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Diffiety

In mathematics, a diffiety (/dəˈfəˌt/) is a geometrical object which plays the same role in the modern theory of partial differential equations that algebraic varieties play for algebraic equations, that is, to encode the space of solutions in a more conceptual way. The term was coined in 1984 by Alexandre Mikhailovich Vinogradov as portmanteau from differential variety.[1]

Intuitive definition edit

In algebraic geometry the main objects of study (varieties) model the space of solutions of a system of algebraic equations (i.e. the zero locus of a set of polynomials), together with all their "algebraic consequences". This means that, applying algebraic operations to this set (e.g. adding those polynomials to each other or multiplying them with any other polynomials) will give rise to the same zero locus. In other words, one can actually consider the zero locus of the algebraic ideal generated by the initial set of polynomials.

When dealing with differential equations, apart from applying algebraic operations as above, one has also the option to differentiate the starting equations, obtaining new differential constraints. Therefore, the differential analogue of a variety should be the space of solutions of a system of differential equations, together with all their "differential consequences". Instead of considering the zero locus of an algebraic ideal, one needs therefore to work with a differential ideal.

An elementary diffiety will consist therefore of the infinite prolongation  of a differential equation  , together with an extra structure provided by a special distribution. Elementary diffieties play the same role in the theory of differential equations as affine algebraic varieties do in the theory of algebraic equations. Accordingly, just like varieties or schemes are composed of irreducible affine varieties or affine schemes, one defines a (non-elementary) diffiety as an object that locally looks like an elementary diffiety.

Formal definition edit

The formal definition of a diffiety, which relies on the geometric approach to differential equations and their solutions, requires the notions of jets of submanifolds, prolongations, and Cartan distribution, which are recalled below.

Jet spaces of submanifolds edit

Let   be an  -dimensional smooth manifold. Two  -dimensional submanifolds  ,   of   are tangent up to order   at the point   if one can locally describe both submanifolds as zeroes of functions defined in a neighbourhood of  , whose derivatives at   agree up to order  .

One can show that being tangent up to order   is a coordinate-invariant notion and an equivalence relation.[2] One says also that   and   have same  -th order jet at  , and denotes their equivalence class by   or  .

The  -jet space of  -submanifolds of  , denoted by  , is defined as the set of all  -jets of  -dimensional submanifolds of   at all points of  :

 
As any given jet   is locally determined by the derivatives up to order   of the functions describing   around  , one can use such functions to build local coordinates   and provide   with a natural structure of smooth manifold.[2]

 
  and   have the same 1-jet at   while   and   have the same 3-jet.

For instance, for   one recovers just points in   and for   one recovers the Grassmannian of  -dimensional subspaces of  . More generally, all the projections   are fibre bundles.

As a particular case, when   has a structure of fibred manifold over an  -dimensional manifold  , one can consider submanifolds of   given by the graphs of local sections of  . Then the notion of jet of submanifolds boils down to the standard notion of jet of sections, and the jet bundle   turns out to be an open and dense subset of  .[3]

Prolongations of submanifolds edit

The  -jet prolongation of a submanifold   is

 

The map   is a smooth embedding and its image  , called the prolongation of the submanifold  , is a submanifold of   diffeomorphic to  .

Cartan distribution on jet spaces edit

A space of the form  , where   is any submanifold of   whose prolongation contains the point  , is called an  -plane (or jet plane, or Cartan plane) at  . The Cartan distribution on the jet space   is the distribution   defined by

 
where   is the span of all  -planes at  .[4]

Differential equations edit

A differential equation of order   on the manifold   is a submanifold  ; a solution is defined to be an  -dimensional submanifold   such that  . When   is a fibred manifold over  , one recovers the notion of partial differential equations on jet bundles and their solutions, which provide a coordinate-free way to describe the analogous notions of mathematical analysis. While jet bundles are enough to deal with many equations arising in geometry, jet spaces of submanifolds provide a greater generality, used to tackle several PDEs imposed on submanifolds of a given manifold, such as Lagrangian submanifolds and minimal surfaces.

As in the jet bundle case, the Cartan distribution is important in the algebro-geometric approach to differential equations because it allows to encode solutions in purely geometric terms. Indeed, a submanifold   is a solution if and only if it is an integral manifold for  , i.e.   for all  .

One can also look at the Cartan distribution of a PDE   more intrinsically, defining

 
In this sense, the pair   encodes the information about the solutions of the differential equation  .

Prolongations of PDEs edit

Given a differential equation   of order  , its  -th prolongation is defined as

 
where both   and   are viewed as embedded submanifolds of  , so that their intersection is well-defined. However, such an intersection is not necessarily a manifold again, hence   may not be an equation of order  . One therefore usually requires   to be "nice enough" such that at least its first prolongation is indeed a submanifold of  .

