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Because the particle density is uniform in the fluid phase, this joint probability density is also proportional to the conditional probability density that, given a particle at x0 right before the cross-linking, it is found at { x1,..., xn }, respectively, in n independent measurements after cross-linking.
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Because the particle density is uniform in the fluid phase, this joint probability density is also proportional to the conditional probability density that, given a particle at x0 right before the cross-linking, it is found at { x1,..., xn }, respectively, in n independent measurements after cross-linking.
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We note that, in the isotropic limit, this deformed saddle-point solution differs slightly from the type of Goldstone fluctuations studied in Ref., partly due to different parametrizations. A detailed discussion of the similarities and distinctions between these two analyses will be presented elsewhere.
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We note that, in the isotropic limit, this deformed saddle-point solution differs slightly from the type of Goldstone fluctuations studied in Ref., partly due to different parametrizations. A detailed discussion of the similarities and distinctions between these two analyses will be presented elsewhere.
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A similar result was found for isotropic vulcanized systems; see Ref..
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A similar result was found for isotropic vulcanized systems; see Ref..
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