Title of article
Sensitivity and uncertainty analysis of the mechanism of gas-phase chlorine production from NaCl aerosols in the MAGIC model
Author/Authors
Paul Nissenson، نويسنده , , Jennie L. Thomas، نويسنده , , Barbara J. Finlayson-Pitts، نويسنده , , Donald Dabdub، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2008
Pages
8
From page
6934
To page
6941
Abstract
This paper presents a global sensitivity and uncertainty analyses of the chlorine chemistry included in the Model of Aqueous, Gaseous and Interfacial Chemistry (MAGIC). Uncertainty ranges are established for input parameters (e.g. chemical rate constants, Henryʹs law constants, etc.) and are used in conjunction with Latin hypercube sampling and multiple linear regression to conduct a sensitivity analysis which determines the correlation between each input parameter and the model output. The contribution of each input parameter to the uncertainty in the model output is calculated by combining the results of the sensitivity analysis with the input parametersʹ uncertainty ranges. The peak concentration of molecular chlorine, [Cl2(g)]peak, is used to compare model runs since MAGIC has demonstrated previously the importance of an interfacial reaction between OH(g) and Cl−(aq,surface) in the production of Cl2(g). Results indicate that the interface reaction rate is most strongly correlated with [Cl2(g)]peak and is most responsible for the uncertainty in MAGICʹs ability to calculate precisely [Cl2(g)]peak. In addition, the mass accommodation coefficient for OH and the aqueous-phase reaction rate for Cl2 + OH− → HOCl + Cl− and 2CO3− + O2 + 2H2O → 2CO2•H2O + 2O2− also contribute significantly to the uncertainty in [Cl2(g)]peak.
Keywords
Interface chemistrySea-salt aerosolSensitivity analysisChlorine chemistry
Journal title
Atmospheric Environment
Serial Year
2008
Journal title
Atmospheric Environment
Record number
761299
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