论文标题
最初加热的无柄液滴的蒸发以及在环境温度下固定的底物上产生的干胶体沉积物
Evaporation of initially heated sessile droplets and the resultant dried colloidal deposits on substrates held at ambient temperature
论文作者
论文摘要
本研究通过实验和数字研究了水胶体缝线液滴的干燥沉积物的蒸发和结果模式,当液滴最初升至高温之前,然后将其放置在固定在环境温度下的底物上。然后,该系统将自然蒸发释放,而无需应用任何外部扰动。红外热仪和光学文献学分别用作界面温度测量的必需工具和咖啡环尺寸的定量。最初,一旦液滴沉积在底物上,就会沿着液态气体界面存在明显的温度梯度,从而触发了从液滴沿液滴沿液态 - 气体界面朝着接触线的Marangoni应力诱导的再循环流。因此,流动与常规底物加热情况下的流动相反。有趣的是,该温度梯度迅速衰减 - 在总蒸发时间的前10%,而液滴 - 基底系统在此后与周围环境达到热平衡。尽管温度梯度快速衰减,但咖啡环尺寸显着减小,导致内部沉积物。这种对咖啡环效应的抑制归因于以下事实:即使在界面温度梯度消失之后,最初的Marangoni应力诱导的再循环一直持续到蒸发的最后阶段。这本质上是液体惯性的结果。总体而言,与新的实验条件一起,本研究揭示了Marangoni应力诱导的干液中流动的独特性质及其在影响相关胶体沉积物中的作用,这是先前未探索的。
The present study experimentally and numerically investigates the evaporation and resultant patterns of dried deposits of aqueous colloidal sessile droplets, when the droplets are initially elevated to a high temperature before being placed on a substrate held at ambient temperature. The system is then released for natural evaporation without applying any external perturbation. Infrared thermography and optical profilometry were used as essential tools for interfacial temperature measurements and quantification of the coffee-ring dimensions, respectively. Initially, a significant temperature gradient exists along the liquid-gas interface as soon as the droplet is deposited on the substrate which triggers a Marangoni stress-induced recirculation flow directed from the top of the droplet towards the contact line along the liquid-gas interface. Thus, the flow is in the reverse direction to that seen in the conventional substrate heating case. Interestingly, this temperature gradient decays rapidly -- within the first 10% of the total evaporation time and the droplet-substrate system reaches thermal equilibrium with ambient thereafter. Despite fast decay of the temperature gradient, the coffee-ring dimensions significantly diminish, leading to an inner deposit. This suppression of the coffee-ring effect is attributed to the fact that the initial Marangoni stress-induced recirculation flow continues until the last stage of the evaporation, even after the interfacial temperature gradient vanishes. This is essentially a consequence of liquid inertia. Overall, together with a new experimental condition, the present investigation discloses a distinct nature of Marangoni stress-induced flow in the drying droplet and its role in influencing the associated colloidal deposits, which was not explored previously.