Nitric acid uptake by sulfuric acid solutions under stratospheric conditions: Determination of Henry's Law solubility

Journal Article · Thu Sep 20 00:00:00 EDT 1990 · Journal of Geophysical Research; (USA)

DOI:https://doi.org/10.1029/JD095iD10p16545· OSTI ID:5938045

Reihs, C M; Golden, D M; Tolbert, M A ^[1]

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1. SRI International, Menlo Park, CA (USA)

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 {times} 10{sup {minus}8} M/atm, B = 7.16 {times} 10{sup 3}K for 58% H{sub 2}SO{sub 4}; A = 0.202 M/atm, B = 3.19 {times} 10{sup 3}K for 66% H{sub 2}SO{sub 4}; A = 8.54 {times} 10{sup {minus}3} M/atm, B = 3.55 {times} 10{sup 3} K for 74% H{sub 2}SO{sub 4}; and A = 3.56 {times} 10{sup {minus}3} M/atm, B = 3.32 {times} 10{sup 3} K for 87% H{sub 2}SO{sub 4}. 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{sup {minus}4} even under conditions of highly elevated sulfuric acid loading.

• OSTI ID: 5938045
• Journal Information: Journal of Geophysical Research; (USA), Vol. 95:D10; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
NITRIC ACID
SOLUBILITY
STRATOSPHERE
ATMOSPHERIC CHEMISTRY
SULFURIC ACID
SOLVENT PROPERTIES
CLOUDS
GASES
KNUDSEN FLOW
LOW TEMPERATURE
PARTICULATES
PHASE STUDIES
PHOTOCHEMICAL REACTIONS
QUANTITY RATIO
TEMPERATURE DEPENDENCE
TIME DEPENDENCE
CHEMICAL REACTIONS
CHEMISTRY
EARTH ATMOSPHERE
FLUID FLOW
FLUIDS
GAS FLOW
HYDROGEN COMPOUNDS
INORGANIC ACIDS
PARTICLES
540110*