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Towards Generalized Hydrodynamic Integrability via the Characteristic Variety Abraham D. Smith Fordham University, Bronx, NY, USA December 9, 2013 Fields Institute, Toronto A.Smith (Fordham) EDS 2013-12-09 1 / 13 Short talk Get to the


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Towards Generalized Hydrodynamic Integrability via the Characteristic Variety

Abraham D. Smith

Fordham University, Bronx, NY, USA

December 9, 2013 Fields Institute, Toronto

A.Smith (Fordham) EDS 2013-12-09 1 / 13

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SLIDE 2

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.”

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 3

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.” The traditional representation theory of Lie groups begins with the question “how hard is it to integrate the infinitesimal structure of the Lie algebra into the local structure of the Lie group?”

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 4

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.” The traditional representation theory of Lie groups begins with the question “how hard is it to integrate the infinitesimal structure of the Lie algebra into the local structure of the Lie group?” Answering gives useful classes like abelian, solvable, and semi-simple and Levi’s thm.

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 5

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.” The traditional representation theory of Lie groups begins with the question “how hard is it to integrate the infinitesimal structure of the Lie algebra into the local structure of the Lie group?” Answering gives useful classes like abelian, solvable, and semi-simple and Levi’s thm. Cartan–K¨ ahler (Cauchy–Kowalevski) is the weakest (requiring strongest regularity) in a family of Cauchy integration theorems.

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 6

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.” The traditional representation theory of Lie groups begins with the question “how hard is it to integrate the infinitesimal structure of the Lie algebra into the local structure of the Lie group?” Answering gives useful classes like abelian, solvable, and semi-simple and Levi’s thm. Cartan–K¨ ahler (Cauchy–Kowalevski) is the weakest (requiring strongest regularity) in a family of Cauchy integration theorems. Therefore, examination of regularity and micro-local analysis (“how difficult is integration?”) of involutive PDE/EDS should help build our knowledge Lie pseudogroups.

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 7

Short talk – Get to the point!

Lie Pseudogroup = “sub-pseudogroup of the diffeomorphisms of a manifold that can be written as solutions of an involutive PDE/EDS, by Cartan–K¨ ahler.” The traditional representation theory of Lie groups begins with the question “how hard is it to integrate the infinitesimal structure of the Lie algebra into the local structure of the Lie group?” Answering gives useful classes like abelian, solvable, and semi-simple and Levi’s thm. Cartan–K¨ ahler (Cauchy–Kowalevski) is the weakest (requiring strongest regularity) in a family of Cauchy integration theorems. Therefore, examination of regularity and micro-local analysis (“how difficult is integration?”) of involutive PDE/EDS should help build our knowledge Lie pseudogroups. Where to find invariant notions of “difficult to integrate?”

A.Smith (Fordham) EDS 2013-12-09 2 / 13

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SLIDE 8

Dans certains cas, le nombre de ces familles de car- act´ eristiques peut ˆ etre r´ eduit, certaines familles de- venant double, triples, etc. Ces cas de r´ eduction sont analogues ` a ceux qui se pr´ esentent dans la r´ eduction d’une substitution lin´ eaire ` a sa forme normale et la rerecherche des caract´ eristiques d´ epend d’ailleurs d’une telle r´ eduction.

—Cartan, 102 years ago.

A.Smith (Fordham) EDS 2013-12-09 3 / 13

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SLIDE 9

Dans certains cas, le nombre de ces familles de car- act´ eristiques peut ˆ etre r´ eduit, certaines familles de- venant double, triples, etc. Ces cas de r´ eduction sont analogues ` a ceux qui se pr´ esentent dans la r´ eduction d’une substitution lin´ eaire ` a sa forme normale et la rerecherche des caract´ eristiques d´ epend d’ailleurs d’une telle r´ eduction.

—Cartan, 102 years ago. Moreover, those multiplicities in the charac- teristic variety can be accessed via the incidence correspondence given by the rank-one variety

  • f the tableau.

For involutive systems with higher Cartan int, submanifolds secant to the rank-one cone give hydrodynamic reductions, and the secant system indicates hydrodynamic integrability in local coordinates.