Below we will assume that the PDE is formally integrable, i.e. all prolongations   are smooth manifolds and all projections   are smooth surjective submersions. Note that a suitable version of Cartan–Kuranishi prolongation theorem guarantees that, under minor regularity assumptions, checking the smoothness of a finite number of prolongations is enough. Then the inverse limit of the sequence   extends the definition of prolongation to the case when   goes to infinity, and the space   has the structure of a profinite-dimensional manifold.[5]

Definition of a diffiety edit

An elementary diffiety is a pair   where   is a  -th order differential equation on some manifold,   its infinite prolongation and   its Cartan distribution. Note that, unlike in the finite case, one can show that the Cartan distribution   is  -dimensional and involutive. However, due to the infinite-dimensionality of the ambient manifold, the Frobenius theorem does not hold, therefore   is not integrable

A diffiety is a triple  , consisting of

  • a (generally infinite-dimensional) manifold  
  • the algebra of its smooth functions  
  • a finite-dimensional distribution  ,

such that   is locally of the form  , where   is an elementary diffiety and   denotes the algebra of smooth functions on  . Here locally means a suitable localisation with respect to the Zariski topology corresponding to the algebra  .

The dimension of   is called dimension of the diffiety and its denoted by  , with a capital D (to distinguish it from the dimension of   as a manifold).

Morphisms of diffieties edit

A morphism between two diffieties   and   consists of a smooth map   whose pushforward preserves the Cartan distribution, i.e. such that, for every point  , one has  .

Diffieties together with their morphisms define the category of differential equations.[3]

Applications edit

Vinogradov sequence edit

The Vinogradov  -spectral sequence (or, for short, Vinogradov sequence) is a spectral sequence associated to a diffiety, which can be used to investigate certain properties of the formal solution space of a differential equation by exploiting its Cartan distribution  .[6]

Given a diffiety  , consider the algebra of differential forms over  

 

and the corresponding de Rham complex:

 

Its cohomology groups   contain some structural information about the PDE; however, due to the Poincaré Lemma, they all vanish locally. In order to extract much more and even local information, one thus needs to take the Cartan distribution into account and introduce a more sophisticated sequence. To this end, let

 

be the submodule of differential forms over   whose restriction to the distribution   vanishes, i.e.

 

Note that   is actually a differential ideal since it is stable w.r.t. to the de Rham differential, i.e.  .

Now let   be its  -th power, i.e. the linear subspace of   generated by  . Then one obtains a filtration

 

and since all ideals   are stable, this filtration completely determines the following spectral sequence:

 

The filtration above is finite in each degree, i.e. for every  

 

so that the spectral sequence converges to the de Rham cohomology   of the diffiety. One can therefore analyse the terms of the spectral sequence order by order to recover information on the original PDE. For instance:[7]

  •   corresponds to action functionals constrained by the PDE  . In particular, for  , the corresponding Euler-Lagrange equation is  .
  •   corresponds to conservation laws for solutions of  .
  •   is interpreted as characteristic classes of bordisms of solutions of  .

Many higher-order terms do not have an interpretation yet.

Variational bicomplex edit

As a particular case, starting with a fibred manifold   and its jet bundle   instead of the jet space  , instead of the  -spectral sequence one obtains the slightly less general variational bicomplex. More precisely, any bicomplex determines two spectral sequences: one of the two spectral sequences determined by the variational bicomplex is exactly the Vinogradov  -spectral sequence. However, the variational bicomplex was developed independently from the Vinogradov sequence.[8][9]

Similarly to the terms of the spectral sequence, many terms of the variational bicomplex can be given a physical interpretation in classical field theory: for example, one obtains cohomology classes corresponding to action functionals, conserved currents, gauge charges, etc.[10]

Secondary calculus edit

Vinogradov developed a theory, known as secondary calculus, to formalise in cohomological terms the idea of a differential calculus on the space of solutions of a given system of PDEs (i.e. the space of integral manifolds of a given diffiety).[11][12][13][3]

In other words, secondary calculus provides substitutes for functions, vector fields, differential forms, differential operators, etc., on a (generically) very singular space where these objects cannot be defined in the usual (smooth) way on the space of solution. Furthermore, the space of these new objects are naturally endowed with the same algebraic structures of the space of the original objects.[14]

More precisely, consider the horizontal De Rham complex   of a diffiety, which can be seen as the leafwise de Rham complex of the involutive distribution  or, equivalently, the Lie algebroid complex of the Lie algebroid  . Then the complex   becomes naturally a commutative DG algebra together with a suitable differential  . Then, possibly tensoring with the normal bundle  , its cohomology is used to define the following "secondary objects":

  • secondary functions are elements of the cohomology  , which is naturally a commutative DG algebra (it is actually the first page of the  -spectral sequence discussed above);
  • secondary vector fields are elements of the cohomology  , which is naturally a Lie algebra; moreover, it forms a graded Lie-Rinehart algebra together with  ;
  • secondary differential  -forms are elements of the cohomology  , which is naturally a commutative DG algebra.

