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Chemistry · Ch 2 — Quantum Mechanical Model of Atom

Summary

Summary

  • Atoms were once believed to be non-divisible, until the discovery of sub-atomic particles. J.J. Thomson proposed the atom as a positively charged sphere with electrons embedded in it, but this could not explain why atoms are stable.
  • Rutherford's alpha-scattering experiment introduced the nucleus - a tiny, positively charged core with negatively charged electrons revolving around it at high speed. Bohr modified this picture by introducing quantised, non-radiating stationary orbits.
  • Louis de Broglie proposed that all matter has dual (wave and particle) character, with de Broglie wavelength λ=h/mv=h/mev\lambda=h/mv=h/m_ev - significant only for a microscopic particle such as an electron. Davisson and Germer proved the electron's wave nature experimentally through electron diffraction.
  • For a microscopic particle, position and momentum cannot both be measured simultaneously with full precision - Heisenberg's uncertainty principle, Δx⋅Δp≥h/4π\Delta x\cdot\Delta p\geq h/4\pi.
  • De Broglie's concept and Heisenberg's principle together led to the quantum mechanical model of the atom. Schrödinger's wave equation, H^ψ=Eψ\hat{H}\psi=E\psi, is exactly solvable for one-electron systems (H, He+\text{He}^+, etc.) but is far too complex to solve exactly for multi-electron systems. It is solvable only for certain energy values (eigenvalues), whose corresponding wavefunctions are called atomic orbitals. ψ\psi itself has no physical meaning, but ∣ψ∣2|\psi|^2 gives the probability of finding the electron. This is the origin of the orbital: the three-dimensional region of space where the probability of finding the electron is maximum.
  • An electron in an orbital is described by four quantum numbers: principal (nn, the shell/energy level), azimuthal (ll, the subshell/shape), magnetic (mm, the spatial orientation) and spin (ss, the electron's intrinsic spin).
  • The general one-electron solution in spherical polar coordinates is Ψ(r,θ,φ)=R(r)⋅f(θ)⋅g(φ)\Psi(r,\theta,\varphi)=R(r)\cdot f(\theta)\cdot g(\varphi). Plotting 4πr2⋅R(r)24\pi r^2\cdot R(r)^2 against rr gives the radial distribution curve, with (n−l−1)(n-l-1) radial nodes; the angular distribution gives the orbital's boundary shape, with ll angular nodes. s orbitals are spherical; p orbitals are dumbbell-shaped; d orbitals are clover-leaf shaped. …