Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 1
Collective Effects
in
Equilibrium and Nonequilibrium Physics
Website: http://cncs.bnu.edu.cn/mccross/Course/ Caltech Mirror: http://haides.caltech.edu/BNU/
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 2
Today’s Lecture
Superfluids and superconductors
• What are superfluidity and superconductivity? • Review of phase dynamics • Description in terms of a macroscopic phase • Supercurrents that flow for ever • Josephson effect • Four sounds
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 3
The Amazing World of Superfluidity and Superconductivity
• Electric currents in loops that flow for ever (measured for ∼ decade) • Beakers of fluid that empty them- selves • Fluids that flow without resistance through tiny holes • Flow in surface films less than an atomic layer thick • Flow driven by temperature differ- ences (fountain effect)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 4
History of Superfluidity and Superconductivity 1908 Liquefaction of 4He by Kamerlingh Onnes
1911 Discovery of superconductivity by Onnes (resistance drops to zero)
1933 Meissner effect: superconductors expel magnetic field
1937 Discovery of superfluidity in 4He by Allen and Misener
1938 Connection of superfluidity with Bose-Einstein condensation by London
1955 Feynman’s theory of quantized vortices
1956 Onsager and Penrose identify the broken symmetry in superfluidity ODLRO
1957 BCS theory of superconductivity
1962 Josephson effect
1973 Discovery of superfluidity in 3He at 2mK by Osheroff, Lee, and Richardson
1986 Discovery of high-Tc superconductors by Bednorz and Müller 1995- Study of superfluidity in ultracold trapped dilute gases
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 5
Review of Phase Dynamics with a Conserved Quantity
Rotational symmetry in the XY plane (angle 2)
Sz The XY and Z components of the spin have different prop- erties: S⊥ P −1 Θ Sz = hsizi is a conserved quantity i inP −1 S⊥ = hsi⊥i is the XY order parameter i in
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 5
Review of Phase Dynamics with a Conserved Quantity
Rotational symmetry in the XY plane (angle 2)
Sz The XY and Z components of the spin have different prop- erties: S⊥ P −1 Θ Sz = hsizi is a conserved quantity i inP −1 S⊥ = hsi⊥i is the XY order parameter i in
Sz and 2 are canonically conjugate variables, so that with the free energy Z " # 1 S2 F = dd x K (∇2)2 + z − S b 2 2χ z z
we get δF S˙ =− giving S˙ =−∇·j with j =−K ∇2 z δ2 z Sz Sz δ ˙ F ˙ −1 2 = giving 2 = χ (Sz − χbz) δSz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 6
Spin Current ˙ =−∇· Sz jSz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 6
Spin Current ˙ =−∇· Sz jSz
This is a conservation law with a current jSz of the conserved quantity Sz given by a phase gradient =− ∇2 jSz K
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 6
Spin Current ˙ =−∇· Sz jSz
This is a conservation law with a current jSz of the conserved quantity Sz given by a phase gradient =− ∇2 jSz K
For example
Θ(r)
L
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
• No dynamics in full thermodynamic equilibrium: Sz = χb0z
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
• No dynamics in full thermodynamic equilibrium: Sz = χb0z
• Add an additional external field b1z = γ B1z ˙ 2 =−b1z =−γ B1z
the usual precession of a magnetic moment in an applied field (Larmor precession).
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
• No dynamics in full thermodynamic equilibrium: Sz = χb0z
• Add an additional external field b1z = γ B1z ˙ 2 =−b1z =−γ B1z
the usual precession of a magnetic moment in an applied field (Larmor precession).
• Note that this is an equilibrium state: Sz 6= χ(b0z + b1z) but is a conserved quantity
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
• No dynamics in full thermodynamic equilibrium: Sz = χb0z
• Add an additional external field b1z = γ B1z ˙ 2 =−b1z =−γ B1z
the usual precession of a magnetic moment in an applied field (Larmor precession).
• Note that this is an equilibrium state: Sz 6= χ(b0z + b1z) but is a conserved quantity— no approximations
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 7
Phase Dynamics
˙ −1 2 = χ (Sz − χbz)
• No dynamics in full thermodynamic equilibrium: Sz = χb0z
• Add an additional external field b1z = γ B1z ˙ 2 =−b1z =−γ B1z
the usual precession of a magnetic moment in an applied field (Larmor precession).
