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My PhD thesis - Condensed Matter Theory - Imperial College London

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Chapter 7<br />

The electronic ground-state wave<br />

function from classical plasmon<br />

normal modes<br />

A prerequisite for a successful quantum Monte Carlo simulation is a trial wave<br />

function of good quality. Conventionally, the many-electron trial wave function<br />

takes the form<br />

Ψ T (X) = e J(X) D ↑ (R ↑ )D ↓ (R ↓ ) (7.1)<br />

where D ↑ and D ↓ are up- and down-spin determinants made up of density-functional<br />

or Hartree-Fock single-electron orbitals. The quality of these orbitals sets a hard<br />

limit on the accuracy of the QMC simulation in variational or fixed-node diffusion<br />

Monte Carlo. The Jastrow factor, J, cannot alter the position of the nodes, and<br />

therefore cannot improve the fixed-node DMC energy; however, a good Jastrow factor<br />

significantly improves both the ground-state energy in VMC and the efficiency<br />

of fixed-node DMC simulations. In certain circumstances, a poor-quality Jastrow<br />

factor can make DMC simulations impossible, because the consequent population<br />

fluctuations become unmanageable. This is the case for the jellium slab system,<br />

which also suffers from the problem that optimising the Jastrow factor is very difficult;<br />

in systems such as this, it is very important to obtain as much information as<br />

106

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