trini said:
from what i understand, the procedure for determining the energy of an electron in a particular energy state is done by expressing the electrostatic potential of an initial arrangement of electrons around a nucleus as a function of position of each of the electrons(within the shells and orbitals)
No see, electrons don't have a definite position. The Hamiltonian operator for the electrons, which defines the Schrödinger Equation (SE) for the electrons has a coordinate for each electron, but it is
not the location of the electron, rather it's a coordinate in the wavefunction's 'configuration space'. For instance, for a single particle wave function |\psi(x)|^2 is the probability that the particle is located at the coordinate x. For two particle wave function, |\psi(x_1,x_2)|^2 is the probability particle 1 is at location x
1 and that particle 2 is at location x
2. Note that for identical particles |\psi(x_1,x_2)|^2 = |\psi(x_2,x_1)|^2, which is a boundary condition your solution to the SE must statisfy. (and even more specifically, for electrons and other fermions, you must satisfy antisymmetry, which means \psi(x_1,x_2) = -\psi(x_2,x_1). This is a consequence of the spin-statistics theorem and ulitmately, relativistic theory, but at the level of non-relativistic QM you can just regard it as a postulate)
Another important thing is the variational theorem: Any normalized function, if you insert it into the SE for a system and calculate the energy, will result in an energy that is higher or equal to the ground-state energy. In other words, if you're approximating the solution to the S.E., the lower the energy the better the approximation. This theorem is a consequence of the solutions to the S.E. forming a complete set. (Descriptive proof: If the solutions form a complete set, any function can be expressed as a linear combination of the solutions, multiplied by some set of constants. Meaning the energy corresponding to that function, if inserted into the S.E., is the sum of the energies of the respective solutions, multiplied by the same constants squared. So the energy for the function cannot be lower than the ground-state, and is equal to the ground-state energy if and only if the function is identical to the ground-state solution)
Now, shells and orbitals; These are
derived results from quantum mechanics. They don't actually exist in themselves, they're an interpretation of a particular mathematical description. Typically you start with the solving the SE for the hydrogen atom (which has an analytical solution). You have a bunch of different energy states, corresponding to different linear and angular momenta (n and l eigenvalues). The different states for a single electron are dubbed 'orbitals' and we call the different states with the same n 'shells' and with different l values 'sub-shells'.
Now if electrons didn't interact, you could simply separate the SE into single-electron equations and write your total wavefunction as a product of these single-electron functions. (basic separation-of-variables approach to solving differential equations, which an engineer should know about). Actually you'd have to create an "anti-symmetrized" product, so that you satisfied the condition mentioned above. Such an anti-symmetrized product is called a Slater determinant (SD), and the single-electron functions are orbitals.
But for a many-electron system, the SE is inseparable and you
cannot divide it into independent single-electron states and have an accurate solution; since they interact they're not independent. This is what the earlier discussion was about, but I'll get back to that. In any case, let's just assume that this is fine and write your SD of N/2 functions (orbitals). The 1/2 comes in because of spin, which allows you to put two electrons in each orbital (for the sake of simplicity I'm leaving that bit out). If you stick this SD into the electronic SE, and do a lot of math (covered in most QC textbooks), you end up with the Hartree-Fock equations. In this approximation, the electrons aren't
totally independent; they just move in an averaged field of every other electron.
But you
still have a bunch simultaneous differential equations to solve! The way this is solved is by expressing each orbital as a linear combination of basis functions (again, these are abitrary), and solving it using the Self-Consistent-Field (SCF) approach. You can view it as starting from a guess (for which you usually use the totally non-interacting system, which can be solved directly), then minimizing the energy of an orbital without changing any other orbital, and then minimizing the next orbital and so on, and then starting over, and (with a little luck) this will converge to the correct solution.
The Hartree-Fock/SCF method is generally the simplest method of solving the S.E., and it gives qualitively correct results for a large amount of chemistry (including, say, the potassium ground-state configuration). It gets about 95% or so of the ground-state energy, and works as the starting point for most QC methods. Configuration Interaction, for instance, is essentially just an expanded HF method which has the important characteristic that it's
exact, in principle. (the drawback with full-CI is that the amount of calculating needed grows factorially with the number of electrons) With CI you use mutliple SDs (ground state and excited state SDs) to describe the system - the works because the SDs are solutions to the SE for 'non-interacting electrons', and thus form a complete set. While you get an accurate solution, it's no longer true that a single electron is fully described by a single orbital.
Finally, I should say that orbitals are not a necessary part of a quantum-mechanical description of an atom or molecule. It's a convenient way to do so because:
1) Given that HF gives you 95% or so accuracy, it's easier to start with HF and find corrections to it
2) Mathematically describing the kinetic energy is very difficult without assuming electrons move independently, at least as a starting approximation
3) It becomes difficult to satisfy the anti-symmetry condition above. If you ignore it, you end up with another error in your energy (dubbed "exchange energy").
That said, there
are methods of calculating the energy that do not use orbitals. The Thomas-Fermi model for instance, and other 'orbital-free' density-functional methods. (Which have problems with 2 and 3)
The first really accurate QM calculation of a many-electron system, Hylleraas calculation of helium (1929), did not use orbitals. By using a clever ansatz and a lot of algebra, he arrived at an equation that could be solved variationally, and got the ground-state energy with 98% accuracy with two parameters, and 99.9% accuracy with six. (IIRC)