Atmospheric chemistry of nitrogenous aerosols in northeastern Asia: biological sources and secondary formation

To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios ( delta 15N) of T...

Full description

Saved in:
Bibliographic Details
Published inAtmospheric chemistry and physics Vol. 15; no. 17; pp. 9883 - 9896
Main Authors Pavuluri, C M, Kawamura, K, Fu, P Q
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 02.09.2015
Copernicus Publications
Subjects
Aerosols
Ageing
Aging
Air pollution
Atmospheric chemistry
Autumn
Biogeochemistry
Biological
Biomass
Biomass burning
Burning
Carbon
Carbonyl compounds
Carbonyls
Combustion
Emissions
Formations
Fossil fuels
Fuel combustion
Gases
Hydrocarbons
Isotope ratios
Nitrates
Nitrogen
Nitrogen (Chemical element)
Nitrogen isotopes
Organic nitrogen
Pollution sources
Ratios
Seasonal variation
Seasonal variations
Seasonality
Spring
Spring (season)
Summer
Suspended particulate matter
Terrestrial environments
Tracers
Water chemistry
Winter
Asia
Japan
Japan, Hokkaido, Sapporo
INW, Japan
Online AccessGet full text

Cover

Abstract To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios ( delta 15N) of TN ( delta 15NTN) and WSTN ( delta 15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 plus or minus 117 ng m-3), whereas WSON was 89.7 plus or minus 80.6 ng m-3, accounting for 14 plus or minus 11 % and 9.2 plus or minus 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m-3) and WION peaked in mid-spring to early summer (454 ng m-3). delta 15NTN (21.9 plus or minus 4.1 ppt) and delta 15NWSTN (25.8 plus or minus 8.2 ppt) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of delta 15NTN and delta 15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas-particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
AbstractList To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios (δ15N) of TN (δ15NTN) and WSTN (δ15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 ± 117 ng m-3), whereas WSON was 89.7 ± 80.6 ng m-3, accounting for 14 ± 11 % and 9.2 ± 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m-3) and WION peaked in mid-spring to early summer (454 ng m-3). δ15NTN (21.9 ± 4.1 [per thousand]) and δ15NWSTN (25.8 ± 8.2 [per thousand]) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of δ15NTN and δ15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas-particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios (δ15N) of TN (δ15NTN) and WSTN (δ15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126±117 ngm-3), whereas WSON was 89.7±80.6 ngm-3, accounting for 14±11 % and 9.2±7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ngm-3) and WION peaked in mid-spring to early summer (454 ngm-3). δ15NTN (21.9±4.1 ‰) and δ15NWSTN (25.8±8.2 ‰) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of δ15NTN andδ15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas–particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios (δ15N) of TN (δ15NTN) and WSTN (δ15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 ± 117 ng m−3), whereas WSON was 89.7 ± 80.6 ng m−3, accounting for 14 ± 11 % and 9.2 ± 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m−3) and WION peaked in mid-spring to early summer (454 ng m−3). δ15NTN (21.9 ± 4.1 ‰) and δ15NWSTN (25.8 ± 8.2 ‰) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of δ15NTN and δ15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas–particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios ( delta 15N) of TN ( delta 15NTN) and WSTN ( delta 15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 plus or minus 117 ng m-3), whereas WSON was 89.7 plus or minus 80.6 ng m-3, accounting for 14 plus or minus 11 % and 9.2 plus or minus 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m-3) and WION peaked in mid-spring to early summer (454 ng m-3). delta 15NTN (21.9 plus or minus 4.1 ppt) and delta 15NWSTN (25.8 plus or minus 8.2 ppt) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of delta 15NTN and delta 15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas-particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios ([delta].sup.15 N) of TN ([delta].sup.15 N.sub.TN) and WSTN (δ.sup.15 N.sub.WSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 ± 117 ng m.sup.−3 ), whereas WSON was 89.7 ± 80.6 ng m.sup.−3, accounting for 14 ± 11 % and 9.2 ± 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m.sup.−3) and WION peaked in mid-spring to early summer (454 ng m.sup.−3). [delta].sup.15 N.sub.TN (21.9 ± 4.1 ‰) and [delta].sup.15 N.sub.WSTN (25.8 ± 8.2 ‰) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH.sub.3 are suggested as an important source of WION. The seasonality of [delta].sup.15 N.sub.TN and [delta].sup.15 N.sub.WSTN, together with the comparisons to literature values, implies that chemical aging (including gas-particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.
