scholarly journals Size distributions and dry deposition fluxes of water-soluble inorganic nitrogen in atmospheric aerosols in Xiamen Bay, China

2021 ◽  
Author(s):  
Shui-Ping Wu ◽  
Xiang Li ◽  
Yang Gao ◽  
Mei-Jun Cai ◽  
Chao Xu ◽  
...  
Keyword(s):  
Atmospheric Aerosols ◽  
Dry Deposition ◽  
Inorganic Nitrogen ◽  
Water Soluble ◽  
Size Distributions ◽  
Xiamen Bay ◽  
Deposition Fluxes

scholarly journals Dry and wet deposition of inorganic nitrogen compounds to a tropical pasture site (Rondônia, Brazil)

2006 ◽  
Vol 6 (2) ◽  
pp. 447-469 ◽  
Author(s):  
I. Trebs ◽  
L. L. Lara ◽  
L. M. M. Zeri ◽  
L. V. Gatti ◽  
P. Artaxo ◽  
...  
Keyword(s):  
Biomass Burning ◽  
Dry Deposition ◽  
Wet Deposition ◽  
Particle Deposition ◽  
Inorganic Nitrogen ◽  
N Deposition ◽  
Deposition Fluxes ◽  
Dry And Wet Deposition ◽  
Surface Atmosphere ◽  
Nh3 Emission

Abstract. The input of nitrogen (N) to ecosystems has increased dramatically over the past decades. While total (wet + dry) N deposition has been extensively determined in temperate regions, only very few data sets of N wet deposition exist for tropical ecosystems, and moreover, reliable experimental information about N dry deposition in tropical environments is lacking. In this study we estimate dry and wet deposition of inorganic N for a remote pasture site in the Amazon Basin based on in-situ measurements. The measurements covered the late dry (biomass burning) season, a transition period and the onset of the wet season (clean conditions) (12 September to 14 November 2002) and were a part of the LBA-SMOCC (Large-Scale Biosphere-Atmosphere Experiment in Amazonia – Smoke, Aerosols, Clouds, Rainfall, and Climate) 2002 campaign. Ammonia (NH3), nitric acid (HNO3), nitrous acid (HONO), nitrogen dioxide (NO2), nitric oxide (NO), ozone (O3), aerosol ammonium (NH4+) and aerosol nitrate (NO3-) were measured in real-time, accompanied by simultaneous meteorological measurements. Dry deposition fluxes of NO2 and HNO3 are inferred using the ''big leaf multiple resistance approach'' and particle deposition fluxes are derived using an established empirical parameterization. Bi-directional surface-atmosphere exchange fluxes of NH3 and HONO are estimated by applying a ''canopy compensation point model''. N dry and wet deposition is dominated by NH3 and NH4+, which is largely the consequence of biomass burning during the dry season. The grass surface appeared to have a strong potential for daytime NH3 emission, owing to high canopy compensation points, which are related to high surface temperatures and to direct NH3 emissions from cattle excreta. NO2 also significantly accounted for N dry deposition, whereas HNO3, HONO and N-containing aerosol species were only minor contributors. Ignoring NH3 emission from the vegetation surface, the annual net N deposition rate is estimated to be about −11 kgN ha-1 yr-1. If on the other hand, surface-atmosphere exchange of NH3 is considered to be bi-directional, the annual net N budget at the pasture site is estimated to range from −2.15 to −4.25 kgN ha-1 yr-1.

scholarly journals Isotopic composition of water-soluble nitrate in bulk atmospheric deposition at Dongsha Island: sources and implications of external N supply to the northern South China Sea

2014 ◽  
Vol 11 (7) ◽  
pp. 1833-1846 ◽  
Author(s):  
J.-Y. T. Yang ◽  
S.-C. Hsu ◽  
M. H. Dai ◽  
S. S.-Y. Hsiao ◽  
S.-J. Kao
Keyword(s):  
South China Sea ◽  
Isotopic Composition ◽  
Atmospheric Deposition ◽  
South China ◽  
Dry Deposition ◽  
Wet Deposition ◽  
Hot Spot ◽  
Inorganic Nitrogen ◽  
Water Soluble ◽  
China Sea

