Nuclear fission
Nuclear fission
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Induced fission reaction. A neutron is absorbed by a uranium-235 nucleus, turning it briefly into an excited uranium-236 nucleus, with the excitation energy provided by the kinetic energy of the neutron plus the forces that bind the neutron. The uranium-236, in turn, splits into fast-moving lighter elements (fission products) and releases several free neutrons, one or more "prompt gamma rays" (not shown) and a (proportionally) large amount of kinetic energy.

Nuclear fission is a reaction in which the nucleus of an atom splits into two or more smaller nuclei. The fission process often produces gamma photons, and releases a very large amount of energy even by the energetic standards of radioactive decay.

Nuclear fission was discovered by chemists Otto Hahn and Fritz Strassmann and physicists Lise Meitner and Otto Robert Frisch. Hahn and Strassmann proved that a fission reaction had taken place on 19 December 1938, and Meitner and her nephew Frisch explained it theoretically in January 1939. Frisch named the process "fission" by analogy with biological fission of living cells. In their second publication on nuclear fission in February 1939, Hahn and Strassmann predicted the existence and liberation of additional neutrons during the fission process, opening up the possibility of a nuclear chain reaction.

For heavy nuclides, it is an exothermic reaction which can release large amounts of energy both as electromagnetic radiation and as kinetic energy of the fragments (heating the bulk material where fission takes place). Like nuclear fusion, for fission to produce energy, the total binding energy of the resulting elements must be greater than that of the starting element. The fission barrier must also be overcome. Fissionable nuclides primarily split in interactions with fast neutrons, while fissile nuclides easily split in interactions with "slow" i.e. thermal neutrons, usually originating from moderation of fast neutrons.

Fission is a form of nuclear transmutation because the resulting fragments (or daughter atoms) are not the same element as the original parent atom. The two (or more) nuclei produced are most often of comparable but slightly different sizes, typically with a mass ratio of products of about 3 to 2, for common fissile isotopes.[1][2] Most fissions are binary fissions (producing two charged fragments), but occasionally (2 to 4 times per 1000 events), three positively charged fragments are produced, in a ternary fission. The smallest of these fragments in ternary processes ranges in size from a proton to an argon nucleus.

Apart from fission induced by an exogenous neutron, harnessed and exploited by humans, a natural form of spontaneous radioactive decay (not requiring an exogenous neutron, because the nucleus already has an overabundance of neutrons) is also referred to as fission, and occurs especially in very high-mass-number isotopes. Spontaneous fission was discovered in 1940 by Flyorov, Petrzhak, and Kurchatov[3] in Moscow. In contrast to nuclear fusion, which drives the formation of stars and their development, one can consider nuclear fission as negligible for the evolution of the universe. Nonetheless, natural nuclear fission reactors may form under very rare conditions. Accordingly, all elements (with a few exceptions, see "spontaneous fission") which are important for the formation of solar systems, planets and also for all forms of life are not fission products, but rather the results of fusion processes.

The unpredictable composition of the products (which vary in a broad probabilistic and somewhat chaotic manner) distinguishes fission from purely quantum tunneling processes such as proton emission, alpha decay, and cluster decay, which give the same products each time. Nuclear fission produces energy for nuclear power and drives the explosion of nuclear weapons. Both uses are possible because certain substances called nuclear fuels undergo fission when struck by fission neutrons, and in turn emit neutrons when they break apart. This makes a self-sustaining nuclear chain reaction possible, releasing energy at a controlled rate in a nuclear reactor or at a very rapid, uncontrolled rate in a nuclear weapon.

The amount of free energy released in the fission of an equivalent amount of 235
U
is a million times more than that released in the combustion of methane or from hydrogen fuel cells.[4]

The products of nuclear fission, however, are on average far more radioactive than the heavy elements which are normally fissioned as fuel, and remain so for significant amounts of time, giving rise to a nuclear waste problem. However, the seven long-lived fission products make up only a small fraction of fission products. Neutron absorption which does not lead to fission produces plutonium (from 238
U
) and minor actinides (from both 235
U
and 238
U
) whose radiotoxicity is far higher than that of the long lived fission products. Concerns over nuclear waste accumulation and the destructive potential of nuclear weapons are a counterbalance to the peaceful desire to use fission as an energy source. The thorium fuel cycle produces virtually no plutonium and much less minor actinides, but 232
U
- or rather its decay products - are a major gamma ray emitter. All actinides are fertile or fissile and fast breeder reactors can fission them all albeit only in certain configurations. Nuclear reprocessing aims to recover usable material from spent nuclear fuel to both enable uranium (and thorium) supplies to last longer and to reduce the amount of "waste". The industry term for a process that fissions all or nearly all actinides is a "closed fuel cycle".

Physical overview

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Mechanism

[edit]

Younes and Loveland define fission as, "...a collective motion of the protons and neutrons that make up the nucleus, and as such it is distinguishable from other phenomena that break up the nucleus. Nuclear fission is an extreme example of large-amplitude collective motion that results in the division of a parent nucleus into two or more fragment nuclei. The fission process can occur spontaneously, or it can be induced by an incident particle." The energy from a fission reaction is produced by its fission products, though a large majority of it, about 85 percent, is found in fragment kinetic energy, while about 6 percent each comes from initial neutrons and gamma rays and those emitted after beta decay, plus about 3 percent from neutrinos as the product of such decay.[4]: 21–22, 30 

A visual representation of an induced nuclear fission event where a slow-moving neutron is absorbed by the nucleus of a uranium-235 atom, which fissions into two fast-moving lighter elements (fission products) and additional neutrons. Most of the energy released is in the form of the kinetic velocities of the fission products and the neutrons.
Fission product yields by mass for thermal neutron fission of uranium-235, plutonium-239, a combination of the two typical of current nuclear power reactors, and uranium-233, used in the thorium cycle

Radioactive decay

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Nuclear fission can occur without neutron bombardment as a type of radioactive decay. This type of fission is called spontaneous fission, and was first observed in 1940.[4]: 22 

Nuclear reaction

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During induced fission, a compound system is formed after an incident particle fuses with a target. The resultant excitation energy may be sufficient to emit neutrons, or gamma-rays, and nuclear scission. Fission into two fragments is called binary fission, and is the most common nuclear reaction. Occurring least frequently is ternary fission, in which a third particle is emitted. This third particle is commonly an α particle.[4]: 21–24  Since in nuclear fission, the nucleus emits more neutrons than the one it absorbs, a chain reaction is possible.[5]: 291, 296 

Binary fission may produce any of the fission products, at 95±15 and 135±15 daltons. One example of a binary fission event in the most commonly used fissile nuclide, 235
U
, is given as:

However, the binary process happens merely because it is the most probable. In anywhere from two to four fissions per 1000 in a nuclear reactor, ternary fission can produce three positively charged fragments (plus neutrons) and the smallest of these may range from so small a charge and mass as a proton (Z = 1), to as large a fragment as argon (Z = 18). The most common small fragments, however, are composed of 90% helium-4 nuclei with more energy than alpha particles from alpha decay (so-called "long range alphas" at ~16 megaelectronvolts (MeV)), plus helium-6 nuclei, and tritons (the nuclei of tritium). Though less common than binary fission, it still produces significant helium-4 and tritium gas buildup in the fuel rods of modern nuclear reactors.[6]

Bohr and Wheeler used their liquid drop model, the packing fraction curve of Arthur Jeffrey Dempster, and Eugene Feenberg's estimates of nucleus radius and surface tension, to estimate the mass differences of parent and daughters in fission. They then equated this mass difference to energy using Einstein's mass-energy equivalence formula. The stimulation of the nucleus after neutron bombardment was analogous to the vibrations of a liquid drop, with surface tension and the Coulomb force in opposition. Plotting the sum of these two energies as a function of elongated shape, they determined the resultant energy surface had a saddle shape. The saddle provided an energy barrier called the critical energy barrier. Energy of about 6 MeV provided by the incident neutron was necessary to overcome this barrier and cause the nucleus to fission.[4]: 10–11 [7][8] According to John Lilley, "The energy required to overcome the barrier to fission is called the activation energy or fission barrier and is about 6 MeV for A ≈ 240. It is found that the activation energy decreases as A increases. Eventually, a point is reached where activation energy disappears altogether...it would undergo very rapid spontaneous fission."[9]

Maria Goeppert Mayer later proposed the nuclear shell model for the nucleus. The nuclides that can sustain a fission chain reaction are suitable for use as nuclear fuels. The most common nuclear fuels are 235U (the isotope of uranium with mass number 235 and of use in nuclear reactors) and 239Pu (the isotope of plutonium with mass number 239). These fuels break apart into a bimodal range of chemical elements with atomic masses centering near 95 and 135 daltons (fission products). Most nuclear fuels undergo spontaneous fission only very slowly, decaying instead mainly via an alpha-beta decay chain over periods of millennia to eons. In a nuclear reactor or nuclear weapon, the overwhelming majority of fission events are induced by bombardment with another particle, a neutron, which is itself produced by prior fission events.

Fissionable isotopes such as uranium-238 require additional energy provided by fast neutrons (such as those produced by nuclear fusion in thermonuclear weapons). While some of the neutrons released from the fission of 238
U
are fast enough to induce another fission in 238
U
, most are not, meaning it can never achieve criticality. While there is a very small (albeit nonzero) chance of a thermal neutron inducing fission in 238
U
, neutron absorption is orders of magnitude more likely.

Energetics

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Input

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The stages of binary fission in a liquid drop model. Energy input deforms the nucleus into a fat "cigar" shape, then a "peanut" shape, followed by binary fission as the two lobes exceed the short-range nuclear force attraction distance, and are then pushed apart and away by their electrical charge. In the liquid drop model, the two fission fragments are predicted to be the same size. The nuclear shell model allows for them to differ in size, as usually experimentally observed.

Fission cross sections are a measurable property related to the probability that fission will occur in a nuclear reaction. Cross sections are a function of incident neutron energy, and those for 235
U
and 239
Pu
are a million times higher than 238
U
at lower neutron energy levels. Absorption of any neutron makes available to the nucleus binding energy of about 5.3 MeV. 238
U
needs a fast neutron to supply the additional 1 MeV needed to cross the critical energy barrier for fission. In the case of 235
U
however, that extra energy is provided when 235
U
adjusts from an odd to an even mass. In the words of Younes and Lovelace, "...the neutron absorption on a 235
U
target forms a 236
U
nucleus with excitation energy greater than the critical fission energy, whereas in the case of n + 238
U
, the resulting 239
U
nucleus has an excitation energy below the critical fission energy."[4]: 25–28 [5]: 282–287 [10][11]

About 6 MeV of the fission-input energy is supplied by the simple binding of an extra neutron to the heavy nucleus via the strong force; however, in many fissionable isotopes, this amount of energy is not enough for fission. Uranium-238, for example, has a near-zero fission cross section for neutrons of less than 1 MeV energy. If no additional energy is supplied by any other mechanism, the nucleus will not fission, but will merely absorb the neutron, as happens when 238
U
absorbs slow and even some fraction of fast neutrons, to become 239
U
. The remaining energy to initiate fission can be supplied by two other mechanisms: one of these is more kinetic energy of the incoming neutron, which is increasingly able to fission a fissionable heavy nucleus as it exceeds a kinetic energy of 1 MeV or more (so-called fast neutrons). Such high energy neutrons are able to fission 238
U
directly (see thermonuclear weapon for application, where the fast neutrons are supplied by nuclear fusion). However, this process cannot happen to a great extent in a nuclear reactor, as too small a fraction of the fission neutrons produced by any type of fission have enough energy to efficiently fission 238
U
. (For example, neutrons from thermal fission of 235
U
have a mean energy of 2 MeV, a median energy of 1.6 MeV, and a mode of 0.75 MeV,[12][13] and the energy spectrum for fast fission is similar.[citation needed])

Among the heavy actinide elements, however, those isotopes that have an odd number of neutrons (such as 235U with 143 neutrons) bind an extra neutron with an additional 1 to 2 MeV of energy over an isotope of the same element with an even number of neutrons (such as 238U with 146 neutrons). This extra binding energy is made available as a result of the mechanism of neutron pairing effects, which itself is caused by the Pauli exclusion principle, allowing an extra neutron to occupy the same nuclear orbital as the last neutron in the nucleus. In such isotopes, therefore, no neutron kinetic energy is needed, for all the necessary energy is supplied by absorption of any neutron, either of the slow or fast variety (the former are used in moderated nuclear reactors, and the latter are used in fast-neutron reactors, and in weapons).

