Organic Mechanisms. Xiaoping Sun

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Organic Mechanisms - Xiaoping Sun

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orbitals.

equation equation

      Since 1sA and 1sB are identical, their contributions to each of the MOs (σ1s and σ1s*) should be equal. Therefore, we have c1 = c2 = c (>0) and c1′ = c2′ = c′ (>0).

      In order to normalize the molecular orbital σ1s, the following integral must have the value unity

equation

      where dτ is the volume factor.

      Therefore,

equation equation

      Since the wavefunction of the 1s orbital is normalized, we have

equation

      The term S = ∫(1sA1sB)dτ is referred to as the overlap integral. Therefore, we have

equation equation

      Similarly, by normalizing σ1s*, we can obtain

equation

      (1.60)equation

      (1.61)equation

      The overlap integral S is determined by the internuclear distance. At equilibrium H─H bond distance, the electron density of σ1s in the midregion of the bond is maximum, while the electron density of σ1s* in the midregion of the bond is zero. Therefore, σ1s is called bonding molecular orbital. It is formed by constructive interaction (overlap) of two atomic orbitals and is responsible for the formation of the H─H σ bond. σ1s* is called antibonding molecular orbital. It is formed by destructive interaction (overlap) of two atomic orbitals and is responsible for dissociation of the H─H bond. Since each of the 1s orbitals makes the same contribution to the bonding σ1s and antibonding σ1s* MOs, the coefficients 1/[2(1 + S)]1/2 and 1/[2(1 − S)]1/2 are often omitted when writing the LCAOs. Therefore, the bonding and antibonding MOs in H2 can be simply written as σ1s = 1sA + 1sB and σ1s* = 1sA − 1sB.

Schematic illustration of the formation of the fluorine molecule (F2) from two fluorine (F) atoms. Schematic illustration of the formation of (a) the C-C π bond from two equivalent p orbitals and (b) the C-O π bond from two nonequivalent p orbitals. equation equation

      The above equations show that for the formation of πp, the p orbital in oxygen (more electronegative) makes a greater contribution than does the p orbital in carbon (less electronegative). For the formation of πp*, the p orbital in carbon (less electronegative) makes a greater contribution than does the p orbital in oxygen (more electronegative). In each case, the bonding πp MO is responsible for the formation of a π bond, and antibonding orbital πp* is responsible for dissociation of the

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