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Walters WW, Pye HOT, Kim H, Hastings MG. Modeling the Oxygen Isotope Anomaly (Δ17O) of Reactive Nitrogen in the Community Multiscale Air Quality Model: Insights into Nitrogen Oxide Chemistry in the Northeastern United States. ACS ES&T AIR 2024; 1:451-463. [PMID: 38884197 PMCID: PMC11151734 DOI: 10.1021/acsestair.3c00056] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/13/2023] [Revised: 04/09/2024] [Accepted: 04/10/2024] [Indexed: 06/18/2024]
Abstract
Atmospheric nitrate, including nitric acid (HNO3), particulate nitrate (pNO3), and organic nitrate (RONO2), is a key atmosphere component with implications for air quality, nutrient deposition, and climate. However, accurately representing atmospheric nitrate concentrations within atmospheric chemistry models is a persistent challenge. A contributing factor to this challenge is the intricate chemical transformations involving HNO3 formation, which can be difficult for models to replicate. Here, we present a novel model framework that utilizes the oxygen stable isotope anomaly (Δ17O) to quantitatively depict ozone (O3) involvement in precursor nitrogen oxidesN O x = N O + N O 2 photochemical cycling and HNO3 formation. This framework has been integrated into the US EPA Community Multiscale Air Quality (CMAQ) modeling system to facilitate a comprehensive assessment of NO x oxidation and HNO3 formation. In application across the northeastern US, the model Δ17O compares well with recently conducted diurnal Δ17O(NO2) and spatiotemporal Δ17O(HNO3) observations, with a root mean square error between model and observations of 2.6 ‰ for Δ17O(HNO3). The model indicates the major formation pathways of annual HNO3 production within the northeastern US are NO+OH (46 %), N2O5 hydrolysis (34 %), and organic nitrate hydrolysis (12 %). This model can evaluate NO x chemistry in CMAQ in future air quality and deposition studies involving reactive nitrogen.
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Affiliation(s)
- Wendell W. Walters
- Department
of Chemistry and Biochemistry, University
of South Carolina, Columbia, South Carolina 29208, United States
- Office
of Research and Development, U.S. Environmental
Protection Agency, Durham, North Carolina 27703, United States
| | - Havala O. T. Pye
- Office
of Research and Development, U.S. Environmental
Protection Agency, Durham, North Carolina 27703, United States
| | - Heejeong Kim
- Department
of Earth, Environment, and Planetary Sciences, Brown University, Providence, Rhode Island 02912, United States
- Institute
at Brown for Environment and Society, Brown
University, Providence, Rhode Island 02912, United States
| | - Meredith G. Hastings
- Department
of Earth, Environment, and Planetary Sciences, Brown University, Providence, Rhode Island 02912, United States
- Institute
at Brown for Environment and Society, Brown
University, Providence, Rhode Island 02912, United States
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2
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Chen H, Liu P, Wang Q, Huang R, Sarwar G. Impact and pathway of halogens on atmospheric oxidants in coastal city clusters in the Yangtze River Delta region in China. ATMOSPHERIC POLLUTION RESEARCH 2024; 15:10.1016/j.apr.2023.101979. [PMID: 39026942 PMCID: PMC11254322 DOI: 10.1016/j.apr.2023.101979] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 07/20/2024]
Abstract
Halogens (chlorine, bromine, and iodine) are known to profoundly influence atmospheric oxidants (hydroxyl radical (OH), hydroperoxyl radical (HO2), ozone (O3), and nitrate radical (NO3)) in the troposphere and subsequently affecting air quality. However, their impact on atmospheric oxidation and air pollution in coastal areas in China is poorly characterized. In this study, we use the WRF-CMAQ (Weather Research and Forecasting-Community Multiscale Air Quality) model with full halogen chemistry and process analysis to assess the influences and pathways of halogens on atmospheric oxidants in the Yangtze River Delta (YRD) region, a typical coastal city cluster in China. Halogens cause the annual OH radical increase by up to 16.4% and NO3 decrease by up to 45.3%. O3 increases by 2.0% in the YRD but decreases by 3.3% in marine environment. Halogen induced changes in atmospheric oxidants lead to a general increase of atmospheric oxidation capacity by 5.1% (maximum 48.4%). The production rate of OH (POH) in the YRD is enhanced by anthropogenic chlorine through both increased HO2 pathway and hypohalous acid photolysis pathway, while POH over ocean is enhanced by oceanic halogens through converting HO2 into hypohalous acid. Anthropogenic chlorine enhances both O3 and NO3 production (PNO3) rates through influencing their precursors while oceanic halogens reduce PNO3 and directly destroy ozone. Iodine contributed most (on average of 91% in oceanic halogens) in reducing production rates of oxidants. Thus, halogen emissions and potential effects of halogens on air quality need to be considered in air quality policies and regulations in the YRD region.