According to Younes and Loveland, "Actinides like 235
U
that fission easily following the absorption of a thermal (0.25 meV) neutron are called fissile, whereas those like 238
U
that do not easily fission when they absorb a thermal neutron are called fissionable."[4]: 25 

Output

[edit]

After an incident particle has fused with a parent nucleus, if the excitation energy is sufficient, the nucleus breaks into fragments. This is called scission, and occurs at about 10−20 seconds. The fragments can emit prompt neutrons at between 10−18 and 10−15 seconds. At about 10−11 seconds, the fragments can emit gamma rays. At 10−3 seconds β decay, β-delayed neutrons, and gamma rays are emitted from the decay products.[4]: 23–24 

Typical fission events release about two hundred million eV (200 MeV) of energy for each fission event. The exact isotope which is fissioned, and whether or not it is fissionable or fissile, has only a small impact on the amount of energy released. This can be easily seen by examining the curve of binding energy (image below), and noting that the average binding energy of the actinide nuclides beginning with uranium is around 7.6 MeV per nucleon. Looking further left on the curve of binding energy, where the fission products cluster, it is easily observed that the binding energy of the fission products tends to center around 8.5 MeV per nucleon. Thus, in any fission event of an isotope in the actinide mass range, roughly 0.9 MeV are released per nucleon of the starting element. The fission of 235U by a slow neutron yields nearly identical energy to the fission of 238U by a fast neutron. This energy release profile holds for thorium and the various minor actinides as well.[14]

Animation of a Coulomb explosion in the case of a cluster of positively charged nuclei, akin to a cluster of fission fragments. Hue level of color is proportional to (larger) nuclei charge. Electrons (smaller) on this time-scale are seen only stroboscopically and the hue level is their kinetic energy.

When a uranium nucleus fissions into two daughter nuclei fragments, about 0.1 percent of the mass of the uranium nucleus[15] appears as the fission energy of ~200 MeV. For uranium-235 (total mean fission energy 202.79 MeV[16]), typically ~169 MeV appears as the kinetic energy of the daughter nuclei, which fly apart at about 3% of the speed of light, due to Coulomb repulsion. Also, an average of 2.5 neutrons are emitted, with a mean kinetic energy per neutron of ~2 MeV (total of 4.8 MeV).[17] The fission reaction also releases ~7 MeV in prompt gamma ray photons. The latter figure means that a nuclear fission explosion or criticality accident emits about 3.5% of its energy as gamma rays, less than 2.5% of its energy as fast neutrons (total of both types of radiation ~6%), and the rest as kinetic energy of fission fragments (this appears almost immediately when the fragments impact surrounding matter, as simple heat).[18][19]

Some processes involving neutrons are notable for absorbing or finally yielding energy — for example neutron kinetic energy does not yield heat immediately if the neutron is captured by a uranium-238 atom to breed plutonium-239, but this energy is emitted if the plutonium-239 is later fissioned. On the other hand, so-called delayed neutrons emitted as radioactive decay products with half-lives up to several minutes, from fission-daughters, are very important to reactor control, because they give a characteristic "reaction" time for the total nuclear reaction to double in size, if the reaction is run in a "delayed-critical" zone which deliberately relies on these neutrons for a supercritical chain-reaction (one in which each fission cycle yields more neutrons than it absorbs). Without their existence, the nuclear chain-reaction would be prompt critical and increase in size faster than it could be controlled by human intervention. In this case, the first experimental atomic reactors would have run away to a dangerous and messy "prompt critical reaction" before their operators could have manually shut them down (for this reason, designer Enrico Fermi included radiation-counter-triggered control rods, suspended by electromagnets, which could automatically drop into the center of Chicago Pile-1). If these delayed neutrons are captured without producing fissions, they produce heat as well.[20]

Binding energy

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The "curve of binding energy": A graph of binding energy per nucleon of common isotopes.

The binding energy of the nucleus is the difference between the rest-mass energy of the nucleus and the rest-mass energy of the neutron and proton nucleons. The binding energy formula includes volume, surface and Coulomb energy terms that include empirically derived coefficients for all three, plus energy ratios of a deformed nucleus relative to a spherical form for the surface and Coulomb terms. Additional terms can be included such as symmetry, pairing, the finite range of the nuclear force, and charge distribution within the nuclei to improve the estimate.[4]: 46–50  Normally binding energy is referred to and plotted as average binding energy per nucleon.[9]

According to Lilley, "The binding energy of a nucleus B is the energy required to separate it into its constituent neutrons and protons."[9] where A is mass number, Z is atomic number, mH is the atomic mass of a hydrogen atom, mn is the mass of a neutron, and c is the speed of light. Thus, the mass of an atom is less than the mass of its constituent protons and neutrons, assuming the average binding energy of its electrons is negligible. The binding energy B is expressed in energy units, using Einstein's mass-energy equivalence relationship. The binding energy also provides an estimate of the total energy released from fission.[9]

The curve of binding energy is characterized by a broad maximum near mass number 60 at 8.6 MeV, then gradually decreases to 7.6 MeV at the highest mass numbers. Mass numbers higher than 238 are rare. At the lighter end of the scale, peaks are noted for helium-4, and the multiples such as beryllium-8, carbon-12, oxygen-16, neon-20 and magnesium-24. Binding energy due to the nuclear force approaches a constant value for large A, while the Coulomb acts over a larger distance so that electrical potential energy per proton grows as Z increases. Fission energy is released when a A is larger than approx. 60. Fusion energy is released when lighter nuclei combine.[9]

Carl Friedrich von Weizsäcker's semi-empirical mass formula may be used to express the binding energy as the sum of five terms, which are the volume energy, a surface correction, Coulomb energy, a symmetry term, and a pairing term:[9]

where the nuclear binding energy is proportional to the nuclear volume, while nucleons near the surface interact with fewer nucleons, reducing the effect of the volume term. According to Lilley, "For all naturally occurring nuclei, the surface-energy term dominates and the nucleus exists in a state of equilibrium." The negative contribution of Coulomb energy arises from the repulsive electric force of the protons. The symmetry term arises from the fact that effective forces in the nucleus are stronger for unlike neutron-proton pairs, rather than like neutron–neutron or proton–proton pairs. The pairing term arises from the fact that like nucleons form spin-zero pairs in the same spatial state. The pairing is positive if N and Z are both even, adding to the binding energy.[9]

In fission there is a preference for fission fragments with even Z, which is called the odd–even effect on the fragments' charge distribution. This can be seen in the empirical fragment yield data for each fission product, as products with even Z have higher yield values. However, no odd–even effect is observed on fragment distribution based on their A. This result is attributed to nucleon pair breaking.

In nuclear fission events the nuclei may break into any combination of lighter nuclei, but the most common event is not fission to equal mass nuclei of about mass 120; the most common event (depending on isotope and process) is a slightly unequal fission in which one daughter nucleus has a mass of about 90 to 100 daltons and the other the remaining 130 to 140 daltons.[21]

Stable nuclei, and unstable nuclei with very long half-lives, follow a trend of stability evident when Z is plotted against N. For lighter nuclei less than N = 20, the line has the slope N = Z, while the heavier nuclei require additional neutrons to remain stable. Nuclei that are neutron- or proton-rich have excessive binding energy for stability, and the excess energy may convert a neutron to a proton or a proton to a neutron via the weak nuclear force, a process known as beta decay.[9]

Neutron-induced fission of U-235 emits a total energy of 207 MeV, of which about 200 MeV is recoverable, Prompt fission fragments amount to 168 MeV, which are easily stopped with a fraction of a millimeter. Prompt neutrons total 5 MeV, and this energy is recovered as heat via scattering in the reactor. However, many fission fragments are neutron-rich and decay via β emissions. According to Lilley, "The radioactive decay energy from the fission chains is the second release of energy due to fission. It is much less than the prompt energy, but it is a significant amount and is why reactors must continue to be cooled after they have been shut down and why the waste products must be handled with great care and stored safely."[9]

Chain reactions

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A schematic nuclear fission chain reaction. 1. A uranium-235 atom absorbs a neutron and fissions into two new atoms (fission fragments), releasing three new neutrons and some binding energy. 2. One of those neutrons is absorbed by an atom of uranium-238 and does not continue the reaction. Another neutron is simply lost and does not collide with anything, also not continuing the reaction. However, the one neutron does collide with an atom of uranium-235, which then fissions and releases two neutrons and some binding energy. 3. Both of those neutrons collide with uranium-235 atoms, each of which fissions and releases between one and three neutrons, which can then continue the reaction.

John Lilley states, "...neutron-induced fission generates extra neutrons which can induce further fissions in the next generation and so on in a chain reaction. The chain reaction is characterized by the neutron multiplication factor k, which is defined as the ratio of the number of neutrons in one generation to the number in the preceding generation. If, in a reactor, k is less than unity, the reactor is subcritical, the number of neutrons decreases and the chain reaction dies out. If k > 1, the reactor is supercritical and the chain reaction diverges. This is the situation in a fission bomb where growth is at an explosive rate. If k is exactly unity, the reactions proceed at a steady rate and the reactor is said to be critical. It is possible to achieve criticality in a reactor using natural uranium as fuel, provided that the neutrons have been efficiently moderated to thermal energies." Moderators include light water, heavy water, and graphite.[9]: 269, 274 

According to John C. Lee, "For all nuclear reactors in operation and those under development, the nuclear fuel cycle is based on one of three fissile materials, 235U, 233U, and 239Pu, and the associated isotopic chains. For the current generation of LWRs, the enriched U contains 2.5~4.5 wt% of 235U, which is fabricated into UO2 fuel rods and loaded into fuel assemblies."[22]

Lee states, "One important comparison for the three major fissile nuclides, 235U, 233U, and 239Pu, is their breeding potential. A breeder is by definition a reactor that produces more fissile material than it consumes and needs a minimum of two neutrons produced for each neutron absorbed in a fissile nucleus. Thus, in general, the conversion ratio (CR) is defined as the ratio of fissile material produced to that destroyed...when the CR is greater than 1.0, it is called the breeding ratio (BR)...233U offers a superior breeding potential for both thermal and fast reactors, while 239Pu offers a superior breeding potential for fast reactors."[22]

Fission reactors

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The cooling towers of the Philippsburg Nuclear Power Plant in Germany

Critical fission reactors are the most common type of nuclear reactor. In a critical fission reactor, neutrons produced by fission of fuel atoms are used to induce yet more fissions, to sustain a controllable amount of energy release. Devices that produce engineered but non-self-sustaining fission reactions are subcritical fission reactors. Such devices use radioactive decay or particle accelerators to trigger fissions.

Critical fission reactors are built for three primary purposes, which typically involve different engineering trade-offs to take advantage of either the heat or the neutrons produced by the fission chain reaction:

While, in principle, all fission reactors can act in all three capacities, in practice the tasks lead to conflicting engineering goals and most reactors have been built with only one of the above tasks in mind. (There are several early counter-examples, such as the Hanford N reactor, now decommissioned).

