Articles | Volume 20, issue 24
Atmos. Chem. Phys., 20, 16117–16133, 2020
https://doi.org/10.5194/acp-20-16117-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 20, 16117–16133, 2020
https://doi.org/10.5194/acp-20-16117-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
23 Dec 2020
Research article
| 23 Dec 2020
Soil–atmosphere exchange flux of total gaseous mercury (TGM) at subtropical and temperate forest catchments
Jun Zhou et al.
Related authors
Jun Zhou, Zhangwei Wang, Xiaoshan Zhang, Charles Driscoll, and Che-Jen Lin
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2019-161, https://doi.org/10.5194/acp-2019-161, 2019
Preprint withdrawn
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Previous studies showed that Hg emissions from the natural resource exists large uncertainty, which was mainly derived from the forest with a large uncertainty range. Long-term and multi-plot (five) study of soil-air fluxes and the vertical distribution of Hg in a subtropical forest were conducted to reduce the uncertainty. Additionally, The Hg diffusion coefficients (Ds) between soil and atmosphere was investigated, which should provide a foundation for future model development.
Jun Zhou, Buyun Du, Zhangwei Wang, Lihai Shang, and Jing Zhou
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2017-794, https://doi.org/10.5194/acp-2017-794, 2018
Preprint withdrawn
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The current knowledge concerning mercury budgets and pools of forest in China is reviewed, including THg and MeHg input fluxes by precipitation, throughfall and litterfall, output by runoffs and soil-atmosphere exchange fluxes, Hg storage in soils and biomass, and their risk assessment. The annual THg retentions at forests of China are about 1.2 to 7.9-fold higher compared to those in North America, and THg retention in forest is much high than that in global scale estimated by models.
Lyla L. Taylor, Charles T. Driscoll, Peter M. Groffman, Greg H. Rau, Joel D. Blum, and David J. Beerling
Biogeosciences, 18, 169–188, https://doi.org/10.5194/bg-18-169-2021, https://doi.org/10.5194/bg-18-169-2021, 2021
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Enhanced rock weathering (ERW) is a carbon dioxide removal (CDR) strategy involving soil amendments with silicate rock dust. Over 15 years, a small silicate application led to net CDR of 8.5–11.5 t CO2/ha in an acid-rain-impacted New Hampshire forest. We accounted for the total carbon cost of treatment and compared effects with an adjacent, untreated forest. Our results suggest ERW can improve the greenhouse gas balance of similar forests in addition to mitigating acid rain effects.
Chunjie Wang, Zhangwei Wang, Fan Hui, and Xiaoshan Zhang
Atmos. Chem. Phys., 19, 10111–10127, https://doi.org/10.5194/acp-19-10111-2019, https://doi.org/10.5194/acp-19-10111-2019, 2019
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A low GEM level indicated that the SCS suffered less anthropogenic influence. There was no significant difference in GEM and HgP2.5 values between day and night, but the RGM level was higher in daytime than in nighttime. The size distribution of HgP in PM10 was observed to be bi-modal, but the coarse modal was the dominant size. The annual emission flux of Hg0 from the SCS was estimated to be 159 ton yr-1. The dry deposition was an important pathway for the input of atmospheric Hg to the SCS.
Jun Zhou, Zhangwei Wang, Xiaoshan Zhang, Charles Driscoll, and Che-Jen Lin
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2019-161, https://doi.org/10.5194/acp-2019-161, 2019
Preprint withdrawn
Short summary
Short summary
Previous studies showed that Hg emissions from the natural resource exists large uncertainty, which was mainly derived from the forest with a large uncertainty range. Long-term and multi-plot (five) study of soil-air fluxes and the vertical distribution of Hg in a subtropical forest were conducted to reduce the uncertainty. Additionally, The Hg diffusion coefficients (Ds) between soil and atmosphere was investigated, which should provide a foundation for future model development.
Jun Zhou, Buyun Du, Zhangwei Wang, Lihai Shang, and Jing Zhou
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2017-794, https://doi.org/10.5194/acp-2017-794, 2018
Preprint withdrawn
Short summary
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The current knowledge concerning mercury budgets and pools of forest in China is reviewed, including THg and MeHg input fluxes by precipitation, throughfall and litterfall, output by runoffs and soil-atmosphere exchange fluxes, Hg storage in soils and biomass, and their risk assessment. The annual THg retentions at forests of China are about 1.2 to 7.9-fold higher compared to those in North America, and THg retention in forest is much high than that in global scale estimated by models.
Longfei Yu, Yihao Wang, Xiaoshan Zhang, Peter Dörsch, and Jan Mulder
Biogeosciences, 14, 3097–3109, https://doi.org/10.5194/bg-14-3097-2017, https://doi.org/10.5194/bg-14-3097-2017, 2017
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In this study, we applied phosphorus (P) to a nitrogen (N)-saturated forest in the Chinese subtropics and observed significant decreases in both N2O and CH4 emission from soil within 1.5 years. This was associated with a strong decrease of mineral N in soil water, likely due to stimulated N uptake. Our findings suggest that P limitation could be one important reason for large greenhouse gas emissions reported in the subtropical forests receiving excessive N input.
Zhijia Ci, Fei Peng, Xian Xue, and Xiaoshan Zhang
Atmos. Chem. Phys., 16, 14741–14754, https://doi.org/10.5194/acp-16-14741-2016, https://doi.org/10.5194/acp-16-14741-2016, 2016
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We performed field measurements and controlled field experiments to examine the flux, temporal variation and influencing factors of air–surface Hg(0) exchange at a high-altitude and remote site in the central Qinghai–Tibet Plateau. We found that the environmental conditions greatly influenced the air–surface Hg dynamics. Our results have important implications for the Hg biogeochemical cycle in the soils of Qinghai–Tibet Plateau under rapid climate warming and environmental change.
Hui Zhang, Xuewu Fu, Che-Jen Lin, Lihai Shang, Yiping Zhang, Xinbin Feng, and Cynthia Lin
Atmos. Chem. Phys., 16, 13131–13148, https://doi.org/10.5194/acp-16-13131-2016, https://doi.org/10.5194/acp-16-13131-2016, 2016
Xun Wang, Che-Jen Lin, Wei Yuan, Jonas Sommar, Wei Zhu, and Xinbin Feng
Atmos. Chem. Phys., 16, 11125–11143, https://doi.org/10.5194/acp-16-11125-2016, https://doi.org/10.5194/acp-16-11125-2016, 2016
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We developed a mechanistic model for estimating the emission of elemental mercury vapor (Hg0) from natural surfaces in China. The development implements recent advancements in the understanding of air–soil and air–foliage exchange of Hg0 and redox chemistry in soil and on surfaces, incorporates the effects of soil characteristics and landuse changes by agricultural activities, and is examined through a systematic set of sensitivity simulations.
Zhuyun Ye, Huiting Mao, Che-Jen Lin, and Su Youn Kim
Atmos. Chem. Phys., 16, 8461–8478, https://doi.org/10.5194/acp-16-8461-2016, https://doi.org/10.5194/acp-16-8461-2016, 2016
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In this study, a state-of-the-art chemical mechanism was incorporated into a box model to investigate the atmospheric Hg cycling in different environments. As a result, for each of the three environments, GOM diurnal cycles of over half the selected cases were reasonably represented by the box model. A realistic model can be a powerful tool, providing important information on atmospheric Hg cycling and implications for policy makers.
Phil-Goo Kang, Myron J. Mitchell, Patrick J. McHale, Charles T. Driscoll, Shreeram Inamdar, and Ji-Hyung Park
Biogeosciences, 13, 2787–2801, https://doi.org/10.5194/bg-13-2787-2016, https://doi.org/10.5194/bg-13-2787-2016, 2016
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Lakes play important roles in controlling organic matter derived from watersheds and within-lake production. The organic matter is normally measured by elemental quantities, such as carbon(C) and nitrogen(N), because the two elements are essential for aquatic ecosystems. We observed an decrease of C, but an increase of N in organic matters in a lake. The reason of the different pattern might be that inorganic N in the lake appeared to be recycled to produce organic N due to within-lake processes.
Wei Zhu, Che-Jen Lin, Xun Wang, Jonas Sommar, Xuewu Fu, and Xinbin Feng
Atmos. Chem. Phys., 16, 4451–4480, https://doi.org/10.5194/acp-16-4451-2016, https://doi.org/10.5194/acp-16-4451-2016, 2016
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Reliable quantification of air-surfaces flux of elemental mercury vapor (Hg0) is crucial for understanding Hg global biogeochemical cycles. In this study, we provide a comprehensive review on the state of science in the atmosphere-surface exchange of elemental Hg. We compiled an up-to-date global observational flux database and discuss the implication of flux data on global Hg budget. The knowledge gap and research needs for future measurements and modeling efforts were discussed.
Jonas Sommar, Wei Zhu, Lihai Shang, Che-Jen Lin, and Xinbin Feng
Biogeosciences, 13, 2029–2049, https://doi.org/10.5194/bg-13-2029-2016, https://doi.org/10.5194/bg-13-2029-2016, 2016
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A micrometeorological method (REA) has been implemented to assess the role of cereal crop fields in the North China Plain as a source or sink of elemental mercury vapor (Hg0) during the course of a full year. In combination with chamber measurements under the canopy, the above-canopy REA measurements provided evidence for a balance between Hg0 ground emissions and uptake of Hg0 by the crop foliage, with net emissions prevailing from the ecosystem during the majority of a year.
Lei Zhang, Shuxiao Wang, Qingru Wu, Fengyang Wang, Che-Jen Lin, Leiming Zhang, Mulin Hui, Mei Yang, Haitao Su, and Jiming Hao
Atmos. Chem. Phys., 16, 2417–2433, https://doi.org/10.5194/acp-16-2417-2016, https://doi.org/10.5194/acp-16-2417-2016, 2016
X. W. Fu, H. Zhang, B. Yu, X. Wang, C.-J. Lin, and X. B. Feng
Atmos. Chem. Phys., 15, 9455–9476, https://doi.org/10.5194/acp-15-9455-2015, https://doi.org/10.5194/acp-15-9455-2015, 2015
W. Zhu, J. Sommar, C.-J. Lin, and X. Feng
Atmos. Chem. Phys., 15, 5359–5376, https://doi.org/10.5194/acp-15-5359-2015, https://doi.org/10.5194/acp-15-5359-2015, 2015
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Bias and uncertainty in Hg flux measured by micrometeorological methods (MM) and dynamic flux chambers (DFCs) are assessed from two field inter-comparison campaigns.
DFC flux bias follows a diurnal cycle due to modified temperature and radiation balance inside the chamber.
The precision in concentration difference measurements poses critical constraint on obtaining a larger fraction of significant MM flux. Asynchronous sampling impairs flux accuracy under varying atmospheric Hg concentration.
X. W. Fu, H. Zhang, C.-J. Lin, X. B. Feng, L. X. Zhou, and S. X. Fang
Atmos. Chem. Phys., 15, 1013–1028, https://doi.org/10.5194/acp-15-1013-2015, https://doi.org/10.5194/acp-15-1013-2015, 2015
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This paper is the first to report correlation slopes of GEM/CO, GEM/CO2, GEM/CH4, CH4/CO, CH4/CO2, and CO/CO2 for mainland China, South Asia, the Indochinese Peninsula, and Central Asia, and applied the values to estimate GEM emissions in the four source regions. The estimated Hg0 emissions for mainland China, South Asia, the Indochinese Peninsula, and Central Asia using GEM/CO and GEM/CO2 correlation slopes are in the ranges of 1071-1187, 340-470, 125, and 54-90t, respectively.