Secondary calculus can also be related to the covariant Phase Space, i.e. the solution space of the Euler-Lagrange equations associated to a Lagrangian field theory.[15]

See also edit

Another way of generalizing ideas from algebraic geometry is differential algebraic geometry.

References edit

  1. ^ Vinogradov, A. M. (March 1984). "Local symmetries and conservation laws". Acta Applicandae Mathematicae. 2 (1): 21–78. doi:10.1007/BF01405491. ISSN 0167-8019. S2CID 121860845.
  2. ^ a b Saunders, D. J. (1989). The Geometry of Jet Bundles. London Mathematical Society Lecture Note Series. Cambridge: Cambridge University Press. doi:10.1017/cbo9780511526411. ISBN 978-0-521-36948-0.
  3. ^ a b c Vinogradov, A. M. (2001). Cohomological analysis of partial differential equations and secondary calculus. Providence, R.I.: American Mathematical Society. ISBN 0-8218-2922-X. OCLC 47296188.
  4. ^ Krasil'shchik, I. S.; Lychagin, V. V.; Vinogradov, A. M. (1986). Geometry of jet spaces and nonlinear partial differential equations. Adv. Stud. Contemp. Math., N. Y. Vol. 1. New York etc.: Gordon and Breach Science Publishers. ISBN 978-2-88124-051-5.
  5. ^ Güneysu, Batu; Pflaum, Markus J. (2017-01-10). "The Profinite Dimensional Manifold Structure of Formal Solution Spaces of Formally Integrable PDEs". SIGMA. Symmetry, Integrability and Geometry: Methods and Applications. 13: 003. arXiv:1308.1005. Bibcode:2017SIGMA..13..003G. doi:10.3842/SIGMA.2017.003. S2CID 15871902.
  6. ^ Vinogradov, A. M. (1978). "A spectral sequence associated with a nonlinear differential equation and algebro-geometric foundations of Lagrangian field theory with constraints". Soviet Math. Dokl. (in Russian). 19: 144–148 – via Math-Net.Ru.
  7. ^ Symmetries and conservation laws for differential equations of mathematical physics. A. V. Bocharov, I. S. Krasilʹshchik, A. M. Vinogradov. Providence, R.I.: American Mathematical Society. 1999. ISBN 978-1-4704-4596-6. OCLC 1031947580.{{cite book}}: CS1 maint: others (link)
  8. ^ Tulczyjew, W. M. (1980). García, P. L.; Pérez-Rendón, A.; Souriau, J. M. (eds.). "The Euler-Lagrange resolution". Differential Geometrical Methods in Mathematical Physics. Lecture Notes in Mathematics. 836. Berlin, Heidelberg: Springer: 22–48. doi:10.1007/BFb0089725. ISBN 978-3-540-38405-2.
  9. ^ Tsujishita, Toru (1982). "On variation bicomplexes associated to differential equations". Osaka Journal of Mathematics. 19 (2): 311–363. ISSN 0030-6126.
  10. ^ "variational bicomplex in nLab". ncatlab.org. Retrieved 2021-12-11.
  11. ^ Vinogradov, A.M. (1984-04-30). "The b-spectral sequence, Lagrangian formalism, and conservation laws. I. The linear theory". Journal of Mathematical Analysis and Applications. 100 (1): 1–40. doi:10.1016/0022-247X(84)90071-4.
  12. ^ Vinogradov, A. M. (1984-04-30). "The b-spectral sequence, Lagrangian formalism, and conservation laws. II. The nonlinear theory". Journal of Mathematical Analysis and Applications. 100 (1): 41–129. doi:10.1016/0022-247X(84)90072-6. ISSN 0022-247X.
  13. ^ Henneaux, Marc; Krasil′shchik, Joseph; Vinogradov, Alexandre, eds. (1998). Secondary Calculus and Cohomological Physics. Contemporary Mathematics. Vol. 219. Providence, Rhode Island: American Mathematical Society. doi:10.1090/conm/219. ISBN 978-0-8218-0828-3.
  14. ^ Vitagliano, Luca (2014). "On the strong homotopy Lie–Rinehart algebra of a foliation". Communications in Contemporary Mathematics. 16 (6): 1450007. arXiv:1204.2467. doi:10.1142/S0219199714500072. ISSN 0219-1997. S2CID 119704524.
  15. ^ Vitagliano, Luca (2009-04-01). "Secondary calculus and the covariant phase space". Journal of Geometry and Physics. 59 (4): 426–447. arXiv:0809.4164. Bibcode:2009JGP....59..426V. doi:10.1016/j.geomphys.2008.12.001. ISSN 0393-0440. S2CID 21787052.

