Emergence of quantum dynamics in hyperbolic dynamical systems
Based onarxiv:1706.09307andarxiv:2102.11196 Slides are on myweb-page.
F. Faure(Grenoble) with M. Tsujii (Kyushu),
March 8, 2022, Roscoff
Question
Does aquantum behaviornaturally emerges in anAnosov geodesic flowon a compact Riemannian manifold(N,g)(i.e. a model of deterministic chaos)?
What meansAnosov geodesic flow? this is for example the motion of a free (classical) particle with , constant velocity on a negatively curved manifold(N,g), (with HamiltonianH(q,p) =kpkg onT∗N). See movie1, movie2,movie3.
Question
Does aquantum behaviornaturally emerges in anAnosov geodesic flowon a compact Riemannian manifold(N,g)(i.e. a model of deterministic chaos)?
What meansAnosov geodesic flow? this is for example the motion of a free (classical) particle with , constant velocity on a negatively curved manifold(N,g), (with HamiltonianH(q,p) =kpkg onT∗N). See movie1, movie2,movie3.
Question
Does aquantum behaviornaturally emerges in anAnosov geodesic flowon a compact Riemannian manifold(N,g)(i.e. a model of deterministic chaos)?
What meansAnosov geodesic flow? this is for example the motion of a free (classical) particle with , constant velocity on a negatively curved manifold(N,g), (with HamiltonianH(q,p) =kpkg onT∗N). See movie1, movie2,movie3.
geodesic flow
compact surface N
X X
Es Eu
q
φt(m)
M= (T∗N)1=S∗N m= (q,p)
Question
Does aquantum behaviornaturally emerges in anAnosov geodesic flowon a compact Riemannian manifold(N,g)(i.e. a model of deterministic chaos)?
What meansAnosov geodesic flow? this is for example the motion of a free (classical) particle with , constant velocity on a negatively curved manifold(N,g), (with HamiltonianH(q,p) =kpkg onT∗N). See movie1, movie2,movie3.
Does quantum behavior emerges in an Anosov geodesic flow?
What meansquantum behavior? From quantization procedureOp(.), (e.g.
Op(pj) =−i∂q∂
j), from the geodesic flow, we get the“wave operator”
√∆≈Op kpkg
(with the Hodge Laplacian∆ =d†d), that generates the wave equation, forut ∈C∞(N),t∈R:
∂tut =i√
∆ut =⇒ ∂t2ut =−∆ut
Does quantum behavior emerges in an Anosov geodesic flow?
What meansquantum behavior? From quantization procedureOp(.), (e.g.
Op(pj) =−i∂q∂
j), from the geodesic flow, we get the“wave operator”
√∆≈Op kpkg
(with the Hodge Laplacian∆ =d†d), that generates the wave equation, forut ∈C∞(N),t∈R:
∂tut =i√
∆ut =⇒ ∂t2ut =−∆ut
Semi-classical analysis(WKB theory, Egorov’s Theorem etc) shows that for small wave-lengthλ1, functionut is approximately transported by the geodesics:
wave equation =⇒
tfixed,λ→0 geodesic flow
Ex: geometrical optics is a limit of wave optics with λ≈0.5µm. Classical Newto- nian mechanics is a limit of quantum Schrödinger mechanics. See movie
N waveut
Does quantum behavior emerges in an Anosov geodesic flow?
What meansquantum behavior? From quantization procedureOp(.), (e.g.
Op(pj) =−i∂q∂
j), from the geodesic flow, we get the“wave operator”
√∆≈Op kpkg
(with the Hodge Laplacian∆ =d†d), that generates the wave equation, forut ∈C∞(N),t∈R:
∂tut =i√
∆ut =⇒ ∂t2ut =−∆ut
Semi-classical analysis gives:
wave equation =⇒
tfixed,λ→0 geodesic flow Curiously, our question concerns theopposite direction:
geodesic flow=⇒
??! wave equation What does it mean? are thereindicationsfor this?