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Affiliation(s)
- Haoran Chen
- School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai 200240, China
| | - Ping Liu
- School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai 200240, China
| | - Qian Wang
- Shanghai Environmental Monitoring Center, Shanghai 200235, China
| | - RuiZhu Huang
- Shanghai Environmental Monitoring Center, Shanghai 200235, China
| | - Golam Sarwar
- Center for Environmental Measurement & Modeling, U.S. Environmental Protection Agency, Research Triangle Park, NC 27711, USA
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3
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Jung D, Soler R, de la Paz D, Notario A, Muñoz A, Ródenas M, Vera T, Borrás E, Borge R. Oxidation capacity changes in the atmosphere of large urban areas in Europe: Modelling and experimental campaigns in atmospheric simulation chambers. CHEMOSPHERE 2023; 341:139919. [PMID: 37611775 DOI: 10.1016/j.chemosphere.2023.139919] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/28/2023] [Revised: 06/30/2023] [Accepted: 08/20/2023] [Indexed: 08/25/2023]
Abstract
Air pollution is a major concern for human health and the environment. Consequently, environmental standards have become stricter to improve air quality. Thanks to this, the ambient levels of O3 precursors such as VOCs and NOX have decreased. However, O3 levels in Europe, especially during winter, have increased, potentially impacting on atmospheric oxidation capacity and the associated chemistry of tropospheric oxidants. In this work, we focus on recent changes in the oxidation capacity of urban atmospheres. The study is conducted with the results of the CMAQ modelling system with a regional resolution with 12 × 12 km2 across the entire European continent for the winter (January) and summer (July) of 2007 and 2015. The 2015 meteorological data is used for both years to emphasise emission changes during the studied period. We scrutinise the changes in ambient concentration levels of the main tropospheric oxidants (O3 and HOX radicals) in five representative cities, Valencia, Madrid, Milan, Berlin, and The Hague. The enhanced O3 formation in winter seems to be due to the low VOC/NOX ratio, while the opposite trend in summer may be related to a relatively high ratio. Additionally, photooxidation experiments are carried out in the EUPHORE chambers to study the effect of changes in NOX concentration and NO/NO2 ratio on the variation of the given oxidants at constant VOCs concentrations. For the baseline experiments, two scenarios are selected based on the model results of 2015: two representative winter and summer days of low and high pollution in Berlin and Madrid, respectively. The role of VOC/NOX and NO/NO2 ratios on atmospheric reactivity is discussed. As a result, it is first suggested that further decreases in ambient NOX levels are required to reduce ambient O3 levels. Moreover, additional factors should be considered when designing local-specific emission abatement strategies.
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Affiliation(s)
- Daeun Jung
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (UPM), C/ José Gutiérrez Abascal 2, 28006, Madrid, Spain.
