Electron orbital: Difference between revisions

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==Applications==
==Applications==
Before the advent of electronic computers, orbitals (molecular as well as atomic) were used extensively in qualitative arguments explaining several properties of atoms and molecules. Orbitals still play this role in introductory texts and also in organic chemistry, where orbitals serve in the explanation of some reaction mechanisms, for instance in the [[Woodward-Hoffmann rules]].  
Before the advent of electronic computers, orbitals (molecular as well as atomic) were used extensively in qualitative arguments explaining several properties of atoms and molecules. Orbitals still play this role in introductory texts and also in organic chemistry, where orbitals serve in the explanation of some reaction mechanisms, for instance in the [[Woodward-Hoffmann rules]].  
In modern computational quantum chemistry the role of atomic orbitals is  different; they serve as a convenient expansion basis, comparable to powers of ''x'' in a Taylor expansion of a function ''f(x)'', or sines and cosines in a Fourier series. Below, the role of atomic and molecular orbitals in qualitative theories will be discussed. The final subsection is devoted to the use of AOs in modern quantum chemistry.  
In modern computational quantum chemistry the role of atomic orbitals is  different; they serve as a convenient expansion basis, comparable to powers of ''x'' in a Taylor expansion of a function ''f(x)'', or sines and cosines in a Fourier series. Below, the role of molecular orbitals in qualitative theories will be discussed.  
===Atomic orbitals===
===Atomic orbitals===
Bohr<ref>N. Bohr, Zeitschrift für Physik, vol. '''9''', p. 1 (1922)</ref> was the first to see
Originally AOs were defined as approximate  solutions of atomic Schrödinger equations,
how atomic orbitals form a basis for an understanding of the [[Periodic Table]] of elements. In Bohr's explanation of the Periodic Table, the atomic orbitals carry the same labels as [[hydrogen-like atom|hydrogen orbitals]]. That is, they have  a principal quantum number ''n'' and a letter (''s'', ''p'',...) designating the [[azimuthal quantum number]] (angular momentum quantum number) ''l''.  
see the section ''solution of the atomic Schrödinger equation'' in [[atomic orbital]]'' for more on this.  


The quantum numbers ''n'' and ''l'' are also valid labels for AOs that arise as solutions from an ''N''-electron [[independent-particle model]] with a central (spherically symmetric) potential field. The [[central field]] approximation, which entails the spherical averaging of the field due to the electrons, is necessary to have ''l'' as a good quantum number.  An independent-particle model leads to an effective-one-electron Schrödinger equation&mdash;one electron in the averaged (mean) field of the other electrons. The solutions  of a mean field equation are orbitals and orbital-energies. So, orbitals and orbital-energies do not only arise in real one-electron systems, such as the H-atom,  but also in independent-particle approximations of  ''N''-electron systems.
Recently, AOs are simply seen as convenient basis functions for quantum chemical computations.
 
See the section ''AO basis sets'' in the article [[atomic orbital]] for more on the use of atomic orbitals in quantum chemistry. See [[Slater orbital]]
Two major differences between an atomic effective-one-electron  model and the hydrogen-like atom  are:
for the explicit analytic form of orbitals and see [[Gauss type orbitals]] for a discussion
# The radial solutions are given numerically, and are no longer known analytic functions, such as the Laguerre functions for the hydrogen-like atom. The angular parts, however, are the same analytic functions (spherical harmonics) as in the case of the hydrogen-like-atom.
of the type of AOs that are most frequently used in computations.
# The high degeneracy of the H-atom is lifted. In the hydrogen atom all orbitals of certain ''n'' are degenerate.  For instance, the orbitals in the ''n'' = 4 shell: 4''s'', 4''p'', 4''d'', and 4''f'', all have the same energy (proportional to 1/''n''<sup>2</sup> = 1/16). In the ''N''-electron atom  only the AOs of the  same azimuthal quantum number ''l'' are degenerate.  
 