Audience Academic
Author Fu, P Q
Kawamura, K
Pavuluri, C M
Author_xml – sequence: 1
  givenname: C
  surname: Pavuluri
  middlename: M
  fullname: Pavuluri, C M
– sequence: 2
  givenname: K
  surname: Kawamura
  fullname: Kawamura, K
– sequence: 3
  givenname: P
  surname: Fu
  middlename: Q
  fullname: Fu, P Q
BookMark eNqNkk2LFDEQhhtZwd3Vu8cGL3roNekk3R1vw-LHwILgxzlUJ5XZLD3JmGRA_701jqgjopJDQuWptyqV96I5iyli0zzm7EpxLZ-D3XVcdXqaRNczru4153yYWDeKXp79cn7QXJRyx1ivGJfnTVzVbSq7W8zBtvYWt6HU_KVNvo2h5rTBmPalBcyppKW0IbYx5XqLUCrm2K5KgBftHNKSNsHC0pa0zxYpI7q2oE3RAcn5lLdQQ4oPm_seloKPvu-XzcdXLz9cv-lu3r5eX69uOjvysXbe214qFLPVk529U1PvXS9RKBjoqu-9tdIBcjYpjWrWUsPMLAzgBsFAiMtmfdR1Ce7MLocttWESBPMtkPLGQK7BLmgYzoOe-KwtgETtJj660aK3Qkg3O0VaT49au5w-7bFUQ0OyuCwQkYZjuOZaj5x6_Dc6KqGYlvx_UIIZk0wT-uQ39I6mHGl-ppdcqoGrfvgbxUeqqTiJ_aQ2QG8P0aeawR5Km5WcuJJcTCNRV3-gaDkyCH0q-kDxk4RnJwnEVPxcN7Avxazfvztl2ZG1ZKqS0f_4H87MwcuGvGy4Mgcvm4OXxVeU7efo
CitedBy_id crossref_primary_10_1016_j_scitotenv_2017_06_214
crossref_primary_10_1016_j_chemosphere_2024_142356
crossref_primary_10_1016_j_atmosres_2017_09_005
crossref_primary_10_1016_j_chemosphere_2021_131316
crossref_primary_10_5194_acp_19_3463_2019
crossref_primary_10_1016_j_envpol_2023_121069
crossref_primary_10_1016_j_atmosres_2020_105376
crossref_primary_10_1007_s11356_018_2567_0
crossref_primary_10_1038_s41612_024_00620_6
crossref_primary_10_1016_j_scitotenv_2022_160895
crossref_primary_10_1029_2023JD038921
crossref_primary_10_2139_ssrn_4461559
crossref_primary_10_5194_acp_23_2119_2023
crossref_primary_10_1016_j_scitotenv_2020_143032
crossref_primary_10_1016_j_scitotenv_2023_165880
crossref_primary_10_1016_j_envpol_2023_122906
crossref_primary_10_1016_j_chemosphere_2023_138473
crossref_primary_10_5194_acp_18_6207_2018
crossref_primary_10_1016_j_atmosenv_2021_118905
crossref_primary_10_1016_j_atmosres_2024_107343
crossref_primary_10_1080_16000889_2017_1299672
crossref_primary_10_1016_j_jes_2021_06_018
crossref_primary_10_1016_j_atmosenv_2018_09_006
crossref_primary_10_1016_j_marpolbul_2021_112866
crossref_primary_10_1021_acs_est_3c01541
crossref_primary_10_1016_j_envint_2015_10_016
crossref_primary_10_3390_atmos14030484
crossref_primary_10_1016_j_atmosenv_2024_120555
crossref_primary_10_1016_j_atmosres_2020_105414
crossref_primary_10_1016_j_scitotenv_2022_158540
crossref_primary_10_1016_j_atmosres_2018_03_001
crossref_primary_10_5194_acp_17_3199_2017
crossref_primary_10_1007_s10874_022_09429_0
crossref_primary_10_1021_acs_est_9b03999
crossref_primary_10_1029_2020EA001615
crossref_primary_10_1016_j_atmosenv_2020_117795
crossref_primary_10_1021_acsearthspacechem_8b00105
crossref_primary_10_1016_j_atmosenv_2018_02_007
crossref_primary_10_1021_acs_est_1c04876
Cites_doi 10.1029/2009JD013238
10.1007/978-94-017-3405-9_3
10.1016/j.atmosenv.2012.09.012
10.1016/S1352-2310(01)00454-X
10.1002/jgrd.50244
10.5194/bg-9-4921-2012
10.1016/j.atmosres.2011.07.009
10.5194/acp-12-10125-2012
10.1016/j.atmosenv.2012.02.061
10.1104/pp.112.1.67
10.1016/j.atmosenv.2006.11.009
10.1016/j.atmosenv.2010.05.039
