Relative Order of Sulfuric Acid, Bisulfate, Hydronium, and Cations at the Air鈥揥ater Interface
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- 作者：Wei Hua ; Dominique Verreault ; Heather C. Allen
- 刊名：Journal of the American Chemical Society
- 出版年：2015
- 出版时间：November 4, 2015
- 年：2015
- 卷：137
- 期：43
- 页码：13920-13926
- 全文大小：481K
- ISSN：1520-5126
文摘
Sulfuric acid (H2SO4), bisulfate (HSO4鈥?/sup>), and sulfate (SO42鈥?/sup>) are among the most abundant species in tropospheric and stratospheric aerosols due to high levels of atmospheric SO2 emitted from biomass burning and volcanic eruptions. The air/aqueous interfaces of sulfuric acid and bisulfate solutions play key roles in heterogeneous reactions, acid rain, radiative balance, and polar stratospheric cloud nucleation. Molecular-level knowledge about the interfacial distribution of these inorganic species and their perturbation of water organization facilitates a better understanding of the reactivity and growth of atmospheric aerosols and of the aerosol surface charge, thus shedding light on topics of air pollution, climate change, and thundercloud electrification. Here, the air/aqueous interface of NaHSO4, NH4HSO4, and Mg(HSO4)2 salt solutions as well as H2SO4 and HCl acid solutions are investigated by means of vibrational sum frequency generation (VSFG) and heterodyne-detected (HD) VSFG spectroscopy. VSFG spectra of all acid solutions show higher SFG response in the OH-bonded region relative to neat water, with 1.1 M H2SO4 being more enhanced than 1.1 M HCl. In addition, VSFG spectra of bisulfate salt solutions highly resemble that of the dilute H2SO4 solution (0.26 M) at a comparable pH. HD-VSFG (Im 蠂(2)) spectra of acid and bisulfate salt solutions further reveal that hydrogen-bonded water molecules are oriented preferentially toward the bulk liquid phase. General agreement between Im 蠂(2) spectra of 1.1 M H2SO4 and 1.1 M HCl acid solutions indicate that HSO4鈥?/sup> ions have a similar surface preference as that of chloride (Cl鈥?/sup>) ions. By comparing the direction and magnitude of the electric fields arising from the interfacial ion distributions and the concentration of each species, the most reasonable relative surface preference that can be deduced from a simplified model follows the order H3O+ > HSO4鈥?/sup> > Na+, NH4+, Mg2+ > SO42鈥?/sup>. Interestingly, contrary to some other near-neutral salt solution interfaces (e.g., chlorides and nitrates), cation-specific effects are here overshadowed by hydronium ions.