Nitric acid uptake by sulfuric acid solutions under stratospheric conditions : determination of Henry's law solubility

A Knudsen cell flow reactor is used to study the uptake of nitric acid by sulfuric acid solutions representative of stratospheric particulate. Henry's law solubility constants are determined using the time dependence of the measured nitric acid uptake efficiencies. Solubilities are reported for sulfuric acid solutions ranging from 58 to 87 weight percent sulfuric acid over a temperature range from 188 to 240 K. In general, the solubility of nitric acid increases with decreasing sulfuric acid concentration and decreasing temperature. Over the reported temperature range the solubilities are cast in the form H* = A exp(B/T), where A = 7.47 × 10−8 M/atm, B = 7.16 × 103 K for 58% H2SO4; A = 0.202 M/atm, B = 3.19 × 103 K for 66% H2SO4; A = 8.54 × 10−3 M/atm, B = 3.55 × 103 K for 74% H2SO4; and A = 3.56 × 10−3 M/atm, B = 3.32 × 103 K for 87% H2SO4. The measured solubilities indicate that nitric acid in the global stratosphere will be found predominantly in the gas phase. The ratio of condensed to gas phase nitric acid is less than 10−4 even under conditions of highly elevated sulfuric acid loading.

[1]  D. Golden,et al.  Heterogeneous Reactions on Model Polar Stratospheric Cloud Surfaces: Reaction of N2O5 on Ice and Nitric Acid Trihydrate. , 1990 .

[2]  M. Zahniser,et al.  Uptake of HCl molecules by aqueous sulfuric acid droplets as a function of acid concentration , 1990 .

[3]  Quinlan,et al.  Heterogeneous reactions on model polar stratospheric cloud surfaces: reaction of dinitrogen pentoxide on ice and nitric acid trihydrate , 1990 .

[4]  M. McCormick,et al.  Implications of AAOE observations for proposed chemical explanations of the seasonal and interannual behavior of Antarctic ozone , 1989 .

[5]  David W. Fahey,et al.  Measurements of nitric oxide and total reactive nitrogen in the Antarctic stratosphere: Observations and chemical implications , 1989 .

[6]  C. B. Farmer,et al.  Nitrogen and chlorine species in the spring Antarctic stratosphere - Comparison of models with Airborne Antarctic Ozone Experiment observations , 1989 .

[7]  C. B. Farmer,et al.  Lagrangian photochemical modeling studies of the 1987 Antarctic spring vortex: 1. Comparison with AAOE observations , 1989 .

[8]  S. Solomon,et al.  Ozone destruction through heterogeneous chemistry following the eruption of El Chichón , 1989 .

[9]  M. Zahniser,et al.  The temperature dependence of mass accommodation of sulfur dioxide and hydrogen peroxide on aqueous surfaces , 1989 .

[10]  M. Mozurkewich,et al.  Reaction probability of N2O5 on aqueous aerosols , 1988 .

[11]  S. Wofsy,et al.  Influence of polar stratospheric clouds on the depletion of Antarctic ozone , 1988 .

[12]  M. Leu Heterogeneous reactions of N2O5 with H2O and HCl on ice surfaces: Implications for Antarctic ozone depletion , 1988 .

[13]  David M. Golden,et al.  Heterogeneous interactions of chlorine nitrate, hydrogen chloride, and nitric acid with sulfuric acid surfaces at stratospheric temperatures , 1988 .

[14]  M. Kurylo,et al.  Present state of knowledge of the upper atmosphere 1988: An assessment report , 1988 .

[15]  D. Golden,et al.  Antarctic Ozone Depletion Chemistry: Reactions of N2O5 with H2O and HCl on Ice Surfaces , 1988, Science.

[16]  M. Ko,et al.  Antarctic chlorine chemistry: Possible global implications , 1988 .

[17]  Stanley C. Solomon,et al.  The mystery of the Antarctic Ozone “Hole” , 1988 .

[18]  E. W. Pearson,et al.  Laboratory Studies of Sticking Coefficients and Heterogeneous Reactions Important in the Antarctic Stratosphere (Paper 7L6697) , 1988 .

[19]  D. Golden,et al.  Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures , 1987, Science.

[20]  M. Molina,et al.  Antarctic Stratospheric Chemistry of Chlorine Nitrate, Hydrogen Chloride, and Ice: Release of Active Chlorine , 1987, Science.

[21]  M. Molina,et al.  Production of Cl2O2 from the self-reaction of the ClO radical , 1987 .

[22]  P. Crutzen,et al.  Nitric acid cloud formation in the cold Antarctic stratosphere: a major cause for the springtime ‘ozone hole’ , 1986, Nature.

[23]  S. Wofsy,et al.  Antarctic O3: Chemical mechanisms for the spring decrease , 1986 .

[24]  R. Turco,et al.  Condensation of HNO3 and HCl in the winter polar stratospheres , 1986 .

[25]  S. Wofsy,et al.  Reductions of Antarctic ozone due to synergistic interactions of chlorine and bromine , 1986, Nature.

[26]  R. Garcia,et al.  On the atmospheric photochemistry of nitric acid , 1986 .

[27]  S. Solomon,et al.  On the depletion of Antarctic ozone , 1986, Nature.

[28]  Stephen E. Schwartz,et al.  Mass-Transport Considerations Pertinent to Aqueous Phase Reactions of Gases in Liquid-Water Clouds , 1986 .

[29]  Michel Boudart,et al.  Kinetics of Heterogeneous Catalytic Reactions , 1984 .

[30]  M. P. McCormick,et al.  The Formation of Polar Stratospheric Clouds , 1983 .

[31]  A. Harker,et al.  Kinetics of the Heterogeneous Hydrolysis of Dinitrogen Pentoxide over the Temperature Range 214-263 K. , 1981 .

[32]  R. Battino,et al.  Low-pressure solubility of gases in liquid water , 1977 .

[33]  P. Hamill,et al.  H2SO4-HNO3-H2O ternary system in the stratosphere , 1974, Nature.

[34]  David M. Golden,et al.  Very Low-Pressure Pyrolysis (VLPP); A Versatile Kinetic Tool , 1973 .

[35]  E. Sacher,et al.  NITRIC ACID EQUILIBRIA IN WATER—SULFURIC ACID1 , 1961 .

[36]  John Howard Perry,et al.  Chemical Engineers' Handbook , 1934 .