Note the role of the principal quantum number ''n'' in the effective-one-electron model. It is simply an index that counts increasing orbital energies, starting at ''n'' = ''l'' + 1 (to be in line with the hydrogen-like AOs). In summary,  an atomic orbital of an ''N''-electron atom is labeled by ''n'' (indicating its energy) and ''l'' (indicating its angular momentum).
 
It is found<ref>J. C. Slater, ''Quantum Theory of Atomic Structure'', vol. I, McGraw-Hill, New York (1960), p. 193</ref> that the orbitals arising from the central field, independent-particle model applied to different atoms have the following order in increasing energy
:<em> 1s, 2s, 2p, 3s, 3p, 3d, 4s, 4p, 4d, 5s, 5p, 6s, 4f, 5d, 6p, 7s, 5f, 6d.</em>
 
For some atoms the order of 3''d'' and 4''s'' is flipped and for some other atoms the order of 4''d'' and 5''s'' is flipped.  Note further that, for example 4''f'' is ''not'' degenerate with 4''d'', which is the case for hydrogen-like atoms.
 
Knowing this order, one can build up the atoms in the Periodic Table by the ''Aufbau'' (building-up) principle: fill orbitals in increasing energy. Doing this one must obey the Pauli exclusion principle that forbids more than two electrons per spatial orbital. Allowed is at most one electron with &alpha; spin  and one with &beta; spin. In addition recall  that there are 2''l''+1 orbitals of certain ''l''.
For instance, the neon atom (atomic number ''Z'' = 10) has the electronic configuration (''n'' = 1 and ''n'' = 2 shells are completely filled):
:<math>{\scriptstyle  1s^2\, 2s^2\, 2p^6,} </math>
meaning two electrons are in the 1''s'', two electrons in the 2''s'', and six electrons in the 2''p'' AOs. Similarly, chlorine (''Z'' = 17) has
:<math>{\scriptstyle 1s^2\, 2s^2\, 2p^6\, 3s^2\, 3p^5\,}. </math>
For more details the article [[Periodic Table]] may be consulted. A list of the electronic configurations of the ground states of the first 94 elements may be found [[Atomic Electron configuration|here]].


