Vortical flows over spinning cones at incidence

Vortical flows over spinning cones with half-angles of θ c = 10^∘ , 15^∘ , 22.5^∘ , 30^∘ and 45^∘ at incidence angles of α between 0 ^∘ and 36 ^∘ are experimentally studied employing smoke streak flow visualisation and planar particle image velocimetry at Reynolds numbers of O(10⁴) and base rotational speed ratios between 0 and 3. Symmetric vortex triads are observed on the leeward side of the stationary cones at incidence that grow in cross-section and strength along the surface. Spin breaks down this symmetry. Asymmetries in the vortex systems over the spinning cones are characterised by anti-cyclonic vortices forming in the counter-rotating meridian and cyclonic vortices in the co-rotating meridian. The anti-cyclonic vortices increase in strength as they are pushed in the direction of rotation and embrace the surface of the cone, whereas cyclonic vortices detach from the surface and exhibit unchanging vortex strength. For the most slender cone of θ c = 10^∘ , the cyclonic vortices are pushed past the plane of symmetry into the counter-rotating meridian and are squeezed between the anti-cyclonic vortex and the surface of the cone. This appears to trigger the detachment of the anti-cyclonic vortices. The thickest cone of θ c = 45^∘ exhibits characteristics similar to flows over a disc (Kuraan & Savaş J. Visual. vol. 23 , 2024, pp. 191–205), a limiting case of the cone family. As α increases, the stagnation point departs from the vertex and monotonically shifts along the windward surface. Regular vortex shedding events in the wake region behind the θ c=45^∘ cone are detected in the streakline images, also a common characteristic of flows over discs. Wave patterns are observed near the leeward surface of spinning cones, which are likely signatures of the well-known centrifugal spiral wave instabilities. The bead-like features leave small-scale wave patterns on detached portions of the neighbouring trailing vortices. Inclined wave patterns form on streaklines over the entire surface of the cones, and are present in both non-spinning and spinning cases; hence, they are likely signatures of classical cross-flow boundary layer instabilities.