Abstract. Increased reactive nitrogen (Nr, NO3− + NH4++ + dissolved organic nitrogen) emission from the Asian continent poses profound threats to ecosystem safety from terrestrial throughout the ocean proper. To quantify atmospheric Nr input, diagnose its sources, and evaluate influence on marine nitrogen cycle of the South China Sea (SCS), an oligotrophic marginal sea adjacent to the emission hot spot China, we conducted measurements of concentrations of nitrate and ammonium as well as other major ions and dual isotopes of nitrate (δ15NNO3 and δ18ONO3) in atmospheric deposition collected from Dongsha Island off southern China. The δ15NNO3 and δ18ONO3 for dry deposition averaged at −2.8‰ and +58.8‰, ranging from −7.5 to +3.7‰ and from ∼ +17 to +88‰, respectively. Wet deposition, although with limited samples, showed a similar flux-weighted mean in δ15NNO3 (−2.6‰) yet a significantly higher mean in δ18ONO3 (+78.8‰). The dual isotope ratios showed an anti-correlation and an inverse seasonality; the δ15NNO3 values were higher in summer compared to those in winter, while the δ18ONO3 values were higher in winter than those in summer. In winter, not only dual isotopic compositions of nitrate but also the ammonium and nitrate dry deposition fluxes were relatively uniform, demonstrating a persistent influence of fossil fuel combustion sourced from Asian continental outflows via the northeasterly monsoon winds. More variable isotopic values in summer likely suggest varying sources and dynamical formation processes of dry deposition nitrate. Biomass burning and lightning are suggested to be responsible for the observed higher δ15NNO3 values in summer. Atmospheric nitrate and ammonium deposition together was estimated to be ∼50 mmol N m−2 year−1, with the dominance of nitrate in dry deposition but ammonium slightly higher in wet deposition. If not including this additional fertilization of atmospheric inorganic nitrogen deposition to enhance the carbon sequestration, CO2 release out of the SCS would be double than that of the present amount, 460 ± 430 mmol C m−2 year−1. Our study demonstrates that atmospheric deposition may serve as an important external Nr supplier to the SCS; however it is difficult to separate the isotopic signal from N2 fixation (−2–0‰) due to their similarity in δ15NNO3. More studies related to isotopic composition of nitrogen speciation in atmospheric Nr deposition, their relative contributions and source identification, and the role of typhoons in the SCS are required.

Dry Deposition Fluxes and Size Distributions of Heavy Metals in Seoul, Korea During Yellow-Sand Events

2001 ◽  
Vol 35 (1) ◽  
pp. 569-576 ◽  
Author(s):  
Seung-Muk Yi ◽  
Eun-Young Lee ◽  
Thomas M. Holsen
Keyword(s):  
Heavy Metals ◽  
Dry Deposition ◽  
Size Distributions ◽  
Deposition Fluxes ◽  
Yellow Sand

scholarly journals Soluble trace metals in aerosols over the tropical south east Pacific offshore of Peru

2015 ◽  
Vol 12 (20) ◽  
pp. 17219-17243 ◽  
Author(s):  
A. R. Baker ◽  
M. Thomas ◽  
H. W. Bange ◽  
E. Plasencia Sánchez
Keyword(s):  
Trace Metals ◽  
Dry Deposition ◽  
Inorganic Nitrogen ◽  
Northern Chile ◽  
Marine Atmosphere ◽  
The South ◽  
Atmospheric Input ◽  
Deposition Fluxes ◽  
The North ◽  
East Pacific

Abstract. Bulk aerosol samples collected during cruise M91 of FS Meteor off the coast of Peru in December 2012 were analysed for their soluble trace metal (Fe, Al, Mn, Ti, Zn, V, Ni, Cu, Co, Cd, Pb, Th) and major ion (including NO3− and NH4+) content. These data are among the first recorded for trace metals in this relatively poorly studied region of the global marine atmosphere. To the north of ∼ 13° S, the concentrations of several elements (Fe, Ti, Zn, V, Ni, Pb) appear to be related to distance from the coast. At the south of the transect (∼ 15–16° S), elevated concentrations of Fe, Cu, Co and Ni were observed. These may be related to the activities of the large smelting facilities in the south of Peru or northern Chile. Calculated dry deposition fluxes (3370–17 800 and 16–107 nmol m−2 d−1 for inorganic nitrogen and soluble Fe respectively) indicated that atmospheric input to the waters of the Peru upwelling system contains an excess of Fe over N, with respect to phytoplankton requirements. This may be significant as primary production in these waters has been reported to be limited by Fe availability, but atmospheric deposition is unlikely to be the dominant source of Fe to the system.