As of 2019, the 448 nuclear power plants worldwide provided a capacity of 398 GWE, with about 85% being light-water cooled reactors such as pressurized water reactors or boiling water reactors. Energy from fission is transmitted through conduction or convection to the nuclear reactor coolant, then to a heat exchanger, and the resultant generated steam is used to drive a turbine or generator.[22]: 1–4 

Fission bombs

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The mushroom cloud of the atomic bomb dropped on Nagasaki, Japan, on 9 August 1945 rose over 12 kilometres (7.5 mi) above the bomb's hypocenter. An estimated 39,000 people were killed by the atomic bomb,[23] of whom 23,145–28,113 were Japanese factory workers, 2,000 were Korean slave laborers, and 150 were Japanese combatants.[24][25][26]

The objective of an atomic bomb is to produce a device, according to Serber, "...in which energy is released by a fast neutron chain reaction in one or more of the materials known to show nuclear fission." According to Rhodes, "Untamped, a bomb core even as large as twice the critical mass would completely fission less than 1 percent of its nuclear material before it expanded enough to stop the chain reaction from proceeding. Tamper always increased efficiency: it reflected neutrons back into the core and its inertia...slowed the core's expansion and helped keep the core surface from blowing away." Rearrangement of the core material's subcritical components would need to proceed as fast as possible to ensure effective detonation. Additionally, a third basic component was necessary, "...an initiator—a Ra + Be source or, better, a Po + Be source, with the radium or polonium attached perhaps to one piece of the core and the beryllium to the other, to smash together and spray neutrons when the parts mated to start the chain reaction." However, any bomb would "necessitate locating, mining and processing hundreds of tons of uranium ore...", while U-235 separation or the production of Pu-239 would require additional industrial capacity.[5]: 460–463 

History

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Discovery of nuclear fission

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Otto Hahn and Lise Meitner in 1912

The discovery of nuclear fission occurred in 1938 in the buildings of the Kaiser Wilhelm Society for Chemistry, today part of the Free University of Berlin, following over four decades of work on the science of radioactivity and the elaboration of new nuclear physics that described the components of atoms. In 1911, Ernest Rutherford proposed a model of the atom in which a very small, dense and positively charged nucleus of protons was surrounded by orbiting, negatively charged electrons (the Rutherford model).[27] Niels Bohr improved upon this in 1913 by reconciling the quantum behavior of electrons (the Bohr model). In 1928, George Gamow proposed the Liquid drop model, which became essential to understanding the physics of fission.[5]: 49–51, 70–77, 228 [4]: 6–7 

In 1896, Henri Becquerel had found, and Marie Curie named, radioactivity. In 1900, Rutherford and Frederick Soddy, investigating the radioactive gas emanating from thorium, "conveyed the tremendous and inevitable conclusion that the element thorium was slowly and spontaneously transmuting itself into argon gas!"[5]: 41–43 

In 1919, following up on an earlier anomaly Ernest Marsden noted in 1915, Rutherford attempted to "break up the atom." Rutherford was able to accomplish the first artificial transmutation of nitrogen into oxygen, using alpha particles directed at nitrogen 14N + α → 17O + p.  Rutherford stated, "...we must conclude that the nitrogen atom is disintegrated," while the newspapers stated he had split the atom. This was the first observation of a nuclear reaction, that is, a reaction in which particles from one decay are used to transform another atomic nucleus. It also offered a new way to study the nucleus. Rutherford and James Chadwick then used alpha particles to "disintegrate" boron, fluorine, sodium, aluminum, and phosphorus before reaching a limitation associated with the energy of his alpha particle source.[5] Eventually, in 1932, a fully artificial nuclear reaction and nuclear transmutation was achieved by Rutherford's colleagues Ernest Walton and John Cockcroft, who used artificially accelerated protons against lithium-7, to split this nucleus into two alpha particles. The feat was popularly known as "splitting the atom", and would win them the 1951 Nobel Prize in Physics for "Transmutation of atomic nuclei by artificially accelerated atomic particles", although it was not the nuclear fission reaction later discovered in heavy elements.[28][29][30]

English physicist James Chadwick discovered the neutron in 1932.[31] Chadwick used an ionization chamber to observe protons knocked out of several elements by beryllium radiation, following up on earlier observations made by Joliot-Curies. In Chadwick's words, "...In order to explain the great penetrating power of the radiation we must further assume that the particle has no net charge..." The existence of the neutron was first postulated by Rutherford in 1920, and in the words of Chadwick, "...how on earth were you going to build up a big nucleus with a large positive charge? And the answer was a neutral particle."[5]: 153–165  Subsequently, he communicated his findings in more detail.[32]

In the words of Richard Rhodes, referring to the neutron, "It would therefore serve as a new nuclear probe of surpassing power of penetration." Philip Morrison stated, "A beam of thermal neutrons moving at about the speed of sound...produces nuclear reactions in many materials much more easily than a beam of protons...traveling thousands of times faster." According to Rhodes, "Slowing down a neutron gave it more time in the vicinity of the nucleus, and that gave it more time to be captured." Fermi's team, studying radiative capture which is the emission of gamma radiation after the nucleus captures a neutron, studied sixty elements, inducing radioactivity in forty. In the process, they discovered the ability of hydrogen to slow down the neutrons.[5]: 165, 216–220 

Enrico Fermi and his colleagues in Rome studied the results of bombarding uranium with neutrons in 1934.[33] Fermi concluded that his experiments had created new elements with 93 and 94 protons, which the group dubbed ausenium and hesperium. However, not all were convinced by Fermi's analysis of his results, though he would win the 1938 Nobel Prize in Physics for his "demonstrations of the existence of new radioactive elements produced by neutron irradiation, and for his related discovery of nuclear reactions brought about by slow neutrons". The German chemist Ida Noddack notably suggested in 1934 that instead of creating a new, heavier element 93, that "it is conceivable that the nucleus breaks up into several large fragments."[34] However, the quoted objection comes some distance down, and was but one of several gaps she noted in Fermi's claim. Although Noddack was a renowned analytical chemist, she lacked the background in physics to appreciate the enormity of what she was proposing.[35]

The nuclear fission display at the Deutsches Museum in Munich. The table and instruments are originals,[36][37] but would not have been together in the same room.

After the Fermi publication, Otto Hahn, Lise Meitner, and Fritz Strassmann began performing similar experiments in Berlin. Meitner, an Austrian Jew, lost her Austrian citizenship with the Anschluss, the union of Austria with Germany in March 1938, but she fled in July 1938 to Sweden and started a correspondence by mail with Hahn in Berlin. By coincidence, her nephew Otto Robert Frisch, also a refugee, was also in Sweden when Meitner received a letter from Hahn dated 19 December describing his chemical proof that some of the product of the bombardment of uranium with neutrons was barium. Hahn suggested a bursting of the nucleus, but he was unsure of what the physical basis for the results were. Barium had an atomic mass 40% less than uranium, and no previously known methods of radioactive decay could account for such a large difference in the mass of the nucleus. Frisch was skeptical, but Meitner trusted Hahn's ability as a chemist. Marie Curie had been separating barium from radium for many years, and the techniques were well known. Meitner and Frisch then correctly interpreted Hahn's results to mean that the nucleus of uranium had split roughly in half. Frisch suggested the process be named "nuclear fission", by analogy to the process of living cell division into two cells, which was then called binary fission. Just as the term nuclear "chain reaction" would later be borrowed from chemistry, so the term "fission" was borrowed from biology.[38]

News spread quickly of the new discovery, which was correctly seen as an entirely novel physical effect with great scientific—and potentially practical—possibilities. Meitner's and Frisch's interpretation of the discovery of Hahn and Strassmann crossed the Atlantic Ocean with Niels Bohr, who was to lecture at Princeton University. I.I. Rabi and Willis Lamb, two Columbia University physicists working at Princeton, heard the news and carried it back to Columbia. Rabi said he told Enrico Fermi; Fermi gave credit to Lamb. Bohr soon thereafter went from Princeton to Columbia to see Fermi. Not finding Fermi in his office, Bohr went down to the cyclotron area and found Herbert L. Anderson. Bohr grabbed him by the shoulder and said: "Young man, let me explain to you about something new and exciting in physics."[39]

It was clear to a number of scientists at Columbia that they should try to detect the energy released in the nuclear fission of uranium from neutron bombardment. On 25 January 1939, a Columbia University team conducted the first nuclear fission experiment in the United States,[40] which was done in the basement of Pupin Hall. The experiment involved placing uranium oxide inside of an ionization chamber and irradiating it with neutrons, and measuring the energy thus released. The results confirmed that fission was occurring and hinted strongly that it was the isotope uranium 235 in particular that was fissioning. The next day, the fifth Washington Conference on Theoretical Physics began in Washington, D.C. under the joint auspices of the George Washington University and the Carnegie Institution of Washington. There, the news on nuclear fission was spread even further, which fostered many more experimental demonstrations.[41] The 6 January 1939 Hahn and Strassman paper announced the discover of fission. In their second publication on nuclear fission in February 1939, Hahn and Strassmann used the term Uranspaltung (uranium fission) for the first time, and predicted the existence and liberation of additional neutrons during the fission process, opening up the possibility of a nuclear chain reaction.[42] The 11 February 1939 paper by Meitner and Frisch compared the process to the division of a liquid drop and estimated the energy released at 200 MeV.[43] The 1 September 1939 paper by Bohr and Wheeler used this liquid drop model to quantify fission details, including the energy released, estimated the cross section for neutron-induced fission, and deduced 235
U
was the major contributor to that cross section and slow-neutron fission.[44][5]: 262, 311 [4]: 9–13 

Fission chain reaction realized

[edit]

During this period the Hungarian physicist Leó Szilárd realized that the neutron-driven fission of heavy atoms could be used to create a nuclear chain reaction. Such a reaction using neutrons was an idea he had first formulated in 1933, upon reading Rutherford's disparaging remarks about generating power from neutron collisions. However, Szilárd had not been able to achieve a neutron-driven chain reaction using beryllium. Szilard stated, "...if we could find an element which is split by neutrons and which would emit two neutrons when it absorbs one neutron, such an element, if assembled in sufficiently large mass, could sustain a nuclear chain reaction." On 25 January 1939, after learning of Hahn's discovery from Eugene Wigner, Szilard noted, "...if enough neutrons are emitted...then it should be, of course, possible to sustain a chain reaction. All of the things which H. G. Wells predicted appeared suddenly real to me." After the Hahn-Strassman paper was published, Szilard noted in a letter to Lewis Strauss, that during the fission of uranium, "the energy released in this new reaction must be very much higher than all previously known cases...," which might lead to "large-scale production of energy and radioactive elements, unfortunately also perhaps to atomic bombs."[45][5]: 26–28, 203–204, 213–214, 223–225, 267–268 

Szilard now urged Fermi (in New York) and Frédéric Joliot-Curie (in Paris) to refrain from publishing on the possibility of a chain reaction, lest the Nazi government become aware of the possibilities on the eve of what would later be known as World War II. With some hesitation Fermi agreed to self-censor. But Joliot-Curie did not, and in April 1939 his team in Paris, including Hans von Halban and Lew Kowarski, reported in the journal Nature that the number of neutrons emitted with nuclear fission of uranium was then reported at 3.5 per fission.[46] Szilard and Walter Zinn found "...the number of neutrons emitted by fission to be about two." Fermi and Anderson estimated "a yield of about two neutrons per each neutron captured."[5]: 290–291, 295–296 

Drawing of the first artificial reactor, Chicago Pile-1

With the news of fission neutrons from uranium fission, Szilárd immediately understood the possibility of a nuclear chain reaction using uranium. In the summer, Fermi and Szilard proposed the idea of a nuclear reactor (pile) to mediate this process. The pile would use natural uranium as fuel. Fermi had shown much earlier that neutrons were far more effectively captured by atoms if they were of low energy (so-called "slow" or "thermal" neutrons), because for quantum reasons it made the atoms look like much larger targets to the neutrons. Thus to slow down the secondary neutrons released by the fissioning uranium nuclei, Fermi and Szilard proposed a graphite "moderator", against which the fast, high-energy secondary neutrons would collide, effectively slowing them down. With enough uranium, and with sufficiently pure graphite, their "pile" could theoretically sustain a slow-neutron chain reaction. This would result in the production of heat, as well as the creation of radioactive fission products.[5]: 291, 298–302 

