Iodine
plays a key role in tropospheric ozone destruction, atmospheric
new particle formation, as well as growth. Air–water interface
happens to be an important reaction site pertaining to such phenomena.
However, except iodide (I–), the behavior of other
iodine species, for example, triiodide (I3
–) and iodate (IO3
–, the most abundant
iodine species in seawater) at the aqueous interface and their effect
on the interfacial water are largely unknown. Using interface-specific
vibrational spectroscopy (heterodyne-detected vibrational sum frequency
generation), we recorded the imaginary-χ(2) spectra
(Imχ(2); χ(2) is the second-order
electric susceptibility in OH stretch region) of the air–water
interface in the presence of IO3
–, I3
–, and I– (≤0.3
M) in the aqueous subphase. The Imχ(2) spectra reveal
that the chaotropic I3
– is the most surface-active
anion among the iodine species studied and decreases the vibrational
coupling and hydrogen-bonding of interfacial water. Interestingly,
the IO3
–, even being a kosmotrope, is
quite prevalent in the interfacial region and preferentially orients
the interfacial water as “H-down” (i.e., water dipole
moment is pointed toward the bulk water). Mapping of the OH stretch
response of ion-affected water at interface (i.e., ΔImχ(2) = Imχ(2)
air–water−iodine salt – Imχ(2)
air–water) with
that in the hydration shell of the respective ion (hydration shell
water response is obtained by Raman multivariate curve resolution
spectroscopy) reveals a correlative link between the ion’s
influence on the interfacial water and their hydration shell structure.
The distinct water structure of stronger as well as weaker H-bonding
in the hydration shell of the polyatomic IO3
– anion promotes the anion to stay at the interfacial region. Thus,
the surface prevalence of the iodine species and their effect on the
interfacial water are perceived to be crucial for the transfer of
iodine from seawater to the atmosphere across the marine boundary
layer and the chemistry of iodine at aqueous aerosol surface.