Xi Zhang, Xiandong Liu, Yingchun Zhang, Xiancai Lu
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Interfacial structure and acidity of orthoclase (001) surface: understanding the effect of surface metal cation
Surface acid chemistry is central to interfacial properties of orthoclase. In this study, we report a first principles molecular dynamics (FPMD) study of interfacial structures and acid constants (pKa) of orthoclase (001) with the presence of Na+/K+ cation on the surface. Detailed structural analyses show that Na+ and K+ show similar coordination structures on the surface while the exchange of Na+ for K+ hardly changes hydration structures of surface groups. The surface groups (i.e., ≡SiOH, ≡AlOH, and ≡AlOH2) have pKas of 11.5, 18.5, and 7.8 with K+ on the surface and 5.5, 17.7, and 4.3 with Na+ on the surface, respectively. FPMD derived pKas indicate that with K+ on the surface ≡AlOH2 is the only active group in the common pH range while Na+ decreases surface pKas of surface groups, that makes ≡AlOH2 and ≡SiOH active. Based on the pKas, we derive a PZC (point of zero charge) of 9.7 and 4.9 for orthoclase (001) with surface K+ and Na+, respectively. This means that Na+ significantly enhances surface acid reactivity. The implication for understanding geochemical properties of orthoclase was discussed with the focus on surface complexation of metal cations.
期刊介绍:
American Mineralogist: Journal of Earth and Planetary Materials (Am Min), is the flagship journal of the Mineralogical Society of America (MSA), continuously published since 1916. Am Min is home to some of the most important advances in the Earth Sciences. Our mission is a continuance of this heritage: to provide readers with reports on original scientific research, both fundamental and applied, with far reaching implications and far ranging appeal. Topics of interest cover all aspects of planetary evolution, and biological and atmospheric processes mediated by solid-state phenomena. These include, but are not limited to, mineralogy and crystallography, high- and low-temperature geochemistry, petrology, geofluids, bio-geochemistry, bio-mineralogy, synthetic materials of relevance to the Earth and planetary sciences, and breakthroughs in analytical methods of any of the aforementioned.