In August 1939, Szilard, Teller and Wigner thought that the Germans might make use of the fission chain reaction and were spurred to attempt to attract the attention of the United States government to the issue. Towards this, they persuaded Albert Einstein to lend his name to a letter directed to President Franklin Roosevelt. On 11 October, the Einstein–Szilárd letter was delivered via Alexander Sachs. Roosevelt quickly understood the implications, stating, "Alex, what you are after is to see that the Nazis don't blow us up." Roosevelt ordered the formation of the Advisory Committee on Uranium.[5]: 303–309, 312–317 

In February 1940, encouraged by Fermi and John R. Dunning, Alfred O. C. Nier was able to separate U-235 and U-238 from uranium tetrachloride in a glass mass spectrometer. Subsequently, Dunning, bombarding the U-235 sample with neutrons generated by the Columbia University cyclotron, confirmed "U-235 was responsible for the slow neutron fission of uranium."[5]: 297–298, 332 

At the University of Birmingham, Frisch teamed up with Peierls, who had been working on a critical mass formula. assuming isotope separation was possible, they considered 235U, which had a cross section not yet determined, but which was assumed to be much larger than that of natural uranium. They calculated only a pound or two in a volume less than a golf ball, would result in a chain reaction faster than vaporization, and the resultant explosion would generate temperature greater than the interior of the sun, and pressures greater than the center of the earth. Additionally, the costs of isotope separation "would be insignificant compared to the cost of the war." By March 1940, encouraged by Mark Oliphant, they wrote the Frisch–Peierls memorandum in two parts, "On the construction of a 'super-bomb; based on a nuclear chain reaction in uranium," and "Memorandum on the properties of a radioactive 'super-bomb.' ". On 10 April 1940, the first meeting of the MAUD Committee was held.[5]: 321–325, 330–331, 340–341 

In December 1940, Franz Simon at Oxford wrote his Estimate of the size of an actual separation plant." Simon proposed gaseous diffusion as the best method for uranium isotope separation.[5]: 339, 343 

On 28 March 1941, Emilio Segré and Glen Seaborg reported on the "strong indications that 239Pu undergoes fission with slow neutrons." This meant chemical separation was an alternative to uranium isotope separation. Instead, a nuclear reactor fueled with ordinary uranium could produce a plutonium isotope as a nuclear explosive substitute for 235U. In May, they demonstrated the cross section of plutonium was 1.7 times that of U235. When plutonium's cross section for fast fission was measured to be ten times that of U238, plutonium became a viable option for a bomb.[5]: 346–355, 366–368 

In October 1941, MAUD released its final report to the U.S. Government. The report stated, "We have now reached the conclusion that it will be possible to make an effective uranium bomb...The material for the first bomb could be ready by the end of 1943..."[5]: 368–369 

In November 1941, John Dunning and Eugene T. Booth were able to demonstrate the enrichment of uranium through gaseous barrier diffusion. On 27 November, Bush delivered to third National Academy of Sciences report to Roosevelt. The report, amongst other things, called for parallel development of all isotope-separation systems. On 6 December, Bush and Conant reorganized the Uranium Committee's tasks, with Harold Urey developing gaseous diffusion, Lawrence developing electromagnetic separation, Eger V. Murphree developing centrifuges, and Arthur Compton responsible for theoretical studies and design.[5]: 381, 387–388 

On 23 April 1942, Met Lab scientists discussed seven possible ways to extract plutonium from irradiated uranium, and decided to pursue investigation of all seven. On 17 June, the first batch of uranium nitrate hexahydrate (UNH) was undergoing neutron bombardment in the Washington University in St. Louis cyclotron. On 27 July, the irradiated UNH was ready for Glenn T. Seaborg's team. On 20 August, using ultramicrochemistry techniques, they successfully extracted plutonium.[5]: 408–415 

In April 1939, creating a chain reaction in natural uranium became the goal of Fermi and Szilard, as opposed to isotope separation. Their first efforts involved five hundred pounds of uranium oxide from the Eldorado Radium Corporation. Packed into fifty-two cans two inches in diameter and two feet long in a tank of manganese solution, they were able to confirm more neutrons were emitted than absorbed. However, the hydrogen within the water absorbed the slow neutrons necessary for fission. Carbon in the form of graphite, was then considered, because of its smaller capture cross section. In April 1940, Fermi was able to confirm carbon's potential for a slow-neutron chain reaction, after receiving National Carbon Company's graphite bricks at their Pupin Laboratories. In August and September, the Columbia team enlarged upon the cross section measurements by making a series of exponential "piles". The first piles consisted of a uranium-graphite lattice, consisting of 288 cans, each containing 60 pounds of uranium oxide, surrounded by graphite bricks. Fermi's goal was to determine critical mass necessary to sustain neutron generation. Fermi defined the reproduction factor k for assessing the chain reaction, with a value of 1.0 denoting a sustained chain reaction. In September 1941, Fermi's team was only able to achieve a k value of 0.87. In April 1942, before the project was centralized in Chicago, they had achieved 0.918 by removing moisture from the oxide. In May 1942, Fermi planned a full-scale chain reacting pile, Chicago Pile-1, after one of the exponential piles at Stagg Field reached a k of 0.995. Between 15 September and 15 November, Herbert L. Anderson and Walter Zinn built sixteen exponential piles. Acquisition of purer forms of graphite, without traces of boron and its large cross section, became paramount. Also important was the acquisition of highly purified forms of oxide from Mallinckrodt Chemical Works. Finally, acquiring pure uranium metal from the Ames process, meant the replacement of oxide pseudospheres with Frank Spedding's "eggs". Starting on 16 November 1942, Fermi had Anderson and Zinn working in two twelve-hours shifts, constructing a pile that eventually reached 57 layers by 1 Dec. The final pile consisted of 771,000 pounds of graphite, 80,590 pounds of uranium oxide, and 12,400 pounds of uranium metal, with ten cadmium control rods. Neutron intensity was measured with a boron trifluoride counter, with the control rods removed, after the end of each shift. On 2 Dec. 1942, with k approaching 1.0, Fermi had all but one of the control rod removed, and gradually removed the last one. The neutron counter clicks increased, as did the pen recorder, when Fermi announced "The pile has gone critical." They had achieved a k of 1.006, which meant neutron intensity doubled every two minutes, in addition to breeding plutonium.[5]: 298–301, 333–334, 394–397, 400–401, 428–442 

Manhattan Project and beyond

[edit]

In the United States, an all-out effort for making atomic weapons was begun in late 1942. This work was taken over by the U.S. Army Corps of Engineers in 1943, and known as the Manhattan Engineer District. The top-secret Manhattan Project, as it was colloquially known, was led by General Leslie R. Groves. Among the project's dozens of sites were: Hanford Site in Washington, which had the first industrial-scale nuclear reactors and produced plutonium; Oak Ridge, Tennessee, which was primarily concerned with uranium enrichment; and Los Alamos, in New Mexico, which was the scientific hub for research on bomb development and design. Other sites, notably the Berkeley Radiation Laboratory and the Metallurgical Laboratory at the University of Chicago, played important contributing roles. Overall scientific direction of the project was managed by the physicist J. Robert Oppenheimer.

In July 1945, the first atomic explosive device, dubbed "The Gadget", was detonated in the New Mexico desert in the Trinity test. It was fueled by plutonium created at Hanford. In August 1945, two more atomic devices – "Little Boy", a uranium-235 bomb, and "Fat Man", a plutonium bomb – were used against the Japanese cities of Hiroshima and Nagasaki.

Natural fission chain-reactors on Earth

[edit]

Criticality in nature is uncommon. At three ore deposits at Oklo in Gabon, sixteen sites (the so-called Oklo Fossil Reactors) have been discovered at which self-sustaining nuclear fission took place approximately 2 billion years ago. French physicist Francis Perrin discovered the Oklo Fossil Reactors in 1972, but it was postulated by Paul Kuroda in 1956.[47] Large-scale natural uranium fission chain reactions, moderated by normal water, had occurred far in the past and would not be possible now. This ancient process was able to use normal water as a moderator only because 2 billion years before the present, natural uranium was richer in the shorter-lived fissile isotope 235U (about 3%), than natural uranium available today (which is only 0.7%, and must be enriched to 3% to be usable in light-water reactors).

See also

[edit]

References

[edit]

Further reading

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Nuclear fission occurs when a heavy nucleus, such as uranium-235 or plutonium-239, absorbs a neutron and splits into lighter fission products, releasing additional neutrons, gamma rays, and substantial energy—primarily as kinetic energy of the fragments.[1] This release arises because the fission products have greater binding energy per nucleon than the original nucleus, converting nuclear mass into energy via Einstein's equivalence principle.[2] First observed in 1938 by Otto Hahn and Fritz Strassmann through neutron bombardment of uranium, the process was theoretically explained by Lise Meitner and Otto Frisch, who termed it "fission" by analogy to cell division.[3] Fission enables chain reactions, in which released neutrons trigger further splits, yielding exponential energy amplification at criticality—a foundation for both controlled nuclear reactors generating electricity and explosive atomic bombs.[1] Nuclear power plants use enriched uranium to maintain controlled chain reactions, producing heat to drive steam turbines and supply about 10% of global electricity, with lifecycle deaths per terawatt-hour lower than fossil fuels.[4] In contrast, fission weapons, developed via the Manhattan Project and tested at Trinity in 1945 before deployment on Hiroshima and Nagasaki, deliver yields equivalent to thousands of tons of TNT.[3] Though challenged by proliferation, waste management, and rare accidents like Chernobyl, fission's energy density—millions of times that of chemical reactions—establishes it as a reliable, low-carbon energy option, despite public perceptions distorted by incident-focused coverage.[5]

Fundamentals of Nuclear Fission

Definition and Basic Process

Nuclear fission is a nuclear reaction in which the nucleus of a heavy atom, such as uranium-235 or plutonium-239, splits into two or more lighter nuclei (fission products), releasing neutrons and substantial energy.[1] Unlike radioactive decay, it requires an external trigger and yields net exothermic output from binding energy differences.[6] The process starts with a fissile nucleus absorbing a neutron, forming an excited compound nucleus. For uranium-235, a thermal neutron produces unstable uranium-236, whose excess internal energy causes deformation that overcomes proton repulsion, leading to scission into unequal-mass fragments (typically ~95 and ~140), plus prompt neutrons and gamma rays.[7][6] Each event releases ~2.45 neutrons (for uranium-235) and ~200 MeV of recoverable energy, mostly as kinetic energy of recoiling fragments that thermalize in surrounding material.[6] These neutrons can sustain a chain reaction if absorbed by other fissile nuclei, enabling reactors and weapons.[7] Neutron-rich products undergo beta decay, yielding delayed neutrons (~0.66% for uranium-235) and additional radiation.[6]

