Abstract
In the transition regions of the periodic table of the elements, atomic d or f orbitals undergo a fairly sudden change from hydrogenic to fully collapsed form. This transition involves a large reduction in the mean orbital radius - by about 95% for the 4f orbital - and results in corresponding qualitatitive changes in physical processes sensitive to orbital size (e. g. excitation cross sections, bonding character). It is caused by a shift, as the nuclear charge Z increases, in the close balance between repulsive centrifugal and attractive atomic forces on the electron. The balance can also be tilted within a given element in the transition region, for instance by a change in the occupancy of its core or valence orbitals, or by the formation of a molecular bond. Transition region elements are thus characterized by an unusual sensitivity of gross orbital properties to external perturbations; and, from the standpoint of theoretical representation, to the effects of electron correlation, LS term dependence, and special relativity.
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Clark, C.W., Lucatorto, T.B. (1987). Giant Resonances in the Transition Regions of the Periodic Table. In: Connerade, J.P., Esteva, J.M., Karnatak, R.C. (eds) Giant Resonances in Atoms, Molecules, and Solids. NATO ASI Series, vol 151. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-2004-1_7
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