H. Zhang, X. W. Fu, C.-J. Lin, X. Wang, and X. B. Feng
Atmos. Chem. Phys., 15, 653–665, https://doi.org/10.5194/acp-15-653-2015, https://doi.org/10.5194/acp-15-653-2015, 2015
W. Zhu, J. Sommar, C.-J. Lin, and X. Feng
Atmos. Chem. Phys., 15, 685–702, https://doi.org/10.5194/acp-15-685-2015, https://doi.org/10.5194/acp-15-685-2015, 2015
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Mercury vapor fluxes measured by the micrometeorological (MM) and dynamic flux chambers (DFCs) methods were compared. Distinct temporal trends existed between MM and DFCs fluxes; the novel chamber method provided net cumulative flux on a level with those derived by MM methods. Statistical analysis indicated that the medians of turbulent fluxes estimated by three MM techniques were not significantly different. Recommendations are given regarding the deployment of Hg flux quantification methods.
X. Wang, C.-J. Lin, and X. Feng
Atmos. Chem. Phys., 14, 6273–6287, https://doi.org/10.5194/acp-14-6273-2014, https://doi.org/10.5194/acp-14-6273-2014, 2014
Z. W. Wang, J. C. Gallet, C. A. Pedersen, X. S. Zhang, J. Ström, and Z. J. Ci
Atmos. Chem. Phys., 14, 629–640, https://doi.org/10.5194/acp-14-629-2014, https://doi.org/10.5194/acp-14-629-2014, 2014
Related subject area
Subject: Gases | Research Activity: Field Measurements | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
Variations and sources of volatile organic compounds (VOCs) in urban region: insights from measurements on a tall tower
Tropical peat fire emissions: 2019 field measurements in Sumatra and Borneo and synthesis with previous studies
Sulfuric acid in the Amazon basin: measurements and evaluation of existing sulfuric acid proxies
Seasonal variation in oxygenated organic molecules in urban Beijing and their contribution to secondary organic aerosol
Oxygenated volatile organic compounds (VOCs) as significant but varied contributors to VOC emissions from vehicles
The impacts of wildfires on ozone production and boundary layer dynamics in California's Central Valley
Distribution of hydrogen peroxide over Europe during the BLUESKY aircraft campaign
Eddy covariance measurements highlight sources of nitrogen oxide emissions missing from inventories for central London
Budget of nitrous acid (HONO) at an urban site in the fall season of Guangzhou, China
Long-term trend of ozone pollution in China during 2014–2020: distinct seasonal and spatial characteristics and ozone sensitivity
Investigation of new particle formation mechanisms and aerosol processes at Marambio Station, Antarctic Peninsula
Composition and Reactivity of Volatile Organic Compounds in the South Coast Air Basin and San Joaquin Valley of California
Measurement report: Variations in surface SO2 and NOx mixing ratios from 2004 to 2016 at a background site in the North China Plain
Fate of the nitrate radical at the summit of a semi-rural mountain site in Germany assessed with direct reactivity measurements
Spatiotemporal variations of the δ(O2 ∕ N2), CO2 and δ(APO) in the troposphere over the western North Pacific
OH and HO2 radical chemistry at a suburban site during the EXPLORE-YRD campaign in 2018
Towards reconstructing the Arctic atmospheric methane history over the 20th century: measurement and modelling results for the North Greenland Ice Core Project firn
Atmospheric gas-phase composition over the Indian Ocean
Joint occurrence of heatwaves and ozone pollution and increased health risks in Beijing, China: role of synoptic weather pattern and urbanization
Using atmospheric trace gas vertical profiles to evaluate model fluxes: a case study of Arctic-CAP observations and GEOS simulations for the ABoVE domain
An evaluation of new particle formation events in Helsinki during a Baltic Sea cyanobacterial summer bloom
Oceanic emissions of dimethyl sulfide and methanethiol and their contribution to sulfur dioxide production in the marine atmosphere
An investigation into the chemistry of HONO in the marine boundary layer at Tudor Hill Marine Atmospheric Observatory in Bermuda
Tropospheric ozone production and chemical regime analysis during the COVID-19 lockdown over Europe
Overview: On the transport and transformation of pollutants in the outflow of major population centres – observational data from the EMeRGe European intensive operational period in summer 2017
Interannual variability of terpenoid emissions in an alpine city
Observations and modelling of glyoxal in the tropical Atlantic marine boundary layer
Top-down and bottom-up estimates of anthropogenic methyl bromide emissions from eastern China
Direct measurements of ozone response to emissions perturbations in California
Reconciling the total carbon budget for boreal forest wildfire emissions using airborne observations
Ground-based investigation of HOx and ozone chemistry in biomass burning plumes in rural Idaho
Insights into the significant increase in ozone during COVID-19 in a typical urban city of China
Quantification and assessment of methane emissions from offshore oil and gas facilities on the Norwegian continental shelf
Full latitudinal marine atmospheric measurements of iodine monoxide
Direct observations indicate photodegradable oxygenated volatile organic compounds (OVOCs) as larger contributors to radicals and ozone production in the atmosphere
Assessing vehicle fuel efficiency using a dense network of CO2 observations
Odds and ends of atmospheric mercury in Europe and over the North Atlantic Ocean: temporal trends of 25 years of measurements
Interpretation of NO3–N2O5 observation via steady state in high-aerosol air mass: the impact of equilibrium coefficient in ambient conditions
Global emissions of perfluorocyclobutane (PFC-318, c-C4F8) resulting from the use of hydrochlorofluorocarbon-22 (HCFC-22) feedstock to produce polytetrafluoroethylene (PTFE) and related fluorochemicals
Atmospheric measurements at Mt. Tai – Part I: HONO formation and its role in the oxidizing capacity of the upper boundary layer
Urban inland wintertime N2O5 and ClNO2 influenced by snow-covered ground, air turbulence, and precipitation
First observation of mercury species on an important water vapor channel in the southeastern Tibetan Plateau
Swiss halocarbon emissions for 2019 to 2020 assessed from regional atmospheric observations
Radical chemistry in the Pearl River Delta: observations and modeling of OH and HO2 radicals in Shenzhen 2018
Measurement report: Long-term measurements of aerosol precursor concentrations in the Finnish subarctic boreal forest
The Fires, Asian, and Stratospheric Transport–Las Vegas Ozone Study (FAST-LVOS)
Measurement report: Intra-, inter-annual variability and source apportionment of VOCs during 2018–2020 in Zhengzhou, Central China
Measurement report: Long-term variations in surface NOx and SO2 mixing ratios from 2006 to 2016 at a background site in the Yangtze River Delta region, China
Atmospheric measurements at Mt. Tai – Part II: HONO budget and radical (ROx + NO3) chemistry in the lower boundary layer
Exploration of the atmospheric chemistry of nitrous acid in a coastal city of southeastern China: results from measurements across four seasons
Xiao-Bing Li, Bin Yuan, Sihang Wang, Chunlin Wang, Jing Lan, Zhijie Liu, Yongxin Song, Xianjun He, Yibo Huangfu, Chenglei Pei, Peng Cheng, Suxia Yang, Jipeng Qi, Caihong Wu, Shan Huang, Yingchang You, Ming Chang, Huadan Zheng, Wenda Yang, Xuemei Wang, and Min Shao
Atmos. Chem. Phys., 22, 10567–10587, https://doi.org/10.5194/acp-22-10567-2022, https://doi.org/10.5194/acp-22-10567-2022, 2022
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High-time-resolution measurements of volatile organic compounds (VOCs) were made using an online mass spectrometer at a 600 m tall tower in urban region. Compositions, temporal variations, and sources of VOCs were quantitatively investigated in this study. We find that VOC measurements in urban regions aloft could better characterize source characteristics of anthropogenic emissions. Our results could provide important implications in making future strategies for control of VOCs.
Robert J. Yokelson, Bambang H. Saharjo, Chelsea E. Stockwell, Erianto I. Putra, Thilina Jayarathne, Acep Akbar, Israr Albar, Donald R. Blake, Laura L. B. Graham, Agus Kurniawan, Simone Meinardi, Diah Ningrum, Ati D. Nurhayati, Asmadi Saad, Niken Sakuntaladewi, Eko Setianto, Isobel J. Simpson, Elizabeth A. Stone, Sigit Sutikno, Andri Thomas, Kevin C. Ryan, and Mark A. Cochrane
Atmos. Chem. Phys., 22, 10173–10194, https://doi.org/10.5194/acp-22-10173-2022, https://doi.org/10.5194/acp-22-10173-2022, 2022
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Fire plus non-fire GHG emissions associated with draining peatlands are the largest per area of any land use change considered by the IPCC. To characterize average and variability for tropical peat fire emissions, highly mobile smoke sampling teams were deployed across four Indonesian provinces to explore an extended interannual, climatic, and spatial range. Large adjustments to IPCC-recommended emissions are suggested. Lab data bolster an extensive emissions database for tropical peat fires.
Deanna C. Myers, Saewung Kim, Steven Sjostedt, Alex B. Guenther, Roger Seco, Oscar Vega Bustillos, Julio Tota, Rodrigo A. F. Souza, and James N. Smith
Atmos. Chem. Phys., 22, 10061–10076, https://doi.org/10.5194/acp-22-10061-2022, https://doi.org/10.5194/acp-22-10061-2022, 2022
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We present the first measurements of gas-phase sulfuric acid from the Amazon basin and evaluate the efficacy of existing sulfuric acid parameterizations in this understudied region. Sulfuric acid is produced during the daytime and nighttime, though current proxies underestimate nighttime production. These results illustrate the need for better parameterizations of sulfuric acid and its precursors that are informed by measurements across a broad range of locations.
Yishuo Guo, Chao Yan, Yuliang Liu, Xiaohui Qiao, Feixue Zheng, Ying Zhang, Ying Zhou, Chang Li, Xiaolong Fan, Zhuohui Lin, Zemin Feng, Yusheng Zhang, Penggang Zheng, Linhui Tian, Wei Nie, Zhe Wang, Dandan Huang, Kaspar R. Daellenbach, Lei Yao, Lubna Dada, Federico Bianchi, Jingkun Jiang, Yongchun Liu, Veli-Matti Kerminen, and Markku Kulmala
Atmos. Chem. Phys., 22, 10077–10097, https://doi.org/10.5194/acp-22-10077-2022, https://doi.org/10.5194/acp-22-10077-2022, 2022
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Gaseous oxygenated organic molecules (OOMs) are able to form atmospheric aerosols, which will impact on human health and climate change. Here, we find that OOMs in urban Beijing are dominated by anthropogenic sources, i.e. aromatic (29 %–41 %) and aliphatic (26 %–41 %) OOMs. They are also the main contributors to the condensational growth of secondary organic aerosols (SOAs). Therefore, the restriction on anthropogenic VOCs is crucial for the reduction of SOAs and haze formation.
