Classical Field Theory Φ

Classical Field Theory Φ

Classical Field Theory φ x ● Consider waves on a string, mass per unit length ρ, tension T , displacement φ(x, t). ∂φ 2 K.E. T = 1 ρ dx 2 ∂t ! " # ∂φ 2 ∂φ 2 P.E. V = 1 T dx = 1 ρc2 dx 2 ∂x 2 ∂x ! " # ! " # where wave velocity c = T/ρ. $ 1 ● Lagrangian L = T V = dx with Lagrangian density − L % ∂φ 2 ∂φ 2 = 1 ρ c2 L 2 ∂t − ∂x &" # " # ' For brevity, write ∂φ ∂φ = φ˙ , = φ! ∂t ∂x 1 2 2 2 = ρ φ˙ c φ! ⇒ L 2 − ( ) ● Equations of motion given by least action δS = 0 where S = L dt. Now ∂ ∂ ∂ % δS = Lδφ + L δφ! + Lδφ˙ dx dt ∂φ ∂φ! ∂φ˙ ! " # But + ∂ ∂ ∂ ∂ ∞ ∂ ∂ L δφ! dx = L δφ dx = L δφ L δφ dx ∂φ! ∂φ! ∂x ∂φ! − ∂x ∂φ! ! ! * +−∞ ! " # 2 We can assume the boundary terms vanish. Similarly ∂ ∂ ∂ Lδφ˙ dt = L δφ dt ∂φ˙ − ∂t ∂φ˙ ! ! " # and so ∂ ∂ ∂ ∂ ∂ δS = L L L δφ dx dt ∂φ − ∂x ∂φ! − ∂t ∂φ˙ ! * " # " #+ ● This has to vanish for any δφ(x, t), so we obtain the Euler-Lagrange equation of motion for the field φ(x, t): ∂ ∂ ∂ ∂ ∂ L L L = 0 ∂φ − ∂x ∂φ − ∂t ˙ " ! # " ∂φ # 1 2 2 2 ● For the string, = ρ φ˙ c φ! . Hence L 2 − ( ) ∂φ ∂φ˙ ρc2 ! ρ = 0 ∂x − ∂t 3 which gives the wave equation ∂2φ ∂2φ c2 = 0 ∂x2 − ∂t2 ● We shall also need the Hamiltonian H = dx H ! Recall that for a single coordinate q we have L = L(q˙, q) and H = pq˙ L − where p is the generalized momentum ∂L p = ∂q˙ ● Similarly, for a field φ(x, t, ) we define momentum density ∂ π(x, t) = L ∂φ˙ 4 Then (π, φ) = πφ˙ H − L ● For the string π = ρφ˙ (as expected) and 2 π 1 π 1 2 2 = π ρ + ρc φ! H ρ − 2 ρ 2 " # " # 1 ∂φ 2 = π2 + 1 ρc2 2ρ 2 ∂x " # 5 Klein-Gordon Field ● We choose the Lagrangian density (! = c = 1) ∂φ 2 ∂φ 2 = 1 1 1 m2φ2 L 2 ∂t − 2 ∂x − 2 " # " # to obtain the Klein-Gordon equation of motion: ∂ ∂ ∂ ∂ ∂ L L L = 0 ∂φ − ∂x ∂φ − ∂t ˙ " ! # " ∂φ # ∂2φ ∂2φ m2φ + = 0 ⇒ − ∂x2 − ∂t2 ● The momentum density is ∂ ∂φ π = L = ∂φ˙ ∂t and so the Klein-Gordon Hamiltonian density is ∂φ 2 = 1 π2 + 1 + 1 m2φ2 H 2 2 ∂x 2 " # 6 ● In 3 spatial dimensions ∂φ/∂x φ, → ∇ ∂ ∂ ∂ ∂ ∂ ∂ ∂ ∂ ∂ L L L L L = 0 ∂φ − ∂x ∂(∂φ/∂x) − ∂y ∂(∂φ/∂y) − ∂z ∂(∂φ/∂z) − ∂t ˙ " # " # " # " ∂φ # ∂2φ m2φ + 2φ = 0 ⇒ − ∇ − ∂t2 ● Covariant notation: = 1 g (∂µφ) (∂ν φ) 1 m2φ2 L 2 µν − 2 Euler-Lagrange equation: ∂ ∂ L ∂µ L = m2φ ∂µ (g ∂ν φ) = 0 ∂φ − ∂(∂µφ) − − µν " # i.e. µ 2 ∂ ∂µφ + m φ = 0 7 ● Note that the Lagrangian density and the action S = d3r dt = d4x L L L are scalars (invariant functions), like φ. % % ● On the other hand the momentum density π = ∂φ/∂t and the Hamiltonian density = 1 π2 + 1 ( φ)2 + 1 m2φ2 H 2 2 ∇ 2 are not: time development frame dependence. ⇒ 8 Fourier Analysis ● We can express any real field φ(x, t) as a Fourier integral: ikx iωt ikx+iωt φ(x, t) = dk N(k) a(k)e − + a∗(k)e− ! , - where N(k) is a convenient normalizing factor for the Fourier transform a(k). The frequency ω(k) is obtained by solving the equation of motion: KG equation ω = +√k2 + m2. ⇒ ● The Hamiltonian 1 2 1 2 1 2 2 H = 2 π + 2 φ! + 2 m φ dx ! takes a simpler form in terms o.f the Fourier amplitud/es a(k). We can write e.g. 2 φ = dk N(k) [. .] dk! N(k!) [. .] ! ! and use i(k k!)x dx e ± = 2π δ(k k!) ± ! 