10.1021/es0108077
10.5194/acp-9-5131-2009
10.1890/1051-0761(1997)007[0737:HAOTGN]2.0.CO;2
10.1029/2009JD012864
10.5194/bg-9-385-2012
10.1016/j.atmosenv.2014.06.037
10.1029/2010JD015205
10.1016/j.atmosenv.2011.03.071
10.1016/S0009-2541(98)00105-3
10.1016/j.jaerosci.2009.08.006
10.1111/j.1757-1707.2010.01070.x
10.1029/2011GB004277
10.1016/j.atmosenv.2007.06.045
10.1016/j.atmosenv.2006.06.026
10.5194/acp-13-4667-2013
10.1016/j.atmosenv.2010.07.056
10.1029/2003JD003557
10.1029/2000JD900655
10.1890/1051-0761(1997)007[0034:SASVIN]2.0.CO;2
10.5194/acp-9-6685-2009
10.1029/2007JD009365
10.1029/2003JD003736
10.5194/acp-9-1431-2009
10.1071/EN14186
10.1007/s004420050122
10.1126/science.1221520
10.1016/j.atmosenv.2005.10.023
10.5194/acp-9-3331-2009
10.1002/2013JD020713
10.1029/2010JD014130
10.1038/nature11917
10.1016/0304-4203(94)90005-1
10.5194/acp-11-3037-2011
10.1029/2009JD013323
10.5194/bg-11-5675-2014
10.1007/s10533-004-0370-0
10.1098/rstb.2013.0115
10.1021/jp8078293
10.1016/j.atmosenv.2004.08.026
10.1029/92JD00411
10.1126/science.1150369
10.5194/acp-10-2663-2010
10.1021/es1001117
10.5194/acp-13-1927-2013
10.1002/2014GL059665
10.1016/j.atmosenv.2007.12.015
10.1016/S0883-2927(01)00061-0
10.1029/2002JD003051
10.1021/es803456n
10.1029/2005GB002672
10.1021/es902476f
10.1029/2001JD000870
10.4319/lo.2002.47.3.0713
ContentType Journal Article
Copyright COPYRIGHT 2015 Copernicus GmbH
Copyright Copernicus GmbH 2015
2015. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
Copyright_xml – notice: COPYRIGHT 2015 Copernicus GmbH
– notice: Copyright Copernicus GmbH 2015
– notice: 2015. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
DBID AAYXX
CITATION
ISR
7QH
7TG
7TN
7UA
8FD
8FE
8FG
ABUWG
AFKRA
ARAPS
ATCPS
AZQEC
BENPR
BFMQW
BGLVJ
BHPHI
BKSAR
C1K
CCPQU
DWQXO
F1W
GNUQQ
H8D
H96
HCIFZ
KL.
L.G
L7M
P5Z
P62
PATMY
PCBAR
PIMPY
PQEST
PQQKQ
PQUKI
PRINS
PYCSY
7U5
DOA
DOI 10.5194/acp-15-9883-2015
DatabaseName CrossRef
Gale In Context: Science
Aqualine
Meteorological & Geoastrophysical Abstracts
Oceanic Abstracts
Water Resources Abstracts
Technology Research Database
ProQuest SciTech Collection
ProQuest Technology Collection
ProQuest Central (Alumni)
ProQuest Central
Advanced Technologies & Aerospace Collection
Agricultural & Environmental Science Collection
ProQuest Central Essentials
ProQuest Central
Continental Europe Database
Technology Collection
ProQuest Natural Science Collection
Earth, Atmospheric & Aquatic Science Collection
Environmental Sciences and Pollution Management
ProQuest One Community College
ProQuest Central
ASFA: Aquatic Sciences and Fisheries Abstracts
ProQuest Central Student
Aerospace Database
Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources
SciTech Premium Collection
Meteorological & Geoastrophysical Abstracts - Academic
Aquatic Science & Fisheries Abstracts (ASFA) Professional
Advanced Technologies Database with Aerospace
Advanced Technologies & Aerospace Database
ProQuest Advanced Technologies & Aerospace Collection
Environmental Science Database