Sihang Wang, Bin Yuan, Caihong Wu, Chaomin Wang, Tiange Li, Xianjun He, Yibo Huangfu, Jipeng Qi, Xiao-Bing Li, Qing'e Sha, Manni Zhu, Shengrong Lou, Hongli Wang, Thomas Karl, Martin Graus, Zibing Yuan, and Min Shao
Atmos. Chem. Phys., 22, 9703–9720, https://doi.org/10.5194/acp-22-9703-2022, https://doi.org/10.5194/acp-22-9703-2022, 2022
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Volatile organic compound (VOC) emissions from vehicles are measured using online mass spectrometers. Differences between gasoline and diesel vehicles are observed with higher emission factors of most oxygenated VOCs (OVOCs) and heavier aromatics from diesel vehicles. A higher aromatics / toluene ratio could provide good indicators to distinguish emissions from both vehicle types. We show that OVOCs account for significant contributions to VOC emissions from vehicles, especially diesel vehicles.
Keming Pan and Ian C. Faloona
Atmos. Chem. Phys., 22, 9681–9702, https://doi.org/10.5194/acp-22-9681-2022, https://doi.org/10.5194/acp-22-9681-2022, 2022
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This work represents a unique analysis of 10 existing air quality network sites and meteorological sites, two AmeriFlux sites, and a radio acoustic sounding system in the Central Valley of California during five consecutive fire seasons, June through September, from 2016 to 2020. We find that the ozone production rate increases by ~ 50 % during wildfire influenced periods. Wildfire smoke also decreases the heat flux by 30 % and results in 12 % lower mixed-layer height.
Zaneta T. Hamryszczak, Andrea Pozzer, Florian Obersteiner, Birger Bohn, Benedikt Steil, Jos Lelieveld, and Horst Fischer
Atmos. Chem. Phys., 22, 9483–9497, https://doi.org/10.5194/acp-22-9483-2022, https://doi.org/10.5194/acp-22-9483-2022, 2022
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Hydrogen peroxide plays a pivotal role in the chemistry of the atmosphere. Together with organic hydroperoxides, it forms a reservoir for peroxy radicals, which are known to be the key contributors to the self-cleaning processes of the atmosphere. Hydroperoxides were measured over Europe during the BLUESKY campaign in May–June 2020. The paper gives an overview of the distribution of the species in the troposphere and investigates the impact of wet scavenging and deposition on the budget of H2O2.
Will S. Drysdale, Adam R. Vaughan, Freya A. Squires, Sam J. Cliff, Stefan Metzger, David Durden, Natchaya Pingintha-Durden, Carole Helfter, Eiko Nemitz, C. Sue B. Grimmond, Janet Barlow, Sean Beevers, Gregor Stewart, David Dajnak, Ruth M. Purvis, and James D. Lee
Atmos. Chem. Phys., 22, 9413–9433, https://doi.org/10.5194/acp-22-9413-2022, https://doi.org/10.5194/acp-22-9413-2022, 2022
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Measurements of NOx emissions are important for a good understanding of air quality. While there are many direct measurements of NOx concentration, there are very few measurements of its emission. Measurements of emissions provide constraints on emissions inventories and air quality models. This article presents measurements of NOx emission from the BT Tower in central London in 2017 and compares them with inventories, finding that they underestimate by a factor of ∼1.48.
Yihang Yu, Peng Cheng, Huirong Li, Wenda Yang, Baobin Han, Wei Song, Weiwei Hu, Xinming Wang, Bin Yuan, Min Shao, Zhijiong Huang, Zhen Li, Junyu Zheng, Haichao Wang, and Xiaofang Yu
Atmos. Chem. Phys., 22, 8951–8971, https://doi.org/10.5194/acp-22-8951-2022, https://doi.org/10.5194/acp-22-8951-2022, 2022
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We have investigated the budget of HONO at an urban site in Guangzhou. Budget and comprehensive uncertainty analysis suggest that at such locations as ours, HONO direct emissions and NO + OH can become comparable or even surpass other HONO sources that typically receive greater attention and interest, such as the NO2 heterogeneous source and the unknown daytime photolytic source. Our findings emphasize the need to reduce the uncertainties of both conventional and novel HONO sources and sinks.
Wenjie Wang, David D. Parrish, Siwen Wang, Fengxia Bao, Ruijing Ni, Xin Li, Suding Yang, Hongli Wang, Yafang Cheng, and Hang Su
Atmos. Chem. Phys., 22, 8935–8949, https://doi.org/10.5194/acp-22-8935-2022, https://doi.org/10.5194/acp-22-8935-2022, 2022
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Tropospheric ozone is an air pollutant that is detrimental to human health, vegetation and ecosystem productivity. A comprehensive characterisation of the spatial and temporal distribution of tropospheric ozone is critical to our understanding of these issues. Here we summarise this distribution over China from the available observational records to the extent possible. This study provides insights into efficient future ozone control strategies in China.
Lauriane L. J. Quéléver, Lubna Dada, Eija Asmi, Janne Lampilahti, Tommy Chan, Jonathan E. Ferrara, Gustavo E. Copes, German Pérez-Fogwill, Luis Barreira, Minna Aurela, Douglas R. Worsnop, Tuija Jokinen, and Mikko Sipilä
Atmos. Chem. Phys., 22, 8417–8437, https://doi.org/10.5194/acp-22-8417-2022, https://doi.org/10.5194/acp-22-8417-2022, 2022
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Understanding how aerosols form is crucial for correctly modeling the climate and improving future predictions. This work provides extensive analysis of aerosol particles and their precursors at Marambio Station, Antarctic Peninsula. We show that sulfuric acid, ammonia, and dimethylamine are key contributors to the frequent new particle formation events observed at the site. We discuss nucleation mechanisms and highlight the need for targeted measurement to fully understand these processes.
Shang Liu, Barbara Barletta, Rebecca S. Hornbrook, Alan Fried, Jeff Peischl, Simone Meinardi, Matthew Coggon, Aaron Lamplugh, Jessica B. Gilman, Georgios I. Gkatzelis, Carsten Warneke, Eric C. Apel, Alan J. Hills, Ilann Bourgeois, James Walega, Petter Weibring, Dirk Richter, Toshihiro Kuwayama, Michael FitzGibbon, and Donald Blake
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2022-399, https://doi.org/10.5194/acp-2022-399, 2022
Revised manuscript accepted for ACP
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California’s ozone persistently exceeds the air quality standards. We studied the spatial distribution of volatile organic compounds (VOCs) that produce ozone over the most polluted regions in California using aircraft measurements. We find that the oxygenated VOCs have the highest ozone formation potential. Spatially, biogenic VOCs are important during high ozone episodes in the South Coast Air Basin, while dairy emissions may be critical for ozone production in the San Joaquin Valley.
Xueli Liu, Liang Ran, Weili Lin, Xiaobin Xu, Zhiqiang Ma, Fan Dong, Di He, Liyan Zhou, Qingfeng Shi, and Yao Wang
Atmos. Chem. Phys., 22, 7071–7085, https://doi.org/10.5194/acp-22-7071-2022, https://doi.org/10.5194/acp-22-7071-2022, 2022
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Significant decreases in annual mean NOx from 2011 to 2016 and SO2 from 2008 to 2016 confirm the effectiveness of relevant control measures on the reduction in NOx and SO2 emissions in the North China Plain (NCP). NOx at SDZ had a weaker influence than SO2 on the emission reduction in Beijing and other areas in the NCP. An increase in the number of motor vehicles and weak traffic restrictions have caused vehicle emissions of NOx, which indicates that NOx emission control should be strengthened.
Patrick Dewald, Clara M. Nussbaumer, Jan Schuladen, Akima Ringsdorf, Achim Edtbauer, Horst Fischer, Jonathan Williams, Jos Lelieveld, and John N. Crowley
Atmos. Chem. Phys., 22, 7051–7069, https://doi.org/10.5194/acp-22-7051-2022, https://doi.org/10.5194/acp-22-7051-2022, 2022
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We measured the gas-phase reactivity of the NO3 radical on the summit (825 m a.s.l.) of a semi-rural mountain in southwestern Germany in July 2021. The impact of VOC-induced NO3 losses (mostly monoterpenes) competing with a loss by reaction with NO and photolysis throughout the diel cycle was estimated. Besides chemistry, boundary layer dynamics and plant-physiological processes presumably have a great impact on our observations, which were compared to previous NO3 measurements at the same site.
Shigeyuki Ishidoya, Kazuhiro Tsuboi, Yosuke Niwa, Hidekazu Matsueda, Shohei Murayama, Kentaro Ishijima, and Kazuyuki Saito
Atmos. Chem. Phys., 22, 6953–6970, https://doi.org/10.5194/acp-22-6953-2022, https://doi.org/10.5194/acp-22-6953-2022, 2022
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The atmospheric O2 / N2 ratio and CO2 concentration over the western North Pacific are presented. We found significant modification of the seasonal APO cycle in the middle troposphere due to the interhemispheric mixing of air. APO driven by the net marine biological activities indicated annual sea–air O2 flux during El Niño. Terrestrial biospheric and oceanic CO2 uptakes during 2012–2019 were estimated to be 1.8 and 2.8 Pg C a−1, respectively.
Xuefei Ma, Zhaofeng Tan, Keding Lu, Xinping Yang, Xiaorui Chen, Haichao Wang, Shiyi Chen, Xin Fang, Shule Li, Xin Li, Jingwei Liu, Ying Liu, Shengrong Lou, Wanyi Qiu, Hongli Wang, Limin Zeng, and Yuanhang Zhang
Atmos. Chem. Phys., 22, 7005–7028, https://doi.org/10.5194/acp-22-7005-2022, https://doi.org/10.5194/acp-22-7005-2022, 2022
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This paper presents the first OH and HO2 radical observations made in the Yangtze River Delta in China, and strong oxidation capacity is discovered based on direct measurements. The impacts of new OH regeneration mechanisms, monoterpene oxidation, and HO2 uptake processes are examined and discussed. The sources and the factors to sustain such strong oxidation are the key to understanding the ozone pollution formed in this area.
Taku Umezawa, Satoshi Sugawara, Kenji Kawamura, Ikumi Oyabu, Stephen J. Andrews, Takuya Saito, Shuji Aoki, and Takakiyo Nakazawa
Atmos. Chem. Phys., 22, 6899–6917, https://doi.org/10.5194/acp-22-6899-2022, https://doi.org/10.5194/acp-22-6899-2022, 2022
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Greenhouse gas methane in the Arctic atmosphere has not been accurately reported for 1900–1980 from either direct observations or ice core reconstructions. By using trace gas data from firn (compacted snow layers above ice sheet), air samples at two Greenland sites, and a firn air transport model, this study suggests a likely range of the Arctic methane reconstruction for the 20th century. Atmospheric scenarios from two previous studies are also evaluated for consistency with the firn data sets.
Susann Tegtmeier, Christa Marandino, Yue Jia, Birgit Quack, and Anoop S. Mahajan
Atmos. Chem. Phys., 22, 6625–6676, https://doi.org/10.5194/acp-22-6625-2022, https://doi.org/10.5194/acp-22-6625-2022, 2022
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In the atmosphere over the Indian Ocean, intense anthropogenic pollution from Southeast Asia mixes with pristine oceanic air. During the winter monsoon, high pollution levels are regularly observed over the entire northern Indian Ocean, while during the summer monsoon, clean air dominates. Here, we review current progress in detecting and understanding atmospheric gas-phase composition over the Indian Ocean and its impacts on the upper atmosphere, oceanic biogeochemistry, and marine ecosystems.
