2021
DOI: 10.1103/physreve.104.014603
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Complete absorption of topologically protected waves

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Cited by 7 publications
(5 citation statements)
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“…In systems without antisymmetric stress, odd viscosity induces distinct chiral surface waves with dispersion ≈ −2ν o q|q| at a free surface (with a no-stress boundary condition), in which (53)(54)(55). Another class of boundary effects are topological sound waves (40,56,57). These occur in compressible odd viscous flows under the combined influence of the Lorentz (or Coriolis) body force and odd viscosity.…”
Section: Boundary Effectsmentioning
confidence: 99%
“…In systems without antisymmetric stress, odd viscosity induces distinct chiral surface waves with dispersion ≈ −2ν o q|q| at a free surface (with a no-stress boundary condition), in which (53)(54)(55). Another class of boundary effects are topological sound waves (40,56,57). These occur in compressible odd viscous flows under the combined influence of the Lorentz (or Coriolis) body force and odd viscosity.…”
Section: Boundary Effectsmentioning
confidence: 99%
“…In systems without antisymmetric stress, odd viscosity induces distinct chiral surface waves with dispersion Ω ≈ −2νoq|q| at a free surface (with a no-stress boundary condition) (32,33,34). Another class of boundary effects are topological sound waves (35,36,37). These occur in compressible odd viscous flows, under the combined influence of the Lorentz (or Coriolis) body force and odd viscosity.…”
Section: Boundary Effectsmentioning
confidence: 99%
“…Averaging the incompressibility condition (11), and making use of the kinematic boundary conditions ( 6)- (7), we obtain the exact conservation of mass equation…”
Section: Shallow-water Approximation and Depth Averagingmentioning
confidence: 99%
“…where we have used that h and w are zero at z = 0, and we have included the upper boundary terms in square brackets. Both of the boundary terms are in fact zero: the first follows from the kinematic boundary condition (7), while the second follows from the original construction of the stress tensor. Significantly, the odd-viscous contributions on the left-hand side in ( 22) can be rewritten as a sum of two terms:…”
Section: Shallow-water Approximation and Depth Averagingmentioning
confidence: 99%
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