论文标题

液滴蒸发的耦合级别集和流体量(I-CLSVOF)框架的改进

An improved Coupled Level Set and Volume of Fluid (i-CLSVoF) framework for droplet evaporation

论文作者

Xia, Huihuang, Kamlah, Marc

论文摘要

表面张力主导的液滴蒸发无处不在,对于许多应用而言至关重要。我们提出了改进的耦合级别集和流体(I-CLSVOF)框架的体积,而无需显式接口重建,用于建模有或没有蒸发的微型液滴。在I-CLSVOF框架中,开发和实现了一个改进的表面张力模型,该模型具有其他过滤步骤,以滤波非物理伪造的速度。提出了一种简单但有效的基于速度的方法,以重建无差异速度场,以使液滴蒸发过程中自由表面的对流。这种方法修复了由于界面处蒸发引起的速度跳跃而引起的数值问题。这项工作中包含的涂抹质量源方法方法可确保比非缝制方法更大的数值稳定性。在I-CLSVOF中实现了三种不同的蒸发模型(室温下恒定质量通量,热驱动的蒸发和液滴蒸发)。进行了相应的数值基准案例(大坝断裂,液滴松弛和液滴蒸发均经过不同的蒸发模型),以验证表面张力和蒸发模型。发现数值和相应的分析解决方案之间的良好一致性。在这项工作中开发的模型表明,在没有蒸发的情况下进行表面张力降低的流量进行建模时令人信服的性能。

Surface-tension-dominant droplet evaporation is ubiquitous and of importance to many applications. We present an improved Coupled Level Set and Volume of Fluid (i-CLSVoF) framework without explicit interface reconstruction for modelling micro-sized droplets with and without evaporation. In the i-CLSVoF framework, an improved surface tension force model with additional filtering steps to filter un-physical spurious velocities is developed and implemented. A simple, yet efficient, velocity-potential based approach is proposed to reconstruct a divergence-free velocity field for the advection of the free surface during droplet evaporation. This approach fixes the numerical issues resulting from the evaporation-induced velocity jump at the interface. The smeared mass source term approach incorporated in this work guarantees greater numerical stability than the non-smeared approach. Three different evaporation models (constant mass flux, thermally driven evaporation and droplet evaporation at room temperature) are implemented in the i-CLSVoF. Corresponding numerical benchmark cases (dam break, droplet relaxation and droplet evaporation subjected to different evaporation models) are conducted to validate the surface tension and the evaporation models. Good agreement between the numerical and corresponding analytical solutions is found. The model developed in this work shows convincing performance in modelling surface-tension-dominant flow with and without evaporation.

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