Essay On Energy Power And Human Development

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Energy and Human Evolution
by David Price

Please address correspondence to Dr. Price,
254 Carpenter Hall, Cornell University,
Ithaca, NY 14853.
From Population and Environment: A Journal of Interdisciplinary Studies
Volume 16, Number 4, March 1995, pp. 301-19
1995 Human Sciences Press, Inc.

Life on Earth is driven by energy. Autotrophs take it from solar radiation and heterotrophs take it from autotrophs. Energy captured slowly by photosynthesis is stored up, and as denser reservoirs of energy have come into being over the course of Earth's history, heterotrophs that could use more energy evolved to exploit them, Homo sapiens is such a heterotroph; indeed, the ability to use energy extrasomatically (outside the body) enables human beings to use far more energy than any other heterotroph that has ever evolved. The control of fire and the exploitation of fossil fuels have made it possible for Homo sapiens to release, in a short time, vast amounts of energy that accumulated long before the species appeared.

By using extrasomatic energy to modify more and more of its environment to suit human needs, the human population effectively expanded its resource base so that for long periods it has exceeded contemporary requirements. This allowed an expansion of population similar to that of species introduced into extremely, propitious new habitats, such as rabbits in Australia or Japanese beetles in the United States. The world's present population of over 5.5 billion is sustained and continues to grow through the use of extrasomatic energy.

But the exhaustion of fossil fuels, which supply three quarters of this energy, is not far off, and no other energy source is abundant and cheap enough to take their place. A collapse of the earth's human population cannot be more than a few years away. If there are survivors, they will not be able to carry on the cultural traditions of civilization, which require abundant, cheap energy. It is unlikely, however, that the species itself can long persist without the energy whose exploitation is so much a part of its modus vivendi.

The human species may be seen as having evolved in the service of entropy, and it cannot be expected to outlast the dense accumulations of energy that have helped define its niche. Human beings like to believe they are in control of their destiny, but when the history of life on Earth is seen in perspective, the evolution of Homo sapiens is merely a transient episode that acts to redress the planet's energy balance.

Ever since Malthus, at least, it has been clear that means of subsistence do not grow as fast as population. No one has ever liked the idea that famine, plague, and war are nature's way of redressing the imbalance -- Malthus himself suggested that the operation of "preventive checks," which serve to reduce the birth rate, might help prolong the interval between such events (1986, vol. 2, p. 10 [1826, vol. 1, p. 7]). 1 And in the two hundred years since Malthus sat down to pen his essay, there has been no worldwide cataclysm. But in the same two centuries world population has grown exponentially while irreplaceable resources were used up. Some kind of adjustment is inevitable.

Today, many people who are concerned about overpopulation and environmental degradation believe that human actions can avert catastrophe. The prevailing view holds that a stable population that does not tax the environment's "carrying capacity" would be sustainable indefinitely, and that this state of equilibrium can be achieved through a combination of birth control, conservation, and reliance on "renewable" resources. Unfortunately, worldwide implementation of a rigorous program of birth control is politically impossible. Conservation is futile as long as population continues to rise. And no resources are truly renewable. 2

The environment, moreover, is under no obligation to carry a constant population of any species for an indefinite period of time. If all of nature were in perfect balance, every species would have a constant population, sustained indefinitely at carrying capacity. But the history of life involves competition among species, with new species evolving and old ones dying out. In this context, one would expect populations to fluctuate, and for species that have been studied, they generally do (ecology texts such as Odum, 1971 and Ricklefs, 1979 give examples).

The notion of balance in nature is an integral part of traditional western cosmology. But science has found no such balance. According to the Second Law of Thermodynamics, energy flows from areas of greater concentration to areas of lesser concentration, and local processes run down. Living organisms may accumulate energy temporarily but in the fullness of time entropy prevails. While the tissue of life that coats the planet Earth has been storing up energy for over three billion years, it cannot do so indefinitely. Sooner or later, energy that accumulates must be released. This is the bioenergetic context in which Homo sapiens evolved, and it accounts for both the wild growth of human population and its imminent collapse.

We are caught up, as organic beings, in the natural process through which the earth accepts energy from the sun and then releases it. There has been life on Earth for at least three and a half billion years, and over this time there has been a clear and constant evolution in the way energy is used. The first living things may have obtained energy from organic molecules that had accumulated in their environment, but photosynthetic autotrophs, able to capture energy from sunlight, soon evolved, making it possible for life to escape this limited niche. The existence of autotrophs made a place for heterotrophs, which use energy that has already been captured by autotrophs.

It is not clear how photosynthesis got started, although it is a combination of two systems that can be found singly in some life forms that still exist. But blue-green algae, which are among the earliest organisms documented in the fossil record, already employed the two-stage process that was eventually handed down to green plants. This is a complex sequence of events that has a simple outcome. Carbon dioxide (of which there was an abundance in the earth's early atmosphere) reacts with water through energy from light, fixing carbon and releasing oxygen, and a portion of the energy remains captive as long as the carbon and the oxygen remain apart. Plants release this energy when and where necessary to conduct their metabolic business (Starr & Taggart, 1987).

As time passed, the sheer bulk of life increased, so that more and more energy was, at any given time, stored in living matter. Additional energy was stored when carbon from once-living matter was buried, in ever-so-tiny increments, under the surface of the earth-in deposits that became coal, petroleum, and natural gas as well as in sedimentary rocks containing calcium and magnesium carbonates derived from shells. Of all the carbon that has played a part in the life process, very little was separated out and held apart in this way, but over the course of millions and millions of years, it has mounted up. More and more carbon wound up under the ground, with a greater and greater amount of oxygen in the earth's atmosphere. This separation of carbon and oxygen from a primeval atmosphere in which carbon dioxide and water were abundant represents a vast accumulation of solar energy from the past.

Life evolves to exploit every possible niche, and as autotrophs developed better ways to capture and store the sun's energy, heterotrophs developed better ways to steal it. Independent locomotion was adaptive in the search for nutrients, although it took a little more energy than being buffeted about by the elements. Cold-blooded fish and amphibians were followed by warm-blooded species, which reap the benefits of remaining active at lower temperatures, while using yet more energy in the process. The development of predation opened access to a supply of high-energy food with a further energy investment in procuring it. Throughout the history of life, as increasingly dense reservoirs of energy became available, species that made use of increasing amounts of energy evolved (see Simpson, 1949, pp. 256-57). This is the natural context of Homo sapiens, the most energy-using species the world has ever known.

The extent of human energy use is a consequence of the human capacity for extrasomatic adaptation. This capacity makes it possible for human beings to adjust to a wide variety of novel circumstances without having to wait many generations for evolution to change their bodies. A comparison of somatic and extrasomatic adaptation will show just how remarkable an ability this is: If longer, sharper teeth are adaptive for a predator, animals with teeth that are slightly longer and sharper than those of their fellows will have a slight reproductive advantage, so that genes for longer and sharper teeth will have a slightly greater likelihood of being passed on, and so, over the course of time, the teeth of average members of the population will come to be, little by little, longer and sharper. In contrast, a human hunter can imagine a longer, sharper arrowhead; he can fashion it with nimble hands; and if it is really more efficient than the short, blunt arrowheads that everybody else has been using, his peers will soon adopt the new invention. The chief difference between the two means of adaptation is speed: Humans can adapt, relatively speaking, in a flash.

