Journal
CHEMPHYSCHEM
Volume 13, Issue 1, Pages 323-329Publisher
WILEY-V C H VERLAG GMBH
DOI: 10.1002/cphc.201100558
Keywords
atmospheric chemistry; density functional calculations; formic acid; gas-phase reactions; reaction mechanisms
Funding
- Science and Technology Foundation of GuiZhou Province, China [2011-2107]
- National Natural Science Foundation of China [41165007]
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The formic acid catalyzed gas-phase reaction between H2O and SO3 and its reverse reaction are respectively investigated by means of quantum chemical calculations at the CCSD(T)//B3LYP/cc-pv(T+d)z and CCSD(T)//MP2/aug-cc-pv(T+d)z levels of theory. Remarkably, the activation energy relative to the reactants for the reaction of H2O with SO3 is lowered through formic acid catalysis from 15.97 kcal mol(-1) to -15.12 and -14.83 kcal mol(-1) for the formed H2O center dot center dot center dot SO3 complex plus HCOOH and the formed H2O center dot center dot center dot HCOOH complex plus SO3, respectively, at the CCSD(T)//MP2/aug-cc-pv(T+d)z level. For the reverse reaction, the energy barrier for decomposition of sulfuric acid is reduced to -3.07 kcal mol(-1) from 35.82 kcal mol(-1) with the aid of formic acid. The results show that formic acid plays a strong catalytic role in facilitating the formation and decomposition of sulfuric acid. The rate constant of the SO3+H2O reaction with formic acid is 10(5) times greater than that of the corresponding reaction with water dimer. The calculated rate constant for the HCOOH+H2SO4 reaction is about 10(-13) cm(3) molecule(-1) s(-1) in the temperature range 200-280 K. The results of the present investigation show that formic acid plays a crucial role in the cycle between SO3 and H2SO4 in atmospheric chemistry.
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