===Molecular orbitals===
===Molecular orbitals===
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If we apply the model to He<sub>2</sub>, which has four electrons, we find that we must place two electrons in the bonding orbital and two electrons in the ''antibonding MO'' &sigma;<sub>''u''</sub>, with the total energy being 2&beta; &minus; 2&beta; = 0. So, this simple application of molecular orbital theory predicts that H<sub>2</sub> is bound and that He<sub>2</sub> is not, which is in agreement with the observed facts.
If we apply the model to He<sub>2</sub>, which has four electrons, we find that we must place two electrons in the bonding orbital and two electrons in the ''antibonding MO'' &sigma;<sub>''u''</sub>, with the total energy being 2&beta; &minus; 2&beta; = 0. So, this simple application of molecular orbital theory predicts that H<sub>2</sub> is bound and that He<sub>2</sub> is not, which is in agreement with the observed facts.
===Atomic orbital basis sets===
As stated above, in computational quantum chemistry atomic orbitals are used as a mathematical device to obtain good approximations of ''N''-electron molecular wave functions&mdash;solutions of the time-independent electronic Schrödinger equation.
A computation of a molecular wave function usually goes through the following steps:
# A geometry of the molecule is chosen (in accordance with the [[Born-Oppenheimer approximation]] the nuclei are clamped in space).
# A set of AOs is chosen which are centered on the nuclei. Sometimes the AO set is augmented with orbitals in the middle of bonds, where there are no nuclei. Preferably the AO basis set is as close as possible to a complete basis of one-electron [[Hilbert space]], <math>{\scriptstyle L^2[\mathbb{R}^3]}</math>, but computer time is a practical limit. (Many methods require computer times proportional to ''n''<sup>6</sup> or ''n''<sup>7</sup>, where ''n'' is the number of AOs.)
# An LCAO [[Hartree-Fock]] calculation yields the MO coefficients ''c''<sub>''A i''</sub> and the same number of MOs as AOs (namely ''n'').
# The MOs are used in a [[post-Hartree-Fock]] calculation ([[configuration interaction]], [[Møller-Plesset]] perturbation theory, [[coupled cluster]] theory, etc.).
The AOs and MOs spanning the very same orbital subspace of one-electron Hilbert space,  it would be conceivable to skip the Hartree-Fock calculation. However, it turns out that the post-Hartree-Fock methods converge much better when they are based on MOs instead of on (orthogonalized) AOs.
The size of an AO basis is of crucial importance. The qualitative, pre-computer, MO-theoretical studies were invariably based on ''minimum basis sets''. That is, only orbitals  occupied in the free atoms were included in the basis. (But note that, for instance for the ground state boron atom with its electron configuration 1''s''<sup>2</sup>2''s''<sup>2</sup>2''p'', it cannot be said whether 2''p''<sub>''x''</sub>,  2''p''<sub>''y''</sub>, or  2''p''<sub>''z''</sub> is occupied. In such a case all three degenerate ''p'' orbitals are included in the minimum basis set). It was natural  that the first computer calculations followed this pattern and  applied minimum basis sets. However, it soon was found that such  basis sets give very disappointing results. After this became clear in the late 1960s and early 1970s, search for good AO basis became an important subject of research.
For the mathematical definition of basis sets, we  refer to the article [[Gauss type orbitals]] (GTOs), because the majority of present-day computer programs handle only GTOs. In the GTO article the concepts of [[Gaussian type orbitals#Primitive GTOs and contracted sets|primitive orbital]] and [[Gaussian type orbitals#Primitive GTOs and contracted sets|contracted set]] are introduced. In a minimum GTO basis set (also known as a ''single-zeta basis set'') every atomic orbital  occupied in the free atom is represented by a single contracted set. The term "single-zeta" is historic and refers back to the days that [[Slater orbital|Slater type orbital]]s were universally used and to the fact that the screening constant in an STO is conventionally indicated by the Greek letter zeta (&zeta;). Single-zeta (SZ) basis sets giving poor quantitative results, the next step is the use of ''double-zeta'' (DZ) basis set, which involves a doubling of the SZ basis. Triple-zeta (TZ) (tripling of the minimum basis), quadruple-zeta (QZ), quintuple-zeta (5Z), sextuple-zeta (6Z) basis sets all have been proposed and have been constructed.
For instance a QZ GTO basis for HCN includes : 4 ''s''-orbitals (''s''-type contracted sets) on H, 8 ''s''-orbitals  on both C and N, 4 ''p''<sub>''x''</sub>-, 4 ''p''<sub>''y''</sub>-, and 4 ''p''<sub>''z''</sub>-orbitals  on C and N.
In all these cases the construction of the contracted set (AO) involves  the determination of the exponents of the [[Gaussian type orbitals#Primitive GTOs and contracted sets|primitive Gaussians]] and the corresponding [[Gaussian type orbitals#Primitive GTOs and contracted sets|contraction coefficients]].
It is known that an atom polarizes (gets a [[dipole moment]]) under influence of an external electric field. It is also known that, in the presence of such a field, AOs of higher ''l'' quantum numbers must be included in the basis in order to obtain reliable results. When, for instance, the ground state boron atom (1''s''<sup>2</sup>2''s''<sup>2</sup>2''p'') is polarized, there will be a mixing, linear in the strength of the external field, between 2''p'' and 3''d''. That is, to describe the polarization of the boron atom  correctly, one or more 3''d'' sets (sets of five degenerate AOs) must be added to the basis of boron. Since in molecules strong electric fields, due to the nuclei, are present, it stands to reason that ''polarization functions'' improve the computational results. For an atom that only has occupied ''s'' orbitals, like hydrogen and helium,  polarization functions start at ''l'' = 1. For atoms such as boron with occupied ''p''-orbitals, the polarization functions are by definition  ''d'', ''f'', ''g'', etc. orbitals.
As a final conclusion it must be pointed out that the present-day elaborate AO bases do not have the  physical meaning that was attached to AOs in precomputer times. The AOs are now looked upon as building bricks in  a numerical approximation, no chemical of physical conclusions  are to be drawn from the AOs themselves.  The relevant conclusions about nature emerge from the final computational results. Especially in the post Hartree-Fock methods, the contribution of the AOs to the conclusions is deeply hidden in the output and not at all transparent.


