首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Effects of aerosol dynamics and gas–particle conversion on dry deposition of inorganic reactive nitrogen in a temperate forest
【24h】

Effects of aerosol dynamics and gas–particle conversion on dry deposition of inorganic reactive nitrogen in a temperate forest

机译:气溶胶动力学和气体颗粒转化对温带林中无机反应性氮干沉积的影响

获取原文
           

摘要

Dry deposition has an impact on nitrogen status in forest environments. However, the mechanism for the high dry-deposition rates of fine nitrate particles (NO3-) observed in forests remains unknown and is thus a potential source of error in chemical transport models (CTMs). Here, we modified and applied a multilayer land surface model coupled with dry-deposition and aerosol dynamic processes for a temperate mixed forest in Japan. This represents the first application of such a model to ammonium nitrate (NH4NO3) gas–particle conversion (gpc) and the aerosol water uptake of reactive nitrogen compounds. Thermodynamics, kinetics, and dry deposition for mixed inorganic particles are modeled by a triple-moment modal method. Data for inorganic mass and size-resolved total number concentrations measured by a filter pack and electrical low-pressure impactor in autumn were used for model inputs and subsequent numerical analysis. The model successfully reproduces turbulent fluxes observed above the canopy and vertical micrometeorological profiles noted in our previous studies. The sensitivity tests with and without gpc demonstrated clear changes in the inorganic mass and size-resolved total number concentrations within the canopy. The results also revealed that within-canopy evaporation of NH4NO3 under dry conditions significantly enhances the deposition flux of fine-NO3- and fine-NH4+ particles, while reducing the deposition flux of nitric acid gas (HNO3). As a result of the evaporation of particulate NH4NO3, the calculated daytime mass flux of fine NO3- over the canopy was 15 times higher in the scenario of “gpc” than in the scenario of “no gpc”. This increase caused high contributions from particle deposition flux (NO3- and NH4+) to total nitrogen flux over the forest ecosystem (~39%), although the contribution of NH3 was still considerable. A dry-deposition scheme coupled with aerosol dynamics may be required to improve the predictive accuracy of chemical transport models for the surface concentration of inorganic reactive nitrogen.
机译:干沉积对森林环境中的氮气状况产生影响。然而,在森林中观察到的细硝酸盐颗粒(NO 3-)的高干沉积速率的机制仍然未知,因此是化学传输模型(CTMS)中的潜在误差源。在这里,我们修改并应用了与日本温带混合森林的干沉积和气溶胶动力过程相结合的多层陆地表面模型。这表示将这种模型的第一次施用于硝酸铵(NH 4 NO 3)气体颗粒转化率(GPC)和活性氮化合物的气溶胶水吸收。用于混合无机颗粒的热力学,动力学和干沉积是通过三力矩模拟方法进行建模的。用于秋季滤布包和电低压撞击器测量的无机质量和尺寸分辨总数浓度的数据用于模型输入和随后的数值分析。该模型成功地再现了在我们以前的研究中指出的冠层上方观察到的湍流助熔剂。具有和无GPC的敏感性测试证明了树冠内无机质量和尺寸分辨的总数浓度的明显变化。结果还显示,在干燥条件下NH 4 NO 3的冠层内蒸发显着增强了细NO3和细NH4 +颗粒的沉积通量,同时减少了硝酸气体(HNO3)的沉积通量。由于颗粒状NH4NO3的蒸发,在“GPC”的情况下,在树冠上的细微NO3-过度的计算的白天质量通量比“NO GPC”的情景更高的15倍。这种增加引起了粒子沉积通量(NO 3和NH4 +)对森林生态系统(〜39%)的总氮气通量的高贡献,尽管NH3的贡献仍然相当大。可能需要一种与气溶胶动力学联接的干沉积方案来提高化学传输模型的预测精度,用于无机反应性氮的表面浓度。

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号