Extrasomatic adaptation is possible because humans are, in the idiom of the computer age, programmable. Somatic adaptation is like building a hard-wired computer to perform a certain task better than a previous hardwired computer. Extrasomatic adaptation is like writing a new program to perform the task better, without having to build new hardware. The use of language, with its arbitrary relationship between signs and referents, makes possible a wide variety of different software.

Programmability -- the ability to learn -- is not unique with human beings, but they have developed the capacity much further than any other species. Programmability probably developed as an evolutionary response to pressure for flexibility. The ability to make use of a variety of different resources runs deep in the human background, for placental mammals arose from ancestral forms in the order Insectivora that presumably ate insects, seeds, buds, eggs, and other animals. When our hominid ancestors came down from the trees to exploit the African savannas, flexibility was again advantageous. Homo habilis and his fellows were furtive little scavengers who picked what they could from carcasses that leopards left behind and rounded out their diet with fruits and nuts and roots (see Binford, 1981; Brain, 1981). They lived by their wits, and natural selection favored hardware that would permit quick-wittedness.

Programmability -- and the consequent capacity for extrasomatic adaptation -- have made it possible for human beings to advance a very old evolutionary trend at a vastly increased rate. Humans are the most recent in the series of heterotrophs that use increasing amounts of energy, but they differ from other species in this lineup in their ability to use more energy without further speciation. Over the course of humanity's short history, greater and greater amounts of energy have been used by the same biological species (see White, 1949, chapter 13).

Some human innovations have dealt with the fate of energy channeled through metabolic processes. The development of weapons, for example, made it possible to focus somatic energy so as to obtain high-energy foods with much greater efficiency. Man became a hunter. This may have been the innovation that let Homo erectus prosper and permitted his species to radiate out of the African cradle, pursuing game throughout the tropics of the Old World (Binford, 1981, p. 296). Similarly, the use of clothes brought about a conservation of bodily energy that helped make possible the conquest of more temperate regions.

But the most remarkable human innovation is the use of extrasomatic energy, wherein energy is made to accomplish human ends outside the bodies of its users. And the most important source of extrasomatic energy, by far, is fire. Fire was used by Homo erectus in northern China more than 400,000 years ago, and there is sketchy evidence suggesting that it may have been used long before that (Gowlett, 1984, pp. 181-82). Through the use of fire, meat did not have to be rent by main strength; it could be cooked until tender. Fire could be used to hollow out a log or harden the point of a stick. Fire could drive game from cover and smoke out bees. Fire could hold fierce animals at bay.

The exploitation of animal power played an important role in the densification of population that was at the root of what we call civilization. Animals pulled the plow, animals carried produce to market, and animals provided a protein-rich complement to a diet of grain. Wind power was soon utilized to carry cargo by water. But fire remained the most important source of extrasomatic energy, and it made possible the development of ceramics and metallurgy.

Until quite recently, however, there was no real innovation in the fuel used to make fire. For hundreds of thousands of years, fire was made with the tissues of recently deceased organisms-principally wood. The development of charcoal improved on the energy density of untreated wood, and made a substantial contribution to metallurgy. Then, just a few millennia later, the same oxygen-deprived roasting process was applied to coal. In England, coal had been used to heat living space since the Norman Conquest, but the development of coke and its suitability for steelmaking set off the Industrial Revolution. Within an evolutionary wink, petroleum and natural gas were also being exploited, and Homo sapiens had begun to dissipate the rich deposits of organic energy that had been accumulating since the beginning of life. If the slow accretion of these deposits in the face of universal entropy can be likened to the buildup of water behind a dam, then with the appearance of a species capable of dissipating that energy, the dam burst.

According to the American Heritage Dictionary, resources are "An available supply that can be drawn upon when needed" and "Means that can be used to advantage." In other words, resources include all the things found in nature that people use-not just the things people use for survival, but things they use for any purpose whatever. This is a very broad concept, as required by the nature of the defining animal. The resources used by other animals consist primarily of food, plus a few other materials such as those used for nest building. But for Homo sapiens, almost everything "can be used to advantage."

For something to be a resource, it must be concentrated or organized in a particular way, and separate, or separable, from its matrix. Ore from an iron mine is a resource in a way that garden soil is not-even though both do contain iron. Similarly, wood from the trunk of an oak tree is a resource in a way that wood from its twigs is not.

Usinga resource means dispersing it. When we quarry limestone and send it off to build public monuments, or when we mine coal and burn it to drive turbines, we are making use of a concentrated resource, and dispersing it. A large, continuous mass of limestone winds up as a number of discrete blocks spread around in different locations; and coal, after briefly giving off heat and light, becomes a small amount of ash and a large amount of gas. Resources may be temporarily accumulated in a stockpile, but their actual use always results in dispersal.

Resources may be used for their material properties or for the energy they contain. Bauxite is a material resource, while coal is an energy resource. Some resources may be used either way; wood, for example, may be used as a construction material or burned in a wood stove, and petroleum may be used to make plastics or to power cars.

The exploitation of all resources requires an investment in energy; it takes energy to knap flint or drill for oil. The exploitation of energy resources must entail a good return on investment; unless the energy they release is considerably more than the energy used to make them release it, they are not worth exploiting.

Since nothing is a resource unless it can be used, resources are defined by the technology that makes it possible to exploit them. Since exploiting a resource always requires energy, the evolution of technology has meant the application of energy to a growing array of substances so that they can be "used to advantage." In the brief time since humans began living in cities, they have used more and more energy to exploit more and more resources.

The cost of energy limited the growth of technology until fossil fuels came into use, a little less than three hundred years ago. Fossil fuels contain so much energy that they provide a remarkable return on investment even when used inefficiently. When coal is burned to drive dynamos, for example, only 35% of its energy ultimately becomes electricity (Ross & Steinmeyer, 1990, p. 89). Nevertheless, an amount of electricity equal to the energy used by a person who works all day, burning up 1,000 calories worth of food, can be bought for less than ten cents (Loftness, 1984, p. 2). 3

The abundant, cheap energy provided by fossil fuels has made it possible for humans to exploit a staggering variety of resources, effectively expanding their resource base. In particular, the development of mechanized agriculture has allowed relatively few farmers to work vast tracts of land, producing an abundance of food and making possible a wild growth of population.

All species expand as much as resources allow and predators, parasites, and physical conditions permit. When a species is introduced into a new habitat with abundant resources that accumulated before its arrival, the population expands rapidly until all the resources are used up. In wine making, for example, a population of yeast cells in freshly-pressed grape juice grows exponentially until nutrients are exhausted-or waste products become toxic (Figure 1).