==References and notes==
==References and notes==
<references />
<references />

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In quantum chemistry, an electron orbital (or more often just orbital) is a synonym for a one-electron function. Here "orbital" is used as a noun. In quantum mechanics, the adjective orbital is often used as a synonym of "spatial" (as in orbital angular momentum), in contrast to spin (as in spin angular momentum).

The majority of quantum chemical methods expect that an orbital has a finite norm, i.e., that the orbital is normalizable (quadratically integrable), and hence this requirement is often added to the definition.

Outside of quantum chemistry an orbital is often seen as a wave function. This point of view is a narrowing of the quantum chemical definition, but not contradictory to it, provided a wave function is seen in this context as a solution of an (effective) one-electron Schrödinger equation. Indeed, in the past quantum chemists, too, distinguished one-electron functions from orbitals, the former being fairly arbitrary and the latter being solutions of certain one-electron Schrödinger equations. This distinction faded away from quantum chemistry, leading to the present definition as "normalizable one-electron function."

Usually on distinguishes two kinds of orbitals: atomic orbitals and molecular orbitals. Atomic orbitals are expressed with respect to one Cartesian system of axes centered on a single atom. Molecular orbitals (MOs) are "spread out" over a molecule. Usually this is a consequence of an MO being a linear combination (weighted sum) of atomic orbitals centered on different atoms.

Definitions of orbitals

Several kinds of orbitals can be distinguished.

Atomic orbital

See the article atomic orbital

Molecular orbital

The second kind of orbital is the molecular orbital (MO). Such a one-electron function depends on several vectors: rA1, rB1, rC1, ... where A, B, C, ... are different points in space (usually nuclear positions). The oldest example of an MO (without use of the name MO yet) is in the work of Burrau (1927) on the single-electron ion H2+. Burrau applied spheroidal coordinates (a bipolar coordinate system) to describe the wave functions of the electron of H2+.

Lennard-Jones[1] introduced the following linear combination of atomic orbitals (LCAO) way of writing an MO φ:

where A runs over Nnuc different points in space (usually A runs over all the nuclei of a molecule, hence the name molecular orbital), and i runs over the nA different AOs centered at A. The complex coefficients c Ai can be calculated by any of the existing effective-one-electron quantum chemical methods. Examples of such methods are the Hückel method and the Hartree-Fock method.

Spinorbitals

The AOs and MOs defined so far depend only on the spatial coordinate vector rA1 of electron 1. In addition, an electron has a spin coordinate μ, which can have two values: spin-up or spin-down. A complete set of functions of μ consists of two functions only, traditionally these are denoted by α(μ) and β(μ). These functions are eigenfunctions of the z-component sz of the spin angular momentum operator with eigenvalues ±½.

Spin atomic orbital

The most general spin atomic orbital of electron 1 is of the form

which in general is not an eigenfunction of sz. More common is the use of either

which are eigenfunctions of sz. Since it is rare that different AOs are used for spin-up and spin-down electrons, we dropped the superscripts + and −.