External links edit

  • (frozen since 2010)
  • The Levi-Civita Institute (successor of above site)
  • Geometry of Differential Equations
  • Differential Geometry and PDEs

diffiety, confused, with, diffeology, mathematics, diffiety, geometrical, object, which, plays, same, role, modern, theory, partial, differential, equations, that, algebraic, varieties, play, algebraic, equations, that, encode, space, solutions, more, conceptu. Not to be confused with Diffeology In mathematics a diffiety d e ˈ f aɪ e ˌ t iː is a geometrical object which plays the same role in the modern theory of partial differential equations that algebraic varieties play for algebraic equations that is to encode the space of solutions in a more conceptual way The term was coined in 1984 by Alexandre Mikhailovich Vinogradov as portmanteau from differential variety 1 Contents 1 Intuitive definition 2 Formal definition 2 1 Jet spaces of submanifolds 2 2 Prolongations of submanifolds 2 3 Cartan distribution on jet spaces 2 4 Differential equations 2 5 Prolongations of PDEs 2 6 Definition of a diffiety 2 7 Morphisms of diffieties 3 Applications 3 1 Vinogradov sequence 3 1 1 Variational bicomplex 3 2 Secondary calculus 4 See also 5 References 6 External linksIntuitive definition editIn algebraic geometry the main objects of study varieties model the space of solutions of a system of algebraic equations i e the zero locus of a set of polynomials together with all their algebraic consequences This means that applying algebraic operations to this set e g adding those polynomials to each other or multiplying them with any other polynomials will give rise to the same zero locus In other words one can actually consider the zero locus of the algebraic ideal generated by the initial set of polynomials When dealing with differential equations apart from applying algebraic operations as above one has also the option to differentiate the starting equations obtaining new differential constraints Therefore the differential analogue of a variety should be the space of solutions of a system of differential equations together with all their differential consequences Instead of considering the zero locus of an algebraic ideal one needs therefore to work with a differential ideal An elementary diffiety will consist therefore of the infinite prolongation E displaystyle mathcal E infty nbsp of a differential equation E J k E m displaystyle mathcal E subset J k E m nbsp together with an extra structure provided by a special distribution Elementary diffieties play the same role in the theory of differential equations as affine algebraic varieties do in the theory of algebraic equations Accordingly just like varieties or schemes are composed of irreducible affine varieties or affine schemes one defines a non elementary diffiety as an object that locally looks like an elementary diffiety Formal definition editThe formal definition of a diffiety which relies on the geometric approach to differential equations and their solutions requires the notions of jets of submanifolds prolongations and Cartan distribution which are recalled below Jet spaces of submanifolds edit Let E displaystyle E nbsp be an m e displaystyle m e nbsp dimensional smooth manifold Two m displaystyle m nbsp dimensional submanifolds M displaystyle M nbsp M displaystyle M nbsp of E displaystyle E nbsp are tangent up to order k displaystyle k nbsp at the point p M M E displaystyle p in M cap M subset E nbsp if one can locally describe both submanifolds as zeroes of functions defined in a neighbourhood of p displaystyle p nbsp whose derivatives at p displaystyle p nbsp agree up to order k displaystyle k nbsp One can show that being tangent up to order k displaystyle k nbsp is a coordinate invariant notion and an equivalence relation 2 One says also that M displaystyle M nbsp and M displaystyle M nbsp have same k displaystyle k nbsp th order jet at p displaystyle p nbsp and denotes their equivalence class by M p k displaystyle M p k nbsp or j p k M displaystyle j p k M nbsp The k displaystyle k nbsp jet space of k displaystyle k nbsp submanifolds of E displaystyle E nbsp denoted by J k E m displaystyle J k E m nbsp is defined as the set of all k displaystyle k nbsp jets of m displaystyle m nbsp dimensional submanifolds of E displaystyle E nbsp at all points of E displaystyle E nbsp J k E m M p k p M dim M m M E submanifold displaystyle J k E m M p k p in M text dim M m M subset E text submanifold nbsp As any given jet M p k displaystyle M p k nbsp is locally determined by the derivatives up to order k displaystyle k nbsp of the functions describing M displaystyle M nbsp around p displaystyle p nbsp one can use such functions to build local coordinates x i u s j displaystyle x i u sigma j nbsp and provide J k E m displaystyle J k E m nbsp with a natural structure