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Monte Carlo Methods in Statistical Mechanics: Foundations and ...

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d = 2 Is<strong>in</strong>g Model<br />

L <strong>in</strong>tE<br />

64 1575 ( 10) 5.25 (0.30)<br />

128 5352 ( 53) 7.05 (0.67)<br />

256 17921 (109) 6.83 (0.40)<br />

512 59504 (632) 7.99 (0.81)<br />

Table 1: Susceptibility <strong>and</strong>autocorrelation time <strong>in</strong>tE (E =energy slowest mode) for<br />

two-dimensional Is<strong>in</strong>g model at criticality, us<strong>in</strong>gSwendsen-Wang algorithm. St<strong>and</strong>ard<br />

error is shown <strong>in</strong> parentheses.<br />

nonzero FKSW-measure is accessible from every other. So the SW algorithm is at<br />

least a correct algorithm for simulat<strong>in</strong>g the FKSWmodel. It is also an algorithm for<br />

simulat<strong>in</strong>gthe Potts <strong>and</strong> r<strong>and</strong>om-cluster models, s<strong>in</strong>ce expectations <strong>in</strong> these two models<br />

are equal to the correspond<strong>in</strong>g expectations <strong>in</strong> the FKSWmodel.<br />

Historical remark. The r<strong>and</strong>om-cluster model was <strong>in</strong>troduced <strong>in</strong> 1969 by Fortu<strong>in</strong><br />

<strong>and</strong> Kasteleyn [58] they derived the identity ZPotts = ZRC, alongwiththe correlationfunction<br />

identity (6.9) <strong>and</strong> some generalizations. These relations were rediscovered<br />

several times dur<strong>in</strong>g the subsequent two decades [59]. Surpris<strong>in</strong>gly, however, no one<br />

seems to have noticed the jo<strong>in</strong>t probability distribution FKSW that underlay all these<br />

identities this was discovered implicitly by Swendsen <strong>and</strong> Wang [27], <strong>and</strong> was made<br />

explicit by Edwards <strong>and</strong> Sokal [60].<br />

It is certa<strong>in</strong>ly plausible that the SW algorithm might have lesscritical slow<strong>in</strong>g-down<br />

than the conventional (s<strong>in</strong>gle-sp<strong>in</strong>-update) algorithms: the reasonisthat a local move<strong>in</strong><br />

one setofvariables can have highly nonlocal e ects <strong>in</strong>the other. For example, sett<strong>in</strong>g<br />

nb =0onas<strong>in</strong>gle bond may disconnect a cluster, caus<strong>in</strong>g abigsubset of the sp<strong>in</strong>s <strong>in</strong><br />

that cluster to be ipped simultaneously. In some sense,therefore, the SW algorithm<br />

is a collective-mode algorithm <strong>in</strong> which the collective modes are chosen by the system<br />

rather than imposed from the outside as<strong>in</strong>multi-grid. (The miracle is that thisisdone<br />

<strong>in</strong> a way that preserves the correct Gibbs measure.)<br />

How well does the SW algorithm perform? In at least some cases,the performance<br />

is noth<strong>in</strong>g short of extraord<strong>in</strong>ary. Table 1 shows some prelim<strong>in</strong>ary data [61]onatwodimensional<br />

Is<strong>in</strong>g model at the bulkcritical temperature. These data are consistent<br />

with the estimate SW L 0:35 [27]. 25 By contrast, the conventional s<strong>in</strong>gle-sp<strong>in</strong>- ip<br />

25 But precisely because rises so slowly with L, good estimates of the dynamic critical exponent<br />

will require the useofextremely large lattices. Even with lattices up to L =512,weareunable to<br />

dist<strong>in</strong>guish conv<strong>in</strong>c<strong>in</strong>gly between z 0:35 <strong>and</strong> z 0. Note Added 1996: For more recent <strong>and</strong><br />

49

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