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sci lesson 3: energy from volcanoes
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geothermal system
is described schematically as convecting water in the upper crust
geothermal system has 3 components
heat source
reservoir
fluid
heat source
can be very high temperature
reservoir
is a volume of hot permeable rocks
geothermal fluid
is the carrier that transfer the heat.
often carry with other chemicals and gas compounds
fluid convection-
the mechanism that governs this geothermal system
geothermal power plant
is like a regular power plant except that no fuel is burned to heat water into steam
the
steam
in geothermal power plant is heated ny the eARTH
production well
is drilled into geothermal reservoir
injection well
is also drilled
hot geothermal fluid flow
through pipes to apower plant to use in generating electricity
hot pressurized geothermal fluid
is allowed to generate rapidly
rotational energy
from the turning turbine shaft is utilized to spin magnets inside a large coil and create electrical current
2 primary pieces of equipement of geothermal energy
turbine and generator
electrical current
is sent to a step-up transformer outside the power plant
voltage
is increased in the transformer and electrical current
dry steam power plant-
uses hydrothermal fluids such as steams
dry steam power plant
is the first type to be developed in italy
dry steam power plant
reached the temperature 150c
dry steam power plant is
still being used in the greysers in california
flash steam power plant- water is pumped from the reservoir under a high pressure
flash steam power plant temp is
182c
binary cycle power plant
does not use water or steam to turn he turbine blades for power generation
advantages of geothermal energy
eco-friendly
high reliability
flexibility
minimum land space
cost-effective
helps developing countries flow
disadvantages of geothermal energy
limited accessibility
financial constraint
possible pollution
metamorphic rocks
- rocks that have undergone a change
sulfur-
mineral found in sedimentary rocks
sulfur
was called
brimstone
in the bible
sulfur
can be found in its elemental states around volcano vents
volcano eruption can be explaihned using the following methods
formation by subduction
and
formation by distension