of smooth manifold 2 nbsp M displaystyle M nbsp and M displaystyle M nbsp have the same 1 jet at p E displaystyle p in E nbsp while M displaystyle M nbsp and M displaystyle M nbsp have the same 3 jet For instance for k 1 displaystyle k 1 nbsp one recovers just points in E displaystyle E nbsp and for k 1 displaystyle k 1 nbsp one recovers the Grassmannian of n displaystyle n nbsp dimensional subspaces of T E displaystyle TE nbsp More generally all the projections J k E J k 1 E displaystyle J k E to J k 1 E nbsp are fibre bundles As a particular case when E displaystyle E nbsp has a structure of fibred manifold over an n displaystyle n nbsp dimensional manifold X displaystyle X nbsp one can consider submanifolds of E displaystyle E nbsp given by the graphs of local sections of p E X displaystyle pi E to X nbsp Then the notion of jet of submanifolds boils down to the standard notion of jet of sections and the jet bundle J k p displaystyle J k pi nbsp turns out to be an open and dense subset of J k E m displaystyle J k E m nbsp 3 Prolongations of submanifolds edit The k displaystyle k nbsp jet prolongation of a submanifold M E displaystyle M subseteq E nbsp isj k M M J k E m p M p k displaystyle j k M M rightarrow J k E m quad p mapsto M p k nbsp The map j k M displaystyle j k M nbsp is a smooth embedding and its image M k im j k M displaystyle M k text im j k M nbsp called the prolongation of the submanifold M displaystyle M nbsp is a submanifold of J k E m displaystyle J k E m nbsp diffeomorphic to M displaystyle M nbsp Cartan distribution on jet spaces edit A space of the form T 8 M k displaystyle T theta M k nbsp where M displaystyle M nbsp is any submanifold of E displaystyle E nbsp whose prolongation contains the point 8 J k E m displaystyle theta in J k E m nbsp is called an R displaystyle R nbsp plane or jet plane or Cartan plane at 8 displaystyle theta nbsp The Cartan distribution on the jet space J k E m displaystyle J k E m nbsp is the distribution C T J k E m displaystyle mathcal C subseteq T J k E m nbsp defined byC J k E m T J k E m 8 C 8 T 8 J k E m displaystyle mathcal C J k E m rightarrow TJ k E m qquad theta mapsto mathcal C theta subset T theta J k E m nbsp where C 8 displaystyle mathcal C theta nbsp is the span of all R displaystyle R nbsp planes at 8 J k E m displaystyle theta in J k E m nbsp 4 Differential equations edit A differential equation of order k displaystyle k nbsp on the manifold E displaystyle E nbsp is a submanifold E J k E m displaystyle mathcal E subset J k E m nbsp a solution is defined to be an m displaystyle m nbsp dimensional submanifold S E displaystyle S subset mathcal E nbsp such that S k E displaystyle S k subseteq mathcal E nbsp When E displaystyle E nbsp is a fibred manifold over X displaystyle X nbsp one recovers the notion of partial differential equations on jet bundles and their solutions which provide a coordinate free way to describe the analogous notions of mathematical analysis While jet bundles are enough to deal with many equations arising in geometry jet spaces of submanifolds provide a greater generality used to tackle several PDEs imposed on submanifolds of a given manifold such as Lagrangian submanifolds and minimal surfaces As in the jet bundle case the Cartan distribution is important in the algebro geometric approach to differential equations because it allows to encode solutions in purely geometric terms Indeed a submanifold S E displaystyle S subset mathcal E nbsp is a solution if and only if it is an integral manifold for C displaystyle mathcal C nbsp i e T 8 S C 8 displaystyle T theta S subset mathcal C theta nbsp for all 8 S displaystyle theta in S nbsp One can also look at the Cartan distribution of a PDE E J k E m displaystyle mathcal E subset J k E m nbsp more intrinsically definingC E C 8 T 8 E 8 E displaystyle mathcal C mathcal E mathcal C theta cap T theta mathcal E theta in mathcal E nbsp In this sense the pair E C E displaystyle mathcal E mathcal C mathcal E nbsp encodes the information about the solutions of the differential equation E displaystyle mathcal E nbsp Prolongations of PDEs edit Given a differential equation E J l E m displaystyle mathcal E subset J l E m nbsp of order l displaystyle l nbsp its k displaystyle k nbsp th prolongation is defined asE k J k E m J k l E m J k l E m displaystyle mathcal E k J k mathcal E m cap J k l E m subseteq J k l E m nbsp where both J k E m displaystyle J k mathcal E m nbsp and J k l E m displaystyle J k l E m nbsp are viewed as embedded submanifolds of J k J l E m m displaystyle J k J l E m m nbsp so that their intersection is well defined However such an intersection is not necessarily a manifold again hence E k displaystyle mathcal E k nbsp may not be an equation of order k l displaystyle k l nbsp One therefore usually requires E displaystyle