Lian Zong, Yuanjian Yang, Haiyun Xia, Meng Gao, Zhaobin Sun, Zuofang Zheng, Xianxiang Li, Guicai Ning, Yubin Li, and Simone Lolli
Atmos. Chem. Phys., 22, 6523–6538, https://doi.org/10.5194/acp-22-6523-2022, https://doi.org/10.5194/acp-22-6523-2022, 2022
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Heatwaves (HWs) paired with higher ozone (O3) concentration at surface level pose a serious threat to human health. Taking Beijing as an example, three unfavorable synoptic weather patterns were identified to dominate the compound HW and O3 pollution events. Under the synergistic stress of HWs and O3 pollution, public mortality risk increased, and synoptic patterns and urbanization enhanced the compound risk of events in Beijing by 33.09 % and 18.95 %, respectively.
Colm Sweeney, Abhishek Chatterjee, Sonja Wolter, Kathryn McKain, Robert Bogue, Stephen Conley, Tim Newberger, Lei Hu, Lesley Ott, Benjamin Poulter, Luke Schiferl, Brad Weir, Zhen Zhang, and Charles E. Miller
Atmos. Chem. Phys., 22, 6347–6364, https://doi.org/10.5194/acp-22-6347-2022, https://doi.org/10.5194/acp-22-6347-2022, 2022
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The Arctic Carbon Atmospheric Profiles (Arctic-CAP) project demonstrates the utility of aircraft profiles for independent evaluation of model-derived emissions and uptake of atmospheric CO2, CH4, and CO from land and ocean. Comparison with the Goddard Earth Observing System (GEOS) modeling system suggests that fluxes of CO2 are very consistent with observations, while those of CH4 have some regional and seasonal biases, and that CO comparison is complicated by transport errors.
Roseline C. Thakur, Lubna Dada, Lisa J. Beck, Lauriane L. J. Quéléver, Tommy Chan, Marjan Marbouti, Xu-Cheng He, Carlton Xavier, Juha Sulo, Janne Lampilahti, Markus Lampimäki, Yee Jun Tham, Nina Sarnela, Katrianne Lehtipalo, Alf Norkko, Markku Kulmala, Mikko Sipilä, and Tuija Jokinen
Atmos. Chem. Phys., 22, 6365–6391, https://doi.org/10.5194/acp-22-6365-2022, https://doi.org/10.5194/acp-22-6365-2022, 2022
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Every year intense cyanobacterial and macroalgal blooms occur in the Baltic Sea and in the coastal areas surrounding Helsinki, yet no studies have addressed the impact of biogenic emissions from these blooms on gas vapor concentrations, which in turn could influence new particle formation. This is the first study of its kind to address the chemistry driving new particle formation (NPF) during a bloom period in this region, highlighting the role of biogenic sulfuric acid and iodic acid.
Gordon A. Novak, Delaney B. Kilgour, Christopher M. Jernigan, Michael P. Vermeuel, and Timothy H. Bertram
Atmos. Chem. Phys., 22, 6309–6325, https://doi.org/10.5194/acp-22-6309-2022, https://doi.org/10.5194/acp-22-6309-2022, 2022
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We describe field measurements of the mixing ratio and oceanic emission flux of dimethyl sulfide (DMS) and methanethiol (MeSH) from a coastal ocean site. DMS is known to impact aerosol formation and growth in the marine atmosphere, influencing cloud formation and climate. Measurements of MeSH, which is produced by the same oceanic source as DMS, are rare. We show that MeSH emissions are large and must be measured alongside DMS to understand marine sulfur chemistry and aerosol formation.
Yuting Zhu, Youfeng Wang, Xianliang Zhou, Yasin F. Elshorbany, Chunxiang Ye, Matthew Hayden, and Andrew J. Peters
Atmos. Chem. Phys., 22, 6327–6346, https://doi.org/10.5194/acp-22-6327-2022, https://doi.org/10.5194/acp-22-6327-2022, 2022
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The daytime chemistry of nitrous acid (HONO), which plays an important role in the oxidation capacity of the troposphere, is not well understood. In this work, we report new field measurement results of HONO and the relevant parameters in the marine boundary layer at Tudor Hill Marine Atmospheric Observatory in Bermuda. We evaluate the daytime HONO budgets in air masses under different types of interaction with the island and examine the strengths of different HONO formation and loss mechanisms.
Clara M. Nussbaumer, Andrea Pozzer, Ivan Tadic, Lenard Röder, Florian Obersteiner, Hartwig Harder, Jos Lelieveld, and Horst Fischer
Atmos. Chem. Phys., 22, 6151–6165, https://doi.org/10.5194/acp-22-6151-2022, https://doi.org/10.5194/acp-22-6151-2022, 2022
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The European COVID-19 lockdowns have significantly reduced the emission of primary pollutants such as NOx, which impacts the tropospheric photochemical processes and the abundance of O3. In this study, we present how the lockdowns have affected tropospheric trace gases and ozone production based on in situ observations and modeling simulations. We additionally show that the chemical regime shifted from a transition point to a NOx limitation in the upper troposphere.
M. Dolores Andrés Hernández, Andreas Hilboll, Helmut Ziereis, Eric Förster, Ovid O. Krüger, Katharina Kaiser, Johannes Schneider, Francesca Barnaba, Mihalis Vrekoussis, Jörg Schmidt, Heidi Huntrieser, Anne-Marlene Blechschmidt, Midhun George, Vladyslav Nenakhov, Theresa Harlass, Bruna A. Holanda, Jennifer Wolf, Lisa Eirenschmalz, Marc Krebsbach, Mira L. Pöhlker, Anna B. Kalisz Hedegaard, Linlu Mei, Klaus Pfeilsticker, Yangzhuoran Liu, Ralf Koppmann, Hans Schlager, Birger Bohn, Ulrich Schumann, Andreas Richter, Benjamin Schreiner, Daniel Sauer, Robert Baumann, Mariano Mertens, Patrick Jöckel, Markus Kilian, Greta Stratmann, Christopher Pöhlker, Monica Campanelli, Marco Pandolfi, Michael Sicard, José L. Gómez-Amo, Manuel Pujadas, Katja Bigge, Flora Kluge, Anja Schwarz, Nikos Daskalakis, David Walter, Andreas Zahn, Ulrich Pöschl, Harald Bönisch, Stephan Borrmann, Ulrich Platt, and John P. Burrows
Atmos. Chem. Phys., 22, 5877–5924, https://doi.org/10.5194/acp-22-5877-2022, https://doi.org/10.5194/acp-22-5877-2022, 2022
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EMeRGe provides a unique set of in situ and remote sensing airborne measurements of trace gases and aerosol particles along selected flight routes in the lower troposphere over Europe. The interpretation uses also complementary collocated ground-based and satellite measurements. The collected data help to improve the current understanding of the complex spatial distribution of trace gases and aerosol particles resulting from mixing, transport, and transformation of pollution plumes over Europe.
Lisa Kaser, Arianna Peron, Martin Graus, Marcus Striednig, Georg Wohlfahrt, Stanislav Juráň, and Thomas Karl
Atmos. Chem. Phys., 22, 5603–5618, https://doi.org/10.5194/acp-22-5603-2022, https://doi.org/10.5194/acp-22-5603-2022, 2022
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Biogenic volatile organic compounds (e.g., terpenoids) play an essential role in atmospheric chemistry. Urban greening activities need to consider the ozone- and aerosol-forming potential of these compounds released from vegetation. NMVOC emissions in urban environments are complex, and the biogenic component remains poorly quantified. For summer conditions biogenic emissions dominate terpene emissions and heat waves can significantly modulate urban biogenic terpenoid emissions.
Hannah Walker, Daniel Stone, Trevor Ingham, Sina Hackenberg, Danny Cryer, Shalini Punjabi, Katie Read, James Lee, Lisa Whalley, Dominick V. Spracklen, Lucy J. Carpenter, Steve R. Arnold, and Dwayne E. Heard
Atmos. Chem. Phys., 22, 5535–5557, https://doi.org/10.5194/acp-22-5535-2022, https://doi.org/10.5194/acp-22-5535-2022, 2022
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Glyoxal is a ubiquitous reactive organic compound in the atmosphere, which may form organic aerosol and impact the atmosphere's oxidising capacity. There are limited measurements of glyoxal's abundance in the remote marine atmosphere. We made new measurements of glyoxal using a highly sensitive technique over two 4-week periods in the tropical Atlantic atmosphere. We show that daytime measurements are mostly consistent with our chemical understanding but a potential missing source at night.
Haklim Choi, Mi-Kyung Park, Paul J. Fraser, Hyeri Park, Sohyeon Geum, Jens Mühle, Jooil Kim, Ian Porter, Peter K. Salameh, Christina M. Harth, Bronwyn L. Dunse, Paul B. Krummel, Ray F. Weiss, Simon O'Doherty, Dickon Young, and Sunyoung Park
Atmos. Chem. Phys., 22, 5157–5173, https://doi.org/10.5194/acp-22-5157-2022, https://doi.org/10.5194/acp-22-5157-2022, 2022
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We observed 12-year continuous CH3Br pollution signals at Gosan and estimated anthropogenic CH3Br emissions in eastern China. The analysis revealed a significant discrepancy between top-down estimates and the bottom-up emissions from the fumigation usage reported to the United Nations Environment Programme, likely due to unreported or inaccurately reported fumigation usage. This result provides information to monitor international compliance with the Montreal Protocol.
Shenglun Wu, Hyung Joo Lee, Andrea Anderson, Shang Liu, Toshihiro Kuwayama, John H. Seinfeld, and Michael J. Kleeman
Atmos. Chem. Phys., 22, 4929–4949, https://doi.org/10.5194/acp-22-4929-2022, https://doi.org/10.5194/acp-22-4929-2022, 2022
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An ozone control experiment usually conducted in the laboratory was installed in a trailer and moved to the outdoor environment to directly confirm that we are controlling the right sources in order to lower ambient ozone concentrations. Adding small amounts of precursor oxides of nitrogen and volatile organic compounds to ambient air showed that the highest ozone concentrations are best controlled by reducing concentrations of oxides of nitrogen. The results confirm satellite measurements.
Katherine Hayden, Shao-Meng Li, John Liggio, Michael Wheeler, Jeremy Wentzell, Amy Leithead, Peter Brickell, Richard Mittermeier, Zachary Oldham, Cris Mihele, Ralf Staebler, Samar Moussa, Andrea Darlington, Alexandra Steffen, Mengistu Wolde, Daniel Thompson, Jack Chen, Debora Griffin, Ellen Eckert, Jenna Ditto, Megan He, and Drew Gentner
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2022-245, https://doi.org/10.5194/acp-2022-245, 2022
Revised manuscript accepted for ACP
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In this study, airborne measurements provided the most detailed characterization, to date, of boreal forest wildfire emissions. Measurements showed a large diversity of air pollutants expanding the volatility range typically reported. A large portion of organic species was unidentified, likely comprised of complex organic compounds. Aircraft-derived emissions improve wildfire chemical speciation and can support reliable model predictions of pollution from boreal forest wildfires.
