capillary pressure
TRANSCRIPT
Capillary Pressure
H. MahdiyarShiraz University, Aban-1391
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Definition:
PC = Curvature × Surface Tension
The Higher Curvature,
The Higher Capillary Pressure
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Thus:
In the smaller pores,
The Higher Curvature of the Interface
»»» The Higher PC
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AS Sw Decreases:
Wetting Phase will be drawn into
The smaller PoresResulting in:
The Increase in PC
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The lower Sw,
The Higher Curvature in smaller pores,
The Higher PC
At Swi : w phase : 1-In very small pores (infinite PC)
2- Spreads over the solid Surface (Thin Film)
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Dipping a Lump of Sugar in a Cup of Tea
Hydrophilic Sugar: Tea Flows Upward Spontaneously to reach a
New Equilibrium State:Pn = Pw + PC
Hydrophobic Sugar: Tea Would not move into the cube at the 1st
contact. Cube must be Pushed Down into the Tea.7
Controlling Forces:
1- Viscous Force (Friction): Always acting against the flow depending on Velocity
2- Capillary force: ?
Drainage: Against the Flow
Imbibition: In Favor of Flow
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2rfc
2ruf
Entry or Threshold Pressure
• Required (Pn - Pw ) to enable:
n-Phase to invade a porous medium saturated with w-Phase (Sw = 1).
Entry Pressure is related to the largest pore diameter.
9 max
2rCosPd
:Thus• Drainage begins only when an entry pressure pn
− pw > 0 is applied. Related to the largest pore.
• Imbibition occurs spontaneously, does not require an entry pressure.
W-phase goes to the smallest pores with highest Pc. Pc increases as Sw decreases.
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In Drainage:
The Smaller pore, the Higher required Pn
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The Influence of Varying Pore Diameter
rCosPP wn
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X6 : An Unstable equilibrium location.Interface jumping from X 6 to X5 is called a
Haines jump corresponding to a locally abrupt .change in saturation12
The Influence of Varying Pore Diameter
In Imbibition:
The Larger pore, the Higher required Pw
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The Influence of Varying Pore Diameter
rCosPP nw
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HYSTERSIS:Different Behavior of the Process
depending on its direction.
The Difference Occurs because:The Small Pores Control Drainage.The Large Pores Control Imbibition.
»»» for a certain Sw
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imbibitionCDrainageC PP
Hysteresis Loop: The Path of the full Cycle
Scanning Curves: Shortcuts across the Hysteresis Loop.
Example of Hysteresis: Driving between home and workTwo paths together: Hysteresis loopScanning Curve: Halfway
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Fluid Entrapment
e.g: Drying a porous Solid by Passing air through it.
(some water remains in the small pores and is only released due to evaporation)
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Entrapped Saturation
• Irreducible saturation for w- Phase
• Residual Saturation for n-Phase
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Irreducible Saturation, Swi At Swi
--Some w-phase molecules are strongly adsorbed onto the solid surface.-- Capillary w-phase is held tightly in the Corners and Crevices.
So: w-Phase will no longer flow in response to a gradient in a hydraulic head.
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At Swi Actually: w-Phase is Hydraulically connected
{coating the solid surface with a thin film}
However effective conductivity is negligible.
Thus:In Practice: w-Phase is Hydraulically Disconnected.
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Trapped-Phase volume:
The Volume Which will no-longer Respond to a gradient in Hydraulic Potential.
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TrappedFree SSS
Entrapment in Imbibition
• More Complicated
• Two Primary Mechanisms:
1- Snap-off2- Bypassing
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Snap-Off
• W-Phase tends to flow along the pore wall as it displaces the n-Phase.
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Snap-Off
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..
diamThroatPorediamBodyPore
ARRatioAspect
The Higher AR, The More Snap-Off
The Smaller θ, The More Snap-Off
Bypassing
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Pore doublet
Residual Saturation depends on:• Pore Network Geometry
• Fluid Properties, Surface Tension Density Ratio Viscosity Ratio
• Potential Gradient (Flow)
• Incomplete Displacement
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In another View
• Sor depends on the Magnitude of Viscous and Capillary Forces.
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If Capillary force is dominantThe Higher Capillarity Effect, The Higher Sor
Capillary Number
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ww
c
uN
For Nc < 10-4
Capillary Forces Dominate Over Viscous Forces
2ruf
2rfc
Why?
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r
klu
essureCapillarydropessureViscous
forceCapillaryforceViscous
2PrPr
Carmen-Kozeny Eq.:
232.02 1054
rkrk
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rlN
rlu
forceCapillaryforceViscous
C
500
102 3
For common porous Medium:
41020
CNforceCapillary
forceViscousrl
Thus if Nc < 10-4
Capillary Forces Dominate Over Viscous Forces
In an ordinary water flooding:
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Sm
daymUw
5101
paScpw3101
mn31050
7102 CN
Effects of Flow Properties
when Nc < 10-4
Sor Can be Decreased by the Increase in Nc
The Increase in Water velocity, Viscosity
The decrease in Surface Tension
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wn
wwc
uN
Effect of Incomplete Displacement
• The Higher Initial Sn, The Higher Snr
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In incomplete drainage smaller pores are not occupied by the n-Phase resulting in
smaller Snr , If Nc < 10-4