Department of Applied Mathematics, Research School of Physics and Engineering, The Australian National University, Canberra, ACT 0200, Australia.
Faraday Discuss. 2010;146:141-51; discussion 195-215, 395-403. doi: 10.1039/b924965f.
We present an investigation of the change in wettability of water droplets on 3 different flat, smooth substrates with an elevation in temperature. Two methods were employed. In the first method the droplet was placed on the substrate before it was heated and in the second method the droplets were induced to fall onto a preheated substrate. We find that the intrinsic wettability of the surface is important and that fundamentally different behavior is observed on a hydrophobic surface relative to hydrophilic surfaces. For the hydrophobic surface and employing the first method, we have observed three different regimes over the temperature range of 65 degrees C to 270 degrees C. In regime I (65 degrees C to 110 degrees C), the contact angle of water droplets exhibit a slight decrease from 108 degrees to 105 degrees and an accompanying significant decrease in droplet lifetime (tau) from approximately 111 s to approximately 30 s is observed. In regime II (120 degrees C to 190 degrees C), tau remains constant at approximately 20 s however the contact angle significantly increases from 127 degrees to 158 degrees--that is we enter a superhydrophobic regime on a flat surface. In this regime the droplet remains stationary on the surface. Regime III (210 degrees C to 270 degrees C), is the Leidenfrost regime in which the water droplet exhibits a rapid motion on the solid surface with a contact angle higher than 160 degrees. In comparison, the wetting behavior of a water droplet on two relatively hydrophilic surfaces (Au and GaAs) have also been investigated as a function of temperature. Here no wetting transition is observed from 65 degrees C up to 365 degrees C. In the second method, the wetting behavior on the hydrophobic surface is similar to that observed in the first method for temperatures below the Leidenfrost temperature and the water droplet rebounds from the solid surface at higher temperatures. Additionally, the Leidenfrost phenomenon can be observed above 280 degrees C for the hydrophilic surfaces.
我们研究了在温度升高的情况下,3 种不同的平整、光滑基底上水滴润湿性的变化。我们采用了两种方法。在第一种方法中,将基底加热前,将液滴滴在基底上;在第二种方法中,液滴被诱导落在预热基底上。我们发现,表面的固有润湿性很重要,在疏水表面相对于亲水表面,观察到完全不同的行为。对于疏水表面,并采用第一种方法,我们在 65°C 至 270°C 的温度范围内观察到三种不同的状态。在状态 I(65°C 至 110°C)中,水滴滴的接触角从 108°略微下降到 105°,同时液滴寿命(τ)从大约 111 秒显著下降到大约 30 秒。在状态 II(120°C 至 190°C)中,τ保持在大约 20 秒不变,但接触角从 127°显著增加到 158°——即在平坦表面上进入超疏水状态。在这个状态下,液滴停留在表面上。状态 III(210°C 至 270°C)是莱顿弗罗斯特状态,其中水滴滴在固体表面上快速运动,接触角大于 160°。相比之下,作为温度函数,我们还研究了两个相对亲水表面(Au 和 GaAs)上水滴的润湿行为。在这里,从 65°C 到 365°C 没有观察到润湿转变。在第二种方法中,在莱顿弗罗斯特温度以下,疏水表面的润湿行为与第一种方法中观察到的相似,并且在较高温度下,水滴从固体表面反弹。此外,在亲水表面上,莱顿弗罗斯特现象可以在 280°C 以上观察到。