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Real-time chemical characterization of primary and aged biomass burning aerosols derived from sub-Saharan African biomass fuels in smoldering fires. 对撒哈拉以南非洲生物质燃料燃烧产生的原始气溶胶和老化生物质燃烧气溶胶进行实时化学特征描述。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-28 DOI: 10.1039/d4ea00110a
Markie'Sha James, Vaios Moschos, Megan M McRee, Marc N Fiddler, Barbara J Turpin, Jason D Surratt, Solomon Bililign

The influence of biomass burning (BB)-derived organic aerosol (OA) emissions on solar radiation via absorption and scattering is related to their physicochemical properties and can change upon atmospheric aging. We systematically examined the compositionally-resolved mass concentration and production of primary and secondary organic aerosol (POA and SOA, respectively) in the NC A&T University smog chamber facility. Mass spectral profiles of OA measured by the Aerosol Chemical Speciation Monitor (ACSM) revealed the influence of dark- and photo-aging, fuel type, and relative humidity. Unit mass resolution (UMR) mapping, the ratio of the fraction of the OA mass spectrum signal at m/z 55 and 57 (f 55/f 57) vs. the same fraction at m/z 60 (f 60) was used to identify source-specific emission profiles. Furthermore, Positive Matrix Factorization (PMF) analysis was conducted using OA mass spectra, identifying four distinct factors: low-volatility oxygenated OA (LV-OOA), primary biomass-burning OA (BBOA), BB secondary OA (BBSOA), and semi-volatile oxygenated OA (SV-OOA). Data supports a robust four-factor solution, providing insights into the chemical transformations under different experimental conditions, including dark- and photo-aged, humidified, and dark oxidation with NO3 radicals. This work presents the first such laboratory study of African-derived BBOA particles, addressing a gap in global atmospheric chemistry research.

生物质燃烧(BB)产生的有机气溶胶(OA)排放物通过吸收和散射对太阳辐射的影响与其理化性质有关,并会随着大气老化而发生变化。我们在北卡罗来纳农工大学烟雾室设施中系统地研究了一次有机气溶胶和二次有机气溶胶(分别为 POA 和 SOA)的成分分辨质量浓度和生成量。气溶胶化学特性监测仪(ACSM)测量的有机气溶胶质谱图显示了暗老化和光老化、燃料类型和相对湿度的影响。单位质量分辨率(UMR)绘图,即 m/z 55 和 57(f 55/f 57)处的 OA 质谱信号分数与 m/z 60(f 60)处的相同分数之比,用于识别特定来源的排放剖面。此外,利用 OA 质谱进行了正矩阵因式分解(PMF)分析,确定了四个不同的因子:低挥发性含氧 OA(LV-OOA)、原生生物质燃烧 OA(BBOA)、BB 次生 OA(BBSOA)和半挥发性含氧 OA(SV-OOA)。数据支持稳健的四因素解决方案,为不同实验条件下的化学转化提供了见解,包括黑暗和光照老化、加湿以及使用 NO3 自由基进行黑暗氧化。这项工作首次对源自非洲的 BBOA 粒子进行了此类实验室研究,填补了全球大气化学研究的空白。
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引用次数: 0
A framework for describing and classifying methane reporting requirements, emission sources, and monitoring methods† 甲烷报告要求、排放源和监测方法的描述和分类框架†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-24 DOI: 10.1039/D4EA00120F
Andy Connor, Jacob T. Shaw, Nigel Yarrow, Neil Howes, Jon Helmore, Andrew Finlayson, Patrick Barker and Rod Robinson

Industries, governments, and regulators need trustworthy emissions data to enable them to make informed decisions regarding methane abatement strategy and policies. There are many differing data reporting metrics, as well as a diverse range of both emission sources and methods for monitoring emissions. Different data structures and terminologies can be used to describe similar objects, activities, or characteristics associated with methane monitoring. There is no currently accepted definition of what constitutes a methane monitoring method. Since there is no common basis to describe this information, confusion concerning language, definitions, and terminology can arise which can undermine confidence in data. This paper describes a framework, based on a set of taxonomies and a common lexicon, which aims to address these issues by providing a common structure in which data requirements, emission sources and monitoring methods can be described. The principles of metrology and quality assurance are embedded into this framework along with a means to define the temporal and spatial scales of the reporting and monitoring. It is envisaged that this framework will be developed into a standard to help facilitate more reliable transfer of information between stakeholders internationally. Usage examples for this framework include: to aid the development of test standards (between test laboratories, site operators, and standards bodies); to help ensure the most cost-effective monitoring methods are deployed for a specific purpose; to help identify technological and methodological gaps between what monitoring is needed and what is available, or to help drive more focused innovation in this field.

