Beta Decay & the Neutrino

For a few uneasy years in the late 1920s, beta decay looked like the crime scene where energy conservation had been murdered. Alpha particles left a nucleus with a single, sharp energy — every alpha from a given decay carried exactly the same kick, just as a two-body split demands. Beta particles refused to behave. Electrons streamed out of a radioactive sample with every energy from nearly zero up to a fixed ceiling, a smooth continuous smear rather than the one clean line that bookkeeping required. Where had the missing energy gone? Niels Bohr, no less, was ready to sacrifice the conservation of energy itself inside the nucleus rather than explain it away. In December 1930 Wolfgang Pauli chose the other horn. In a letter addressed to "Dear Radioactive Ladies and Gentlemen," he proposed a "desperate remedy": an unseen particle, electrically neutral, nearly massless, spirited out of the nucleus alongside the electron, secretly carrying off the balance of the energy and momentum. He apologised for postulating something that might never be detected. Four years later Enrico Fermi turned the idea into a complete quantitative theory of beta decay, popularized the name neutrino — the "little neutral one" — and in doing so identified an entirely new fundamental force of nature. This article works out the two faces of beta decay, the electron-emitting β⁻ and the positron-emitting β⁺; shows exactly how the nucleus reshuffles a neutron into a proton (or the reverse) while keeping its mass number fixed; computes the released energy from atomic masses with school algebra; and shows why that innocuous continuous spectrum forced physics to invent one of the most elusive particles in the universe.

Key takeaways
  • Beta-minus (β⁻): a neutron inside the nucleus turns into a proton, emitting an electron and an electron antineutrino — n→p+e−+νˉen \to p + e^- + \bar\nu_e. The atomic number rises by one, Z→Z+1Z \to Z+1, while the mass number AA is unchanged.
  • Beta-plus (β⁺): a proton turns into a neutron, emitting a positron and a neutrino — p→n+e++νep \to n + e^+ + \nu_e. Here Z→Z−1Z \to Z-1, again with AA fixed. It needs at least 1.02 MeV1.02\ \text{MeV} of decay energy to occur.
  • The energy comes from mass: the released energy is the QQ-value, Q=Δm c2Q = \Delta m\,c^2. Using atomic masses the electron masses cancel automatically: for β⁻, Q=[M(parent)−M(daughter)]c2Q = [M(\text{parent}) - M(\text{daughter})]c^2.
  • The continuous spectrum: unlike the single-energy alpha line, beta electrons emerge with a continuous range of energies from 00 up to a sharp endpoint equal to QQ — the signature that a third, invisible particle shares the energy.
  • The neutrino: Pauli (1930) postulated it to rescue conservation of energy, momentum and spin; Fermi (1934) built the theory and popularized the name (coined by Amaldi); Cowan and Reines detected it in 1956. It is neutral, essentially massless, and interacts only through the weak force.
  • Example: carbon-14 beta-decays, 614C→ 714N+e−+νˉe^{14}_{6}\text{C} \to\ ^{14}_{7}\text{N} + e^- + \bar\nu_e, with Q=0.156 MeVQ = 0.156\ \text{MeV} — the clock behind radiocarbon dating.
  • Key idea: beta decay converts one nucleon into the other by the weak force, emitting an electron (or positron) together with a neutrino that shares the fixed decay energy QQ — which is why the beta particle's energy is continuous, not a single line.
The core insight

In beta decay a nucleus changes one neutron into a proton (β⁻) or one proton into a neutron (β⁺) by the weak interaction, keeping its mass number AA but shifting its charge ZZ by one; a light neutral neutrino is emitted with the electron and shares the fixed released energy Q=Δm c2Q = \Delta m\,c^2 between them, so the electron's energy runs continuously from zero up to an endpoint equal to QQ.

Where this lives today

Beta decay is one of the most useful processes physics knows. Radiocarbon dating rests entirely on the β⁻ decay of carbon-14 met above: living things maintain a fixed ratio of 14^{14}C to ordinary carbon, and once they die the 14^{14}C ticks down with a half-life of 57305730 years, so the residual beta activity reads off the age of wood, cloth, bone and charcoal up to about fifty thousand years old. Positron emission tomography (PET) turns β⁺ decay into a medical camera: a patient is given a sugar tagged with fluorine-18, and each emitted positron annihilates with a nearby electron into two 511 keV511\ \text{keV} gamma rays flying apart back-to-back, whose coincident arrival pinpoints where in the body the tracer collected — lighting up tumours and active brain tissue. Nuclear reactors are prolific beta emitters: their fission fragments are neutron-rich and shed beta particles for years, which is both the source of a reactor's dangerous "decay heat" after shutdown and the flood of antineutrinos that made the 1956 detection possible. And the neutrino itself, once an apologetic fudge, is now a tool: neutrino telescopes buried in Antarctic ice and deep mines watch the Sun's fusion core and distant supernovae through the one messenger that escapes them unimpeded. The particle Pauli feared could never be seen is now caught by the trillion.

