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PhD thesis in English

PhD thesis in English

PhD thesis in English

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4. Mean-field description of an <strong>in</strong>teract<strong>in</strong>g BECthe vic<strong>in</strong>ity of the BEC phase transition. We focus on harmonically trapped bosonsfor two reasons: the trapp<strong>in</strong>g is always present <strong>in</strong> the experiments, and also thecalculation of the condensation temperature of the homogenous system turned out tobe a notorious problem, debated <strong>in</strong> many ways for several decades [79]. We scrut<strong>in</strong>yand compare several widely used implementations of the HF approximation with theemphasis on their advantages and drawbacks. The <strong>in</strong>terest <strong>in</strong> the topic <strong>in</strong>creases asnew experiments have reported the observation of beyond mean-field effects [80, 81],which should be <strong>in</strong>corporated <strong>in</strong>to the exist<strong>in</strong>g models.The partition function of the system <strong>in</strong> the grand canonical ensemble is given byZ(β) = Tr e −β(Ĥ−µ ˆN) , (4.2)and can be rewritten as a bosonic functional <strong>in</strong>tegral <strong>in</strong> the imag<strong>in</strong>ary time [32]:∮Z(β) =∮DΨDΨ ∗ e −A E[Ψ(⃗r,τ),Ψ ∗ (⃗r,τ)]/ , (4.3)where Ψ(⃗r, τ) and Ψ ∗ (⃗r, τ) are periodic functions, with the period β:Ψ(⃗r, τ) = Ψ(⃗r, τ + β) , Ψ ∗ (⃗r, τ) = Ψ ∗ (⃗r, τ + β) . (4.4)For the Hamiltonian (4.1) the Euclidean action A E is given byA E [Ψ(⃗r, τ), Ψ ∗ (⃗r, τ)] =∫ β0+ g 2∫dτ∫ β0(d⃗r Ψ ∗ (⃗r, τ) ∂)∂τ − 22M △ + V (⃗r) − µ Ψ(⃗r, τ)∫d⃗r Ψ ∗ (⃗r, τ)Ψ(⃗r, τ)Ψ ∗ (⃗r, τ)Ψ(⃗r, τ) . (4.5)dτA presence of the <strong>in</strong>teract<strong>in</strong>g Ψ 4 term <strong>in</strong> the action makes the calculation of the partitionfunction analytically <strong>in</strong>tractable, and to proceed further we apply the standardmean-field approach. In order to study Bose-E<strong>in</strong>ste<strong>in</strong> condensation, accord<strong>in</strong>g tothe Bogoliubov prescription (1.27), we first decompose the field Ψ <strong>in</strong>to the orderparameter ψ(⃗r, τ), which corresponds to the macroscopic condensate wave-function,and fluctuations δψ(⃗r, τ):Ψ(⃗r, τ) = ψ(⃗r, τ) + δψ(⃗r, τ) . (4.6)In the functional formalism this represents a change of variables, and the action now85

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