A.Smith (Fordham) EDS 2013-12-09 3 / 13

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Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol:

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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SLIDE 11

Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol: dθa ≡

  • τ(η)

a

i ∧ ωi + 1 2T a ij ωi ∧ ωj

mod θ

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol: dθa ≡

  • τ(η)

a

i ∧ ωi + 1 2T a ij ωi ∧ ωj

mod θ 0 → Z

τ

→ W ⊗ V ∗

σ

→ U ∗ → 0

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol: dθa ≡

  • τ(η)

a

i ∧ ωi + 1 2T a ij ωi ∧ ωj

mod θ 0 → Z

τ

→ W ⊗ V ∗

σ

→ U ∗ → 0 0 → Z (1) → Z ⊗ V ∗

δ

→ W ⊗ ∧2V ∗ → H 0,2(Z) → 0

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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SLIDE 14

Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol: dθa ≡

  • τ(η)

a

i ∧ ωi + 1 2T a ij ωi ∧ ωj

mod θ 0 → Z

τ

→ W ⊗ V ∗

σ

→ U ∗ → 0 0 → Z (1) → Z ⊗ V ∗

δ

→ W ⊗ ∧2V ∗ → H 0,2(Z) → 0 Characteristic Variety and Rank-One Variety:

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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SLIDE 15

Characteristic and Rank-One Variety

Two interwoven stories: rank-one variety & hydrodynamic integrability.

M, I M (1), I(1) M (2), I(2) Tp M Te M (1) TE M (2) W V Z Z (1) ω θ η κ Tableau and Symbol: dθa ≡

  • τ(η)

a

i ∧ ωi + 1 2T a ij ωi ∧ ωj

mod θ 0 → Z

τ

→ W ⊗ V ∗

σ

→ U ∗ → 0 0 → Z (1) → Z ⊗ V ∗

δ

→ W ⊗ ∧2V ∗ → H 0,2(Z) → 0 Characteristic Variety and Rank-One Variety: Ξ = {ξ ∈ V ∗ : ∃w, σξ(w) = σ(w ⊗ ξ) = 0} C = {z ∈ Z : τ(z) = w ⊗ ξ, has rank 1} (slides sloppy about P’s)

A.Smith (Fordham) EDS 2013-12-09 4 / 13

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Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 17

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 18

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 19

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. 3 The last Cartan character is sdim ˆ

ΞC = deg ˆ

ΞC.

A.Smith (Fordham) EDS 2013-12-09 5 / 13

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Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. 3 The last Cartan character is sdim ˆ

ΞC = deg ˆ

ΞC.

4 If I has no Cauchy characteristics, then ˆ

ΞC spans e∗

C.

A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 21

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. 3 The last Cartan character is sdim ˆ

ΞC = deg ˆ

ΞC.

4 If I has no Cauchy characteristics, then ˆ

ΞC spans e∗

C.

5 If ΞC = ∅, then I is Frobenius (totally integrable). A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 22

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. 3 The last Cartan character is sdim ˆ

ΞC = deg ˆ

ΞC.

4 If I has no Cauchy characteristics, then ˆ

ΞC spans e∗

C.

5 If ΞC = ∅, then I is Frobenius (totally integrable). 6 If ΞR = ∅, then I is elliptic. A.Smith (Fordham) EDS 2013-12-09 5 / 13

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SLIDE 23

Characteristic and Rank-One Variety

C Gr•(W ) Ξ Wξ ⊗ ξ Wξ = ker σξ ξ Some properties if I is involutive:

1 The eikonal system E(ΞC) is involutive on any ordinary integral N. (Typically, difficult.) 2 Ξ is essentially preserved under prolongation. 3 The last Cartan character is sdim ˆ

ΞC = deg ˆ

ΞC.

4 If I has no Cauchy characteristics, then ˆ

ΞC spans e∗

C.

