In differential geometry, the Yang–Mills flow is a gradient flow described by the Yang–Mills equations, hence a method to describe a gradient descent of the Yang–Mills action functional. Simply put, the Yang–Mills flow is a path always going in the direction of steepest descent, similar to the path of a ball rolling down a hill. This helps to find critical points, called Yang–Mills connections or instantons, which solve the Yang–Mills equations, as well as to study their stability. Illustratively, they are the points on the hill on which the ball can rest.

Visualization of gradient descent with one flow line

The Yang–Mills flow is named after Yang Chen-Ning and Robert Mills, who formulated the underlying Yang–Mills theory in 1954, although it was first studied by Michael Atiyah and Raoul Bott in 1982. It was also studied by Simon Donaldson in the context of the Kobayashi–Hitchin correspondence (or Donaldson–UhlenbeckYau theorem).

Definition

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Let   be a compact Lie group with Lie algebra   and   be a principal  -bundle with a compact orientable Riemannian manifold   having a metric   and a volume form  . Let   be its adjoint bundle. One has  , which are either under the adjoint representation   invariant Lie algebra–valued or vector bundle–valued differential forms. Since the Hodge star operator   is defined on the base manifold   as it requires the metric   and the volume form  , the second space is usually used.

All spaces   are vector spaces, which from   together with the choice of an   invariant pairing on   (which for semisimple   must be proportional to its Killing form) inherit a local pairing  . It defines the Hodge star operator by   for all  . Through postcomposition with integration there is furthermore a scalar product  . Its induced norm is exactly the   norm.

A connection   induces a differential  , which has an adjoint codifferential  . Unlike the Cartan differential   with  , the differential   fulfills   with the curvature form:

 

The Yang–Mills action functional is given by:[1][2][3]

 

Hence the gradient of the Yang–Mills action functional gives exactly the Yang–Mills equations:

 

For an open interval  , a   map   (hence continuously differentiable) fulfilling:[4][2][3]

 

is a Yang–Mills flow.

Properties

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  • For a Yang–Mills connection  , the constant path on it is a Yang–Mills flow.
  • For a Yang–Mills flow   one has:
 
Hence   is a monotonically decreasing function. Alternatively with the above equation, the derivative can be connected to the Bi-Yang–Mills action functional:
 
Since the Yang–Mills action functional is always positive, a Yang–Mills flow which is continued towards infinity must inevitably converge to a vanishing derivative and hence a Yang–Mills connection according to the above equation.
  • For any connection  , there is a unique Yang–Mills flow   with  . Then   is a Yang–Mills connection.
  • For a stable Yang–Mills connection  , there exists a neighborhood so that every unique Yang–Mills flow   with initial condition in it fulfills:
     

Literature

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  • Kelleher, Casey Lynn; Streets, Jeffrey (2016-02-09). "Singularity formation of the Yang-Mills flow". arXiv:1602.03125 [math.DG].
  • Alex, Waldron (2016-10-16). "Long-time existence for Yang–Mills flow". Inventiones Mathematicae. 217 (3): 1069–1147. arXiv:1610.03424. doi:10.1007/s00222-019-00877-2.
  • Zhang, Pan (2020-03-30). "Gradient Flows of Higher Order Yang-Mills-Higgs Functionals". arXiv:2004.00420 [math.DG].

See also

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References

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  1. ^ Kelleher & Streets 2016, p. 3
  2. ^ a b Waldron 2016, p. 1
  3. ^ a b Zhang 2020, p. 1
  4. ^ Kelleher & Streets 2016, p. 1 & 3