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Alpha decay
Alpha decay
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Alpha decay or α-decay is a type of radioactive decay in which an atomic nucleus emits an alpha particle (helium nucleus). The parent nucleus transforms or "decays" into a daughter product, with a mass number that is reduced by four and an atomic number that is reduced by two. An alpha particle is identical to the nucleus of a helium-4 atom, which consists of two protons and two neutrons. For example, uranium-238 undergoes alpha decay to form thorium-234.

While alpha particles have a charge +2 e, this is not usually shown because a nuclear equation describes a nuclear reaction without considering the electrons – a convention that does not imply that the nuclei necessarily occur in neutral atoms.

Alpha decay typically occurs in the heaviest nuclides. Theoretically, it can occur only in nuclei somewhat heavier than nickel (element 28), where the overall binding energy per nucleon is no longer a maximum and the nuclides are therefore unstable toward spontaneous fission-type processes. In practice, this mode of decay has only been observed in nuclides considerably heavier than nickel, with the lightest known alpha emitter being the second lightest isotope of antimony, 104Sb.[1] Exceptionally, however, beryllium-8 decays to two alpha particles.

Alpha decay is by far the most common form of cluster decay, where the parent atom ejects a defined daughter collection of nucleons, leaving another defined product behind. It is the most common form because of the combined extremely high nuclear binding energy and relatively small mass of the alpha particle. Like other cluster decays, alpha decay is fundamentally a quantum tunneling process. Unlike beta decay, it is governed by the interplay between both the strong nuclear force and the electromagnetic force.

Alpha particles have a typical kinetic energy of 5 MeV (or ≈ 0.13% of their total energy, 110 TJ/kg) and have a speed of about 15,000,000 m/s, or 5% of the speed of light. There is surprisingly small variation around this energy, due to the strong dependence of the half-life of this process on the energy produced. Because of their relatively large mass, the electric charge of +2 e and relatively low velocity, alpha particles are very likely to interact with other atoms and lose their energy, and their forward motion can be stopped by a few centimeters of air.

Approximately 99% of the helium produced on Earth is the result of the alpha decay of underground deposits of minerals containing uranium or thorium. The helium is brought to the surface as a by-product of natural gas production.

History

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Alpha particles were first described in the investigations of radioactivity by Ernest Rutherford in 1899, and by 1907 they were identified as He2+ ions. By 1928, George Gamow had solved the theory of alpha decay via tunneling. The alpha particle is trapped inside the nucleus by an attractive nuclear potential well and a repulsive electromagnetic potential barrier. Classically, it is forbidden to escape, but according to the (then) newly discovered principles of quantum mechanics, it has a tiny (but non-zero) probability of "tunneling" through the barrier and appearing on the other side to escape the nucleus. Gamow solved a model potential for the nucleus and derived, from first principles, a relationship between the half-life of the decay, and the energy of the emission, which had been previously discovered empirically and was known as the Geiger–Nuttall law.[2]

Mechanism

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The nuclear force holding an atomic nucleus together is very strong, in general much stronger than the repulsive electromagnetic forces between the protons. However, the nuclear force is also short-range, dropping quickly in strength beyond about 3 femtometers, while the electromagnetic force has an unlimited range. The strength of the attractive nuclear force keeping a nucleus together is thus proportional to the number of the nucleons, but the total disruptive electromagnetic force of proton-proton repulsion trying to break the nucleus apart is roughly proportional to the square of its atomic number. A nucleus with 210 or more nucleons is so large that the strong nuclear force holding it together can just barely counterbalance the electromagnetic repulsion between the protons it contains. Alpha decay occurs in such nuclei as a means of increasing stability by reducing size.[3]

One curiosity is why alpha particles, helium nuclei, should be preferentially emitted as opposed to other particles like a single proton or neutron or other atomic nuclei.[note 1] Part of the reason is the high binding energy of the alpha particle, which means that its mass is less than the sum of the masses of two free protons and two free neutrons. This increases the disintegration energy. Computing the total disintegration energy given by the equation where mi is the initial mass of the nucleus, mf is the mass of the nucleus after particle emission, and mp is the mass of the emitted (alpha-)particle, one finds that in certain cases it is positive and so alpha particle emission is possible, whereas other decay modes would require energy to be added. For example, performing the calculation for uranium-232 shows that alpha particle emission releases 5.4 MeV of energy, while a single proton emission would require 6.1 MeV. Most of the disintegration energy becomes the kinetic energy of the alpha particle, although to fulfill conservation of momentum, part of the energy goes to the recoil of the nucleus itself (see atomic recoil). However, since the mass numbers of most alpha-emitting radioisotopes exceed 210, far greater than the mass number of the alpha particle (4), the fraction of the energy going to the recoil of the nucleus is generally quite small, less than 2%.[3] Nevertheless, the recoil energy (on the scale of keV) is still much larger than the strength of chemical bonds (on the scale of eV), so the daughter nuclide will break away from the chemical environment the parent was in. The energies and ratios of the alpha particles can be used to identify the radioactive parent via alpha spectrometry.

