The classical view of the atom as an indivisible sphere, postulated by John Dalton in 1808, was challenged toward the close of the nineteenth century by a succession of electrical discharge experiments proving the existence of subatomic particles.
- The Electron (Cathode Rays): In 1897, J.J. Thomson investigated electrical discharge through rarefied gases in Crookes tubes at low pressure (~0.01 mm Hg) and high voltage (~10,000 V). Cathode rays traveled in straight lines, cast sharp shadows of opaque objects, exerted mechanical force on paddle wheels, and deflected toward the positive plate in electric and magnetic fields. Thomson determined their universal charge-to-mass ratio: \[\frac{e}{m_e} = 1.758820 \times 10^{11}\text{ C/kg}\] Robert A. Millikan (1909) determined the fundamental charge of the electron via the Oil Drop Experiment: \(e = -1.602176 \times 10^{-19}\text{ C}\). Consequently, the rest mass of the electron was calculated as: \[m_e = \frac{e}{e/m_e} = \frac{1.602176 \times 10^{-19}\text{ C}}{1.758820 \times 10^{11}\text{ C/kg}} = 9.109383 \times 10^{-31}\text{ kg} \approx \frac{1}{1837}\text{ u}\]
- The Proton (Anode / Canal Rays): E. Goldstein (1886) utilized a perforated cathode in discharge tubes and observed canal rays traveling toward the cathode. Unlike cathode rays, their \(e/m\) ratio depended upon the residual gas, reaching a maximum value when hydrogen was used: \(e/m = 9.58 \times 10^7\text{ C/kg}\). The particle was identified as the proton: charge \(+1.6022 \times 10^{-19}\text{ C}\), mass \(m_p = 1.67262 \times 10^{-27}\text{ kg} = 1.00727\text{ u}\).
- The Neutron: James Chadwick (1932) bombarded thin sheets of beryllium with high-velocity \(\alpha\)-particles and detected neutral penetrating radiation consisting of neutral particles with mass slightly greater than a proton: \[^9_4\text{Be} + ^4_2\alpha \rightarrow ^{12}_6\text{C} + ^1_0\text{n}\] Mass of neutron \(m_n = 1.67493 \times 10^{-27}\text{ kg} = 1.00866\text{ u}\).
Thomson (1898) proposed that an atom is a positively charged spherical cloud (~\(10^{-10}\text{ m}\) radius) with electrons embedded like raisins in a pudding. This model could not explain large-angle scattering of charged particles.
In 1911, Ernest Rutherford, Hans Geiger, and Ernest Marsden directed a collimated beam of \(5.5\text{ MeV}\) \(\alpha\)-particles (\(^4_2\text{He}^{2+}\)) onto an ultra-thin gold foil (~\(100\text{ nm}\) thick) surrounded by a fluorescent zinc sulfide (ZnS) screen:
- Observations: Most \(\alpha\)-particles (~99.9%) passed through undeflected; a small fraction (~1 in 8,000) was deflected by angles \(\theta > 90^\circ\); and extremely rarely (~1 in 20,000), an \(\alpha\)-particle bounced almost directly backward (\(\theta \approx 180^\circ\)).
- Conclusions & Nuclear Model: Most of the atom is empty space. All positive charge and virtually all mass are concentrated in an extraordinarily minute, dense central core termed the nucleus (radius \(r_N \sim 10^{-15}\text{ m}\) compared to atomic radius \(r_A \sim 10^{-10}\text{ m}\); volume fraction \(\sim 10^{-15}\)). Electrons orbit the nucleus in circular paths, held by electrostatic Coulombic attraction.
- Limitations of Rutherford Model:
- Instability under Classical Electrodynamics: According to Maxwell electromagnetic theory, an accelerating charged particle (in circular orbit) must continuously radiate energy. The electron would lose kinetic energy, spiral inward in \(\sim 10^{-8}\text{ s}\), and collapse into the nucleus.
- Failure to Explain Atomic Spectra: If the spiral is continuous, the emitted radiation must form a continuous spectrum; experimentally, atoms emit sharp, discrete line spectra.
| Term | Definition | Key Relationships / Examples |
|---|---|---|
| Atomic Number (\(Z\)) | Number of protons in the nucleus of an atom | \(Z = p = e\) (in a neutral atom) |
| Mass Number (\(A\)) | Total number of nucleons (protons + neutrons) | \(A = Z + n \implies n = A - Z\) |
| Isotopes | Nuclides of the same element with identical \(Z\) but different \(A\) | \(^1_1\text{H}, ^2_1\text{H}, ^3_1\text{H}\) and \(^{35}_{17}\text{Cl}, ^{37}_{17}\text{Cl}\) |
| Isobars | Nuclides of different elements with identical \(A\) but different \(Z\) | \(^{40}_{18}\text{Ar}, ^{40}_{19}\text{K}, ^{40}_{20}\text{Ca}\) |
| Isotones | Nuclides containing identical number of neutrons (\(A - Z\)) | \(^{14}_6\text{C}, ^{15}_7\text{N}, ^{16}_8\text{O}\) (all have 8 neutrons) |
| Isoelectronic Species | Atoms or ions possessing an identical number of electrons | \(\text{N}^{3-}, \text{O}^{2-}, \text{F}^-, \text{Ne}, \text{Na}^+, \text{Mg}^{2+}\) (all 10 electrons) |