Hoffmann, M. R. and Colussi, A. J. (2010) Proton availability at the air/aerosol/water interface. In: International Chemical Congress of Pacific Basin Societies (Pacifichem 2010), December 15-20, 2010, Honolulu, HI. http://resolver.caltech.edu/CaltechAUTHORS:20120816-084429838
Full text not available from this repository.
Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20120816-084429838
The acidity of the water surface of aquated aerosols is examd. in expts. in which the uptake of gaseous trimethylamine, TMA, as TMAH+ on the surface of aquated aerosols is monitored via online electrospray mass spectrometry as a function of bulk pH, pHb. TMAH+ signal intensities track pHb along a titrn. curve displaying an equivalence point at pHb = 3.2, instead of the pKa(TMA) = 10.0 value measured on aq. TMA-HCl microdroplets. Inert X+ (X = Li, Na) cations, however, catalyze TMA uptake at pHb 4. The direct kinetic hydrogen isotope effects (1 < TMAH+/TMAD+ < 3.5 on H2O/D2O microdroplets) assocd. with TMA uptake enhancements reveal that they are driven by the competitive protonation (vs. desorption) of interfacial TMA. These outcomes are consistent with thermochem. data on gas-phase clusters showing that TMA can be protonated by the stronger acid H2O only after extensive solvation, but readily so by H3O+ or small (H2O)n.4Li+ clusters at the interface. We infer that protons become available at the aerial interface of neat water about its isoelec. point pIw = 3.2 rather than below pHb 7, and over broader pHb ranges in the presence of other cations.
|Item Type:||Conference or Workshop Item (Paper)|
|Additional Information:||© 2012 American Chemical Society.|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Tony Diaz|
|Deposited On:||16 Aug 2012 18:41|
|Last Modified:||16 Aug 2012 18:41|
Repository Staff Only: item control page