Geothermal power

The invention: Energy generated from the earth’s natural hot
springs.
The people behind the invention:
Prince Piero Ginori Conti (1865-1939), an Italian nobleman and
industrialist
Sir Charles Parsons (1854-1931), an English engineer
B. C. McCabe, an American businessman
Developing a Practical System
The first successful use of geothermal energy was at Larderello in
northern Italy. The Larderello geothermal field, located near the city
of Pisa about 240 kilometers northwest of Rome, contains many hot
springs and fumaroles (steam vents). In 1777, these springs were
found to be rich in boron, and in 1818, Francesco de Larderel began
extracting the useful mineral borax from them. Shortly after 1900,
Prince Piero Ginori Conti, director of the Larderello borax works,
conceived the idea of using the steam for power production. An experimental
electrical power plant was constructed at Larderello in
1904 to provide electric power to the borax plant. After this initial
experiment proved successful, a 250-kilowatt generating station
was installed in 1913 and commercial power production began.
As the Larderello field grew, additional geothermal sites throughout
the region were prospected and tapped for power. Power production
grew steadily until the 1940’s, when production reached
130 megawatts; however, the Larderello power plants were destroyed
late inWorldWar II (1939-1945). After the war, the generating
plants were rebuilt, and they were producing more than 400
megawatts by 1980.
The Larderello power plants encountered many of the technical
problems that were later to concern other geothermal facilities. For
example, hydrogen sulfide in the steam was highly corrosive to copper,
so the Larderello power plant used aluminum for electrical connections
much more than did conventional power plants of the time. Also, the low pressure of the steam in early wells at Larderello
presented problems. The first generators simply used steam to drive
a generator and vented the spent steam into the atmosphere. Asystem
of this sort, called a “noncondensing system,” is useful for small
generators but not efficient to produce large amounts of power.
Most steam engines derive power not only from the pressure of
the steam but also from the vacuum created when the steam is condensed
back to water. Geothermal systems that generate power
from condensation, as well as direct steam pressure, are called “condensing
systems.” Most large geothermal generators are of this
type. Condensation of geothermal steam presents special problems
not present in ordinary steam engines: There are other gases present
that do not condense. Instead of a vacuum, condensation of steam
contaminated with other gases would result in only a limited drop
in pressure and, consequently, very low efficiency.
Initially, the operators of Larderello tried to use the steam to heat
boilers that would, in turn, generate pure steam. Eventually, a device
was developed that removed most of the contaminating gases from
the steam. Although later wells at Larderello and other geothermal
fields produced steam at greater pressure, these engineering innovations
improved the efficiency of any geothermal power plant.
Expanding the Idea
In 1913, the English engineer Sir Charles Parsons proposed drilling
an extremely deep (12-kilometer) hole to tap the earth’s deep
heat. Power from such a deep hole would not come from natural
steam as at Larderello but would be generated by pumping fluid
into the hole and generating steam (as hot as 500 degrees Celsius) at
the bottom. In modern terms, Parsons proposed tapping “hot dryrock”
geothermal energy. (No such plant has been commercially operated
yet, but research is being actively pursued in several countries.)
The first use of geothermal energy in the United States was for direct
heating. In 1890, the municipal water company of Boise, Idaho,
began supplying hot water from a geothermal well. Water was
piped from the well to homes and businesses along appropriately
namedWarm Springs Avenue. At its peak, the system served more than four hundred customers, but as cheap natural gas became
available, the number declined.
Although Larderello was the first successful geothermal electric
power plant, the modern era of geothermal electric power began
with the opening of the Geysers Geothermal Field in California.
Early attempts began in the 1920’s, but it was not until 1955 that B.
C. McCabe, a Los Angeles businessman, leased 14.6 square kilometers
in the Geysers area and founded the Magma Power Company.
The first 12.5-megawatt generator was installed at the Geysers in
1960, and production increased steadily from then on. The Geysers
surpassed Larderello as the largest producing geothermal field in
the 1970’s, and more than 1,000 megawatts were being generated by
1980. By the end of 1980, geothermal plants had been installed in
thirteen countries, with a total capacity of almost 2,600 megawatts,
and projects with a total capacity of more than 15,000 megawatts
were being planned in more than twenty countries.
Impact
Geothermal power has many attractive features. Because the
steam is naturally heated and under pressure, generating equipment
can be simple, inexpensive, and quickly installed. Equipment
and installation costs are offset by savings in fuel. It is economically
practical to install small generators, a fact that makes geothermal
plants attractive in remote or underdeveloped areas. Most important
to a world faced with a variety of technical and environmental
problems connected with fossil fuels, geothermal power does not
deplete fossil fuel reserves, produces little pollution, and contributes
little to the greenhouse effect.
Despite its attractive features, geothermal power has some limitations.
Geologic settings suitable for easy geothermal power production
are rare; there must be a hot rock or magma body close to
the surface. Although it is technically possible to pump water from
an external source into a geothermal well to generate steam, most
geothermal sites require a plentiful supply of natural underground
water that can be tapped as a source of steam. In contrast, fossil-fuel
generating plants can be at any convenient location.