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Thermal convection in laboratory-scale porous media.

机译:实验室规模的多孔介质中的热对流。

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Convection experiments were conducted in laboratory-scale porous media with overall heights of 1 m and 0.24 m. The objective of these experiments was to observe the temperature and mass flow characteristics of convection structures within porous media heated from below. A thermochromic liquid crystal (TLC) tracer was used in combination with a charge couple device (CCD) digital camera to observe temperature and mass flow characteristics. The TLC tracer proved to be useful in qualitatively observing temperature and mass flow within the system. Color-temperature calibration for the tracer often had high uncertainties and non-unique color-temperature behavior limiting the quantitative quality of the data. Convection was typically characterized by the formation of plumes or fingers. Plumes tended to widen when flowing from a high to low permeability region in agreement with Darcy's law and conservation of mass. Steady-state conditions appeared to develop when temperature gradients and permeabilities were highest.
机译:对流实验是在实验室规模的多孔介质中进行的,总高度分别为1 m和0.24 m。这些实验的目的是观察从下方加热的多孔介质中对流结构的温度和质量流量特性。热致变色液晶(TLC)示踪剂与电荷耦合器件(CCD)数码相机结合使用以观察温度和质量流量特性。事实证明,TLC示踪剂可用于定性观察系统内的温度和质量流量。示踪剂的色温校准通常具有很高的不确定性,并且色温行为不均匀,从而限制了数据的定量质量。对流通常以羽状或手指状形成为特征。当从高渗透性区域流向低渗透性区域时,与达西定律和质量守恒相一致,羽状流往往会扩大。当温度梯度和磁导率最高时,就会出现稳态条件。

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