The effect of moisture on volatile organic chemical gas-to-particle partitioning with atmospheric aerosols—competitive adsorption theory predictions

1991 ◽  
Vol 25 (8) ◽  
pp. 1649-1656 ◽  
Author(s):  
L.J. Thibodeaux ◽  
K.C. Nadler ◽  
K.T. Valsaraj ◽  
D.D. Reible
Author(s):  
Hind A. A. Al-Abadleh

Extensive research has been done on the processes that lead to the formation of secondary organic aerosol (SOA) including atmospheric oxidation of volatile organic compounds (VOCs) from biogenic and anthropogenic...


Chemosphere ◽  
2021 ◽  
pp. 131288
Author(s):  
Hamid Rajabi ◽  
Mojgan Hadi Mosleh ◽  
Tirto Prakoso ◽  
Negin Ghaemi ◽  
Parthasarathi Mandal ◽  
...  

2015 ◽  
Vol 12 (2) ◽  
pp. 236 ◽  
Author(s):  
Cristina Iuga ◽  
C. Ignacio Sainz-Díaz ◽  
Annik Vivier-Bunge

Environmental context The presence of air-borne mineral dust containing silicates in atmospheric aerosols should be considered in any exploration of volatile organic compound chemistry. This work reports the mechanisms, relative energies and kinetics of free-radical reactions with formic acid adsorbed on silicate surface models. We find that silicate surfaces are more likely to act as a trap for organic radicals than to have a catalytic effect on their reactions. Abstract Heterogeneous reactions of atmospheric volatile organic compounds on aerosol particles may play an important role in atmospheric chemistry. Silicate particles are present in air-borne mineral dust in atmospheric aerosols, and radical reactions can be different in the presence of these mineral particles. In this work, we use quantum-mechanical calculations and computational kinetics to explore the reaction of a hydroxyl free radical with a formic acid molecule previously adsorbed on several models of silicate surfaces. We find that the reaction is slower and takes place according to a mechanism that is different than the one in the gas phase. It is especially interesting to note that the reaction final products, which are the formyl radical attached to the cluster surface, and a water molecule, are much more stable than those formed in the gas phase, the overall reaction being highly exothermic in the presence of the surface model. This suggests that the silicate surface is a good trap for the formed formyl radical. In addition, we have noted that, if a second hydroxyl radical approaches the adsorbed formyl radical, the formation of carbonic acid on the silicate surface is a highly exothermic and exergonic process. The carbonic acid molecule remains strongly attached to the surface, thus blocking CO2 formation in the formic acid oxidation reaction. The spectroscopic properties of the systems involved in the reaction have been calculated, and interesting frequency shifts have been identified in the main vibration modes.


1996 ◽  
Vol 30 (4) ◽  
pp. 1081-1091 ◽  
Author(s):  
David R. Unger ◽  
Thientu T. Lam ◽  
Charles E. Schaefer ◽  
David S. Kosson

2004 ◽  
Vol 4 (2) ◽  
pp. 557-562 ◽  
Author(s):  
M. Kulmala ◽  
T. Suni ◽  
K. E. J. Lehtinen ◽  
M. Dal Maso ◽  
M. Boy ◽  
...  

Abstract. The possible connections between the carbon balance of ecosystems and aerosol-cloud-climate interactions play a significant role in climate change studies. Carbon dioxide is a greenhouse gas, whereas the net effect of atmospheric aerosols is to cool the climate. Here, we investigated the connection between forest-atmosphere carbon exchange and aerosol dynamics in the continental boundary layer by means of multiannual data sets of particle formation and growth rates, of CO2 fluxes, and of monoterpene concentrations in a Scots pine forest in southern Finland. We suggest a new, interesting link and a potentially important feedback among forest ecosystem functioning, aerosols, and climate: Considering that globally increasing temperatures and CO2 fertilization are likely to lead to increased photosynthesis and forest growth, an increase in forest biomass would increase emissions of non-methane biogenic volatile organic compounds and thereby enhance organic aerosol production. This feedback mechanism couples the climate effect of CO2 with that of aerosols in a novel way.


2004 ◽  
Vol 130 (10) ◽  
pp. 1210-1216 ◽  
Author(s):  
Wei-Han Tao ◽  
Thomas C.-K. Yang ◽  
Yaw-Nan Chang ◽  
Li-Kai Chang ◽  
Tsair-Wang Chung

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