| | - Rubén Soler
- EUPHORE Labs., Atmospheric Chemistry Area, Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), 46980, Paterna, Spain
| | - David de la Paz
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (UPM), C/ José Gutiérrez Abascal 2, 28006, Madrid, Spain
| | - Alberto Notario
- Universidad de Castilla-La Mancha, Physical Chemistry Department, Faculty of Chemical Science and Technologies, Ciudad Real, Spain
| | - Amalia Muñoz
- EUPHORE Labs., Atmospheric Chemistry Area, Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), 46980, Paterna, Spain
| | - Milagros Ródenas
- EUPHORE Labs., Atmospheric Chemistry Area, Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), 46980, Paterna, Spain
| | - Teresa Vera
- EUPHORE Labs., Atmospheric Chemistry Area, Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), 46980, Paterna, Spain
| | - Esther Borrás
- EUPHORE Labs., Atmospheric Chemistry Area, Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), 46980, Paterna, Spain
| | - Rafael Borge
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (UPM), C/ José Gutiérrez Abascal 2, 28006, Madrid, Spain
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Zhang Q, Hadizadeh MH, Hu Y, Zhang X, Su Z, Wu Z, Wang X, Xu F, Sun Y, Zhang Q, Wang W. The effects of the gas-liquid interface and gas phase on Cl/ClO radical interaction with water molecules. Phys Chem Chem Phys 2023; 25:23296-23305. [PMID: 37609804 DOI: 10.1039/d3cp02796a] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 08/24/2023]
Abstract
In the marine boundary layer (MBL), chlorine (Cl) and chlorine monoxide (ClO) are powerful oxidants with high concentrations. The gas-liquid interface is also ubiquitous in the MBL as a favorable site for atmospheric reactions. Understanding the role of water in Cl/ClO radical chemistry is essential for predicting their behavior in the atmosphere and developing effective strategies for mitigating their harmful effects. However, the research studies on the system of Cl/ClO radicals on the surface of water droplets are still insufficient. In previous studies, we have found unique results related to the hydroxyl radical at the interface using ab initio molecular dynamics (AIMD). In this work, we have used AIMD to investigate interactions between Cl/ClO radicals and water molecules at the gas-liquid interface. Radical mobility, radial distribution functions, coordination, and population analyses were conducted to investigate the surface preference, bonding pattern, and track Cl/ClO radicals in the water droplets. In addition, density functional theory (DFT) analysis was conducted to compare the results at the gas-liquid interface with those in the gas phase. We found that Cl/ClO radicals tend to remain near the gas-liquid interface in water droplet systems and outside of water clusters in gas phase systems. The ClO radical can form O*-H and Cl-O bonds with water molecules; however, neither the O*-O hemibond nor the Cl-H bond was detected in all systems. Different dominant structures were obtained for ClO in the interface and gas phase. The ClO radical can be bonded to one water molecule from its oxygen side, (H2O)0-Cl-O*-(H2O)1 at the interface, or to two water molecules from the chlorine and oxygen sides, (H2O)1-Cl-O*-(H2O)1 in the gas phase. Meanwhile, the Cl radical can only form a dominant structure like Cl*-(H2O)1 at the gas-liquid interface by making a Cl*-O hemibond. Providing a thorough explanation of the Cl/ClO radical behavior at the gas-liquid interface, this study will improve our understanding of the MBL's oxidizing capacity and pollution causes.
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Affiliation(s)
- Qi Zhang
- Environment Research Institute, Shandong University, Qingdao 266237, China.
| | - Mohammad Hassan Hadizadeh
- Environment Research Institute, Shandong University, Qingdao 266237, China.
- International Center for Quantum Design of Functional Materials (ICQD), Hefei National Laboratory for Physical Sciences at the Microscale, and Synergetic Innovation Center of Quantum Information and Quantum Physics, University of Science and Technology of China, Hefei 230026, China
| | - Yongxia Hu
- Environment Research Institute, Shandong University, Qingdao 266237, China.
| | - Xiaoyu Zhang
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Zupeng Su
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Zihan Wu
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Xiaotong Wang
- Environment Research Institute, Shandong University, Qingdao 266237, China.
| | - Fei Xu
- Environment Research Institute, Shandong University, Qingdao 266237, China.
- Shenzhen Research Institute of Shandong University, Shenzhen 518057, China
| | - Yanhui Sun
- College of Environment and Safety Engineering, Qingdao University of Science & Technology, Qingdao 266042, China
| | - Qingzhu Zhang
- Environment Research Institute, Shandong University, Qingdao 266237, China.
| | - Wenxing Wang
- Environment Research Institute, Shandong University, Qingdao 266237, China.
