P. Wiegmann- Quantum Shock Waves and Emergence of Quantized Edge States
Transcript of P. Wiegmann- Quantum Shock Waves and Emergence of Quantized Edge States
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Quantum Shock Waves andEmergence of Quantized Edge States
Together with Alexander Abanov and Eldad Bettelheim
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P. Wiegmann
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FQHE - topological quantum liquid: a gapped state on a closed manifold with a monodromy.
The ground state is degenerate on a multiply-connected closed maniol
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Probing is possible only through a boundary
Point like, or extended
Extended boundary - an Edge
Topological liquid is not gapped any longer -
Edge states propagate as a sound - subject to decoherence
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Edge state carries the information of the topology:
Edge tunneling, noise measurements.
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Topological aspects:
fractional charge and braidingcan be measured in edge states out-of- equlibrium
Quantum Shock Wave
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A smooth bump in density propagating:
all gradients
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(i) transport on the edge is essentially non-linear,
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Disipativeless shock waves
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Each Soliton carries a FRACTIONAL CHARGE
Soliton Train
time
space
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How to describe quantum dynamics of Edge State?
Step 1: Conjecture:
Edge state (Abelian state) is effectivelydescribed by Calogero model
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V (x ) = (x ) 1
x 2,
1sinh 2 x
,
Interpolates between Lattinger liquid and Calogeromodel - quantum wires, edge states of FQHE
Model Hamiltonian: Calogero model
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Shock wave: Riemann-Hopf Equation
+ ( x )2 = 0
Classical Riemann equations are ill-dened (no single valued solutions)
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Stabilization of shock waves by:
(i) by quantum corrections;
(ii) by interaction
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V (x ) = (x ) 1
x 2,
1sinh 2 x
,
=12
( x )2 + 2x
=1
L cotx x
L (x )dx
Interaction -- stabilizes shock wave through dispersion
(x + iL ) = (x )
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=12
( x )2 + 2x
=1
L cotx x
L (x )dx
L 0 : =12
( x )2 + 3x
ILW-equation
KdV-equation
L : = 12
( x )2 + 2x (x )x x dx
Benjamin-Ono equation
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(i) Lattinger Liquid - short range interaction:
+ ( x )2
+ 3x
= 0 KdV-equation
(ii)Fractional Hall Edge State - long range interaction (Calogero model)
+ ( x )2 + 2x H = 0 Benjamin-Ono equation
H (x ) = (z )x z dz2 i
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(i) KdV-equation: Non-linear waves in shallow water
+ ( x )2
+ 3x
= 0
(ii) Benjamin-Ono equation: Non-linear waves in deep water
+ ( x )2 + 2x H = 0
H (x ) = (z )x z dz2 i
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On the relation between Calogero model and CFT
=
xT
T = ( x )2 + 0 2x
0 =
1 /
( 1)(x i x j )2
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Period of oscillations is
(interaction) () 1 >> k 1F
Quantum Non-linear Equations can be treated semiclassically
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Conclusions:
Transport is 1D-electronic systems is essentially non-linear,
Any smooth semiclassical excitation evolving in timeis unstable, and eventually sharp,
will be fragmented to individual soliton-likeparticles,
Fermi-surface is an essentially semiclassical , it is destroyed inevolution.
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M i Gl
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Morning Glory
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Chain of rolling cloudsMorning glory
South Australia Believed to be Benjamin-Ono eq
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