行业、政府和监管机构需要可靠的排放数据,以便就甲烷减排战略和政策做出明智的决策。有许多不同的数据报告指标,以及各种排放源和排放监控方法。不同的数据结构和术语可用于描述与甲烷监测相关的类似对象、活动或特征。对于什么是甲烷监测方法,目前还没有公认的定义。由于没有共同的基础来描述这些信息,因此可能会出现语言、定义和术语方面的混乱,从而影响对数据的信心。本文介绍了一个基于一套分类标准和通用词汇的框架,旨在通过提供一个通用结构来描述数据要求、排放源和监测方法,从而解决这些问题。该框架包含计量和质量保证原则,以及确定报告和监测的时间和空间范围的方法。预计该框架将发展成为一个标准,以帮助促进利益相关者之间在国际范围内更可靠地传递信息。该框架的使用实例包括:帮助制定测试标准(测试实验室、现场操作人员和标准机构之间);帮助确保为特定目的部署最具成本效益的监测方法;帮助确定所需监测与现有监测之间的技术和方法差距,或帮助推动该领域更有针对性的创新。
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引用次数: 0
Does gas-phase sulfur dioxide remove films of atmosphere-extracted organic material from the aqueous aerosol air–water interface?† 气相二氧化硫是否能从水性气溶胶的空气-水界面上去除大气萃取的有机物薄膜?
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-16 DOI: 10.1039/D4EA00098F
Edward J. Stuckey, Rebecca J. L. Welbourn, Stephanie H. Jones, Alexander J. Armstrong, Matthew Wilkinson, James I. L. Morison and Martin D. King

The reaction of gas-phase SO2 with unsaturated carbon–carbon double bonds forms organosulfates at the surface of the aerosol. Previous studies have focused on the reaction products and not the fate of organic films in the atmosphere. Neutron reflectometry was used to study the interaction of gas-phase SO2 at the air–water interface with organic material extracted from atmospheric particulate matter and pure proxy chemicals to determine whether the reaction of organic films with SO2 removes the film and if a product film is formed. Films formed from atmospheric aerosol collected in urban and woodland environments typically produced a layer of approximately 0.6 nm thickness, whereas a thick (>40 nm) film was formed by the woodsmoke sample. Fitting of this thicker woodsmoke film suggested a three-layered structure at the interface that has been interpreted to be consistent with a surfactant-rich layer next to the air–water interface, a mid-layer rich in polyaromatic hydrocarbons (PAH), and topped with a more aliphatic region. The multilayer structure of atmospheric extracted material at the air–water interface is potentially an exciting result that requires further study. Gas-phase SO2 was confirmed to react with pure insoluble surfactant molecules at the air–water interface that contained carbon–carbon double bonds (oleic acid) and did not react with a similar saturated surfactant (stearic acid). No reaction was observed during the interaction of SO2 and atmospheric material extracted from urban and woodland environments, and no material appeared to be removed from the interface; however, films made from woodsmoke-extracted material did appear to be altered by SO2 but there was no significant loss of material. In addition, the gas-phase ozone mixing ratios in the neutron blockhouse, which have historically been of some concern for reactions with organics, were found to be of the order 15 ppb, with no evidence of additional production in the neutron beam-path. Owing to a lack of substantial removal of material from real atmospheric extracted films, SO2 is not considered atmospherically significant for the removal of organic films from the air–water interface.

气相二氧化硫与不饱和碳碳双键反应,在气溶胶表面形成有机硫酸盐。以往的研究侧重于反应产物,而不是有机薄膜在大气中的归宿。中子反射仪被用来研究气相二氧化硫在空气-水界面与从大气颗粒物和纯代理化学品中提取的有机物的相互作用,以确定有机薄膜与二氧化硫的反应是否会去除薄膜,以及是否会形成产物薄膜。在城市和林地环境中收集的大气气溶胶所形成的薄膜通常只有大约 0.6 纳米厚,而木烟样品则形成了一层厚(40 纳米)的薄膜。对这层较厚的木烟薄膜进行拟合后发现,在界面处有一个三层结构,这与空气-水界面旁富含表面活性剂的一层、富含多芳烃(PAH)的中层以及顶部脂肪族较多的区域是一致的。大气提取物在空气-水界面的多层结构可能是一个令人兴奋的结果,需要进一步研究。经证实,气相二氧化硫会与空气-水界面上含有碳碳双键的纯不溶性表面活性剂分子(油酸)发生反应,而不会与类似的饱和表面活性剂(硬脂酸)发生反应。在二氧化硫与从城市和林地环境中提取的大气材料相互作用的过程中,没有观察到任何反应,也没有材料从界面上脱落;不过,从木质烟雾中提取的材料制成的薄膜似乎被二氧化硫改变了,但材料没有明显损失。此外,中子屏蔽室中的气相臭氧混合比历来是与有机物发生反应的一些问题,但研究发现,该混合比约为 15 ppb,没有证据表明中子束路径中产生了额外的臭氧。由于从大气中萃取的真实薄膜中没有大量物质被去除,因此认为二氧化硫对去除空气-水界面上的有机薄膜并不重要。
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引用次数: 0
Enhanced detection of aromatic oxidation products using NO3 - chemical ionization mass spectrometry with limited nitric acid. 利用 NO3 - 有限硝酸化学电离质谱法增强对芳香族氧化产物的检测。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-15 DOI: 10.1039/d4ea00087k
Olga Garmash, Avinash Kumar, Sakshi Jha, Shawon Barua, Noora Hyttinen, Siddharth Iyer, Matti Rissanen