Nuclear Binding Energy and Fission Barriers

The nuclear binding energy B(A,Z)B(A, Z) of a nucleus with atomic number ZZ, mass number AA, and neutron number N=AZN = A - Z equals the mass defect's energy equivalent: B(A,Z)=[ZmH+NmnM(A,Z)]c2B(A, Z) = [Z m_H + N m_n - M(A, Z)] c^2, where mHm_H is the hydrogen atom mass, mnm_n the neutron mass, M(A,Z)M(A, Z) the neutral atom mass, and cc the speed of light.[8] This represents the energy to separate the nucleus into protons and neutrons, with the strong force countering proton repulsion.[9] Per-nucleon binding energy B/AB/A rises with AA to a peak at iron-56 (56Fe^{56}\mathrm{Fe}, ~8.8 MeV/nucleon), then declines for heavier nuclei like uranium-235 (~7.6 MeV/nucleon).[10] Fission of such heavy nuclei into medium-mass fragments thus releases energy, as products' total binding exceeds the original by ~200 MeV per uranium event.[11] The semi-empirical mass formula approximates BavAasA2/3acZ2A1/3aa(A2Z)2A±δB \approx a_v A - a_s A^{2/3} - a_c \frac{Z^2}{A^{1/3}} - a_a \frac{(A - 2Z)^2}{A} \pm \delta, with coefficients av15.5a_v \approx 15.5 MeV (volume), as16.8a_s \approx 16.8 MeV (surface), ac0.72a_c \approx 0.72 MeV (Coulomb), aa23a_a \approx 23 MeV (asymmetry), and δ\delta (pairing).[12] For large AA, volume dominates, but Coulomb's Z2Z^2 scaling reduces stability in heavy elements, enabling exothermic fission.[12] Fission barriers provide the activation energy for deformation to scission, appearing as a saddle-point maximum in the liquid drop model between surface minimization and Coulomb-driven elongation.[13] For 235U^{235}\mathrm{U}, height is ~5.7 MeV with ωB0.5\hbar \omega_B \approx 0.5 MeV, inferred from transfer reactions.[14] This elevates spontaneous fission rarity (half-life ~101710^{17} years) despite favorability, as thermal excitations rarely suffice. Neutron-induced fission bypasses it: absorption yields 236U^{236}\mathrm{U}^* at ~6.5 MeV (neutron binding energy), enabling barrier surmount and asymmetric division. Shell effects reduce barriers for specific neutron counts, promoting asymmetry, though liquid drop models the core macroscopic barrier.[13][14]

Mechanism and Energetics

Fission Reaction Dynamics

Nuclear fission dynamics begin with a neutron absorbed by a fissile nucleus like uranium-235, forming an excited uranium-236 compound nucleus (~6.5 MeV excitation from neutron binding energy in thermal capture). This instability drives deformation, modeled by the liquid drop approach where nuclear surface tension balances Coulomb repulsion.[15][16] The nucleus overcomes the fission barrier (~5.5–6 MeV for uranium-236) via quantum tunneling or thermal fluctuations, passing a saddle-point to the scission point.[17] There, the neck ruptures, producing deformed, excited fragments that accelerate apart under strong Coulomb repulsion (due to high atomic numbers), reaching ~10^7 m/s and converting potential to kinetic energy—about 80% of total fission energy.[18] Prompt neutrons (~2.45 per thermal uranium-235 fission) evaporate from these highly excited fragments (excitation >7–10 MeV neutron binding per fragment) within ~10^{-14} seconds post-scission, during acceleration, which broadens the spectrum via Doppler shift from fragment motion. Prompt gammas and later beta decays partition remaining energy, ending the primary phase with fragment separation and de-excitation.[6][19][7]

Energy Release and Outputs

Nuclear fission releases energy from the binding energy difference between the original heavy nucleus and fission products, which have higher average binding energy per nucleon near the iron peak. For thermal neutron-induced uranium-235 fission, the uranium-236 compound nucleus has ~7.6 MeV per nucleon, while typical products like strontium-95 and xenon-139 have ~8.5 MeV, yielding ~0.9 MeV excess per nucleon or ~200 MeV total across ~236 nucleons.[20][6] This vastly exceeds chemical reactions' eV-scale energies per atom, enabling applications in power and weapons.[21] Of the ~200 MeV per uranium-235 fission, outputs distribute as follows: kinetic energy of two primary fragments (majority, rapidly converting to thermal energy via surrounding material); prompt neutrons (2-3 per event); prompt gamma rays during scission; delayed radiation from fission product decay; and neutrinos (~10-12 MeV from beta decays, escaping without deposition).[6][22]
Energy FormApproximate Share (MeV)Notes
Fission fragment kinetic energy~170Prompt; ~85% of total, decelerated in fuel to produce heat.[6]
Neutron kinetic energy~5Prompt; from 2-3 neutrons at ~2 MeV each on average.[6]
Prompt gamma rays~7Emitted during fission process.[6]
Delayed beta particles and gamma rays~18From radioactive decay of neutron-rich fission products.[6]
This partitioning enables sustained chain reactions, with neutron kinetic energy supporting chains and fragment motion dominating recoverable heat in reactors.[23] Yields vary slightly by fissile isotope (e.g., higher for plutonium-239) and incident neutron energy but center around these values for thermal fission.[24]

Chain Reactions and Criticality

A nuclear chain reaction in fission occurs when neutrons from one fissile nucleus split—such as uranium-235—are absorbed by others, triggering further fissions and neutron release.[25] Exponential propagation requires enough neutrons to sustain fissions, with each uranium-235 thermal event yielding 2.43 neutrons on average.[21] Yet not all contribute effectively: some escape, others are captured without fission, or induce non-sustaining reactions. Criticality balances this neutron economy via the effective multiplication factor keffk_{\text{eff}}, the ratio of neutrons produced in one generation to the prior.[26] Subcritical (keff<1k_{\text{eff}} < 1) yields declining neutron populations and reaction fade; critical (keff=1k_{\text{eff}} = 1) maintains steady flux; supercritical (keff>1k_{\text{eff}} > 1) drives rapid neutron growth and energy surges.[27] Criticality demands a minimum fissile mass, the critical mass, varying with geometry, density, enrichment, and materials. A bare sphere of 93.5% enriched uranium-235 metal at standard density requires about 47 kg.[28] Spheres curb leakage through low surface-to-volume ratios; reflectors like beryllium or water cut the mass by redirecting strays.[29] Neutron-absorbing impurities raise it, while moderators such as graphite or heavy water boost fission odds by thermalizing fast neutrons.[30]

Historical Development

Discovery and Early Experiments

The discovery of nuclear fission arose from 1930s experiments on neutron-induced transmutations in heavy elements.[31] After James Chadwick identified the neutron in 1932, researchers bombarded nuclei to induce radioactivity.[31] In 1934, Enrico Fermi's group at the University of Rome irradiated uranium with neutrons, detecting radioactive products they viewed as transuranic elements.[31] Ida Noddack suggested the uranium nucleus might instead split into lighter elements of comparable mass, but this was dismissed for lacking evidence of such massive fragmentation.[32] In Berlin, Otto Hahn, Fritz Strassmann, and Lise Meitner at the Kaiser Wilhelm Institute sought to replicate Fermi's results.[33] From 1936, they bombarded uranium with slow neutrons, identifying isotopes initially linked to elements near uranium, such as radium or actinium.[34] By mid-1938, analyses showed activities akin to lighter elements like radium (atomic number 88).[35] Meitner, who was Jewish, fled Nazi Germany to Sweden in July 1938, leaving Hahn and Strassmann to proceed under political strain.[31] In December 1938, Hahn and Strassmann irradiated uranyl nitrate solutions with neutrons from radon-beryllium sources.[33] Chemical separation and crystallization revealed barium (atomic number 56) as a key product, verified by sulfate precipitation and spectral lines—contrary to expectations of heavier residues.[35] Their December 22, 1938, publication in Die Naturwissenschaften described uranium nuclei splitting into roughly half-mass fragments, challenging assumptions of gradual alpha or beta decay.[33] Hahn informed Meitner of the baffling barium yield in a December 19 letter.[31] During a late December 1938 walk in Sweden, Meitner and nephew Otto Robert Frisch theorized the process using Niels Bohr's liquid drop model: deformation overcomes the fission barrier, releasing about 200 MeV per event.[36] They termed it "fission," analogous to biological cell division, and predicted secondary neutrons—verified by Frisch's January 1939 ionization pulse experiments on fragments.[36] Their February 11, 1939, Nature paper clarified the anomalies and affirmed fission as a nuclear reaction.[31] Teams in Paris and the United States, including Frederic Joliot-Curie and Enrico Fermi, soon confirmed it and its chain reaction potential.[35]

Realization of Controlled Chain Reactions

After the 1938 discovery of nuclear fission, physicists identified potential for self-sustaining chain reactions with uranium-235, but control demanded experimental management of neutron production and absorption to prevent escalation.[37] In 1942, Enrico Fermi, leading the Manhattan Project's Metallurgical Laboratory at the University of Chicago, constructed Chicago Pile-1 (CP-1): a lattice of uranium metal and oxide embedded in graphite moderator blocks to slow neutrons and sustain fission.[38] Built without blueprints starting in October, it involved iterative assembly by about 30 scientists—including Leo Szilard, Walter Zinn, and Herbert Anderson—stacking over 40 tons of graphite and 6 tons of uranium.[39] On December 2, 1942, beneath the west stands of the University of Chicago's Stagg Field, the team initiated the first artificial self-sustaining chain reaction in CP-1, achieving criticality at a neutron multiplication factor of about 1.006 and 0.5 watts thermal power, then shutting it down after 28 minutes with cadmium absorbers.[40] This proved fission chain reactions could be regulated via absorbers and fuel-moderator geometry, validating theory and informing later reactor designs.[41] Verified by neutron counters and power rise data, it guided plutonium production under the Manhattan Project, scaling principles to Hanford's water-cooled graphite reactors.[38] Disassembled in 1943 due to safety risks from absent containment, CP-1 nonetheless established controlled fission's viability for energy and isotope production, underpinning all subsequent reactors despite early low efficiency and manual controls.[39] Fermi prioritized empirical tests with safeguards like slide-wire control rods, averting supercriticality.[37] Unlike uncontrolled bomb reactions, this demonstrated fission's moderated dual use.[42]

World War II Applications and Post-War Expansion

The Manhattan Project, a classified U.S. effort launched in 1942 under the Army Corps of Engineers and directed by J. Robert Oppenheimer at Los Alamos, developed the first fission-based atomic bombs to counter potential Axis powers advances. The Trinity test on July 16, 1945, detonated a plutonium implosion device yielding 21 kilotons of TNT equivalent at Alamogordo, New Mexico, proving explosive chain reactions viable.[43] Two bombs followed: "Little Boy," a uranium-235 gun-type device dropped on Hiroshima from the B-29 Enola Gay on August 6, 1945, destroyed much of the city and killed 70,000–80,000 immediately from blast, heat, and radiation.[44] "Fat Man," a plutonium implosion bomb like Trinity, struck Nagasaki on August 9, killing 35,000–40,000 instantly and aiding Japan's surrender on August 15.[45] These events showcased fission's destructive power, with project costs over $2 billion (about $30 billion in 2023 dollars).[46] Postwar, Cold War demands drove rapid military and civilian expansion of fission technology. The U.S. ran Operation Crossroads in 1946 at Bikini Atoll, testing bombs up to 23 kilotons on naval targets, and built over 300 warheads by 1950 via Hanford plutonium and Oak Ridge enrichment.[47] The Soviet Union tested its first plutonium implosion device, RDS-1 (aided by espionage), on August 29, 1949, at Semipalatinsk, spurring U.S. stockpiles beyond 1,000 by 1953.[48] United Kingdom (1952, Monte Bello Islands), France (1960, Algeria), and China (1964, Lop Nur) followed, creating five nuclear states by the mid-1960s with arsenals peaking at 70,000 warheads in the 1980s.[49] Civilian efforts repurposed wartime designs for power. Experimental Breeder Reactor-I (EBR-I) in Idaho produced the first fission-generated electricity on December 20, 1951, lighting four 200-watt bulbs in a sodium-cooled fast reactor with enriched uranium.[50] Eisenhower's 1953 "Atoms for Peace" speech promoted peaceful sharing, culminating in the 1955 Geneva Conference and the International Atomic Energy Agency (IAEA) in 1957 for safeguards.[51] This accelerated builds: the U.S. Shippingport Atomic Power Station, a 60-megawatt pressurized water reactor, joined the grid on December 2, 1957; by 1970, over 100 reactors supplied 1% of global electricity, including naval uses like the USS Nautilus submarine (1954).[48] Dual-use risks surfaced, with IAEA-monitored facilities enabling tests by India (1974) and Pakistan (1998), highlighting fission's scalable dual nature.[52]

