Atomic silicon has ground configuration

PHYSICS · Multi-part · Fermi University Physics · Atomic, Molecular & Optical Physics · Many-electron atoms and the periodic table · Many-electron atoms and the periodic table

Deriving the Spectrum, Ch Many-electron terms, levels and Hund's rules

Problem

Atomic silicon has ground configuration 3p23p^2, giving the same terms as carbon's 2p22p^2: 3P^3P, 1D^1D, 1S^1S. The measured levels are 3P0=0 cm−1^3P_0=0\,\mathrm{cm^{-1}}, 3P1=77.115 cm−1^3P_1=77.115\,\mathrm{cm^{-1}}, 3P2=223.157 cm−1^3P_2=223.157\,\mathrm{cm^{-1}}, 1D2=6298.850 cm−1^1D_2=6298.850\,\mathrm{cm^{-1}}, 1S0=15394.370 cm−1^1S_0=15394.370\,\mathrm{cm^{-1}}. ((a)) Compute the (2J+1)(2J+1)-weighted centroid of the 3P^3P term. ((b)) The single-configuration Slater-integral treatment of p2p^2 predicts E(1S)−E(1D)E(1D)−E(3P)=32\dfrac{E(^1S)-E(^1D)}{E(^1D)-E(^3P)}=\dfrac32. Test this using the centroid from (a) in place of a single 3P^3P energy, and compare with carbon's measured value of 1.131.13. ((c)) Test the Lande interval rule on the 3P^3P term: compute the two intervals, their ratio, and the two estimates of ζLS\zeta_{LS} they give. State whether the term is normal or inverted. ((d)) Comment briefly on why silicon's Slater-integral ratio sits closer to 3/23/2 than carbon's does, given that both deviations are blamed on configuration interaction with same-parity configurations.

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