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5
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Fan S, Li Y. Potential deterioration of ozone pollution in coastal areas caused by marine-emitted halogens: A case study in the Guangdong-Hong Kong-Macao Greater Bay Area. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 860:160456. [PMID: 36436642 DOI: 10.1016/j.scitotenv.2022.160456] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/03/2022] [Revised: 11/04/2022] [Accepted: 11/20/2022] [Indexed: 06/16/2023]
Abstract
Ozone (O3) is one of the most important air pollutants worldwide in terms of its great damage to human health and agriculture. Previous studies show that marine-emitted halogens significantly influence O3 concentrations, mainly through the consumption of O3 by bromine and iodine atoms. In this study, we investigate the temporal variation at finer time scales (daily and hourly) than previous studies (annual or monthly) to better characterize the influence of marine-emitted halogens on coastal O3. In contrast to previous studies that mainly reported a decrease in O3, our results show significant temporal variations in halogen-induced O3 changes. More specifically, the halogen-induced decrease in coastal O3 in southern China is concentrated on clean days, while an unexpected increase in some regions of up to >10 ppbv could occur on polluted days. On polluted days, the activation of particulate chloride (Cl-) in sea salt aerosol (SSA) is effective due to the high level of dinitrogen pentoxide (N2O5) that is formed from the reactions of O3 and nitrogen dioxide (NO2). In addition, the wind fields are unfavorable for the transport of marine air masses with large O3 depletion inland. These two factors together result in the increase in hourly and MDA8 O3 on polluted days in some regions in the GBA. The locations of O3 increases are controlled by the distribution of nitryl chloride (ClNO2) at sunrise, which is influenced by O3 and NO2 during the previous night. As a result, the increase in O3 is a continuation of the O3 pollution from the previous day, and the whole area is under potential threat of this worsening pollution.
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Affiliation(s)
- Shidong Fan
- Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China; Center for the Oceanic and Atmospheric Science at SUSTech (COAST), Southern University of Science and Technology, Shenzhen 518055, China
| | - Ying Li
- Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China; Center for the Oceanic and Atmospheric Science at SUSTech (COAST), Southern University of Science and Technology, Shenzhen 518055, China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China.
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6
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Jung D, de la Paz D, Notario A, Borge R. Analysis of emissions-driven changes in the oxidation capacity of the atmosphere in Europe. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 827:154126. [PMID: 35219666 DOI: 10.1016/j.scitotenv.2022.154126] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/16/2021] [Revised: 02/16/2022] [Accepted: 02/21/2022] [Indexed: 06/14/2023]
Abstract
Anthropogenic emissions in Europe have been gradually reduced thanks to a combination of factors, including restrictive regulation and policy implementation, fuel switching, technological developments, and improved energy efficiencies. Many measures have been specifically introduced to meet the annual and hourly limit value of NO2 for the protection of human health, mainly targeting traffic emissions. Due to NOX reduction policies in Europe, NO2 levels have generally declined, but O3 concentrations have been found to increase. This phenomenon would cause changes in the oxidant capacity of the atmosphere, altering the concentration of tropospheric oxidants in urban areas. The Community Multiscale Air Quality (CMAQ) modelling system has been used to study concentration changes of NO2, O3 and the main radicals in Europe between 2007 and 2015 for two months representatives of winter and summer conditions (January and July). In addition to describing the general situation in Europe, variations in pollutants along with NOX emission changes over 67 large European cities have been analysed by means of statistical methods. NOX emissions and NO2 concentrations decreased in both seasons during the period in all the selected cities. In most of them O3 concentrations increased in winter but decreased in summer. The concentration of the OH radical, the main oxidant during the daytime, shows an increase in winter. This is also the case for the main cities in summer although we found a general decrease in continent for this season. The NO3 radical, the main night-time oxidant, was found to increase in winter and decrease in summer. HNO3 shows a concentration decline in both seasons. The studied cities are classified in five groups by means of k-mean clustering procedure. We identified five groups with specific patterns, suggesting that the oxidant capacity of the European urban atmospheres has reacted differently to NOX emission abatement policies.
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Affiliation(s)
- Daeun Jung
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (ETSII - UPM), Madrid, Spain
| | - David de la Paz
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (ETSII - UPM), Madrid, Spain
| | - Alberto Notario
- Universidad de Castilla-La Mancha, Physical Chemistry Department, Faculty of Chemical Science and Technologies, Ciudad Real, Spain
| | - Rafael Borge
- Environmental Modelling Laboratory, Department of Chemical & Environmental Engineering, Universidad Politécnica de Madrid (ETSII - UPM), Madrid, Spain.
