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PhD thesis in English

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4. Mean-field description of an <strong>in</strong>teract<strong>in</strong>g BEC-0.015-0.02-0.025-0.03-0.035-0.04Numerical resultsFirst-order correction-0.04510 5 10 6 10 7Figure 4.9: A relative shift <strong>in</strong> the condensation temperature δT c as a function of thenumber of particles <strong>in</strong> the trap N for ω = 100 Hz.Nwe approach the BEC phase transition from the gas phase. We stress that the sameresult can be obta<strong>in</strong>ed by consider<strong>in</strong>g condensate phase <strong>in</strong> the vic<strong>in</strong>ity of the phasetransition with<strong>in</strong> the TFSC model. It is important to note that we only obta<strong>in</strong>the <strong>in</strong>teraction-<strong>in</strong>duced shift <strong>in</strong> the condensation temperature. F<strong>in</strong>ite-size effects[91, 92] are beyond our consideration, because we rely on the TF and semiclassicalapproximation. A comparison of the analytical expression (4.34), which gives a firstordercorrection to T c <strong>in</strong> the <strong>in</strong>teraction strength, and numerical results based onEqs. (4.26) and (4.27), is shown <strong>in</strong> Fig. 4.9. In this graph, δT c is given as a functionof the number of particles <strong>in</strong> the trap. We observe a reasonable agreement of theTFSC result (4.34) with the numerical data.4.3 Experimental assessment of different modelsDensity profile of a BEC cloud is experimentally measurable quantity, us<strong>in</strong>g eitherthe absorption TOF imag<strong>in</strong>g or <strong>in</strong>-situ techniques described <strong>in</strong> Chapter 1. Thevalues of other physical quantities are then extracted from the experimental data <strong>in</strong>a roundabout way.Early experimental efforts [93, 94] to measure the occupation of the ground stateas a function of the temperature have usually employed the absorption TOF imag<strong>in</strong>g.Thermometry was then performed by fitt<strong>in</strong>g the semiclassical result (1.17)100

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