Environmental science: atmospheres最新文献

The role of biogenic emissions in forming ozone (O₃) and secondary organic aerosol (SOA) is increasingly important with decreasing anthropogenic emissions in China. However, biogenic volatile organic compounds (BVOCs) from urban green spaces are often neglected mainly because available land cover datasets do not reflect the distribution and density of vegetation in urban areas. In this study, urban BVOC emissions in Beijing at 1 km spatial resolution are estimated based on Google Earth Engine and a high-resolution land cover dataset and then used for air quality simulation in the summer of 2017. The updated urban BVOC emissions show better agreement with observed isoprene emission fluxes than other inventories. Air quality simulation shows that the contribution of urban BVOCs to the maximum daily averaged 8 h O₃ in Beijing typically exceeds 5 ppb with the maximum value of 8 ppb. Although BVOC emissions are higher in rural areas than urban areas, their contributions to O₃ concentrations are lower in rural regions. In contrast, the mean concentrations of biogenic SOA (BSOA) in urban areas (1.44 μg m⁻³) are 17% lower than in rural areas. Compared to other inventories, the average difference in BSOA concentrations in urban areas reached 0.18 μg m⁻³, and the relative changes in ISOA, MSOA, and SSOA were 14.3%, 17.7%, and 32.6%, respectively. This study emphasizes the importance of considering BVOC emissions from urban green spaces in understanding urban atmospheric chemistry. The methodology used to update urban green spaces in this study is equally applicable to other cities.

The global attention on indoor air quality is progressively increasing as people spend ca. 80 to 90% of their lives indoors. Therefore, a substantial fraction of exposure to air pollution occurs in different indoor environments. However, there is a lack of information on how different time and activity dependent sources and built environment characteristics affect air pollutant emissions and their distribution. There is an urgent need to develop indoor emissions inventories to estimate the contribution of multiple and time-dependent sources and activities to air pollutant emissions. This paper reviews the current state-of-the-art of indoor air pollution research in the UK, categorises the published literature according to pollutant types, built environments and activities, provides an overview of typical levels of indoor air pollutants with a focus on UK-specific measurements and identifies the research gaps and future directions to progress towards developing indoor emission inventories. In the UK, researchers have investigated indoor air quality since the nineties producing many studies from different perspectives. However, a cohesive methodological approach is lacking in most of the studies. Several important sources/species are not represented, ancillary information relating to environment characteristics (volumes and ventilation) and occupants' behaviours during the measurements is not reported and too little information on the indoor–outdoor continuum is provided. Despite the gaps identified, the existing evidence base on indoor air pollution in the UK can be categorised in an easy-to-use database of indoor air pollutant concentrations and characteristic emission rates for specific activities, pollutants and environments. This will provide a platform for designing standardised approaches for indoor air quality measurements and the development of activity-based indoor emission inventories, which will be a step-change in indoor air pollution research in the UK and globally.

There is no standard sampling and analysis method for vapor phase per- and polyfluoroalkyl substances (PFAS) that can be routinely applied to soil gas, sewer/conduit gas, and indoor air samples. We have validated a thermal desorption GC/MS/MS method for the measurement of a set of fluorotelomer alcohols and perfluorooctanesulfonamides collected on multi-bed sorbent tubes. Applications to perfluorocarboxylic acids were also evaluated since there is debate regarding under what circumstances these compounds could be observed moving into gas phase. Perfluorooctanoic acid (PFOA) met Method TO-17 calibration requirements when calibrated using National Institute of Standards and Technology (NIST) traceable standard solutions introduced through the thermal desorption system and using multiple reaction monitoring (MRM) transitions based on precursor mass ions identified in the PFOA spectra. However, subsequent detailed studies suggested that PFOA was decomposing during the thermal desorption sample introduction step when comparing two alternative GC/MS sample introduction techniques. The primary peak resulting from the thermal desorption of PFOA standard had spectra consistent with perfluoro-1-heptene (PFHp-1), suggesting that a degradation reaction was occurring. Therefore, the identification of the PFCA compounds in this method is currently subject to a potential positive interference from the corresponding perfluoroalkene and other thermally labile PFAS. Thus, it may be beneficial to limit the application of the thermal desorption GC/MS/MS method to the fluorotelomer alcohols and perfluorooctanesulfonamides and use a parallel solvent extraction approach to quantify the PFCA-related compounds. Method validation including desorption efficiency, second source verification, storage stability and method detection limit tests were successfully completed for the fluorotelomer alcohols and perfluorooctanesulfonamides target analytes.

