permeability flow of liquids in porous media

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PERMEABILITY Flow of Liquids in Porous Media

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PERMEABILITY Flow of Liquids in Porous Media. A. q. 2. L. 1. Linear Flow, Incompressible Liquid. 1-D Linear Flow System Assumptions steady state flow incompressible fluid, q(0  s  L) = constant d includes effect of dZ/ds (change in elevation) A(0  s  L) = constant - PowerPoint PPT Presentation

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Page 1: PERMEABILITY Flow of Liquids in Porous Media

PERMEABILITY

Flow of Liquids in Porous Media

Page 2: PERMEABILITY Flow of Liquids in Porous Media

Linear Flow, Incompressible Liquid• 1-D Linear Flow System Assumptions

• steady state flow

• incompressible fluid, q(0s L) = constant

• d includes effect of dZ/ds (change in elevation)

• A(0s L) = constant

• Darcy flow (Darcy’s Law is valid)

• k = constant (non-reactive fluid)

• single phase (S=1)

• isothermal (constant )

Lq

A

1

2

Page 3: PERMEABILITY Flow of Liquids in Porous Media

Linear Flow, Incompressible Liquid

• Darcy’s Law:

• q12 > 0, if 1 > 2

• Use of flow potential, , valid for horizontal, vertical or inclined flow

Lq

A

1

2

ds

μ

k

A

qvs

dΦμ

kAdsq

2

1

dΦμ

kAdsq

L

0

21Lμ

Akq

Page 4: PERMEABILITY Flow of Liquids in Porous Media

Radial Flow, Incompressible Liquid• 1-D Radial Flow System Assumptions

• steady state flow• incompressible fluid, q(rws re) = constant• horizontal flow (dZ/ds = 0 = p)• A(rws re) = 2rh where, h=constant• Darcy flow (Darcy’s Law is valid)• k = constant (non-reactive fluid)• single phase (S=1)• isothermal (constant )• ds = -dr

q

rerw

Page 5: PERMEABILITY Flow of Liquids in Porous Media

Radial Flow, Incompressible Liquid

• Darcy’s Law:

• qew > 0, if pe > pw

ds

μ

k

A

qvs

dpμ

kdr

rh2π

q

q

rerw

w

e

w

e

p

p

r

r

dpμ

kh2πdr

r

1q

wewe

pp)/rln(rμ

kh2πq

Page 6: PERMEABILITY Flow of Liquids in Porous Media

Flow Potential - Gravity TermSI

= p - gZ Z+ Z is elevation measured from a datum

has dimension of pressure In SI Z is measured in m, both and p are in

Pa, ρ is in kg/m3 and g is 9.81 m/s2

The second term can also be written as S.G * 9810 Pa where S.G. is specific gravity

w.r.t. water

Page 7: PERMEABILITY Flow of Liquids in Porous Media

Flow Potential - Gravity TermField

In Field units: = p – Z ρ g / conversions = p – Z (S.G.) c

Z+ Z is elevation measured from a datum

Both and p are measured in psi Z is measured in ft, ρ is in lbm/ft3 and g is 32.7 ft/s2 conversions are complicated S.G. is specific gravity with respect to water and is

dimensionless c is 0.433 psi/ft

Page 8: PERMEABILITY Flow of Liquids in Porous Media

Flow Potential - Darcy’s Experiment

Discuss ABW, Fig. 2-26 (pg. 68) Confirm that for the static (no flow) case, the flow

potential is constant (there is no potential gradient to cause flow)

top of sand pack bottom of sand pack

Page 9: PERMEABILITY Flow of Liquids in Porous Media

Flow Potential - Example Problem

Discuss ABW, Example 2-8 (pg. 75) Solve this problem using flow potential

Page 10: PERMEABILITY Flow of Liquids in Porous Media

Permeability Units

Discuss ABW, Example 2-9 (pg. 79) 2 conversion factors needed to illustrate

permeability units of cm2

cp Pas atm Pa