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7
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Alkorta I, Plane JMC, Elguero J, Dávalos JZ, Acuña AU, Saiz-Lopez A. Theoretical study of the NO 3 radical reaction with CH 2ClBr, CH 2ICl, CH 2BrI, CHCl 2Br, and CHClBr 2. Phys Chem Chem Phys 2022; 24:14365-14374. [PMID: 35642918 DOI: 10.1039/d2cp00021k] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/20/2023]
Abstract
The potential reaction of the nitrate radical (NO3), the main nighttime atmospheric oxidant, with five alkyl halides, halons (CH2ClBr, CH2ICl, CH2BrI, CHCl2Br, and CHClBr2) has been studied theoretically. The most favorable reaction corresponds to a hydrogen atom transfer. The stationary points on the potential energy surfaces of these reactions have been characterized. The reactions can be classified into two groups based on the number of hydrogen atoms in the halon molecules (1 or 2). The reactions with halons with only one hydrogen atom show more exothermic profiles than those with two hydrogen atoms. In addition, the kinetics of the reaction of NO3 + CH2BrI was studied in much higher detail using a multi-well Master Equation solver as a representative example of the nitrate radical reactivity against these halocarbons. These results indicate that the chemical lifetime of the alkyl halides would not be substantially affected by nitrate radical reactions, even in the case of NO3-polluted atmospheric conditions.
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Affiliation(s)
- Ibon Alkorta
- Instituto de Química Médica (CSIC), Juan de la Cierva, 3, E-28006 Madrid, Spain.
| | - John M C Plane
- School of Chemistry, University of Leeds, LS2 9TJ Leeds, UK
| | - José Elguero
- Instituto de Química Médica (CSIC), Juan de la Cierva, 3, E-28006 Madrid, Spain.
| | - Juan Z Dávalos
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano (CSIC), Madrid E-28006, Spain.
| | - A Ulises Acuña
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano (CSIC), Madrid E-28006, Spain.
| | - Alfonso Saiz-Lopez
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano (CSIC), Madrid E-28006, Spain.
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Zhang B, Shen H, Yun X, Zhong Q, Henderson BH, Wang X, Shi L, Gunthe SS, Huey LG, Tao S, Russell AG, Liu P. Global Emissions of Hydrogen Chloride and Particulate Chloride from Continental Sources. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:3894-3904. [PMID: 35319880 PMCID: PMC10558010 DOI: 10.1021/acs.est.1c05634] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/14/2023]
Abstract
Gaseous and particulate chlorine species play an important role in modulating tropospheric oxidation capacity, aerosol water uptake, visibility degradation, and human health. The lack of recent global continental chlorine emissions has hindered modeling studies of the role of chlorine in the atmosphere. Here, we develop a comprehensive global emission inventory of gaseous HCl and particulate Cl- (pCl), including 35 sources categorized in six source sectors based on published up-to-date activity data and emission factors. These emissions are gridded at a spatial resolution of 0.1° × 0.1° for the years 1960 to 2014. The estimated emissions of HCl and pCl in 2014 are 2354 (1661-3201) and 2321 (930-3264) Gg Cl a-1, respectively. Emissions of HCl are mostly from open waste burning (38%), open biomass burning (19%), energy (19%), and residential (13%) sectors, and the major sources classified by fuel type are combustion of waste (43%), biomass (32%), and coal (25%). Emissions of pCl are mostly from biofuel (29%) and open biomass burning processes (44%). The sectoral and spatial distributions of HCl and pCl emissions are very heterogeneous along the study period, and the temporal trends are mainly driven by the changes in emission factors, energy intensity, economy, and population.