• Note that this is an equilibrium state: Sz 6= χ(b0z + b1z) but is a conserved quantity— no approximations • For formal proof see Halperin and Saslow, Phys. Rev. B 16, 2154 (1977), Appendix: “the Larmor precession theorem”
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 8
Hydrodynamic Approach Hydrodynamics: a formal derivation of long wavelength dynamics of conserved quantities and broken symmetry variables in a thermodynamic approach
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 8
Hydrodynamic Approach Hydrodynamics: a formal derivation of long wavelength dynamics of conserved quantities and broken symmetry variables in a thermodynamic approach Starting points
• generalized rigidity: extra contribution to the energy density from gradients of the broken symmetry variable 1 ε = K (∇2)2 2 • thermodynamic identity
dε = Tds+ µzdsz + 8 · d(∇2) with 8 = K ∇2
• equilibrium phase dynamics (Larmor precession theorem) ˙ 2 = µz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 8
Hydrodynamic Approach Hydrodynamics: a formal derivation of long wavelength dynamics of conserved quantities and broken symmetry variables in a thermodynamic approach Starting points
• generalized rigidity: extra contribution to the energy density from gradients of the broken symmetry variable 1 ε = K (∇2)2 2 • thermodynamic identity
dε = Tds+ µzdsz + 8 · d(∇2) with 8 = K ∇2
• equilibrium phase dynamics (Larmor precession theorem) ˙ 2 = µz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 8
Hydrodynamic Approach Hydrodynamics: a formal derivation of long wavelength dynamics of conserved quantities and broken symmetry variables in a thermodynamic approach Starting points
• generalized rigidity: extra contribution to the energy density from gradients of the broken symmetry variable 1 ε = K (∇2)2 2 • thermodynamic identity
dε = Tds+ µzdsz + 8 · d(∇2) with 8 = K ∇2
• equilibrium phase dynamics (Larmor precession theorem) ˙ 2 = µz
Derive • dynamical equations for conserved quantities and broken symmetry variables for slowly varying disturbances
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 9
Rigidity and the Thermodynamic Identity In terms of the energy density
dε = Tds + µzdsz + 8 · d(∇2)
• conjugate fields are ∂ε ∂ε µ = and 8 = z ∂s ∂∇2 z s,∇2 s,sz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 9
Rigidity and the Thermodynamic Identity In terms of the energy density
dε = Tds + µzdsz + 8 · d(∇2)
• conjugate fields are ∂ε ∂ε µ = and 8 = z ∂s ∂∇2 z s,∇2 s,sz
Or with the free energy density f = ε − Ts
df =−sdT + µzdsz + 8 · d(∇2)
• conjugate fields are ∂ f ∂ f µ = and 8 = z ∂s ∂∇2 z T,∇2 T,sz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 9
Rigidity and the Thermodynamic Identity In terms of the energy density
dε = Tds + µzdsz + 8 · d(∇2)
• conjugate fields are ∂ε ∂ε µ = and 8 = z ∂s ∂∇2 z s,∇2 s,sz
Or with the free energy density f = ε − Ts
df =−sdT + µzdsz + 8 · d(∇2)
• conjugate fields are ∂ f ∂ f µ = and 8 = z ∂s ∂∇2 z T,∇2 T,sz
These give −1 µz = χ (Sz − χbz) and 8 = K ∇2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 10
Entropy Production
Tds = dε − µzdsz − 8 · d(∇2)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 10
Entropy Production
Tds = dε − µzdsz − 8 · d(∇2)
• Form time derivative of entropy density ε µ 8 (∇2) ds = 1 d − z dsz − · d dt T dt T dt T dt
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 10
Entropy Production
Tds = dε − µzdsz − 8 · d(∇2)
• Form time derivative of entropy density ε µ 8 (∇2) ds = 1 d − z dsz − · d dt T dt T dt T dt ε • Conservation laws and dynamics of broken symmetry variable (j , jsz unknown)
ds 1 ε µ 8 =− ∇·j + z ∇·jsz − ·∇µ dt T T T z
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 10
Entropy Production
Tds = dε − µzdsz − 8 · d(∇2)
• Form time derivative of entropy density ε µ 8 (∇2) ds = 1 d − z dsz − · d dt T dt T dt T dt ε • Conservation laws and dynamics of broken symmetry variable (j , jsz unknown)
ds 1 ε µ 8 =− ∇·j + z ∇·jsz − ·∇µ dt T T T z • Entropy production equation ds =−∇·js + R with R ≥ 0 dt
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 10
Entropy Production
Tds = dε − µzdsz − 8 · d(∇2)
• Form time derivative of entropy density ε µ 8 (∇2) ds = 1 d − z dsz − · d dt T dt T dt T dt ε • Conservation laws and dynamics of broken symmetry variable (j , jsz unknown)
ds 1 ε µ 8 =− ∇·j + z ∇·jsz − ·∇µ dt T T T z • Entropy production equation ds =−∇·js + R with R ≥ 0 dt • Identify the entropy current and production
s −1 ε sz j = T (j − µzj )
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8)·∇µz
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) · ∇T − (j + 8) · ∇µz
(strategy: R should be a function of gradients of the conjugate variables)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero.
