Leaf-Level Bidirectional Exchange of Formaldehyde on Deciduous and Evergreen Tree Saplings

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY ACS Earth and Space Chemistry Pub Date : 2024-03-18 DOI:10.1021/acsearthspacechem.3c00325
Joshua D. Shutter, Joshua L. Cox and Frank N. Keutsch*, 
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Abstract

Gas-phase formaldehyde (HCHO) is formed in high yield from the oxidation of many volatile organic compounds (VOCs) and is commonly used as a constraint when testing the performance of VOC oxidation mechanisms in models. However, prior to using HCHO as a model constraint for VOC oxidation in forested regions, it is essential to have a thorough understanding of its foliar exchange. Therefore, a controlled laboratory setup was designed to measure the emission and dry deposition of HCHO at the leaf-level to red oak (Quercus rubra) and Leyland cypress (Cupressus × leylandii) tree saplings. The results show that HCHO has a compensation point (CP) that rises exponentially with temperature (22–35 °C) with a mean range of 0.3–0.9 ppbv. The HCHO CP results are also found to be independent of the studied tree species and 40–70% relative humidity. Given that HCHO mixing ratios in forests during the daytime are usually greater than 1 ppbv, the magnitude of the CP suggests that trees generally act as a net sink of HCHO. Additionally, the results show that HCHO foliar exchange is stomatally controlled and better matches a reactivity factor (f0) of 0 as opposed to 1 in conventional dry deposition parametrizations. At 30 °C, daytime HCHO dry deposition fluxes are reduced by upward of 50% when using f0 = 0 and a nonzero HCHO CP, although deposition remains the dominant canopy sink of HCHO. A reduced deposition sink also implies the increased importance of the gas-phase photolysis of HCHO as a source of HO2.

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落叶树和常绿树苗叶片上的甲醛双向交换
许多挥发性有机化合物(VOC)在氧化过程中会产生大量气相甲醛(HCHO),在测试模型中 VOC 氧化机制的性能时,气相甲醛通常被用作一种约束条件。然而,在使用 HCHO 作为森林地区挥发性有机化合物氧化的模型约束条件之前,必须对其叶面交换有透彻的了解。因此,我们设计了一个受控实验室装置,以测量红栎(Quercus rubra)和莱兰柏(Cupressus × leylandii)树苗叶片层面的 HCHO 排放和干沉积。结果表明,HCHO 的补偿点(CP)随温度(22-35 °C)呈指数上升,平均范围为 0.3-0.9 ppbv。研究还发现,HCHO CP 结果与所研究的树种和 40-70% 的相对湿度无关。鉴于白天森林中的 HCHO 混合比通常大于 1 ppbv,CP 的大小表明树木通常是 HCHO 的净吸收汇。此外,研究结果表明,HCHO 的叶面交换受气孔控制,与传统干沉降参数中反应系数 (f0) 为 0 而不是 1 更为匹配。在 30 °C 温度条件下,使用 f0 = 0 和非零 HCHO CP 时,白天 HCHO 干沉积通量最多可减少 50%,尽管沉积仍是 HCHO 的主要冠层吸收汇。沉积汇的减少也意味着 HCHO 的气相光解作为 HO2 来源的重要性增加。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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