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Water surface is acidic

V. Buch*Fritz Haber Institute for Molecular Dynamics, Hebrew University, Jerusalem 91904, Israel;Anne MiletDépartement de Chimie Moléculaire, Unité Mixte de Recherche 5250, Centre National de la Recherche Scientifique, Université Joseph Fourier, BP53, 38041 Grenoble, France;Robert VáchaInstitute of Organic Chemistry and Biochemistry, Academy of Sciences Sciences of the Czech Republic and Center for Biomolecules and Complex Molecular Systems, 16610 6 Prague, Czech Republic; andPavel JungwirthInstitute of Organic Chemistry and Biochemistry, Academy of Sciences Sciences of the Czech Republic and Center for Biomolecules and Complex Molecular Systems, 16610 6 Prague, Czech Republic; andJ. Paul DevlinDepartment of Chemistry, Oklahoma State University, Stillwater, OK 74078
2007en
ABI

Annotatsiya

Water autoionization reaction 2H2O --> H3O- + OH- is a textbook process of basic importance, resulting in pH = 7 for pure water. However, pH of pure water surface is shown to be significantly lower, the reduction being caused by proton stabilization at the surface. The evidence presented here includes ab initio and classical molecular dynamics simulations of water slabs with solvated H3O+ and OH- ions, density functional studies of (H2O)(48)H+ clusters, and spectroscopic isotopic-exchange data for D2O substitutional impurities at the surface and in the interior of ice nanocrystals. Because H3O+ does, but OH- does not, display preference for surface sites, the H2O surface is predicted to be acidic with pH < 4.8. For similar reasons, the strength of some weak acids, such as carbonic acid, is expected to increase at the surface. Enhanced surface acidity can have a significant impact on aqueous surface chemistry, e.g., in the atmosphere.

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