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8 =−K ∇2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8 =−K ∇2
• Energy current ε sz j = µzj
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8 =−K ∇2
• Energy current ε sz j = µzj =−µz K ∇2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8 =−K ∇2
• Energy current ε sz j = µzj =−µz K ∇2
• Entropy current js = 0
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 11
Equilibrium Dynamics Entropy Production
−1 ε sz sz RT =−T (j − µzj ) ·∇T − (j + 8) ·∇µz
(strategy: R should be a function of gradients of the conjugate variables) In the absence of dissipation the rate of entropy production must be zero. • Spin current jsz =−8 =−K ∇2
• Energy current ε sz j = µzj =−µz K ∇2
• Entropy current js = 0
We will consider adding dissipation later.
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
• superfluidity occurs due to Bose condensation
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
• superfluidity occurs due to Bose condensation • the order parameter is “the expectation value of the quantum field operator for destroying a particle” 9 =hψi
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
• superfluidity occurs due to Bose condensation • the order parameter is “the expectation value of the quantum field operator for destroying a particle” 9 =hψi • 9 is a complex variable: 9 =|9|ei2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
• superfluidity occurs due to Bose condensation • the order parameter is “the expectation value of the quantum field operator for destroying a particle” 9 =hψi • 9 is a complex variable: 9 =|9|ei2 2 |9| gives the “condensate density” n0: the fraction of particles in the zero momentum state is n0/n 2 is the phase of the condensate wave function
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 12
Superfluidity
• superfluidity occurs due to Bose condensation • the order parameter is “the expectation value of the quantum field operator for destroying a particle” 9 =hψi • 9 is a complex variable: 9 =|9|ei2 2 |9| gives the “condensate density” n0: the fraction of particles in the zero momentum state is n0/n 2 is the phase of the condensate wave function There are a macroscopic number of particles in a single wave function and so 2 is a macroscopic thermodynamic variable,andis the broken symmetry variable.
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
• Any phase gives an equivalent state; the ordered state is characterized by a particular phase
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
• Any phase gives an equivalent state; the ordered state is characterized by a particular phase • There is an energy cost for gradients of the phase Z 1 h¯ 2 E = n (∇2)2 dd x 2 s m
2 Stiffness constant K is written as ns(h¯ /m) and ns is called the superfluid density
Stiffness constant not the same as the condensate density ns 6= n0
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
• Any phase gives an equivalent state; the ordered state is characterized by a particular phase • There is an energy cost for gradients of the phase Z 1 h¯ 2 E = n (∇2)2 dd x 2 s m
2 Stiffness constant K is written as ns(h¯ /m) and ns is called the superfluid density
Stiffness constant not the same as the condensate density ns 6= n0 • Conjugate variable to the phase 2 is the number of particles N
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
• Any phase gives an equivalent state; the ordered state is characterized by a particular phase • There is an energy cost for gradients of the phase Z 1 h¯ 2 E = n (∇2)2 dd x 2 s m
2 Stiffness constant K is written as ns(h¯ /m) and ns is called the superfluid density
Stiffness constant not the same as the condensate density ns 6= n0 • Conjugate variable to the phase 2 is the number of particles N • Currents and dynamics of the phase are coupled to the density, i.e., mass or electric currents
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 13
Broken Phase (Gauge) Symmetry
• Any phase gives an equivalent state; the ordered state is characterized by a particular phase • There is an energy cost for gradients of the phase Z 1 h¯ 2 E = n (∇2)2 dd x 2 s m
2 Stiffness constant K is written as ns(h¯ /m) and ns is called the superfluid density
