Nuclear physics §
Nuclear physics describes the structure and behavior of atomic nuclei: the strong-interaction bound states of protons and neutrons (nucleons), the reactions that transform them, and the radioactive decays that reveal the weak interaction. It is relevant whenever the nucleus itself matters: energy production (fission reactors, fusion), medical imaging and radiotherapy, radiometric dating, and the nucleosynthesis that built the elements (see Cosmology).
The nucleus sits between two levels of description. Below it, nucleons are bound states of quarks and gluons (see Elementary particles); the force between nucleons is a residual of the strong interaction, just as the van der Waals force between molecules is a residual of electromagnetism. Above it, the nucleus is simply the positive charge that anchors the electron shells of atomic physics. And because nuclei are quantum objects, the tools come from quantum mechanics: bound states and shell filling from the Pauli principle, and decay through barriers from tunneling.
Authoritative sources
The nuclear force §
Definition. The nuclear force is the residual strong interaction between nucleons: a short-range attraction (range ≈ 1–2 fm) with a repulsive core, approximately charge-independent, plus the long-range Coulomb repulsion between protons.
Details
Where the force comes from §
Quantum chromodynamics confines quarks into protons and neutrons (see Elementary particles). Each nucleon is color-neutral, so — like two neutral atoms — two nucleons feel almost no force at large distance. But their quark clouds polarize each other, leaving a residual attraction at short range, analogous to the van der Waals force between molecules (see molecular bonds). This residual force is what binds nuclei.
Properties §
- Short range: effective range ≈ 1–2 fm ( m); beyond ~3 fm it is negligible. Yukawa explained the exponential falloff as exchange of a massive particle: with fm — the pion (mass ≈ 140 MeV) is the force carrier.
- Repulsive core: below ~0.5 fm the force turns strongly repulsive, which is why nuclei have a nearly constant density (saturation) rather than collapsing.
- Charge independence: approximately the same for p–p, n–n, and p–n pairs in the same spin-isospin channel.
- Spin dependence: the deuteron (p + n) is bound only in the spin-triplet channel ( MeV); the spin-singlet state is unbound. A tensor component mixes S and D waves.
- Saturation: each nucleon interacts mainly with its nearest neighbors, so total binding energy grows roughly as , not .
The potential between two nucleons §
For two protons, the effective potential is the sum of the short-range nuclear well and the long-range Coulomb repulsion :
The Coulomb tail looks tiny on this scale — but it is the whole story of alpha decay and fission: for an particle facing a heavy daughter (), the same term reaches ≈ 30 MeV at the nuclear surface, forming a barrier that the can only escape by quantum tunneling.
Example: why the deuteron is fragile §
The deuteron’s binding energy (2.22 MeV) is tiny compared with typical nuclear wells (~40 MeV) because it is bound only by the tensor part of the force in the spin-triplet channel — there is no bound p–p or n–n nucleus. This is direct evidence that the nuclear force depends on spin and isospin, not just position.
Authoritative sources
Example problem
Yukawa proposed that a force of range is carried by a particle of mass . The nuclear force has range ≈ 1.4 fm. Estimate the mass of its carrier, in MeV/. (Use MeV·fm.)
Solution
This matches the pion mass ( MeV) — the prediction that led to the discovery of the pion in 1947, and the first concrete picture of a force as particle exchange (see Elementary particles).
Nuclear structure: liquid drop and shell models §
Definition. A nucleus with protons and neutrons (mass number ) is a quantum bound state of nucleons. Its binding energy is described by two complementary models: the liquid drop (collective, like an incompressible fluid) and the shell model (independent nucleons filling quantized orbits, like electrons in atoms).
Details
Step 1: the liquid drop model §
Because the nuclear force is short-ranged and saturating, a nucleus behaves like a droplet of incompressible fluid: each nucleon contributes a fixed volume energy, only surface nucleons lose neighbors, protons repel each other via Coulomb, and the Pauli exclusion principle penalizes proton–neutron imbalance. The Bethe–Weizsäcker semi-empirical mass formula:
with MeV (volume), MeV (surface), MeV (Coulomb), MeV (asymmetry), and a pairing term (positive for even–even nuclei, negative for odd–odd, zero for odd ).
Example. For iron-56 (, ): volume term ; surface ; Coulomb ; asymmetry ; pairing . Total MeV, i.e. MeV — within 0.4% of the measured 8.79 MeV.
Step 2: where the liquid drop fails — magic numbers §
The liquid drop formula predicts binding energy varying smoothly with and . But experiment shows certain nuclei are exceptionally stable and abundant: those with
the magic numbers. Nuclei with both and magic (doubly magic: He, O, Ca, Ca, Pb) are spherical, rigid, and tightly bound. A smooth droplet model cannot explain this — just as classical physics could not explain the discrete spectral lines that revealed electron shells.
