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Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of Excellence TIG-10 Workshop, Adelaide 11/2010

Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

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Page 1: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Combined Geological Modelling and Flow SimulationJ. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of Excellence

TIG-10 Workshop, Adelaide 11/2010

Page 2: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Outline

• Addressing the problem that geological modelling and geothermal simulation are usually separated (and geological uncertainty not considered – even if significant)

• Workflow to integrate both steps into one framework

• Two example models:

1. Hypothesis testing for different geological scenarios2. Combination with geological uncertainty simulation

Page 3: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Geological Modelling

• Construction of a structural representation of the subsurface

• Interpolation based on discretized geological observations (e.g. from drillholes, seismics, field work)

• Applied modelling tool: GeoModeller (Intrepid Geophysics, BRGM)

(Calcgano et al., 2008)

Page 4: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Geothermal Flow Simulation

• Coupled simulation of fluid and heat transport equations in the subsurface

• Based on property distribution (e.g. permeability, porosity, thermal conductivity, heat capacity) in subsurface and boundary conditions (e.g. basal heat flux)

• Applied simulators: TOUGH2, SHEMAT

Permeability Porosity

Page 5: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Boundary conditions

Geological Model

Mesh

Property assignment

Simulation

Discretized geological model

Geological Data

Manual steps

Page 6: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Critical steps

• Mainly related to

– model construction, – mesh generation and – processing to flow simulation

Once constructed, the geological model is rarely changed or extended, even if significant source of uncertainty!

Steps before flow simulation

Page 7: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Automation steps

Geological modeling

Discretization

Model simulation setup

Simulation and analysis

Implicit potential-field method (GeoModellerTM); enables direct model update

Automated rectilinear mesh discretization (python scripts)

Direct update of input files for simulation with SHEMAT and TOUGH2 (python scripts)

Simulation with available codes, post-processing and analysis (python scripts)

Change one data point

Evaluate effect on flow field

Page 8: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Geological Hypothesis Testing

near-surface heat flux (z-dir)

Page 9: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Combination with Uncertainty Simulation

• Consider uncertainties in structural geological models (one of main sources of uncertainty)

• Approach: random change of input data (discretized surface position, orientation data)

Page 10: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of
Page 11: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Wells don’t penetrate basement!

Assume: structure more or less well defined (seismics) but exact position at depth unknown

Example model North Perth Basin

Page 12: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Change bottom of formations randomly

Formation Name Standard deviation

Cadda 20m

Woodada-Kockatea 100m

Permian 200m

Standard deviation for data points defined at bottom of formation

Position of formation bottoms changed about random value

Create 20 different input data sets and 20 different models

Page 13: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Results of simulation

• For 20 geological models, we obtain 20 simulated flow and heat flow fields (drawing from the uncertainty distributions)

Example of one temperature model

Page 14: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Local mean and standard deviation of Temperature

mean

stdev

Page 15: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Conclusion

• Uncertainties in structural model influence simulated geothermal flow field but they are usually not considered

• Developed integrated workflow

– enables hypothesis testing and consideration of geological uncertainty

– compliments and extends other approaches (e.g. stochastic simulation, as presented by Tony Meixner), e.g.:

• physics (multi-phase, thermo-hydro)• mesh (rectilinear)• consideration of uncertainties in geological data (not the

model)

• Specifically suited for early exploration stages and resource evaluation where uncertainties in the structural model are dominant.

Page 16: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Outlook

• Complete implementation on supercomputer

• Optimal mesh construction for geological models (e.g. automatic rectilinear refinement, extruded triangular for TOUGH2)

• Coupling to advanced resource estimation methods (talk at AGEC)

• Combination with GIS methods

Thank you for your attention!

Page 17: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Appendix

Page 18: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Uncertainty in Geology models: different types

Incomplete knowledge

Are all relevant structures known?

How to analyse uncertainties in structural models?

Page 19: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Uncertainty in Geology models: different types

Uncertainty of interpolation

How good is the interpolation between data points?

How to analyse uncertainties in structural models?

Page 20: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Uncertainty in Geology models: different types

How exact is the data?

Uncertainty in raw data

How to analyse uncertainties in structural models?

• Applies specifically to interpreted data and assumptions• We consider this to be a significant part of model uncertainties(Wellmann et al, 2010)

Page 21: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

“Complex” and “simple” geological settings

Page 22: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Mesh geometries

• Regular mesh

• Rectilinear mesh

• Extruded triangular mesh (only TOUGH2)

(work in progress: optimal mesh generation from geological models)

(Include example extruded triangular?)

Page 23: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Processing simulated models to simulation

Coupled fluid and heat flow simulation in a 2-D subset of the model

Discretization in a regular grid

Two highly permeable formations

Page 24: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Convective vs. conductive heat transfer

• Local Peclet number

Pe = l v /

In our case:- l: characteristic length- v: fluid velocity (model

result)- : thermal diffusivity

(10-6 m2/s)Conduction dominated: low Pe-Number

Convection dominated: high Pe-Number

As characteristic length scale, we use engineering lifetime of 30 years and get l approx 60 m

Page 25: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Example of local Pe-Numbers for one model

Pex

Pez

left right

down up

Page 26: Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of

Local mean and standard deviation: Pe z-direction