Abstract

The ground and 1s core hole state molecular wave functions of CH4, NH3, H2O, and HF obtained from Xα–SW calculations using the touching spheres (TS) and overlapping spheres (OS) approximations are used to calculate the intensity of shakeup satellites observed in their ls core level photoelectron spectra. The sudden approximation was assumed in the calculation. In case of TS Xα–SW wave functions, the one electron overlap integral inside the intersphere was calculated via Green’s theorem. For OS Xα–SW wave functions, the integration over the awkwardly shaped intersphere region was circumvented by distributing the intersphere charge into the atomic spheres according to the charge partition scheme suggested by Case and Karplus. Our results show that there are no significant differences between the shakeup energies calculated from the TS and OS approximations. However, shakeup intensities calculated from TS Xα–SW wave functions are more reliable and in better numerical agreement with experiment.

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