Step 3: the shell model §
The nuclear shell model (Mayer and Jensen, 1949) treats each nucleon as moving independently in the average potential well created by all the others (a Woods–Saxon well, similar in spirit to the electron shells of atomic physics). Because nucleons are fermions, the Pauli exclusion principle forces them to fill discrete levels: closed shells correspond to the magic numbers.
The crucial difference from atoms is the spin–orbit coupling: the nuclear spin–orbit splitting is strong and has the opposite sign to the atomic case (where it is a small relativistic effect). A level with orbital angular momentum splits into (lower) and (higher), and the large gaps after the lowered levels reproduce the magic numbers 28, 50, 82, and 126.
The shell model explains why He (closed 1s shell), O (closed 1p shell), and the calcium isotopes () are so stable, and why neutron shell closures at shape the abundance peaks of the heavy elements formed in nucleosynthesis.
Authoritative sources
Example problem
The bottom of the valley of stability is well approximated by . Predict the most stable for (use , ), and identify the element.
Solution
, so the denominator is .
is tin — and 50 is a magic number. Tin has the largest number of stable isotopes (10) of any element, a direct signature of the shell closure.
Binding energy: the energy landscape of fission and fusion §
Definition. The binding energy per nucleon measures how tightly a nucleus is bound. Energy is released by any rearrangement — fission or fusion — that moves nuclei up the curve toward its maximum at iron.
Details
Step 1: the curve §
Plotting against mass number gives the most important single picture in nuclear energy physics:
Three features to read off the curve:
- Rapid rise up to : each added nucleon is grabbed by the short-range force (this is why nucleosynthesis in stars releases energy).
- Broad peak at iron ( MeV): iron-group nuclei are the most tightly bound — the ash of nuclear burning, and the endpoint of exothermic fusion.
- Slow decline beyond : the Coulomb repulsion of the growing proton population wins out (the term in the mass formula), so very heavy nuclei are less bound per nucleon and can release energy by splitting.
Step 2: reading energy release off the curve §
The energy released by a rearrangement is the total binding energy gained:
- Fission: uranium at MeV splitting into fragments near at MeV gains ≈ 0.9 MeV per nucleon → ≈ 200 MeV per fission.
- Fusion: four protons → one He climbs from 0 (free protons) to 7.07 MeV per nucleon; after paying the proton→neutron conversions and the positron rest masses, ≈ 26.7 MeV per helium made (this is the Sun’s energy source).
Step 3: energy per kilogram §
Because nuclear binding energies (~MeV per nucleon) are ~10⁶ times larger than chemical bond energies (~eV per molecule), nuclear fuels are enormously more energy-dense than chemical ones:
| Energy source | Energy density (J/kg) | Mechanism |
|---|---|---|
| Coal (chemical) | ≈ 3 × 10⁷ | Electron rearrangement (eV-scale bonds) |
| U-235 fission | ≈ 8 × 10¹³ | Heavy nucleus splits toward the peak of the curve |
| D–T fusion | ≈ 3.4 × 10¹⁴ | Light nuclei climb toward the peak of the curve |
Applications. Fission reactors exploit the neutron multiplication of the fission reaction (see Nuclear reactions) to sustain a controlled chain reaction. Fusion powers the stars (see Cosmology) and drives terrestrial fusion-energy research, where the D–T reaction is the leading candidate because it has the largest cross-section at reachable temperatures.
Authoritative sources
Example problem
Verify the energy density of D–T fusion fuel. One D–T reaction releases 17.6 MeV; the reactants (deuteron + triton) have a total mass of 5 u. (1 u = 1.6605 × 10⁻²⁷ kg; 1 MeV = 1.602 × 10⁻¹³ J.)
Solution
Energy per reaction: J.
Mass per reaction: kg.
Compare coal at J/kg: fusion fuel is about 10 million times more energy-dense — the direct macroscopic consequence of the MeV-vs-eV scale difference between nuclear and chemical binding.
Nuclear reactions §
Definition. A nuclear reaction transforms one set of nuclei into another, conserving charge, baryon number, lepton number, energy, and momentum. Its energy balance is the Q-value: , positive for exothermic reactions.
Details
Step 1: the conservation laws §
Whatever happens in a nuclear reaction, the books must balance: total charge , total baryon number (for nucleons), lepton number, energy, and momentum are conserved. Writing a reaction is therefore bookkeeping: match the superscripts (mass numbers) and subscripts (atomic numbers) on both sides.
Step 2: the main reaction types §
- Elastic scattering: the projectile and target exchange kinetic energy but keep their identity and internal state: . This is how Rutherford discovered the nucleus, and how neutron moderators slow neutrons in reactors.
- Inelastic scattering: the target is left in an excited state: , followed by (4.44 MeV). The outgoing neutron carries less energy.
- Charge-exchange (transfer) reactions: a nucleon is exchanged, changing the product’s species: is a (p,n) reaction that converts a target proton into a neutron, moving the residual nucleus one step up in — not mere scattering, since the projectile changes identity too.