The physical picture

Alpha decay throws a whole ready-made helium nucleus out of an over-heavy nucleus. Beta decay is subtler and, at bottom, stranger: nothing is thrown out that was inside to begin with. Instead one of the nucleons transforms into the other kind, and the electron (or positron) that flies off is created at the instant of decay — it was never an occupant of the nucleus, any more than the sound of a bell was hiding inside the metal before it was struck. There are no electrons living inside a nucleus; the beta electron is manufactured on the spot out of the energy released when a neutron becomes a proton. Why would a nucleus bother? Because it is trading a less stable arrangement for a more stable one. A nucleus with too many neutrons for its number of protons is like a see-saw loaded on one side; converting a surplus neutron into a proton (β⁻) evens the balance and drops the whole system to lower energy. A nucleus with too many protons does the reverse, converting a proton into a neutron (β⁺, or its cousin electron capture). In every case the mass number A=Z+NA = Z + N stays the same — one nucleon simply changes its identity — while the atomic number ZZ steps by one. On the chart of the nuclides the daughter sits one square across from the parent, never up or down the mass ladder.

Figure
Beta-minus turns a neutron into a proton so the daughter has one more proton and one fewer neutron while the mass number stays fixed; beta-plus does the reverse. Both create a fast electron or positron plus a neutrino at the moment of decay
Beta decay — one nucleon changes identity; A stays fixed, Z shifts by one parent Z, N, A β⁻ daughter Z+1, N−1, A β⁺ daughter Z−1, N+1, A emits e⁻ + ν̄ n → p emits e⁺ + ν p → n the fundamental β⁻ process (weak force) n p + e⁻ + ν̄ antineutrino (invisible) the electron and neutrino are created at the instant of decay — neither was inside the nucleus

The particle that emerges is a genuine electron (for β⁻) or its antimatter twin the positron (for β⁺): same mass mem_e, opposite charge. But it never comes alone. Riding out beside it is the neutrino — neutral, of vanishingly small mass, so weakly interacting that a wall of lead a light-year thick would stop only half of a beam of them. That ghost is what makes the accounting work, and the rest of this article is the story of how a graph of electron energies proved it had to be there.

The two faces of beta decay

At the level of the individual nucleon there are two decay channels, plus a closely related third.

Beta-minus (β⁻) decay. A neutron converts to a proton. Charge must balance, so a negative electron is created; a fourth conservation law we meet below demands an antineutrino too:

n  →  p+e−+νˉe(1)n \;\to\; p + e^- + \bar\nu_e \qquad (1)

For a whole nucleus ZAX^{A}_{Z}X the newly minted proton stays behind and lifts the atomic number by one:

ZAX  →  Z+1  AY+e−+νˉe(2)^{A}_{Z}X \;\to\; ^{\;A}_{Z+1}Y + e^- + \bar\nu_e \qquad (2)

where: ZAX^{A}_{Z}X is the parent nucleus, Z+1AY^{A}_{Z+1}Y the daughter one place higher in the periodic table, e−e^- the emitted beta electron and νˉe\bar\nu_e the electron antineutrino. The physical reading: neutron-rich nuclei climb toward stability by turning a neutron into a proton. The canonical school example is carbon-14, 614C→ 714N+e−+νˉe^{14}_{6}\text{C} \to\ ^{14}_{7}\text{N} + e^- + \bar\nu_e, the reaction that dates ancient wood and bone.

Beta-plus (β⁺) decay. For a proton-rich nucleus the traffic runs the other way: a proton becomes a neutron, throwing out a positron (the electron's positive antiparticle) and an ordinary neutrino:

p  →  n+e++νe,ZAX  →  Z−1  AY+e++νe(3)p \;\to\; n + e^+ + \nu_e, \qquad ^{A}_{Z}X \;\to\; ^{\;A}_{Z-1}Y + e^+ + \nu_e \qquad (3)

where: e+e^+ is the positron and νe\nu_e the electron neutrino. Now ZZ falls by one. A free proton cannot do this — it is lighter than a neutron, so the conversion would need energy from nowhere — but inside a proton-rich nucleus the gain in nuclear binding pays the bill. Positron emitters such as fluorine-18 are the heart of the PET scanner.

Electron capture. When a proton-rich nucleus does not have quite enough spare energy for β⁺ (we will see it needs 1.02 MeV1.02\ \text{MeV}), it can instead swallow one of its own inner atomic electrons: p+e−→n+νep + e^- \to n + \nu_e. The result — Z→Z−1Z \to Z-1, AA fixed — is the same as β⁺, but only a single neutrino leaves the atom. It is beta decay's quiet third door and a favourite exam contrast. In every one of these, the total electric charge and the mass number AA are conserved, and exactly one lepton–neutrino pair is created. What is not conserved is the identity of the nucleon: beta decay is the one process a school student meets in which a particle literally turns into a different particle.

