GEOTHERMAL ENERGY Flashcards
Geo - Earth, Thermal - Heat
Natural Heat of the Earth
Source of Heat
?Heat flows outwar from Earth’s Interior
?the crust insulates us from the interior Hear
?Mantle is Semi Molten
?Outer Core is liquid and Inner Core is Solid
Regions where geothermal system is situated
Volcanic Regions
Heat source
Magma intruded to shallow levels (<6 KM) in the crust in the Recent Past (<100K years)
Reservoir Characteristics
?Fractured Rocks (3-10km)
?Permeable and Porous
?Needs water to sustain Convection and ?Produce Steam
Seal / Cap Rock
Impermeabl or Semi-Permeable
Elemets of a Geothermal System
1) Water - Sufficient to effect Convection needs recharge
2) Cap Rock - Impermeable Rock Formation
3) Reservoir - Permeable and Porous Rocks neutral kasi nagreact na sa wall rocks, if directly above the magma acidic
4) Heat Source - Shallow levels (<6km) in the recent (<100,000 yrs) past
Geysers
Alternating eruption and quiessence of Water due to heating and pressure
Silica Sinter Terrace
Form in neutral areas, deposits from the boiling water, mountains of silica terraces
Blue Water - Neutral
Fumaroles
Steam Vents
Hot Spring
Hot Boiling Waters
Thermal Area/ Steaming Ground
May usok lang
Mud Pool
bubbling of mud
Algal Mat
Emerald Green Waters due to algae with Gold at the side due to oxidation
Travertine
Form if limestone deposited by Mineral Springs
Edge of the reservoir
Hot pool
Blue water due to nuetrality
Solfatara
Steam Vents with significant Sulfur Deposition fumarole rich in Sulfur
Saffioni
Fumaroles with high Boric Acid
Kaipohan
Cold Gas emission w/ intense argillic alteration
?A place in Valencia Negros Oriental
?Trees are dead
Enthalpy
Total Heat content of a system
Critical Pt of Water
374 deg C
Classes of Geothermal Systems are based on
Entalphy (Heat Content) and
Pressure
Classes 1 -4
Low Entalphy
All Liquids
Class 5-6
Twophased
High Entalphy