Abstract. Aerosol pH is a fundamental property of aerosols
in terms of atmospheric chemistry and its impact on air quality, climate, and
health. Precise estimation of aerosol pH in chemical transport models (CTMs)
is critical for aerosol modeling and thus influences policy development
that partially relies on results from model simulations. We report the Weather Research and Forecasting Model coupled with Chemistry (WRF-Chem)
simulated PM2.5 pH over China during a period with heavy haze episodes
in Beijing, and explore the sensitivity of the modeled aerosol pH to factors
including emissions of nonvolatile cations (NVCs) and NH3, aerosol
phase state assumption, and heterogeneous production of sulfate. We find that default WRF-Chem could predict spatial patterns of PM2.5 pH over China
similar to other CTMs, but with generally lower pH values, largely due to the
underestimation of alkaline species (NVCs and NH3) and the difference in
thermodynamic treatments between different models. Increasing NH3
emissions in the model would improve the modeled pH in comparison with
offline thermodynamic model calculations of pH constrained by observations.
In addition, we find that the aerosol phase state assumption and heterogeneous sulfate production are important in aerosol pH predictions for regions with
low relative humidity (RH) and high anthropogenic SO2 emissions,
respectively. These factors should be better constrained in model
simulations of aerosol pH in the future. Analysis of the modeled temporal
trend of PM2.5 pH in Beijing over a haze episode reveals a clear
decrease in pH from 5.2 ± 0.9 in a clean period to 3.6 ± 0.5 in a heavily polluted period. The increased acidity under more polluted conditions
is largely due to the formation and accumulation of secondary species
including sulfuric acid and nitric acid, even though being modified by
alkaline species (NVCs, NH3). Our result suggests that NO2
oxidation is unlikely to be important for heterogeneous sulfate production
during the Beijing haze as the effective pH for NO2 oxidation of S(IV) is at a higher pH of ∼ 6.