Converting Geothermal To Electric Energy (2)

Dry Steam Power Plant Geothermal EnergyIn basic terms, geothermal energy is thermal power (the energy that determines the temperature of matter) generated and stored in the Earth. The geothermal power of the Earth’s crust originates from the original formation of the planet and from radioactive decay of minerals, resulting in continual production of geothermal power below the earth’s surface. The geothermal gradient, which is the distinction in temperature involving the core of the planet and its surface, drives a continuous conduction of thermal power in the kind of heat from the core to the surface.

The United States generates the most amount of geothermal power of any other nation. Every single year, the U.S. generates about 15 billion kilowatt-hours, or the equivalent of burning about 25 million barrels of oil. Industrial geothermal technologies have been concentrated in the western U.S. In 2012, Nevada had 59 geothermal projects either operational or in improvement, followed by California with 31 projects, and Oregon with 16 projects.

In a geothermal dry steam energy plant, steam alone is made directly from the geothermal reservoir and is employed to run the turbines that energy the generator (Figure 6). Due to the fact there is no water, the steam separator employed in a flash plant is not necessary. Dry-steam energy plants account for around 50% of installed geothermal capacity in the U.S. and are located in California.

Binary cycle power plants operate on water at reduce temperatures of about 225°-360°F (107°-182°C). Binary cycle plants use the heat from the hot water to boil a operating fluid, typically an organic compound with a low boiling point. The operating fluid is vaporized in a heat exchanger and applied to turn a turbine. The water is then injected back into the ground to be reheated. The water and the operating fluid are kept separated during the whole course of action, so there are tiny or no air emissions.

Ocean – substantial bodies of water up to 3.7 km deep sitting on best of the oceanic crust. The water temperature at the surface is larger than the deep water temperature due to solar heating and thermal convection in the water which keeps it that way given that the heavier cold water remains in the depths and the warmer, less dense water stays on the surface.