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Modeling of retention and re-entrainment of mono- and poly-disperse particles: Effects of hydrodynamics, particle size and interplay of different-sized particles retention

机译:单分散和多分散颗粒的保留和再夹带模型:流体动力学,粒径和不同尺寸颗粒保留的相互作用的影响

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In this paper, numerical simulations of experimental data were performed with kinetic rate coefficients to characterize the retention and re-entrainment dynamics under different hydrodynamic conditions for monodisperse and polydisperse latex particles (3,10,16μτη and the mixture). The results show that drastic increase in fluid velocity provokes hardly any remarkable decrease in retention in the presence of large energy barriers (>2000 kT). Systematical increases in deposition and re-entrainment dynamic rates were observed with fluid velocity and/or particle size. Increased irreversible deposition rate indicates straining and wedging dominate deposition in this study. Excess retention of 3 μπι particle in the polydisperse particle suspension was observed. The origins are reckoned that deposited larger particles may hinder the re-entrainment of smaller particles near the grain-to-grain contact and can provide additional sites of attachment
机译:在本文中,用动力学速率系数进行了实验数据的数值模拟,以表征在单分散和多分散胶乳颗粒(3、10、16μm和混合物)的不同流体动力学条件下的保留和重新夹带动力学。结果表明,在存在较大的能垒(> 2000 kT)的情况下,流体速度的急剧增加几乎不会引起滞留率的任何显着降低。随着流体速度和/或粒径观察到沉积和重新夹带动态速率的系统增加。不可逆沉积速率增加表明,在这项研究中,应变和楔形作用是沉积的主导。观察到3μm颗粒在多分散颗粒悬浮液中过量保留。据推测,沉积的原因可能是较大的颗粒沉积会阻碍较小的颗粒在颗粒与谷物之间的接触附近重新夹带,并可能提供其他附着点

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