Andrew J. Lindsay, Daniel C. Anderson, Rebecca A. Wernis, Yutong Liang, Allen H. Goldstein, Scott C. Herndon, Joseph R. Roscioli, Christoph Dyroff, Ed C. Fortner, Philip L. Croteau, Francesca Majluf, Jordan E. Krechmer, Tara I. Yacovitch, Walter B. Knighton, and Ezra C. Wood
Atmos. Chem. Phys., 22, 4909–4928, https://doi.org/10.5194/acp-22-4909-2022, https://doi.org/10.5194/acp-22-4909-2022, 2022
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Wildfire smoke dramatically impacts air quality and often has elevated concentrations of ozone. We present measurements of ozone and its precursors at a rural site periodically impacted by wildfire smoke. Measurements of total peroxy radicals, key ozone precursors that have been studied little within wildfires, compare well with chemical box model predictions. Our results indicate no serious issues with using current chemistry mechanisms to model chemistry in aged wildfire plumes.
Kun Zhang, Zhiqiang Liu, Xiaojuan Zhang, Qing Li, Andrew Jensen, Wen Tan, Ling Huang, Yangjun Wang, Joost de Gouw, and Li Li
Atmos. Chem. Phys., 22, 4853–4866, https://doi.org/10.5194/acp-22-4853-2022, https://doi.org/10.5194/acp-22-4853-2022, 2022
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A significant increase in O3 concentrations was found during the lockdown period of COVID-19 in most areas of China. By field measurements coupled with machine learning, an observation-based model (OBM) and sensitivity analysis, we found the changes in the NOx / VOC ratio were a key reason for the significant rise in O3. To restrain O3 pollution, more efforts should be devoted to the control of anthropogenic OVOCs, alkenes and aromatics.
Amy Foulds, Grant Allen, Jacob T. Shaw, Prudence Bateson, Patrick A. Barker, Langwen Huang, Joseph R. Pitt, James D. Lee, Shona E. Wilde, Pamela Dominutti, Ruth M. Purvis, David Lowry, James L. France, Rebecca E. Fisher, Alina Fiehn, Magdalena Pühl, Stéphane J. B. Bauguitte, Stephen A. Conley, Mackenzie L. Smith, Tom Lachlan-Cope, Ignacio Pisso, and Stefan Schwietzke
Atmos. Chem. Phys., 22, 4303–4322, https://doi.org/10.5194/acp-22-4303-2022, https://doi.org/10.5194/acp-22-4303-2022, 2022
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We measured CH4 emissions from 21 offshore oil and gas facilities in the Norwegian Sea in 2019. Measurements compared well with operator-reported emissions but were greatly underestimated when compared with a 2016 global fossil fuel inventory. This study demonstrates the need for up-to-date and accurate inventories for use in research and policy and the important benefits of best-practice reporting methods by operators. Airborne measurements are an effective tool to validate such inventories.
Hisahiro Takashima, Yugo Kanaya, Saki Kato, Martina M. Friedrich, Michel Van Roozendael, Fumikazu Taketani, Takuma Miyakawa, Yuichi Komazaki, Carlos A. Cuevas, Alfonso Saiz-Lopez, and Takashi Sekiya
Atmos. Chem. Phys., 22, 4005–4018, https://doi.org/10.5194/acp-22-4005-2022, https://doi.org/10.5194/acp-22-4005-2022, 2022
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We have undertaken atmospheric iodine monoxide (IO) observations in the global marine boundary layer with a wide latitudinal coverage and sea surface temperature (SST) range. We conclude that atmospheric iodine is abundant over the Western Pacific warm pool, appearing as an iodine fountain, where ozone (O3) minima occur. Our study also found negative correlations between IO and O3 concentrations over IO maxima, which requires reconsideration of the initiation process of halogen activation.
Wenjie Wang, Bin Yuan, Yuwen Peng, Hang Su, Yafang Cheng, Suxia Yang, Caihong Wu, Jipeng Qi, Fengxia Bao, Yibo Huangfu, Chaomin Wang, Chenshuo Ye, Zelong Wang, Baolin Wang, Xinming Wang, Wei Song, Weiwei Hu, Peng Cheng, Manni Zhu, Junyu Zheng, and Min Shao
Atmos. Chem. Phys., 22, 4117–4128, https://doi.org/10.5194/acp-22-4117-2022, https://doi.org/10.5194/acp-22-4117-2022, 2022
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From thorough measurements of numerous oxygenated volatile organic compounds, we show that their photodissociation can be important for radical production and ozone formation in the atmosphere. This effect was underestimated in previous studies, as measurements of them were lacking.
Helen L. Fitzmaurice, Alexander J. Turner, Jinsol Kim, Katherine Chan, Erin R. Delaria, Catherine Newman, Paul Wooldridge, and Ronald C. Cohen
Atmos. Chem. Phys., 22, 3891–3900, https://doi.org/10.5194/acp-22-3891-2022, https://doi.org/10.5194/acp-22-3891-2022, 2022
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On-road emissions are thought to vary widely from existing predictions, as the effects of the age of the vehicle fleet, the performance of emission control systems, and variations in speed are difficult to assess under ambient driving conditions. We present an observational approach to characterize on-road emissions and show that the method is consistent with other approaches to within ~ 3 %.
Danilo Custódio, Katrine Aspmo Pfaffhuber, T. Gerard Spain, Fidel F. Pankratov, Iana Strigunova, Koketso Molepo, Henrik Skov, Johannes Bieser, and Ralf Ebinghaus
Atmos. Chem. Phys., 22, 3827–3840, https://doi.org/10.5194/acp-22-3827-2022, https://doi.org/10.5194/acp-22-3827-2022, 2022
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As a poison in the air that we breathe and the food that we eat, mercury is a human health concern for society as a whole. In that regard, this work deals with monitoring and modelling mercury in the environment, improving wherewithal, identifying the strength of the different components at play, and interpreting information to support the efforts that seek to safeguard public health.
Xiaorui Chen, Haichao Wang, and Keding Lu
Atmos. Chem. Phys., 22, 3525–3533, https://doi.org/10.5194/acp-22-3525-2022, https://doi.org/10.5194/acp-22-3525-2022, 2022
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We use a complete set of simulations to evaluate whether equilibrium and steady state are appropriate for a chemical system involving several reactive nitrogen-containing species (NO2, NO3, and N2O5) under various conditions. A previously neglected bias for the coefficient applied for interpreting their effects is disclosed, and the relevant ambient factors are examined. We therefore provide a good solution to an accurate representation of nighttime chemistry in high-aerosol areas.
Jens Mühle, Lambert J. M. Kuijpers, Kieran M. Stanley, Matthew Rigby, Luke M. Western, Jooil Kim, Sunyoung Park, Christina M. Harth, Paul B. Krummel, Paul J. Fraser, Simon O'Doherty, Peter K. Salameh, Roland Schmidt, Dickon Young, Ronald G. Prinn, Ray H. J. Wang, and Ray F. Weiss
Atmos. Chem. Phys., 22, 3371–3378, https://doi.org/10.5194/acp-22-3371-2022, https://doi.org/10.5194/acp-22-3371-2022, 2022
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Emissions of the strong greenhouse gas perfluorocyclobutane (c-C4F8) into the atmosphere have been increasing sharply since the early 2000s. These c-C4F8 emissions are highly correlated with the amount of hydrochlorofluorocarbon-22 produced to synthesize polytetrafluoroethylene (known for its non-stick properties) and related chemicals. From this process, c-C4F8 by-product is vented to the atmosphere. Avoiding these unnecessary c-C4F8 emissions could reduce the climate impact of this industry.
Chaoyang Xue, Can Ye, Jörg Kleffmann, Chenglong Zhang, Valéry Catoire, Fengxia Bao, Abdelwahid Mellouki, Likun Xue, Jianmin Chen, Keding Lu, Yong Zhao, Hengde Liu, Zhaoxin Guo, and Yujing Mu
Atmos. Chem. Phys., 22, 3149–3167, https://doi.org/10.5194/acp-22-3149-2022, https://doi.org/10.5194/acp-22-3149-2022, 2022
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Summertime measurements of nitrous acid (HONO) and related parameters were conducted at the foot and the summit of Mt. Tai (1534 m above sea level). We proposed a rapid vertical air mass exchange between the foot and the summit level, which enhances the role of HONO in the oxidizing capacity of the upper boundary layer. Kinetics for aerosol-derived HONO sources were constrained. HONO formation from different paths was quantified and discussed.
Kathryn D. Kulju, Stephen M. McNamara, Qianjie Chen, Hannah S. Kenagy, Jacinta Edebeli, Jose D. Fuentes, Steven B. Bertman, and Kerri A. Pratt
Atmos. Chem. Phys., 22, 2553–2568, https://doi.org/10.5194/acp-22-2553-2022, https://doi.org/10.5194/acp-22-2553-2022, 2022
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N2O5 uptake by chloride-containing surfaces produces ClNO2, which photolyzes, producing NO2 and highly reactive Cl radicals that impact air quality. In the inland urban atmosphere, ClNO2 was elevated during lower air turbulence and over snow-covered ground, from snowpack ClNO2 production. N2O5 and ClNO2 levels were lowest, on average, during rainfall and fog because of scavenging, with N2O5 scavenging by fog droplets likely contributing to observed increased particulate nitrate concentrations.
Huiming Lin, Yindong Tong, Chenghao Yu, Long Chen, Xiufeng Yin, Qianggong Zhang, Shichang Kang, Lun Luo, James Schauer, Benjamin de Foy, and Xuejun Wang
Atmos. Chem. Phys., 22, 2651–2668, https://doi.org/10.5194/acp-22-2651-2022, https://doi.org/10.5194/acp-22-2651-2022, 2022
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The Tibetan Plateau is known as
The Third Poleand is generally considered to be a clean area owing to its high altitude. However, it may receive be impacted by air pollutants transported from the Indian subcontinent. Pollutants generally enter the Tibetan Plateau in several ways. Among them is the Yarlung Zangbu–Brahmaputra Grand Canyon. In this study, we identified the influence of the Indian summer monsoon on the origin, transport, and behavior of mercury in this area.
Dominique Rust, Ioannis Katharopoulos, Martin K. Vollmer, Stephan Henne, Simon O'Doherty, Daniel Say, Lukas Emmenegger, Renato Zenobi, and Stefan Reimann
Atmos. Chem. Phys., 22, 2447–2466, https://doi.org/10.5194/acp-22-2447-2022, https://doi.org/10.5194/acp-22-2447-2022, 2022
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Artificial halocarbons contribute to ozone layer depletion and to global warming. We measured the atmospheric concentrations of halocarbons at the Beromünster tower, modelled the Swiss emissions, and compared the results to the internationally reported Swiss emissions inventory. For most of the halocarbons, we found good agreement, whereas one refrigerant might be overestimated in the inventory. In addition, we present first emission estimates of the newest types of halocarbons.