9 to show that 2 i(ω+ω!)t φ dx = 2π dk dk! N(k) N(k!) a(k)a(k!)δ(k + k!)e− ! ! i(ω,+ω!)t i(ω ω!)t + a∗(k)a∗(k!)δ(k + k!)e + a(k)a∗(k!)δ(k k!)e− − − i(ω ω!)t + a∗(k)a(k!)δ(k k!)e − − ● Noting that ω( k) = ω(k) and choosing N(k-) such that N( k) = N(k), this − − gives 2 2 2iωt φ dx = 2π dk [N(k)] a(k)a( k)e− − ! ! 2iωt + a∗(k)a∗( k)e , + a(k)a∗(k) + a∗(k)a(k) − ● Similarly - 2 2 2iωt φ! dx = 2π dk [kN(k)] a(k)a( k)e− − ! ! 2iωt + a∗(k)a∗( k)e ,+ a(k)a∗(k) + a∗(k)a(k) − - 10 while 2 2 2iωt φ˙ dx = 2π dk [ω(k)N(k)] a(k)a( k)e− − − ! ! +2iωt a∗(k)a∗( k)e ,+ a(k)a∗(k) + a∗(k)a(k) − − and hence, using k2 = ω2 m2, - − 2 H = 2π dk [N(k)ω(k)] [a(k)a∗(k) + a∗(k)a(k)] ! or, choosing 1 N(k) = 2π 2ω(k) · 1 H = dk N(k) 2 ω(k) [a(k)a∗(k) + a∗(k)a(k)] ! i.e. the integrated density of modes N(k) times the energy per mode ω(k) a(k) 2. | | Each normal mode of the system behaves like an independent harmonic ⇒ oscillator with amplitude a(k). 11 ● In 3 spatial dimensions we write 3 ik r iωt ik r+iωt φ(r, t) = d k N(k) a(k)e · − + a∗(k)e− · ! , - and use 3 i(k k!) r 3 3 d r e ± · = (2π) δ (k k!) ± ! Therefore we should choose 1 N(k) = (2π)3 2ω(k) to obtain an integral with the usual relativistic phase space (density of states) factor: d3k H = ω(k) a(k) 2 (2π)3 2ω(k) | | ! 12 Second Quantization ● First quantization was the procedure of replacing classical dynamical variables q and p by quantum operators qˆ and pˆ such that [qˆ, pˆ] = i (! = 1) ● Second quantization is replacing the field variable φ(x, t) and its conjugate momentum density π(x, t) by operators such that [φˆ(x, t), πˆ(x!, t)] = i δ(x x!) − N.B. x and x! are not dynamical variables but labels for the field values at different points. Compare (and contrast) [qˆj, pˆk] = i δjk (j, k = x, y, z) ● The wave function φ satisfying the Klein-Gordon equation is replaced by the field operator φˆ, satisfying the same equation. 13 ● The Fourier representation becomes ikx iωt ikx+iωt φˆ(x, t) = dk N(k) aˆ(k)e − + aˆ†(k)e− ! , - i.e. φˆ is hermitian but the Fourier conjugate operator aˆ is not. ● Keeping track of the order of operators, the Hamiltonian operator is ˆ 1 H = dk N(k) 2 ω(k) [aˆ(k)aˆ†(k) + aˆ†(k)aˆ(k)] ! ● Comparing this with the simple harmonic oscillator, ˆ 1 HSHO = 2 ω (aˆaˆ† + aˆ†aˆ) we see that aˆ†(k) and aˆ(k) must be the ladder operators for the mode of wave number k. They add/remove one quantum of excitation of the mode. These quanta are the particles corresponding to that field: aˆ†(k) = creation operator , aˆ(k) = annihilation operator ⇒ for Klein-Gordon particles. 