Nitrate ion-based chemical ionization mass spectrometry (NO3 --CIMS) is widely used for detection of highly oxygenated organic molecules (HOMs). HOMs are known to participate in molecular clustering and new particle formation and growth, and hence understanding the formation pathways and amounts of these compounds in the atmosphere is essential. However, the absence of analytical standards prevents robust quantification of HOM concentrations. In addition, nitrate-based ionization is usually very selective towards the most oxygenated molecules and blind to less oxygenated compounds hindering the investigation of molecular formation pathways. Here, we explore varying concentrations of nitric acid reagent gas in the sheath flow of a chemical ionization inlet as a method for detecting a wider range of oxidation products in laboratory-simulated oxidation of benzene and naphthalene. When the concentration of reagent nitric acid is reduced, we observe an increase in signals of many oxidation products for both precursors suggesting that they are not detected at the collision limit. The sensitivity of naphthalene oxidation products is enhanced to a larger extent than that of benzene products. This enhancement in sensitivity has a negative relationship with molecular oxygen content, the oxygen-to-carbon ratio, the oxidation state of carbon, and lowered volatility. In addition, the sensitivity enhancement is lower for species that contain more exchangeable H-atoms, particularly for accretion products. While more experimental investigations are needed for providing the relationship between enhancement ratios and instrumental sensitivities, we suggest this method as a tool for routine check of collision-limited sensitivities and enhanced detection of lower-oxygenated species.

基于硝酸根离子的化学电离质谱(NO3-CIMS)被广泛用于检测高含氧有机分子(HOMs)。众所周知,高含氧有机分子参与分子聚类和新粒子的形成与生长,因此了解这些化合物在大气中的形成途径和数量至关重要。然而,由于缺乏分析标准,无法对 HOM 的浓度进行可靠的量化。此外,基于硝酸盐的电离通常对含氧量最高的分子具有很强的选择性,而对含氧量较低的化合物则视而不见,这阻碍了对分子形成途径的研究。在此,我们探讨了在化学电离进气口的鞘流中加入不同浓度的硝酸试剂气体的方法,以便在实验室模拟苯和萘的氧化过程中检测更广泛的氧化产物。当试剂硝酸的浓度降低时,我们观察到这两种前体的许多氧化产物的信号增加,这表明它们在碰撞极限时没有被检测到。萘氧化产物的灵敏度比苯产物的灵敏度更高。灵敏度的提高与分子氧含量、氧碳比、碳的氧化态和挥发性降低呈负相关。此外,对于含有更多可交换 H 原子的物种,尤其是增殖产物,灵敏度的提高幅度较低。虽然还需要更多的实验研究来提供增强比和仪器灵敏度之间的关系,但我们建议将此方法作为常规检查碰撞限制灵敏度和增强低氧物种检测的工具。
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引用次数: 0
Toxicological evaluation of SVOCs in exhaust emissions from light-duty vehicles using different fuel alternatives under sub-freezing conditions† 亚冰冻条件下使用不同燃料替代品的轻型汽车尾气排放中 SVOC 的毒理学评估†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-10 DOI: 10.1039/D4EA00062E
Mo Yang, Päivi Aakko-Saksa, Henri Hakkarainen, Topi Rönkkö, Päivi Koponen, Xiao-Wen Zeng, Guang-Hui Dong and Pasi I. Jalava

Semivolatile organic compounds (SVOCs) in exhaust gas, though not directly regulated by emission standards, play a crucial role in assessing both conventional and alternative fuels. Our aim is to compare the differences in and toxicological effects of SVOC exhaust emissions from conventional and alternative fuels under sub-freezing conditions. High levels of NOx, CO2 and PAHs in SVOCs were observed in DI-E2 (EN590 winter-grade diesel), with E10 (gasoline with 10% ethanol) exhibiting higher CO2 and PAH levels compared to E85 (high-blend ethanol with an 83/17% ethanol–gasoline ratio). SVOCs from DI-E6 (EN590 diesel) demonstrated significant cytotoxicity, while E10 resulted in higher inflammatory mediators and genotoxicity. Our findings show that SVOC composition and toxicity in exhaust gas differ based on the fuel type. Despite new emissions regulations reducing diesel vehicle emissions, SVOC toxicity remains unchanged. Toxicity from SVOCs in compressed natural gas and ethanol/gasoline vehicles is notable, with gasoline exhaust showing high inflammatory and genotoxic potential.