The geodesic flow in functional analysis
It will be convenient to consider thevector fieldX =P
jXj(x)∂x∂
j as a derivation operator, generator of the pull back of functionsv by the flowφt:
etXu=u◦φt. Then itsL2-adjoint etX†
called “Ruelle transfer operator”, transports probabilities, e.g.
etX†
δm=δφt(m) :particle dynamics.
Vector field stable
E0(x)
Eu(x)
unstable direction
X X
Es
Eu
Flowφt(m) Es(x)
M t1 u
v etXu
etXu
m
The geodesic flow in functional analysis
It will be convenient to consider thevector fieldX =P
jXj(x)∂x∂
j as a derivation operator, generator of the pull back of functionsv by the flowφt:
etXu=u◦φt. Then itsL2-adjoint etX†
called “Ruelle transfer operator”, transports probabilities, e.g.
etX†
δm=δφt(m) :particle dynamics.
Vector field stable
E0(x)
Eu(x)
unstable direction
X X
Es
Eu
Flowφt(m) Es(x)
M t1 u
v etXu
etXu
m
Ruelle resonances
A lot of contributions in mathematics: D. Ruelle, D. Bowen, M. Pollicott, H.
Rugh, Blank, Keller, V. Baladi, O. Butterley, C. Liverani, M. Tsujii, S. Gouëzel, Giullietti, F. Naud, N. Roy, F.F., J. Sjöstrand, M. Zworski, S. Dyatlov, C.
Guillarmou, T. Weich, Hilgert, B. Küster, J. Slipantschuk, O. Bandtlow, V. Dang, G. Rivière, T. Lefeuvre, Y. Chaubet, M. Jezequel, Y.G. Bonthonneau, M.Cekic, A.
Medanne, etc
Theorem
(Butterley-Liverani 07, Sjöstrand-F.F. 11) IfX is AnosovthenX has intrinsic discrete spectrum in some anisotropic Sobolev space, calledRuelle spectrumof X.
Theonly obvious eigenvalue isX1=0. Are there other eigenvalues? what are they?
Ruelle resonances
A lot of contributions in mathematics: D. Ruelle, D. Bowen, M. Pollicott, H.
Rugh, Blank, Keller, V. Baladi, O. Butterley, C. Liverani, M. Tsujii, S. Gouëzel, Giullietti, F. Naud, N. Roy, F.F., J. Sjöstrand, M. Zworski, S. Dyatlov, C.
Guillarmou, T. Weich, Hilgert, B. Küster, J. Slipantschuk, O. Bandtlow, V. Dang, G. Rivière, T. Lefeuvre, Y. Chaubet, M. Jezequel, Y.G. Bonthonneau, M.Cekic, A.
Medanne, etc
Theorem
(Butterley-Liverani 07, Sjöstrand-F.F. 11) IfX is AnosovthenX has intrinsic discrete spectrum in some anisotropic Sobolev space, calledRuelle spectrumof X.
Theonly obvious eigenvalue isX1=0. Are there other eigenvalues? what are they?
Ruelle resonances
A lot of contributions in mathematics: D. Ruelle, D. Bowen, M. Pollicott, H.
Rugh, Blank, Keller, V. Baladi, O. Butterley, C. Liverani, M. Tsujii, S. Gouëzel, Giullietti, F. Naud, N. Roy, F.F., J. Sjöstrand, M. Zworski, S. Dyatlov, C.
Guillarmou, T. Weich, Hilgert, B. Küster, J. Slipantschuk, O. Bandtlow, V. Dang, G. Rivière, T. Lefeuvre, Y. Chaubet, M. Jezequel, Y.G. Bonthonneau, M.Cekic, A.
Medanne, etc
Theorem
(Butterley-Liverani 07, Sjöstrand-F.F. 11) IfX is AnosovthenX has intrinsic discrete spectrum in some anisotropic Sobolev space, calledRuelle spectrumof X.