Xinping Yang, Keding Lu, Xuefei Ma, Yue Gao, Zhaofeng Tan, Haichao Wang, Xiaorui Chen, Xin Li, Xiaofeng Huang, Lingyan He, Mengxue Tang, Bo Zhu, Shiyi Chen, Huabin Dong, Limin Zeng, and Yuanhang Zhang
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2022-113, https://doi.org/10.5194/acp-2022-113, 2022
Revised manuscript accepted for ACP
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The STORM campaign was carried out at Shenzhen site in autumn 2018. The maximum diurnal OH and HO2 concentrations were 4.5 × 106 cm−3 and 4.5 × 108 cm−3, respectively. The unclassical OH recycling was identified again. AOC exhibited well-defined diurnal patterns, and OH was the dominant oxidant as expected. The strong positive correlation between F(O3) and AOC makes the quantification of F(O3) achieved, indicating AOC is the core driving force for the generation of secondary pollutants.
Tuija Jokinen, Katrianne Lehtipalo, Roseline Cutting Thakur, Ilona Ylivinkka, Kimmo Neitola, Nina Sarnela, Totti Laitinen, Markku Kulmala, Tuukka Petäjä, and Mikko Sipilä
Atmos. Chem. Phys., 22, 2237–2254, https://doi.org/10.5194/acp-22-2237-2022, https://doi.org/10.5194/acp-22-2237-2022, 2022
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New particle formation is an important source of cloud condensation nuclei; however, long-term measurements of aerosol-forming vapors are close to nonexistent in the Arctic. Here, we report 7 months of CI-APi-TOF measurements of sulfuric acid, iodic acid, methane sulfonic acid and the sum of highly oxygenated organic molecules from the SMEAR I station in the Finnish subarctic. The results help us to understand atmospheric chemical processes and aerosol formation in this rapidly changing area.
Andrew O. Langford, Christoph J. Senff, Raul J. Alvarez II, Ken C. Aikin, Sunil Baidar, Timothy A. Bonin, W. Alan Brewer, Jerome Brioude, Steven S. Brown, Joel D. Burley, Dani J. Caputi, Stephen A. Conley, Patrick D. Cullis, Zachary C. J. Decker, Stéphanie Evan, Guillaume Kirgis, Meiyun Lin, Mariusz Pagowski, Jeff Peischl, Irina Petropavlovskikh, R. Bradley Pierce, Thomas B. Ryerson, Scott P. Sandberg, Chance W. Sterling, Ann M. Weickmann, and Li Zhang
Atmos. Chem. Phys., 22, 1707–1737, https://doi.org/10.5194/acp-22-1707-2022, https://doi.org/10.5194/acp-22-1707-2022, 2022
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The Fires, Asian, and Stratospheric Transport–Las Vegas Ozone Study (FAST-LVOS) combined lidar, aircraft, and in situ measurements with global models to investigate the contributions of stratospheric intrusions, regional and Asian pollution, and wildfires to background ozone in the southwestern US during May and June 2017 and demonstrated that these processes contributed to background ozone levels that exceeded 70 % of the US National Ambient Air Quality Standard during the 6-week campaign.
Shijie Yu, Shenbo Wang, Ruixin Xu, Dong Zhang, Meng Zhang, Fangcheng Su, Ruiqin Zhang, and Lingling Wang
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2021-1016, https://doi.org/10.5194/acp-2021-1016, 2022
Revised manuscript accepted for ACP
Short summary
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In this study, the hourly data of 57 VOC species were collected during 2018 to 2020 at an urban site in Zhengzhou, China. The research of concentrations, source apportionment and atmospheric environmental implications clearly elucidated the differences in major reactants observed in different seasons and years. Therefore, the control strategy should focus on key species and source among inter-annual and seasonal variations. The results can provide references to develope control strategies.
Qingqing Yin, Qianli Ma, Weili Lin, Xiaobin Xu, and Jie Yao
Atmos. Chem. Phys., 22, 1015–1033, https://doi.org/10.5194/acp-22-1015-2022, https://doi.org/10.5194/acp-22-1015-2022, 2022
Short summary
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China has been experiencing rapid changes in emissions of air pollutants in recent decades. NOx and SO2 measurements from 2006 to 2016 at the Lin’an World Meteorological Organization Global Atmospheric Watch station were used to characterize the seasonal and diurnal variations and study the long-term trends. This study reaffirms China’s success in controlling both NOx and SO2 in the Yangtze River Delta but indicates at the same time a necessity to strengthen the NOx emission control.
Chaoyang Xue, Can Ye, Jörg Kleffmann, Wenjin Zhang, Xiaowei He, Pengfei Liu, Chenglong Zhang, Xiaoxi Zhao, Chengtang Liu, Zhuobiao Ma, Junfeng Liu, Jinhe Wang, Keding Lu, Valéry Catoire, Abdelwahid Mellouki, and Yujing Mu
Atmos. Chem. Phys., 22, 1035–1057, https://doi.org/10.5194/acp-22-1035-2022, https://doi.org/10.5194/acp-22-1035-2022, 2022
Short summary
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Nitrous acid (HONO) and related parameters were measured at the foot and the summit of Mt. Tai in the summer of 2018. Based on measurements at the foot station, we utilized a box model to explore the roles of different sources in the HONO budget. We also studied radical chemistry in this high-ozone region.
Baoye Hu, Jun Duan, Youwei Hong, Lingling Xu, Mengren Li, Yahui Bian, Min Qin, Wu Fang, Pinhua Xie, and Jinsheng Chen
Atmos. Chem. Phys., 22, 371–393, https://doi.org/10.5194/acp-22-371-2022, https://doi.org/10.5194/acp-22-371-2022, 2022
Short summary
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There has been a lack of research into HONO in coastal cities with low concentrations of PM2.5, but strong sunlight and high humidity. Insufficient research on coastal cities with good air quality has resulted in certain obstacles to assessing the photochemical processes in these areas. Furthermore, HONO contributes to the atmospheric photochemistry depending on the season. Therefore, observations of HONO across four seasons in the southeastern coastal area of China are urgently needed.
Cited articles
Agnan, Y., Le, D. T., Moore, C., Edwards, G., and Obrist, D.: New
constraints on terrestrial surface-atmosphere fluxes of gaseous elemental
mercury using a global database, Environ. Sci. Techol., 50,
507–524, https://doi.org/10.1021/acs.est.5b04013, 2016.
Angot, H., Dastoor, A., De Simone, F., Gårdfeldt, K., Gencarelli, C. N., Hedgecock, I. M., Langer, S., Magand, O., Mastromonaco, M. N., Nordstrøm, C., Pfaffhuber, K. A., Pirrone, N., Ryjkov, A., Selin, N. E., Skov, H., Song, S., Sprovieri, F., Steffen, A., Toyota, K., Travnikov, O., Yang, X., and Dommergue, A.: Chemical cycling and deposition of atmospheric mercury in polar regions: review of recent measurements and comparison with models, Atmos. Chem. Phys., 16, 10735–10763, https://doi.org/10.5194/acp-16-10735-2016, 2016.
Breuer, L., Kiese, R., and Butterbachbahl, K.: Temperature and moisture
effects on nitrification rates in tropical rain-forest soils, Soil Sci.
Soc. Am. J., 66, 399–402, 2002.
Carpi, A., Fostier, A. H., Orta, O. R., dos Santos, J. C., and Gittings, M.:
Gaseous mercury emissions from soil following forest loss and land use
changes: Field experiments in the United States and Brazil, Atmos.
Environ., 96, 423–429, https://doi.org/10.1016/j.atmosenv.2014.08.004, 2014.
Chen, Y., Yin, Y., Shi, J., Liu, G., Hu, L., Liu, J., Cai, Y., and Jiang,
G.: Analytical methods, formation, and dissolution of cinnabar and its
impact on environmental cycle of mercury, Critical Reviews in Environmental
Science and Technology, 47, 2415–2447, https://doi.org/10.1080/10643389.2018.1429764, 2017.
Cheng, Z., Tang, Y., Li, E., Wu, Q., Wang, L., Liu, K., Wang, S., Huang, Y.,
and Duan, L.: Mercury accumulation in soil from atmospheric deposition in
temperate steppe of Inner Mongolia, China, Environ. Poll., 258, 113692,
https://doi.org/10.1016/j.envpol.2019.113692, 2020.
Choi, H.-D. and Holsen, T. M.: Gaseous mercury emissions from unsterilized
and sterilized soils: The effect of temperature and UV radiation,
Environ. Poll., 157, 1673–1678, https://doi.org/10.1016/j.envpol.2008.12.014,
2009a.
Choi, H. D. and Holsen, T. M.: Gaseous mercury fluxes from the forest floor
of the Adirondacks, Environ. Pollut., 157, 592–600, 2009b.
Du, B., Zhou, J., Zhou, L., Fan, X., and Zhou, J.: Mercury distribution in
the foliage and soil profiles of a subtropical forest: Process for mercury
retention in soils, J. Geochem. Explor., 205, 106337,
https://doi.org/10.1016/j.gexplo.2019.106337, 2019.
Durnford, D. and Dastoor, A.: The behavior of mercury in the cryosphere: A
review of what we know from observations, J. Geophys. Res.-Atmos., 116, D06305, https://doi.org/10.1029/2010jd014809, 2011.
Eckley, C. S., Gustin, M., Lin, C. J., Li, X., and Miller, M. B.: The
influence of dynamic chamber design and operating parameters on calculated
surface-to-air mercury fluxes, Atmos. Environ., 44, 194–203,
https://doi.org/10.1016/j.atmosenv.2009.10.013, 2010.
Eckley, C. S., Blanchard, P., Mclennan, D., Mintz, R., and Sekela, M.:
Soil–air mercury flux near a large industrial emission source before and
after closure (Flin Flon, Manitoba, Canada), Environ. Sci. Technol., 49, 9750–9757, 2015.
Fang, J., Liu, G., Zhu, B., Wang, X., and Liu, S.: Carbon budgets of three
temperate forest ecosystems in Dongling Mt., Beijing, China, Sci.
China Ser. D, 50, 92–101, https://doi.org/10.1007/s11430-007-2031-3, 2007.
FAO: UNESCO soil map of the world, revised legend, in: World Res. Rep., FAO, Rome, 138,
1988.
Fraser, A., Dastoor, A., and Ryjkov, A.: How important is biomass burning in Canada to mercury contamination?, Atmos. Chem. Phys., 18, 7263–7286, https://doi.org/10.5194/acp-18-7263-2018, 2018.
Fu, X., Feng, X., and Wang, S.: Exchange fluxes of Hg between surfaces and
atmosphere in the eastern flank of Mount Gongga, Sichuan province,
southwestern China, J. Geophys. Res.-Atmos., 113, 253–270, 2008.
Gao, Y., Wang, Z., Zhang, X., and Wang, C.: Observation and estimation of
mercury exchange fluxes from soil under different crop cultivars and
planting densities in North China Plain, Environ. Pollut., 259,
113833, https://doi.org/10.1016/j.envpol.2019.113833, 2020.
Gustin, M. S.: Are mercury emissions from geologic sources significant? A
status report, Sci. Total Environ., 304, 153–167, https://doi.org/10.1016/S0048-9697(02)00565-X, 2003.
Gustin, M. S. and Stamenkovic, J.: Effect of watering and soil moisture on
mercury emissions from soils, Biogeochemistry, 76, 215–232, 2005.
Gustin, M. S., Engle, M., Ericksen, J., Lyman, S., Stamenkovic, J., and Xin,
M.: Mercury exchange between the atmosphere and low mercury containing
substrates, Appl. Geochem., 21, 1913–1923, 2006.