Earth, Atmospheric & Aquatic Science Database
Publicly Available Content Database
ProQuest One Academic Eastern Edition (DO NOT USE)
ProQuest One Academic
ProQuest One Academic UKI Edition
ProQuest Central China
Environmental Science Collection
Solid State and Superconductivity Abstracts
Directory of Open Access Journals
DatabaseTitle CrossRef
Publicly Available Content Database
Aquatic Science & Fisheries Abstracts (ASFA) Professional
ProQuest Central Student
Technology Collection
Technology Research Database
ProQuest Advanced Technologies & Aerospace Collection
ProQuest Central Essentials
ProQuest Central (Alumni Edition)
SciTech Premium Collection
ProQuest One Community College
ProQuest Central China
Water Resources Abstracts
Environmental Sciences and Pollution Management
Earth, Atmospheric & Aquatic Science Collection
ProQuest Central
Aerospace Database
Meteorological & Geoastrophysical Abstracts
Oceanic Abstracts
Natural Science Collection
ProQuest Central Korea
Agricultural & Environmental Science Collection
Advanced Technologies Database with Aerospace
Advanced Technologies & Aerospace Collection
ProQuest One Academic Eastern Edition
Earth, Atmospheric & Aquatic Science Database
ProQuest Technology Collection
Continental Europe Database
ProQuest SciTech Collection
Aqualine
Environmental Science Collection
Advanced Technologies & Aerospace Database
Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources
ProQuest One Academic UKI Edition
ASFA: Aquatic Sciences and Fisheries Abstracts
Environmental Science Database
ProQuest One Academic
Meteorological & Geoastrophysical Abstracts - Academic
Solid State and Superconductivity Abstracts
DatabaseTitleList Publicly Available Content Database
Publicly Available Content Database

Aerospace Database
Meteorological & Geoastrophysical Abstracts - Academic

Aquatic Science & Fisheries Abstracts (ASFA) Professional
CrossRef
Database_xml – sequence: 1
  dbid: DOA
  name: Directory of Open Access Journals
  url: https://www.doaj.org/
  sourceTypes: Open Website
– sequence: 2
  dbid: 8FG
  name: ProQuest Technology Collection
  url: https://search.proquest.com/technologycollection1
  sourceTypes: Aggregation Database
DeliveryMethod fulltext_linktorsrc
Discipline Meteorology & Climatology
EISSN 1680-7324
EndPage 9896
ExternalDocumentID oai_doaj_org_article_0eb6981b9caa4e9d817d7cefc334dbd5
3797423441
A481541387
10_5194_acp_15_9883_2015
GeographicLocations Asia
Japan
Japan, Hokkaido, Sapporo
INW, Japan
GeographicLocations_xml – name: Asia
– name: Japan
– name: Japan, Hokkaido, Sapporo
– name: INW, Japan
GroupedDBID 23N
2WC
3V.
4P2
5GY
5VS
6J9
7XC
8FE
8FG
8FH
8R4
8R5
AAFWJ
AAYXX
ABUWG
ACGFO
ADBBV
AENEX
AFKRA
AFPKN
AFRAH
AHGZY
AIAGR
ALMA_UNASSIGNED_HOLDINGS
ARAPS
ATCPS
BBORY
BCNDV
BENPR
BFMQW
BGLVJ
BHPHI
BKSAR
BPHCQ
CCPQU
CITATION
D1K
E3Z
EBS
EDH
EJD
FD6
GROUPED_DOAJ
GX1
H13
HCIFZ
HH5
IAO
IEA
IPNFZ
ISR
ITC
K6-
KQ8
M~E
OK1
P2P
P62
PATMY
PCBAR
PIMPY
PQQKQ
PROAC
PYCSY
Q2X
RIG
RKB
RNS
TR2
XSB
~02
7QH
7TG
7TN
7UA
8FD
AZQEC
C1K
DWQXO
F1W
GNUQQ
H8D
H96
KL.