These disintegration energies, however, are substantially smaller than the repulsive potential barrier created by the interplay between the strong nuclear and the electromagnetic force, which prevents the alpha particle from escaping. The energy needed to bring an alpha particle from infinity to a point near the nucleus just outside the range of the nuclear force's influence is generally in the range of about 25 MeV. An alpha particle within the nucleus can be thought of as being inside a potential barrier whose walls are 25 MeV above the potential at infinity. However, decay alpha particles only have energies of around 4 to 9 MeV above the potential at infinity, far less than the energy needed to overcome the barrier and escape.

Quantum tunneling

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Quantum mechanics, however, allows the alpha particle to escape via quantum tunneling. The quantum tunneling theory of alpha decay, independently developed by George Gamow[4] and by Ronald Wilfred Gurney and Edward Condon in 1928,[5] was hailed as a very striking confirmation of quantum theory. Essentially, the alpha particle escapes from the nucleus not by acquiring enough energy to pass over the wall confining it, but by tunneling through the wall. Gurney and Condon made the following observation in their paper on it:

It has hitherto been necessary to postulate some special arbitrary "instability" of the nucleus, but in the following note, it is pointed out that disintegration is a natural consequence of the laws of quantum mechanics without any special hypothesis... Much has been written of the explosive violence with which the α-particle is hurled from its place in the nucleus. But from the process pictured above, one would rather say that the α-particle almost slips away unnoticed.[5]

The theory supposes that the alpha particle can be considered an independent particle within a nucleus, that is in constant motion but held within the nucleus by strong interaction. At each collision with the repulsive potential barrier of the electromagnetic force, there is a small non-zero probability that it will tunnel its way out. An alpha particle with a speed of 1.5×107 m/s within a nuclear diameter of approximately 10−14 m will collide with the barrier more than 1021 times per second. However, if the probability of escape at each collision is very small, the half-life of the radioisotope will be very long, since it is the time required for the total probability of escape to reach 50%. As an extreme example, the half-life of the isotope bismuth-209 is 2.01×1019 years.

The isotopes in beta-decay stable isobars that are also stable with regards to double beta decay with mass number A = 5, A = 8, 143 ≤ A ≤ 155, 160 ≤ A ≤ 162, and A ≥ 165 are theorized to undergo alpha decay. All other mass numbers (isobars) have exactly one theoretically stable nuclide. Those with mass 5 decay to helium-4 and a proton or a neutron, and those with mass 8 decay to two helium-4 nuclei; their half-lives (helium-5, lithium-5, and beryllium-8) are very short, unlike the half-lives for all other such nuclides with A ≤ 209, which are very long. (Such nuclides with A ≤ 209 are primordial nuclides except 146Sm.)[6]

Working out the details of the theory leads to an equation relating the half-life of a radioisotope to the decay energy of its alpha particles, a theoretical derivation of the empirical Geiger–Nuttall law.

Uses

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Alpha emitters are used in smoke detectors. The alpha particles ionize air in an open ion chamber and a small current flows through the ionized air. Smoke particles from the fire that enter the chamber reduce the current, triggering the smoke detector's alarm.[7]

Radium-223 is also an alpha emitter. Its use has been trialed and saw successful results in treating bone metastasis resulting from Castration-resistant metastatic prostate cancer.[8]

Alpha decay can provide a safe power source for radioisotope thermoelectric generators used for space probes[9] and were used for artificial heart pacemakers.[10] Alpha decay is much more easily shielded against than other forms of radioactive decay.[11]

Static eliminators typically use polonium-210, an alpha emitter, to ionize the air, allowing the "static cling" to dissipate more rapidly.[citation needed]

Toxicity

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Highly charged and heavy, alpha particles lose their several MeV of energy within a small volume of material, along with a very short mean free path. This increases the chance of double-strand breaks to the DNA in cases of internal contamination, when ingested, inhaled, injected or introduced through the skin. Otherwise, touching an alpha source is typically not harmful, as alpha particles are effectively shielded by a few centimeters of air, a piece of paper, or the thin layer of dead skin cells that make up the epidermis; however, many alpha sources are also accompanied by beta-emitting radio daughters, and both are often accompanied by gamma photon emission.[citation needed]

Relative biological effectiveness (RBE) quantifies the ability of radiation to cause certain biological effects, notably either cancer or cell-death, for equivalent radiation exposure. Alpha radiation has a high linear energy transfer (LET) coefficient, which is about one ionization of a molecule/atom for every angstrom of travel by the alpha particle. The RBE has been set at the value of 20 for alpha radiation by various government regulations. The RBE is set at 10 for neutron irradiation, and at 1 for beta radiation and ionizing photons.