Hararuk, O., Obrist, D., and Luo, Y.: Modelling the sensitivity of soil mercury storage to climate-induced changes in soil carbon pools, Biogeosciences, 10, 2393–2407, https://doi.org/10.5194/bg-10-2393-2013, 2013.
Hartman, J. S., Weisberg, P. J., Pillai, R., Ericksen, J. A., Kuiken, T.,
Lindberg, S. E., Zhang, H., Rytuba, J. J., and Gustin, M. S.: Application of
a rule-based model to estimate mercury exchange for three background biomes
in the continental United States, Environ. Sci. Technol., 43,
4989–4994, https://doi.org/10.1021/es900075q, 2009.
Haynes, K. M., Kane, E. S., Potvin, L., Lilleskov, E. A., Kolka, R. K., and
Mitchell, C. P. J.: Gaseous mercury fluxes in peatlands and the potential
influence of climate change, Atmos. Environ., 154, 247–259,
https://doi.org/10.1016/j.atmosenv.2017.01.049, 2017.
Hou, H. Y.: Vegetation Map of P.R. China (1:4,000,000), Map Press of China, Beijing, 1982.
Howard, D. and Edwards, G. C.: Mercury fluxes over an Australian alpine grassland and observation of nocturnal atmospheric mercury depletion events, Atmos. Chem. Phys., 18, 129–142, https://doi.org/10.5194/acp-18-129-2018, 2018.
Johnson, D. W., Benesch, J. A., Gustin, M. S., Schorran, D. S., Lindberg, S.
E., and Coleman, J. S.: Experimental evidence against diffusion control of
Hg evasion from soils, Sci. Total Environ., 304, 175–184, https://doi.org/10.1016/S0048-9697(02)00567-3, 2003.
Kamp, J., Skov, H., Jensen, B., and Sørensen, L. L.: Fluxes of gaseous elemental mercury (GEM) in the High Arctic during atmospheric mercury depletion events (AMDEs), Atmos. Chem. Phys., 18, 6923–6938, https://doi.org/10.5194/acp-18-6923-2018, 2018.
Kiese, R. and Butterbach-Bahl, K.: N2O and CO2 emissions from three
different tropical forest sites in the wet tropics of Queensland, Australia,
Soil Biol. Biochem., 34, 975–987, 2002.
Kocman, D. and Horvat, M.: A laboratory based experimental study of mercury emission from contaminated soils in the River Idrijca catchment, Atmos. Chem. Phys., 10, 1417–1426, https://doi.org/10.5194/acp-10-1417-2010, 2010.
Kumari, A., Kumar, B., Manzoor, S., and Kulshrestha, U.: Status of
Atmospheric Mercury Research in South Asia: A Review, Aerosol Air
Qual. Res., 15, 1092–1109, https://doi.org/10.4209/aaqr.2014.05.0098, 2015.
Kuss, J., Krüger, S., Ruickoldt, J., and Wlost, K.-P.: High-resolution measurements of elemental mercury in surface water for an improved quantitative understanding of the Baltic Sea as a source of atmospheric mercury, Atmos. Chem. Phys., 18, 4361–4376, https://doi.org/10.5194/acp-18-4361-2018, 2018.
Li, F., Ma, C., and Zhang, P.: Mercury Deposition, Climate Change and
Anthropogenic Activities: A Review, Front. Earth Sci., 8, 316,
https://doi.org/10.3389/feart.2020.00316, 2020.
Lin, C. J., Gustin, M. S., Singhasuk, P., Eckley, C., and Miller, M.:
Empirical models for estimating mercury flux from soils, Environ.
Sci. Technol., 44, 8522–8528, 2010.
Lin, H., Tong, Y., Yin, X., Zhang, Q., Zhang, H., Zhang, H., Chen, L., Kang, S., Zhang, W., Schauer, J., de Foy, B., Bu, X., and Wang, X.: First measurement of atmospheric mercury species in Qomolangma Natural Nature Preserve, Tibetan Plateau, and evidence oftransboundary pollutant invasion, Atmos. Chem. Phys., 19, 1373–1391, https://doi.org/10.5194/acp-19-1373-2019, 2019.
Liu, K., Wu, Q., Wang, L., Wang, S., Liu, T., Ding, D., Tang, Y., Li, G.,
Tian, H., Duan, L., Wang, X., Fu, X., Feng, X., and Hao, J.:
Measure-specific effectiveness of air pollution control on China's
atmospheric mercury concentration and deposition during 2013-2017,
Environ. Sci. Technol., 53, 8938–8946,
https://doi.org/10.1021/acs.est.9b02428, 2019.
Luo, Y.: Mercury input, output and transport in forest ecosystems in
southern China, PhD thesis, Tsinghua University, Beijing, China,
1–112, 2015.
Ly Sy Phu, N., Zhang, L., Lin, D.-W., Lin, N.-H., and Sheu, G.-R.:
Eight-year dry deposition of atmospheric mercury to a tropical high mountain
background site downwind of the East Asian continent, Environ.
Pollut., 255, 113128, https://doi.org/10.1016/j.envpol.2019.113128, 2019.
Ma, J., Hu, Y., Bu, R., Chang, Y., Deng, H., and Qin, Q.: Predicting Impacts
of Climate Change on the Aboveground Carbon Sequestration Rate of a
Temperate Forest in Northeastern China, Plos One, 9, e96157,
https://doi.org/10.1371/journal.pone.0096157, 2014.
Ma, M., Wang, D., Sun, R., Shen, Y., and Huang, L.: Gaseous mercury
emissions from subtropical forested and open field soils in a national
nature reserve, southwest China, Atmos. Environ., 64, 116–123, 2013.
Ma, M., Sun, T., Du, H., and Wang, D.: A Two-Year Study on Mercury Fluxes
from the Soil under Different Vegetation Cover in a Subtropical Region,
South China, Atmosphere-Basel, 9, 30, https://doi.org/10.3390/atmos9010030, 2018.
Manca, G., Ammoscato, I., Esposito, G., Ianniello, A., Nardino, M., and
Sprovieri, F.: Dynamics of snow-air mercury exchange at Ny Ålesund
during springtime 2011, E3S Web of Conferences, EDP Sciences, 1, 03010, https://doi.org/10.1051/e3sconf/20130103010, 2013.
Maxwell, J. A., Holsen, T. M., and Mondal, S.: Gaseous elemental mercury
(GEM) emissions from snow surfaces in northern New York, Plos One, 8,
e69342, https://doi.org/10.1371/journal.pone.0069342, 2013.
Mo, F., Li, X., He, S., and Wang, X.: Evaluation of soil and water
conservation capacity of different forest types in Dongling Mountain,
Shengtai Xuebao, Acta Ecologica Sinica, 31, 5009–5016, 2011.
Nagati, M., Roy, M., DesRochers, A., Bergeron, Y., and Gardes, M.:
Importance of soil, stand, and mycorrhizal fungi
inabiesbalsameaestablishment in the boreal forest, Forests, 11, 815,
https://doi.org/10.3390/f11080815, 2020.
Obrist, D.: Mercury distribution across 14 U.S. forests. Part II: Patterns
of methyl mercury concentrations and areal mass of total and methyl mercury,
Environ. Sci. Technol., 46, 5921–5930, https://doi.org/10.1021/es2045579, 2012.
Obrist, D., Faïn, X., and Berger, C.: Gaseous elemental mercury
emissions and CO2 respiration rates in terrestrial soils under controlled
aerobic and anaerobic laboratory conditions, Sci. Total
Environ., 408, 1691–1700, 2010.
Obrist, D., Pokharel, A. K., and Moore, C.: Vertical profile measurements of
soil air suggest immobilization of gaseous elemental mercury in mineral
soil, Environ. Sci. Technol., 48, 2242–2252, https://doi.org/10.1021/es4048297, 2014.
Obrist, D., Kirk, J. L., Zhang, L., Sunderland, E. M., Jiskra, M., and
Selin, N. E.: A review of global environmental mercury processes in response
to human and natural perturbations: Changes of emissions, climate, and land
use, Ambio, 47, 116–140, https://doi.org/10.1007/s13280-017-1004-9, 2018.
O'Connor, D., Hou, D., Ok, Y. S., Mulder, J., Duan, L., Wu, Q., Wang, S.,
Tack, F. M. G., and Rinklebe, J.: Mercury speciation, transformation, and
transportation in soils, atmospheric flux, and implications for risk
management: A critical review, Environ. Int., 126, 747–761,
https://doi.org/10.1016/j.envint.2019.03.019, 2019.
Olson, C., Jiskra, M., Biester, H., Chow, J., and Obrist, D.: Mercury in
Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and
Spatial Distribution, Global Biogeochem. Cy., 32, 1058–1073,
https://doi.org/10.1029/2017gb005840, 2018.
Osterwalder, S., Sommar, J., Akerblom, S., Jocher, G., Fritsche, J.,
Nilsson, M. B., Bishop, K., and Alewell, C.: Comparative study of elemental
mercury flux measurement techniques over a Fennoscandian boreal peatland,
Atmos. Environ., 172, 16–25, https://doi.org/10.1016/j.atmosenv.2017.10.025, 2018.
Osterwalder, S., Huang, J.-H., Shetaya, W. H., Agnan, Y., Frossard, A.,
Frey, B., Alewell, C., Kretzschmar, R., Biester, H., and Obrist, D.: Mercury
emission from industrially contaminated soils in relation to chemical,
microbial, and meteorological factors, Environ. Pollut., 250,
944–952, https://doi.org/10.1016/j.envpol.2019.03.093, 2019.
Outridge, P. M., Mason, R. P., Wang, F., Guerrero, S., and
Heimburger-Boavida, L. E.: Updated global and oceanic mercury budgets for
the united nations global mercury assessment 2018, Environ. Sci. Technol., 52, 11466–11477, https://doi.org/10.1021/acs.est.8b01246, 2018.
Pan, L., Lin, C.-J., Carmichael, G. R., Streets, D. G., Tang, Y., Woo,
J.-H., Shetty, S. K., Chu, H.-W., Ho, T. C., Friedli, H. R., and Feng, X.:
Study of atmospheric mercury budget in East Asia using STEM-Hg modeling
system, Sci. Total Environ., 408, 3277–3291,
https://doi.org/10.1016/j.scitotenv.2010.04.039, 2010.
Pannu, R., Siciliano, S. D., and O'Driscoll, N. J.: Quantifying the effects
of soil temperature, moisture and sterilization on elemental mercury
formation in boreal soils, Environ. Poll., 193, 138–146, https://doi.org/10.1016/j.envpol.2014.06.023, 2014.
Peleg, M., Tas, E., Matveev, V., Obrist, D., Moore, C. W., Gabay, M., and
Luria, M.: Observational evidence for involvement of nitrate radicals in
nighttime oxidation of mercury, Environ. Sci. Technol., 49,
14008–14018, https://doi.org/10.1021/acs.est.5b03894, 2015.
Perez-Rodriguez, M., Biester, H., Aboal, J. R., Toro, M., and Martinez
Cortizas, A.: Thawing of snow and ice caused extraordinary high and fast
mercury fluxes to lake sediments in Antarctica, Geochim. Cosmochim.
Ac., 248, 109–122, https://doi.org/10.1016/j.gca.2019.01.009, 2019.
