Non-Linear Σ Model

Non-Linear Σ Model

Contents Non-linear σ model 1 Introduction1 Renormalisation Group Flow 2 NLσM (Non-Linear Sigma Model)3 Lukas Barth 3 β-function8 4 Calculation of β-function of NLσM 10 Summer 2016 5 Heisenberg Spins on an elastic Torus 13 References 15 1 Introduction 1.1 Motivation The Non-linear Sigma Model originated in a quantum field theoretic context as a generalisation of the linear Sigma Model. It includes non-linear couplings of scalar fields while maintaining the masslessness of the excitations. It therefore became especially important in String Theory where the massless excitations already give rise to the full theory as the interactions only depend on the global properties of the interacting strings. As a result, the NLσM is the most general model that one could employ in a bosonic String Theory. Even more importantly, the quantum field theoretical beta functions arising in a renormalisation group flow treatment of the NLσM will give rise to the Einstein field equations demonstrating how these could emerge in the limit of a String theoretic context (this will be shown in the following). Simultaneously, the Sigma Model and its renormalisation group flow can also be studied as an abstract mathematical model with fields mapping from a curved surface into a curved target space. It can then be brought into different contexts, also outside quantum field theory, yielding new appli- cations like the Heisenberg Spin Torus which we will elaborate upon in the last section. 1.2 Structure of treatise As the relationships of the topics we are going to investigate are quite intertwined, I decided to give a short overview in advance. Basically, the combination of the four topics \NLσM", \Riemann normal coordinates", \Path integral quantisation" and \Beta functions" leads us to our end result. These are all themes existing in their own right independent of each other. However, we will 1. expand the NLσM in normal coordinates and combine that expansion with the background field method of path integral quantisation. 2. Simultaneously, we will introduce the beta function (corresponding to the response of the cou- plings to a variation in the energy scale) and its interpretation in order to point out its relation- ship with the energy momentum tensor. 1 3. The energy momentum tensor has also a relationship to the full quantum effective action which therefore leads to a relationship between the full quantum effective action and the beta functions. 4. Combining this relationship with the SO(1,D-1) formulation of our expanded effective action (named in 1.), we can compute the beta functions. 5. Finally the interpretation of the result will lead us to the Einstein field equations and further applications like \Spins on an elastic torus section". The structure of this write up is depicted in diagrammatic form below for clarity. Normal coordinate Other applications NLSMNLSM Construction Construction Field equations expansion of NLSM E.g. Spin Torus Normal coord. expansion of Full Quantum Effective action of NLSM Calculation of Riemann Normal Coordinates beta function SO(1,D-1) reformulation Path integral Background Relation of energy momentum Relation of beta function quantisation Field Method to full quantum effective action to full quantum effective action Relation of beta function Beta function Interpretation to energy momentum tensor 2 2 NLσM (Non-Linear Sigma Model) 2.1 Construction We want the most general action in a bosonic setting. For that, one can use the correspondence between vertex operators and variations of background fields given in [1]. 2 Assuming a string state of squared mass M = −2 + 2p, and defining the fields Eµ1···µ2p (X) associated with these states, the employed correspondence gives the contribution to the action as Z 2 p µ1···µ2p 2 SE[x; g] = d σ g Eµ1···µ2p (X)P (@; @ x; ··· ); (1) Σ where P µ1···µ2p denotes a Polynomial in the derivatives of x. For p = 1, one obtains a familiar massless string action. For p > 1, it turns out that the resulting contributions are non-renormalizable on WS (so called world sheet Σ). Therefore these are considered irrelevant in a consistent theory and the most general bosonic action for a String Theory is thus made up by massless fields. The result of putting these together (except for the tachyon which would produce negative states) is the non-linear sigma-model. The NLσM is a bosonic theory with the following symmetries: (a) Diff(Σ) (Diffeomorphism (Reparameterisation) invariance on the world sheet) (b) Diff(M) (Diffeomorphism invariance on the target space) (1) (c) U(1)B gauge invariance, B ! B + dγ, γ 2 Ω (M) The most general such action that can be constructed out of massless fields is then given by 1 Z p n o ) S = d2σ g (gabG (X) + abB (X))@ Xµ@ Xν + l R(2)Φ(X) (2) σ 8πl2 µν µν a b with the metric Gµν (a symmetric 2-tensor), Bµν = −Bνµ, the so-called Kalb-Ramond gauge field, and Φ, the dilaton (which in String theory gives rise to a dynamical coupling of the String: g = eΦ(X)). p ps gmn and mn are the symmetric and antisymmetric metrics on Σ respectively and g = det gmn. R(2) is the Riemann tensor on Σ. (l, the coupling constant, is sometimes enframed in blue for clarity.) Some more information (a) The name σ-model has its roots in the history of pions. (b) The model is a generalisation of the Polyakov action to a model that includes a general metric and all possible fields of a bosonic theory. (c) One could also apply the model to the study of field theoretic effects where the X- fields not necessarily embody space time coordinates any more. In the last section we will see the example, where the \world sheet" is a magnetized torus and the fields are associated to magnetic fields having another dynamical topological shape. 3 2.2 Quantum Dynamics −2 To obtain the quantum dynamics of the system, one can use the path integral and introduce l , the −1 \String length" perturbation parameter instead of ~ . The full effective action Γ is defined as usual. Z −2 δΓ eW [J] := DX e−l Sσ[X]+X·J ; Γ[hXi] := J · hXi − W [J];J = (3) δhXi R 2 p µ ν with the short hand notation X · J := d σ g Gµν(X) X J . This is not exactly solvable. One thus needs perturbation theory. The metric is non-flat ) One would like to retain the covariant formulation while renormalising. For that we will introduce the Background Field Quantization Method. 2.3 Background Field Quantization Method As a first step, we will only rewrite the full quantum effective action in such a way that we obtain a perturbation series relating Γ and S. This can be done likewise in any QFT. We shift the integration variable (X ! X + hXi) while D(X + hXi) = DX is invariant. Z δΓ[hXi] ) e−Γ[hXi] = DX exp −l−2 S [X + hXi] + X · σ δhXi (4) (X ! l X) Z δΓ[hXi] = D(lX) exp −l−2 S [lX + hXi] + lX · σ δhXi The last transformation (X ! lX) allows us to expand in a Laurent series: 1 1 1 δS(hXi) S[hXi + lX] = S[hXi] + X · + S~[hXi; X](l); l2 l2 l δhXi (5) 1 δΓ[hXi] 1 δS[hXi] δΓ[~ hXi](l) Γ(hXi) = S[hXi] + Γ[~ hXi](l) ) lX · = X · + lX · l2 δhXi l δhXi δhXi S~ and Γ~ denominate Taylor series expansions in l. We thus obtain a recursive relation between S~(l) and Γ(~ l) in path integral form: ! ~ Z δΓ[~ hXi](l) e−Γ[hXi](l) = D(lX) exp −S~ [hXi; X](l) + l X · : (6) σ δhXi To proceed, we need to expand our action and thus its fields. However, to do this properly, our non-flat background will require us to introduce normal coordinates. 2.4 Riemann normal coordinates The next step is to expand the metric around a background: Gµν(X) = Gµν(X0) + ···. µ µ µ l2 µ 2 This is possible by expanding the fields X ! X0 + lξ (X0) + 2 (ξ ) (X0) + ··· on which the metric depends. But addition of coordinates is not covariant under Diff(M), so one needs to do it with care. 4 Illustration taken from [1]. µ µ Suppose X0 and X are sufficiently close to each other such that there is a unique geodesic curve C µ parameterised by Xτ on the manifold interpolating between them. µ µ µ µ We set Xτ=0 = X0 and Xτ=l = X and require D X_ µ = X¨ µ + Γµ (X )X_ νX_ ρ = 0: (7) Dτ τ τ νρ τ τ τ ∗ Now let ξ(X) be a section on the pullback tangent bundle ξ(X) 2 Γ(X TM). We want to choose Xτ such that we can extend ξ(X) to ξ(X; t) by requiring @ ξ(X; τ) = X∗ ; r ξ(X; τ) = 0 =: r ξ (8) @τ τ ξ In the last step, we made a slight abuse of notation, because ξ is actually not a vector on M but on the WS, but this will be corrected when we pull back to Σ. [3] Comparing to the above equation, one sees that this is fulfilled for ξ(X; t) = X_ τ , that is we parallel µ _ µ transport ξ(X; 0) along Xτ . The tangent vector at τ = 0 is ξ := X0 ∗ @ Now imagine we have an arbitrary vector v = X @µ on the pullback tangent bundle, then [@t;@µ] = 0 (we use a torsion free connection here for demonstration) and we get by the same abusive notation 2 rξv = rvξ ) rξv = rξrvξ = R(ξ; v)ξ (9) where the last term is the equation of geodesic deviation.

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