Nitrate and its precursor (gaseous HNO
3) in China are generally overestimated by current chemical transport models in comparison to in-situ observations. In this study, we used an observation-based box model and in-situ measurements at a rural site in southern China to investigate possible missing sinks of nitrate. We found that a heterogeneous reaction of HNO
3 to NO
x on soot can better balance the NO
x/HNO
3 chemistry in models and improve model performance with regard to nitrate, particularly where an additional HONO source (the heterogeneous reaction of NO
2 on soot) is incorporated into current models. Through a series of sensitivity simulations, the uptake coefficients of heterogeneous reactions were suggested to be 3.0 × 10
−3 and 1 × 10
−4 for HNO
3 and HONO over southern China in fall, respectively. A 3-D simulation with the suggested uptake coefficients further confirmed that heterogeneous reactions significantly decreased the nitrate concentrations (PNO
3) in southern China, by up to 10 μg m
−3 (50%-80% of simulated PNO
3) in polluted regions (e.g., the Yangtze River). In contrast to nitrate and HNO
3, NO
x concentrations in China were enhanced, which partly explained the underestimation of NO
2 in current models compared to satellite observations.
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