Atmospheric
cloud, fog and aerosol microdroplets are more acidic
than previously assumed. The fact that interfacial reactions on microdroplets
are faster than anticipated has enhanced their role in atmospheric
chemistry and raised the question of whether their interfaces are
more or less acidic than the bulk phase. It turns out that acidity
and its pH dependence sharply change across interfacial layers. Surface-specific
experiments show that the protonations of gas-phase molecules at the
outermost layer (OTL) of aqueous microdroplets are very different
from those dissolved in deeper layers. Trimethylamine (TMA) is protonated,
whereas the weak base isoprene (ISO) is not as expected, when dissolved
in pH < pK
a(TMA) = 9.8 microdroplets.
In dramatic contrast, both gas-phase TMA and ISO are protonated at
the OTL of pH < 4 microdroplets. Because ISO is only protonated
in concentrated acids H3O+ ions at the OTL of
pH < 4 microdroplets are superacidic. Conversely, the OTL of pH
> 4 microdroplets lacks the H3O+ ions that
protonate
TMA in deeper layers. H3O+ ions become more
acidic toward the surface (i.e., the free energies of proton transfer,
H3O+ + B = H2O + BH+,
become more negative) because hydration losses in lower density OTL
water destabilize the small H3O+ ion relative
to the larger protonated bases BH+. Because the OTL behaves
as neutral at pH ∼ 4 (i.e., its pK
w ∼ 8) interfacial water may be more dissociated than in the
bulk. In short, the acidity of aqueous microdroplets probed by gas-phase
molecules at the OTL is different from the acidity experienced by
solutes in deeper layers and should not be confused with pH, which
represents the uniform thermodynamic activity rather than the local
acidities of H3O+ ions as a function of depth.
These concepts should become standard in interfacial atmospheric
chemistry.