Geothermal Flashcards

1
Q

Earth’s heating?

A
  • Much of the internal heat of the Earth is thought to come from the decay of radioactive thorium.
  • Thorium-232 is the main natural radioactive isotope. It decays to Lead- 208 via alpha decay* and has a half-life of 14 billion years.
  • The Earth still has about 85% of the thorium it had when it formed.
  • Convection in mantle
  • Emplacement of granites
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2
Q

Iceland and UK heat sources?

A

Iceland: 30 high temperature systems: T>250 degrees C

UK:
• Only area higher than 120 millawatts per m2 is South West – Cornwall – granites – high abundance of thorium
• Average heat flow in Whin Sill in north
• Average thermal gradient 26 degrees per km

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3
Q

Types of geothermal?

A
•	Shallow
•	Hydrothermal Systems
o	Confined to areas of high heat flow on plate boundaries
•	Engineered geothermal systems
o	Redruth, Cornwall
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4
Q

Shallow?

A

Ground source heat pumps:
• An energy efficient heat/cooling device that absorbs heat from or rejects heat to the ground
• Uses the earth as a heat source in winter and sink in summer
• Based on convection cycle

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5
Q

Hydrothermal?

A
  • Water moves down through the ground
  • Reaches hot rock
  • Heated
  • Moves in a convection cycle
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6
Q

Engineered Geothermal Systems?

A
  • Fracture stimulation of hot, dry rock
  • Increasing permeability and therefore flow in rock
  • Injects water into the rock
  • Hot water rises back up production well
  • Generates electricity
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7
Q

Europe’s capabilities?

A
  • At 5km if it utilised 5% of the rock volume with greater temperatures than 160 degrees
  • Would support 130 GWe of power generation
  • Generate 900 TWh

Currently Geothermal Power plants using hydrothermal systems are confined to areas of high heat flow on plate boundaries

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8
Q

Geothermal Power Generation (Dry Steam Power)?

A
o	Only 5 Dry Steam Fields worldwide
o	Hydrothermal fluids used directly to turn turbine
o	No need for separation
o	20-100 MWe
o	Temperature above 210 degrees C
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9
Q

Geothermal Power Generation (Flash Power Plant)?

A
o	Steam used for electricity production
o	Brine and steam separated
o	High pressure steam contains more energy than brine
o	20-100 MWe
o	Temperature above 210 degrees C
o	Iceland – Hellisheioi Power Plant
•	Combined heat and power
•	300 MWe and 100 MWt
•	50 boreholes – 2000m deep
•	Re-inject non-condensable gases into ground (H2S)
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10
Q

Binary Power Plant?

A

o Use in lower temperature fields
o Hydrothermal fluids separate from ‘binary’ fluid
o Binary fluid has low boiling point (butane, pentane) – vaporised in heat exchanger that drives turbine

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11
Q

Weardale?

A

• NW England
o Modest heat flow
o Mining history from coal mining
o Warm water known from the mines
• Granite proved 1961
• 1962 Woodlands confirmed the high heat flow
• 2004 Eastgate 1 confirmed high fluid flow
• 2010 Eastgate 2 tested the geological model
• Trial pits – proved local till deposits contain huge boulders (erratics) in silty matrix
o Inclined boreholes proved Slitt Vein 8m wide
• Eastgate geothermal gradient 38 degrees per km (UK average of 21)

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12
Q

UK warm water deep basin potential?

A
  • Southampton District Energy Scheme
  • Single borehole to 2km into Triassic Sherwood Sandstone
  • Temp 75 degrees C
  • Power 1.7MW
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13
Q

Triassic Sherwood Sandstone – Outcrop

A
  • High net to gross reservoir
  • High porosity
  • High permeability
  • High kv/kh
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14
Q

Formation resource evaluation:

A

• Geothermal resource calculation requires:
o A geological model of the aquifer (reservoir)
o Maps of the temperature field
o Estimates of the hydraulic properties of the aquifer, especially porosity
• Permeable, porous rocks are mainly found at depth in the Mesozoic basins
• Five main basins in the UK:
o Northern Ireland
o East Yorkshire and Lincolnshire
o Cheshire
o Worcester
o Wessex

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15
Q

Hydraulic Properties of the Aquifer:

A

• Porosity
• Permeability
o From interconnections between voids in the rock
o Primary permeability from interconnected pores
o Secondary permeability from fracking
o Pumping test reliable way to measure
• Transmissivity = permeability x thickness
o Transmissivity limits can be used to define the productive reservoir
o Much of the reservoir transmissivity is often contained in a few highly permeable zones

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