However, the recoil of the parent nucleus (alpha recoil) gives it a significant amount of energy, which also causes ionization damage (see ionizing radiation). This energy is roughly the weight of the alpha (Da) divided by the weight of the parent (typically about 200 Da) times the total energy of the alpha. By some estimates, this might account for most of the internal radiation damage, as the recoil nucleus is part of an atom that is much larger than an alpha particle, and causes a very dense trail of ionization; the atom is typically a heavy metal, which preferentially collect on the chromosomes. In some studies,[12] this has resulted in an RBE approaching 1,000 instead of the value used in governmental regulations.

The largest natural contributor to public radiation dose is radon, a naturally occurring, radioactive gas found in soil and rock.[13] If the gas is inhaled, some of the radon particles may attach to the inner lining of the lung. These particles continue to decay, emitting alpha particles, which can damage cells in the lung tissue.[14] The death of Marie Curie at age 66 from aplastic anemia was probably caused by prolonged exposure to high doses of ionizing radiation, but it is not clear if this was due to alpha radiation or X-rays. Curie worked extensively with radium, which decays into radon,[15] along with other radioactive materials that emit beta and gamma rays. However, Curie also worked with unshielded X-ray tubes during World War I, and analysis of her skeleton during a reburial showed a relatively low level of radioisotope burden.

The Russian defector Alexander Litvinenko's 2006 murder by radiation poisoning is thought to have been carried out with polonium-210, an alpha emitter.

References

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Notes

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See also

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Alpha decay is a type of in which an unstable emits an —a nucleus consisting of two protons and two neutrons—transforming into a daughter nucleus with an reduced by two and a reduced by four, while releasing and sometimes gamma radiation. This process primarily occurs in heavy elements with atomic numbers greater than 82, such as and , providing a mechanism for these nuclei to achieve greater stability by shedding mass and reducing electrostatic repulsion within the nucleus. The discovery of alpha decay is credited to Ernest Rutherford and Frederick Soddy, who in 1902–1903 observed that thorium compounds produced a radioactive gas (later identified as radon) and demonstrated that radioactive decay involves the transmutation of elements, challenging the prevailing view of elemental immutability. Their work established alpha particles as positively charged emissions distinct from beta rays, with Rutherford later identifying them as helium nuclei in 1908 through experiments showing the particles' ability to ionize air and their deflection in magnetic fields. Early empirical observations, including the Geiger–Nuttall law formulated in 1911, revealed a relationship between the alpha particle's energy and the decay half-life, noting that higher-energy emissions correlate with shorter half-lives across isotopic chains. The underlying mechanism of alpha decay was explained in 1928 by George Gamow through quantum mechanical tunneling, where the alpha particle, pre-formed within the nucleus, overcomes the Coulomb barrier—the electrostatic repulsion between the positively charged alpha particle and daughter nucleus—despite lacking sufficient classical energy to surmount it. In this model, the decay rate depends exponentially on the Gamow factor, which integrates the tunneling probability through the barrier, quantitatively accounting for the Geiger–Nuttall law and the wide range of observed half-lives from microseconds to billions of years. The energy released, known as the Q-value, is determined by the mass difference between parent, daughter, and alpha particle, typically ranging from 2 to 9 MeV, with the alpha particle carrying away about 98% of this kinetic energy due to momentum conservation. Alpha decay plays a crucial role in nuclear physics, contributing to the stability of heavy isotopes and featuring prominently in natural decay chains like those of uranium-238 and uranium-235, which power geothermal heat and enable radiometric dating techniques. It also has practical applications in alpha-emitting radioisotopes used for cancer therapy, where the short-range, high-ionizing alpha particles target tumors with minimal damage to surrounding tissue, and in smoke detectors employing americium-241. Theoretical extensions of the Gamow model continue to refine predictions for superheavy elements and cluster decays, underscoring alpha decay's enduring significance in understanding nuclear structure and stability.