mathcal E nbsp to be nice enough such that at least its first prolongation is indeed a submanifold of J k 1 E m displaystyle J k 1 E m nbsp Below we will assume that the PDE is formally integrable i e all prolongations E k displaystyle mathcal E k nbsp are smooth manifolds and all projections E k E k 1 displaystyle mathcal E k to mathcal E k 1 nbsp are smooth surjective submersions Note that a suitable version of Cartan Kuranishi prolongation theorem guarantees that under minor regularity assumptions checking the smoothness of a finite number of prolongations is enough Then the inverse limit of the sequence E k k N displaystyle mathcal E k k in mathbb N nbsp extends the definition of prolongation to the case when k displaystyle k nbsp goes to infinity and the space E displaystyle mathcal E infty nbsp has the structure of a profinite dimensional manifold 5 Definition of a diffiety edit An elementary diffiety is a pair E C E displaystyle mathcal E infty mathcal C mathcal E infty nbsp where E J k E m displaystyle mathcal E subset J k E m nbsp is a k displaystyle k nbsp th order differential equation on some manifold E displaystyle mathcal E infty nbsp its infinite prolongation and C E displaystyle mathcal C mathcal E infty nbsp its Cartan distribution Note that unlike in the finite case one can show that the Cartan distribution C E displaystyle mathcal C mathcal E infty nbsp is m displaystyle m nbsp dimensional and involutive However due to the infinite dimensionality of the ambient manifold the Frobenius theorem does not hold therefore C E displaystyle mathcal C mathcal E infty nbsp is not integrableA diffiety is a triple O F O C O displaystyle mathcal O mathcal F mathcal O mathcal C mathcal O nbsp consisting of a generally infinite dimensional manifold O displaystyle mathcal O nbsp the algebra of its smooth functions F O displaystyle mathcal F mathcal O nbsp a finite dimensional distribution C O displaystyle mathcal C mathcal O nbsp such that O F O C O displaystyle mathcal O mathcal F mathcal O mathcal C mathcal O nbsp is locally of the form E F E C E displaystyle mathcal E infty mathcal F mathcal E infty mathcal C mathcal E infty nbsp where E C E displaystyle mathcal E infty mathcal C mathcal E infty nbsp is an elementary diffiety and F E displaystyle mathcal F mathcal E infty nbsp denotes the algebra of smooth functions on E displaystyle mathcal E infty nbsp Here locally means a suitable localisation with respect to the Zariski topology corresponding to the algebra F O displaystyle mathcal F mathcal O nbsp The dimension of C O displaystyle mathcal C mathcal O nbsp is called dimension of the diffiety and its denoted by D i m O displaystyle mathrm Dim mathcal O nbsp with a capital D to distinguish it from the dimension of O displaystyle mathcal O nbsp as a manifold Morphisms of diffieties edit A morphism between two diffieties O F O C O displaystyle mathcal O mathcal F mathcal O mathcal C mathcal O nbsp and O F O C O displaystyle mathcal O mathcal F mathcal O mathcal C mathcal O nbsp consists of a smooth map F O O displaystyle Phi mathcal O rightarrow mathcal O nbsp whose pushforward preserves the Cartan distribution i e such that for every point 8 O displaystyle theta in mathcal O nbsp one has d 8 F C 8 C F 8 displaystyle d theta Phi mathcal C theta subseteq mathcal C Phi theta nbsp Diffieties together with their morphisms define the category of differential equations 3 Applications editVinogradov sequence edit The Vinogradov C displaystyle mathcal C nbsp spectral sequence or for short Vinogradov sequence is a spectral sequence associated to a diffiety which can be used to investigate certain properties of the formal solution space of a differential equation by exploiting its Cartan distribution C displaystyle mathcal C nbsp 6 Given a diffiety O F O C O displaystyle mathcal O mathcal F mathcal O mathcal C mathcal O nbsp consider the algebra of differential forms over O displaystyle mathcal O nbsp W O i 0 W i O displaystyle Omega mathcal O sum i geq 0 Omega i mathcal O nbsp and the corresponding de Rham complex C O W 1 O W 2 O displaystyle C infty mathcal O longrightarrow Omega 1 mathcal O longrightarrow Omega 2 mathcal O longrightarrow cdots nbsp Its cohomology groups H i O ker d i im d i 1 displaystyle H i mathcal O text ker text d i text im text d i 1 nbsp contain some structural information about the PDE however due to the Poincare Lemma they all vanish locally In order to extract much more and even local information one thus needs to take the Cartan distribution into account and introduce a more sophisticated sequence To this end let C W O i 0 C W i O W O displaystyle mathcal C Omega mathcal O sum i geq 0 mathcal C Omega i mathcal O subseteq Omega mathcal O nbsp be the submodule of differential forms over O displaystyle mathcal O nbsp whose restriction to the distribution