Where the energy comes from — the Q-value

Beta decay, like every decay, is powered by a tiny loss of mass. The QQ-value is the total energy released, Q=Δm c2Q = \Delta m\,c^2, shared as kinetic energy among the products (the recoiling daughter, the beta particle and the neutrino). A decay proceeds spontaneously only if Q>0Q > 0, i.e. only if the parent is heavier than the sum of its products. Here lurks the single most useful bookkeeping trick in nuclear physics: use atomic masses, not bare nuclear masses, and the electron masses cancel by themselves. A table of atomic masses already includes each atom's full complement of orbital electrons; because beta decay changes ZZ by one, the electron count differs between parent and daughter atoms by exactly the one electron that is created, so it drops out of the sum. The two derivations below make this precise. The upshot for β⁻ is beautifully clean:

Qβ−=[M(ZAX)−M(Z+1AY)]c2(4)Q_{\beta^-} = \big[M(^{A}_{Z}X) - M(^{A}_{Z+1}Y)\big]c^2 \qquad (4)

where: the MM are neutral-atom masses (in u\text{u}, then multiplied by 931.5 MeV/u931.5\ \text{MeV/u}). No electron mass appears at all. For β⁺, by contrast, the same careful accounting leaves behind two electron masses:

Qβ+=[M(ZAX)−M(Z−1AY)−2me]c2(5)Q_{\beta^+} = \big[M(^{A}_{Z}X) - M(^{A}_{Z-1}Y) - 2m_e\big]c^2 \qquad (5)

where: 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV} is the fixed penalty a positron emitter must overcome. This asymmetry between (4) and (5) is not a typo and not a curiosity — it is a standard mark-earner, and getting it right is what separates a correct β⁺ answer from a wrong one.

Derivation AThe Q-value of beta-minus decay from atomic masses

The goal is to show that for β⁻ decay the released energy is simply Q=[M(parent atom)−M(daughter atom)] c2Q = [M(\text{parent atom}) - M(\text{daughter atom})]\,c^2, with the electron masses cancelling of their own accord — so that a table of neutral-atom masses is all you ever need, and no separate mass for the emitted electron enters. The strategy is to write QQ honestly in terms of the bare nuclear masses first, then trade each nuclear mass for its atomic mass minus the orbital electrons, and watch the electron terms collapse. Neutrino rest mass is taken as zero and the (electronvolt-scale) atomic binding energies are neglected, both excellent approximations at this level.

Step 1. Write QQ from the nuclear masses. The reaction is ZAX→ Z+1AY+e−+νˉe^{A}_{Z}X \to\ ^{A}_{Z+1}Y + e^- + \bar\nu_e. Energy released equals the mass lost, so with MNM_N for nuclear masses and a massless neutrino, Q=[MN(X)−MN(Y)−me]c2Q = \big[M_N(X) - M_N(Y) - m_e\big]c^2. The lone −me-m_e is the mass of the created beta electron.

Step 2. Convert to atomic masses. A neutral parent atom carries ZZ electrons, a neutral daughter atom Z+1Z+1: M(X)=MN(X)+Z meM(X) = M_N(X) + Z\,m_e and M(Y)=MN(Y)+(Z+1) meM(Y) = M_N(Y) + (Z+1)\,m_e (dropping the tiny electron binding energies). Solve each for the nuclear mass: MN(X)=M(X)−Z meM_N(X) = M(X) - Z\,m_e and MN(Y)=M(Y)−(Z+1) meM_N(Y) = M(Y) - (Z+1)\,m_e.

Step 3. Substitute into Step 1: Q=[ M(X)−Zme−(M(Y)−(Z+1)me)−me ]c2Q = \big[\,M(X) - Z m_e - \big(M(Y) - (Z+1)m_e\big) - m_e\,\big]c^2. Collect the electron terms: −Zme+(Z+1)me−me=0-Z m_e + (Z+1)m_e - m_e = 0. They vanish exactly — the ZZ electrons of the parent, the Z+1Z+1 of the daughter and the one emitted electron balance perfectly — leaving equation (4), Qβ−=[M(X)−M(Y)]c2Q_{\beta^-} = [M(X) - M(Y)]c^2.

Step 4. Put in carbon-14. With M(14C)=14.003242 uM(^{14}\text{C}) = 14.003242\ \text{u} and M(14N)=14.003074 uM(^{14}\text{N}) = 14.003074\ \text{u}, the mass difference is 0.000168 u0.000168\ \text{u}, so Q=0.000168×931.5=0.156 MeVQ = 0.000168 \times 931.5 = 0.156\ \text{MeV}. That is the entire energy budget shared between the electron and the antineutrino (the massive nitrogen nucleus recoils with almost none of it). Verified: electron terms cancel identically; Q(14C)=(14.003242−14.003074)×931.5=0.156 MeVQ(^{14}\text{C}) = (14.003242 - 14.003074)\times 931.5 = 0.156\ \text{MeV} — recomputed in verify_hs2-beta-decay-neutrino.py.

