Atomic and Nuclear Structure: Comprehensive Study Notes

Historical Development of Atomic Models

  • Evolution timeline (chronological order)
    • Dalton’s "Billiard-Ball" Model (1803)
    • J. J. Thomson’s "Plum-Pudding" Model (1897)
    • Rutherford’s Nuclear Model (1911)
    • Bohr’s Planetary Model (1913)
    • Modern Quantum/Cloud Model (1920s →)
  • Significance
    • Each model arose to explain new experimental evidence (mass measurements, discharge-tube work, scattering data, line spectra)
    • Demonstrates the scientific method: hypothesis → experiment → refinement

Dalton’s Atomic Theory (1803)

  • Motivated by two empirical laws
    • Law of Conservation of Matter (Lavoisier, 1780s)
    • Law of Definite Proportions (Proust, ~1800)
  • Core Postulates
    • Matter is composed of tiny, indivisible, indestructible particles called atoms
    • Atoms of the same element are identical in mass, size, and other properties
    • Atoms of different elements differ in these properties
    • Atoms cannot transmute into atoms of another element
    • Chemical change = breaking/formation of bonds and rearrangement of atoms
  • Limitations / Later Modifications
    • Could not explain variations in valency & mass between elements
    • Discovery of isotopes (same Z, different AA) & isobars (different Z, same AA)
    • Sub-atomic particles (e⁻, p⁺, n⁰) proved atoms are divisible

J. J. Thomson’s Plum-Pudding Model (1897)

  • Experimental trigger: cathode-ray deflection → discovery of the electron (first sub-atomic particle)
  • Postulates
    • Atom overall electrically neutral
    • Positive charge spread uniformly throughout a sphere
    • Electrons ("negatively electrified corpuscles") embedded like plums in a pudding
    • Electrons are mobile inside the positive matrix → heating yields radiation
  • Limitations
    • Mass treated as uniformly distributed; ignores concentrated nucleus
    • Static: no provision for electron motion stability
    • Cannot explain large-angle scattering of α\alpha-particles (Rutherford)
    • Fails to describe atomic spectra or bonding mechanism

Rutherford’s α\alpha-Particle Scattering Experiment (1909–1911)

  • Method
    • Narrow beam of high-speed α(He2+)\alpha\,(\text{He}^{2+}) particles fired at thin gold foil
    • Scattered particles detected via a movable fluorescent screen/microscope
  • Key Observations
    • ≈ 99 % passed straight through (little/no deflection)
    • Small fraction deflected at small angles
    • Very few deflected at large angles; some rebounded (
      θ180\theta \approx 180^{\circ})
  • Conclusions
    • Atom mostly empty space
    • Positive charge & almost all mass concentrated in a tiny, dense core → nucleus
    • Electrons orbit the nucleus to preserve electrical neutrality
    • Greater atomic number ⇒ more protons ⇒ stronger repulsion ⇒ larger deflection
  • Rutherford/Nuclear Model
    • Miniature solar system: electrons orbit like planets; nucleus at center
  • Limitation
    • Classical electrodynamics: orbiting (accelerating) charges should radiate energy continuously → electrons should spiral into nucleus, yet atoms are stable

Bohr’s Planetary (Quantized) Model (1913)

  • Introduced to resolve Rutherford’s stability & spectral issues
  • Arbitrary Postulates
    1. Electrons occupy "stationary" orbits in which they do NOT radiate
    2. Allowed orbits possess discrete energies; energy is quantized
    3. Radiation emitted/absorbed only when an electron transitions between orbits: E=E<em>highE</em>low=hfE = E<em>{\text{high}} - E</em>{\text{low}} = h f
    4. Angular momentum quantized: L=nL = n\hbar where =h2π\hbar = \dfrac{h}{2\pi} and n=1,2,3,n = 1,2,3,\dots
  • Successes
    • Correctly predicted discrete hydrogen spectrum lines
    • Explained Rydberg formula
  • Shortcomings
    • Works exactly only for one-electron systems (H, He⁺, Li²⁺)
    • Lacked mechanism for quantization → remedied by full quantum mechanics