C displaystyle mathcal C nbsp vanishes i e C W p O w W p O w X 1 X p 0 X 1 X p C O displaystyle mathcal C Omega p mathcal O w in Omega p mathcal O mid w X 1 cdots X p 0 quad forall X 1 ldots X p in mathcal C mathcal O nbsp Note that C W i O W i O displaystyle mathcal C Omega i mathcal O subseteq Omega i mathcal O nbsp is actually a differential ideal since it is stable w r t to the de Rham differential i e d C W i O C W i 1 O displaystyle text d mathcal C Omega i mathcal O subset mathcal C Omega i 1 mathcal O nbsp Now let C k W O displaystyle mathcal C k Omega mathcal O nbsp be its k displaystyle k nbsp th power i e the linear subspace of C W displaystyle mathcal C Omega nbsp generated by w 1 w k w i C W displaystyle w 1 wedge cdots wedge w k w i in mathcal C Omega nbsp Then one obtains a filtration W O C W O C 2 W O displaystyle Omega mathcal O supset mathcal C Omega mathcal O supset mathcal C 2 Omega mathcal O supset cdots nbsp and since all ideals C k W displaystyle mathcal C k Omega nbsp are stable this filtration completely determines the following spectral sequence C E O E r p q d r p q where E 0 p q C p W p q O C p 1 W p q O and E r 1 p q H E r p q d r p q displaystyle mathcal C E mathcal O E r p q text d r p q qquad text where qquad E 0 p q frac mathcal C p Omega p q mathcal O mathcal C p 1 Omega p q mathcal O qquad text and qquad E r 1 p q H E r p q d r p q nbsp The filtration above is finite in each degree i e for every k 0 displaystyle k geq 0 nbsp W k O C 1 W k O C k 1 W k O 0 displaystyle Omega k mathcal O supset mathcal C 1 Omega k mathcal O supset cdots supset mathcal C k 1 Omega k mathcal O 0 nbsp so that the spectral sequence converges to the de Rham cohomology H O displaystyle H mathcal O nbsp of the diffiety One can therefore analyse the terms of the spectral sequence order by order to recover information on the original PDE For instance 7 E 1 0 n displaystyle E 1 0 n nbsp corresponds to action functionals constrained by the PDE E displaystyle mathcal E nbsp In particular for L E 1 0 n displaystyle mathcal L in E 1 0 n nbsp the corresponding Euler Lagrange equation is d 1 0 n L 0 displaystyle text d 1 0 n mathcal L 0 nbsp E 1 0 n 1 displaystyle E 1 0 n 1 nbsp corresponds to conservation laws for solutions of E displaystyle mathcal E nbsp E 2 displaystyle E 2 nbsp is interpreted as characteristic classes of bordisms of solutions of E displaystyle mathcal E nbsp Many higher order terms do not have an interpretation yet Variational bicomplex edit As a particular case starting with a fibred manifold p E X displaystyle pi E to X nbsp and its jet bundle J k p displaystyle J k pi nbsp instead of the jet space J k E m displaystyle J k E m nbsp instead of the C displaystyle mathcal C nbsp spectral sequence one obtains the slightly less general variational bicomplex More precisely any bicomplex determines two spectral sequences one of the two spectral sequences determined by the variational bicomplex is exactly the Vinogradov C displaystyle mathcal C nbsp spectral sequence However the variational bicomplex was developed independently from the Vinogradov sequence 8 9 Similarly to the terms of the spectral sequence many terms of the variational bicomplex can be given a physical interpretation in classical field theory for example one obtains cohomology classes corresponding to action functionals conserved currents gauge charges etc 10 Secondary calculus edit Vinogradov developed a theory known as secondary calculus to formalise in cohomological terms the idea of a differential calculus on the space of solutions of a given system of PDEs i e the space of integral manifolds of a given diffiety 11 12 13 3 In other words secondary calculus provides substitutes for functions vector fields differential forms differential operators etc on a generically very singular space where these objects cannot be defined in the usual smooth way on the space of solution Furthermore the space of these new objects are naturally endowed with the same algebraic structures of the space of the original objects 14 More precisely consider the horizontal De Rham complex W O G C O displaystyle overline Omega bullet mathcal O Gamma wedge bullet mathcal C O nbsp of a diffiety which can be seen as the leafwise de Rham complex of the involutive distribution C O displaystyle mathcal C O nbsp or equivalently the Lie algebroid complex of the Lie algebroid C O displaystyle mathcal C O nbsp Then the complex W O displaystyle overline Omega bullet mathcal O nbsp becomes naturally a commutative DG algebra together with a suitable differential d displaystyle overline d nbsp Then possibly tensoring with the normal bundle V T O C O O displaystyle mathcal V T mathcal O mathcal C O to mathcal O nbsp its cohomology is used to define the following secondary objects secondary functions are elements of the