Stiffness constant not the same as the condensate density ns 6= n0 • Conjugate variable to the phase 2 is the number of particles N • Currents and dynamics of the phase are coupled to the density, i.e., mass or electric currents • Currents are present in equilibrium, and so are supercurrents
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 14
Supercurrents by Analogy
• One-to-one correspondence at the quantum operator level
hN¯ ≡ Sz and 2phase ≡−2spin
(e.g., ↑≡ particle, ↓≡ no particle)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 14
Supercurrents by Analogy
• One-to-one correspondence at the quantum operator level
hN¯ ≡ Sz and 2phase ≡−2spin
(e.g., ↑≡ particle, ↓≡ no particle) • Gradient of the phase gives a flow of particles ∂n =−∇·j with j = n (h¯/m)∇2 ∂t s
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 14
Supercurrents by Analogy
• One-to-one correspondence at the quantum operator level
hN¯ ≡ Sz and 2phase ≡−2spin
(e.g., ↑≡ particle, ↓≡ no particle) • Gradient of the phase gives a flow of particles ∂n =−∇·j with j = n (h¯/m)∇2 ∂t s
• Often associate a flow with a velocity: introduce superfluid velocity
vs = (h¯/m)∇2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 14
Supercurrents by Analogy
• One-to-one correspondence at the quantum operator level
hN¯ ≡ Sz and 2phase ≡−2spin
(e.g., ↑≡ particle, ↓≡ no particle) • Gradient of the phase gives a flow of particles ∂n =−∇·j with j = n (h¯/m)∇2 ∂t s
• Often associate a flow with a velocity: introduce superfluid velocity
vs = (h¯/m)∇2 and then j = nsvs
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 14
Supercurrents by Analogy
• One-to-one correspondence at the quantum operator level
hN¯ ≡ Sz and 2phase ≡−2spin
(e.g., ↑≡ particle, ↓≡ no particle) • Gradient of the phase gives a flow of particles ∂n =−∇·j with j = n (h¯/m)∇2 ∂t s
• Often associate a flow with a velocity: introduce superfluid velocity
vs = (h¯/m)∇2 and then j = nsvs • Or write in terms of flow of mass ∂ρ =−∇·g with g = ρ v ,ρ = mn ∂t s s s s
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 15
Hydrodynamic Derivation • Free energy expression: generalized rigidity and energy in external potential V h¯ 2n 1 f = s (∇2)2 + Kn2 + Vn 2m 2 (K is bulk modulus)
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 15
Hydrodynamic Derivation • Free energy expression: generalized rigidity and energy in external potential V h¯ 2n 1 f = s (∇2)2 + Kn2 + Vn 2m 2 (K is bulk modulus) • Equilibrium phase dynamics (Larmor precession theorem) from dynamics with added constant potential δV : − δ 9(V, t) = 9(0, t)e ihN¯ Vt
gives ∂ f ¯2˙ =−δ ¯2˙ =− =−µ h V or in general h ∂ n T
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 15
Hydrodynamic Derivation • Free energy expression: generalized rigidity and energy in external potential V h¯ 2n 1 f = s (∇2)2 + Kn2 + Vn 2m 2 (K is bulk modulus) • Equilibrium phase dynamics (Larmor precession theorem) from dynamics with added constant potential δV : − δ 9(V, t) = 9(0, t)e ihN¯ Vt
gives ∂ f ¯2˙ =−δ ¯2˙ =− =−µ h V or in general h ∂ n T • Entropy production argument from the thermodynamic identity
2 dε = Tds+ µdn + 8 · d(∇2) with 8 = (h¯ ns/m)∇2 gives the current of particles
n˙ =−∇·j with j = ns (h¯/m)∇2
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 16
Currents that Flow Forever
Θ
Θ(r)
L
= ρ ( / )( π/ ) g = ρs(h¯/m)(π/L) g s h¯ m 2 L H · = h vs dl m quantum of circulation
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 17
Josephson Effect
y
x 12
• Energy depends on phase difference. For weak coupling
E =−Jc cos(22 − 21)
• Change in number of particles: current I = dN2/dt dE I = d22
d.c. Josephson effect I = Jc sin(22 − 21)
• Time dependence of phase is given by the potential ˙ h¯2i =−µi ˙ ˙ a.c. Josephson effect h¯(22 − 21) =−1µ
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 18
Breakdown of Superfluidity n∆µ = −s∆T + ∆P
vs
˙ h¯12 =−1µ, vs = (h¯/m)ns 12/L
• pressure or temperature difference accelerates superflow • constant superflow does not require pressure drop
Back Forward Collective Effects in Equilibrium and Nonequilibrium Physics: Lecture 4, April 7, 2006 18
Breakdown of Superfluidity n∆µ = −s∆T + ∆P
vs
˙ h¯12 =−1µ, vs = (h¯/m)ns 12/L
• pressure or temperature difference accelerates superflow • constant superflow does not require pressure drop n∆µ = −s∆T + ∆P