Comprehensive theory, key formulas, diagrams, and memory aids for Modern Physics.
Classical wave theory predicted that light should continuously transfer energy to electrons in a metal surface. However, experiments with the photoelectric effect revealed that energy is transferred in discrete packets — quanta. This led to the modern understanding that electromagnetic radiation behaves as both a wave and a particle.
A photon is a quantum (a discrete packet) of electromagnetic radiation. The energy of a single photon: $$E = hf = \frac{hc}{\lambda}$$
Where: - $h = 6.63 \times 10^{-34}$ J s (Planck's constant) - $f$ = frequency (Hz) - $c = 3.00 \times 10^8$ m s⁻¹ (speed of light in vacuum) - $\lambda$ = wavelength (m)
Higher frequency radiation (e.g., gamma rays) carries more energy per photon than lower frequency radiation (e.g., radio waves). The electron-volt (eV) is a convenient unit for photon energies at the atomic scale: 1 eV = 1.6 × 10⁻¹⁹ J.
When electromagnetic radiation of sufficient frequency illuminates a metal surface, electrons are emitted. These are called photoelectrons. Key experimental observations:
Einstein's explanation: Each electron absorbs exactly one photon. The photon's energy is used first to overcome the work function ($\Phi$) — the minimum energy needed to liberate an electron from the metal surface — and the rest appears as kinetic energy:
$$hf = \Phi + E_{k,max}$$
The work function relates to the threshold frequency: $\Phi = hf_0$
Stopping potential ($V_s$): The minimum reverse potential needed to stop all emitted electrons: $eV_s = E_{k,max}$
| Metal | Work Function (eV) |
|---|---|
| Caesium | 2.1 |
| Sodium | 2.3 |
| Zinc | 4.3 |
| Platinum | 5.7 |
Light demonstrates duality — sometimes behaving as a wave (interference, diffraction) and sometimes as a particle (photoelectric effect). In 1924, Louis de Broglie extended this idea to matter: every moving particle has an associated wave (matter wave).
The de Broglie wavelength: $$\lambda = \frac{h}{p} = \frac{h}{mv}$$
Where $p = mv$ is the momentum of the particle. A fast-moving electron with $v = 1 \times 10^7$ m s⁻¹ has: $\lambda = \frac{6.63\times10^{-34}}{9.11\times10^{-31} \times 10^7} \approx 7.3 \times 10^{-11}$ m — comparable to atomic spacings!
This explains why electron diffraction is observable when electrons are directed at a crystal lattice — the lattice spacing acts as a diffraction grating for the electron waves. Confirmed by Davisson and Germer (1927).
Heavier, faster particles have smaller wavelengths and exhibit less obvious wave properties. A cricket ball at 30 m s⁻¹ has $\lambda \approx 10^{-34}$ m — utterly undetectable.
graph TD
A[Electromagnetic Radiation] --> B[Wave behaviour: interference, diffraction]
A --> C[Particle behaviour: photoelectric effect, photon]
D[Matter, e.g. electrons] --> E[Particle behaviour: momentum, KE]
D --> F[Wave behaviour: electron diffraction, de Broglie λ = h/p]
In the Bohr model, electrons occupy discrete energy levels around the nucleus. Each level has a specific energy value (negative, because energy must be supplied to remove the electron). The ground state (n=1) is the lowest.
This explains emission spectra (bright lines on a dark background): excited atoms emit photons of specific frequencies when electrons de-excite, producing a unique spectral "fingerprint" for each element.
Absorption spectra (dark lines on a continuous spectrum): When white light passes through a cool gas, atoms absorb photons of specific frequencies, causing dark lines at exactly the same wavelengths as the emission lines.
The nucleus contains protons (charge +e) and neutrons (neutral), collectively called nucleons. Notation: $^A_Z X$ where $A$ = mass number (nucleons), $Z$ = atomic number (protons), and $A - Z$ = number of neutrons.
Isotopes have the same $Z$ but different $A$ — same element, different neutron count. Some isotopes are unstable and undergo radioactive decay.
| Type | Nature | Stopped by | Range in air | Ionising power |
|---|---|---|---|---|
| Alpha ($\alpha$) | $^4_2$He nucleus | Few cm of air / paper | ~5 cm | Highest |
| Beta⁻ ($\beta^-$) | Fast electron | Thin aluminium (~3mm) | ~1 m | Moderate |
| Gamma ($\gamma$) | EM radiation (photon) | Several cm of lead | Very large | Lowest |
Radioactive decay is spontaneous (unaffected by physical/chemical conditions) and random (impossible to predict which nucleus decays next). However, statistically, large samples follow an exponential decay law.
The activity $A$ (in Becquerels, Bq) = decays per second: $$A = -\frac{dN}{dt} = \lambda N$$
The decay constant $\lambda$ (s⁻¹) is the probability of decay per unit time for a single nucleus.
Exponential decay of nuclei: $$N = N_0 e^{-\lambda t}$$
Similarly: $A = A_0 e^{-\lambda t}$
The half-life ($t_{1/2}$) is the time for activity (or number of undecayed nuclei) to halve: $$t_{1/2} = \frac{\ln 2}{\lambda} = \frac{0.693}{\lambda}$$
Einstein's famous equation: $E = mc^2$ ($c = 3 \times 10^8$ m s⁻¹)
The mass defect ($\Delta m$) of a nucleus is the difference between the mass of its separated nucleons and its actual nuclear mass. This "missing" mass was converted to energy when the nucleus formed: $$E_{binding} = \Delta m \cdot c^2$$
The binding energy per nucleon peaks for iron-56 (~8.8 MeV/nucleon). Elements lighter than iron release energy by nuclear fusion (combining nuclei); elements heavier than iron release energy by nuclear fission (splitting nuclei).
Both processes release enormous energy — nuclear power stations and stars operate on these principles.