Spin molecular orbital

A spin molecular orbital is usually either

Here the superscripts + and − might be necessary, because some quantum chemical methods distinguish the spatial wave functions of electrons with different spins. These are the so-called different orbitals for different spins (DODS) (or spin-unrestricted) methods. However, many quantum chemical methods apply the spin-restriction:

Chemists express this spin-restriction by stating that two electrons [electron 1 with spin up (α), and electron 2 with spin down (β)] are placed in the same spatial orbital φ. This means that the total N-electron wave function contains a factor of the type φ(r1)α(μ1)φ(r2)β(μ2).

History of term

Orbit is an old noun introduced by Johannes Kepler in 1609 to describe the paths of the earth and the planets. The adjective "orbital" had (and still has) the meaning "relating to an orbit". When Ernest Rutherford in 1911 postulated his planetary model of the atom (the nucleus as the Sun, and the electrons as the planets) it was natural to call the paths of the electrons "orbits". Bohr, although he was the first to recognize (1913) orbits as stationary states of the hydrogen atom, used the word as well. However, after Schrödinger (1926) had solved his wave equation for the hydrogen atom (see this article for details), it became clear that the electronic "orbits" did not resemble planetary orbits at all. The wave functions of the hydrogen electron are time-independent and smeared out. They are more like unmoving clouds than like planetary orbits. As a matter of fact, the angular parts of the hydrogen wave functions are spherical harmonics and hence they have the same appearance as spherical harmonics. (See spherical harmonics for a few graphical illustrations).

In the 1920s electron spin was discovered, whereupon the adjective "orbital" started to be used in the meaning of "non-spin", that is, as a synonym of "spatial". In scientific papers of around 1930 one finds discussions about "orbital degeneracy", meaning that the spatial (non-spin) parts of several one-electron wave functions have the same energy. Also the terms orbital- and spin-angular momentum date form these days.

In 1932 Robert S. Mulliken[2] coined the noun "orbital". He wrote: From here on, one-electron orbital wave functions will be referred to for brevity as orbitals.[3] Then he went on to distinguish atomic and molecular orbitals.

Later the somewhat unfortunate term "spinorbital" was introduced for the product functions φ(r1)α(μ1) and φ(r1)β(μ1) in which φ(r1) has the tautological name "spatial orbital" and α(μ1) and β(μ1) are called "one-electron spin functions". The term "spinorbital" is unfortunate because it merges in one word the concepts of spin and orbital, which were distinguished carefully by early writers on quantum mechanics. For instance, one of the pioneers of theoretical chemistry, Walter Heitler, juxtaposes two-electron spin functions and two-electron orbital functions.[4] In the phrase "two-electron orbital function", Heitler uses orbital as an adjective synonymous with spatial (non-spin). Note, parenthetically, that Heitler does not refer to a "two-electron orbital", (there is no such thing as a two-electron orbital!). However, an inexperienced reader may easily and erroneously interpret the term "two-electron orbital function" as "two-electron orbital".

Applications

Before the advent of electronic computers, orbitals (molecular as well as atomic) were used extensively in qualitative arguments explaining several properties of atoms and molecules. Orbitals still play this role in introductory texts and also in organic chemistry, where orbitals serve in the explanation of some reaction mechanisms, for instance in the Woodward-Hoffmann rules. In modern computational quantum chemistry the role of atomic orbitals is different; they serve as a convenient expansion basis, comparable to powers of x in a Taylor expansion of a function f(x), or sines and cosines in a Fourier series. Below, the role of molecular orbitals in qualitative theories will be discussed.

Atomic orbitals

Originally AOs were defined as approximate solutions of atomic Schrödinger equations, see the section solution of the atomic Schrödinger equation in atomic orbital for more on this.

Recently, AOs are simply seen as convenient basis functions for quantum chemical computations. See the section AO basis sets in the article atomic orbital for more on the use of atomic orbitals in quantum chemistry. See Slater orbital for the explicit analytic form of orbitals and see Gauss type orbitals for a discussion of the type of AOs that are most frequently used in computations.