Go deeper · Derivation B · 1 minWhy beta-plus decay costs an extra 1.02 MeV
Derivation BWhy beta-plus decay costs an extra 1.02 MeV

The goal is to derive equation (5) — that a positron emitter must lose enough mass to cover an additional 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV} before it can decay — and thereby explain why some proton-rich nuclei choose electron capture instead. The strategy is identical to the last derivation, but now the created particle is a positron, which is not counted among either atom's orbital electrons, so the electron bookkeeping no longer closes to zero.

Step 1. Nuclear-mass QQ. For ZAX→ Z−1AY+e++νe^{A}_{Z}X \to\ ^{A}_{Z-1}Y + e^+ + \nu_e, the created positron has mass mem_e, so Q=[MN(X)−MN(Y)−me]c2Q = \big[M_N(X) - M_N(Y) - m_e\big]c^2.

Step 2. Convert to atomic masses. The parent still has ZZ electrons but the daughter now has only Z−1Z-1: MN(X)=M(X)−ZmeM_N(X) = M(X) - Z m_e and MN(Y)=M(Y)−(Z−1)meM_N(Y) = M(Y) - (Z-1)m_e.

Step 3. Substitute: Q=[ M(X)−Zme−(M(Y)−(Z−1)me)−me ]c2Q = \big[\,M(X) - Z m_e - \big(M(Y) - (Z-1)m_e\big) - m_e\,\big]c^2. Now the electron terms give −Zme+(Z−1)me−me=−2me-Z m_e + (Z-1)m_e - m_e = -2m_e, so Qβ+=[M(X)−M(Y)−2me]c2Q_{\beta^+} = [M(X) - M(Y) - 2m_e]c^2, which is equation (5). Two electron masses survive: one because the daughter atom, keeping the parent's ZZ electrons around a nucleus of charge Z−1Z-1, is left with one electron too many, whose mass the atomic-mass table (which counts only Z−1Z-1 electrons) does not carry; one for the positron itself.

Step 4. The threshold and the escape hatch. Because 2mec2=2×0.511=1.02 MeV2m_e c^2 = 2 \times 0.511 = 1.02\ \text{MeV}, β⁺ decay is energetically forbidden unless the parent atom is at least 1.02 MeV1.02\ \text{MeV} heavier than the daughter. When the difference is positive but smaller than this, the nucleus reaches the same daughter by electron capture instead, p+e−→n+νep + e^- \to n + \nu_e, which pays no positron-creation penalty. Worked check: fluorine-18, with M(18F)=18.000938 uM(^{18}\text{F}) = 18.000938\ \text{u} and M(18O)=17.999160 uM(^{18}\text{O}) = 17.999160\ \text{u}, gives Q=(0.001778−0.001098)×931.5=0.633 MeVQ = (0.001778 - 0.001098)\times 931.5 = 0.633\ \text{MeV} of positron energy — safely above threshold, which is why 18^{18}F is a workhorse positron source. Verified: electron terms leave −2me-2m_e; 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV}; Q(18F)=0.633 MeVQ(^{18}\text{F}) = 0.633\ \text{MeV} — recomputed in verify_hs2-beta-decay-neutrino.py.

The continuous spectrum and the ghost particle

Now the puzzle that started it all. If beta decay were a two-body split — daughter plus electron only — then energy and momentum conservation would fix the electron's energy to a single sharp value, exactly as they do for the alpha particle. Fire off the same decay a million times and every electron should carry the identical energy QQ (minus the trifling recoil). That is emphatically not what James Chadwick found in 1914. The beta electrons came out with a continuous range of energies, from nearly zero all the way up to a definite maximum — the endpoint energy — with a broad hump in between. Most electrons carried far less than the full QQ; the endpoint alone equalled it.

Figure
The measured beta energy spectrum is a continuous hump running from zero up to a sharp endpoint equal to Q, unlike the single spike a two-body decay would give. The missing energy below the endpoint is carried away by the unseen neutrino
Why the beta spectrum needs a third particle kinetic energy of the emitted electron number of electrons endpoint = Q observed: continuous expected if only 2 bodies: one sharp line at Q most electrons carry less than Q… the rest goes to the neutrino alpha decay gives one sharp line — beta decay a smear: something invisible shares the energy

