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PreprintCC BY 4.0arXiv

Liouville Theorems for Stationary Navier-Stokes Equations via the Radial Velocity Component

Abstract

We study Liouville-type results for the stationary Navier--Stokes equations in ℝ3. We prove that any Ḣ1(ℝ3) solution is trivial under an integrability condition imposed only on the radial component of the velocity, namely uρ(x) ∈ Lp(ℝ3) with 3/2 < p ≤ 3. We also establish a uniqueness result in a variable-exponent setting, where an L6-type condition is required only on a bounded region, while the exponent approaches the critical value $3$ at infinity. Our analysis reveals that the rigidity of the stationary Navier--Stokes system can be driven by localized and radial integrability properties, rather than uniform global conditions.

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BibTeX
@misc{vergarahermosilla2026liouville,
  title = {{Liouville Theorems for Stationary Navier-Stokes Equations via the Radial Velocity Component}},
  author = {Gaston Vergara-Hermosilla},
  howpublished = {arXiv},
  year = {2026},
  month = oct,
  doi = {10.48550/arxiv.2605.05647},
  eprint = {2605.05647},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2605.05647},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Liouville Theorems for Stationary Navier-Stokes Equations via the Radial Velocity Component
AU  - Gaston Vergara-Hermosilla
PY  - 2026
DA  - 2026/10/10
PB  - arXiv
DO  - 10.48550/arxiv.2605.05647
UR  - https://arxiv.org/abs/2605.05647
AB  - We study Liouville-type results for the stationary Navier--Stokes equations in ℝ^3. We prove that any Ḣ^1(ℝ^3) solution is trivial under an integrability condition imposed only on the radial component of the velocity, namely u_ρ(x) ∈ L^p(ℝ^3) with 3/2 < p ≤ 3. We also establish a uniqueness result in a variable-exponent setting, where an L^6-type condition is required only on a bounded region, while the exponent approaches the critical value $3$ at infinity. Our analysis reveals that the rigidity of the stationary Navier--Stokes system can be driven by localized and radial integrability properties, rather than uniform global conditions.
ER  -