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Solid velocity and concentration fluctuations in highly concentrated liquid–solid (slurry) pipe flows

机译:高浓度液固(浆)管道中的固体速度和浓度波动

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Solid velocity and concentration fluctuations were measured for concentrated sand-water mixtures (20–35% solid by volume) in horizontal pipe flow using Electrical Impedance Tomography (EIT). Narrowly sized sand (d_(50) = 100 lm) was used to prepare each slurry tested in a 52 mm (i.d.) horizontal pipe loop at mixture velocities (2–5 m/s) that were significantly above the deposition velocity. The EIT measurements were used to obtain solid velocity and concentration fluctuation maps. Results show that the magnitude of the local solid concentration fluctuations is greater near the pipe wall and increases as the mixture velocity increases. Additionally, the concentration fluctuations are greater near the pipe invert, particularly at lower mixture velocities and/or concentrations where the solid concentration profiles are asymmetric. The Fast Fourier Transform (FFT) method was employed to study the power spectral density of these fluctuations. This analysis indicates that concentration fluctuations are produced almost entirely by particle–fluid turbulence interactions, rather than through particle–particle or particle–wall interactions. Comparison of the particle diameter with the characteristic turbulent length scales shows that the particles interact with turbulent eddies in the dissipative range, which is in accordance with the power spectral density analysis. The findings presented here are consistent with previous studies of fluidized beds and gravity-driven flows.
机译:使用电阻层析成像(EIT)对水平管道中浓砂水混合物(体积分数为20–35%的固体)的固体速度和浓度波动进行了测量。窄砂(d_(50)= 100 lm)用于制备在52 mm(i.d.)水平管道回路中以明显高于沉积速度的混合速度(2-5 m / s)测试的每种浆料。 EIT测量用于获得固体速度和浓度波动图。结果表明,局部固体浓度波动的幅度在管壁附近更大,并且随着混合速度的增加而增加。另外,在管道内腔附近,浓度波动更大,尤其是在较低的混合速度和/或固体浓度分布不对称的浓度下。快速傅里叶变换(FFT)方法用于研究这些波动的功率谱密度。该分析表明,浓度波动几乎完全是由颗粒-流体湍流相互作用产生的,而不是由颗粒-颗粒或颗粒-壁相互作用产生的。粒径与特征湍流长度尺度的比较表明,在耗散范围内,颗粒与湍流相互作用,这与功率谱密度分析一致。这里介绍的发现与以前对流化床和重力驱动流的研究一致。

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