My PhD thesis - Condensed Matter Theory - Imperial College London
My PhD thesis - Condensed Matter Theory - Imperial College London
My PhD thesis - Condensed Matter Theory - Imperial College London
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CHAPTER 3.<br />
QUANTUM MONTE CARLO METHODS<br />
as long as τ is large. Rearranging this formula gives<br />
This is the motivation for the growth estimator<br />
E 0 = E T (τ) − 1<br />
∆τ ln 〈<br />
M(τ + ∆τ)<br />
〉<br />
〈<br />
M(τ)<br />
〉 . (3.69)<br />
E growth (τ) = E T (τ) − 1<br />
∆τ<br />
M(τ + ∆τ)<br />
ln . (3.70)<br />
M(τ)<br />
More than one time step can be included in the growth estimator; however, E T<br />
is updated after every step, and this effect must then be unravelled.<br />
The same<br />
‘unravelling’ procedure can also be applied to the mixed estimator to account for<br />
changes in E T [79].<br />
When<br />
[Ĥ, Ô] ≠ 0, the mixed estimator is no longer equal to the ground-state<br />
expectation value O 0 . However, although now more difficult, it is still possible to<br />
construct an estimator for this quantity by combining the mixed estimate with the<br />
VMC result, O VMC . The extrapolated estimator is<br />
O ext = 2O mixed − O VMC . (3.71)<br />
To see why this estimator works, consider the integrals which the VMC and mixed<br />
estimators attempt to solve:<br />
O VMC →<br />
∫<br />
ΨT (R)ÔΨ T (R) dR<br />
∫<br />
Ψ<br />
2<br />
T<br />
(R) dR<br />
(3.72)<br />
O mixed →<br />
∫<br />
Φ0 (R)ÔΨ T (R) dR<br />
∫<br />
Φ0 (R)Ψ T (R) dR . (3.73)<br />
Suppose that the trial wave function differs from the true wave function only slightly,<br />
so that<br />
Ψ T = Φ 0 + ∆Φ. (3.74)<br />
Then substitution shows that the extrapolated estimator samples<br />
(∫<br />
Φ0<br />
2<br />
(R)ÔΨ ) ∫<br />
T (R) dR ΨT<br />
∫ −<br />
(R)ÔΨ ∫<br />
T (R) dR Φ0<br />
∫ =<br />
(R)ÔΦ 0(R) dR<br />
∫<br />
Φ0 (R)Ψ T (R) dR<br />
Ψ<br />
2<br />
T<br />
(R) dR<br />
Φ<br />
2<br />
0 (R) dR<br />
+ O [ (∆Φ) 2]<br />
(3.75)<br />
= O 0 + O [ (∆Φ) 2] ,<br />
so that the error in the extrapolated estimate is of order (∆Φ) 2 . However, in order<br />
for this method to be useful, the trial wave function must be of very high quality.<br />
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