Theonly obvious eigenvalue isX1=0. Are there other eigenvalues? what are they?
Preliminary on Ruelle spectrum: a toy model to have in mind
The simple 1 dim contracting vector fieldX =−xd.
dx on R≡Es, gives∀k ∈N, Xxk = (−k)xk. X generates the flowφt(x) =e−tx.
OnT∗R≡T∗Es, the induced flow isφ˜t(x, ξ) = (etx,e−tξ).
0 e−tx x
ξ
0 x
Preliminary on Ruelle spectrum: a toy model to have in mind
The simple 1 dim contracting vector fieldX =−xd.
dx on R≡Es, gives∀k ∈N, Xxk = (−k)xk. X generates the flowφt(x) =e−tx.
OnT∗R≡T∗Es, the induced flow isφ˜t(x, ξ) = (etx,e−tξ).
0 e−tx x
ξ
0 x
Preliminary on Ruelle spectrum: a toy model to have in mind
The simple 1 dim contracting vector fieldX =−xd.
dx on R≡Es, gives∀k ∈N, Xxk = (−k)xk. X generates the flowφt(x) =e−tx.
OnT∗R≡T∗Es, the induced flow isφ˜t(x, ξ) = (etx,e−tξ).
0 e−tx x
ξ
0 x
Formal spectrum:
∀k∈N, Xxk = (−k)xk, "Taylor" spectral projectors: Tk =xkh1
k!δ(k)|.iL2. butxk, δ(k)∈/L2(R).
Preliminary on Ruelle spectrum: a toy model to have in mind
The simple 1 dim contracting vector fieldX =−xd.
dx on R≡Es, gives∀k ∈N, Xxk = (−k)xk. X generates the flowφt(x) =e−tx.
OnT∗R≡T∗Es, the induced flow isφ˜t(x, ξ) = (etx,e−tξ).
0 e−tx x
ξ
0 x
InL2(R),Spec(X) =iR+12,becauseX†=−X +1⇔ X−12
=− X−12†
.
Preliminary on Ruelle spectrum: a toy model to have in mind
The simple 1 dim contracting vector fieldX =−xd.
dx on R≡Es, gives∀k ∈N, Xxk = (−k)xk. X generates the flowφt(x) =e−tx.
OnT∗R≡T∗Es, the induced flow isφ˜t(x, ξ) = (etx,e−tξ).
0 e−tx x
ξ
0 x
InHW (R) :={u∈ S(R)} withkukH
W(R):=
D√
hξEm FD√
hxE−m
u L2
, 0<h1,m≥0, the spectrumofX is:
Ess. spec. discrete Ruelle spectrum
−2 −1 0
−2m−o(1) −m−k+2+...o(1)
Ex: geodesic flow on a surface with const. neg.
curv.
Usingsl2Ralgebra[X,U±] =±U±,[U+,U−] =2X,∆ :=−X2−X−U−U+, (ref: Selberg, M. Ratner, Flaminio-Forni 02, Dyatlov-Guillarmou-F 15), theRuelle spectrum ofX onΓ\SL2(R)is on vertical lineszk,l =−12−k±iq
µl−14:
Finite rank contribution Equilibrium (mixing) z0,l
z1,l
0 Im(z)
z0,l+1
zk,l=−1/2−k±iq µl−14
−5/2 γ1=−3/2 γ0=−1/2
onN= Γ\SL2(R)/SO2
µ0=1≤µ1≤µ2...
with∆ul=µlul
k,l∈N
Re(z)
¯ z0,l
Wave operator on each line, fluctuations∼e−12teiωjt
∼e−32teiωjt
Ruelle eigenvalues ofX(from ppcal series) are
Rem: if X has eigenvaluea+iω∈Cthen etX has eigenvalue eat
|{z}
decay
eiωt
|{z}
oscillation
.
Quantum behavior emerges in an Anosov geodesic flow?