Fundamentals

Definition and Process

Alpha decay is a type of radioactive decay in which an unstable atomic nucleus spontaneously emits an alpha particle, transforming into a daughter nucleus of a different element. An alpha particle is identical to the nucleus of a helium-4 atom, consisting of two protons and two neutrons bound together. This emission reduces the atomic number of the daughter nucleus by 2 and its mass number by 4 compared to the parent nucleus. To contextualize alpha decay, note that an atom comprises a dense central nucleus made up of positively charged protons and neutral neutrons, surrounded by a cloud of negatively charged electrons; isotopes of an element share the same number of protons (defining the ) but differ in the number of neutrons (affecting the ). Alpha decay typically occurs in heavy, unstable isotopes with atomic numbers greater than 82, such as those in elements beyond lead, where the strong binding the nucleus begins to weaken relative to the electrostatic repulsion among protons. In the decay process, the parent nucleus ejects the pre-formed , resulting in a more nucleus. For instance, undergoes alpha decay to form thorium-234: 92238U90234Th+24He^{238}_{92}\mathrm{U} \to ^{234}_{90}\mathrm{Th} + ^{4}_{2}\mathrm{He} Similarly, decays to lead-206: 84210Po82206Pb+24He^{210}_{84}\mathrm{Po} \to ^{206}_{82}\mathrm{Pb} + ^{4}_{2}\mathrm{He}

Properties of Alpha Particles

Alpha particles are helium-4 nuclei, composed of two protons and two neutrons, and are emitted during alpha decay from unstable heavy atomic nuclei. They carry a positive charge of +2e, where e is the , due to the absence of electrons. The mass of an alpha particle is approximately 4 units (u), making it relatively heavy compared to other forms of such as beta particles. Typical kinetic energies of alpha particles range from 2 to 9 MeV, resulting in velocities of about 5% the (c). This high energy, combined with their large mass and charge, limits their range in matter to a few centimeters in air—for instance, a 5.5 MeV alpha particle travels approximately 4 cm in dry air at standard conditions. The short range arises from rapid energy loss through interactions with atomic electrons and nuclei. As a form of , alpha particles possess high ionizing power due to their +2 charge, which enables strong interactions with , primarily producing pairs by stripping electrons from atoms. Each interaction transfers significant energy, leading to thousands of ionizations per particle before it stops, but this also results in low compared to less massive radiations. Upon slowing down and losing kinetic energy, alpha particles capture two electrons from surrounding matter to form neutral atoms, exhibiting no further chemical reactivity in this state. This transformation underscores their identity as helium nuclei, which become stable He atoms post-emission.

Historical Development

Early Observations

The discovery of radioactivity by in 1896 laid the groundwork for subsequent investigations into its components, as he observed that salts emitted rays capable of penetrating opaque materials and fogging photographic plates, independent of external excitation. Building on this, began systematic studies of radiation in 1899 at , initially classifying emissions into penetrating (later beta) and less penetrating types based on their interactions with matter. From 1901 onward, Rutherford collaborated with , who joined him to examine and compounds, leading to the identification of alpha rays as a distinct form of radiation emanating from and . Their experiments, conducted between 1899 and 1903, demonstrated that alpha rays were positively charged particles through deflection in electric and , with scattering patterns indicating substantial compared to beta rays. These observations isolated alpha emissions as discrete, ionized particles responsible for much of the ionizing power in radioactive sources like emanation. Concurrent work by and in 1903 provided early hints of composition, as they detected gas evolving from bromide through spectroscopic analysis of the emanation spectrum, linking it to radioactive processes in uranium-derived minerals. This finding suggested a connection between alpha emissions and production, though the precise mechanism remained unclear at the time. In 1909, Rutherford and Robert B. Royds confirmed that alpha particles are doubly ionized nuclei ( ions) by trapping the particles in an evacuated tube and observing the characteristic spectrum upon recombination with electrons. Further empirical characterization came in 1911 from and John Mitchell Nuttall, who measured the ranges of alpha particles from various radioactive substances in air and established a between particle (inferred from range) and the decay constant of the parent , with higher-energy alphas associated with shorter half-lives. Their deflection and scintillation experiments confirmed the particles' charged, massive nature, reinforcing alpha rays as distinct from lighter radiations. These studies, using screens to count scintillations, quantified alpha emission rates and properties for elements like and , setting the stage for later identifications of alpha particles as nuclei.

