Influence of aerosol copper on HO<sub>2</sub> uptake: A novel parameterized equation
Abstract. The heterogeneous uptake of hydroxyl peroxy radicals (HO2) on aerosol has been proposed to be a significant sink of HOx, thus could influence the atmospheric oxidation capacity. Accurate calculation of the uptake coefficient γHO2 is the key to quantifying its atmospheric effects. Laboratory studies show that γHO2 varies by orders of magnitude due to change in aerosol properties, especially those of aerosol soluble copper (Cu) and aerosol liquid water content (ALWC). In this study, we develop a state-of-the-art model to simulate both gas and aerosol phase chemistry. A novel parameterized equation of HO2 considering change in RH and aerosol Cu is developed based on model optimization toward all available lab experiments. 1 / γ = 1 / α + (3 × v) / (4 × 106 × Rd Hcorr RT × (5.87 + 3.2 × ln(ALWC / [PM] + 0.067)) × [PM]−0.2 × [Cu2+]0.65) According to the new equation, highly variable HO2 uptake coefficients (median value ∼0.1) were diagnosed for North China Plain and the impact of HO2 uptake on the ROx budget is assessed.