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Direct measurement of heat flux from cooling lake thermal imagery

机译:从冷却湖热量图像直接测量热通量

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Laboratory experiments show a linear relationship between the total heat flux from a water surface to air and thestandard deviation of the surface temperature field, a, derived from thermal images of the water surface over a range ofheat fluxes from 400 to 1800 Wm~(-2). Thermal imagery and surface data were collected at two power plant cooling lakesto determine if the laboratory relationship between heat flux and a exists in large heated bodies of water. The heat fluxescomputed from the cooling lake data range from 200 to 1400 Wm~(-2). The linear relationship between a and Q is evidentin the cooling lake data, but it is necessary to apply band pass filtering to the thermal imagery to remove camera artifactsand non-convective thermal gradients. The correlation between a and Q is improved if a correction to the measured σ ismade that accounts for wind speed effects on the thermal convection. Based on more than a thousand cooling lakeimages, the correlation coefficients between σ and Q ranged from about 0.8 to 0.9.
机译:实验室实验表明,从水面到空气的总热量通量与表面温度场的偏差之间的线性关系,a,从400到1800wm的水分助焊剂范围内衍生自水面的热图像〜(-2 )。在两个发电厂冷却Lakesto收集热图像和表面数据,确定热量和A之间的实验室关系是否存在于大型水中的水中。从冷却湖数据的热量计算为200至1400WM〜(-2)。 A和Q之间的线性关系是Apidentin冷却湖数据,但是必须将带通滤波施加到热图像中以去除相机艺术和非对流热梯度。如果对测量ΣIsmade的校正,则A和Q之间的相关性得到改善,该σ是对热对流的风速效应的校正。基于一千多个冷却湖皮,σ和Q之间的相关系数范围为约0.8至0.9。

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