Theoretical Advancements

The theoretical understanding of alpha decay faced significant challenges following Rutherford's 1911 proposal of the nuclear model of the atom, based on scattering experiments. This model portrayed the atom with a compact, positively charged nucleus at its center, implying a strong repulsion that would form a barrier preventing an from escaping without acquiring energies of approximately 20-30 MeV to overcome it classically. However, experimental observations revealed emitted with much lower kinetic energies, typically 4-9 MeV, highlighting the inadequacy of to explain the process. In the same year, and John Mitchell Nuttall established an empirical relationship, now known as the Geiger-Nuttall law, correlating the logarithm of the alpha decay constant with the range of the emitted particles, which indirectly relates to their energy. This law captured systematic trends across radioactive elements but remained descriptive without a underlying physical mechanism. A pivotal advancement occurred in 1928 when applied the liquid drop model—treating the nucleus as a charged liquid—to alpha decay, introducing quantum tunneling as the mechanism by which the preformed could probabilistically penetrate the despite insufficient classical energy. Gamow's approach not only predicted decay rates based on tunneling probability but also independently derived the form of the Geiger–Nuttall relation from the exponential dependence of transmission through the barrier. Concurrently, and Ronald Gurney provided a complementary explanation using wave mechanics, demonstrating how the 's extends beyond the barrier, enabling escape and aligning with observed disintegration rates. Post-1928 developments refined these ideas by integrating nuclear shell effects into the , which enhances predictions of nuclear binding energies and stability by incorporating quantum shell closures that modulate the and other terms. This inclusion accounts for variations in alpha decay favorability near , where shell structures increase resistance to decay, improving the accuracy of estimates beyond the uniform liquid drop assumptions.

Decay Mechanism

Classical Perspective

In the early , alpha decay presented a profound puzzle within the classical framework of physics. first distinguished alpha rays from and other heavy elements in 1899, later identifying them as nuclei in 1909 through an experiment with William Royds that demonstrated the formation of the spectrum. These observations revealed alpha particles emitted with discrete kinetic energies typically ranging from 4 to 9 MeV, yet offered no viable mechanism for their escape from the nucleus. The potential governing the motion of an alpha particle within and beyond the nucleus combines the short-range attractive strong nuclear force, which forms a deep potential well of approximately 30 MeV depth for heavy nuclei like uranium-235, and the long-range repulsive Coulomb interaction between the positively charged alpha particle and the daughter nucleus. This Coulomb term creates a formidable barrier whose height is on the order of VZ1Z2e2rV \approx \frac{Z_1 Z_2 e^2}{r}, where Z1=2Z_1 = 2 for the alpha particle, Z2Z_2 is the atomic number of the daughter nucleus, ee is the elementary charge, and rr is the distance near the nuclear surface (roughly 10-12 fm), yielding a barrier height of about 25-30 MeV for heavy elements with Z>82Z > 82. Classically, an alpha particle formed inside the nucleus—bound by the strong force—would lack the energy to surmount this barrier, as the available decay energy (Q-value) is only a few MeV, far below the required threshold; the particle would simply reflect repeatedly at the barrier's edge, remaining trapped indefinitely. To classically overcome such a barrier, the nucleus would need thermal excitation energies exceeding 25 MeV, corresponding to temperatures around 101110^{11} K—vastly unattainable under any natural conditions, including where thermal energies are mere 0.025 eV. Rutherford's measurements of decay rates further exacerbated the enigma, showing half-lives spanning over 20 orders of magnitude (from microseconds to billions of years) without any classical explanation for the variability or the emission process itself. Early classical-inspired models sought to address these issues through analogies to macroscopic phenomena. Early classical-inspired models, drawing on analogies to macroscopic phenomena like evaporation from excited states, struggled to explain ground-state alpha decays without invoking unrealistically high excitation energies.

Quantum Tunneling Model

In quantum mechanics, particles possess wave-like properties that enable a non-zero probability of penetrating regions where classical mechanics would prohibit passage due to insufficient energy, a phenomenon known as quantum tunneling. In the context of alpha decay, this principle resolves the classical impasse by positing that an alpha particle, preformed within the parent nucleus, can tunnel outward through the Coulomb barrier formed by the electrostatic repulsion between the positively charged alpha particle and the daughter nucleus. The alpha particle, treated as a helium-4 cluster, exists in a potential well dominated by the strong nuclear force at short distances but must surmount the long-range Coulomb potential to escape. George Gamow developed the foundational quantum tunneling model for alpha decay in 1928, calculating the transmission probability through the barrier using the . The decay probability PP is exponentially suppressed and given by Pexp(2Rrtκ(r)dr),P \approx \exp\left(-2 \int_{R}^{r_t} \kappa(r) \, dr \right), where κ(r)=2m(V(r)E)/\kappa(r) = \sqrt{2m (V(r) - E)} / \hbar
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