This study investigates aerosol and wet deposition chemistry at Acadia National Park (Maine, U.S.) using data between 1 January 2001 and 31 December 2021. Results show that PM_2.5 is highest in summer and dominated by sulfate salts and organics (less contribution from elemental carbon), whereas nitrate salts and sea salt were highest in winter. Fine soil is most pronounced from March through August due most likely to long-range transport. Residual mass (PM_2.5 – reconstructed PM_2.5) was negative from November–March, with reasons discussed for its seasonal changes. Major regional sources of pollution are upwind from populated cities generally to the southwest of Acadia. Extreme PM_2.5 events are mostly driven by regional pollution events with others due to transported summertime biomass burning plumes that increased in frequency in the most recent years. Aerosol composition on cold air outbreak days showed that ammonium sulfate and organics dominated PM_2.5, which provides useful information for studies focused on understanding the formation and evolution of offshore cloud decks during the winter. Monthly mean pH in wet deposition ranges from 4.8 to 5.1 with the lowest values in July when contributions from acidic ions are highest (sulfate, nitrate). Average annual pH increased from 4.64 to 5.23 over the study period coincident with reductions in sulfate and nitrate levels. Sea salt constituents dominated the wet deposition aqueous ion concentrations from November to March, whereas in the other months sulfate and nitrate were highest. Interrelationships between aerosol and wet deposition species relevant to secondarily produced species, dust, and sea salt provide support for aerosol–precipitation interactions that warrant a further look with more robust methods.

This study investigates the impact of forest fires on air quality in India's northeastern (NE) region, focusing on Guwahati, Tezpur, and Aizawl. The North-Eastern Forest cluster, contributing 36% to the total forest cover, emerges as a hotspot with the highest number of fire detections (40%). Population growth and shifting cultivation practices have intensified the frequency of fires. The study spans 2013–2016, assessing PM₁₀, PM_2.5, ozone (O₃), carbon monoxide (CO) and nitrogen oxide (NO_x) concentrations in the three NE cities. Guwahati consistently recorded PM₁₀ concentrations above National Ambient Air Quality Standards (NAAQS), indicating persistent air quality challenges. Tezpur and Aizawl maintained concentrations below NAAQS, with Aizawl displaying Good to Satisfactory air quality on a significant portion of observed days. During forest fire (FF) events from 2013 to 2016, PM₁₀, PM_2.5, O₃, CO, and NO_x concentrations rose, suggesting a direct correlation between FF and deteriorating air quality, especially when FF counts were above 100. During these events, a shift in air quality levels was observed, affecting most parameters in Aizawl and varying for other cities. Diurnal patterns during FF events indicated increased pollutant levels. The most prominent change was observed in PM₁₀ in all stations. Backward air–mass trajectory analysis confirms the influence of NE-India as a significant pollution source during FF. This study underscores the urgent need for targeted interventions to mitigate the impact of FF on air quality in the NE region, emphasising the intricate relationship between ecological practices, forest fires and atmospheric conditions.

Health-related impacts e.g. respiratory and cardiovascular morbidity and mortality, associated with exposure to atmospheric particulate matter (PM) are globally considered important and are not completely understood. Oxidative potential (OP), defined as a measure of the capacity of PM to oxidise target molecules, has been previously proposed as an alternative relevant biological metric in health studies to better quantify toxicological responses associated with PM exposure than aerosol mass alone. Several methods are currently used to assess the oxidative capacity of PM. In this study, the dithiothreitol (DTT) assay was used, which is the most commonly used technique to estimate OP. This assessment is easy-to-operate, low-cost, effective and reproducible. The first step was to modify the DTT methodology based on previous applications, which entailed choosing an appropriate extraction procedure and -setup. The redox activity of size-resolved PM samples collected in three low-income urban settlements in South Africa, i.e. Jouberton, KwaZamokuhle and Zamdela was evaluated and related to their chemical composition through correlation analysis. Furthermore, it was attempted to determine seasonal variations of DTT redox activity through normalisation according to PM mass (DTTm) and sampled volume (DTTv) for outdoor and indoor environments. The results indicated higher redox activity for the finest (<1 μm) particles compared to the coarser particulates (1–10 μm) for both outdoor and indoor environments. DTT redox activity of PM, especially, in the PM_1–10 particle size fraction, had strong correlations with elemental (EC) and organic carbon (OC), as well as trace elements and water-soluble inorganic species for outdoor and indoor samples. Possible atmospheric aerosol emission sources suggested from these correlations include primary emissions from domestic- and open biomass burning, vehicles and industrial activities, as well as secondary particle formation (e.g. sulphate).

Delhi is one of the most polluted regions in the world, yet studies focusing simultaneously on atmospheric aerosol particle size distribution (PSD) and chemical composition, as well as their inter-relationship, are still lacking. Additionally, the high condensation sink (CS) in Delhi has drawn less attention to new particle formation (NPF) and the role of chemical composition. This study explored the intricate interplay among particle size distribution, meteorology, and chemical composition within the atmospheric environment of Delhi. Our findings reveal pronounced seasonal variations in the particle number and mass concentration levels following variations in atmospheric conditions and emission sources across different seasons. Furthermore, we identified condensation sink as a primary factor governing the NPF, with no NPF event observed when daytime CS was above 0.06 s⁻¹. While precursors such as H₂SO₄ and NH₃ were abundant, they did not appear to be limiting factors for NPF. However, due to the lack of direct measurements of sub-10 nm particles and precursor gases such as H₂SO₄, amines, and organic vapours, the conclusions regarding the role of chemical precursors remain speculative. Furthermore, on days with comparable condensation sinks, the chemical composition exhibits no significant variation between NPF and non-NPF days, with organics contributing to about 50% of the PM_2.5, emphasizing the dominance of physical processes. Our observations highlight the critical influence of relative humidity on particle formation, with higher atmospheric liquid water content inhibiting NPF. Additionally, we investigated the simultaneous time variations in PSD and mass composition of PM_2.5, revealing significant mass composition variations during the first (daytime) and second (night-time) growth. Notably, during the daytime growth of nucleated particles, increases in sulphate and low volatile oxygenated organics suggest the involvement of sulphuric acid and oxidized vapours in early particle growth. However, the unclear relationship between the growth rate and chemical composition reveals the complexity of new particle formation in polluted environments such as Delhi. While PM_2.5 composition offers insights into growth processes, its relevance to nucleation-mode particles is limited. Thus, this study further emphasizes the need for sub-10 nm PSD and precursor gaseous measurements to seek a better understanding of NPF in a high CS environment in the Global South.

