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Horizontal convection in shallow enclosures scales with height, not length, at low Rayleigh numbers

机译:在低瑞利数下,浅罩中的水平对流与高度成比例,而不是长度成比例

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Horizontal convection is a distinct type of natural convection, where the flow is driven by non-uniform buoyancy supplied along a horizontal boundary. Horizontal convection has been studied in enclosures with aspect ratios (ratio of enclosure height H to length L) down to O(10(-1)), though the flow dynamics and heat transfer in very shallow enclosures remain unexplored. This study employs a high-order spectral-element method and the Boussinesq buoyancy approximation to simulate horizontal convection in rectangular enclosures for aspect ratios 10(-3) <= A = H/L <= 0.16, over Rayleigh numbers 10 <= Ra <= 10(16) and a fixed Prandtl number Pr = 6.14 representative of water. The flow is driven by imposing a linear temperature variation along the bottom boundary of the enclosure, and insulating temperature conditions on the remaining boundaries.This work, for the first time, explores small aspect ratios towards the shallow-enclosure limit up to 100 times shallower than those studied previously to elucidate the effect of ocean-relevant confinement on horizontal convection. The Rayleigh number delineating the transition between the diffusion-dominated and convection-influenced regime is identified. The aspect ratio dependence of these Rayleigh numbers and their corresponding Nusselt numbers are found to follow power-law scalings Nu similar to A and Ra similar to A(-4). These scalings illuminate a modified Nusselt number and Rayleigh number that govern horizontal convection at lower Rayleigh numbers, and reveal that height, rather than the horizontal length, governs the flow dynamics. Away from the side-walls the velocity and temperature profiles in these regimes exhibit self-similarity features and are well-described by the analytical solution for a one-dimensional horizontal channel flow driven by horizontal temperature gradient. A previously unseen behaviour is discovered whereby at aspect ratios A less than or similar to 0.1, an increasingly broad horizontally uniform zone with no heat transfer into the base occupies the middle of the enclosure, thereby localising the heating and cooling to within a distance of approximately 4H of the sidewalls.
机译:水平对流是自然对流的一种独特类型,其流动是由沿水平边界提供的非均匀浮力驱动的。在深宽比(外壳高度H与长度L的比率)低至O(10(-1))的外壳中,已经研究了水平对流,尽管在非常浅的外壳中的流动动力学和热传递仍未探索。这项研究采用高阶频谱元素方法和Boussinesq浮力逼近来模拟矩形围护结构中水平比10(-3)<= A = H / L <= 0.16,瑞利数10 <= Ra < = 10(16)和固定的普朗特数Pr = 6.14,代表水。通过沿着外壳的底​​部边界施加线性温度变化并在其余边界上施加绝缘温度条件来驱动流动。这项工作首次探索了朝浅外壳极限的小长宽比,最高可达浅外壳的100倍。比以前研究过的那些研究来阐明与海洋有关的限制对水平对流的影响。确定了瑞利数,该瑞利数描述了以扩散为主和对流影响的状态之间的过渡。发现这些瑞利数及其对应的努塞尔特数的长宽比依赖性遵循与A相似的幂律比例Nu和与A(-4)相似的Ra。这些缩放比例照亮了修改后的Nusselt数和Rayleigh数,它们控制了较低Rayleigh数下的水平对流,并揭示了高度而不是水平长度决定了流动力学。在远离侧壁的情况下,这些状态下的速度和温度分布显示出自相似的特征,并且由水平温度梯度驱动的一维水平通道流的解析解很好地描述了这一点。发现了一种以前看不见的行为,其中在宽高比A小于或等于0.1的情况下,越来越大的水平均匀区域(没有热量传递到底部)占据了外壳的中部,从而将加热和冷却的位置限制在大约侧壁的4H。

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