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Lattice Boltzmann simulation of droplet dynamics on granular surfaces with variable wettability

机译:晶格Boltzmann模拟可变润湿性颗粒状曲面上的液滴动力学

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摘要

Soil-composing particles undergo wettability changes, impacting hydraulic and mechanical processes such as erosion and landslides. Such processes evolve at very small scales, typically at the particle level. Here we capture the evolution of liquid interfaces in a single particle and several particles with the lattice Boltzmann (LB) method. The paper presents a three-dimensional LB study on the droplet dynamics on a layer of uniformly packed spherical particles with varying size and intrinsic contact angle (CA) aimed at mimicking conditions comparable to those of real soils. The numerical droplet is initialized close to the granular surface and deposited by gravity. Three spreading and infiltration behaviors were identified: a droplet with a stable apparent CA, a droplet with a metastable apparent CA before infiltration, and immediate infiltration. The results showed that the formation of a droplet with a stable or metastable spherical-cap shape depends on the particle size and the intrinsic CA. Furthermore, the initial wetted zone expansion was found to be governed by inertial effects with its behavior characterized by a power law. Finally, the apparent CA, which is closely related to the intrinsic CA, was found to be influenced by the particle size due to a significant portion of the droplet being embedded into the granular surface for the larger particles and reducing the apparent CA. This paper provides a basis for future research targeting the behavior of droplet interaction with granular surfaces with variable intrinsic CAs (from wettable to superhydrophobic) such as soils and other granular materials for industrial applications. The numerical approach implemented can also be extended to model other dynamic processes for a droplet, such as evaporation, high-velocity impacting, and lateral sliding.
机译:土壤构成颗粒经历润湿性变化,影响液压和机械过程,如侵蚀和山体滑坡。这种过程在非常小的尺度上演化,通常在粒度下。在这里,我们在单个粒子中捕获液体界面的演变和用晶格玻璃板(LB)方法。本文呈现了具有不同尺寸和固有的球形颗粒层上的液滴动力学的三维LB研究,其尺寸和固有的固有接触角(CA)旨在模仿与真实土壤相当的条件。数值液滴靠近粒状表面初始化并通过重力沉积。鉴定了三种扩散和渗透行为:具有稳定表观Ca的液滴,渗透前具有稳定的表观Ca的液滴,并立即渗透。结果表明,具有稳定或稳定球形帽形状的液滴的形成取决于粒度和固有的CA.此外,发现最初的湿润区域扩张是通过惯性效应来控制其特征的惯性效应。最后,发现与本征Ca密切相关的表观型Ca受到粒径的影响,由于液滴的大部分液滴被嵌入到粒状表面上,并减少明显的Ca.本文为未来的研究提供了靶向液滴与颗粒表面的行为的基础,该颗粒表面具有可变的内在CAS(可润湿至超疏水),例如土壤和其他工业应用的颗粒材料。实现的数值方法也可以扩展到模拟液滴的其他动态过程,例如蒸发,高速冲击和横向滑动。

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