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Polymers in Confined Geometry.pdf

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38 CHAPTER 4. SIMULATION METHODS<br />

polymer with N ≫ 1 monomers. S<strong>in</strong>ce <strong>in</strong> MD simulation the smallest time-scale<br />

of the model must be simulated, it cannot be effectively applied to our problem.<br />

We therefore concentrate on the Monte-Carlo simulation <strong>in</strong> the follow<strong>in</strong>g sections.<br />

For a very good <strong>in</strong>troduction also refer to [35].<br />

4.2 The Monte-Carlo method<br />

In statistical physics ensemble averages of fluctuat<strong>in</strong>g quantities are of special<br />

<strong>in</strong>terest. To obta<strong>in</strong> these averages, <strong>in</strong>tegrals of the follow<strong>in</strong>g form have to be<br />

evaluated (schematically for one dimension)<br />

〈A〉 p =<br />

+∞<br />

−∞<br />

dx A(x)p(x) . (4.1)<br />

<br />

φ(x)<br />

This example could be an average of an observable A(x) (“score function”)<br />

weighted by the probability distribution p(x), where the <strong>in</strong>tegral corresponds—<strong>in</strong><br />

the language of statistical mechanics—to a ‘sum’ over all states. But the method<br />

expla<strong>in</strong>ed <strong>in</strong> the follow<strong>in</strong>g is applicable to every <strong>in</strong>tegral presentable <strong>in</strong> this form.<br />

When eq. (4.1) is not analytically solvable then one has to resort to numerical<br />

methods. The direct way would be to divide the <strong>in</strong>tegration range—which can<br />

be of any dimension—<strong>in</strong>to n equidistant <strong>in</strong>tervals and evaluate the sum over<br />

{φ(xi)} on the discrete set of po<strong>in</strong>ts {xi} (Riemann <strong>in</strong>tegral). In this way the<br />

error of the approximative result <strong>in</strong> this determ<strong>in</strong>istic algorithm reduces with<br />

n −1/d depend<strong>in</strong>g on the dimensionality d. Therefore this method becomes very<br />

<strong>in</strong>effective for higher dimensions d. But <strong>in</strong> particular high-dimensional <strong>in</strong>tegrals<br />

is what we are calculat<strong>in</strong>g <strong>in</strong> statistical mechanical problems, therefore we need<br />

a smart way to <strong>in</strong>crease the efficiency of the numerical <strong>in</strong>tegration.<br />

The basic idea of Monte-Carlo 1 evaluation of an <strong>in</strong>tegral is to choose the n<br />

discretization po<strong>in</strong>ts/sample po<strong>in</strong>ts {xi} randomly out of the probability distribution<br />

p(x) such that the sum has to be performed only over the observable<br />

quantity at the so generated po<strong>in</strong>ts {A(xi)}. This algorithm has the advantage<br />

of a statistical error proportional to n −1/2 , <strong>in</strong>dependent of the dimension which<br />

outperforms the determ<strong>in</strong>istic calculation for n ≥ 3. But both algorithms have<br />

the problem, that they are very <strong>in</strong>efficient, when the problem under <strong>in</strong>vestigation<br />

has a large <strong>in</strong>herent variance, due to the fact that the computational time grows<br />

proportional to n and the variance is <strong>in</strong>versely proportional to √ n.<br />

This problem is seen <strong>in</strong> the follow<strong>in</strong>g way: If the probability distribution of<br />

the random numbers is such, that the important region of the observable is poorly<br />

sampled and therefore the variance is large, a huge number of samples may be<br />

needed to get a reliable result. It may happen, that the <strong>in</strong>terest<strong>in</strong>g region is<br />

1 The name ought to br<strong>in</strong>g the cas<strong>in</strong>os of Monte-Carlo to m<strong>in</strong>d.

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