For constant neg. surfaceN = Γ\SL R2
/SO R2
, we have seen the appearance of the spectrum ofq
∆−14 in the Ruelle spectrum ofX, i.e some indication that
geodesic flow=⇒
??! wave equation Is it anexceptional algebraic phenomenon?
What about ageneral Anosov geodesic flowφt =etX (with non constant curvature)?
Quantum behavior emerges in an Anosov geodesic flow?
For constant neg. surfaceN = Γ\SL R2
/SO R2
, we have seen the appearance of the spectrum ofq
∆−14 in the Ruelle spectrum ofX, i.e some indication that
geodesic flow=⇒
??! wave equation Is it anexceptional algebraic phenomenon?
What about ageneral Anosov geodesic flowφt =etX (with non constant curvature)?
“Effective classical dynamics”. Vertical bands.
Consider a generalAnosov geodesic vector fieldX onM = (T∗N)1. LetF →M a vector bundle andXF aderivationon C∞(M;F)overX:
XF(fu) =X(f)u+fXF(u), ∀f ∈C∞(M),∀u∈C∞(M;F). Consider evolution of sections ofFk by the flow, with a generator denoted XFk :C(M;Fk) , calledeffective classical dynamics.
Then thespectrumof the operatorXFk in L2(M;Fk)is contained in the vertical bandBk :=
γk−, γk+
×iR,
γ2+ γ1− γ+1γ0− γ+0
B0
Re(z)
boundedresolvent boundedresolvent ω=Im(z)
γ−2
B2 B1
“Effective classical dynamics”. Vertical bands.
Consider a generalAnosov geodesic vector fieldX onM = (T∗N)1. For everyk ∈N, we introduce thefinite rank vector bundleoverM:
Fk :=|detEs|−1/2⊗Polk(Es)⊗F →M, (1) Consider evolution of sections ofFk by the flow, with a generator denoted XFk :C(M;Fk) , calledeffective classical dynamics.
Then thespectrumof the operatorXFk in L2(M;Fk)is contained in the vertical bandBk :=
γk−, γk+
×iR,
γ2+ γ1− γ+1γ0− γ+0
B0
Re(z)
boundedresolvent boundedresolvent ω=Im(z)
γ−2
B2 B1
“Effective classical dynamics”. Vertical bands.
Consider a generalAnosov geodesic vector fieldX onM = (T∗N)1. For everyk ∈N, we introduce thefinite rank vector bundleoverM:
Fk :=|detEs|−1/2⊗Polk(Es)⊗F →M, (1) Consider evolution of sections ofFk by the flow, with a generator denoted XFk :C(M;Fk) , calledeffective classical dynamics.
Then thespectrumof the operatorXFk in L2(M;Fk)is contained in the vertical bandBk :=
γk−, γk+
×iR,
γ2+ γ1− γ+1γ0− γ+0
B0
Re(z)
boundedresolvent boundedresolvent ω=Im(z)
γ−2
B2 B1
“Effective classical dynamics”. Vertical bands.
Consider a generalAnosov geodesic vector fieldX onM = (T∗N)1. For everyk ∈N, we introduce thefinite rank vector bundleoverM:
Fk :=|detEs|−1/2⊗Polk(Es)⊗F →M, (1) Consider evolution of sections ofFk by the flow, with a generator denoted XFk :C(M;Fk) , calledeffective classical dynamics.
Then thespectrumof the operatorXFk in L2(M;Fk)is contained in the vertical bandBk :=
γk−, γk+
×iR, with
γk±:= lim
t→±∞log
etXFk
1/t L∞. Ex: forX on M= Γ\SL2R, F=C, thenγk±=−12−k.
γ2+ γ1− γ+1γ0− γ+0
B0
Re(z)
boundedresolvent boundedresolvent ω=Im(z)
γ−2
B2 B1
“Effective classical dynamics”. Vertical bands.