废气中的半挥发性有机化合物(SVOC)虽然不受排放标准的直接管制,但在评估传统燃料和替代燃料时却起着至关重要的作用。我们的目的是比较传统燃料和替代燃料在亚冰冻条件下排放的 SVOC 废气的差异和毒理学影响。在 DI-E2(EN590 冬季等级柴油)中观察到 SVOC 中的氮氧化物、二氧化碳和多环芳烃含量较高,与 E85(乙醇-汽油比例为 83/17% 的高混合乙醇)相比,E10(含 10%乙醇的汽油)的二氧化碳和多环芳烃含量较高。DI-E6(EN590 柴油)产生的 SVOC 具有显著的细胞毒性,而 E10 产生的炎症介质和基因毒性更高。我们的研究结果表明,废气中的 SVOC 成分和毒性因燃料类型而异。尽管新的排放法规减少了柴油车的排放量,但 SVOC 的毒性仍然没有改变。压缩天然气和乙醇/汽油车辆中的 SVOC 毒性显著,其中汽油废气具有较高的炎症和基因毒性潜能。
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引用次数: 0
Trace elements in PM2.5 shed light on Saharan dust incursions over the Munich airshed in spring 2022† PM2.5 中的痕量元素揭示了 2022 年春季撒哈拉沙尘入侵慕尼黑上空的情况†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-08 DOI: 10.1039/D4EA00092G
Sara Padoan, Alessandro Zappi, Jan Bendl, Tanja Herrmann, Ajit Mudan, Carsten Neukirchen, Erika Brattich, Laura Tositti and Thomas Adam

The influence of a prolonged Saharan Dust event across Europe and specifically in Munich (Germany) in March 2022 was detected and analyzed in detail. The event arose from a sequence of Saharan Dust incursions intertwined with a stagnation in the regional circulation leading to the persistence of a mineral dust plume for several weeks over the region. Trace element and meteorological data were collected. Enrichment factors, size distribution analyses, and multivariate techniques such as Varimax and Self-Organizing Maps (SOM) were applied to highlight the influence of Saharan Dusts and to evaluate the pollution sources in Munich municipality. The overall results revealed how the Munich airshed was clearly affected by long-distance mineral dusts from the North African desert, that increased the concentrations of natural (e.g. Al, Mg, Ca) and anthropogenic (e.g. Sb, Mo, Pb) elements based on the different paths followed by the dusts. Moreover, the chemometric analyses revealed a range of well-defined local anthropogenic emission sources including road traffic, energy production by coal combustion (S and Se), traffic (Cu, Sb), and waste incineration (Zn).

检测并详细分析了 2022 年 3 月撒哈拉沙尘事件对整个欧洲,特别是对慕尼黑(德国)的影响。该事件源于一连串撒哈拉沙尘的入侵,与区域环流的停滞交织在一起,导致矿物尘羽在该地区上空持续数周。收集了痕量元素和气象数据。应用富集因子、粒度分布分析和多元技术(如 Varimax 和自组织图 (SOM))来突出撒哈拉沙尘的影响,并评估慕尼黑市的污染源。总体结果显示,慕尼黑空气流域明显受到来自北非沙漠的长距离矿物尘埃的影响,根据尘埃的不同路径,增加了天然(如 Al、Mg、Ca)和人为(如 Sb、Mo、Pb)元素的浓度。此外,化学计量学分析还揭示了一系列明确的当地人为排放源,包括道路交通、燃煤能源生产(S 和 Se)、交通(Cu、Sb)和垃圾焚烧(Zn)。
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引用次数: 0
Evaluating emissions and meteorological contributions to air quality trends in northern China based on measurements at a regional background station† 基于区域本底站的测量结果,评估排放和气象对中国北方空气质量趋势的影响†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-08 DOI: 10.1039/D4EA00070F
Weiwei Pu, Yingruo Li, Xiaowan Zhu, Xiangxue Liu, Di He, Fan Dong, Heng Guo, Guijie Zhao, Liyan Zhou, Shuangshuang Ge and Zhiqiang Ma