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Affiliation(s)
- Bingqing Zhang
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
| | - Huizhong Shen
- School of Environmental science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Xiao Yun
- College of Urban and Environmental Sciences, Laboratory for Earth Surface Processes, Sino-French Institute for Earth System Science, Peking University, Beijing 100871, China
| | - Qirui Zhong
- Department of Earth Science, Vrije Universiteit Amsterdam, 1081 HV Amsterdam, the Netherlands
| | - Barron H. Henderson
- United States Environmental Protection Agency, Research Triangle Park, Durham, North Carolina 27709, USA
| | - Xuan Wang
- School of Energy and Environment, City University of Hong Kong, Hong Kong SAR, China
| | - Liuhua Shi
- Gangarosa Department of Environmental Health, Rollins School of Public Health, Emory University, Atlanta, Georgia 30322, USA
| | - Sachin S. Gunthe
- EWRE Division, Department of Civil Engineering, Indian Institute of Technology Madras, Chennai, Tamil Nadu 600036, India
- Laboratory for Atmospheric and Climate Sciences, Indian Institute of Technology Madras, Chennai, Tamil Nadu 600036, India
| | - Lewis Gregory Huey
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
| | - Shu Tao
- School of Environmental science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
- College of Urban and Environmental Sciences, Laboratory for Earth Surface Processes, Sino-French Institute for Earth System Science, Peking University, Beijing 100871, China
| | - Armistead G. Russell
- School of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
| | - Pengfei Liu
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
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9
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Li Q, Tham YJ, Fernandez RP, He X, Cuevas CA, Saiz‐Lopez A. Role of Iodine Recycling on Sea-Salt Aerosols in the Global Marine Boundary Layer. GEOPHYSICAL RESEARCH LETTERS 2022; 49:e2021GL097567. [PMID: 35859565 PMCID: PMC9285722 DOI: 10.1029/2021gl097567] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 12/21/2021] [Accepted: 02/25/2022] [Indexed: 06/15/2023]
Abstract
Heterogeneous uptake of hypoiodous acid (HOI), the dominant inorganic iodine species in the marine boundary layer (MBL), on sea-salt aerosol (SSA) to form iodine monobromide and iodine monochloride has been adopted in models with assumed efficiency. Recently, field measurements have reported a much faster rate of this recycling process than previously assumed in models. Here, we conduct global model simulations to quantify the range of effects of iodine recycling within the MBL, using Conventional, Updated, and Upper-limit coefficients. When considering the Updated coefficient, iodine recycling significantly enhances gaseous inorganic iodine abundance (∼40%), increases halogen atom production rates (∼40% in I, >100% in Br, and ∼60% in Cl), and reduces oxidant levels (-7% in O3, -2% in OH, and -4% in HO2) compared to the simulation without the process. We appeal for further direct measurements of iodine species, laboratory experiments on the controlling factors, and multiscale simulations of iodine heterogeneous recycling.
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Affiliation(s)
- Qinyi Li
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry Rocasolano, CSICMadridSpain
| | - Yee Jun Tham
- School of Marine SciencesSun Yat‐Sen UniversityZhuhaiChina
- Institute for Atmospheric and Earth System Research / Physics, Faculty of ScienceUniversity of HelsinkiHelsinkiFinland
| | - Rafael P. Fernandez
- Institute for Interdisciplinary ScienceNational Research Council (ICB‐CONICET)MendozaArgentina
- School of Natural SciencesNational University of Cuyo (FCEN‐UNCuyo)MendozaArgentina
| | - Xu‐Cheng He
- Institute for Atmospheric and Earth System Research / Physics, Faculty of ScienceUniversity of HelsinkiHelsinkiFinland
| | - Carlos A. Cuevas
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry Rocasolano, CSICMadridSpain
| | - Alfonso Saiz‐Lopez
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry Rocasolano, CSICMadridSpain
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10
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Li Q, Badia A, Fernandez RP, Mahajan AS, López‐Noreña AI, Zhang Y, Wang S, Puliafito E, Cuevas CA, Saiz‐Lopez A. Chemical Interactions Between Ship-Originated Air Pollutants and Ocean-Emitted Halogens. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2021; 126:e2020JD034175. [PMID: 33816042 PMCID: PMC8008258 DOI: 10.1029/2020jd034175] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 10/31/2020] [Revised: 12/09/2020] [Accepted: 12/27/2020] [Indexed: 06/12/2023]
Abstract
