Santos Jaciara C C, Negreiros Fabio R, Pedroza Luana S, Dalpian Gustavo M, Miranda Paulo B
Instituto de Física de São Carlos , Universidade de São Paulo , CP 369, São Carlos , São Paulo 13560-970 , Brazil.
Centro de Ciências Naturais e Humanas , Universidade Federal do ABC , Santo André , São Paulo 09210-580 , Brazil.
J Am Chem Soc. 2018 Dec 12;140(49):17141-17152. doi: 10.1021/jacs.8b09907. Epub 2018 Dec 3.
Water-mineral interfaces are important for several environmental, industrial, biological, and geological processes. Gypsum, CaSO·2HO, is a widespread mineral of high technological, medical, and environmental relevance, but little is known about its surface structure and its interaction with water. A molecular-level understanding of gypsum/water interface is given here by a combined experimental/theoretical study. We investigate the structure and dynamics of water adsorbed from vapor on the gypsum (010) single-crystal surface at room temperature, combining sum-frequency generation (SFG) vibrational spectroscopy experiments and ab initio molecular dynamics (AIMD) simulations. The SFG spectra of gypsum at low relative humidity (RH) show an anisotropic arrangement of structural water molecules and the presence of dangling OH groups. The AIMD simulations allow a detailed assignment of the SFG spectra and show that the cleaved (010) surface rearranges to have only 25% of the OH groups pointing away from the surface. At higher RHs, the first adsorbed water layer binds to these OH groups and forms an anisotropic arrangement, but with the amount of free OH groups significantly suppressed and without any significant diffusion. Upon adsorption of a second water layer, although the topmost layer of molecules is more disordered and dynamic than the previous one, its structure is still influenced by the gypsum surface underneath because it has a much reduced amount of free OH groups with respect to the free surface of water, and a slower surface diffusion with respect to bulk water. The theoretical results corroborate the experimental ones and provide an accurate atomic characterization of the surface structure.
水 - 矿物界面对于多种环境、工业、生物和地质过程都很重要。石膏(CaSO₄·2H₂O)是一种广泛存在的矿物,在高科技、医学和环境方面具有重要意义,但人们对其表面结构以及与水的相互作用了解甚少。本文通过实验与理论相结合的研究,从分子层面给出了对石膏/水界面的理解。我们结合和频振动光谱(SFG)实验与从头算分子动力学(AIMD)模拟,研究了室温下石膏(010)单晶表面上从气相吸附的水的结构和动力学。低相对湿度(RH)下石膏的SFG光谱显示结构水分子呈各向异性排列且存在悬垂的OH基团。AIMD模拟能够对SFG光谱进行详细归属,并表明解理后的(010)表面重新排列,使得只有25%的OH基团指向远离表面的方向。在较高相对湿度下,第一层吸附水与这些OH基团结合并形成各向异性排列,但自由OH基团的数量显著减少且没有明显扩散。吸附第二层水时,尽管最顶层分子比前一层更无序且更具动态性,但其结构仍受下方石膏表面的影响,因为相对于水的自由表面,其自由OH基团数量大幅减少,且相对于 bulk water,表面扩散较慢。理论结果证实了实验结果,并提供了表面结构的精确原子表征。