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Effects of circulation and buoyancy on the transition from a fire whirl to a blue whirl

Sriram Bharath Hariharan*

Yu Hu*

Michael J. Gollner

Elaine S. Oran

  • Department of Mechanical Engineering, University of Maryland, College Park, Maryland 20742, USA

  • Laboratory of Advanced Space Propulsion, Beijing Institute of Control Engineering, Beijing, People's Republic of China

  • Department of Mechanical Engineering, University of California, Berkeley, Berkeley, California 94720, USA

  • Department of Aerospace Engineering, Texas A&M University, College Station, Texas 77843, USA

  • *S.B.H. and Y.H. contributed equally to this article.
  • mgollner@berkeley.edu

Phys. Rev. Fluids 5, 103201 – Published 14 October, 2020

DOI: https://doi.org/10.1103/PhysRevFluids.5.103201

Abstract

The relative influence of circulation and buoyancy on fire whirls (FWs), blue whirls (BWs), and the transition between these regimes of a whirling flame is investigated using a combination of experimental data and scaling analyses. FWs are whirling, turbulent, cylindrical yellow (sooting) flame structures that form naturally in fires and are here created in laboratory experiments. In contrast, a BW is a laminar, blue flame (nonsooting) with an inverted conical shape. Measurements of the circulation and heat-release rate are combined with measurements of the flame geometry, defined by the flame width and the height, to provide characteristic length scales for these whirling-flame regimes. Using these, a nondimensional circulation (Γf*) and a heat-release rate (Q̇f*) were defined and shown to correspond to azimuthal and axial (buoyancy driven) momenta, respectively. The ratio R*=Γf*/Q̇f*, a quantity analogous to the swirl number used to characterize swirling jets, was evaluated for FWs and BWs. For FWs, R*<1, so that axial momentum is greater than azimuthal momentum and the flame is dominated by buoyant momentum. For BWs, R*>1, so that the flame is circulation dominated. This is argued to be consistent with vortex breakdown being an important part of the transition of FWs to BWs. This work presents a basis for predicting when a BW will form and remain a stable regime.

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