5 If ΞC = ∅, then I is Frobenius (totally integrable). 6 If ΞR = ∅, then I is elliptic. 7 If ΞR has appropriate space-like hyperplanes, then I is hyperbolic. A.Smith (Fordham) EDS 2013-12-09 5 / 13

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Characteristic and Rank-One Variety

Some examples with dim Z = s = s1 = dim Z (1) = 4

involutive tableau ⇐ ⇒ commuting symbol relations compatible primary decompositions.

distinct     η1 λ1η1 µ1η1 η2 λ2η2 µ2η2 η3 λ3η3 µ3η3 η4 λ4η4 µ4η4     Ξ [1 : λ1 : µ1], [1 : λ2 : µ2], [1 : λ3 : µ3], [1 : λ4 : µ4]. C     1    ,     1    ,     1    ,     1    . Sec3(C) = 4P0. duplicates     η1 λ1η1 µ1η1 η2 λ1η2 µ1η2 η3 λ3η3 µ3η3 η4 λ4η4 µ4η4     Ξ [1 : λ1 : µ1], [1 : λ1 : µ1], [1 : λ3 : µ3], [1 : λ4 : µ4]. C     ∗ ∗    ,     1    ,     1    . Sec3(C) = 1P1 ⊔ 2P0. nilpotents     η1 λ1η1 + η2 µ1η1 + η2 η2 λ1η2 µ1η2 η3 λ3η3 µ3η3 η4 λ4η4 µ4η4     Ξ [1 : λ1 : µ1], [1 : λ1 : µ1], [1 : λ3 : µ3], [1 : λ4 : µ4]. C     1    ,     1    ,     1    . Sec3(C) = 1P0.

These systems are easier to distinguish with C than with Ξ.

A.Smith (Fordham) EDS 2013-12-09 6 / 13

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SLIDE 25

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1).

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 26

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 27

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 28

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 29

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), defined by some ideal. . . A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 30

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), defined by some ideal. . . 2 Also, as usual, M (2) ⊂ Grn(T M (1)) defined by I(1). A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 31

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), defined by some ideal. . . 2 Also, as usual, M (2) ⊂ Grn(T M (1)) defined by I(1). 3 So, there is an ideal on M (1) whose variety is Secn(C) ∩ M (2).

(how to compute it?)

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 32

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), defined by some ideal. . . 2 Also, as usual, M (2) ⊂ Grn(T M (1)) defined by I(1). 3 So, there is an ideal on M (1) whose variety is Secn(C) ∩ M (2).

(how to compute it?) Prolong once and use Terracini’s Lemma: If E = l1 + l2 + · · · + ln ∈ Secn(C), then TE Secn(C) =

  • i

Tli C Ann(TE Secn(C)) =

  • i

Ann Tli C ⊂ T∗

E M (2)

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 33

Characteristic and Rank-One Variety

The Secants of the Rank-One Cone

Fix e ∈ M (1). Ξe ⊂ e∗ ∼ = V ∗, defined by characteristic ideal Ce ⊂ Ze, defined by 2 × 2 minors on τ(Ze) ⊂ W ⊗ V ∗.

1 Note that Secn(Ce) ⊂ Grn(Ze) = Grn(Te M (1)), defined by some ideal. . . 2 Also, as usual, M (2) ⊂ Grn(T M (1)) defined by I(1). 3 So, there is an ideal on M (1) whose variety is Secn(C) ∩ M (2).

(how to compute it?) Prolong once and use Terracini’s Lemma: If E = l1 + l2 + · · · + ln ∈ Secn(C), then TE Secn(C) =

  • i

Tli C Ann(TE Secn(C)) =

  • i

Ann Tli C ⊂ T∗

E M (2)

Call it A(I).

A.Smith (Fordham) EDS 2013-12-09 7 / 13

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SLIDE 34

Characteristic and Rank-One Variety

I → I(1) → A(I). What does this give?

A.Smith (Fordham) EDS 2013-12-09 8 / 13

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SLIDE 35

Characteristic and Rank-One Variety

I → I(1) → A(I). What does this give?

I I(1) A(I) A(I)(1) A(A(I)) A2(I)(1) A3(I) Ak−1(I)(1) Ak(I) (Where) Does this end?

A.Smith (Fordham) EDS 2013-12-09 8 / 13

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SLIDE 36

Hydrodynamic Integrability

Wanted: A general notion of integrability.

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 37

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 38

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 39

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 40

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 41

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 42

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats.

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 43

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats. Additionally, the following properties would be convenient:

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 44

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats. Additionally, the following properties would be convenient:

1 the notion should be testable in real-world examples; A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 45

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats. Additionally, the following properties would be convenient:

1 the notion should be testable in real-world examples; 2 the notion should provide a means of constructing actual solutions; and A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 46

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats. Additionally, the following properties would be convenient:

1 the notion should be testable in real-world examples; 2 the notion should provide a means of constructing actual solutions; and 3 the notion should provide a means for constructing Lax pairs, τ functions, or loop group

formulations when those theories also apply.

