Slide 7
1. Left-over heat from the time of the accretion of the earth (4.6 By BC) (30%)
2. heat generated by the decay of the long-lived radioactive isotopes of uranium (U238, U235), thorium (Th232) and potassium (K40) (70%).
Slide 8
1 Origins of geothermal energy Temperature distribution in the earth
Temperatures in the earth Geothermal gradient in the upper 150km
dT/dz ~ 30 oC/km
Slide 9
1 Origins of geothermal energy Mechanisms of heat transport in the earth
1) Heat transport by conduction
Fourier’s law
Thermal conductivity of rocks
Slide 10
1 Origins of geothermal energy Mechanisms of heat transport in the earth
(2) Heat transport by
convection
Mantle convection driving
the plates
Numerical simulation of
Mantle convection
Slide 11
1 Origins of geothermal energy Heat flow at the earth’s surface
Average heat flow
= 60mW/m2
Compare with
Solar Constant
S= 1360 W/m2
Note the large lateral variations across the surface of the earth
Explanation by
Theory of
Plate Tectonics
Slide 12
1 Origins of geothermal energy The earth’s thermal regime and relation with plate tectonics
Slide 13
1 Origins of geothermal energy The earth’s thermal regime and relation with plate tectonics
Plates, plate boundaries and distribution of volcanoes across the earth
Slide 14
1 Origins of geothermal energy Plate tectonics and geothermal fields
World pattern of plates, oceanic ridges, oceanic trenches, subduction zones, and geothermal fields.
http://www.geothermal-energy.org/105,interactive_map.html
Slide 15
The “ideal geothermal reservoir”
= high temperatures + water
= steam!!!
Slide 16
2. Classification of geothermal systems/reservoirs
Thermal processes in an “ideal geothermal reservoir” resulting in the
formation of hot steam
Slide 17