Figure 1.  Growth of yeast in a 10% sugar solution (After Dieter, 1962:45).  The fall of the curve is slowed by cytolysis, which recycles nutrients from dead cells.

An example featuring mammals is provided by the reindeer of St. Matthew Island, in the Bering Sea (Klein, 1968). This island had a mat of lichens more than four inches deep, but no reindeer until 1944, when a herd of 29 was introduced. By 1957 the population had increased to 1,350; and by 1963 it was 6,000. But the lichens were gone, and the next winter the herd died off. Come spring, only 41 females and one apparently dysfunctional male were left alive (Figure 2). 4

Figure 2. Growth of reindeer herd introduced to St. Matthew Island, Alaska (After Klein, 1968:352).

The use of extrasomatic energy, and especially energy from fossil fuels, has made it possible for humans to exploit a wealth of resources that accumulated before they evolved. This has resulted in population growth typical of introduced species (Figure 3).

Figure 3. Growth of worldwide human population (Adapted from Corson, 1990:25).

Around 8,000 BC, world population was something like five million. By the time of Christ, it was 200 to 300 million. By 1650, it was 500 million, and by 1800 it was one billion. The population of the world reached two billion by 1930. By the beginning of the '60s it was three billion; in 1975 it was four billion; and after only eleven more years it was five billion (McEvedy & Jones, 1978; Ehrlich & Ehrlich, 1990, pp. 52-55). This cannot go on forever; collapse is inevitable. The only question is when.

Today, the extrasomatic energy used by people around the world is equal to the work of some 280 billion men. It is as if every man, woman, and child in the world had 50 slaves. In a technological society such as the United States, every person has more than 200 such "ghost slaves." 5

Figure 4. Worldwide energy consumption. Estimates of the world's annual consumption of energy, at twenty-year intervals beginning in 1860, appear in Dorf, 1981:194. World population for these years is calculated from a graph in Corson, 1990:25. Per-capita energy use for more recent years is given in the Energy Statistics Yearbook, which is published yearly by the United Nations. Figures differ somewhat from volume to volume; I have chosen to use more recent ones, which are presumably based on more accurate information.

Most of this energy comes from fossil fuels, which supply nearly 75% of the world's energy (see note 5). But fossil fuels are being depleted a hundred thousand times faster than they are being formed (Davis, 1990, P. 56). At current rates of consumption, known reserves of Petroleum will be gone in about thirty-five years; natural gas in fifty-two years; and coal in some two hundred years PRIMED, 1990, p. 145). 6

It should not be supposed that additional reserves, yet to be discovered, will significantly alter these figures. Recent advances in the geological sciences have taken much of the guesswork out of locating fossil hydrocarbons and the surface of the earth has been mapped in great detail with the aid of orbiting satellites. Moreover, these figures are optimistic because the demand for energy will not remain at current rates; it can be expected to grow at an ever-quickening pace. The more concentrated a resource, the less energy it takes to make use of it; and the less concentrated a resource, the more energy it takes. Consequently, the richest deposits of any resource are used first, and then lower-grade deposits are exploited, at an ever-increasing cost. As high-grade mineral ores are worked out, more and more energy is needed to mine and refine lower-grade ores. As oldgrowth timber vanishes, more and more energy is necessary to make lumber and paper out of smaller trees. As the world's fisheries are worked out, it takes more and more energy to find and catch the remaining fish. And as the world's topsoil is lost -- at a rate of 75 billion tons a year (Myers, 1993, p. 37) -- more and more energy must be used to compensate for the diminished fertility of remaining agricultural land.

The system that sustains world population is already under stress. The growth in per-capita energy use, which had been increasing continually since the advent of fossil fuels, began to slow down some twenty years ago -- and the accelerating pace at which it has been slowing down suggests that there will be no growth at all by the year 2000 (Figure 4). Agriculture is in trouble; it takes more and more fertilizer to compensate for lost topsoil (Ehrlich & Ehrlich, 1990, p. 92), and nearly one-fifth of the world's population is malnourished (Corson, 1990, p. 68). In fact, the growth rate of the earth's human population has already begun to fall (Figure 5).

Figure 5. Growth rate of world population.  Based on an average of estimates by Willcox (1940) and Carr-Saunders (1936) as adjusted and presented in United Nations, 1953:12; United Nations, 1993:6-7; and CIA, 1993:422.

People who believe that a stable population can live in balance with the productive capacity of the environment may see a slowdown in the growth of population and energy consumption as evidence of approaching equilibrium. But when one understands the process that has been responsible for population growth, it becomes clear that an end to growth is the beginning of collapse. Human population has grown exponentially by exhausting limited resources, like yeast in a vat or reindeer on St. Matthew Island, and is destined for a similar fate.

To take over for fossil fuels as they run out, an alternative energy source would have to be cheap and abundant, and the technology to exploit it would have to be mature and capable of being operationalized all over the world in what may turn out to be a rather short time. No known energy source meets these requirements.

Today's second-most-important source of energy, after fossil fuels, is biomass conversion. But all the world's wood fires, all the grain alcohol added to gasoline, and all the agricultural wastes burned as fuel only provide 15% of the world's energy (WRI/IIED, 1988, p. 111). And biomass conversion has little growth potential, since it competes for fertile land with food crops and timber.

Hydropower furnishes about 5.5% of the energy currently consumed (see note 5). Its potential may be as much as five times greater (Weinberg & Williams, 1990, p. 147), but this is not sufficient to take over from fossil fuels, and huge dams would submerge rich agricultural soils.

The production of electricity from nuclear fission has been increasing, but nuclear sources still supply only about 5.2% of the world's total energy needs (see note 5). Fission reactors could produce a great deal more, especially if fast-breeder reactors were used. 7 But anyone with a fast-breeder reactor can make nuclear weapons, so there is considerable political pressure to prevent their proliferation. Public confidence in all types of reactors is low, and the cost of their construction is high. These social constraints make it unlikely that fission's contribution to the world's energy needs will grow fifteen-fold in the next few years.

Controlled thermonuclear fusion is an alluring solution to the world's energy problems because the "fuel" it would use is deuterium, which can be extracted from plain water. The energy from one percent of the deuterium in the world's oceans would be about five hundred thousand times as great as all the energy available from fossil fuels. But controlled fusion is still experimental, the technology for its commercialization has not yet been developed, and the first operational facility could not come on line much before 2040 (Browne, 1993, p. C12).

Visionaries support the potential of wind, waves, tides, ocean thermal energy conversion, and geothermal sources. All of these might be able to furnish a portion of the energy in certain localities, but none can supply 75% of the world's energy needs. Solar thermal collection devices are only feasible where it is hot and sunny, and photovoltaics are too inefficient to supplant the cheap energy available from fossil fuels.

While no single energy source is ready to take the place of fossil fuels, their diminishing availability may be offset by a regimen of conservation and a combination of alternative energy sources. This will not solve the problem, however. As long as population continues to grow, conservation is futile; at the present rate of growth (1.6% per year), even a 25% reduction in resource use would be obliterated in just over eighteen years. And the use of any combination of resources that permits continued population growth can only postpone the day of reckoning.

