Isolobal species are those pairs whose frontier orbitals are the same in number, have similar symmetry, have approximately the same energy, and have the same number of electrons on them.
The isolobal principle is a concept that has been used in organometallic chemistry to relate the structure of organic and inorganic molecular fragments and to predict the bonding properties of organometallic compounds.
The isolobal Principle is used to describe the reactivity and chemical bonding of an organometallic compound.
A standard approach to determining structure is NMR, infrared spectroscopy, and X-ray diffraction.
Isolobal species are those pairs whose frontal lobes satisfy the following properties:
Isolobal species have similar symmetry.
Isolobal species have the nearby same energy.
They have the same number of electrons.
For example,
All these groups combine to form ordinary bonds like: