Amine reactivity with charged sulfuric acid clusters
BR Bzdek, DP Ridge… - Atmospheric Chemistry and …, 2011 - acp.copernicus.org
BR Bzdek, DP Ridge, MV Johnston
Atmospheric Chemistry and Physics, 2011•acp.copernicus.orgThe distribution of charged species produced by electrospray of an ammonium sulfate
solution in both positive and negative polarities is examined using Fourier transform ion
cyclotron resonance mass spectrometry (FTICR-MS). Positively-charged ammonium
bisulfate cluster composition differs significantly from negatively-charged cluster
composition. For positively-charged clusters all sulfuric acid is neutralized to bisulfate,
whereas for negatively-charged clusters the degree of sulfuric acid neutralization is cluster …
solution in both positive and negative polarities is examined using Fourier transform ion
cyclotron resonance mass spectrometry (FTICR-MS). Positively-charged ammonium
bisulfate cluster composition differs significantly from negatively-charged cluster
composition. For positively-charged clusters all sulfuric acid is neutralized to bisulfate,
whereas for negatively-charged clusters the degree of sulfuric acid neutralization is cluster …
The distribution of charged species produced by electrospray of an ammonium sulfate solution in both positive and negative polarities is examined using Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS). Positively-charged ammonium bisulfate cluster composition differs significantly from negatively-charged cluster composition. For positively-charged clusters all sulfuric acid is neutralized to bisulfate, whereas for negatively-charged clusters the degree of sulfuric acid neutralization is cluster size-dependent. With increasing cluster size (and, therefore, a decreasing role of charge), both positively- and negatively-charged cluster compositions converge toward ammonium bisulfate. The reactivity of negatively-charged sulfuric acid-ammonia clusters with dimethylamine and ammonia is also investigated by FTICR-MS. Two series of negatively-charged clusters are investigated: [(HSO4)(H2SO4)x]− and [(NH4)x(HSO4)x+1(H2SO4)3]−. Dimethylamine substitution for ammonia in [(NH4) x(HSO4) x+1(H2SO4)3]− clusters is nearly collision-limited, and subsequent addition of dimethylamine to neutralize H2SO4 to bisulfate is within one order of magnitude of the substitution rate. Dimethylamine addition to [(HSO4) (H2SO4) x]− clusters is either not observed or very slow. The results of this study indicate that amine chemistry will be evident and important only in large ambient negative ions (>m/z 400), whereas amine chemistry may be evident in small ambient positive ions. Addition of ammonia to unneutralized clusters occurs at a rate that is ~2–3 orders of magnitude slower than incorporation of dimethylamine either by substitution or addition. Therefore, in locations where amine levels are within a few orders of magnitude of ammonia levels, amine chemistry may compete favorably with ammonia chemistry.
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