Natural and Ancient Fission Occurrences

Natural spontaneous fission occurs in heavy nuclei like uranium isotopes and transuranic elements, splitting into lighter fragments and releasing neutrons and energy without external input.[53] Beyond thorium, this process competes with alpha decay but features half-lives of 10^15 to 10^17 years (e.g., uranium-238), rendering it negligible for energy release, chain reactions, or significant background radiation contributions.[54][55] The only verified self-sustaining natural chain reactions happened in the Oklo uranium deposit, Gabon, Africa, about 1.7 billion years ago during the Paleoproterozoic.[56] At least 15 reactor zones in the Franceville Basin operated intermittently for hundreds of thousands to millions of years, enabled by then-higher uranium-235 abundance (~3% versus today's 0.72%), owing to its shorter half-life relative to uranium-238.[57][58] Criticality arose from uranium concentrations over 50% in sandstone aquifers, where groundwater moderated neutrons for thermal fission of uranium-235, aided by deposit geometry as reflectors.[59] Each zone averaged ~100 kilowatts, boiling away water to pause reactions until reflooding restarted them in pulses.[56] Supporting evidence includes uranium-235 depletion to 0.1-0.4%, fission product signatures (e.g., xenon-135 ratios matching thermal uranium-235 yields), and contained remnants over geological time.[60][61] No other terrestrial natural reactors exist, as declining uranium-235 levels and isotopic separations prevent repetition without enrichment or moderators like heavy water.[57] Proposals for deep-Earth or extraterrestrial fission lack Oklo-level geochemical validation.[62] These events highlight the rare geochemical conditions needed for fission chains in natural uranium deposits.[63]

Applications in Energy Production

Principles of Nuclear Reactors

Nuclear reactors sustain controlled fission chain reactions in fissile isotopes such as uranium-235 or plutonium-239. Incoming neutrons split atomic nuclei, releasing about 200 MeV per event—mostly as kinetic energy of fission fragments—plus additional neutrons to propagate the reaction.[7][64] In power plants, a neutron absorbed by a uranium-235 nucleus induces fission, yielding two smaller nuclei, heat, and more neutrons. These sustain a controlled chain reaction, heating a coolant that produces steam to drive turbines and generate electricity. This maintains steady output under precise neutron flux management, avoiding exponential growth seen in weapons.[65][66] The effective neutron multiplication factor keffk_{eff} defines behavior: subcritical (keff<1k_{eff} < 1) for decaying power, critical (keff=1k_{eff} = 1) for steady operation, and supercritical (keff>1k_{eff} > 1) for increasing power. Steady states balance keffk_{eff} at unity, adjusting for losses from absorption, leakage, or non-fission captures.[66][27][64] Fission neutrons, emitted at ~2 MeV, are typically moderated to thermal speeds (<0.025 eV) in commercial designs to boost uranium-235 fission cross-sections, which favor slow neutrons. Moderators include light water, heavy water, or graphite; fast-spectrum reactors skip moderation for fuel breeding.[64][65] Core components feature enriched uranium dioxide fuel pellets in zirconium alloy cladding for neutron efficiency; control rods of boron carbide or hafnium to adjust reactivity; and a coolant loop—often pressurized water, boiling water, gas, or liquid metal—that removes heat and may moderate in light-water types. The vessel houses the core under pressure, with sensors tracking flux, temperature, and pressure for automatic shutdowns via safety rods. Negative temperature coefficients enhance stability by reducing reactivity as heat rises. Fuel burnup depletes fissile material and builds products, requiring refueling every 1-2 years, with 3-5% uranium fissioned in typical light-water reactors.[65][67]

Fission-Based Power Generation Technologies

Fission-based power generation harnesses heat from controlled nuclear fission chain reactions to produce steam that drives turbines for electricity. As of late 2024, about 440 operable reactors worldwide provide 398 GWe capacity at an 83% average capacity factor, supporting reliable baseload power.[68] Most use thermal-neutron reactors with enriched uranium fuel, moderated and cooled by water, heavy water, or gas; fast-neutron designs serve advanced needs.[65] Light-water reactors (LWRs), using ordinary water as moderator and coolant, dominate with over 80% of units. Pressurized water reactors (PWRs)—the most common, at roughly 300 units—keep primary coolant at high pressure (15 MPa) to avoid boiling, transferring heat via steam generators to a secondary loop for turbine steam. This separation boosts safety by isolating radioactive coolant. Operational since the 1950s, modern PWRs add passive safety features.[65] [69] Boiling water reactors (BWRs), about 60 units, boil coolant in the core and separate steam-water mixtures before turbines, simplifying design but demanding strong containment against releases. BWRs make up 15-20% of capacity, with enhancements in fuel efficiency and debris resistance.[70] [71] Heavy-water reactors, like Canada's CANDU design, use deuterium oxide for moderation and cooling, allowing unenriched natural uranium fuel and online refueling. About 50 units, mainly in Canada and exports, offer fuel flexibility (including thorium) and contribute 7-10% of global nuclear output since the 1970s.[72] [73] Gas-cooled reactors, such as the UK's Advanced Gas-cooled Reactors (AGRs), use carbon dioxide coolant and graphite moderator with enriched uranium oxide fuel for higher efficiency (up to 41%). Evolving from Magnox designs, 14 AGR units supply about 10% of UK electricity, facing decommissioning from the 2020s.[74] Fast breeder reactors (FBRs) and Generation IV systems advance fuel use and waste reduction. FBRs employ fast neutrons to breed fissile material (e.g., plutonium-239 from uranium-238), using liquid-metal coolants like sodium for high power density; Russia's BN-800 operates commercially, though economics limit adoption.[75] Generation IV concepts—such as sodium-cooled fast reactors, molten salt reactors, and high-temperature gas reactors—prioritize safety, proliferation resistance, and closed fuel cycles, with demonstrations eyed for the 2030s via the Generation IV International Forum.[76] [77]

Applications in Weapons

Physics of Fission Bombs

Fission bombs, also known as atomic bombs, exploit rapid, uncontrolled nuclear fission chain reactions to release enormous energy quickly. The core physics requires assembling a supercritical mass of fissile material, such as uranium-235 or plutonium-239, where the effective neutron multiplication factor k>1k > 1, causing exponential growth in the neutron population from prompt neutrons.[27] In this state, each fission produces more than one neutron capable of inducing subsequent fissions before explosive expansion disassembles the assembly. Critical mass, the minimum fissile quantity for a self-sustaining reaction under given shape, density, purity, and neutron reflection conditions, is about 52 kilograms for a bare sphere of highly enriched uranium-235, though reflectors like beryllium or uranium significantly reduce it.[78] The reaction achieves prompt criticality when the prompt neutron factor kp>1k_p > 1, ignoring delayed neutrons too slow for explosive yields; neutron generations occur every few nanoseconds, with energy release dominated by fission fragment kinetic energy.[79] Two designs attain supercriticality: gun-type and implosion-type. Gun-type, viable for uranium-235's low spontaneous fission rate, uses conventional explosives to propel a subcritical fissile "bullet" into a subcritical "target," assembling the mass in milliseconds to surpass criticality before predetonation.[80] It demands high uranium purity to limit neutron background, with assembly speeds of hundreds of meters per second ensuring overlap prior to expansion. Implosion-type, necessary for plutonium-239's higher spontaneous fission (e.g., from Pu-240 impurities), employs symmetric high-explosive lenses to compress a subcritical spherical pit, boosting density and halving or thirding the critical mass for supercriticality in microseconds.[81] Uniform compression is vital, often triggered by a polonium-beryllium neutron initiator at peak density, with a dense tamper providing inertia against early disassembly and reflecting neutrons inward.[81] Energy yield stems from fissioning a core fraction, each event liberating about 200 MeV—mostly fragment kinetic energy (82%), plus prompt neutrons, gamma rays, and later radiations—scaling as YfmeY \approx f \cdot m \cdot e, where ff is the fission fraction, mm the fissile mass, and ee the per-fission energy.[6] Full fission of 1 kilogram of uranium-235 or plutonium-239 equates to 17-20 kilotons of TNT, but early bombs achieved only 1-2% efficiency due to disassembly after 50-100 generations, limiting reaction time to about 10610^{-6} seconds and converting thermal energy to shock waves.[82] Boosted designs incorporate deuterium-tritium gas to elevate neutron flux, raising kk and efficiency by 2-3 times.[81]

Development and Deployment History

The United States launched fission-based nuclear weapons development via the Manhattan Project, approved by President Franklin D. Roosevelt on January 19, 1942, amid fears of German atomic progress.[43] Formally established under the U.S. Army Corps of Engineers' Manhattan Engineer District on June 18, 1942, and led by General Leslie Groves, the project appointed J. Robert Oppenheimer as scientific director of the 1943 Los Alamos Laboratory.[43] It yielded two designs: the uranium-235 gun-type Little Boy and the plutonium-239 implosion-type Fat Man.[83] The Trinity test of an implosion fission weapon occurred on July 16, 1945, at New Mexico's Alamogordo Bombing Range, producing 21 kilotons of TNT equivalent and validating the plutonium approach.[83] [84] Three weeks later, on August 6, Little Boy detonated over Hiroshima, Japan, via B-29 Enola Gay at 580 meters altitude, yielding 15 kilotons, devastating the city, and killing 70,000-80,000 instantly.[85] [45] On August 9, Fat Man exploded over Nagasaki with 21 kilotons, causing about 40,000 immediate deaths—the only combat uses of fission weapons.[45] [86] After World War II, the U.S. scaled up plutonium implosion bombs at Hanford, conducted tests like 1946's Operation Crossroads, and shifted toward thermonuclear weapons.[87] Espionage-assisted, the Soviet Union tested its first plutonium implosion device, RDS-1, on August 29, 1949, at Semipalatinsk (22 kilotons), sparking the nuclear arms race.[88] The United Kingdom detonated a 25-kiloton plutonium bomb in Operation Hurricane on October 3, 1952, off Australia's Montebello Islands.[89] Early stockpiles relied on fission designs; the U.S. built over 50,000 warheads by the 1960s, but pure fission gave way to boosted and fusion types for better yield and efficiency.[87] No subsequent combat deployments occurred, though fission primaries underpin modern thermonuclear arsenals by triggering fusion.[90]

Safety, Risks, and Mitigation

Inherent Safety Features of Fission Processes

Nuclear fission chain reactions in power reactors feature inherent physical mechanisms that provide negative reactivity feedback, stabilizing operations independently of active controls. The primary mechanism is the Doppler coefficient of reactivity, caused by broadening neutron absorption resonances in fissile isotopes like uranium-235 with rising fuel temperature. This boosts parasitic neutron capture over fission, lowering the effective multiplication factor (k_eff) and damping power excursions in milliseconds.[91][92] In light-water reactors, it ranges from -1 to -3 pcm/°C (pcm = parts per cent mille, or 10^{-5} reactivity change per °C), so fuel heating suppresses further fission.[93] The moderator temperature coefficient complements this: coolant heating induces thermal expansion and lower moderator density, reducing neutron thermalization and fission rates in thermal-spectrum reactors, with values of -10 to -50 pcm/°C in pressurized water reactors.[93][91] In water-moderated designs, a negative void coefficient adds safety; steam voids displace water, impairing moderation and cutting thermal fission probability, as in boiling water reactors with -20 to -100 pcm per percent void fraction.[94][91] Fission also self-limits via neutron-absorbing products like xenon-135, with a ~2.6 × 10^6 barn thermal neutron capture cross-section, which accumulates and poisons the chain reaction, especially post-power shifts; xenon transients can drop reactivity by several percent in hours, necessitating control rod adjustments during startups.[95] These feedbacks appear in natural reactors like Oklo (1.7 billion years ago), where heat drove out moderator water, quenching reactivity until cooling resumed, enabling pulsed operation over millennia sans containment.[96] Overall, they make supercritical excursions unlikely in subcritical setups, with test data showing power peaks capped at 2-3 times normal before damping restores balance.[95]