Consider a generalAnosov geodesic vector fieldX onM = (T∗N)1. For everyk ∈N, we introduce thefinite rank vector bundleoverM:
Fk :=|detEs|−1/2⊗Polk(Es)⊗F →M, (1) Consider evolution of sections ofFk by the flow, with a generator denoted XFk :C(M;Fk) , calledeffective classical dynamics.
Then thespectrumof the operatorXFk in L2(M;Fk)is contained in the vertical bandBk :=
γk−, γk+
×iR, We have
− d
2 +k
λmax+cF ≤γk−≤γk+≤ − d
2 +k
λmin+CF,
where 0< λmin≤λmax are the minimal/maximal Lyap. exponents,d=dimEu/s.
γ2+ γ1− γ+1γ0− γ+0
B0
Re(z)
boundedresolvent boundedresolvent ω=Im(z)
γ−2
B2 B1
“Emergence of quantum dynamics”
Theorem
(M.Tsujii-F.F. 2021) For a derivationXF on C∞(M;F)over acontact Anosov vector fieldX onM,∀K ∈N,∀ >0,∃anisotropic Sobolev spaceHW(M;F),
∃C >0,∀t >0, etXF
|{z}
classical dynamics
=
K
M
k=0
OpΣ etXFk
| {z }
quantum dynamics
+ Rt
|{z}
finite rank
+OHW
et(γK+1+ +)
| {z }
neglictible
, (2)
Recall thatγK+1+ → −∞asK → ∞.
OpΣ etXFk
is thegeometric quantizationof theeffective classical dynamicsXFk :C(Σ;F) , where Σ = (Eu⊕Es)⊥⊂T∗M is the symplectic trapped set. (More details below...)
Consequences
∀C >0,∀ >0,∃ω>0, s.t. the Ruelle discrete spectrum ofX for Re(z)>−C,|Im(z)|> ω,iscontained in vertical bands
Re(z)∈ [
k≥0
γk−−, γk++
with a precisedensity rank(F(2π)k)Vol(M)d+1 ωd (calledWeyl law).
(a)
γ+2 γ−1 γ1+γ−0 γ0+ B0
Re(z) H
ˇ γ0
−2λmaxr+C0
−λminr+C
B2 B1
boundedresolvent
ωε
ω=Im(z)
Essential spectrum
r1
Intrinsic discrete spectrum
Spectrum that controls emerging behavior
boundedresolvent boundedresolvent
Related papers: Cekic-Guillarmou 20: 1st band for contact Anosov flow in dim. 3 using horocycle operators.
A special and interesting bundle F = |detE
s|
1/2→ M
For the first bandk =0 we get thetrivial bundle:
F0=|detEs|−1/2⊗Polk=0(Es)⊗F =C
From (2), fort 1, the operator etXF is well described by the dominant term OpΣ etXF0
that is the “quantization” of the dynamicsX itself.
The eigenvalues ofXF accumulate on the imaginary axisRe(z) =γ0±=0 with density given by the Weyl law, separated by a uniform spectral gapγ1+<0.
EquilibriumGibbs Re(z) ω=Im(z)
spectral gap
B0
asymptotic
γ1+
−C
A special and interesting bundle F = |detE
s|
1/2→ M
For the first bandk =0 we get thetrivial bundle:
F0=|detEs|−1/2⊗Polk=0(Es)⊗F =C
From (2), fort 1, the operator etXF is well described by the dominant term OpΣ etXF0
that is the “quantization” of the dynamicsX itself.
The eigenvalues ofXF accumulate on the imaginary axisRe(z) =γ0±=0 with density given by the Weyl law, separated by a uniform spectral gapγ1+<0.
EquilibriumGibbs Re(z) ω=Im(z)
spectral gap
B0
asymptotic
γ1+
−C
A special and interesting bundle F = |detE
s|
1/2→ M
For the first bandk =0 we get thetrivial bundle:
F0=|detEs|−1/2⊗Polk=0(Es)⊗F =C
From (2), fort 1, the operator etXF is well described by the dominant term OpΣ etXF0
that is the “quantization” of the dynamicsX itself.
