2004
DOI: 10.1016/j.cocis.2004.05.028
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Propensity of soft ions for the air/water interface

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Cited by 209 publications
(409 citation statements)
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“…(Fig. 2.) Whereas a fully charged iodide anion in nonpolarizable models of this kind exhibits little or no affinity for the liquid-vapor interface (30), the average concentration of I Ϫ3/4 in the interfacial region rises more than 90-fold over its bulk value. Fully charged cations exhibit still less affinity than nonpolarizable monovalent anions; by contrast, I ϩ3/4 is nearly 5ϫ more concentrated at z Ϸz Gibbs than in bulk.…”
Section: Resultsmentioning
confidence: 99%
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“…(Fig. 2.) Whereas a fully charged iodide anion in nonpolarizable models of this kind exhibits little or no affinity for the liquid-vapor interface (30), the average concentration of I Ϫ3/4 in the interfacial region rises more than 90-fold over its bulk value. Fully charged cations exhibit still less affinity than nonpolarizable monovalent anions; by contrast, I ϩ3/4 is nearly 5ϫ more concentrated at z Ϸz Gibbs than in bulk.…”
Section: Resultsmentioning
confidence: 99%
“…We plot the average solute concentration relative to its value deep within bulk solution, c(z) ϭ ͳ ion (z)ʹ/ bulk , as a function of solute height z. For the case ( * ion ϭ 1.5, q* ion ϭ Ϯ7), ion density rises at the interface to a value nearly 3ϫ that in bulk, rivaling the largest magnitudes of surface enhancement reported for computer simulations of atomic ions in water (30). As in the case of hydrated halide anions, adsorption can be suppressed entirely by a modest reduction in solute size, as shown for ( * ion ϭ 1.25, q* ion ϭ Ϯ7).…”
Section: Resultsmentioning
confidence: 99%
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“…In addition, there are also inorganic sources of iodine. For example, the direct photochemical oxidation if iodide at the sea-air interface (Miyake & Tsunogai 1963) is likely to be an important source as is the oxidation by ozone of seawater iodide, followed by the release of I 2 into the gas phase (Vrbka et al 2004). The latter mechanism depends on ozone deposition at the ocean surface and the production of I 2 must take place at the air-sea interface for volatilization to occur.…”
Section: Secondary Aerosol Formation From Iodine Vapoursmentioning
confidence: 99%
“…), i.e., the specific local properties of the liquid were by no means taken into account; here we speak about the dipole moments and polarizabilities of molecules, and their sizes. The subsequent numerous theoretical works allowed for the geometrical characteristics of water molecule [27], numerical MD simulation in the view of the effect of polarization of water molecules [28][29][30][31][32][33][34][35][36][37][38], and also series of experimental results including vibrational sum frequency generation spectroscopy [39][40][41][42][43][44], second harmonic generation spectroscopy [45,46], high-pressure VUV photoelectron spectroscopy [47,48], and X-ray photoelectron spectroscopy combined with scanning electron microscopy [49,50] allow us to make a conclusion about an opportunity of adsorption of some anions, for example, Cl − , I − and Br − on the watergas interface. The fact that basically negative ions are capable of adsorption at this interface is also supported by the data obtained in Ref.…”
Section: Statement Of the Problem Introductionmentioning
confidence: 99%