Operative mechanisms in the collapse of the human population will be starvation, social strife, and disease. These major disasters were recognized long before Malthus and have been represented in western culture as horsemen of the apocalypse. 8 They are all consequences of scarce resources and dense population.

Starvation will be a direct outcome of the depletion of energy resources. Today's dense population is dependent for its food supply on mechanized agriculture and efficient transportation. Energy is used to manufacture and operate farm equipment, and energy is used to take food to market. As less efficient energy resources come to be used, food will grow more expensive and the circle of privileged consumers to whom an adequate supply is available will continue to shrink.

Social strife is another consequence of the rising cost of commercial energy. Everything people want takes energy to produce, and as energy becomes more expensive, fewer people have access to goods they desire. When goods are plentiful, and particularly when per-capita access to goods is increasing, social tensions are muted: Ethnically diverse populations often find it expedient to live harmoniously, governments may be ineffective and slow to respond, and little force is needed to maintain domestic tranquillity. But when goods become scarce, and especially when per-capita access to goods is decreasing, ethnic tensions surface, governments become authoritarian, and goods are acquired, increasingly, by criminal means.

A shortage of resources also cripples public health systems, while a dense population encourages the spread of contagious diseases. Throughout human history, the development of large, dense populations has led to the appearance of contagious diseases that evolved to exploit them. Smallpox and measles were apparently unknown until the second and third centuries AD, when they devastated the population of the Mediterranean basin (McNeill, 1976, p. 105). In the fourteenth century, a yet larger and denser population in both Europe and China provided a hospitable niche for the Black Death. Today, with extremely dense population and all parts of the world linked by air travel, new diseases such as AIDS spread rapidly-and a virus as deadly as AIDS but more easily transmissible could appear at any time.

Starvation, social strife, and disease interact in complex ways. If famine were the sole mechanism of collapse, the species might become extinct quite suddenly. A population that grows in response to abundant but finite resources, like the reindeer of St. Matthew Island, tends to exhaust these resources completely. By the time individuals discover that remaining resources will not be adequate for the next generation, the next generation has already been born. And in its struggle to survive, the last generation uses up every scrap, so that nothing remains that would sustain even a small population. But famine seldom acts alone. It is exacerbated by social strife, which interferes with the production and delivery of food. And it weakens the natural defenses by which organisms fight off disease.

Paradoxically, disease can act to spare resources. If, for example, a new epidemic should reduce the human population to a small number of people who happen to be resistant to it before all the world's resources are severely depleted, the species might be able to survive a while longer.

But even if a few people manage to survive worldwide population collapse, civilization will not. The complex association of cultural traits of which modern humans are so proud is a consequence of abundant resources, and cannot long outlive their depletion.

Civilization refers, in its derivation, to the habit of living in dense nucleated settlements, which appeared as population grew in response to plentiful resources. Many things seem to follow as a matter of course when people live in cities, and wherever civilization occurred, it has involved political consolidation, economic specialization, social stratification, some sort of monumental architecture, and a flowering of artistic and intellectual endeavor (Childe, 1951).

Localized episodes of such cultural elaboration have always been associated with rapid population growth. Reasons for the abundance of resources that promoted this growth vary from one case to another. In some instances, a population moved into a new region with previously untapped resources; in other instances the development or adoption of new crops, new technologies, or new social strategies enhanced production. But the Sumerians, the Greeks, the Romans, the Mayas, and even the Easter Islanders all experienced a surge of creative activity as their populations grew rapidly.

And in all cases, this creative phase, nourished by the same abundance that promoted population growth, came to an end when growth ended. One need not seek esoteric reasons for the decline of Greece or the fall of Rome; in both cases, the growth of population exhausted the resources that had promoted it. After the Golden Age, the population of Greece declined continually for more than a thousand years, from 3 million to about 800,000. The population of the Roman Empire fell from 45 or 46 million, at its height, to about 39 million by 600 AD, and the European part of the empire was reduced by 25% (McEvedy & Jones, 1978).

Even if world population could be held constant, in balance with "renewable" resources, the creative impulse that has been responsible for human achievements during the period of growth would come to an end. And the spiraling collapse that is far more likely will leave, at best, a handfull of survivors. These people might get by, for a while, by picking through the wreckage of civilization, but soon they would have to lead simpler lives, like the hunters and subsistence farmers of the past. They would not have the resources to build great public works or carry forward scientific inquiry. They could not let individuals remain unproductive as they wrote novels or composed symphonies. After a few generations, they might come to believe that the rubble amid which they live is the remains of cities built by gods.

Or it may prove impossible for even a few survivors to subsist on the meager resources left in civilization's wake. The children of the highly technological society into which more and more of the world's peoples are being drawn will not know how to support themselves by hunting and gathering or by simple agriculture. In addition, the wealth of wild animals that once sustained hunting societies will be gone, and topsoil that has been spoiled by tractors will yield poorly to the hoe. A species that has come to depend on complex technologies to mediate its relationship with the environment may not long survive their loss.

For Malthus, the imbalance between the growth of population and means of subsistence might be corrected, from time to time, through natural disasters, but the human species could, in principle, survive indefinitely. Malthus did not know that the universe is governed by the Second Law of Thermodynamics; he did not understand the population dynamics of introduced species; and he did not appreciate that humans, having evolved long after the resource base on which they now rely, are effectively an introduced species on their own planet.

The short tenure of the human species marks a turning point in the history of life on Earth. Before the appearance of Homo sapiens, energy was being sequestered more rapidly than it was being dissipated. Then human beings evolved, with the capacity to dissipate much of the energy that had been sequestered, partially redressing the planet's energy balance. The evolution of a species like Homo sapiens may be an integral part of the life process, anywhere in the universe it happens to occur. As life develops, autotrophs expand and make a place for heterotrophs. If organic energy is sequestered in substantial reserves, as geological processes are bound to do, then the appearance of a species that can release it is all but assured. Such a species, evolved in the service of entropy, quickly returns its planet to a lower energy level. In an evolutionary instant, it explodes and is gone.

If the passage of Homo sapiens across evolution's stage significantly alters Earth's atmosphere, virtually all living things may become extinct quite rapidly. But even if this does not happen, the rise and fall of Homo sapiens will eliminate many species. It has been estimated that they are going extinct at a rate of 17,500 per year (Wilson, 1988, p. 13), and in the next twenty-five years as many as one-quarter of the world's species may be lost (Raven, 1988, p. 121).

This is a radical reduction in biological diversity, although life has survived other die-offs, such as the great collapse at the end of the Permian. It is unlikely, however, that anything quite like human beings will come this way again. The resources that have made humans what they are will be gone, and there may not be time before the sun burns out for new deposits of fossil fuel to form and intelligent new scavengers to evolve. The universe seems to have had a unique beginning, some ten or twenty billion years ago (Hawking, 1988, p. 108). Since that time, a star had to live and die to provide the materials for the solar system -- which, itself, is several billion years old. Perhaps life could not have happened any sooner than it did. Perhaps Homo sapiens could not have evolved any sooner. Or later. Perhaps everything has its season, a window of opportunity that opens for a while, then shuts.