The eigenvalues ofXF accumulate on the imaginary axisRe(z) =γ0±=0 with density given by the Weyl law, separated by a uniform spectral gapγ1+<0.
EquilibriumGibbs Re(z) ω=Im(z)
spectral gap
B0
asymptotic
γ1+
−C
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
etXF is aFourier integral operator: in the limit of high frequencies, evolution of functions by the pull-back operatoretXF is well described on the cotangent bundle T∗M with the induced flowφ˜t:= (dφt)∗,t ∈R.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
We introduce a specific metric g on T∗M, compatible with the symplectic form and then we define an L2-isometric “wave-packet transform” T : C∞(M;F) → S(T∗M;F), that allows to use micro-local analysis on T∗M for the pull back operatoretXF. The unit boxes for the metricg correspond to the effective size of wave-packets and reflect theuncertainty principle.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
The dynamics φ˜t is a “scattering dynamics” on the trapped set Σ = R∗A ⊂ T∗M (Liouville 1-form) and Σ is symplectic and normally hyperbolic. As a consequence, for large time |t| 1, the outer part of the trapped set Σ has a negligible contribution, because information escapes away (i.e. the Sobolev norm measured by the specific weight W decays). So only the dynamics in a vicinity of Σplays a role for our purpose.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
We will hence consider a vicinity ofΣof a giveng−sizeωµ/2, with some 0< µ <1.
Remark that the projection on M has sizeω−(1−µ)/2 1 if ω 1. This will allow us to use thelinearization of the dynamicsφ˜t as a local approximation.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
In this vicinity of Σ there is a micro-local decoupling between the directions tangent to Σ and those (symplectically)normal to Σ, represented by a normal vector bundle denotedN→Σ. Forρ∈Σ,
TρT∗M= TρΣ
|{z}
Tangent
⊕⊥(Nu(ρ)⊕Ns(ρ))
| {z }
normal
:invariant decomp.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
The dynamics on the normal direction N is hyperbolic and responsible for the emergence of polynomial functions along the stable directionNs ≡Es idemX =
−xd.dx, Xxk = (−k)xk on R. We introduce approximate projectors OpΣ(Tk) that restricts functions to the symplectic trapped set Σ and that are polynomial valued alongNs with degreek. This projector plays a similar role as the Bergman projector (or Szegö projector) in geometric quantization. What remains for large time, is aneffective Hilbert spaceof quantum waves that live on the trapped set Σ, valued in the vector bundleFk.
Ideas of the proof
flow
Lifted flow X
Ns(ρ)
m Es
T∗M M
Eu
Sizeω−(1−µ)/21
Nu(ρ)
0
ρ=ωA(m)
Σ = (Eu⊕Es)⊥ symplectic Trapped set
< ω >µ/2 ω
φt
φ˜t N(ρ)
Rem: the main geometrical object considered in this paper is this fibration Ns →Σ→M. Beware that for a geodesic flow on(N,g), this fibration sequence continues withM =T1∗N → N.
What is the meaning of going beyond the equilibrium description for the Ruelle spectrum?
Illustration: the ocean is quite, deep, flat, gentle ≡Equilibrium state, but with a better look, the behavior at the surface may be furious, wavy, and never stop to move. Are they neglictible?
Some very speculative question: can quantum dynamics in the physics world emerges from an underlying chaotic deterministic yet unknown system?
Thank you for your attention!
What is the meaning of going beyond the equilibrium description for the Ruelle spectrum?
Illustration: the ocean is quite, deep, flat, gentle ≡Equilibrium state, but with a better look, the behavior at the surface may be furious, wavy, and never stop to move. Are they neglictible?
Some very speculative question: can quantum dynamics in the physics world emerges from an underlying chaotic deterministic yet unknown system?
Thank you for your attention!
