Hydroelectric power

From AAPG Wiki
Jump to: navigation, search
Energy: A Historical Perspective and 21st Century Forecast
Series Studies in Geology
Chapter Sources of Energy
Author Dr. Amos Salvador
Link Web page
PDF PDF file (requires access)

The energy supplied by flowing water has been used by humans since shortly before the start of the Christian era: the waterwheel, the geared water mill, and the Vitruvian mill received increased use as civilization developed in the Mediterranean region.

Uglich hydroelectric power plant, Russia. Courtesy Wikimedia Commons.

During the Middle Ages, the use of the geared water mill extended throughout Western Europe, where it was used to grind grain, to saw wood and marble, and to crush metallic ores. Water mills became the base for the beginning of industrial development. Flowing water as a source of energy extended to many other regions of the world in subsequent years.

Figure 1 World hydroelectric power generation and percent of the world's total electricity generation.[1]

However, it was not until the flow of water was used in the generation of electricity that water started to make a major contribution to the world's supply of energy. Hydroelectric power is, as of 2005, the second largest source of electricity in the world (18%) after coal, which supplies about 38%, but ahead of nuclear power, natural gas, and oil, which contribute 17, 16, and 10%, respectively, of the total generated electricity.

The world's first hydroelectric power plant was built at Godalming, in England, in 1881. Hydroelectric power developed rapidly during the 20th century, even in countries with other abundant sources of energy.

Hydroelectric power was at first believed to be an attractive source of energy, potentially widely distributed around the world, environmentally clean, inexhaustible, efficient, and economically competitive, especially attractive to countries with limited fossil fuel resources. It has been found that this was not always the case.

Although dams, not only those built for the generation of electricity but also those designed for flood control, irrigation, water supply, or a combination of these purposes, have delivered significant benefits, they have often been the cause of disastrous social upheavals and major negative environmental impacts, and their construction has serious geographic limitations.

  • Large areas upstream from the dam have been flooded, in some cases covering rich and fertile agricultural land.
  • The populations in these flooded areas have been displaced, causing them to lose not only their homes but their livelihoods and their sociocultural foundations as well. It has been estimated that between 40 and 80 million people may have been displaced between 1950 and 1990, 26–58 million of them in India and China. According to the World Commission on Dams
    ...the impacts of dam-building on people and livelihoods—both above and below dams—have been particularly devastating in Asia, Africa, and Latin America, where existing river systems supported local economies and the cultural way of life of a large population containing diverse communities.[2]
  • Dams alter and divert river flow affecting access to water, transforming landscapes, and resulting in significant irreversible impact on the environment both upstream and downstream from the dams. They often have a negative impact on rivers, watersheds, and aquatic ecosystems.
  • Evaporation of the water in the reservoirs upstream from the dams becomes a problem in some cases, particularly in arid regions where fresh water is a priceless commodity, needed for agriculture and human consumption.
  • Hydroelectric plants are not necessarily inexhaustible sources of electricity. They have a limited operating life. The reservoirs behind the dams become silted up in many cases with the consequent long-term loss of water storage capacity. The sediment caught at the dam can sometimes cause the erosion of the turbines if it reaches the power intakes. The retention of sediment behind the dam can also be the cause of serious problems downstream, where the reduced influx of sediment often results in important changes of the river valley, sometimes all the way to its delta. The Aswan High Dam in Egypt and the Hoover Dam in southwestern United States are good examples of such problems. In Egypt, for thousands of years, farmers along the Nile Valley counted on the yearly floods to bring organically rich silt that fertilized their intensely cultivated plots. Now, the silt piles up behind the Aswan Dam.
  • Finally, the development of large-scale hydroelectric power requires sites that allow the building of dams that provide a high head (height of water fall), located in a river with high water flow, with large water-storage capacity, and, preferably, near centers of electricity consumption. These dams are sometimes called "large dams" and are defined as having a height of 15 m (50 ft) or more from the foundation or, if only 5–15 m (16–50 ft) in height, having a reservoir volume of more than 3 million m3 (177 million ft3). Sites favorable for the building of large dams are limited in number and unevenly distributed throughout the world. They are not found, for instance, in arid regions with low rainfall and, therefore, with no permanent streams, or in regions of low relief. Although most of the world's sites for the building of hydroelectric power plants have been identified, only a relatively small proportion have been developed, mostly in the industrialized countries. At least seven European countries (Austria, France, Italy, Norway, Spain, Sweden, and Switzerland) generate substantial percentages of their electricity in hydroelectric plants.

The building of large dams requires large initial capital investment that is not always rewarded with favorable economic profitability. The reported returns on the investments made in hydroelectric power plants have increasingly been questioned.

Small-scale hydroelectric power plants (small dams or run-of-river plants) are widely distributed throughout the world. They can serve local needs and are often the foundation of rural electrification, but they provide overall only a small percentage of the total world hydroelectricity. Many of them are located in mountainous regions with steep, fast-flowing rivers, in which large dams backing sizable reservoirs cannot be built.

Despite these serious problems, the building of hydroelectric dams increased rapidly during the middle years of the 20th century (1930s to 1970s) and peaked in the 1970s, when an average of two or three large dams were commissioned each day somewhere in the world. Their number increased from 5000 in 1949 to 45,000 in the late 1990s[3] However, information on the unfavorable impacts of dams on people, river basins, the environment, and aquatic life, as well as their not-always-favorable economic performance, in the last 20–30 years generated considerable opposition to the building of dams. This opposition has become more widespread, vocal, and organized and has contributed to a decline in the pace of construction of new, large hydroelectric dams over most of the world in the past two decades. The exceptions are China, where the huge Three Gorges hydroelectric dam is expected to be commissioned between 2003 and 2009, India, and Brazil, where a considerable amount of hydroelectric capacity is under construction or planned. Also contributing to this decline in North America and Europe has been the fact that most technically attractive sites have already been developed. The average large dam today is about 35 years old.

Momentum for river restoration is also accelerating in many countries, especially in the United States, where the decommissioning rate for large dams has overtaken the rate of construction since 1998. Antidam strategies developed principally by environmental and human rights activist groups worldwide have been effective in reducing the pace of construction of dams, of all kinds and sizes, in most countries of the world since the 1970s. Although the global effects on the environment are much less damaging than those of other energy options, the local effects have been made to appear greater.

Nevertheless, hydroelectric power is still important in some countries, especially in those that are short of other sources of electricity but have large rivers originating in mountainous regions.

Additional resources

World Energy Council Survey of Energy Resources, 2001. Discerning although somewhat supportive review of the pros and cons of hydropower.

See also


  1. Salvador, A., Energy-A Historical Perspective and 21st Century Forecast: AAPG Studies in Geology 54, 208 p.
  2. World Commission on Dams, 2000, Dams and development-A new framework for decision-making: London, England, Earthscan Publications Ltd., p. 102.
  3. World Commission on Dams, 2000, Dams and development-A new framework for decision-making: London, England, Earthscan Publications Ltd., 404 p.

External links

find literature about
Hydroelectric power
Datapages button.png GeoScienceWorld button.png OnePetro button.png Google button.png