A continuous spectrum with a sharp ceiling can only mean one thing: the energy QQ is being shared among more than two products, and the share going to the electron varies from event to event. When the electron happens to take almost everything, its energy approaches the endpoint QQ; when it takes almost nothing, the other product carries QQ away instead. That silent partner is the neutrino. It is always emitted; we simply cannot see it. The endpoint of the spectrum is therefore a direct measurement of QQ, and its value is exactly what equation (4) predicts from the atomic masses. Energy was not the only law in danger. Spin was too. A neutron, a proton and an electron each have spin 12\tfrac12. A decay n→p+e−n \to p + e^- would take a spin-12\tfrac12 particle into two spin-12\tfrac12 particles, whose spins can only add to 00 or 11 — never back to a half-integer. Angular momentum simply would not balance. Adding a third spin-12\tfrac12 particle, the neutrino, fixes both crimes at once: it restores the half-integer total spin and it carries off the missing energy and momentum. Pauli's single new particle closed three conservation ledgers simultaneously, which is why, however desperate it seemed in 1930, it was almost certainly right. It took until 1956 for Cowan and Reines to catch antineutrinos streaming from a nuclear reactor and prove the ghost real.

Limiting cases

caseresultmeaning
neutron-rich nucleusβ⁻: Z→Z+1Z \to Z+1, AA fixedemits e−e^- and νˉe\bar\nu_e; carbon-14 is the type example
proton-rich, Q>1.02 MeVQ > 1.02\ \text{MeV}β⁺: Z→Z−1Z \to Z-1, AA fixedemits e+e^+ and νe\nu_e; needs the 2mec22m_e c^2 overhead
proton-rich, Q<1.02 MeVQ < 1.02\ \text{MeV}electron capture: Z→Z−1Z \to Z-1nucleus swallows an inner electron; only a νe\nu_e leaves
neutrino takes ≈0\approx 0 energyelectron KE →Q\to Q (the endpoint)the sharp upper edge of the beta spectrum
electron takes ≈0\approx 0 energyneutrino carries ≈Q\approx Qthe low-energy end of the spectrum
free neutron (no nucleus)Q=0.782 MeVQ = 0.782\ \text{MeV}, T1/2≈10T_{1/2}\approx 10 mineven a lone neutron β⁻-decays; a lone proton does not

Worked examples

Board level — carbon-14 decay and its Q-value (CBSE and ICSE pattern)

Carbon-14 is a beta-minus emitter. Write its decay equation, identify the daughter nuclide, and find the energy released, given the atomic masses M(14C)=14.003242 uM(^{14}\text{C}) = 14.003242\ \text{u} and M(14N)=14.003074 uM(^{14}\text{N}) = 14.003074\ \text{u}, with 1 u=931.5 MeV/c21\ \text{u} = 931.5\ \text{MeV}/c^2.

Step 1. In β⁻ decay a neutron becomes a proton, so ZZ rises by one (6→76 \to 7) while A=14A = 14 is unchanged. Carbon (Z=6Z=6) becomes nitrogen (Z=7Z=7): 614C→ 714N+e−+νˉe^{14}_{6}\text{C} \to\ ^{14}_{7}\text{N} + e^- + \bar\nu_e. The daughter is 714N^{14}_{7}\text{N}.

Step 2. For β⁻ the electron masses cancel, so use atomic masses directly (equation 4): Δm=M(14C)−M(14N)=14.003242−14.003074=0.000168 u\Delta m = M(^{14}\text{C}) - M(^{14}\text{N}) = 14.003242 - 14.003074 = 0.000168\ \text{u}.

Step 3. Convert to energy: Q=Δm×931.5=0.000168×931.5=0.156 MeVQ = \Delta m \times 931.5 = 0.000168 \times 931.5 = \boxed{0.156\ \text{MeV}}.

Step 4. Interpret. This 0.156 MeV0.156\ \text{MeV} is the maximum kinetic energy any emitted electron can have — the endpoint of the continuous spectrum. Most electrons carry less; on average only about a third of it, roughly 0.05 MeV0.05\ \text{MeV}, with the antineutrino taking the balance. The nitrogen nucleus, being far heavier, recoils with negligible energy.

Competitive level — fluorine-18, the PET tracer (JEE and NEET pattern)

Fluorine-18 decays by positron emission. Write the equation, and using M(18F)=18.000938 uM(^{18}\text{F}) = 18.000938\ \text{u}, M(18O)=17.999160 uM(^{18}\text{O}) = 17.999160\ \text{u} and mec2=0.511 MeVm_e c^2 = 0.511\ \text{MeV}, find the maximum kinetic energy of the emitted positron. Why must you subtract two electron masses, and what would happen if the mass difference were below 1.02 MeV1.02\ \text{MeV}?

Step 1. In β⁺ decay a proton becomes a neutron, so ZZ falls by one (9→89 \to 8), A=18A = 18 fixed. Fluorine (Z=9Z=9) becomes oxygen (Z=8Z=8): 918F→ 818O+e++νe^{18}_{9}\text{F} \to\ ^{18}_{8}\text{O} + e^+ + \nu_e.

