Beijing International Center for Gas Hydrate, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China; College of Engineering, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China; Department of Mechanical Engineering, City University of Hong Kong, Tat Chee Avenue, Kowloon, Hong Kong 999077, China.
Beijing International Center for Gas Hydrate, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China; School of Physics, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China.
J Colloid Interface Sci. 2022 Feb;607(Pt 2):1699-1708. doi: 10.1016/j.jcis.2021.09.047. Epub 2021 Sep 16.
Quartz is one of the most common but important minerals, and its wettability plays a significant role in affecting various natural and industrial processes. Studies have revealed that different crystal faces of quartz are with different wettabilities, but its mechanism is still vague.
For specifying the mechanism of crystal face dependent wettability, the contact angles of three different liquids on the crystal faces of α-quartz are measured; the time-of-flight secondary ion mass spectrometry (ToF-SIMS) is employed to establish the crystal surface models; molecular dynamics (MD) simulations with the surface models are performed to understand the wetting behavior at molecular scale.
Based on the contact angle measurements, the wettabilities of different crystal faces of α-quartz are found different, which can be directly attributed to the concentration of hydroxyl group on crystal faces based on ToF-SIMS results. MD simulations yield consistent results with the contact angle order recognized from experiments, revealing that the surface hydroxyl group controls the wettability of α-quartz crystal faces. It is also recognized that the pristine surface atomic arrangement, especially the surface concentration of unsaturated bond (an intrinsic property of α-quartz), is the intrinsic cause of the difference in the concentration of hydroxyl group of the crystal surface.
石英是最常见也是最重要的矿物之一,其润湿性在影响各种自然和工业过程中起着重要作用。研究表明,石英的不同晶面具有不同的润湿性,但其中的机制尚不清楚。
为了明确晶面依赖润湿性的机制,我们测量了三种不同液体在α-石英晶面上的接触角;采用飞行时间二次离子质谱(ToF-SIMS)建立晶体表面模型;利用表面模型进行分子动力学(MD)模拟,以了解分子尺度上的润湿行为。
基于接触角测量,我们发现α-石英不同晶面的润湿性不同,这可以直接归因于 ToF-SIMS 结果中晶面上羟基的浓度。MD 模拟得出的结果与实验中识别的接触角顺序一致,表明表面羟基控制着α-石英晶面的润湿性。我们还认识到,原始表面原子排列,特别是不饱和键的表面浓度(α-石英的固有特性),是晶面羟基浓度差异的内在原因。