Abstract
Natural convection over a roof-shaped triangular surface is investigated using direct numerical simulations. The Rayleigh number (Ra) was varied from 1 to with air as working fluid (Prandtl number of 0.71) at a fixed geometrical aspect ratio of 0.1, defined as the ratio of roof height to half-width. The transition route from a steady flow to a chaotic flow on the surface is characterized by the topological method with the increase of Ra. A weak flow, dominated by conduction, occurs when Ra was relatively small. As Ra increases, the convective flow becomes stronger and a sequence of bifurcations is found. Between and , a primary pitchfork bifurcation occurs. Secondary and tertiary pitchfork bifurcations are observed in the range and , respectively. After another pitchfork bifurcation at , which makes the plume tilt to either side of the roof top edge, a Hopf bifurcation is observed in , after which both the slope flow and plume become periodic. This is followed by further bifurcations including a period doubling bifurcation at and a quasiperiodic bifurcation firstly arising at . Finally, the flow becomes chaotic for . The state space, the maximum Lyapunov exponent, the fractal dimension, and the power spectral density are presented to analyze the flows in the transition to chaos. This work is a comprehensive description of the flow transition from steady state to chaos on surface of a section-triangular roof that is pertinent to various settings where fluid flow develops.
9 More- Received 6 September 2020
- Accepted 23 December 2020
DOI:https://doi.org/10.1103/PhysRevFluids.6.013502
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