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 47

Hydrodynamic Integrability

Wanted: A general notion of integrability. To me, this means:

1 for PDEs already seen in the literature, the notion must reproduce the observed geometry; 2 the notion must be applicable to all PDEs of all orders & dimensions (perhaps trivially so); 3 the notion must extend naturally to generic EDS or D-modules (or provide obvious

  • bstructions to such an extension);

4 the notion must be contact invariant; 5 the notion must be preserved under prolongation; and 6 the notion should be equally applicable in the real or complex cases, with the usual

algebraic caveats. Additionally, the following properties would be convenient:

1 the notion should be testable in real-world examples; 2 the notion should provide a means of constructing actual solutions; and 3 the notion should provide a means for constructing Lax pairs, τ functions, or loop group

formulations when those theories also apply. That is, integrable systems should be viewed as a subvariety of involutive/regular systems. What is their defining ideal?

A.Smith (Fordham) EDS 2013-12-09 9 / 13

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SLIDE 48

Hydrodynamic Integrability Semi-Hamiltonian Systems as PDEs

Consider this 1st-order system of PDE on functions (X n, xi) → (Y r, ya): ∂ya ∂xi = Fa

i (y)∂ya

∂x1 (no sum!)

A.Smith (Fordham) EDS 2013-12-09 10 / 13

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SLIDE 49

Hydrodynamic Integrability Semi-Hamiltonian Systems as PDEs

Consider this 1st-order system of PDE on functions (X n, xi) → (Y r, ya): ∂ya ∂xi = Fa

i (y)∂ya

∂x1 (no sum!) with a compatibility condition on Fa

i,b = ∂Fa

i

∂yb :

Fa

i,b

Fa

i − Fb i

= Fa

j,b

Fa

j − Fb j

A.Smith (Fordham) EDS 2013-12-09 10 / 13

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SLIDE 50

Hydrodynamic Integrability Semi-Hamiltonian Systems as PDEs

Consider this 1st-order system of PDE on functions (X n, xi) → (Y r, ya): ∂ya ∂xi = Fa

i (y)∂ya

∂x1 (no sum!) with a compatibility condition on Fa

i,b = ∂Fa

i

∂yb :

Fa

i,b

Fa

i − Fb i

= Fa

j,b

Fa

j − Fb j

This system is called a semi-Hamiltonian or rich system of conservation laws (Tsar¨ ev and D.Serre). They: are uninteresting in r ≤ 2. describe systems of commuting wavefronts admit C ∞ solutions using the generalized hodograph method are characterized as orthogonal coordinate webs (Darboux, Tsar¨ ev) (more on this later) appear in the linearizations of many “integrable” PDEs (more on this later)

A.Smith (Fordham) EDS 2013-12-09 10 / 13

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SLIDE 51

Hydrodynamic Integrability Semi-Hamiltonian Systems as EDS

Let ha = ∂ya

∂x1 = 0, with (ha) valued in some space H. Consider the EDS on

M = X × (Y × H) generated by {θa} =

  • dya − haFa

i (y) dxi

and

A.Smith (Fordham) EDS 2013-12-09 11 / 13

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SLIDE 52

Hydrodynamic Integrability Semi-Hamiltonian Systems as EDS

Let ha = ∂ya

∂x1 = 0, with (ha) valued in some space H. Consider the EDS on

M = X × (Y × H) generated by {θa} =

  • dya − haFa

i (y) dxi

and d

     

θ1 θ2 . . . θr

     

≡ −

     

dh1 F1

2 dh1

F1

3 dh1

· · · F1

ndh1

dh2 F2

2 dh2

F2

3 dh2

· · · F2

ndh2

. . . . . . . . . ... . . . dhr Fr

2 dh2

Fr

3 dhr

· · · Fr

ndhr

     

     

dx1 dx2 . . . dxn

     

+ (hF′hFdx) ∧ dx

A.Smith (Fordham) EDS 2013-12-09 11 / 13

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SLIDE 53

Hydrodynamic Integrability Semi-Hamiltonian Systems as EDS

Let ha = ∂ya

∂x1 = 0, with (ha) valued in some space H. Consider the EDS on

M = X × (Y × H) generated by {θa} =

  • dya − haFa

i (y) dxi

and d

     

