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PhD thesis in English

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5. BEC excitation by modulation of scatter<strong>in</strong>g lengthmodes obta<strong>in</strong>ed previously <strong>in</strong> the l<strong>in</strong>ear regime. As expla<strong>in</strong>ed <strong>in</strong> Chapter 4, thetime-dependent GP equation can be obta<strong>in</strong>ed by extremiz<strong>in</strong>g the functional (4.16)with respect to ψ(⃗r, t). In the core of the variational description is the idea to plug<strong>in</strong> an Ansatz for the condensate wave function <strong>in</strong>to Eq. (4.16) and to derive the correspond<strong>in</strong>gEuler-Lagrange equations of the system with respect to the parameterspresent <strong>in</strong> the Ansatz. In this way, <strong>in</strong>stead of the partial differential GP equation,we reduce the description of a system to ord<strong>in</strong>ary differential equations, which is farsimpler. Naturally, this presents an approximation, and careful exam<strong>in</strong>ation of itsvalidity and associated errors is necessary.To this end, we closely follow derivations presented orig<strong>in</strong>ally <strong>in</strong> Refs. [104, 105].We assume that the condensate wave function has the same Gaussian form <strong>in</strong> the<strong>in</strong>teract<strong>in</strong>g case as <strong>in</strong> the non<strong>in</strong>teract<strong>in</strong>g one, just with renormalized parameters.Thus, we use a time-dependent variational method based on a Gaussian Ansatz,which for the anisotropic harmonic trap (1.19) readsψ G (x, y, z, t) = N(t)∏σ=x,y,z[exp − 1 ](σ − σ 0 (t)) 2+ i σϕ2 u σ (t) 2 σ (t) + iσ 2 φ σ (t) , (5.1)where N(t) = π −3 4u x (t) −1 2u y (t) −1 2u z (t) −1 2 is a time-dependent normalization, whileu σ (t), φ σ (t), σ 0 and ϕ σ are variational parameters. For convenience, throughoutthis Chapter, we normalize the wave function to unity and for consistency we <strong>in</strong>cludethe total number of atoms <strong>in</strong>to the correspond<strong>in</strong>g <strong>in</strong>teraction strength. Thus,we modify the notation <strong>in</strong>troduced earlier by perform<strong>in</strong>g the follow<strong>in</strong>g transformation:ψ(⃗r, t) → ψ(⃗r, t)/ √ N, g → g × N. The <strong>in</strong>troduced variational parametershave straightforward <strong>in</strong>terpretation: u σ (t) parameters correspond to the condensatewidths <strong>in</strong> different directions and are roughly proportional to the root-mean-squarewidths of the exact condensate wave function ψ(x, y, z, t); φ σ (t) and ϕ σ (t) parametersrepresent the correspond<strong>in</strong>g phases of the wave function and are essential forthe proper description of dynamical features; a possible center-of-mass motion iscaptured by the parameters σ 0 .Follow<strong>in</strong>g Ref. [104], we <strong>in</strong>sert Ansatz (5.1) <strong>in</strong>to the Lagrangian (4.16) yield<strong>in</strong>gthe GP equation, and extremize it with respect to variational parameters. All thedetails of the derivation are given <strong>in</strong> Appendix B and here we give only a briefexplanation. By extremiz<strong>in</strong>g the functional, we first obta<strong>in</strong> a coupled system ofdifferential equations of the first order for all variational parameters. The equations108

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