I want to acknowledge the advice and encouragement of Virginia Abernethy, Thomas Eisner, Paul W. Friedrich, Warren M. Hern, David Pimentel, Roy A. Rappaport, Peter H. Raven, and Carl Sagan, who read earlier drafts of this paper.

NOTES

1. In the 1798 version of his essay, Malthus said that population grows geometrically while subsistence grows arithmetically. in later editions, he said that arithmetical growth was the most optimistic possible hypothesis; he was well aware that the availability of fertile soils must actually be diminishing.

2. The distinction between "nonrenewable" and "renewable" is arbitrary. Petroleum is considered nonrenewable, because when it's used, it's gone; while sunlight is considered renewable, because its energy can be used today and the sun will shine again tomorrow.

But given enough time, today's forests could become tomorrow's petroleum, and given an astronomical sweep of time, the sun itself will burn out. Only in terms of human time is an energy resource renewable or nonrenewable; and it is not even clear how human time should be measured. Wood is often considered a renewable resource, because if one tree is chopped down, another will grow in its place. But if a tree is taken off the mountainside rather than allowed to rot where it falls, nutrients that would nourish its successor are removed. If wood is continually removed, the fertility of the forest diminishes, and within a few human generations the forest will be gone.

3. Loftness actually says six cents. I have changed the figure to ten cents as a rough correction for inflation.

4. When the resources exploited by an introduced species are living organisms, they can reproduce -- and they may eventually evolve defense mechanisms that promote an equilibrium between predator and prey (see Pimentel, 1988). The topsoil, minerals, and fossil fuels exploited by human beings do not have this capacity, however. They are more like the finite amount of sugar in a vat or the plentiful but slow-growing lichens on St. Matthew Island.

5. Worldwide production of energy from fossil fuels in 1992 was 302.81 x 1015 Btu, while energy from nuclear reactors was 21.23 x 1015 Btu and from hydroelectric sources was 22.29 x 1015 Btu (Energy Information Administration, 1993:269). Biomass is thought to account for about 15% of the world's extrasomatic energy (WRI/IIED, 1988:111). Other sources of energy make only a minor contribution (Corson, 1990:197). Thus, the total extrasomatic energy used in the world must be on the order of 407.45 x 1015 Btu per year. World population is taken as 5.555 billion (CIA, 1993:422). The energy expended by an individual in doing a hard day's work is taken to be 4,000 Btu (Loftness 1984:2, 756). Energy consumption in the United States is on the order of 82.36 X 1015 Btu (Energy Information Administration, 1993:5). U.S. population is taken as 258 million (CIA, 1993:404).

6. These are reserves known in 1988, depleted at 1988 rates. I have subtracted six years from the figures cited to account for time that has already elapsed.

7. Loftness (1984:48) says the same amount of uranium, used in a fast-breeder reactor, will provide 60 times as much energy as in a light-water reactor. Hafele (1990:142) says one hundred times as much.

8. According to a traditional interpretation, the four horses stand for war, famine pestilence, and the returned Christ. The original text (Revelations 6:2-8) is not so clear.

REFERENCES

Binford, Lewis R. (1981). Bones: Ancient men and modern myths. New York: Academic Press,

Brain, C. K. (1981). The hunters or the hunted? An introduction to African cave taphonomy. Chicago: The University of Chicago Press.

Browne, Malcolm W. (1993). Reactor passes point of no return in uphill path to fusion energy. New York Times, Dec. 7, 1993, pp. C1 & C12.

Central intelligence Agency (CIA). (1993). The World Factbook 1993. Washington, DC: Central Intelligence Agency.

Childe, V. Gordon. (1951). Social evolution. London: Watts.

Corson, Walter H., (Ed.). (1990). The global ecology handbook: What you can do about the environmental crisis. Boston: Beacon Press.

Davis, Ged R. (1990). Energy for planet earth. Scientific American 263(3), 55-62.

Dieter, Georg. (1962). Biologische Strukturen und ihre Ver5nderungen in Raum und Zeit, dargestellt an der Kinetik von Vermehrung, Sterben und Zytolyse bei Saccharomyces cerevisiae. Dissertation zur Erlangung des Doktorgrades bei der Landwirtschaftlichen Fakultat der Justus Leibig-Universitat. Fotodruck: Mikrokopie G.m.b.H. Monchen 2, Weinstr. 4.

Dorf, Richard C. (1981). The energy fact book. New York: McGraw-Hill,

Energy Information Administration. (1993). Annual energy review 1992. Report no. DOE/ EIA-0384(92). Washington, DC: U.S. Department of Energy.

Ehrlich, Paul R., & Ehrlich, Anne H. (1990). The Population explosion. New York: Simon and Schuster.

Gowlett, John A. 1. (1984). Mental abilities of early man: A look at some hard evidence. in R. Foley (Ed.). Hominid evolution and community ecology, pp. 167-92. London: Academic Press.

Hafele, Wolf. (1990). Energy from nuclear power. Scientific American 263(3), 137-44,

Hawking, Stephen. (1988). A brief history of time: From the Big Bang to black holes. New York: Bantam,

Klein, David R. (1968). The introduction, increase, and crash of reindeer on St. Matthew Island. Journal of Wildlife Management 32(2), 350-67.

Loftness, Robert L. (1984). Energy handbook, 2nd ed. New York: Van Nostrand Reinhold.

Malthus, Thomas Robert. (1986 [1826]). An essay on the principle of population. The Works of Thomas Robert Malthus, Ed. E. A. Wrigley and D. Souden, vol. 2 and 3. London: William Pickering.

McEvedy, Colin, & Jones, Richard (1978). Atlas of world population history. New York: Penguin.

McNeill, William H. (1 976). Plagues and peoples. Garden City, NY: Anchor Press.

Myers, Norman (Ed.). (1993). Gaia: An atlas of planet management, rev. ed. Garden City, NY: Anchor/Doubleday.

Odum, Eugene P. (1971). Fundamentals of ecology. 3rd ed. Philadelphia: W. B. Saunders Company.

Pimentel, D. (1988). Herbivore population feeding pressure on plant hosts: Feedback evolution and host conservation. Oikos 53(3), 289-302.

Raven, Peter H. (1988). Our diminishing tropical forests. 1988. In E. 0. Wilson (Ed.). Biodiversity, pp. 119-21. Washington: National Academy Press.

Ricklefs, Robert E. (1979). Ecology. 2nd ed. New York: Chiron Press.

Ross, Marc H., & Steinmeyer, Daniel (1990). Energy for industry. Scientific American 263(3), 89-98.

Simpson, George Gaylord. (1949). The meaning of evolution. New Haven, CT: Yale University Press.