The contributions of meteorology and emissions to air pollutant trends are critical for air quality management, but they have not been fully analyzed, especially in the background area of northern China. Here, we used a machine learning technique to quantify the impacts of meteorological conditions and emissions on PM2.5, NO2, SO2, O3, and CO pollution during 2013–2021 and evaluated their contributions to Clean Air Action policies. The annual effect of the meteorology on PM2.5, NO2, SO2, and CO levels was dominated by the meteorological conditions during the cold season, while that of the O3 level largely depended on the meteorological conditions during the warm season. Meteorology-driven anomalies contributed −14.8 to 10.3%, −8.5 to 7.3%, −11 to 7.1%, −7.9 to 6.0%, and −7.4 to 7.3% to the annual mean concentrations of PM2.5, NO2, SO2, O3, and CO during the study period, respectively. The Clean Air Actions have led to a major improvement in the air quality at regional scale, with the reduction of 1.7 μg m−3 year−1, 0.2 μg m−3 year−1, 1.5 μg m−3 year−1, 0.7 μg m−3 year−1, and 0.03 mg m−3 year−1 for PM2.5, NO2, SO2, O3, and CO at background area, respectively, after meteorological correction. Although emissions dominated the long-term variations in pollutants, the meteorological conditions obviously played a positive role during the action periods for pollutants except for O3. Considering the notable effects of the meteorological conditions on air pollution and the interreaction between pollutants, a more comprehensive control strategy should be considered on a broader regional scale.

