How Can Petrophysics Support Geothermal Exploration? General - - PowerPoint PPT Presentation

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How Can Petrophysics Support Geothermal Exploration? General - - PowerPoint PPT Presentation

How Can Petrophysics Support Geothermal Exploration? General Remarks Specifics for Geothermal Applications Recommendations Mid-Term Conference 9-12 January 2007 E. Spangenberg, S. Raab, D. Bruhn Exploration allows to extract


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SLIDE 1

How Can Petrophysics Support Geothermal Exploration?

  • General Remarks
  • Specifics for Geothermal Applications
  • Recommendations

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 2

Exploration

Geophysics

Distribution of Measurable Physical Properties in the Subsurface

  • Mineralogical Composition
  • Texture and Structure
  • Porosity and Type of Pores
  • Composition of the Pore Fill
  • Pressure and Temperature

Interpretation Geological Model or Reservoir Model

Knowledge of the dependencies of physical properties on: Distribution of Lithologies, Porosities, Pore Fills, etc. allows to extract information of geological relevance

Petrophysics

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 3

Petrophysics for Geothermal Application – A Challenge for Experimentalists

Simulation of in situ conditions in the laboratory is characterized by confining and pore pressure controlled experiments under high temperatures. Requirements and Problems

  • Special materials
  • Special design of internal set up
  • Longer experimental time
  • Higher failure probability
  • Higher costs

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 4

Possible Subjects of Investigation

  • Dependence of physical rock properties on temperature
  • Production stimulated fluid rock interactions under high temperature

Assessment of long term behaviour of the reservoir

  • Phase transitions in the reservoir
  • Mid-Term Conference 9-12 January 2007
  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 5

Examples

Temperature Dependence Influence of “boiling pore water”

Kulenkampff et al., 2005 Basalt: Krafla, Nesjavellir L.H. Kristinsdóttir et al., 2006 Hyaloclastite: Hengill

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 6
  • State of the Art

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 7

Advantages - Limitations

  • Reusable internal set up
  • Shrinkable tubing – FEP, PFA

(Fluoropolymers) 250-300°C

  • Standardized samples

and sample preparation

  • Polymers – PTFE, PEEK

250-300°C

  • Measurement of different

properties in on experiment

  • Seals – Viton, PTFE

250-300°C

  • Piezoceramics – sonic transducers

Curie temperature up to 300°C Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 8

Dehydration of Serpentinite

Fast Dehydration Slow Dehydration

Resistivity [ m ] ฀ 10 10 10 10 10 10

7 6 5 4 3 2

20° 100°

2x10 4x10 6x10

5 5 5

Time [ sec ]

10 kHz 109 Hz 100 mHz

10 kHz 109 Hz 100 mHz

500° 560° 560° 550° 500° 400° 300° 400°

Resistivity [ m ] ฀ 10 10 10 10 10 10 10 0 1x10 2x10 3x10

7 6 5 4 3 2 1 5 5 5

600 °C 600 °C 600 °C 500 °C 400 °C 157 °C 400 °C 300 °C 200 °C 200 °C

Time [ sec ]

256 °C 413 °C 10 kHz 109 Hz 100 mHz

Bruhn et al., 2005

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 9

“The Next Generation”

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
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SLIDE 10

Higher temperatures require:

  • sample protection against confining pressure medium by a metal jacket
  • to avoid chemical reactions between the pore fluid and the jacket is has

to be chemically inert (gold, platinum)

  • high temperature gradients within the pressure vessel
  • high temperature in the centre where the sample is placed
  • low temperature at the closers to protect seals and some

temperature sensible parts (piezoceramic transducers)

  • special design of the internal set up

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn
  • special preparation techniques
  • the parts in the hot zone of the set up are “one way components”
  • Do not underestimate the effort, time, and costs for

experiments under high temperature!

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SLIDE 11

Recommendation

If a problem is identified that requires petrophysical experiments within a geothermal Project it is important to:

  • define the objective of the investigation clearly
  • design an experimental set up for exact this objective
  • budget sufficient
  • lead time for the construction and test of the experimental set up,
  • men power for the design, set up, test, preparation,

and measurement

  • money

Mid-Term Conference 9-12 January 2007

  • E. Spangenberg, S. Raab, D. Bruhn