Starr, Cecie, & Taggart, Ralph (1987). Biology: The unity and diversity of life, 4th ed. Belmont, CA: Wadsworth.

United Nations. (1952-91). Energy statistics yearbook, New York: United Nations (E/F.93.XVII.5).

_. (1953). The determinants and consequences of population trends. New York: United Nations (5T/SOA/Ser.A/I 7).

_. (1993). World population prospects: The 1992 revision. New York: United Nations (ST/ESA/SER.A/135).

Weinberg, Carl J., & Williams, Robert H.. (1990). Energy from the sun. Scientific American 263(3), 147-55.

White, Leslie A.. (1949). The science of culture: A study of man and civilization. New York: Farrar, Strauss and Giroux.

Wilson, E. O. (1988). The current state of biological diversity. In E. O. Wilson (Ed.). Biodiversity, pp. 3-18. Washington, DC: National Academy Press.

World Resources Institute and International Institute for Environment and Development (WRI/IIED). (1988). World Resources 1988-89. New York: Basic Books.

_. (1990). World Resources 1990-91. New York: Oxford University Press.


Further information: Outline of energy development

Energy development

World total primary energy production

  Total world primary energy production (quadrillionBtu)[2]

   China

   Russia

   Africa

   United States

   Europe

   Central and South America

Note the different y-axis for total (left) and regional curves (right)

US Energy Use/Flow in 2011

Energy flow charts show the relative size of primary energy resources and end uses in the United States, with fuels compared on a common energy unit basis (2011: 97.3 quads).[3]

Compounds and Radiant Energy

   Solar

   Nuclear

   Hydro

   Wind

   Geothermal

   Natural gas

   Coal

   Biomass

   Petroleum

Producing Electrical Currents/Utilizing Effects Transmitted

   Electricity generation

   Residential, Commercial, Industrial, transportation

   Rejected energy (waste heat)

   Energy services

Energy development is the field of activities focused on obtaining sources of energy from natural resources. These activities include production of conventional, alternative and renewable sources of energy, and for the recovery and reuse of energy that would otherwise be wasted. Energy conservation and efficiency measures reduce the demand for energy development, and can have benefits to society with improvements to environmental issues.

Societies use energy for transportation, manufacturing, illumination, heating and air conditioning, and communication, for industrial, commercial, and domestic purposes. Energy resources may be classified as primary resources, where the resource can be used in substantially its original form, or as secondary resources, where the energy source must be converted into a more conveniently usable form. Non-renewable resources are significantly depleted by human use, whereas renewable resources are produced by ongoing processes that can sustain indefinite human exploitation.

Thousands of people are employed in the energy industry. The conventional industry comprises the petroleum industry, the natural gas industry, the electrical power industry, and the nuclear industry. New energy industries include the renewable energy industry, comprising alternative and sustainable manufacture, distribution, and sale of alternative fuels.

Classification of resources[edit]

Further information: World energy resources and consumption

See also: Worldwide energy supply, Energy and society, Energy planning, and Energy policy

Energy resources may be classified as primary resources, suitable for end use without conversion to another form, or secondary resources, where the usable form of energy required substantial conversion from a primary source. Examples of primary energy resources are wind power, solar power, wood fuel, fossil fuels such as coal, oil and natural gas, and uranium. Secondary resources are those such as electricity, hydrogen, or other synthetic fuels.

Another important classification is based on the time required to regenerate an energy resource. "Renewable" resources are those that recover their capacity in a time significant by human needs. Examples are hydroelectric power or wind power, when the natural phenomena that are the primary source of energy are ongoing and not depleted by human demands. Non-renewable resources are those that are significantly depleted by human usage and that will not recover their potential significantly during human lifetimes. An example of a non-renewable energy source is coal, which does not form naturally at a rate that would support human use.

Fossil fuels[edit]

Main articles: Fossil fuel and Peak oil

Fossil fuel (primary non-renewable fossil) sources burn coal or hydrocarbon fuels, which are the remains of the decomposition of plants and animals. There are three main types of fossil fuels: coal, petroleum, and natural gas. Another fossil fuel, liquefied petroleum gas (LPG), is principally derived from the production of natural gas. Heat from burning fossil fuel is used either directly for space heating and process heating, or converted to mechanical energy for vehicles, industrial processes, or electrical power generation. These fossil fuels are part of the carbon cycle and thus allow stored solar energy to be used today.

The use of fossil fuels in the 18th and 19th Century set the stage for the Industrial Revolution.

Fossil fuels make up the bulk of the world's current primary energy sources. In 2005, 81% of the world's energy needs was met from fossil sources.[4] The technology and infrastructure already exist for the use of fossil fuels. Liquid fuels derived from petroleum deliver a great deal of usable energy per unit of weight or volume, which is advantageous when compared with lower energy density sources such as a battery. Fossil fuels are currently economical for decentralised energy use.

Energy dependence on imported fossil fuels creates energy security risks for dependent countries.[5][6][7][8][9] Oil dependence in particular has led to war,[10] funding of radicals,[11] monopolization,[12] and socio-political instability.[13]

Fossil fuels are non-renewable resources, which will eventually decline in production [14] and become exhausted. While the processes that created fossil fuels are ongoing, fuels are consumed far more quickly than the natural rate of replenishment. Extracting fuels becomes increasingly costly as society consumes the most accessible fuel deposits.[15] Extraction of fossil fuels results in environmental degradation, such as the strip mining and mountaintop removal of coal.

Fuel efficiency is a form of thermal efficiency, meaning the efficiency of a process that converts chemical potential energy contained in a carrier fuel into kinetic energy or work. The fuel economy is the energy efficiency of a particular vehicle, is given as a ratio of distance travelled per unit of fuel consumed. Weight-specific efficiency (efficiency per unit weight) may be stated for freight, and passenger-specific efficiency (vehicle efficiency per passenger). The inefficient atmospheric combustion (burning) of fossil fuels in vehicles, buildings, and power plants contributes to urban heat islands.[16]

Conventional production of oil has peaked, conservatively, between 2007 and 2010. In 2010, it was estimated that an investment in non-renewable resources of $8 trillion would be required to maintain current levels of production for 25 years.[17] In 2010, governments subsidized fossil fuels by an estimated $500 billion a year.[18] Fossil fuels are also a source of greenhouse gas emissions, leading to concerns about global warming if consumption is not reduced.

The combustion of fossil fuels leads to the release of pollution into the atmosphere. The fossil fuels are mainly carbon compounds. During combustion, carbon dioxide is released, and also nitrogen oxides, soot and other fine particulates. Man-made carbon dioxide according to the IPCC contributes to global warming.[19] Other emissions from fossil fuel power station include sulfur dioxide, carbon monoxide (CO), hydrocarbons, volatile organic compounds (VOC), mercury, arsenic, lead, cadmium, and other heavy metals including traces of uranium.[20][21]

A typical coal plant generates billions of kilowatt hours per year.[22]

Nuclear[edit]

Fission[edit]

Nuclear power is the use of nuclear fission to generate useful heat and electricity. Fission of uranium produces nearly all economically significant nuclear power. Radioisotope thermoelectric generators form a very small component of energy generation, mostly in specialized applications such as deep space vehicles.