Dry deposition (downward, upward) concentration study of particulates and water-soluble ionic species during daytime, night-time period at the traffic sampling site of Sha-Lu, Taiwan

2002 ◽  
Vol 18 (8) ◽  
pp. 405-415 ◽  
Author(s):  
Yuh-Shen Wu ◽  
Guor-Cheng Fang ◽  
Jui-Yeh Rau ◽  
Shih-Han Huang
Keyword(s):  
Dry Deposition ◽  
Sampling Site ◽  
Ionic Species ◽  
Water Soluble ◽  
Total Suspended Particulate ◽  
Night Time ◽  
Deposition Fluxes ◽  
Time Period ◽  
Suspended Particulate ◽  
Central Taiwan

Ambient suspended particulate (dry deposition, TSP) was collected in the traffic sites Sha-Lu, central Taiwan. In addition, the related water-soluble ionic species (Cl1/4, NO31/4, SO421/4, Na+, NH4+, K+, Mg2+and Ca2+) were analysed and wind speed, wind direction and temperature were also measured in this study. The downward dry deposition fluxes (averaged 54.07 mg/m2-sec) were about twice that of upward dry deposition fluxes (averaged 26.48 mg/m2-sec) in the daytime period. Furthermore, the average downward dry deposition fluxes (averaged 26.22 mg/m2-sec) were also about twice that of upward dry deposition fluxes (averaged 12.11 mg/m2-sec) in the night-time period. The results showed that the total suspended particulate concentrations of particulate mass in the daytime period (averaged 996.2 mg/m3) were higher than in the night-time period (averaged 560.7 mg/m3). The results showed that the total suspended particulate concentrations of particulate mass in the daytime period (averaged 996.2 mg/m3) were higher than in night-time period (averaged 560.7 mg/m3). As for water-soluble ionic species, the average dry deposition order and velocity for downward ionic species were Cl1/4 Í-Ca2+Í-NO31/4 Í-K+(2.09 cm/sec Í-1.46 cm/sec Í-1.46 cm/sec Í-1.07 cm/sec) anions during the daytime period. And the average dry deposition order and velocity for downward ionic species were NO31/4 Í / Cl1/4 Í / K+Í / Ca2+(2.92 cm/sec Í / 2.74 cm/sec Í / 0.96 cm/sec Í / 0.93 cm/sec) anions during the night-time period. The average dry deposition order and velocity for upward ionic species were Cl1/4 Í / Ca2+Í / K+Í / Mg2+(4.69 cm/sec Í / 0.62 cm/sec Í / 0.59 cm/sec Í / 0.55 cm/sec) anions during the daytime period. And the average dry deposition order and velocity for upward ionic species were Cl1/4 Í-Ca2+Í-Mg2+Í-K+(1.65 cm/sec Í-0.43 cm/sec Í / 0.37 cm/sec Í / 0.33 cm/sec) anions during the night-time period. The results also indicated that the sodium and chloride concentrations in total suspended particulate were highly positively related, indicating that the sea-salt aerosols were the major contributors for these species at this sampling site of central Taiwan.

scholarly journals Soluble trace metals in aerosols over the tropical south-east Pacific offshore of Peru

2016 ◽  
Vol 13 (3) ◽  
pp. 817-825 ◽  
Author(s):  
A. R. Baker ◽  
M. Thomas ◽  
H. W. Bange ◽  
E. Plasencia Sánchez
Keyword(s):  
Trace Metals ◽  
Dry Deposition ◽  
Inorganic Nitrogen ◽  
Marine Atmosphere ◽  
The South ◽  
Atmospheric Input ◽  
Deposition Fluxes ◽  
The North ◽  
East Pacific ◽  
Order Of Magnitude