- Fusion: light nuclei combine: MeV. Coulomb repulsion makes the rate extremely temperature-sensitive (see the binding energy curve for why it releases energy).
- Fission: a heavy nucleus splits: , releasing ≈ 200 MeV and 2–3 neutrons — the neutrons can fission further nuclei, enabling the chain reaction at the heart of reactors.
Step 3: the Q-value §
The Q-value is the rest-mass difference converted to kinetic energy:
Example. For the D–T reaction, using atomic masses u, u, u, u: u, u, so MeV — exothermic, as the binding-energy curve predicts.
Authoritative sources
Example problem
The proton–proton chain in the Sun converts four protons into one helium-4 nucleus, two positrons, two neutrinos, and energy. Using u and u, compute the total energy released per helium-4 nucleus formed. (Ignore the neutrino rest masses; 1 u = 931.5 MeV/.)
Solution
Initial mass: u.
Final rest mass: u — the helium-4 atomic mass already accounts for the two electrons whose places the two positrons effectively take (the positron masses cancel the missing electron masses in the bookkeeping).
Each positron then annihilates with an electron, releasing MeV; the two annihilations add MeV, bringing the total to MeV — the figure quoted for the Sun’s energy source (see Cosmology).
Radioactivity §
Definition. Radioactivity is the spontaneous transformation of an unstable nucleus: alpha decay (strong + Coulomb, tunneling), beta decay (weak interaction), or gamma decay (electromagnetic). The decay rate follows with half-life .
Details
Step 1: alpha decay — tunneling through the Coulomb barrier §
An particle (a helium-4 nucleus) is preformed inside a heavy nucleus, trapped by the Coulomb barrier described in the nuclear force section. Classically it could never escape; quantum mechanically it tunnels through the barrier with a tiny but nonzero probability per collision — which is why alpha half-lives range from microseconds to billions of years for nearly the same decay energy (the Geiger–Nuttall law).
Example. U Th MeV, with yr — long because the 4.2 MeV sits far below the ≈ 29 MeV barrier top.
Step 2: beta decay — the weak interaction at work §
In beta-minus decay a neutron converts to a proton via the weak interaction, emitting an electron and an antineutrino through a boson (see Elementary particles):
Beta decay moves a nucleus along the valley of stability (changing and at fixed ) and is the dominant decay mode of the neutron-rich fission fragments. The neutrino carries away variable energy — the observation of its continuous electron spectrum was the first evidence for the neutrino.
Step 3: gamma decay — photons from nuclear levels §
After alpha or beta decay the daughter nucleus is often left in an excited state. It sheds the excitation by emitting a high-energy photon — nuclear electromagnetic radiation at the MeV scale. Gamma decay changes neither nor .
Example. Tc Tc (140 keV, h): the workhorse of nuclear medicine, injected into patients for imaging because the 140 keV photon escapes the body and is easily detected.
Step 4: a complete decay scheme §
The classic decay scheme of cobalt-60 ties all three ideas together: the beta decay creates the excited daughter, and the gamma cascade de-excites it.
Note the division of labor: the weak interaction (β⁻) changes the species of nucleus; the electromagnetic interaction (the two γ’s) then drains the excitation energy of the daughter Ni. The two sharp gamma lines (1173 and 1332 keV) are used to calibrate gamma detectors.
Step 5: the decay law and radiometric dating §
Each unstable nucleus decays with a fixed probability per unit time , independent of age and chemistry:
Example. Carbon-14 ( yr) is produced in the atmosphere and taken up by living organisms. When they die, the intake stops and the C/C ratio decays exponentially — measuring it dates organic remains up to ~50 000 years (see the example problem below).
Authoritative sources
Example problem
An archaeological wooden sample has activity equal to one quarter of that of living wood. How old is it? ( yr.)
Solution
The activity is proportional to the number of C nuclei, so .
Each halving of the activity adds one half-life: two halvings → two half-lives.
Interactive simulation §
Explore the binding-energy curve interactively: slide the mass number to see where a nucleus sits on the curve, and read off the energy released by fissioning it or by fusing two copies of it. Near iron, neither direction pays.
Quiz §
Example problem
A uranium-235 nucleus absorbs a thermal neutron and fissions into barium-141 and krypton-92, releasing 3 neutrons. Given the atomic masses: u, u, u, u, compute the Q-value of the reaction in MeV. (1 u = 931.5 MeV/.)
Solution
The reaction is: .
Initial mass: u.
Final mass: u.
Mass defect: u.
Q-value: MeV.
Two remarks. First, using atomic masses is legitimate here: the 92 electrons of the uranium atom cancel exactly against the 56 + 36 = 92 electrons of the barium and krypton atoms, because total is conserved. Second, the measured fission energy is ≈ 200 MeV rather than 173 MeV because the neutron-rich fragments Ba and Kr are radioactive: their subsequent beta decays and gamma emissions add ≈ 30 MeV, and real fission produces a range of fragment splits, not just this symmetric-ish channel.