气象和排放对空气污染物趋势的影响对于空气质量管理至关重要,但目前尚未对其进行全面分析,尤其是在中国北方的背景地区。在此,我们利用机器学习技术量化了 2013-2021 年气象条件和排放对 PM2.5、NO2、SO2、O3 和 CO 污染的影响,并评估了它们对清洁空气行动政策的贡献。气象对 PM2.5、NO2、SO2 和 CO 水平的年度影响主要受寒冷季节气象条件的影响,而对 O3 水平的影响则主要取决于温暖季节的气象条件。在研究期间,气象驱动的异常对 PM2.5、NO2、SO2、O3 和 CO 年平均浓度的影响分别为-14.8%至 10.3%、-8.5%至 7.3%、-11%至 7.1%、-7.9%至 6.0%和-7.4%至 7.3%。清洁空气行动大大改善了区域范围内的空气质量,经气象校正后,背景区域 PM2.5、NO2、SO2、O3 和 CO 的浓度分别降低了 1.7 μg m-3 年-1、0.2 μg m-3 年-1、1.5 μg m-3 年-1、0.7 μg m-3 年-1 和 0.03 mg m-3 年-1。虽然排放主导了污染物的长期变化,但除 O3 外,气象条件在污染物的作用期明显发挥了积极作用。考虑到气象条件对空气污染的显著影响以及污染物之间的相互影响,应在更广泛的区域范围内考虑更全面的控制策略。
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引用次数: 0
Kinetics of the reactions of the Criegee intermediate CH2OO with water vapour: experimental measurements as a function of temperature and global atmospheric modelling† 克里基中间体 CH2OO 与水蒸气反应的动力学:作为温度函数的实验测量结果和全球大气模型†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-09-30 DOI: 10.1039/D4EA00097H
Rachel E. Lade, Mark A. Blitz, Matthew Rowlinson, Mathew J. Evans, Paul W. Seakins and Daniel Stone
<p >The kinetics of reactions between the simplest Criegee intermediate, CH<small><sub>2</sub></small>OO, and water vapour have been investigated at temperatures between 262 and 353 K at a total pressure of 760 Torr using laser flash photolysis of CH<small><sub>2</sub></small>I<small><sub>2</sub></small>–O<small><sub>2</sub></small>–N<small><sub>2</sub></small>–H<small><sub>2</sub></small>O mixtures coupled with broadband time-resolved UV absorption spectroscopy. Results indicate that the reaction with water monomers represents a minor contribution to the total loss of CH<small><sub>2</sub></small>OO under the conditions employed in this work, with an estimated rate coefficient for CH<small><sub>2</sub></small>OO + H<small><sub>2</sub></small>O (R1) of (9.8 ± 5.9) × 10<small><sup>−17</sup></small> cm<small><sup>3</sup></small> molecule<small><sup>−1</sup></small> s<small><sup>−1</sup></small> at 298 K and a temperature dependence described by <em>k</em><small><sub>1</sub></small> = (3.2 ± 1.1) × 10<small><sup>−13</sup></small> exp(−(2410 ± 270)/<em>T</em>) cm<small><sup>3</sup></small> molecule<small><sup>−1</sup></small> s<small><sup>−1</sup></small>. The reaction of CH<small><sub>2</sub></small>OO with water dimers, CH<small><sub>2</sub></small>OO + (H<small><sub>2</sub></small>O)<small><sub>2</sub></small> (R2), dominates under the conditions employed in this work. The rate coefficient for R2 has been measured to be <em>k</em><small><sub>2</sub></small> = (9.5 ± 2.5) × 10<small><sup>−12</sup></small> cm<small><sup>3</sup></small> molecule<small><sup>−1</sup></small> s<small><sup>−1</sup></small> at 298 K, with a negative temperature dependence described by <em>k</em><small><sub>2</sub></small> = (2.85 ± 0.40) × 10<small><sup>−15</sup></small> exp((2420 ± 340)/<em>T</em>) cm<small><sup>3</sup></small> molecule<small><sup>−1</sup></small> s<small><sup>−1</sup></small>, where rate<small><sub>R2</sub></small> = <em>k</em><small><sub>2</sub></small>[CH<small><sub>2</sub></small>OO][(H<small><sub>2</sub></small>O)<small><sub>2</sub></small>]. For use in atmospheric models, we recommend description of the kinetics for R2 in terms of the product of the rate coefficient <em>k</em><small><sub>2</sub></small> and the equilibrium constant <em>K</em><small><sup>D</sup></small><small><sub>eq</sub></small> (<em>k</em><small><sub>2,eff</sub></small> = <em>k</em><small><sub>2</sub></small><em>K</em><small><sup>D</sup></small><small><sub>eq</sub></small>) for water dimer formation to allow the rate of reaction to be expressed in terms of water monomer concentration as rate<small><sub>R2</sub></small> = <em>k</em><small><sub>2,eff</sub></small>[CH<small><sub>2</sub></small>OO][H<small><sub>2</sub></small>O]<small><sup>2</sup></small> to avoid explicit calculation of dimer concentrations and impacts of differences in values of <em>K</em><small><sup>D</sup></small><small><sub>eq</sub></small> reported in the literature. Results from this work give <em>k</em><small
利用激光闪烁光解 CH2I2-O2-N2-H2O 混合物并结合宽带时间分辨紫外吸收光谱,研究了在 262 至 353 K 温度、760 托总压条件下最简单的克里基中间体 CH2OO 与水蒸气之间的反应动力学。结果表明,在本研究采用的条件下,与水单体的反应对 CH2OO 的总损失贡献不大,在 298 K 时,CH2OO + H2O (R1) 的估计速率系数为 (9.8 ± 5.9) × 10-17 cm3 分子-1 s-1,与温度的关系用 k1 = (3.2 ± 1.1) × 10-13 exp(-(2410 ± 270)/T) cm3 分子-1 s-1 描述。在本研究采用的条件下,CH2OO 与水二聚体的反应 CH2OO + (H2O)2 (R2) 占主导地位。在 298 K 时,R2 的速率系数为 k2 = (9.5 ± 2.5) × 10-12 cm3 分子-1 s-1,与温度的负相关关系为 k2 = (2.85 ± 0.40) × 10-15 exp((2420 ± 340)/T) cm3 分子-1 s-1,其中速率 R2 = k2[CH2OO][(H2O)2]。在大气模型中使用时,我们建议用水二聚体形成的速率系数 k2 与平衡常数 KDeq 的乘积(k2,eff = k2KDeq)来描述 R2 的动力学,以便用水单体浓度来表示反应速率,即速率 R2 = k2,eff[CH2OO][H2O]2,从而避免明确计算二聚体浓度和文献中报告的 KDeq 值差异的影响。这项工作的结果表明,在 298 K 时,k2,eff = (1.96 ± 0.51) × 10-32 cm6 molecule-2 s-1,温度依赖性描述为 k2,eff = (2.78 ± 0.28) × 10-38 exp((4010 ± 400)/T) cm6 molecule-2 s-1。在这项工作中,没有观察到 CH2OO 和三个水分子之间的反应有明显的影响,这可能是这项工作中使用的相对湿度(298 K 时高达 57%)的结果。使用全球化学传输模型 GEOS-Chem 对结果对大气的影响进行了研究。模型模拟表明,与水二聚体的反应主导了大气中 CH2OO 的损失,并限制了 CH2OO 其他反应的影响,与水二聚体的反应占对流层中 CH2OO 总损失的 98%。
