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Statistical models of elasticity in main chain and smectic liquid ...

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4.4. COMPARISON WITH EXPERIMENT 1134.4.1 Experimentally measured elastic propertiesFirstly consider the Poisson ratios. When stretched <strong>in</strong> plane, the model consideredhere produces, for large b, Poisson ratios (0,1) which are observedexperimentally <strong>in</strong> [63]. When stretched parallel to the layer normal the observedPoisson ratios are (1/2,1/2). The model is consistent with this beforethe threshold occurs, <strong>and</strong> layer rotation beg<strong>in</strong>s. After threshold the modelpredicts Poisson ratios <strong>of</strong> (1,0) which are not the same as those observed experimentally.This is because the sample, which is cyl<strong>in</strong>drically symmetricabout the stretch axis, ma<strong>in</strong>ta<strong>in</strong>s its cyl<strong>in</strong>drical symmetry by form<strong>in</strong>g microstructureconsist<strong>in</strong>g <strong>of</strong> many small doma<strong>in</strong>s. This po<strong>in</strong>t is crucial <strong>in</strong> theanalysis <strong>of</strong> the x-ray data.In the experimental study <strong>of</strong> Nishikawa <strong>and</strong> F<strong>in</strong>kelmann [66] the elasticmoduli <strong>of</strong> a <strong>smectic</strong> elastomer were measured. Thesample used <strong>in</strong> their experimentswas found to have an anisotropy <strong>of</strong> r ≈ 1.6 from swell<strong>in</strong>g anisotropymeasurements. The threshold stra<strong>in</strong> was found to be ǫ c ≈ 3% with a correspond<strong>in</strong>gstress <strong>of</strong> σ N ≈ 1.12 × 10 5 Pa. The modulus before thresholdwas E before = 3.2 × 10 6 Pa, <strong>and</strong> the modulus after threshold was E after =1.1 × 10 5 Pa. Although they comment that after threshold the modulus issimilar to the <strong>in</strong>-plane modulus they do not give a value for the <strong>in</strong>-plane modulus.Accord<strong>in</strong>g to the theory outl<strong>in</strong>ed above from the reported moduli weexpect ǫ c ≈ E afterE before≈ 3.4% which is extremely close to their reported thresholdstra<strong>in</strong> given that the transition is not totally sharp when observed experimentally.From the values <strong>of</strong> r <strong>and</strong> E after we would expect an <strong>in</strong> plane modulus <strong>of</strong>4 E afterr≈ 2.75×10 5 Pa. Fig. 4.16 shows a fit <strong>of</strong> this theory to the elastic data<strong>of</strong> [66].The fit to the experimental data is good given the small number <strong>of</strong> parameters<strong>in</strong> the model for such a complicated material.4.4.2 X-ray scatter<strong>in</strong>gReference [66] also conta<strong>in</strong>s x-ray data for a <strong>smectic</strong> elastomer as it is be<strong>in</strong>gstretched along the layer normal. It is observed that the x-ray peaks correspond<strong>in</strong>gto the layers rotate as the sample is stretched. There is also a sharpdrop <strong>in</strong> the <strong>in</strong>tensity <strong>of</strong> these peaks which was attributed to melt<strong>in</strong>g <strong>of</strong> the<strong>smectic</strong> phaseto thenematic or isotropic phasebyNishikawa <strong>and</strong>F<strong>in</strong>kelmann.Fig. 4.17 below compares the calculated orientation <strong>of</strong> the director withthe experiment <strong>of</strong> [66]. As is clear from the figure the rotation <strong>of</strong> the <strong>smectic</strong>layers is <strong>in</strong> good agreement with the model discussed here.Theabove theory does not predictthat the <strong>smectic</strong> phasemelts on stretch<strong>in</strong>g.The energy cost to perform this melt<strong>in</strong>g can be calculated as follows: theentropy change found <strong>in</strong> [66] for the <strong>smectic</strong>-isotropic phase transition was∆S = 2.4 × 10 −2 JK −1 g −1 . Thus the cost for melt<strong>in</strong>g at 300K for a samplewith density ρ ∼ 1g cm −3 is T∆Sρ ∼ 7.2 × 10 6 J m −3 . To pay the cost <strong>of</strong>

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