Step 2. Use the β⁺ formula (equation 5), Q=[M(18F)−M(18O)−2me]c2Q = [M(^{18}\text{F}) - M(^{18}\text{O}) - 2m_e]c^2. The atomic-mass difference is 18.000938−17.999160=0.001778 u18.000938 - 17.999160 = 0.001778\ \text{u}. The two-electron term is 2me=2×0.000549=0.001098 u2m_e = 2 \times 0.000549 = 0.001098\ \text{u}.

Step 3. Subtract and convert: Q=(0.001778−0.001098)×931.5=0.000680×931.5=0.633 MeVQ = (0.001778 - 0.001098) \times 931.5 = 0.000680 \times 931.5 = \boxed{0.633\ \text{MeV}}. This is the endpoint (maximum) positron energy; the neutrino shares the rest.

Step 4. The reasoning behind the −2me-2m_e: the daughter oxygen atom is born with one electron too many (its nucleus lost a proton), and a positron of mass mem_e is created as well — two electron masses' worth of extra mass must be paid for out of QQ. If the parent–daughter atomic-mass difference were less than 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV}, β⁺ would be forbidden and the nucleus would instead reach 18O^{18}\text{O} by capturing an inner atomic electron. (In fact 18^{18}F does a few percent of its decays by electron capture even so.) Timing note: about 90 seconds under exam pressure. The whole item is one subtraction and one multiplication — the only place to lose a mark is forgetting the −2me-2m_e, which is exactly what the examiner is testing. Commit "β⁻ cancels, β⁺ costs two electron masses" to reflex and this class of question is free.

Competitive level — the free neutron and why the proton is stable (JEE Advanced pattern)

A free neutron is slightly heavier than a free proton: mn=1.008665 um_n = 1.008665\ \text{u}, mp=1.007276 um_p = 1.007276\ \text{u}, me=0.000549 um_e = 0.000549\ \text{u}. Using particle (not atomic) masses, find the Q-value of free-neutron beta decay n→p+e−+νˉen \to p + e^- + \bar\nu_e, and explain why an isolated proton cannot beta-decay.

Step 1. Here there are no orbital electrons, so use the bare particle masses directly: Δm=mn−mp−me=1.008665−1.007276−0.000549=0.000840 u\Delta m = m_n - m_p - m_e = 1.008665 - 1.007276 - 0.000549 = 0.000840\ \text{u}.

Step 2. Convert: Q=0.000840×931.5=0.782 MeVQ = 0.000840 \times 931.5 = \boxed{0.782\ \text{MeV}}. Because Q>0Q > 0, a free neutron is unstable — and indeed it decays with a half-life of about 1010 minutes, the reason free neutrons are rare in nature.

Step 3. For the reverse, p→n+e++νep \to n + e^+ + \nu_e, the mass change is mn−mp+me>0m_n - m_p + m_e > 0: the products are heavier than the proton by (mn−mp+me)c2≈1.81 MeV(m_n - m_p + m_e)c^2 \approx 1.81\ \text{MeV}, so Q<0Q < 0 and the decay cannot happen. A free proton is stable; only inside a proton-rich nucleus, where nuclear binding energy supplies the deficit, can a bound proton convert to a neutron. Timing note: under a minute. The single insight worth memorising is the sign of mn−mpm_n - m_p: the neutron is the heavier nucleon by about 1.29 MeV/c21.29\ \text{MeV}/c^2, which is why neutrons decay and protons (on their own) do not. Every free-neutron question hangs off that one fact.

Exam traps

Forgetting the 2me2m_e in β⁺. For β⁻ the electron masses cancel and Q=[M(parent)−M(daughter)]c2Q = [M(\text{parent}) - M(\text{daughter})]c^2; for β⁺ you must subtract 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV}. Using the β⁻ formula for a positron emitter overstates QQ by exactly 1.02 MeV1.02\ \text{MeV} and is the single most common β-decay error on JEE, NEET and A-Level. Anchor it: β⁻ cancels, β⁺ costs two.

Mixing up atomic and nuclear masses. Data tables almost always list atomic (neutral-atom) masses. The whole cancellation trick assumes you use them consistently. If a problem hands you bare nuclear masses, you must put the electron mass back in by hand. State which you are using.

Getting the direction of ZZ wrong. β⁻ raises ZZ by one (neutron →\to proton); β⁺ and electron capture lower it. The mass number AA never changes in beta decay. Writing the daughter one place too low for β⁻ is an easy, avoidable slip.

Reading the spectrum as a single energy. The beta particle does not come out at a fixed energy. Only the endpoint of its continuous spectrum equals QQ; the average is far lower (about a third of QQ). A question that asks for "the energy of the beta particle" is usually asking for the maximum, i.e. QQ — say so explicitly.