θ1 θ2 . . . θr

     

≡ −

     

dh1 F1

2 dh1

F1

3 dh1

· · · F1

ndh1

dh2 F2

2 dh2

F2

3 dh2

· · · F2

ndh2

. . . . . . . . . ... . . . dhr Fr

2 dh2

Fr

3 dhr

· · · Fr

ndhr

     

     

dx1 dx2 . . . dxn

     

+ (hF′hFdx) ∧ dx

1 The torsion-free condition δ(hF′hF) = 0 and the involutivity conditions of F imply the

semi-Hamiltonian compatibility condition.

A.Smith (Fordham) EDS 2013-12-09 11 / 13

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SLIDE 54

Hydrodynamic Integrability Semi-Hamiltonian Systems as EDS

Let ha = ∂ya

∂x1 = 0, with (ha) valued in some space H. Consider the EDS on

M = X × (Y × H) generated by {θa} =

  • dya − haFa

i (y) dxi

and d

     

θ1 θ2 . . . θr

     

≡ −

     

dh1 F1

2 dh1

F1

3 dh1

· · · F1

ndh1

dh2 F2

2 dh2

F2

3 dh2

· · · F2

ndh2

. . . . . . . . . ... . . . dhr Fr

2 dh2

Fr

3 dhr

· · · Fr

ndhr

     

     

dx1 dx2 . . . dxn

     

+ (hF′hFdx) ∧ dx

1 The torsion-free condition δ(hF′hF) = 0 and the involutivity conditions of F imply the

semi-Hamiltonian compatibility condition.

2 The tableau is involutive with s1 = n. Cartan–K¨

ahler–Yang Hyperbolic EDS theorem promises C ∞ solutions over R. Ξ is r real, distinct points. C is r real, distinct points.

A.Smith (Fordham) EDS 2013-12-09 11 / 13

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SLIDE 55

Hydrodynamic Integrability Semi-Hamiltonian Systems as EDS

Let ha = ∂ya

∂x1 = 0, with (ha) valued in some space H. Consider the EDS on

M = X × (Y × H) generated by {θa} =

  • dya − haFa

i (y) dxi

and d

     

θ1 θ2 . . . θr

     

≡ −

     

dh1 F1

2 dh1

F1

3 dh1

· · · F1

ndh1

dh2 F2

2 dh2

F2

3 dh2

· · · F2

ndh2

. . . . . . . . . ... . . . dhr Fr

2 dh2

Fr

3 dhr

· · · Fr

ndhr

     

     

dx1 dx2 . . . dxn

     

+ (hF′hFdx) ∧ dx

1 The torsion-free condition δ(hF′hF) = 0 and the involutivity conditions of F imply the

semi-Hamiltonian compatibility condition.

2 The tableau is involutive with s1 = n. Cartan–K¨

ahler–Yang Hyperbolic EDS theorem promises C ∞ solutions over R. Ξ is r real, distinct points. C is r real, distinct points.

3 Best of all possible s1 involutive systems. Every localization of A(I) is Frobenius,

maximal.

A.Smith (Fordham) EDS 2013-12-09 11 / 13

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SLIDE 56

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE?

A.Smith (Fordham) EDS 2013-12-09 12 / 13

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SLIDE 57

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE? “yes, in many ways” = ⇒ “PDE is hydrodynamically integrable.” (see Ferapontov, et al for examples. good collection in 1208.2728 by F and Kruglikov)

A.Smith (Fordham) EDS 2013-12-09 12 / 13

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SLIDE 58

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE? “yes, in many ways” = ⇒ “PDE is hydrodynamically integrable.” (see Ferapontov, et al for examples. good collection in 1208.2728 by F and Kruglikov) X = Rn Y = Rr M ⊂ Jp(Rn, Rq) π

semi-Ham

µ with µ(Y ) integral to M and n ≥ 3.