{"title":"Kinetics of the reactions of the Criegee intermediate CH2OO with water vapour: experimental measurements as a function of temperature and global atmospheric modelling†","authors":"Rachel E. Lade, Mark A. Blitz, Matthew Rowlinson, Mathew J. Evans, Paul W. Seakins and Daniel Stone","doi":"10.1039/D4EA00097H","DOIUrl":"https://doi.org/10.1039/D4EA00097H","url":null,"abstract":"&lt;p &gt;The kinetics of reactions between the simplest Criegee intermediate, CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO, and water vapour have been investigated at temperatures between 262 and 353 K at a total pressure of 760 Torr using laser flash photolysis of CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;I&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;–O&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;–N&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;–H&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;O mixtures coupled with broadband time-resolved UV absorption spectroscopy. Results indicate that the reaction with water monomers represents a minor contribution to the total loss of CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO under the conditions employed in this work, with an estimated rate coefficient for CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO + H&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;O (R1) of (9.8 ± 5.9) × 10&lt;small&gt;&lt;sup&gt;−17&lt;/sup&gt;&lt;/small&gt; cm&lt;small&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;/small&gt; molecule&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; s&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; at 298 K and a temperature dependence described by &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;1&lt;/sub&gt;&lt;/small&gt; = (3.2 ± 1.1) × 10&lt;small&gt;&lt;sup&gt;−13&lt;/sup&gt;&lt;/small&gt; exp(−(2410 ± 270)/&lt;em&gt;T&lt;/em&gt;) cm&lt;small&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;/small&gt; molecule&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; s&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt;. The reaction of CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO with water dimers, CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO + (H&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;O)&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt; (R2), dominates under the conditions employed in this work. The rate coefficient for R2 has been measured to be &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt; = (9.5 ± 2.5) × 10&lt;small&gt;&lt;sup&gt;−12&lt;/sup&gt;&lt;/small&gt; cm&lt;small&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;/small&gt; molecule&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; s&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; at 298 K, with a negative temperature dependence described by &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt; = (2.85 ± 0.40) × 10&lt;small&gt;&lt;sup&gt;−15&lt;/sup&gt;&lt;/small&gt; exp((2420 ± 340)/&lt;em&gt;T&lt;/em&gt;) cm&lt;small&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;/small&gt; molecule&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt; s&lt;small&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;/small&gt;, where rate&lt;small&gt;&lt;sub&gt;R2&lt;/sub&gt;&lt;/small&gt; = &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;[CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO][(H&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;O)&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;]. For use in atmospheric models, we recommend description of the kinetics for R2 in terms of the product of the rate coefficient &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt; and the equilibrium constant &lt;em&gt;K&lt;/em&gt;&lt;small&gt;&lt;sup&gt;D&lt;/sup&gt;&lt;/small&gt;&lt;small&gt;&lt;sub&gt;eq&lt;/sub&gt;&lt;/small&gt; (&lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2,eff&lt;/sub&gt;&lt;/small&gt; = &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;&lt;em&gt;K&lt;/em&gt;&lt;small&gt;&lt;sup&gt;D&lt;/sup&gt;&lt;/small&gt;&lt;small&gt;&lt;sub&gt;eq&lt;/sub&gt;&lt;/small&gt;) for water dimer formation to allow the rate of reaction to be expressed in terms of water monomer concentration as rate&lt;small&gt;&lt;sub&gt;R2&lt;/sub&gt;&lt;/small&gt; = &lt;em&gt;k&lt;/em&gt;&lt;small&gt;&lt;sub&gt;2,eff&lt;/sub&gt;&lt;/small&gt;[CH&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;OO][H&lt;small&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;/small&gt;O]&lt;small&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;/small&gt; to avoid explicit calculation of dimer concentrations and impacts of differences in values of &lt;em&gt;K&lt;/em&gt;&lt;small&gt;&lt;sup&gt;D&lt;/sup&gt;&lt;/small&gt;&lt;small&gt;&lt;sub&gt;eq&lt;/sub&gt;&lt;/small&gt; reported in the literature. Results from this work give &lt;em&gt;k&lt;/em&gt;&lt;small","PeriodicalId":72942,"journal":{"name":"Environmental science: atmospheres","volume":" 11","pages":" 1294-1308"},"PeriodicalIF":2.8,"publicationDate":"2024-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://pubs.rsc.org/en/content/articlepdf/2024/ea/d4ea00097h?page=search","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142595206","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Immersion ice nucleation of atmospherically relevant lipid particles† 与大气相关的脂质颗粒的浸入式冰核形成†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-09-25 DOI: 10.1039/D4EA00066H
Lincoln Mehndiratta, Audrey E. Lyp, Jonathan H. Slade and Vicki H. Grassian