Nuclear power plants, excluding naval reactors, provided about 5.7% of the world's energy and 13% of the world's electricity in 2012.[23]

In 2013, the IAEA report that there are 437 operational nuclear power reactors,[24] in 31 countries,[25] although not every reactor is producing electricity.[26] In addition, there are approximately 140 naval vessels using nuclear propulsion in operation, powered by some 180 reactors.[27][28][29] As of 2013, attaining a net energy gain from sustained nuclear fusion reactions, excluding natural fusion power sources such as the Sun, remains an ongoing area of international physics and engineering research. More than 60 years after the first attempts, commercial fusion power production remains unlikely before 2050.[30]

There is an ongoing debate about nuclear power.[31][32][33] Proponents, such as the World Nuclear Association, the IAEA and Environmentalists for Nuclear Energy contend that nuclear power is a safe, sustainable energy source that reduces carbon emissions.[34]Opponents, such as Greenpeace International and NIRS, contend that nuclear power poses many threats to people and the environment.[35][36][37]

Nuclear power plant accidents include the Chernobyl disaster (1986), Fukushima Daiichi nuclear disaster (2011), and the Three Mile Island accident (1979). There have also been some nuclear submarine accidents.[39][40] In terms of lives lost per unit of energy generated, analysis has determined that nuclear power has caused less fatalities per unit of energy generated than the other major sources of energy generation. Energy production from coal, petroleum, natural gas and hydropower has caused a greater number of fatalities per unit of energy generated due to air pollution and energy accident effects.[41][42][43][44][45] However, the economic costs of nuclear power accidents is high, and meltdowns can take decades to clean up. The human costs of evacuations of affected populations and lost livelihoods is also significant.[46][47]

Comparing Nuclear's latent cancer deaths, such as cancer with other energy sources immediate deaths per unit of energy generated(GWeyr). This study does not include fossil fuel related cancer and other indirect deaths created by the use of fossil fuel consumption in its "severe accident" classification, which would be an accident with more than 5 fatalities.

Nuclear power is a low carbon power generation method of producing electricity, with an analysis of the literature on its total life cycleemission intensity finding that it is similar to renewable sources in a comparison of greenhouse gas(GHG) emissions per unit of energy generated.[48] Since the 1970s, nuclear fuel has displaced about 64 gigatonnes of carbon dioxide equivalent(GtCO2-eq) greenhouse gases, that would have otherwise resulted from the burning of oil, coal or natural gas in fossil-fuel power stations.[49]

As of 2012, according to the IAEA, worldwide there were 68 civil nuclear power reactors under construction in 15 countries,[24] approximately 28 of which in the Peoples Republic of China (PRC), with the most recent nuclear power reactor, as of May 2013, to be connected to the electrical grid, occurring on February 17, 2013 in Hongyanhe Nuclear Power Plant in the PRC.[50] In the United States, two new Generation III reactors are under construction at Vogtle. U.S. nuclear industry officials expect five new reactors to enter service by 2020, all at existing plants.[51] In 2013, four aging, uncompetitive, reactors were permanently closed.[52][53]

Japan's 2011 Fukushima Daiichi nuclear accident, which occurred in a reactor design from the 1960s, prompted a rethink of nuclear safety and nuclear energy policy in many countries.[54] Germany decided to close all its reactors by 2022, and Italy has banned nuclear power.[54] Following Fukushima, in 2011 the International Energy Agency halved its estimate of additional nuclear generating capacity to be built by 2035.[55][56]

Recent experiments in extraction of uranium use polymer ropes that are coated with a substance that selectively absorbs uranium from seawater. This process could make the considerable volume of uranium dissolved in seawater exploitable for energy production. Since ongoing geologic processes carry uranium to the sea in amounts comparable to the amount that would be extracted by this process, in a sense the sea-borne uranium becomes a sustainable resource.[57][58]

Fission economics[edit]

Main article: Economics of new nuclear power plants

The economics of new nuclear power plants is a controversial subject, since there are diverging views on this topic, and multibillion-dollar investments ride on the choice of an energy source. Nuclear power plants typically have high capital costs for building the plant, but low direct fuel costs.

In recent years there has been a slowdown of electricity demand growth and financing has become more difficult, which affects large projects such as nuclear reactors, with very large upfront costs and long project cycles which carry a large variety of risks.[61] In Eastern Europe, a number of long-established projects are struggling to find finance, notably Belene in Bulgaria and the additional reactors at Cernavoda in Romania, and some potential backers have pulled out.[61] Where cheap gas is available and its future supply relatively secure, this also poses a major problem for nuclear projects.[61]

Analysis of the economics of nuclear power must take into account who bears the risks of future uncertainties. To date all operating nuclear power plants were developed by state-owned or regulatedutility monopolies[63][64] where many of the risks associated with construction costs, operating performance, fuel price, and other factors were borne by consumers rather than suppliers. Many countries have now liberalized the electricity market where these risks, and the risk of cheaper competitors emerging before capital costs are recovered, are borne by plant suppliers and operators rather than consumers, which leads to a significantly different evaluation of the economics of new nuclear power plants.[65]

Two of the four EPRs under construction (in Finland and France) are significantly behind schedule and substantially over cost.[66] Following the 2011 Fukushima Daiichi nuclear disaster, costs are likely to go up for currently operating and new nuclear power plants, due to increased requirements for on-site spent fuel management and elevated design basis threats.[67] While first of their kind designs, such as the EPRs under construction are behind schedule and over-budget, of the seven South Korean APR-1400s presently under construction worldwide, two are in S.Korea at the Hanul Nuclear Power Plant and four are at the largest nuclear station construction project in the world as of 2016, in the United Arab Emirates at the planned Barakah nuclear power plant. The first reactor, Barakah-1 is 85% completed and on schedule for grid-connection during 2017.[68][69]

Renewable sources[edit]

Main article: Renewable energy commercialization

Renewable energy is generally defined as energy that comes from resources which are naturally replenished on a human timescale such as sunlight, wind, rain, tides, waves and geothermal heat.[70] Renewable energy replaces conventional fuels in four distinct areas: electricity generation, hot water/space heating, motor fuels, and rural (off-grid) energy services.[71]

About 16% of global final energy consumption presently comes from renewable resources, with 10% [72] of all energy from traditional biomass, mainly used for heating, and 3.4% from hydroelectricity. New renewables (small hydro, modern biomass, wind, solar, geothermal, and biofuels) account for another 3% and are growing rapidly.[73] At the national level, at least 30 nations around the world already have renewable energy contributing more than 20% of energy supply. National renewable energy markets are projected to continue to grow strongly in the coming decade and beyond.[74]Wind power, for example, is growing at the rate of 30% annually, with a worldwide installed capacity of 282,482 megawatts (MW) at the end of 2012.

