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A computational examination of large-scale pool fires: variations in crosswind velocity and pool shape

Published online by Cambridge University Press:  03 November 2022

Sarah N. Scott
Affiliation:
Thermal/Fluid Science and Engineering, Sandia National Laboratories, P.O. Box 969 MS 9042, Livermore, CA 94551, USA
Stefan P. Domino*
Affiliation:
Computational Thermal and Fluid Mechanics Department, Sandia National Laboratories, P.O. Box 5800 MS 0828, Albuquerque, NM 87109-0828, USA Institute for Computational and Mathematical Engineering, Huang Engineering Building, 475 Via Ortega Suite B060, Stanford, CA 94305, USA
*
*Corresponding author. E-mail: spdomin@sandia.gov

Abstract

A high-fidelity large-eddy simulation and unsteady flamelet combustion model construct is deployed to numerically investigate the effects of crosswind magnitude and pool fire shape on large-scale pool fire attributes. These include general flame dynamics, flame shape and radiative flux magnitude in and around the fire. Three pool fire shapes at a nominal length scale of 10 m are subjected to four crosswind magnitudes between 0 and 20 m s$^{-1}$. The pool shapes studied are circular, square and rectangular. The study includes the sensitivity of parameters to mesh and time step refinement. Results demonstrate that the rectangular shape, under crosswind, has low-levels of vertical velocity induction, resulting in a plume that is closer to the ground. In the quiescent regime, under-resolved meshes provide a higher radiative heat flux prediction compared with the most refined mesh. However, as crosswind increases, low mesh resolutions underpredicted radiative flux. This is due to the coarse mesh resolution not capturing small-scale vortical features that increased mixing and combustion efficiency. A transition of peak radiative flux with respect to crosswind occurs from the leeward- to windward-side of the pool, while sharp pool features result in larger radiative heat fluxes concentrated in regions of high scalar dissipation rate.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2022. Published by Cambridge University Press
Figure 0

Figure 1. (a) The domain is 114 m long ($x$ direction), 57 m wide ($z$ direction) and 43 m high ($y$ direction) for the cases with a crosswind. An additional 28 m were added to the height for the quiescent case. The inflow condition is along the $x$ axis. The origin of the domain is on the centre of the pool. (b) Each pool has the same area, $A=\pi 10^2/4\approx 78.53 \ m^2$. The square pool is defined as $W=L=\sqrt {\pi 10^2/4}\approx 8.862 \ m$ and the rectangle is defined as $W=L/3=\sqrt {\pi 10^2/12}\approx 5.122 \ m$.

Figure 1

Figure 2. Coarse (R0) mesh illustration outlining (a) vertical resolution, and the surface-based paving construct for the (b) circle, (c) square and (d) rectangle pool shape configurations.

Figure 2

Table 1. Number of elements for each of the meshes used in the study.

Figure 3

Figure 3. A matrix of volume renderings of instantaneous temperature for the R2 meshes. The back plane is coloured by Favre-averaged vorticity (in the direction normal to the plane, $+x$), where red is positive rotation and black is negative rotation. In our discussion that follows, Favre-averaged variables (in time) for Favre-filtered QoI are labelled as $\hat \phi = \overline {\rho \tilde \phi } / {\bar \rho }$, and referred to as simply ‘Favre-averaged $\phi$’.

Figure 4

Figure 4. Isocontours of the Favre-averaged temperature at 723 and 773 K for the three pool shapes, (a) circular, (b) square, (c) rectangle, showing the four crosswind conditions (0, 5, 10, 20 m s$^{-1}$), R2 mesh. The rectangular pool has shorter contours than the circle and the square. For the rectangular pool shape, pool-generated vortex pair interaction is separated more than in the other two pools, leading to less interaction and a smaller induced velocity in the vertical ($y$) direction.

Figure 5

Table 2. Flame lengths ($L_f$), flame angle ($\theta _d$) and drag lengths ($L_d$), as defined by the 773 K isotherm on the R2 mesh for each crosswind velocity and pool shape.

Figure 6

Figure 5. The Favre-averaged temperature contours and Favre-averaged velocity plots for all pool shapes and for three crosswind values: (a) 5 m s$^{-1}$; (b) 10 m s$^{-1}$; (c) 20 m s$^{-1}$. For each image, the first column shows an isometric projection of an isothermal contour at 350 K of the fire plume, as well as the location of three planes. The second column is the plane at 0 m from the centre of the pool; the third column is the plane at 35 m from the centre of the pool; the fourth column is the plane at 70 m from the centre of the pool. Each plane shows the $y$ component of velocity (colour map), the projection of the velocity on the $z$-plane (arrows) and a contour of 350 K (white lines). If no temperature contour appears on the slice, no temperature on the plane was over 350 K.

Figure 7

Figure 6. A matrix of the magnitude of the Favre-averaged radiative flux on ground with contour lines for the Favre-averaged scalar dissipation rate at $1\times 10^{-2}$, $1\times 10^{-3}$ and $1\times 10^{-4}$ s$^{-1}$ at 1 mm above the ground. Results shown are for the R2 mesh. The rectangular and square pools generally have higher radiative fluxes, particularly as a crosswind is introduced. The location of the highest radiative heat flux transitions from the leeward side of the pool to the windward side.

Figure 8

Figure 7. A matrix of the Favre-averaged subgrid-scale kinetic energy, $\hat {k}_{SGS}$ for each pool shape and crosswind for the R2 mesh at one millimetre above the ground. A similar pattern is seen as with the heat flux (figure 6), where now the rectangular pools have higher modelled turbulence, and increases with crosswind.

Figure 9

Figure 8. (a) Magnitude of the Favre-averaged radiative flux on the ground for two crosswind velocities (5 and 20 m s$^{-1}$), and (b) vorticity on a cut plane 70 m from the centre of the rectangular pool for the same pool and crosswind velocities. The vorticity is shown in the direction normal to the plane, $+x$, where red is positive rotation and black is negative rotation. Here we see that the for both the vorticity and the radiative flux, the 5 m s$^{-1}$, the shape does not change significantly across mesh resolutions. The 20 m s$^{-1}$ shows a significant difference in the shape of the radiative flux across mesh resolutions.

Figure 10

Table 3. The integrated flux over the area of the ground plane, in megawatts, for each pool shape and crosswind combination for each of the mesh resolutions.

Figure 11

Figure 9. Isocontours of the Favre-averaged temperature for the rectangular pool at 723 and 773 K for the three refinements (a) R0, (b) R1 and (c) R2 – each showing the four crosswind conditions (0, 5, 10, 20 m s$^{-1}$). In the under-resolved case, the flame lengths are shorter, while when small-scale mixing is underpredicted, such as in the high cross-flow configuration, drag lengths are poorly predicted.