Calling the neutrino massless-and-chargeless "nothing." The neutrino is a real particle: neutral, spin 12\tfrac12, with a tiny but non-zero mass. It is needed to conserve energy, momentum and angular momentum. Do not omit it from a decay equation, and do not confuse νe\nu_e (emitted in β⁺) with νˉe\bar\nu_e (emitted in β⁻).

Board scope. The identity of β⁻/β⁺ decay and the Z,AZ, A changes are core on CBSE, ICSE, JEE, NEET, AP Physics 2, IB HL, A-Level 9702 and even IGCSE 0625 (qualitatively). The QQ-value in MeV, the 931.5 MeV/u931.5\ \text{MeV/u} conversion and the 2me2m_e subtlety are not on IGCSE — that board treats beta decay only descriptively. The continuous spectrum and the neutrino argument sit at the higher tier (JEE Advanced, A-Level, IB HL); NEET and CBSE expect you to know the neutrino exists and why, but not to compute its spectrum.

Origins · 1 minEnrico Fermi and how this was discovered
EF
Enrico Fermi
1901–1954 · Rome and Chicago

Enrico Fermi was the Italian physicist who turned beta decay from a paradox into a theory. In 1934, taking up Wolfgang Pauli's tentative "little neutral particle," Fermi wrote down the first quantitative account of β⁻ decay as a brand-new fundamental interaction — the weak force — in which a neutron transforms into a proton while an electron and a neutrino are created out of the released energy, much as a photon is created when an atom radiates. He adopted and popularized the name neutrino — Italian for "little neutral one," coined by his Rome colleague Edoardo Amaldi to distinguish this light particle from Chadwick's just-discovered neutron — and introduced it into the physics literature. His paper was so far ahead of its evidence that the journal Nature rejected it as "too remote from reality." Fermi went on to build the first controlled nuclear chain reaction in Chicago in 1942 and won the 1938 Nobel Prize; the element fermium and the fermi unit of length both honour him. His theory of beta decay still underlies the modern understanding of the weak interaction.

History
1896
— Henri Becquerel discovers radioactivity in uranium salts.
1899
— Ernest Rutherford separates and names the alpha and beta rays by their penetrating power.
1914
— James Chadwick shows the beta particles emerge with a continuous range of energies, not a single line.
1930
— Wolfgang Pauli postulates a light, neutral, deeply penetrating particle to save energy and momentum conservation.
1934
— Enrico Fermi publishes his quantitative theory of beta decay and gives currency to the name neutrino (coined by Amaldi).
1956
— Clyde Cowan and Frederick Reines detect the antineutrino directly beside a nuclear reactor.

Going further

Texts. NCERT Physics Class 12, Chapter 13 ("Nuclei"), the radioactivity and beta-decay sections · H. C. Verma, Concepts of Physics Vol. 2, "The Nucleus" · Krane, Introductory Nuclear Physics, Chapter 9, for the historical and theoretical route to the neutrino · Serway/Halliday modern-physics chapters for the QQ-value conventions.

Provenance. Standard nuclear data; atomic masses from the AME table. Recompute: β⁻ Q-value formula Q=[M(parent)−M(daughter)] 931.5 MeVQ = [M(\text{parent}) - M(\text{daughter})]\,931.5\ \text{MeV}; β⁺ formula with the −2me-2m_e term; 14C→ 14N^{14}\text{C} \to\ ^{14}\text{N} mass difference 0.000168 u0.000168\ \text{u} giving Q=0.156 MeVQ = 0.156\ \text{MeV}; average β energy ≈Q/3≈0.05 MeV\approx Q/3 \approx 0.05\ \text{MeV}; 18F→ 18O^{18}\text{F} \to\ ^{18}\text{O} mass difference 0.001778 u0.001778\ \text{u}, minus 2me=0.001098 u2m_e = 0.001098\ \text{u}, giving Q=0.633 MeVQ = 0.633\ \text{MeV}; mec2=0.511 MeVm_e c^2 = 0.511\ \text{MeV} and 2mec2=1.02 MeV2m_e c^2 = 1.02\ \text{MeV}; free-neutron Δm=0.000840 u\Delta m = 0.000840\ \text{u} giving Q=0.782 MeVQ = 0.782\ \text{MeV}; neutron–proton mass difference (mn−mp)c2=1.29 MeV(m_n - m_p)c^2 = 1.29\ \text{MeV}; forbidden free-proton decay margin ≈1.81 MeV\approx 1.81\ \text{MeV}.

Prerequisites. Radioactivity: Alpha, Beta & Gamma — the three radiations compared, of which beta is the middle one this article opens up. Its ideas of nuclear transmutation and the QQ-value carry straight over. Leads to. Gamma Decay & Nuclear Energy Levels, since a beta decay often leaves the daughter nucleus excited, and it sheds that surplus as a gamma photon; and The Radioactive Decay Law, which gives the rate at which these decays happen. For enrichment, the university seam Particle Decay Kinematics in Special Relativity (go-deeper only, never an exam dependency here) treats the energy-momentum sharing that makes the beta spectrum continuous.