Major Accidents: Causes and Lessons

The most significant nuclear power plant accidents, which influenced global safety protocols, include the partial core meltdown at Three Mile Island Unit 2 (March 28, 1979), the explosion and fire at Chernobyl Unit 4 (April 26, 1986), and multiple reactor failures at Fukushima Daiichi after the Tohoku earthquake and tsunami (March 11, 2011).[94] These stemmed from design flaws, operational errors, and external hazards, causing core damage and varying radionuclide releases. No immediate radiation fatalities occurred at TMI or Fukushima, unlike Chernobyl's 31 acute radiation syndrome deaths among workers.[97][98][99] At Three Mile Island, a blocked secondary coolant system from a malfunctioning polisher led to a stuck-open pilot-operated relief valve, resulting in coolant loss and partial melting of about 50% of the fuel. Operators, hampered by misleading instrumentation and poor training, delayed addressing the issue amid alarms.[97][100] Lessons drove improvements in human-machine interfaces (e.g., direct core cooling indicators), operator simulator training, and the U.S. NRC's TMI Action Plan, which added over 160 requirements for redundant safety systems to prevent similar coolant loss events.[101][102] Chernobyl's RBMK-1000 design flaws, including a positive void coefficient, combined with procedural violations during a low-power safety test: operators disabled emergency cooling and withdrew most control rods, causing a reactivity surge, steam explosion, and graphite fire that released 5-10% of the core inventory.[103][98] Key outcomes included eliminating positive void coefficients, enforcing operational limits, and promoting a safety culture favoring caution. This spurred RBMK retrofits and closures, plus the Convention on Nuclear Safety for standardized reporting and peer reviews to avoid design-operation conflicts.[103][104] Fukushima Daiichi Units 1-3 melted down after a 9.0-magnitude earthquake cut off-site power and a 14-15-meter tsunami—exceeding the 5.7-meter design basis—flooded seawater pumps and diesel generators, causing station blackout and active cooling failure, followed by hydrogen explosions.[99][105] Lessons focused on probabilistic external hazard assessments, passive cooling via natural circulation, and enhanced emergency measures like mobile power and filtered venting. The IAEA action plan prompted global stress tests, better multi-unit risk analysis, and regulatory independence to counter underestimation of rare events.[106][107]

Radiation Exposure and Health Impacts

Nuclear fission emits prompt neutrons and gamma rays during nucleus splitting (e.g., uranium-235 or plutonium-239), with fission products like iodine-131, cesium-137, and strontium-90 decaying via beta, gamma, and alpha particles.[108] [109] These ionizing radiations damage biological tissue by ionizing atoms, directly or indirectly harming DNA via free radicals, which can cause cell death, mutation, or repair failure.[110] Effects divide into deterministic (threshold-based, such as acute radiation syndrome above 1 Sv, with nausea, hemorrhage, and death over 4-6 Sv) and stochastic (probabilistic, like cancer risk at ~5% per Sv via linear no-threshold model from high-dose extrapolations).[108] [111] No confirmed hereditary effects appear in exposed humans, including atomic bomb survivors.[112] Routine nuclear power operations yield negligible public exposure (<0.01 mSv/year near plants), far below natural background (~2.4 mSv/year from cosmic rays, radon, and terrestrial sources).[113] Workers average 0.3-1 mSv/year, under the 20 mSv limit; studies of >400,000 show no significant excess cancers, aided by shielding, monitoring, and healthy worker bias.[108] [114] Acute exposures occur mainly in accidents or weapons. Accidents demonstrate localized risks. Chernobyl (1986) exposed 134 workers to 0.7-13.4 Sv, causing 28 acute radiation syndrome deaths; public saw ~6,000 thyroid cancer cases in youth from iodine-131, with ~15 deaths, but no excess leukemia or solid cancers beyond models, and psychological harm outpaced direct effects.[115] [116] Fukushima (2011) had no radiation deaths; public doses averaged <10 mSv, with no expected cancer rises per UNSCEAR, though evacuation caused ~2,300 non-radiation fatalities.[117] [118] Fission weapons produce intense prompt doses. Hiroshima-Nagasaki survivors (~120,000 in Life Span Study, >100 mSv) faced higher leukemia (peaking 5-10 years post) and solid cancers (after 10-20 years), with ~0.5% excess relative risk per 10 mSv under LNT; effects emerged above ~100 mSv, with cataracts at higher acute levels.[119] [120] Data from these and workers suggest dose-rate matters: chronic low exposures (e.g., reactors) risk less than acute highs, questioning LNT for low doses.[108]
Exposure SourceTypical Effective Dose (mSv/year)Health Risk Context
Natural Background (global average)2.4Baseline; no excess cancer attributable
Nuclear Plant Public Vicinity<0.01Negligible compared to background
Nuclear Workers (average)0.3-1No clear excess cancers; below detection threshold
Medical Imaging (e.g., CT scan, one-time)10Equivalent to 3-4 years background; justified by benefits
Chernobyl Liquidators (>0.7 Sv acute)Acute: up to 13.4 Sv28 ARS deaths; thyroid effects
Hiroshima/Nagasaki (>100 mSv)Acute: variable, up to SvLeukemia/solid cancers elevated
Fission exposures add little to global health burdens; energy benefits surpass risks relative to fossil fuel air pollution (~8 million deaths/year).[108] Media often amplifies beyond empirical evidence, as UNSCEAR stresses data over speculation.[115]

Environmental and Economic Dimensions

Energy Density and Low-Carbon Benefits

Nuclear fission releases energy by converting a small fraction of nuclear mass into energy via E=mc², yielding about 200 MeV per uranium-235 fission, mostly as fission fragment kinetic energy.[121] Fission of 1 kg of uranium-235 produces roughly 8 × 10^{13} joules, or 24 million kWh of thermal energy—equivalent to burning 3 million kg of coal or 2 million kg of oil.[122] [123] This confers an energy density over a million times greater than fossil fuels by mass. A single 7-gram uranium pellet matches the output of 1 metric ton of coal, 550 liters of oil, or 17,000 cubic feet of natural gas.[124] High density reduces material needs for mining, processing, and transport, cutting environmental impacts relative to bulkier hydrocarbon fuels.[125] Nuclear's efficiency supports high-capacity, dispatchable electricity generation with low land use: a 1 GW plant requires far less fuel than equivalent coal or gas facilities and occupies less area than intermittent renewables scaled to match output.[126] Lifecycle greenhouse gas emissions stand at 5–12 g CO₂-equivalent per kWh, arising chiefly from uranium mining, enrichment, and plant construction rather than zero-emission operations.[127] [128]
Electricity SourceLifecycle GHG Emissions (g CO₂eq/kWh)
Nuclear12
Onshore Wind11
Solar PV41
Natural Gas490
Coal820 [128][127]
Nuclear emissions match onshore wind and trail solar PV, while dwarfing those of natural gas and coal; variability reflects fuel cycle assumptions. Over five decades, global nuclear output has averted about 70 Gt of CO₂ versus coal displacement.[129] Unlike combustion-based sources, fission delivers reliable baseload power without direct emissions, bolstering decarbonization amid renewables' intermittency—as in France, where nuclear reliance yields per capita emissions one-third of Germany's despite comparable industrialization.[127]

Nuclear Waste Management and Long-Term Storage

Nuclear waste from fission reactors includes spent fuel assemblies, classified as high-level waste (HLW) that forms about 3% of total volume but over 95% of radioactivity, alongside lower-level wastes from operations and decommissioning—demanding isolation due to heat and intense radiation.[130] In 2019, nuclear power generated 2657 TWh of electricity, yielding minimal HLW—roughly 34 grams per person annually if meeting all needs—versus millions of tonnes of often more radioactive ash from coal plants due to concentrated uranium and thorium decay products.[130][131][132] Spent fuel cools in water pools for 2–5 years to reduce decay heat from short-lived fission products, then shifts to dry cask storage in ventilated concrete or steel containers for decades-long interim above-ground holding, with IAEA verifying containment and integrity beyond 100 years.[133] Reprocessing in France and Russia recovers over 95% of uranium and plutonium for reuse, shrinking HLW to vitrified glass while uneconomic political bans limit it in the US despite feasibility.[134] Radioactivity decays exponentially: HLW heat falls tenfold after 50 years for easier handling, most gamma emitters fade within 300 years, and alpha-emitting actinides persist, requiring millennial containment.[133][135] For long-term isolation, deep geological repositories embed waste in stable formations 200–1000 meters underground, exploiting low permeability and scant groundwater flow. Finland's Onkalo, in 1.8-billion-year-old crystalline bedrock at 430 meters, nears 2025 operation for 6500 metric tons of spent fuel via multi-barrier copper canisters and bentonite buffers against radionuclide escape.[136] The US Waste Isolation Pilot Plant (WIPP), running since 1999 in salt beds, manages transuranic defense waste without verified releases, even post-2014 incident.[137] In contrast, US civilian spent fuel awaits a federal site after Yucca Mountain stalled politically, drawing 2024 DOE criticism for program shortfalls, yet experts affirm geological disposal's safety for over 100,000-year HLW containment.[138][139] IAEA standards support this, classifying 95% of global waste as low-level for near-surface disposal, with HLW risks contained far below those of unmanaged fossil wastes.[140]

Cost Structures and Comparative Economics

Nuclear power plants feature high upfront capital costs, typically 60-70% of lifetime generation expenses, due to complex engineering, safety regulations, and 5-10 year construction periods. Fuel costs for enriched uranium are low, about 20% of lifetime costs or 0.5-1 cent per kilowatt-hour, thanks to nuclear fuel's high energy density—a ton of uranium equals millions of tons of coal or oil. Operating and maintenance expenses, covering labor, refueling, and waste, make up the rest, with variable O&M plus fuel at $9-16 per megawatt-hour. Decommissioning, 9-15% of capital or $500 million to $1 billion for a 1.4 gigawatt plant, uses dedicated funds to avoid end-of-life burdens.[125][141][142][143] Western light-water reactor projects often face overruns and delays, doubling estimates from regulatory shifts, supply chain issues, labor declines, and first-of-a-kind challenges. Vogtle Units 3 and 4 in Georgia, USA, added $17 billion and seven years, reaching over $30 billion for two gigawatt reactors by 2023-2024. The V.C. Summer project in South Carolina wasted $8 billion by 2017. Standardized designs in South Korea and China, however, yield $2,000-3,000 per kilowatt overnight costs versus $6,000-10,000 in the US and Europe, showing benefits of learning and stable policy.[144][145][146] Nuclear's unsubsidized levelized cost of electricity (LCOE) is $70-90 per megawatt-hour for new builds in good conditions, matching combined-cycle natural gas ($40-60/MWh) and coal ($60-140/MWh) amid fuel volatility but exceeding solar ($25-50/MWh) or onshore wind ($25-75/MWh) alone. Yet nuclear's 90%+ capacity factor, dispatchability, and lack of weather reliance offset this, avoiding renewables' storage and grid costs that can raise effective LCOE by 50-100%. Full lifecycle analyses show nuclear's baseload reliability and low marginal costs yielding savings, like 44% in Australian models. Small modular reactors (SMRs) could cut capital costs to $3,000-5,000 per kilowatt via factory production, pending validation.[147][148][149][125]

Controversies and Debates

Proliferation and Security Risks

Nuclear fission technologies like uranium enrichment and plutonium reprocessing carry proliferation risks from their dual-use nature, supporting both civilian energy and weapons. Civilian programs can yield fissile materials such as highly enriched uranium (HEU) or weapons-grade plutonium—needing only 25-50 kg of HEU or 4-8 kg of plutonium for a basic implosion device. North Korea exploited this via its Yongbyon reactor, producing plutonium for arms under peaceful research cover before NPT withdrawal in 2003. Iran's enrichment sites, declared civilian, have similarly fueled fears of diversion to over 90% U-235 purity.[150][151] The NPT, opened in 1968 and effective March 5, 1970, binds 191 parties as of 2023: non-nuclear-weapon states forgo arms for peaceful nuclear technology access, while nuclear-weapon states seek disarmament. Proliferation evades this—India, Pakistan, and Israel built arsenals sans membership; North Korea tested post-2003 exit. IAEA safeguards deploy over 275 inspectors across 190 states for inspections, surveillance, and accounting, blocking verified declared-material diversions since 1970. Clandestine risks linger, as in Iraq's 1991 exposures, with efficacy tied to full pacts but gaps in non-NPT nations like India.[152][153][151] Non-state threats include fissile theft for improvised nuclear devices or "dirty bombs." IAEA's ITDB logged ~2,800 trafficking cases of nuclear/radioactive materials from 1993-2022, mainly low-threat sources like cesium-137, but post-1991 Soviet collapse HEU thefts from Russia—several kilograms—expose storage/transport flaws over weapons-usable fissile material. Nuclear terrorism endures, with Al-Qaeda-like groups eyeing 10-20 kg HEU for city-scale blasts. Countermeasures feature IAEA protection norms (guards, detection), global excess HEU repatriation exceeding 6,000 kg since 2005, and Megaports cargo scans covering 10% worldwide. Insider/cyber sabotage risks continue, per 2020 Nuclear Threat Initiative Index on 22 nations securing ≥1 kg plutonium/HEU.[154][155]