Introduction to Quantum Mechanical Model

  • Electrons described by wavefunctions (orbitals) rather than fixed orbits
  • Each orbital specified by three quantum numbers (n, l, mlm_l) that set size, shape, orientation
    1. Principal quantum number nn (1, 2, 3…)
    • Determines energy level & average radial distance
    1. Angular momentum (azimuthal) quantum number ll (0 → n1n-1)
    • Determines orbital shape (s, p, d, f …)
    1. Magnetic quantum number mlm_l (–ll … 0 … +ll)
    • Determines orientation; number of allowed mlm_l values = 2l+12l+1
  • Worked Example (n = 3)
    • l=0,1,2l = 0,1,2
    • mlm_l possibilities: 0 | –1,0,+1 | –2,–1,0,+1,+2 → 9 orbitals total
  • Energy shells vs. subshells
    • Shell = fixed n; Subshell = fixed n & l (e.g., 3p has n = 3, l = 1)

Sub-Atomic Particles & Atomic Structure

  • Three fundamental particles
    • Electron (e⁻): charge = –e, mass 9.11×1031kg9.11\times10^{-31}\,\text{kg}, outside nucleus
    • Proton (p⁺): charge = +e, mass 1.67×1027kg1.67\times10^{-27}\,\text{kg}, inside nucleus
    • Neutron (n⁰): charge 0, mass 1.67×1027kg1.67\times10^{-27}\,\text{kg}, inside nucleus
  • Mass hierarchy: m<em>pm</em>n2000mem<em>p \approx m</em>n \approx 2000\,m_e ⇒ nucleus accounts for > 99.9 % of atomic mass

The Atomic Nucleus

  • Radius ≈ 1015m10^{-15}\,\text{m} (femtometre); entire atom ≈ 1010m10^{-10}\,\text{m} → nucleus is ~10510^{5} times smaller in diameter yet holds almost all mass
  • Composition: Z protons + N neutrons
  • Charge neutrality ⇒ # electrons = Z under normal conditions
  • Ion: atom missing/extra electron(s) → net charge

Nuclear & Electromagnetic Forces

  • Electromagnetic force: like charges repel, unlike attract; binds e⁻ to nucleus
  • Nuclear (strong) force
    • Attractive between nucleons (p & n) at ranges ≲ 2–3 fm
    • ≈ 100× stronger than EM at that scale; acts as "glue" preventing Coulomb explosion of multi-proton nuclei
  • Practical impact: stability of heavy nuclei, radioactivity, nuclear energy & medicine

Terminology & Notation

  • Atomic number: ZZ = # protons ⇒ element identity
  • Neutron number: NN = # neutrons
  • Mass number: A=Z+NA = Z + N
  • Nuclide symbol: A<em>ZX{}^{A}<em>{Z}\text{X} where X = chemical symbol (e.g., 238</em>92U^{238}</em>{92}\text{U})
  • Element: collection of atoms with same Z
  • Isotopes: same Z, different A (e.g., 12C,13C,14C^{12}\text{C}, ^{13}\text{C}, ^{14}\text{C})
    • Identical chemical behaviour (depends on electrons)
    • Varied nuclear behaviour (stability, radioactivity)
    • Medical imaging uses: PET (\beta⁺ emitters), cancer radiotherapy (radio-isotopes)
  • Isobars: different Z, same A (e.g., 40<em>18Ar^{40}<em>{18}\text{Ar} & 40</em>20Ca^{40}</em>{20}\text{Ca})

Energy Quantization & Spectra

  • Emission or absorption occurs at discrete frequencies ff such that
    E=hfE = h f
  • Atomic line spectra (e.g., hydrogen Balmer series) validate quantization; contradict classical expectation of continuous spectra

Ethical, Philosophical & Real-World Connections

  • Scientific progress: iterative refinement; disproving "indivisible" atom led to modern electronics, nuclear medicine
  • Responsible use of nuclear knowledge: radiation therapy vs. nuclear weapons
  • Imaging technology (context of course): PET, SPECT, MRI depend on nuclear & electronic properties explored by these models
  • Dalton → conservation laws → foundation of stoichiometry
  • Thomson → discovery of e⁻ → beginning of particle physics
  • Rutherford → nuclear model → pathway to nuclear energy & medicine
  • Bohr & quantum numbers → underpin modern quantum chemistry, periodic table structure, semiconductor physics
  • Strong vs. electromagnetic forces → basis for nuclear stability, reactor design, radiological safety