Molecular orbitals

In the hands of Friedrich Hund, Robert S. Mulliken, John Lennard-Jones, and others, molecular orbital theory was established firmly in the 1930s as a (mostly qualitative) theory explaining much of chemical bonding, especially the bonding in diatomic molecules.

MO energy level diagram for H2

To give the flavor of the theory we look at the simplest molecule: H2. The two hydrogen atoms, labeled A and B, each have one electron (a red arrow in the figure) in an 1s atomic orbital (AO). These AOs are labeled in the figure 1sA and 1sB. When the atoms start to interact the AOs combine linearly to two molecular orbitals:

Earlier in this article a general expression for an LCAO-MO was given. In the present example of the σg MO of H2, we have Nnuc = 2, nA = nB = 1, χA1 = 1sA, χB1 = 1sB, cA1 = cB1 = Ng. With regard to the form of the MOs the following: Because both hydrogen atoms are identical, the molecule has reflection symmetry with respect to a mirror plane halfway the H—H bond and perpendicular to it. It is one of the basic assumptions in quantum mechanics that wave functions show the symmetry of the system. [Technically: solutions of the Schrödinger equation belong to a subspace of Hilbert (function) space that is irreducible under the symmetry group of the system]. Clearly σg is symmetric (is even, stays the same) under

while σu changes sign (is antisymmetric, is odd). The Greek letter σ indicates invariance under rotation around the bond axis. The subscripts g and u stand for the German words gerade (even) and ungerade (odd). So, because of the high symmetry of the molecule we can immediately write down two molecular orbitals, which evidently are linear combinations of atomic orbitals.

The normalization factors Ng and Nu and the orbital energies are still to be computed. The normalization constants follow from requiring the MOs to be normalized to unity. In the computation we will use the bra-ket notation for the integral over xA1, yA1, and zA1 (or over xB1, yB1, and zB1 when that is easier).

We used here that the AOs are normalized to unity and that the overlap integral is real

Applying the same procedure for Nu, we find for the two normalization factors

At this point one often assumes that S ≅ 0, so that both normalization factors are equal to ½√2.

In order to calculate the energy of an orbital we introduce an effective-one-electron energy operator (Hamiltonian) h,

Since A and B are identical atoms equipped with identical AOs, we were allowed to use

Likewise

The energy term β is negative (causes the attraction between the atoms). One may tempted to assume that q = −½ hartree (the energy of the 1s orbital in the free atom). This is not the case, however, because h contains the attraction with both nuclei, so that q is distance dependent.

If we now look at the figure in which energies are increasing in vertical direction, we see that the two AOs are at the same energy level q, and that the energy of σg is a distance |β| below this level, while the energy of σu is a distance |β| above this level. In the present simple-minded effective-one-electron model we can simply add the orbital energies and find that the bonding energy in H2 is 2β (two electrons in the bonding MO σg, ignoring the distance dependence of q). This model predicts that the bonding energy in the one-electron ion H2+ is half that of H2, which is correct within a 20% margin.

If we apply the model to He2, which has four electrons, we find that we must place two electrons in the bonding orbital and two electrons in the antibonding MO σu, with the total energy being 2β − 2β = 0. So, this simple application of molecular orbital theory predicts that H2 is bound and that He2 is not, which is in agreement with the observed facts.

References and notes

  1. J. E.Lennard-Jones, The Electronic Structure of some Diatomic Molecules;; Trans. Faraday Soc. vol 25, p. 668 (1929).
  2. R. S. Mulliken, Electronic Structures of Molecules and Valence. II General Considerations, Physical Review, vol. 41, pp. 49-71 (1932)
  3. Note that here, evidently, Mulliken uses the adjective "orbital" in the meaning of "spatial" (non-spin) and defines an orbital as, what is now called a "spatial orbital".
  4. W. Heitler, Elementary Wave Mechanics, 2nd edition (1956) Clarendon Press, Oxford, UK.