Richardson, J. B. and Friedland, A. J.: Mercury in coniferous and deciduous upland forests in northern New England, USA: implications of climate change, Biogeosciences, 12, 6737–6749, https://doi.org/10.5194/bg-12-6737-2015, 2015.
Risch, M. R., DeWild, J. F., Gay, D. A., Zhang, L., Boyer, E. W., and
Krabbenhoft, D. P.: Atmospheric mercury deposition to forests in the eastern
USA, Environ. Poll., 228, 8–18, https://doi.org/10.1016/j.envpol.2017.05.004, 2017.
Slemr, F., Weigelt, A., Ebinghaus, R., Bieser, J., Brenninkmeijer, C. A. M., Rauthe-Schöch, A., Hermann, M., Martinsson, B. G., van Velthoven, P., Bönisch, H., Neumaier, M., Zahn, A., and Ziereis, H.: Mercury distribution in the upper troposphere and lowermost stratosphere according to measurements by the IAGOS-CARIBIC observatory: 2014–2016, Atmos. Chem. Phys., 18, 12329–12343, https://doi.org/10.5194/acp-18-12329-2018, 2018.
Sørbotten, L.-E.: Hill slope unsaturated flowpaths and soil moisture
variability in a forested catchment in Southwest China, MSc thesis, Department of Plant and Environmental Sciences, University of Life Sciences, Oslo, Norway, 2011.
Spolaor, A., Barbaro, E., Cappelletti, D., Turetta, C., Mazzola, M., Giardi, F., Björkman, M. P., Lucchetta, F., Dallo, F., Pfaffhuber, K. A., Angot, H., Dommergue, A., Maturilli, M., Saiz-Lopez, A., Barbante, C., and Cairns, W. R. L.: Diurnal cycle of iodine, bromine, and mercury concentrations in Svalbard surface snow, Atmos. Chem. Phys., 19, 13325–13339, https://doi.org/10.5194/acp-19-13325-2019, 2019.
St Louis, V. L., Graydon, J. A., Lehnherr, I., Amos, H. M., Sunderland, E.
M., St Pierre, K. A., Emmerton, C. A., Sandilands, K., Tate, M., Steffen,
A., and Humphreys, E. R.: Atmospheric Concentrations and Wet/Dry Loadings of
Mercury at the Remote Experimental Lakes Area, Northwestern Ontario, Canada,
Environ. Sci. Technol., 53, 8017–8026, https://doi.org/10.1021/acs.est.9b01338, 2019.
Sun, T., Ma, M., Wang, X., Wang, Y., Du, H., Xiang, Y., Xu, Q., Xie, Q., and
Wang, D.: Mercury transport, transformation and mass balance on a
perspective of hydrological processes in a subtropical forest of China,
Environ. Poll., 254, 113065, https://doi.org/10.1016/j.envpol.2019.113065, 2019.
Teixeira, D. C., Lacerda, L. D., and Silva-Filho, E. V.: Foliar mercury
content from tropical trees and its correlation with physiological
parameters in situ, Environ. Pollut., 242, 1050–1057,
https://doi.org/10.1016/j.envpol.2018.07.120, 2018.
Wang, Q., Luo, Y., Du, B., Ye, Z., and Duan, L.: Influencing factors of
mercury emission flux from forest soil at tieshanping, chongqing,
Environ. Sci., 35, 1922–1927, 2014 (in Chinese with English abstract).
Wang, S., Feng, X., Qiu, G., Fu, X., and Wei, Z.: Characteristics of mercury
exchange flux between soil and air in the heavily air-polluted area, eastern
Guizhou, China, Atmos. Environ., 41, 5584–5594, 2007.
Wang, X., Bao, Z., Lin, C.-J., Yuan, W., and Feng, X.: Assessment of global
mercury deposition through litterfall, Environ. Sci. Technol., 50, 8548–8557, 2016.
Wang, X., Lin, C.-J., Feng, X., Yuan, W., Fu, X., Zhang, H., Wu, Q., and
Wang, S.: Assessment of regional mercury deposition and emission outflow in
mainland China, J. Geophys. Res.-Atmos., 123, 9868–9890,
https://doi.org/10.1029/2018jd028350, 2018.
Wang, Z., Zhang, X., Xiao, J., Zhijia, C., and Yu, P.: Mercury fluxes and
pools in three subtropical forested catchments, southwest China,
Environ. Poll., 157, 801–808, https://doi.org/10.1016/j.envpol.2008.11.018, 2009.
Wang, Z. H., Zhang, G., Wang, Y., Zhao, Y. X., and Sun, X. J.: Research on
mercury flux between snow and air under the condition of seasonal snow cover
environment, J. Agro-Environ. Sci., 32, 601–606, 2013.
Wright, L. P., Zhang, L., and Marsik, F. J.: Overview of mercury dry deposition, litterfall, and throughfall studies, Atmos. Chem. Phys., 16, 13399–13416, https://doi.org/10.5194/acp-16-13399-2016, 2016.
Wu, Z., Dai, E., Wu, Z., and Lin, M.: Future forest dynamics under climate
change, land use change, and harvest in subtropical forests in Southern
China, Landscape Ecol., 34, 843–863, https://doi.org/10.1007/s10980-019-00809-8, 2019.
Xin, M. and Gustin, M. S.: Gaseous elemental mercury exchange with low
mercury containing soils: Investigation of controlling factors, Appl.
Geochem., 22, 1451–1466, 2007.
Yu, Q., Luo, Y., Xu, G., Wu, Q., Wang, S., Hao, J., and Duan, L.:
Subtropical forests act as mercury sinks but as net sources of gaseous
elemental mercury in south China, Environ. Sci. Technol., 54,
2772–2779, https://doi.org/10.1021/acs.est.9b06715, 2020.
Yuan, W., Sommar, J., Lin, C.-J., Wang, X., Li, K., Liu, Y., Zhang, H., Lu,
Z., Wu, C., and Feng, X.: Stable Isotope Evidence Shows Re-emission of
Elemental Mercury Vapor Occurring after Reductive Loss from Foliage,
Environ. Sci. Technol., 53, 651–660, https://doi.org/10.1021/acs.est.8b04865,
2019a.
Yuan, W., Wang, X., Lin, C.-J., Sommar, J., Lu, Z., and Feng, X.: Process
factors driving dynamic exchange of elemental mercury vapor over soil in
broadleaf forest ecosystems, Atmos. Environ., 219, 117047,
https://doi.org/10.1016/j.atmosenv.2019.117047, 2019b.
Zarate-Valdez, J. L., Zasoski, R. J., and Lauchli, A.: Short-term effects of
moisture content on soil solution pH and soil Eh, Soil Sci., 171,
423–431, 2006.
Zhang, G., Wang, N., Ai, J.-C., Zhang, L., Yang, J., and Liu, Z.-Q.:
Characteristics of mercury exchange flux between soil and atmosphere under
the snow retention and snow melting control, Huanjing Kexue, Chinese Journal of Environmental Science website, 34, 468–475, 2013.
Zhang, H., Lindberg, S. E., Marsik, F. J., and Keeler, G. J.: Mercury
air/surface exchange kinetics of background soils of the tahquamenon river
watershed in the Michigan Upper Peninsula, Water Air Soil Pollut.,
126, 151–169, 2001.
Zhang, H., Lindberg, S. E., Barnett, M. O., Vette, A. F., and Gustin, M. S.:
Dynamic flux chamber measurement of gaseous mercury emission fluxes over
soils. Part 1: simulation of gaseous mercury emissions from soils using a
two-resistance exchange interface model, Atmos. Environ., 36,
835–846, 2002.
Zhang, H., Nizzetto, L., Feng, X., Borga, K., Sommar, J., Fu, X., Zhang, H.,
Zhang, G., and Larssen, T.: Assessing Air-Surface Exchange and Fate of
Mercury in a Subtropical Forest Using a Novel Passive Exchange-Meter Device,
Environ. Sci. Technol., 53, 4869–4879,
https://doi.org/10.1021/acs.est.8b06343, 2019a.
Zhang, L., Zhou, P., Cao, S., and Zhao, Y.: Atmospheric mercury deposition over the land surfaces and the associated uncertainties in observations and simulations: a critical review, Atmos. Chem. Phys., 19, 15587–15608, https://doi.org/10.5194/acp-19-15587-2019, 2019b.
Zhang, Q., Huang, J., Wang, F., Mark, L., Xu, J., Armstrong, D., Li, C.,
Zhang, Y., and Kang, S.: Mercury distribution and deposition in glacier snow
over western China, Environ. Sci. Technol., 46, 5404–5413, https://doi.org/10.1021/es300166x, 2012.
Zhou, J., Wang, Z., Zhang, X., and Chen, J.: Distribution and elevated soil
pools of mercury in an acidic subtropical forest of southwestern China,
Environ. Poll., 202, 187–195, https://doi.org/10.1016/j.envpol.2015.03.021, 2015.
Zhou, J., Wang, Z., Sun, T., Zhang, H., and Zhang, X.: Mercury in
terrestrial forested systems with highly elevated mercury deposition in
southwestern China: The risk to insects and potential release from
wildfires, Environ. Poll., 212, 188–196, https://doi.org/10.1016/j.envpol.2016.01.003, 2016.
Zhou, J., Wang, Z., Zhang, X., and Gao, Y.: Mercury concentrations and pools
in four adjacent coniferous and deciduous upland forests in Beijing, China,
J. Geophys. Res-Biogeosci., 122, 1260–1274, 2017a.
Zhou, J., Wang, Z., Zhang, X., and Sun, T.: Investigation of factors
affecting mercury emission from subtropical forest soil: A field controlled
study in southwestern China, J. Geochem. Explor., 176,
128–135, https://doi.org/10.1016/j.gexplo.2015.10.007, 2017b.
Zhou, J., Wang, Z., and Zhang, X.: Deposition and fate of mercury in
litterfall, litter, and soil in coniferous and broad-leaved forests, J. Geophys. Res-Biogeo., 123, 2590–2603, https://doi.org/10.1029/2018jg004415, 2018.
Zhou, J., Du, B., Shang, L., Wang, Z., Cui, H., Fan, X., and Zhou, J.:
Mercury fluxes, budgets, and pools in forest ecosystems of China: A review,
Crit. Rev. Env. Sci. Technol., 50, 1411–1450, 2020a.
Zhou, J., Wang, Z., Zhang, X., and Driscoll, C. T.: Measurement of vertical
distribution of gaseous elemental mercury concentration in soil pore air at
subtropical and temperate forests, Environ. Sci. Technol., in review, 2020b.
Zhu, W., Lin, C.-J., Wang, X., Sommar, J., Fu, X., and Feng, X.: Global observations and modeling of atmosphere–surface exchange of elemental mercury: a critical review, Atmos. Chem. Phys., 16, 4451–4480, https://doi.org/10.5194/acp-16-4451-2016, 2016.
Short summary
Mercury (Hg) emissions from natural resources have a large uncertainty, which is mainly derived from the forest. A long-term and multiplot (10) study of soil–air fluxes at subtropical and temperate forests was conducted. Forest soils are an important atmospheric Hg source, especially for subtropical forests. The compensation points imply that the atmospheric Hg concentration plays a critical role in inhibiting Hg emissions from the forest floor. Climate change can enhance soil Hg emissions.
Mercury (Hg) emissions from natural resources have a large uncertainty, which is mainly derived...
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