pore-scale modelling of macroscopic rock properties

23
9th Euroconference on Rock Physics and Geomechanics Trondheim, Norway 17 – 21 October 2011 Pore-scale modelling of macroscopic rock properties Cathrine Ringstad Pål-Eric Øren Thomas Ramstad

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9th Euroconference on

Rock Physics and Geomechanics

Trondheim, Norway

17 – 21 October 2011

Pore-scale modelling of

macroscopic rock properties

Cathrine Ringstad

Pål-Eric Øren

Thomas Ramstad

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK SIZE AND RESOLUTION

Typical grid size

10003 – 12003 voxels

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK SIZE AND RESOLUTION

Pore space

Quartz

Feldspar

Resolution = 10 mm

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK SIZE AND RESOLUTION

Pore space

Quartz

Feldspar

Resolution = 10 mm

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK SIZE AND RESOLUTION

Pore space

Quartz

Feldspar

Resolution = 10 mm

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK SIZE AND RESOLUTION

Typical grid size = 10003 – 12003 voxels

Typical voxel resolution = 2 – 5 µm

Typical sample size = 2 – 6 mm3

Low resolution High resolution

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK PROCESS BASED

PROPERTIES

SEM analyses

Geological modelling

SEM imaging

Sample preparation

WORKFLOW

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK PROCESS BASED

SEM analyses

Geological modelling

SEM imaging

Sample preparation

WORKFLOW

µCT IMAGE

Image processing

Interpretation

µCT imaging

Sample preparation

WORKFLOWPROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK PROCESS BASED µCT IMAGE

Micro-structure

Weakly consolidated

Analogue

Sandstone and carbonate

PROS and CONSPROPERTIES

Segmentation

Consolidated only

Direct model

All types of rocks

PROS and CONS

Pore-scale modelling of macroscopic rock properties

1

10

100

1000

10000

0,0 0,1 0,2 0,3

Porosity [fraction]

Per

mea

bilit

y [m

Dar

cy]

Elasticity

Formation resistivity factor

Absolute permeability

NMR relaxation time

krw_exp1kro_exp1krw_exp2kro_exp2krw_exp3kro_exp3krw simkro simkrw avgkro avg

Rel

ativ

e pe

rmea

bilit

y

1.0

0.8

0.6

0.4

0.2

0.01.00.80.60.40.20.0

Sw [fraction]

Relative permeability

Capillary pressure

Resistivity index

DIGITAL ROCK PETROPHYSICAL FLUID FLOW

PROPERTIES

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK

FLUID FLOW

GRID PORE NETWORK

Resolution limited by grid

Computer intensive

Capillary and viscous flow

Exact pore space

PROS and CONS

Infinite resolution

Capillary flow

Simplified pore space

Fast

PROS and CONSPROPERTIES

Pore-scale modelling of macroscopic rock properties

0.0

1.0

0.8

0.6

0.4

0.2

0.01.00.80.60.40.2

Water saturation Sw [fraction]

krw

kroPrimary drainage

Re

lati

ve p

erm

ea

bil

ity

k r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

krw =kwater

kabs

kro =koil

kabs

Swi

Pore-scale modelling of macroscopic rock properties

0.0

1.0

0.8

0.6

0.4

0.2

0.01.00.80.60.40.2

Water saturation Sw [fraction]

krw

kroImbibition

Re

lati

ve p

erm

ea

bil

ity

k r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

krw =kwater

kabs

kro =koil

kabs

Swi Sor

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Grid Network

Process based µCT image

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Primary drainage

PBM model of Sandstone B

Network

Grid

Lab data

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Primary drainage

PBM model of Sandstone B

Network

Grid

Lab data

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Primary drainage

PBM model of Sandstone B

Network

Grid

Lab data

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Grid Network

Process based µCT image

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Imbibition

Sandstone A – Network simulations

µCT model

PBM model

Lab data

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Imbibition

Sandstone A – Network simulations

µCT model

PBM model

Lab data

Pore-scale modelling of macroscopic rock properties

0,0

0,2

0,4

0,6

0,8

1,0

0,0 0,2 0,4 0,6 0,8 1,0

Water saturation Sw [fraction]

Rela

tive p

erm

eabil

ity k

r

DIGITAL ROCK

FLUID FLOW

PROPERTIES

RELATIVE PERMEABILITY kr

Imbibition

Sandstone A – Network simulations

µCT model

PBM model

Lab data

Pore-scale modelling of macroscopic rock properties

DIGITAL ROCK

FLUID FLOW

PROPERTIES

CONCLUSIONS

1) Pore scale derived properties are

comparable to laboratory data

2) Both µCT imaging and process based

modelling (PBM) may be used to generate

representative digital rock models

3) Grid and network calculations of relative

permeability produce similar results

THANK YOU FOR YOUR ATTENTION!