资源环境科技发展态势分析平台

NO2 foliar deposition through the stomata of leaves has been identified as a significant sink of NO, within a forest canopy. In this study, we investigated NO2 and NO exchange between the atmosphere and the leaves of the native California oak tree Quercus agrifolia using a branch enclosure system. NO2 detection was performed with laser-induced fluorescence (LIF), which excludes biases from other reactive nitrogen compounds and has a low detection limit of 5-50 ppt. We performed both light and dark experiments with concentrations between 0.5 and 10 ppb NO2 and NO under constant ambient conditions. Deposition velocities for NO2 during light and dark experiments were 0.123 +/- 0.009 and 0.015 +/- 0.001 cm s(-1), respectively. Much slower deposition was seen for NO, with deposition velocities of 0.012 +/- 0.002 and 0.005 +/- 0.002 cm s(-1) measured during light and dark experiments, respectively. This corresponded to a summed resistance of the stomata and mesophyll of 6.9 +/- 0.9 s cm(-1) for NO2 and 140 +/- 40 s cm(-1) for NO. No significant compensation point was detected for NO2 uptake, but compensation points ranging from 0.74 to 3.8 ppb were observed for NO. NO2 and NO deposition velocities reported here are comparable both with previous leaf-level chamber studies and inferences from canopy-level field measurements. In parallel with these laboratory experiments, we have constructed a detailed 1-D atmospheric model to assess the contribution of leaf-level NO(x )deposition to the total NOx loss and NOx canopy fluxes. Using the leaf uptake rates measured in the laboratory, these modeling studies suggest that loss of NOx to deposition in a California oak woodland competes with the pathways of HNO3 and RONO2 formation, with deposition making up 3 %-22 % of the total NOx loss. Additionally, foliar uptake of NOx at these rates could account for similar to 15 %-30 % canopy reduction of soil NO(x )emissions.