cohomology H O H W O d displaystyle overline H bullet mathcal O H bullet overline Omega bullet mathcal O overline d nbsp which is naturally a commutative DG algebra it is actually the first page of the C displaystyle mathcal C nbsp spectral sequence discussed above secondary vector fields are elements of the cohomology H O V H W O V d displaystyle overline H bullet mathcal O mathcal V H bullet overline Omega bullet mathcal O otimes mathcal V overline d nbsp which is naturally a Lie algebra moreover it forms a graded Lie Rinehart algebra together with H O displaystyle overline H bullet mathcal O nbsp secondary differential p displaystyle p nbsp forms are elements of the cohomology H O p V H W O p V d displaystyle overline H bullet mathcal O wedge p mathcal V H bullet overline Omega bullet mathcal O otimes wedge p mathcal V overline d nbsp which is naturally a commutative DG algebra Secondary calculus can also be related to the covariant Phase Space i e the solution space of the Euler Lagrange equations associated to a Lagrangian field theory 15 See also editSecondary calculus and cohomological physics Partial differential equations on Jet bundles Differential ideal Differential calculus over commutative algebras Another way of generalizing ideas from algebraic geometry is differential algebraic geometry References edit Vinogradov A M March 1984 Local symmetries and conservation laws Acta Applicandae Mathematicae 2 1 21 78 doi 10 1007 BF01405491 ISSN 0167 8019 S2CID 121860845 a b Saunders D J 1989 The Geometry of Jet Bundles London Mathematical Society Lecture Note Series Cambridge Cambridge University Press doi 10 1017 cbo9780511526411 ISBN 978 0 521 36948 0 a b c Vinogradov A M 2001 Cohomological analysis of partial differential equations and secondary calculus Providence R I American Mathematical Society ISBN 0 8218 2922 X OCLC 47296188 Krasil shchik I S Lychagin V V Vinogradov A M 1986 Geometry of jet spaces and nonlinear partial differential equations Adv Stud Contemp Math N Y Vol 1 New York etc Gordon and Breach Science Publishers ISBN 978 2 88124 051 5 Guneysu Batu Pflaum Markus J 2017 01 10 The Profinite Dimensional Manifold Structure of Formal Solution Spaces of Formally Integrable PDEs SIGMA Symmetry Integrability and Geometry Methods and Applications 13 003 arXiv 1308 1005 Bibcode 2017SIGMA 13 003G doi 10 3842 SIGMA 2017 003 S2CID 15871902 Vinogradov A M 1978 A spectral sequence associated with a nonlinear differential equation and algebro geometric foundations of Lagrangian field theory with constraints Soviet Math Dokl in Russian 19 144 148 via Math Net Ru Symmetries and conservation laws for differential equations of mathematical physics A V Bocharov I S Krasilʹshchik A M Vinogradov Providence R I American Mathematical Society 1999 ISBN 978 1 4704 4596 6 OCLC 1031947580 a href Template Cite book html title Template Cite book cite book a CS1 maint others link Tulczyjew W M 1980 Garcia P L Perez Rendon A Souriau J M eds The Euler Lagrange resolution Differential Geometrical Methods in Mathematical Physics Lecture Notes in Mathematics 836 Berlin Heidelberg Springer 22 48 doi 10 1007 BFb0089725 ISBN 978 3 540 38405 2 Tsujishita Toru 1982 On variation bicomplexes associated to differential equations Osaka Journal of Mathematics 19 2 311 363 ISSN 0030 6126 variational bicomplex in nLab ncatlab org Retrieved 2021 12 11 Vinogradov A M 1984 04 30 The b spectral sequence Lagrangian formalism and conservation laws I The linear theory Journal of Mathematical Analysis and Applications 100 1 1 40 doi 10 1016 0022 247X 84 90071 4 Vinogradov A M 1984 04 30 The b spectral sequence Lagrangian formalism and conservation laws II The nonlinear theory Journal of Mathematical Analysis and Applications 100 1 41 129 doi 10 1016 0022 247X 84 90072 6 ISSN 0022 247X Henneaux Marc Krasil shchik Joseph Vinogradov Alexandre eds 1998 Secondary Calculus and Cohomological Physics Contemporary Mathematics Vol 219 Providence Rhode Island American Mathematical Society doi 10 1090 conm 219 ISBN 978 0 8218 0828 3 Vitagliano Luca 2014 On the strong homotopy Lie Rinehart algebra of a foliation Communications in Contemporary Mathematics 16 6 1450007 arXiv 1204 2467 doi 10 1142 S0219199714500072 ISSN 0219 1997 S2CID 119704524 Vitagliano Luca 2009 04 01 Secondary calculus and the covariant phase space Journal of Geometry and Physics 59 4 426 447 arXiv 0809 4164 Bibcode 2009JGP 59 426V doi 10 1016 j geomphys 2008 12 001 ISSN 0393 0440 S2CID 21787052 External links editThe Diffiety Institute frozen since 2010 The Levi Civita Institute successor of above site Geometry of Differential Equations Differential Geometry and PDEs Retrieved from https en wikipedia org w index php title Diffiety amp oldid 1215932105, wikipedia, wiki, book, books, library,

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