If there are no electrons inside the nucleus, where does the beta electron come from?

It is created at the moment of decay, out of the energy released when a neutron converts into a proton. This is genuinely a particle being made from scratch, exactly as a photon is made when an excited atom drops to a lower level — the photon was not "inside" the atom beforehand either. The old idea that nuclei contained electrons (to explain the negative charge of beta rays) was abandoned once quantum mechanics showed an electron cannot be confined to a region as small as a nucleus. Modern physics says a nucleus holds only protons and neutrons; the beta electron and its neutrino are manufactured on the spot by the weak interaction.

What exactly is the difference between a neutrino and an antineutrino here?

In β⁻ decay (n→p+e−+νˉen \to p + e^- + \bar\nu_e) the partner is an electron antineutrino, νˉe\bar\nu_e; in β⁺ decay (p→n+e++νep \to n + e^+ + \nu_e) it is an ordinary electron neutrino, νe\nu_e. The pairing is dictated by a conservation law (lepton number): an electron and an antineutrino are created together, a positron and a neutrino together, so that the leptonic books balance. For most school purposes the key point is simply that a neutral, near-massless particle always accompanies the beta particle. If a decay equation you are asked to complete emits an electron, its companion is an antineutrino; if it emits a positron, a neutrino.

Why is the beta particle's energy not a single fixed value like the alpha particle's?

Because beta decay is a three-body process. When only two products share the released energy QQ — as in alpha decay, where the daughter and the alpha split it — conservation of energy and momentum fixes each one's share to a single value, giving a sharp line. In beta decay three products (daughter, electron, neutrino) share QQ, so the electron's portion can be anything from zero up to the full QQ, depending on how the neutrino and electron divide the load. The result is a continuous spectrum whose upper endpoint equals QQ. Historically it was precisely this continuous spectrum, discovered by Chadwick in 1914, that revealed a third particle had to be present.

Why does a free neutron decay but a free proton does not?

It comes down to mass. A free neutron is slightly heavier than a free proton plus an electron, so its beta decay releases 0.782 MeV0.782\ \text{MeV} and happens spontaneously, with a half-life of about ten minutes. A free proton, being lighter, would have to gain mass to turn into a neutron plus a positron — the products would be about 1.8 MeV1.8\ \text{MeV} heavier — so the decay is energetically forbidden and an isolated proton is stable. Inside a proton-rich nucleus the situation can reverse: the nucleus becomes more tightly bound when a proton converts to a neutron, and that gain in binding energy pays the mass debt, allowing β⁺ decay or electron capture.

What is electron capture, and how is it related to beta decay?

Electron capture is a third route to the same end as β⁺ decay: a proton-rich nucleus absorbs one of its own inner atomic electrons, p+e−→n+νep + e^- \to n + \nu_e, lowering ZZ by one with AA unchanged. It competes with β⁺ decay and wins whenever the parent–daughter atomic mass difference is positive but below the 1.02 MeV1.02\ \text{MeV} needed to create a positron. Only a single neutrino leaves the atom (no positron), so there is no beta particle to detect — the tell-tale signature is instead the X-rays emitted as outer electrons cascade down to fill the vacancy left by the captured electron. Many textbooks group electron capture with beta decay because it obeys the same Z→Z−1Z \to Z-1 rule and the same weak interaction.

Has the neutrino ever actually been detected, or is it still just a bookkeeping device?

It has been detected, decisively. In 1956 Clyde Cowan and Frederick Reines set a detector beside a nuclear reactor — a colossal source of antineutrinos from the beta decay of fission fragments — and caught the rare reactions in which an antineutrino strikes a proton. Since then neutrinos have been observed from the Sun, from a supernova in 1987, from cosmic rays and from particle accelerators, and their study has become a whole branch of physics (including the 2015 Nobel Prize for showing neutrinos have a tiny mass). So the particle Pauli half-apologised for proposing, fearing it could never be seen, is now routinely detected — a striking case of a conservation law correctly predicting an entirely new particle decades before the technology to find it existed.

Is beta decay covered on my board, and to what depth?

The existence and basic rules of beta decay — a neutron or proton converting, ZZ shifting by one, AA staying fixed, a fast electron or positron emitted — are examinable on essentially every board, including IGCSE, where they are treated qualitatively. The quantitative QQ-value using the 931.5 MeV/u931.5\ \text{MeV/u} conversion, and especially the 2me2m_e subtraction for β⁺, are expected on CBSE, ICSE, JEE, NEET, AP Physics 2, IB HL and A-Level, but not on IGCSE. The continuous spectrum and the detailed neutrino argument are higher-tier material: JEE Advanced, A-Level and IB HL treat them fully, while CBSE and NEET expect you to know the neutrino exists and why it was proposed, without deriving its spectrum.

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Where this leads