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Experimental modelling of crown fire initiation in open and closed shrubland systems

机译:开放和封闭灌木丛系统中树冠起火的实验模型

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The transition of surface fire to live shrub crown fuels was studied through a simplified laboratory experiment using an open-topped wind tunnel. Respective surface and crown fuels used were excelsior (shredded Populus tremuloides wood) and live chamise (Adenostoma fasciculatum, including branches and foliage). A high crown fuel bulk density of 6.8kgm-3 with a low crown fuel base height of 0.20m was selected to ensure successful crown fire initiation. Diagnostics included flame height and surface fire evolution. Experimental results were compared with similar experiments performed in an open environment, in which the side walls of the wind tunnel were removed. The effect of varying wind speed in the range 01.8ms-1, representing a Froude number range of 01.1, on crown fire initiation was investigated. The suppression of lateral entrainment due to wind tunnel walls influenced surface fire behaviour. When wind speed increased from 1.5 to 1.8ms-1, the rate of spread of surface fire and surface fire depth increased from 5.5 to 12.0cms-1 and 0.61 to 1.02m. As a result, the residence time of convective heating significantly increased from 16.0 to 24.0s and the hot gas temperature at the crown base increased from 994 to 1141K. The change in surface fire characteristics significantly affected the convective energy transfer process. Thus, the net energy transfer to the crown fuel increased so the propensity for crown fire initiation increased. In contrast, increasing wind speed decreased the tendency for crown fuel initiation in an open environment because of the cooling effect from fresh air entrainment via the lateral sides of surface fire.
机译:通过使用敞顶式风洞的简化实验室实验,研究了表面火向活性灌木冠状燃料的转变。分别使用的表层燃料和表冠燃料为极好(切碎的胡杨木)和活毛毡(Adenostoma fasciculatum,包括树枝和树叶)。选择了高6.8kgm-3的高冠燃料堆密度和低0.20m的低冠燃料基础高度,以确保成功引发冠火。诊断包括火焰高度和表面着火情况。将实验结果与在开放环境中执行的类似实验进行了比较,在开放环境中风洞的侧壁被移除。研究了01.8ms-1(代表Froude数范围为01.1)范围内的风速变化对冠顶起火的影响。由于风洞壁而引起的侧向夹带的抑制影响了表面火的行为。当风速从1.5增加到1.8ms-1时,地表火的蔓延速率和地表火深度从5.5上升到12.0cms-1,从0.61上升到1.02m。结果,对流加热的停留时间从16.0s显着增加到24.0s,冠底的热气体温度从994k增加到1141k。表面火特性的变化显着影响对流能量传递过程。因此,向顶冠燃料的净能量传递增加,因此顶冠起火的倾向增加。相反,由于来自新鲜空气通过表面火的侧面夹带的冷却效果,增加的风速降低了在开放环境中冠状燃料引发的趋势。

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