Renewable energy resources exist over wide geographical areas, in contrast to other energy sources, which are concentrated in a limited number of countries. Rapid deployment of renewable energy and energy efficiency is resulting in significant energy security, climate change mitigation, and economic benefits.[75] In international public opinion surveys there is strong support for promoting renewable sources such as solar power and wind power.[76]

While many renewable energy projects are large-scale, renewable technologies are also suited to rural and remote areas and developing countries, where energy is often crucial in human development.[77]United Nations' Secretary-General Ban Ki-moon has said that renewable energy has the ability to lift the poorest nations to new levels of prosperity.[78]

Hydroelectricity[edit]

Hydroelectricity is electric power generated by hydropower; the force of falling or flowing water. In 2015 hydropower generated 16.6% of the world's total electricity and 70% of all renewable electricity [79][page needed] and is expected to increase about 3.1% each year for the next 25 years.

Hydropower is produced in 150 countries, with the Asia-Pacific region generating 32 percent of global hydropower in 2010. China is the largest hydroelectricity producer, with 721 terawatt-hours of production in 2010, representing around 17 percent of domestic electricity use. There are now three hydroelectricity plants larger than 10 GW: the Three Gorges Dam in China, Itaipu Dam across the Brazil/Paraguay border, and Guri Dam in Venezuela.[80]

The cost of hydroelectricity is relatively low, making it a competitive source of renewable electricity. The average cost of electricity from a hydro plant larger than 10 megawatts is 3 to 5 U.S. cents per kilowatt-hour.[80] Hydro is also a flexible source of electricity since plants can be ramped up and down very quickly to adapt to changing energy demands. However, damming interrupts the flow of rivers and can harm local ecosystems, and building large dams and reservoirs often involves displacing people and wildlife.[80] Once a hydroelectric complex is constructed, the project produces no direct waste, and has a considerably lower output level of the greenhouse gascarbon dioxide than fossil fuel powered energy plants.[81]

Wind[edit]

Wind power harnesses the power of the wind to propel the blades of wind turbines. These turbines cause the rotation of magnets, which creates electricity. Wind towers are usually built together on wind farms. There are offshore and onshore wind farms. Global wind power capacity has expanded rapidly to 336 GW in June 2014, and wind energy production was around 4% of total worldwide electricity usage, and growing rapidly.[82]

Wind power is widely used in Europe, Asia, and the United States.[83] Several countries have achieved relatively high levels of wind power penetration, such as 21% of stationary electricity production in Denmark,[84] 18% in Portugal,[84] 16% in Spain,[84] 14% in Ireland,[85] and 9% in Germany in 2010.[84][86]:11 By 2011, at times over 50% of electricity in Germany and Spain came from wind and solar power.[87][88] As of 2011, 83 countries around the world are using wind power on a commercial basis.[86]:11

Many of the world's largest onshore wind farms are located in the United States, China, and India. Most of the world's largest offshore wind farms are located in Denmark, Germany and the United Kingdom. The two largest offshore wind farm are currently the 630 MWLondon Array and Gwynt y Môr.

Solar[edit]

Main articles: Solar PV systems and Concentrated solar power

Solar energy, radiant light and heat from the sun, is harnessed using a range of ever-evolving technologies such as solar heating, solar photovoltaics, solar thermal electricity, solar architecture and artificial photosynthesis.[96][97]

Solar technologies are broadly characterized as either passive solar or active solar depending on the way they capture, convert and distribute solar energy. Active solar techniques include the use of photovoltaic panels and solar thermal collectors to harness the energy. Passive solar techniques include orienting a building to the Sun, selecting materials with favorable thermal mass or light dispersing properties, and designing spaces that naturally circulate air.

In 2011, the International Energy Agency said that "the development of affordable, inexhaustible and clean solar energy technologies will have huge longer-term benefits. It will increase countries’ energy security through reliance on an indigenous, inexhaustible and mostly import-independent resource, enhance sustainability, reduce pollution, lower the costs of mitigating climate change, and keep fossil fuel prices lower than otherwise. These advantages are global. Hence the additional costs of the incentives for early deployment should be considered learning investments; they must be wisely spent and need to be widely shared".[96] More than 100 countries use solar PV.

Photovoltaics (PV) is a method of generating electrical power by converting solar radiation into direct currentelectricity using semiconductors that exhibit the photovoltaic effect. Photovoltaic power generation employs solar panels composed of a number of solar cells containing a photovoltaic material. Materials presently used for photovoltaics include monocrystalline silicon, polycrystalline silicon, amorphous silicon, cadmium telluride, and copper indium gallium selenide/sulfide. Due to the increased demand for renewable energy sources, the manufacturing of solar cells and photovoltaic arrays has advanced considerably in recent years.

Solar photovoltaics is a sustainable energy source.[98] By the end of 2011, a total of 71.1 GW[99] had been installed, sufficient to generate 85 TWh/year.[100] And by end of 2012, the 100 GW installed capacity milestone was achieved.[101] Solar photovoltaics is now, after hydro and wind power, the third most important renewable energy source in terms of globally installed capacity. In 2016, after another year of rapid growth, solar generated 1.3% of global power.[102]

Driven by advances in technology and increases in manufacturing scale and sophistication, the cost of photovoltaics has declined steadily since the first solar cells were manufactured,[103] and the levelised cost of electricity (LCOE) from PV is competitive with conventional electricity sources in an expanding list of geographic regions. Net metering and financial incentives, such as preferential feed-in tariffs for solar-generated electricity, have supported solar PV installations in many countries.[104] The Energy Payback Time (EPBT), also known as energy amortization, depends on the location's annual solar insolation and temperature profile, as well as on the used type of PV-technology. For conventional crystalline silicon photovoltaics, the EPBT is higher than for thin-film technologies such as CdTe-PV or CPV-systems. Moreover, the payback time decreased in the recent years due to a number of improvements such as solar cell efficiency and more economic manufacturing processes. As of 2014, photovoltaics recoup on average the energy needed to manufacture them in 0.7 to 2 years. This results in about 95% of net-clean energy produced by a solar rooftop PV system over a 30-year life-time.[105]:30 Installations may be ground-mounted (and sometimes integrated with farming and grazing) or built into the roof or walls of a building (either building-integrated photovoltaics or simply rooftop).

Biofuels[edit]

Main articles: Biofuel and Sustainable biofuel

A biofuel is a fuel that contains energy from geologically recent carbon fixation. These fuels are produced from living organisms. Examples of this carbon fixation occur in plants and microalgae. These fuels are made by a biomass conversion (biomass refers to recently living organisms, most often referring to plants or plant-derived materials). This biomass can be converted to convenient energy containing substances in three different ways: thermal conversion, chemical conversion, and biochemical conversion. This biomass conversion can result in fuel in solid, liquid, or gas

Open System Model (basics)
Two months after the Fukushima I failures, a global public support survey by Ipsos (2011) for energy sources was published and nuclear/fission was found to be the least popular[62]

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