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使用接触角测量法对石墨的本征润湿性进行表征:缺陷对静态和动态接触角的影响。

Characterization of the Intrinsic Water Wettability of Graphite Using Contact Angle Measurements: Effect of Defects on Static and Dynamic Contact Angles.

机构信息

Department of Chemical & Petroleum Engineering, Swanson School of Engineering, ‡Department of Chemistry, and §Department of Mechanical Engineering & Materials Science, Swanson School of Engineering, University of Pittsburgh , Pittsburgh, Pennsylvania 15260, United States.

出版信息

Langmuir. 2017 Jan 31;33(4):959-967. doi: 10.1021/acs.langmuir.6b04193. Epub 2017 Jan 20.

Abstract

Elucidating the intrinsic water wettability of the graphitic surface has increasingly attracted research interests, triggered by the recent finding that the well-established hydrophobicity of graphitic surfaces actually results from airborne hydrocarbon contamination. Currently, static water contact angle (WCA) is often used to characterize the intrinsic water wettability of graphitic surfaces. In the current paper, we show that because of the existence of defects, static WCA does not necessarily characterize the intrinsic water wettability. Freshly exfoliated graphite of varying qualities, characterized using atomic force microscopy and Raman spectroscopy, was studied using static, advancing, and receding WCA measurements. The results showed that graphite of different qualities (i.e., defect density) always has a similar advancing WCA, but it could have very different static and receding WCAs. This finding indicates that defects play an important role in contact angle measurements, and the static contact angle does not always represent the intrinsic water wettability of pristine graphite. On the basis of the experimental results, a qualitative model is proposed to explain the effect of defects on static, advancing, and receding contact angles. The model suggests that the advancing WCA reflects the intrinsic water wettability of pristine (defect-free) graphite. Our results showed that the advancing WCA for pristine graphite is 68.6°, which indicates that graphitic carbon is intrinsically mildly hydrophilic.

摘要

阐明石墨表面的本征亲水性越来越受到研究关注,这是由于最近发现石墨表面公认的疏水性实际上是源自空气中的碳氢化合物污染。目前,静态水接触角(WCA)常用于表征石墨表面的本征亲水性。在本论文中,我们表明,由于存在缺陷,静态 WCA 不一定能表征石墨的本征亲水性。使用原子力显微镜和拉曼光谱对不同质量的新鲜剥离石墨进行了研究,并用静态、前进和后退 WCA 测量法进行了测量。结果表明,不同质量(即缺陷密度)的石墨始终具有相似的前进 WCA,但静态和后退 WCA 可能有很大差异。这一发现表明,缺陷在接触角测量中起着重要作用,而静态接触角并不总是代表原始石墨的本征亲水性。基于实验结果,提出了一个定性模型来解释缺陷对静态、前进和后退接触角的影响。该模型表明,前进 WCA 反映了原始(无缺陷)石墨的本征亲水性。我们的结果表明,原始石墨的前进 WCA 为 68.6°,这表明石墨碳本质上具有轻微的亲水性。

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