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Published on: November 15, 2013
Vertex Constraints in 3D Higher Spin Theories.
Stefan Fredenhagen1, Olaf Krüger2, Karapet Mkrtchyan3
1University of Vienna, Faculty of Physics, Boltzmanngasse 5, 1090 Vienna, Austria and Erwin Schrödinger International Institute for Mathematics and Physics, Boltzmanngasse 9, 1090 Vienna, Austria.
Gauge invariance in 3D higher-spin gravity restricts higher-order interactions. Only scalar and Maxwell fields can form vertices independent of the cubic ones, fixing all nonlinear interactions.
Area of Science:
- Theoretical Physics
- Quantum Field Theory
- String Theory
Background:
- Higher-spin gravities extend Einstein's theory with fields of increasing spin.
- Gauge invariance is a fundamental principle in physics, ensuring physical quantities are independent of certain transformations.
- Understanding interactions in higher-spin theories is crucial for developing a complete theory of quantum gravity.
Purpose of the Study:
- To investigate the constraints imposed by gauge invariance on higher-order interactions.
- To determine the structure of nonlinear interactions between massless bosonic fields in 3D higher-spin gravities.
- To identify which fields can participate in quartic and higher-order interaction vertices independent of cubic ones.
Main Methods:
- Analysis of gauge invariance conditions.
- Focus on the transverse-traceless part of field interactions.
- Derivation of interaction vertices for massless bosonic fields.
Main Results:
- Gauge invariance significantly constrains higher-order interaction vertices.
- Vertices independent of the cubic ones can only involve scalar and Maxwell fields.
- The full nonlinear interactions of massless higher-spin fields are completely determined by the cubic vertex.
Conclusions:
- The structure of nonlinear interactions in 3D higher-spin gravities is highly constrained.
- The cubic vertex plays a pivotal role in defining all higher-order interactions.
- These findings simplify the study of higher-spin theories and their potential applications.
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