ⎟∂ ∂ ∂⎝ ⎠⎝ ⎠
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Simulation of vertical wetting fingers in dry soil
Stability analysis by Dautov et al. (2002) has proven that:
Richards equation is unconditionally stable.It does not produce any fingers, but a monotoniclly
M difi d Ri h d i ( i h d i
p y g , ydecreasing saturation profile toward the wetting front.
Modified Richards equation (with dynamic effect) is conditionally unstable.It is able to produce gravity wetting fingers.
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Dynamic capillary pressure theoryy p y p yUnsaturated flow equations:
Flow equation:
⎛ ⎞⎛ ⎞( )k wrS k S pn g
tρ
μ⎛ ⎞⎛ ⎞∂ ∂ ∂= +⎜ ⎟⎜ ⎟∂ ∂ ∂⎝ ⎠⎝ ⎠
Capillary pressure-saturation relationship:
t z zμ ⎜ ⎟∂ ∂ ∂⎝ ⎠⎝ ⎠
( )a w c SS ∂( )a w cstat
Sp p p St
τ ∂− = −∂
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Development of vertical wetting fingers in dry soil;
Simulations based on new capillarity theory
Dautov et al. (2002)
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A New Theory of yCapillarity in Porous Media
1 Difference in fluids’ pressures are equal1. Difference in fluids pressures are equal to static capillary pressure but only at equilibrium.
2. Capillary pressure is not only a function p y p yof saturation but also of interfacial area
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Imbibition Drainage
P c/ρ
g
P c/ρ
g
e he
ad,
e he
ad,
pres
sure
pres
sure
pilla
ry p
pilla
ry p
Cap
Cap
Water content Water contentCAPILLARY PRESSURE-SATURATION DATA POINTS MEASURED IN LABORATORY
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Imbibition Drainage
P c/ρ
g
P c/ρ
g
e he
ad,
e he
ad,
pres
sure
pres
sure
pilla
ry p
pilla
ry p
Cap
Cap
Water content Water content
CAPILLARY PRESSURE-SATURATION DATA POINTS MEASURED IN LABORATORY
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New capillarity theory with no (need for) hysteresis
( ),c c wnp p S a= ( ),p p
where:
is capillary pressurecp is capillary pressure
S is wetting phase saturation
p
awn is the specific interfacial area between wetting & nonwetting phases
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pc-S-awn Relationships55.0
8000
9000
53.0
54.0
(kP
a)
5000
6000
7000
8000
1/m
)
ress
ure
ea
51 0
52.0
Pre
ssur
e (
2000
3000
4000
5000
IAV
wn
(1
pilla
ry p
r
rfac
ial a
re
50.0
51.0
0.4 0.5 0.6 0.7 0.8 0.9 1
ImbibitionDrainage
Wetting Phase Saturation
1000
2000
0.4 0.5 0.6 0.7 0.8 0.9 1
IAVndWNIAVndWN
Wetting Phase Saturation
Cap
Inte
r
S t tiS t tig g
8000
9000
SaturationSaturation
5000
6000
7000
n (1
/m)
Figures courtesy of ar
ea
1000
2000
3000
4000
ImbibitionDrainage
IAV
wncourtesy of
Laura Pyrak-Nolte of Purdue te
rfac
ial
1000
51 51.5 52 52.5 53 53.5 54 54.5 55Pressure (kPa)
Purdue University
Capillary pressure
Int
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pc-S-Awn Surfacesp
Imbibition Drainage
Figure courtesy of Laura Pyrak-Nolte of Purdue University
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Comparison of Drainage & Imbibition Surfaces
Mean Relative Difference: -3.7%Mean Relative Difference: 3.7%Standard Deviation: 10.6%
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C ill t lCapillary pressure at macroscale
(data obtained from Vahid Joekar-Niasar et al. 2007)
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New theories of two-phase flowExtended Darcy’s law :
( )( )Gα α α αρ= − • ∇ −q K g
where Gα is the Gibbs free energy of a phase:
( )wnG G S Tα α α αρExtended Darcy’s law :
( ), , ,wnG G a S Tα α α αρ=
Extended Darcy s law :
( )a wn Sp a Sα α α α αα αρ σ σ−=− • ∇ ∇ −− ∇q K g( )Equation of motion for interfaces :
( )⎡ ⎤( )wn wn wn wn wn wK a Sγ⎡ ⎤=− ∇ +Ω ∇⎣ ⎦w
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New theories of two-phase flowp
Volume balance equation for each phase
0Snα
α∂ + ∇ • =q 0nt
+ ∇∂
q
Area balance equation for fluid-fluid interfaces
( ) ( ),wn
wn wn wn wn wa a r a S∂ +∇• =w( ) ( ),a r a St
+∇∂
w
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Summary of two-phase flow equationsy p q
0Snα
α∂ + ∇ • =q 0nt
+ ∇∂
q
( )a wn S Sα α α α αα α∇ ∇ ∇Kwn∂
( )a wn Sp a Sα α α α αα αρ σ σ−=− • ∇ ∇ −− ∇q K g
( ) ( ),wn
wn wn wn wn wa a r a St
∂ + ∇ • =∂
w
( )wn wn wn wn wn wK a Sγ⎡ ⎤= − ∇ + Ω ∇⎣ ⎦w
( ),w
n w w nc c wSp p p p f S aτ ∂−∂
− = =
⎣ ⎦
( ),p p p pt
f∂
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CONCLUSIONSDarcy’s law is not really valid for complex porous
media.media.
Difference in fluid pressures is equal to capillary b l d ilib i di ipressure but only under equilibrium conditions.
Under nonequilibrium conditions, the difference inUnder nonequilibrium conditions, the difference in fluid pressures is a function of time rate of change of saturation as well as saturation.of saturation as well as saturation.
Fluid-fluid interfacial areas should be included in lti h fl th imultiphase flow theories.
Hysteresis should be modelled by introducing ys e es s s ou d be ode ed by oduc ginterfacial area into the two-phase flow theory