Public Opposition and Misinformation

Public opposition to nuclear power arose in the mid-20th century, initially tied to anti-nuclear weapons activism before focusing on civilian risks amid environmental worries and major accidents. The 1979 Three Mile Island partial meltdown in Pennsylvania released minimal radiation with no attributable deaths, yet intense media coverage framed it as a near-disaster, slashing U.S. support for new plants from 70% in the 1970s to about 50% by the early 1980s.[156][157] The 1986 Chernobyl disaster in the Soviet Union, stemming from flawed RBMK reactor design and operator errors, caused 31 immediate deaths and an estimated 4,000 long-term cancer fatalities per United Nations assessments—intensifying global fears despite its unrepresentative vulnerabilities compared to Western designs.[158] The 2011 Fukushima accident, triggered by a tsunami beyond design limits, produced no direct radiation deaths but led to over 2,000 excess fatalities from evacuation stress, heightening views of inherent unreliability.[159][160] Misinformation perpetuates opposition by exaggerating risks beyond empirical safety records. Nuclear power's death rate stands at roughly 0.04 per terawatt-hour, including accidents, occupational hazards, and air pollution—far lower than coal's 24.6, oil's 18.4, solar's 0.44, or wind's 0.15 across full lifecycles.[161][162] Claims of widespread cancers from low-level radiation, amplified after Chernobyl, clash with studies showing no detectable public health upticks beyond acute cases, where psychological impacts like anxiety dominate.[163][164] Waste fears overlook spent fuel's small volume—akin to a few Olympic pools annually worldwide—and decades of incident-free storage, contrasting fossil fuel byproducts.[164] Public opinion has shifted toward acceptance, acknowledging nuclear's low-carbon benefits. U.S. polls in 2025 show 61-72% supporting expansion, up from 43% in 2020, fueled by climate needs and alternative comparisons, though fears persist among women and left-leaning groups.[165][166][167] Globally, support averages 46% against 23% opposition in major economies, highlighting a perception-safety gap that transparency and data could close further.[168][169]

Comparative Risks Versus Alternative Energy Sources

Nuclear power has one of the lowest lifecycle mortality rates among energy sources, at 0.03 deaths per terawatt-hour (TWh), covering construction, operation, accidents, and decommissioning. This includes historical accidents like Chernobyl (433 deaths, including long-term cancers) and Fukushima (2,314 mainly from evacuation stress, not radiation), plus occupational risks in uranium mining comparable to other sectors but regulated.[170][162] Fossil fuels pose higher risks from chronic air pollution. Coal causes 24.6 deaths per TWh via particulate matter, sulfur dioxide, and nitrogen oxides leading to respiratory and cardiovascular diseases; the World Health Organization attributes over 8 million annual premature deaths globally to fossil pollution, mostly coal. Oil follows at 18.4 deaths per TWh, natural gas at 2.8, including methane-related climate impacts. Routine emissions from a single coal plant often exceed direct deaths from all civilian nuclear accidents worldwide (under 100).[170] Renewables generally have low risks but exceed nuclear in some full-lifecycle metrics. Rooftop solar incurs 0.44 deaths per TWh from installation falls and manufacturing hazards, though utility-scale solar nears 0.02; wind at 0.04 includes turbine maintenance accidents and bird/bat collisions. Hydropower at 1.3 reflects dam failures like China's 1975 Banqiao disaster (171,000 deaths) and reservoir drowning/malaria risks. Lifecycle analyses highlight nuclear's edge, as renewables demand extensive mining for rare earths and copper, introducing toxicities absent in nuclear's contained fuel cycle.[170][162]
Energy SourceDeaths per TWh (accidents + pollution + occupational)
Coal24.6 [170]
Oil18.4 [170]
Natural Gas2.8 [170]
Hydropower1.3 [170]
Solar (rooftop)0.44 [170]
Wind0.04 [170]
Nuclear0.03 [170]
Modern reactors feature passive cooling and fail-safe designs, with core meltdown probabilities below 1 in 10,000 reactor-years, contrasting fossil fuels' ongoing diffuse exposures. Public perception magnifies nuclear risks despite evidence, as Fukushima evacuation deaths far outnumbered radiation effects, while coal's toll continues in developing regions. Empirical data affirm nuclear fission's superior safety per energy unit compared to combustion-based or large-scale infrastructure alternatives.[162][171]

Recent Advances and Future Outlook

Advanced Reactor Designs

Generation IV (Gen IV) reactors improve on prior designs in fuel efficiency, waste reduction, passive safety, and economics. Many use fast neutron spectra for closed fuel cycles, breeding fissile material from uranium-238 to extend resources 60-fold over light-water cycles. Inherent safety arises from low-pressure coolants avoiding steam explosions and high-boiling coolants preventing meltdowns.[77][172] Sodium-cooled fast reactors (SFRs) employ liquid sodium for unmoderated fast fission, enabling breeding and transmutation of actinides to cut high-level waste by 90%. Low neutron absorption and high heat transfer yield 550°C outlets and over 40% efficiency, versus 33% in light-water reactors. Russia's BN-600 (since 1980) and BN-800 (since 2016) confirm reliability, despite sodium's reactivity with water and air requiring containment. The U.S. TerraPower Natrium (345 MWe) integrates molten salt storage for load-following, with construction starting in 2024 and operation by 2030.[173][75][174] Lead-cooled fast reactors (LFRs) use liquid lead or lead-bismuth eutectic, with boiling points over 1700°C enabling passive cooling and avoiding boiling. This supports breeding ratios above 1.0 for sustainable cycles and plutonium burning, with less corrosion than sodium. Westinghouse pursues modular designs for lower capital costs via factory assembly; Europe's ALFRED demonstrator advances thermal-hydraulics research for flow stability.[175][176][177] Molten salt reactors (MSRs) dissolve fissile material in fluoride or chloride salts acting as both fuel and coolant, allowing online reprocessing for burnups over 20% without cladding failures. Atmospheric pressure and stability to 1400°C provide negative temperature coefficients and drainable fuel for meltdown resistance. Thorium variants enable breeding with lower waste toxicity. Russia nears prototype design completion, China targets a 10 MW thorium MSR by 2025, and U.S. firm Kairos Power aims for fluoride-salt-cooled units in the early 2030s.[178][179][180] High-temperature gas-cooled reactors (HTGRs), including very high-temperature variants, use helium coolant and TRISO-coated fuel in graphite to retain fission products at 1600°C, supporting 1000°C cores for over 50% efficiency or hydrogen cogeneration. Inert helium avoids activation and corrosion; negative void coefficients ensure stability. Japan's HTTR achieved criticality in 1998, China's HTR-PM connected to grid in 2021 (210 MWe), and X-energy's Xe-100 seeks U.S. licensing for scalable 80 MWe modules up to 320 MWe plants.[181][182][183] Gas-cooled fast reactors (GFRs) and supercritical water-cooled reactors (SCWRs) remain in early research, targeting high efficiencies but facing materials issues. Prototypes validate principles, yet commercialization depends on fuel cycle and regulatory advances; none deploy widely as of 2025.[77][172]

Small Modular Reactors and Scalable Deployment

Small modular reactors (SMRs) are advanced nuclear fission reactors with power outputs up to 300 megawatts electric (MWe), designed for factory fabrication and modular assembly to enable scalable deployment.[184] Unlike traditional large-scale reactors, this allows serial production, site transportation, and incremental additions to match electricity demand, reducing financial risk via phased investment.[185] SMRs incorporate passive safety features and compact designs, enabling siting at remote industrial sites or areas with limited grid infrastructure unsuitable for gigawatt-scale plants.[186] SMR modularity aids scalable deployment through factory-based manufacturing, improving quality control and enabling cost reductions from serial production learning curves, in contrast to the delays and overruns of bespoke construction for conventional reactors.[187] Proponents highlight rapid scaling potential: module clusters can achieve large-plant capacities, with operators generating revenue from initial units before completing builds.[188] SMRs offer flexibility for baseload support with renewables, or powering data centers and desalination plants, without full multi-billion-dollar upfront commitments. As of 2025, NuScale Power's VOYGR led regulatory progress with U.S. Nuclear Regulatory Commission (NRC) approval for a 77 MWe design in May, targeting 2030 deployment.[189] In September, the Tennessee Valley Authority (TVA) and ENTRA1 Energy announced a 6-gigawatt NuScale-based program across sites, one of the largest commitments.[190] The global SMR market grew from $270 million in 2024 to $670 million in 2025, driven by low-carbon demand, though most projects remain pre-construction with late-2020s operations expected.[191] Over 80 designs advance per the OECD Nuclear Energy Agency, with initial builds this decade and 2030s rollout depending on supply chains.[192] Scalable deployment faces hurdles: higher per-megawatt costs from limited scale economies and unproven serial benefits, raising levelized costs without high-volume output.[193] Licensing adaptations for multi-module sites and novel fuels prolong timelines, as in NuScale's Romanian project delayed to 2027.[194][195] Supply chain limits on components and labor, plus competition from unsubsidized fossil fuels or renewables, complicate scaling. The Union of Concerned Scientists urges full-scale safety testing before rapid rollout to address risks and cost uncertainties.[196] Policy incentives in the U.S. and Europe, including streamlined approvals and demonstration funding, could mitigate barriers.[197]

Global Expansion and Policy Shifts

Nuclear power capacity has expanded unevenly worldwide, with Asia leading growth amid energy security and decarbonization pressures intensified by the 2022 Russian invasion of Ukraine. As of late 2024, 417 reactors operated globally, providing 377 gigawatts electric (GW(e)) and generating a record 2,667 terawatt-hours (TWh), surpassing the prior peak from 2026.[198] [199] Roughly 70 reactors are under construction—over half in China, India, and Russia—while 110 more are planned, mostly in Asia.[200] China dominates with 30 under construction and capacity growth 15 times the United States since 2000, meeting surging demand.[201] [202] Western progress has been slower yet shows revival. The United States leads with 94 reactors and 97 GW, despite limited recent additions; India operates 23 while building six for industrial needs.[203] The United Arab Emirates finished its Barakah plant's last unit in 2024, launching the Arab world's first nuclear facility through South Korean transfer.[204] Europe contrasts sharply: France derives 70% of electricity from 56 reactors, while Germany ended its phase-out in 2023, overlooking nuclear's lower incident rates than coal.[203] [205] Post-2022 policy shifts address fossil fuel vulnerabilities and net-zero aims, reversing post-Fukushima reluctance. COP28 saw 22 countries, including the US, France, and Japan, pledge to triple capacity by 2050, with over 100 nations' indirect support.[206] More than 40 countries now advance expansion via incentives and reforms, lifting moratoriums in Serbia (November 2024) and others.[207] [208] US 2025 measures seek fourfold growth by 2050 through faster licensing and Inflation Reduction Act credits.[209] The International Energy Agency projects record 2025 output from these policies and Japanese restarts, emphasizing nuclear's energy density and reliable baseload despite uranium supply challenges.[210] [211]

References

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