A.Smith (Fordham) EDS 2013-12-09 12 / 13

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SLIDE 59

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE? “yes, in many ways” = ⇒ “PDE is hydrodynamically integrable.” (see Ferapontov, et al for examples. good collection in 1208.2728 by F and Kruglikov) X = Rn Y = Rr M ⊂ Jp(Rn, Rq) π

semi-Ham

µ with µ(Y ) integral to M and n ≥ 3. Key property involves rank-one fibers: µ∗

∂ya

  • =
  • ∂xi

∂ya , ∂u ∂ya , ∂p1 ∂ya Fa

i , ∂p11

∂ya Fa

i Fa j , ∂p111

∂ya Fa

i Fa j Fa k , . . .

  • A.Smith (Fordham)

EDS 2013-12-09 12 / 13

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SLIDE 60

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE? “yes, in many ways” = ⇒ “PDE is hydrodynamically integrable.” (see Ferapontov, et al for examples. good collection in 1208.2728 by F and Kruglikov) X = Rn Y = Rr M ⊂ Jp(Rn, Rq) π

semi-Ham

µ with µ(Y ) integral to M and n ≥ 3. Key property involves rank-one fibers: µ∗

∂ya

  • =
  • ∂xi

∂ya , ∂u ∂ya , ∂p1 ∂ya Fa

i , ∂p11

∂ya Fa

i Fa j , ∂p111

∂ya Fa

i Fa j Fa k , . . .

  • Depending on the type of PDE M ⊂ Jp(Rn, Rq), these yield many interesting geometries on

M: SL(n), GL(2), CO(n), CSpin(n−1, 1), Einstein–Weyl, etc.

A.Smith (Fordham) EDS 2013-12-09 12 / 13

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SLIDE 61

Hydrodynamic Integrability Hydrodynamic Integrability

Can we embed semi-Hamiltonian systems within a more general PDE? “yes, in many ways” = ⇒ “PDE is hydrodynamically integrable.” (see Ferapontov, et al for examples. good collection in 1208.2728 by F and Kruglikov) X = Rn Y = Rr M ⊂ Jp(Rn, Rq) π

semi-Ham

µ with µ(Y ) integral to M and n ≥ 3. Key property involves rank-one fibers: µ∗

∂ya

  • =
  • ∂xi

∂ya , ∂u ∂ya , ∂p1 ∂ya Fa

i , ∂p11

∂ya Fa

i Fa j , ∂p111

∂ya Fa

i Fa j Fa k , . . .

  • Depending on the type of PDE M ⊂ Jp(Rn, Rq), these yield many interesting geometries on

M: SL(n), GL(2), CO(n), CSpin(n−1, 1), Einstein–Weyl, etc. But can we characterize as EDS with no other restrictions?

A.Smith (Fordham) EDS 2013-12-09 12 / 13

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SLIDE 62

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 63

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 64

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] 3 I is hydro int if and only if A(I) is semi-Hamiltonian [** in known subcases]. A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 65

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] 3 I is hydro int if and only if A(I) is semi-Hamiltonian [** in known subcases]. A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 66

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] 3 I is hydro int if and only if A(I) is semi-Hamiltonian [** in known subcases].

Therefore, the condition “Ak(I) =Frobenius for some k” appears to be a generalization of hydrodynamic integrability that is manifestly invariant.

A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 67

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] 3 I is hydro int if and only if A(I) is semi-Hamiltonian [** in known subcases].

Therefore, the condition “Ak(I) =Frobenius for some k” appears to be a generalization of hydrodynamic integrability that is manifestly invariant. Dear experts: Has this condition been used or named before?

A.Smith (Fordham) EDS 2013-12-09 13 / 13

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SLIDE 68

Hydrodynamic Integrability A new (I think) definition

Proposition Suppose that I is a PDE-type involutive EDS with no Cauchy characteristics or unabsorbable

  • torsion. Then

1 I is Frobenius (over C) if and only if A(I) is always empty. [trivial to prove.] 2 I is semi-Hamiltonian if and only if A(I) is Frobenius [see Cartan’s abstract.] 3 I is hydro int if and only if A(I) is semi-Hamiltonian [** in known subcases].

Therefore, the condition “Ak(I) =Frobenius for some k” appears to be a generalization of hydrodynamic integrability that is manifestly invariant. Dear experts: Has this condition been used or named before? Reminder of the motivation from Lie algebras: Lie algebras: trivial abelian solvable semi-simple D(g) = 0 Dk(g) = 0 D∞(g) = 0 (But, nothing known about truthfulness of this analogy.)

A.Smith (Fordham) EDS 2013-12-09 13 / 13