14 ● Ladder operators of simple harmonic oscillator satisfy [aˆ, aˆ†] = 1 The analogous commutation relation for the creation and annihilation operators is N(k) [aˆ(k), aˆ†(k!)] = δ(k k!) − [aˆ(k), aˆ†(k!)] = 2π 2ω(k) δ(k k!) ⇒ · − or in 3 spatial dimensions 3 3 [aˆ(k), aˆ†(k!)] = (2π) 2ω(k) δ (k k!) · − On the other hand [aˆ(k), aˆ(k!)] = [aˆ†(k), aˆ†(k!)] = 0 15 ● The commutators of the creation and annihilation operators correspond to the field commutation relation 3 3 [φˆ(r, t), πˆ(r!, t)] = d k d k! N(k) N(k!)[ iω(k!)] − × ! ik x ik x ik! x! ik! x! aˆ(k)e− · + aˆ†(k)e · , aˆ(k!)e− · aˆ†(k!)e · − 0 1 3 ik (x x!) ik (x x!) = i d k N(k)ω(k) e− · − + e · − ! 0 1 µ µ where x = (t, r) and x! = (t, r!). Hence 3 [φˆ(r, t), πˆ(r!, t)] = i δ (r r!) − as expected. On the other hand [φˆ(r, t), φˆ(r!, t)] = [πˆ(r, t), πˆ(r!, t)] = 0 16 ● The fact that the field operator has positive- and negative-frequency parts now appears quite natural: ik r iωt ❖ positive frequency part aˆ(k)e · − annihilates particles ik r+iωt ❖ negative frequency part aˆ†(k)e− · creates particles ● !ω is the energy released/absorbed in the annihilation/creation process. ± N.B. The hermitian field describes particles that are identical to their antiparticles, e.g. π0 mesons. ● More generally (as we shall see shortly) the negative-frequency part of φˆ creates antiparticles. 17 Single Particle States ● If 0 represents the state with no particles present (the vacuum), then | ' aˆ†(k) 0 is a state containing a particle with wave vector k, i.e. momentum !k. | ' More generally, to make a state with wave function φ(r, t) where 3 ik r iωt φ(r, t) = d k φ˜(k)e · − ! we should operate on the vacuum with the operator 3 d k φ˜(k)aˆ†(k) ! 3 ● Writing this state as φ = d k φ˜(k)aˆ†(k) 0 we can find the wave function | ' | ' using the relation % 0 φˆ(r, t) φ = φ(r, t) ( | | ' ● Thus the field operator is an operator for “finding out the wave function” (for single-particle states). 18 Two Particle States ● Similarly, we can make a state φ of two particles: | 12' 3 3 φ = d k d k φ˜(k , k )aˆ†(k )aˆ†(k ) 0 | 12' 1 2 1 2 1 2 | ' ! Since the two particles are identical bosons, this state is symmetric in the labels 1 and 2 even if φ˜ isn’t, because aˆ†(k1) and aˆ†(k2) commute: 3 3 φ = d k d k φ˜(k , k )aˆ†(k )aˆ†(k ) 0 | 12' 1 2 1 2 1 2 | ' ! 3 3 = d k d k φ˜(k , k )aˆ†(k )aˆ†(k ) 0 1 2 2 1 2 1 | ' ! = φ | 21' ● The 2-particle wave function is φ(r , r , t) = 0 φˆ(r , t)φˆ(r , t) φ 1 2 ( | 1 2 | 12' = φ(r2, r1, t) Thus quantum field theory is also a good way of dealing with systems of many identical particles.

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