Ocean-going ships supply products from one region to another and contribute to the world's economy. Ship exhaust contains many air pollutants and results in significant changes in marine atmospheric composition. The role of reactive halogen species (RHS) in the troposphere has received increasing recognition and oceans are the largest contributors to their atmospheric burden. However, the impact of shipping emissions on RHS and that of RHS on ship-originated air pollutants have not been studied in detail. Here, an updated Weather Research Forecasting coupled with Chemistry model is utilized to explore the chemical interactions between ship emissions and oceanic RHS over the East Asia seas in summer. The emissions and resulting chemical transformations from shipping activities increase the level of NO and NO2 at the surface, increase O3 in the South China Sea, but decrease O3 in the East China Sea. Such changes in pollutants result in remarkable changes in the levels of RHS (>200% increase of chlorine; ∼30% and ∼5% decrease of bromine and iodine, respectively) as well as in their partitioning. The abundant RHS, in turn, reshape the loadings of air pollutants (∼20% decrease of NO and NO2; ∼15% decrease of O3) and those of the oxidants (>10% reduction of OH and HO2; ∼40% decrease of NO3) with marked patterns along the ship tracks. We, therefore, suggest that these important chemical interactions of ship-originated emissions with RHS should be considered in the environmental policy assessments of the role of shipping emissions in air quality and climate.
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Affiliation(s)
- Qinyi Li
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
| | - Alba Badia
- Institute of Environmental Science and Technology (ICTA)Universitat Autònoma de Barcelona (UAB)BarcelonaSpain
| | - Rafael P. Fernandez
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
- Institute for Interdisciplinary Science (ICB)National Research Council (CONICET)FCEN‐UNCuyoMendozaArgentina
| | - Anoop S. Mahajan
- Centre for Climate Change ResearchIndian Institute of Tropical MeteorologyPuneIndia
| | - Ana Isabel López‐Noreña
- Atmospheric and Environmental Studies Group (GEAA)National Technological University (UTN‐FRM)CONICETMendozaArgentina
| | - Yan Zhang
- Department of Environmental Science and EngineeringShanghai Key Laboratory of Atmospheric Particle Pollution and PreventionFudan UniversityShanghaiChina
| | - Shanshan Wang
- Department of Environmental Science and EngineeringShanghai Key Laboratory of Atmospheric Particle Pollution and PreventionFudan UniversityShanghaiChina
| | - Enrique Puliafito
- Atmospheric and Environmental Studies Group (GEAA)National Technological University (UTN‐FRM)CONICETMendozaArgentina
| | - Carlos A. Cuevas
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
| | - Alfonso Saiz‐Lopez
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
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Huang Y, Lu X, Fung JCH, Sarwar G, Li Z, Li Q, Saiz-Lopez A, Lau AKH. Effect of bromine and iodine chemistry on tropospheric ozone over Asia-Pacific using the CMAQ model. CHEMOSPHERE 2021; 262:127595. [PMID: 32784061 PMCID: PMC7658052 DOI: 10.1016/j.chemosphere.2020.127595] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/28/2020] [Revised: 06/25/2020] [Accepted: 06/30/2020] [Indexed: 05/28/2023]
Abstract
Recent studies have focused on the chemistry of tropospheric halogen species which are able to deplete tropospheric ozone (O3). In this study, the effect of bromine and iodine chemistry on tropospheric O3 within the annual cycle in Asia-Pacific is investigated using the CMAQ model with the newly embedded bromine and iodine chemistry and a blended and customized emission inventory considering marine halogen emission. Results indicate that the vertical profiles of bromine and iodine species show distinct features over land/ocean and daytime/nighttime, related to natural and anthropogenic emission distributions and photochemical reactions. The halogen-mediated O3 loss has a strong seasonal cycle, and reaches a maximum of -15.9 ppbv (-44.3%) over the ocean and -13.4 ppbv (-38.9%) over continental Asia among the four seasons. Changes in solar radiation, dominant wind direction, and nearshore chlorophyll-a accumulation all contribute to these seasonal differences. Based on the distances to the nearest coastline, the onshore and offshore features of tropospheric O3 loss caused by bromine and iodine chemistry are studied. Across a coastline-centric 400-km-wide belt from onshore to offshore, averaged maximum gradient of O3 loss reaches 1.1 ppbv/100 km at surface level, while planetary boundary layer (PBL) column mean of O3 loss is more moderate, being approximately 0.7 ppbv/100 km. Relative high halogen can be found over Tibetan Plateau (TP) and the largest O3 loss (approximately 4-5 ppbv) in the PBL can be found between the western boundary of the domain and the TP. Halogens originating from marine sources can potentially affect O3 concentration transported from the stratosphere over the TP region. As part of efforts to improve our understanding of the effect of bromine and iodine chemistry on tropospheric O3, we call for more models and monitoring studies on halogen chemistry and be considered further in air pollution prevention and control policy.