Ice nucleating particles (INPs) play a crucial role in freezing water droplets by acting as heterogeneous ice nuclei, influencing cloud phase state and climate dynamics. INPs from marine aerosol particles are particularly relevant. Saturated fatty alcohols and acids have been identified in sea spray aerosols (SSA). In this study, we employ a micro-Raman spectrometer integrated with an environmental cell to control relative humidity and temperature and measure the ice nucleation activity of individual lipid particles, including fatty alcohols and fatty acids of varying chain lengths. For fatty acids, we observe little IN activity for these lipid particles as they freeze close to the temperature found for homogeneous freezing. For fatty alcohols, we demonstrate that freezing temperatures depend on the carbon chain length, with longer chains leading to warmer ice nucleating temperatures. Although this result qualitatively agrees with existing literature, we observe that the ice nucleating temperatures of these lipid particles differ from the freezing temperatures measured for fatty alcohol monolayers at the air/water interface for large water droplets. To better understand these differences, we further investigate the effects of droplet size as well as phase state by theoretically determining the wet viscosity on freezing. Our results, taken together, suggest that for fatty alcohol particles, freezing occurs at the lipid particle/water interface. Overall, our findings highlight the influence of lipid chain length, droplet size, and phase state on ice nucleation for lipid particles.

冰核粒子(INPs)通过充当异质冰核在水滴冻结过程中发挥着至关重要的作用,影响着云相状态和气候动力学。来自海洋气溶胶颗粒的 INPs 尤其具有相关性。在海雾气溶胶(SSA)中发现了饱和脂肪醇和酸。在这项研究中,我们利用微拉曼光谱仪与环境电池集成来控制相对湿度和温度,并测量单个脂质颗粒的冰核活性,包括不同链长的脂肪醇和脂肪酸。对于脂肪酸,我们观察到这些脂质微粒几乎没有 IN 活性,因为它们的冻结温度接近均匀冻结时的温度。对于脂肪醇,我们证明冻结温度取决于碳链长度,碳链越长,冰核温度越高。虽然这一结果与现有文献的定性结果一致,但我们观察到这些脂质颗粒的冰核温度与脂肪醇单层在大水滴的空气/水界面上测得的冻结温度不同。为了更好地理解这些差异,我们通过理论测定冻结时的湿粘度,进一步研究了水滴大小和相态的影响。我们的研究结果表明,对于脂肪醇颗粒来说,冻结发生在脂质颗粒/水的界面上。总之,我们的研究结果凸显了脂质链长、液滴大小和相态对脂质颗粒冰核形成的影响。
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引用次数: 0
Particle number size distribution evaluation of Plantower PMS5003 low-cost PM sensors – a field experiment† Plantower PMS5003 低成本可吸入颗粒物传感器的粒度分布评估--现场实验†。
IF 2.8 Q3 ENVIRONMENTAL SCIENCES Pub Date : 2024-09-24 DOI: 10.1039/D4EA00086B
Alexandre Caseiro, Seán Schmitz and Erika von Schneidemesser

The use of low-cost sensors (LCS) for the evaluation of the ambient pollution by particulate matter (PM) has grown and become significant for the scientific community in the past few years. However promising this novel technology is, the characterization of their limitations is still not satisfactory. Reports in the scientific literature rely on calibration, which implies the physical (or geographical) co-location of the LCS with reference in situ (or remote, e.g. onboard satellite platforms) instrumentation. However, calibration is not always feasible, and even when feasible, the validity of the developed relationship, even in similar settings, is subject to large uncertainties. In the present work, the performance of a popular LCS for PM, the Plantower PMS5003, is investigated. The LCS performs particle counts, which is the physical quantity that is input to the black-box model of the manufacturer to compute the ambient PM mass, which is output to the operator. The particle counts of LCS Plantower PMS5003 units were compared to those of the co-located research-grade Grimm EDM-164 monitor. The results show that humidity possibly has a reduced influence on the performance, but the performance can better be constrained, however spanning more than one order of magnitude in terms of agreement ratio, by functions of the actual particle count itself. In view of these results, further development in the field of LCS for PM monitoring should focus on improvements of the physical design of the devices, in order to enhance the sizing of the particles. The use of the actual Plantower PMS5003 models should be limited to the monitoring of PM mass in the smaller size bins.

在过去几年里,使用低成本传感器(LCS)来评估环境颗粒物(PM)污染的情况越来越多,对科学界来说意义重大。尽管这项新技术前景广阔,但对其局限性的描述仍不尽人意。科学文献中的报告依赖于校准,这意味着将 LCS 与参考原地(或远程,如卫星平台上)仪器物理(或地理)同地定位。然而,校准并不总是可行的,即使可行,所建立关系的有效性,即使在类似的环境中,也会受到很大的不确定性影响。在本研究中,对一种常用的可吸入颗粒物 LCS(Plantower PMS5003)的性能进行了调查。该 LCS 可进行颗粒计数,这是输入到制造商黑盒模型中的物理量,用于计算环境 PM 质量,并将其输出给操作员。将 LCS Plantower PMS5003 设备的颗粒计数与同处的研究级 Grimm EDM-164 监测器的颗粒计数进行了比较。结果表明,湿度对性能的影响可能较小,但通过实际颗粒计数本身的功能,可以更好地限制性能,但在一致性比方面,差距超过一个数量级。鉴于这些结果,用于可吸入颗粒物监测的 LCS 领域的进一步发展应侧重于改进设备的物理设计,以提高颗粒的大小。实际使用的 Plantower PMS5003 型号应仅限于监测较小粒径范围内的可吸入颗粒物质量。
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引用次数: 0
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Environmental science: atmospheres
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