What
is Geothermal Energy?
“Geothermal”
comes from the Greek words geo which means earth
and thermo which means heat. It is energy that
taps the natural heat of the earth.
The earth consists of three parts: the core, the
mantle, and the crust. The heat,
which is highly concentrated in the earth’s core, constantly flows
out and transfers to a layer of rock called mantle. Because of high
temperature and pressure, some rocks of the crust melt. This is
called magma which is the most important source of geothermal heat.
Since magma is less dense than nearby rocks, it rises towards the
earth’s crust closer to the earth’s surface. As magma moves up,
it transmits heat through the deeply circulating fluids moving within
the fractured reservoir. When the superheated water or steam rises
to the surface, it forms hot springs, geysers and fumaroles.
What elements compose a geothermal system?
A geothermal system can be likened to a covered pot filled with water.
When heated the water boil and produced steam just like in a geothermal
system.
Four elements compose a geothermal system, namely:
1. A heat source, which is the magma that comes close to the surface
of the earth in volcanic areas.
2. A permeable underground reservoir rock, which can hold or store
water.
3. A solid cap rock, which maintains pressure and does not allow
the heat, water or steam to escape.
4. Water, which serves as the medium for carrying the heat.
Where does the steam come from?
Geothermal reservoirs consist mainly of rainwater or “meteoric water” that
seeps slowly via cracks and faults. This water ultimately reaches
depths of over 3 kilometers where it is heated by hot rocks. Hot
geothermal fluids are tapped by wells at depth and flashed into
steam at the surface or at the wellbore.
One way to recharge a geothermal reservoir is by reinjecting the spent
geothermal fluids. If done properly, reinjection can help maintain
reservoir volume and pressure. However, experience in several geothermal
fields has shown that reinjecting cold brine too close to production
wells can adversely affect steam production.
What signs indicates
the presence of geothermal resources?
The presence of geothermal resources is indicated by volcanoes,
hot spring, fumaroles and solfataras. The Philippine archipelago
hosts several volcanic areas where geothermal resources occur. Geoscientists
believe that a potential of about 4,339 MW (megawatts) can be tapped
from these resources.
How long does a geothermal field lasts?
There is a finite volume of hot fluids available in any geothermal reservoir.
Natural recharge is usually very slow and production wells begin
to decline as soon as commercial operation starts. Therefore the
“lifetime” of a particular field will depend on the development
size (that is, extraction rate) and re-injection strategy.
Many fields have produced geothermal steam and generated power for over
30 years through drilling of new wells to replace declining ones.
The Larderello field in Italy was first developed in 1904 and is still
generating about 547 MW of power today.
Locally, the Makban and Tiwi Geothermal Fields had been in commercial
operation since 1979 or for more than 27 years.
How is geothermal energy converted into electricity?
Geothermal steam is extracted from the reservoir through steel pipes. A mixture
of hot water and steam under its own pressure flows up to the pipe.
Upon reaching the surface, the water and steam pass through a separator
to separate the water and steam and through a scrubber to remove
any impurities. The steam is directed to a power plant to spin the
blades of a turbine while the condensed water is re-injected back
to the reservoir. Attached to the turbine is a generator which produces
the electricity.
The electric current is then transmitted to homes, offices, factories
and other industrial users.
Can a geothermal operation cause a volcanic
eruption?
Scientists agree that no man-made activity can cause a volcanic
eruption. Scientific studies have shown that the drilling of wells
or other geothermal operations have never caused any volcanic eruption.
Geothermal drilling up to 3 km. depth is too shallow to affect a
magma chamber, which typically occurs at a depth of about 15 km.
Where in the Philippines can we find producing
geothermal fields?
Location |
Installed
Capacity |
| Mak-Ban,
Laguna |
458.53
MWe |
|
Tiwi-Albay |
344
MWe |
| Bac-Man,
Sorsogon/Albay |
151.5
MWe |
|
Tongonan, Leyte |
722.68
MWe |
| Palinpinon,
Negros Oriental |
192.5
MWe |
| Mt.
Apo, North Cotabato/Davao |
108.48
Mwe |
The total geothermal power capacity of the Philippines is 1,977.69 megawatts.
|