Molecular Structure of Salt Solutions:  A New View of the Interface with Implications for Heterogeneous Atmospheric Chemistry

2001 ◽  
Vol 105 (43) ◽  
pp. 10468-10472 ◽  
Author(s):  
Pavel Jungwirth ◽  
Douglas J. Tobias

2012 ◽  
Vol 116 (24) ◽  
pp. 6312-6316 ◽  
Author(s):  
D. J. Donaldson ◽  
M. Ammann ◽  
T. Bartels-Rausch ◽  
U. Pöschl


2002 ◽  
Vol 8 (2) ◽  
pp. 131-138 ◽  
Author(s):  
G.B. Pronchev ◽  
I.A. Korobeinikova ◽  
A.N. Yermakov

The application of fast-atom bombardment (FAB) mass spectrometry to solving the problems of heterogeneous atmospheric chemistry is briefly reviewed. The method is useful in studying the state of surfaces and molecules adsorbed thereon and looks appropriate in investigations of the dynamics and mechanisms of chemical reactions occurring both on a surface and in a volume of moving particulate matter suspended in a gas. It was shown that composition of atmospheric aerosols and components dissolved in atmospheric water (clouds, fogs, mists etc.) can be determined by the FAB technique. The given method, as was found in our investigations, allows the discrimination of ferrous and ferric ions. Detection limits for concentrations of H2SO4 and Fe(II / III) ions as essential components of atmospheric water determined in model experiments are established at the level of 10−6 M.



2001 ◽  
Vol 89 (11-12) ◽  
Author(s):  
M. Amman

Current techniques aiming to study heterogeneous atmospheric chemistry under realistic conditions are often subject to restrictions caused by the low amount of processed material, the complex composition of gas and condensed phases and interference issues. The use of the short-lived tracer



Author(s):  
C. E. Kolb ◽  
Douglas R. Worsnop ◽  
M. S. Zahniser ◽  
W. J. De Bruyn ◽  
Jeffrey A. Shorter ◽  
...  






1983 ◽  
Vol 17 (5) ◽  
pp. 1039
Author(s):  
James P. Lodge


2005 ◽  
Vol 39 (23) ◽  
pp. 9009-9015 ◽  
Author(s):  
Rebecca Sutton ◽  
Garrison Sposito


Author(s):  
John Evans

The pressure on planetary resources is substantially driven by increases in energy demands that have been mostly met by the combustion of fossil fuels. The basis of the warming in the troposphere is explained starting from the molecular structure of atmospheric components and their resulting rotational and vibrational spectra. From the absorptions in the infrared, the radiative efficiencies of atmospheric gases can be established. The residence times of gases in the atmosphere is explained on the basis of their atmospheric chemistry. Taking these factors together with atmospheric concentrations, the Global-Warming and -Temperature Potentials can be derived. The overall energy balance in the atmosphere is shown and the resulting net radiative forcing. The principle of the sustainability triangle is explained showing that reduction in radiative forcing may be achievable by a summation of contributions.



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