Cleaning detergents are a source of numerous volatile organic compounds (VOCs) which are highly reactive towards ozone leading to the formation of secondary organic aerosols (SOA) in indoor environments. Here we perform real-time measurements of the organic composition of aerosols produced upon ozone reaction with floor cleaning detergent by extractive electrospray ionization time-of-flight mass spectrometer (EESI-TOF-MS) coupled to a chamber reactor. The experiments were performed in the absence of light and under light irradiation (320 nm < λ < 400 nm) simulating the fraction of sunlight that penetrates indoors. The multiple increases in particle number concentrations correspond to rise in the signal intensity of specific species. Notably, the secondary increase in particle mass concentration is mainly contributed by highly oxidized molecules (HOMs), which increased from 16.5% upon ozone oxidation to 19.9% under photo-oxidation reactions. A large fraction of CHON compounds such as imidazole, pyrazine/pyrimidine, and azaindole was observed most likely formed through the reaction of O₃ with benzothiazole (constituent of the cleaning detergent). The difference between the molecular compositions detected in the absence of light and in the presence of light indicates that sunlight penetrating through the windows can affect the SOA produced by the reaction of ozone with the floor cleaning detergent.

Oxidation of emitted anthropogenic and biogenic volatile organic compounds (VOCs) and subsequent chemical reactions reduce the volatility of the products formed leading to secondary organic aerosol (SOA) formation. Despite the huge diversity of individual SOA compounds, SOA modelling is often simplified and estimated at the initial oxidation step neglecting chemical and physical process influencing SOA formation e.g. advection, deposition, chemical degradation and aging processes. To overcome this shortcoming, the chemical gas-phase mechanism URMELL was developed. URMELL treats more than 40 distinct oxidised gas-phase SOA (gasSOA) precursors with individual molecular characteristics and physico-chemical partitioning properties enabling a much more explicit gasSOA treatment for products of aromatics and isoprene oxidation. In this study, CTM simulations using COSMO-MUSCAT were performed with URMELL and compared with a simplified gasSOA scheme applying the widely used gas-phase mechanism RACM. The comparison indicates a delayed and thereby locally shifted gasSOA formation when applying URMELL. This effect is caused by the formation of multigenerational and multifunctional products along the transport trajectory whereby accounting for changes in the oxidant regime and leading to a multitude of gasSOA substances with URMELL. For isoprene and aromatics, URMELL simulates higher contributions of products with lower volatilities whereby aromatics generate even non-volatile products which can partition in new particle formation. The non-volatile aromatic products increase the average aromatic surface gasSOA concentration (30% on 20^th of May 2014) and show unexpectedly high concentrations in remote spruce forest areas, away from the emission sources, highlighting the potential of the detailed schemes and its need for application in CTMs.

Mt. Etna, an open-vent, persistently degassing volcano, is the tallest and most active volcano in Europe. Aerosols from the summit (Bocca Nuova crater), downwind (about 10 km from the crater) and control sites were collected during the EUROVOLC EPL-REFLECT field campaign in July 2019 and analysed for aerosol mass determination, major inorganic and organic ions, and soluble and insoluble metals. Computational modelling (using the models E-AIM, ISORROPIA, and Visual MINTEQ) was performed to determine the speciation of metal ions in the deliquescent aerosol phase within the volcanic plume and in aerosol collected in the town of Milo (Catania, Italy), a few km downwind of Mt. Etna and influenced by transport of the volcanic plume. The aerosol liquid water concentration at the summit was strongly dependent on the determination method – with ISORROPIA calculating a water concentration a factor of 10² lower than that of E-AIM, which itself was a factor of 10²–10³ lower than the total water content of the plume measured by infrared spectroscopy. The calculated pH was predominantly acidic (except for ISORROPIA calculations in the three samples), with the highest acidity observed where the water concentration was the lowest. Only a few metals were shown to have significant organic–ligand complexation in the aerosol, i.e., Al(III), Cu(II), and Fe(III) with oxalate, in the deliquescent aerosol within the plume. When considering the total amount of water of the plume, lower complexation was observed because of more diluted species concentration and less acidity.