Abstract. Bulk aerosol samples collected during cruise M91 of FS Meteor off the coast of Peru in December 2012 were analysed for their soluble trace metal (Fe, Al, Mn, Ti, Zn, V, Ni, Cu, Co, Cd, Pb, Th) and major ion (including NO3− and NH4+) content. These data are among the first recorded for trace metals in this relatively poorly studied region of the global marine atmosphere. To the north of  ∼  13° S, the concentrations of several elements (Fe, Ti, Zn, V, Ni, Pb) appear to be related to distance from the coast. At the south of the transect ( ∼  15–16° S), elevated concentrations of Fe, Cu, Co, and Ni were observed, and we calculated dry deposition fluxes of soluble Cu approximately an order of magnitude higher than a recent model-based estimate of total Cu deposition to the region. The model did not take account of emissions from the large smelting facilities in the south of Peru and northern Chile, and our results may indicate that these facilities constitute an important source of trace metals to the region. Calculated dry deposition fluxes (3370–17800 and 16–107 nmol m−2 d−1 for inorganic nitrogen and soluble Fe respectively) indicated that atmospheric input to the waters of the Peru upwelling system contains an excess of Fe over N, with respect to phytoplankton requirements. This may be significant as primary production in these waters has been reported to be limited by Fe availability, but atmospheric deposition is unlikely to be the dominant source of Fe to the system.

scholarly journals Spatial-temporal patterns of inorganic nitrogen air concentrations and deposition in eastern China

2018 ◽  
Author(s):  
Wen Xu ◽  
Lei Liu ◽  
Miaomiao Cheng ◽  
Yuanhong Zhao ◽  
Lin Zhang ◽  
...  
Keyword(s):  
Land Use ◽  
Seasonal Variation ◽  
Dry Deposition ◽  
Inorganic Nitrogen ◽  
Eastern China ◽  
N Deposition ◽  
Organic Fertilizers ◽  
Deposition Fluxes ◽  
Significant Seasonal Variation ◽  
Land Use Types

Abstract. Five-year (2011–2015) measurements of gaseous NH3, NO2 and HNO3 and particulate NH4+ and NO3− in air and/or precipitation were conducted at twenty-seven sites in a Nationwide Nitrogen Deposition Monitoring Network (NNDMN) to better understand spatial and temporal (seasonal and annual) characteristics of reactive nitrogen (Nr) concentrations and deposition in eastern China. Our observations reveal annual average concentrations (16.4–32.6 μg N m−3), dry deposition fluxes (15.8–31.7 kg N ha−1 yr−1) and wet/bulk deposition fluxes (18.4–28.0 kg N ha−1 yr−1) based on land use were ranked as urban > rural > background sites. Annual concentrations and dry deposition fluxes of each Nr species in air were comparable at urban and background sites in northern and southern regions, but were significantly higher at northern rural sites. These results, together with good agreement between spatial distributions of NH3 and NO2 concentrations determined from ground measurements and satellite observations, demonstrate that atmospheric Nr pollution is heavier in the northern region than in the southern region. No significant inter-annual trends were found in the annual Nr dry and wet/bulk N deposition at almost all of the selected sites. A lack of significant changes in annual averages between the 2013–2015 and 2011–2012 periods for all land use types, suggests that any effects of current emission controls are not yet apparent in Nr pollution and deposition in the region. Ambient concentrations of total Nr exhibited a non-significant seasonal variation at all land use types, although significant seasonal variations were found for individual Nr species (e.g., NH3, NO2 and pNO3−) in most cases. In contrast, dry deposition of total Nr exhibited a consistent and significant seasonal variation at all land use types, with the highest fluxes in summer and the lowest in winter. Based on sensitivity tests by the GEOS-Chem model, we found that NH3 emissions from fertilizer use (including chemical and organic fertilizers) were the largest contributor (36 %) to total inorganic Nr deposition over eastern China. Our results not only improve the understanding of spatial-temporal variations of Nr concentrations and deposition in this pollution hotspot, but also provide useful information for policy-makers that mitigation of NH3 emissions should be a priority to tackle serious N deposition in eastern China.

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