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Affiliation(s)
- Yeqi Huang
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, China
| | - Xingcheng Lu
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, China
| | - Jimmy C H Fung
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, China; Division of Mathematics, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, China.
| | - Golam Sarwar
- Center for Environmental Measurement and Modeling, Office of Research and Development, U.S. Environmental Protection Agency, Research Triangle Park, NC, USA
| | - Zhenning Li
- Institute of Environment, Energy and Sustainability, The Chinese University of Hong Kong, Shatin, N.T., Hong Kong, China
| | - Qinyi Li
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid, 28006, Spain
| | - Alfonso Saiz-Lopez
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid, 28006, Spain
| | - Alexis K H Lau
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, China; Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Hong Kong, China
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12
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Li Q, Badia A, Wang T, Sarwar G, Fu X, Zhang L, Zhang Q, Fung J, Cuevas CA, Wang S, Zhou B, Saiz-Lopez A. Potential Effect of Halogens on Atmospheric Oxidation and Air Quality in China. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2020; 125:10.1029/2019JD032058. [PMID: 32523860 PMCID: PMC7286431 DOI: 10.1029/2019jd032058] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/04/2023]
Abstract
Air pollution has been a hazard in China over recent decades threatening the health of half a billion people. Much effort has been devoted to mitigating air pollution in China leading to a significant reduction in primary pollutants emissions from 2013 to 2017, while a continuously worsening trend of surface ozone (O3, a secondary pollutant and greenhouse gas) was observed over the same period. Atmospheric oxidation, dominated by daytime reactions involving hydroxyl radicals (OH), is the critical process to convert freshly-emitted compounds into secondary pollutants, and is underestimated in current models of China's air pollution. Halogens (chlorine, bromine, and iodine) are known to profoundly influence oxidation chemistry in the marine environment; however, their impact on atmospheric oxidation and air pollution in China is unknown. In the present study, we report for the first time that halogens substantially enhance the total atmospheric oxidation capacity in polluted areas of China, typically 10% to 20% (up to 87% in winter) and mainly by significantly increasing OH level. The enhanced oxidation along the coast is driven by oceanic emissions of bromine and iodine, and that over the inland areas by anthropogenic emission of chlorine. The extent and seasonality of halogen impact are largely explained by the dynamics of Asian monsoon, location and intensity of halogen emissions, and O3 formation regime. The omission of halogen emissions and chemistry may lead to significant errors in historical re-assessments and future projections of the evolution of atmospheric oxidation in polluted regions.
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Affiliation(s)
- Qinyi Li
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid 28006, Spain
| | - Alba Badia
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid 28006, Spain
| | - Tao Wang
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, China
| | - Golam Sarwar
- National Exposure Research Laboratory, Environmental Protection Agency, Research Triangle Park, NC 27711, United States
| | - Xiao Fu
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, China
| | - Li Zhang
- Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey 08540, USA
- Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration, Princeton, New Jersey, 08544, United States
| | - Qiang Zhang
- Department of Earth System Science, Tsinghua University, Beijing 100084, China
| | - Jimmy Fung
- Division of Environment and Sustainability, Hong Kong University of Science and Technology, Hong Kong, China
| | - Carlos A. Cuevas
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid 28006, Spain
| | - Shanshan Wang
- Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
| | - Bin Zhou
- Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
| | - Alfonso Saiz-Lopez
- Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, Madrid 28006, Spain
- Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
- Corresponding author: Alfonso Saiz-Lopez ()
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