What is the meaning of going beyond the equilibrium description for the Ruelle spectrum?
Illustration: the ocean is quite, deep, flat, gentle ≡Equilibrium state, but with a better look, the behavior at the surface may be furious, wavy, and never stop to move. Are they neglictible?
Some very speculative question: can quantum dynamics in the physics world emerges from an underlying chaotic deterministic yet unknown system?
Thank you for your attention!
(*) Wave packets
Local flow box coordinates onM: y = (x,z)∈Rn×Rs.t. X = ∂z∂ and dual coordinatesη = (ξ, ω)∈Rn×Ron Ty∗M.
η−α
δ x z
X
flow direction
M m
ξ
ω δ−1
0 ω=0
η ηα
T∗mM
Let 12≤α <1 and 0< δ 1. Wave packet functionis:
ϕ(y,η) y0
≈
|η|1aexp iη.y0−
x0−x hηi−α
2
−
z0−z δ
2!
,
ϕ(y,η)
L2(M) ≈
|η|11
Metricg onT∗M, compatible withΩ =dy∧dη:
gy,η= dx
hηi−α 2
+ dξ
hηiα 2
+ dz
δ 2
+ dω
δ−1 2
Rem: α≥12 ⇔g remains equivalent uniformly/η after change of flow box coordinates.
(*) Wave packets
Local flow box coordinates onM: y = (x,z)∈Rn×Rs.t. X = ∂z∂ and dual coordinatesη = (ξ, ω)∈Rn×Ron Ty∗M.
η−α
δ x z
X
flow direction
M m
ξ
ω δ−1
0 ω=0
η ηα
T∗mM
Let 12≤α <1 and 0< δ 1. Wave packet functionis:
ϕ(y,η) y0
≈
|η|1aexp iη.y0−
x0−x hηi−α
2
−
z0−z δ
2!
,
ϕ(y,η)
L2(M) ≈
|η|11
Metricg onT∗M, compatible withΩ =dy∧dη:
gy,η= dx
hηi−α 2
+ dξ
hηiα 2
+ dz
δ 2
+ dω
δ−1 2
Rem: α≥12 ⇔g remains equivalent uniformly/η after change of flow box coordinates.
(*) Wave packets
Local flow box coordinates onM: y = (x,z)∈Rn×Rs.t. X = ∂z∂ and dual coordinatesη = (ξ, ω)∈Rn×Ron Ty∗M.
η−α
δ x z
X
flow direction
M m
ξ
ω δ−1
0 ω=0
η ηα
T∗mM
Let 12≤α <1 and 0< δ 1. Wave packet functionis:
ϕ(y,η) y0
≈
|η|1aexp iη.y0−
x0−x hηi−α
2
−
z0−z δ
2!
,
ϕ(y,η)
L2(M) ≈
|η|11
Metricg onT∗M, compatible withΩ =dy∧dη:
gy,η= dx
hηi−α 2
+ dξ
hηiα 2
+ dz
δ 2
+ dω
δ−1 2
Rem: α≥12 ⇔g remains equivalent uniformly/η after change of flow box coordinates.
(*) Wave packet transform
(or FBI, wavelet, Bargmann, Anti-Wick... transform)(Abuse of notations that forget charts and partitions of unity.) T :
(C∞(M) → S(T∗M)
u(y0) →(Tu) (y, η) :=hϕy,η,uiL2(M)
Lemma (fundamental 1.
”Resolution of identity”)
T∗◦ T =Id
Bergmann projector
L2(M) T
P=T T†
L2(T∗M) u
v
Im(T) T†
Remarks: ∀u∈C∞(M), u(y0) =R
T∗Mϕy,η(y0)hϕy,η,ui(2π)dydηn+1. T :L2(M)→Im(T)⊂L2(T∗M)is an isomorphism. Hencewe “lift the analysis toT∗M”.
Π =T ◦ T∗:L2(T∗M)→Im(T)is an orthogonal projector.