L.G
L7M
PQEST
PQUKI
PRINS
7U5
ID FETCH-LOGICAL-c717t-ffc245e3bc98cbfd582fd24e35a6fc222fcc4dae10859e5b949ab0ca6ad630a33
IEDL.DBID BENPR
ISSN 1680-7324
1680-7316
IngestDate Tue Oct 22 14:49:44 EDT 2024
Fri Oct 25 23:25:16 EDT 2024
Thu Oct 24 23:53:07 EDT 2024
Fri Oct 25 08:32:56 EDT 2024
Thu Oct 10 19:45:19 EDT 2024
Thu Oct 10 15:52:50 EDT 2024
Thu Feb 22 23:30:00 EST 2024
Tue Nov 12 22:59:35 EST 2024
Thu Aug 01 19:19:12 EDT 2024
Fri Aug 23 00:58:18 EDT 2024
IsDoiOpenAccess true
IsOpenAccess true
IsPeerReviewed true
IsScholarly true
Issue 17
Language English
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c717t-ffc245e3bc98cbfd582fd24e35a6fc222fcc4dae10859e5b949ab0ca6ad630a33
Notes ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ORCID 0000-0001-6249-2280
0000-0003-1190-3726
OpenAccessLink https://www.proquest.com/docview/2414561526?pq-origsite=%requestingapplication%
PQID 1709451040
PQPubID 105744
PageCount 14
ParticipantIDs doaj_primary_oai_doaj_org_article_0eb6981b9caa4e9d817d7cefc334dbd5
proquest_miscellaneous_1919971582
proquest_miscellaneous_1753509412
proquest_miscellaneous_1717500409
proquest_journals_2414561526
proquest_journals_1709451040
gale_infotracmisc_A481541387
gale_infotracacademiconefile_A481541387
gale_incontextgauss_ISR_A481541387
crossref_primary_10_5194_acp_15_9883_2015
PublicationCentury 2000
PublicationDate 2015-09-02
PublicationDateYYYYMMDD 2015-09-02
PublicationDate_xml – month: 09
  year: 2015
  text: 2015-09-02
  day: 02
PublicationDecade 2010
PublicationPlace Katlenburg-Lindau
PublicationPlace_xml – name: Katlenburg-Lindau
PublicationTitle Atmospheric chemistry and physics
PublicationYear 2015
Publisher Copernicus GmbH
Copernicus Publications
Publisher_xml – name: Copernicus GmbH
– name: Copernicus Publications
References ref13
ref57
ref12
ref56
ref15
ref59
ref14
ref58
ref53
ref52
ref11
ref55
ref10
ref54
ref17
ref16
ref19
ref18
ref51
ref50
ref46
ref45
ref48
ref47
ref42
ref41
ref44
ref43
ref49
ref8
ref7
ref9
ref4
ref3
ref6
ref5
ref40
ref35
ref34
ref37
ref36
ref31
ref30
ref33
ref32
ref2
ref1
ref39
ref38
ref71
ref70
ref24
ref68
ref23
ref67
ref26
ref25
ref69
ref20
ref64
ref63
ref22
ref66
ref21
ref65
ref28
ref27
ref29
ref60
ref62
ref61
References_xml – ident: ref37
– ident: ref56
  doi: 10.1029/2009JD013238
– ident: ref44
  doi: 10.1007/978-94-017-3405-9_3
– ident: ref61
  doi: 10.1016/j.atmosenv.2012.09.012
– ident: ref38
  doi: 10.1016/S1352-2310(01)00454-X
– ident: ref48
  doi: 10.1002/jgrd.50244
– ident: ref21
  doi: 10.5194/bg-9-4921-2012
– ident: ref27
– ident: ref5
  doi: 10.1016/j.atmosres.2011.07.009
– ident: ref50
  doi: 10.5194/acp-12-10125-2012
– ident: ref14
  doi: 10.1016/j.atmosenv.2012.02.061
– ident: ref24
  doi: 10.1104/pp.112.1.67
– ident: ref66
  doi: 10.1016/j.atmosenv.2006.11.009
– ident: ref47
  doi: 10.1016/j.atmosenv.2010.05.039
– ident: ref55
  doi: 10.1021/es0108077
– ident: ref70
  doi: 10.5194/acp-9-5131-2009
– ident: ref63
  doi: 10.1890/1051-0761(1997)007[0737:HAOTGN]2.0.CO;2
– ident: ref4
  doi: 10.1029/2009JD012864
– ident: ref8
  doi: 10.5194/bg-9-385-2012
– ident: ref39
  doi: 10.1016/j.atmosenv.2014.06.037
– ident: ref42
  doi: 10.1029/2010JD015205
– ident: ref67
  doi: 10.1016/j.atmosenv.2011.03.071
– ident: ref60
  doi: 10.1016/S0009-2541(98)00105-3
– ident: ref31
  doi: 10.1016/j.jaerosci.2009.08.006
– ident: ref59
  doi: 10.1111/j.1757-1707.2010.01070.x
– ident: ref26
  doi: 10.1029/2011GB004277
– ident: ref30
  doi: 10.1016/j.atmosenv.2007.06.045
– ident: ref43
  doi: 10.1016/j.atmosenv.2006.06.026
– ident: ref2
  doi: 10.5194/acp-13-4667-2013
– ident: ref62
  doi: 10.1016/j.atmosenv.2010.07.056
– ident: ref35
  doi: 10.1029/2003JD003557
– ident: ref7
  doi: 10.1029/2000JD900655
– ident: ref18
  doi: 10.1890/1051-0761(1997)007[0034:SASVIN]2.0.CO;2
– ident: ref51
  doi: 10.5194/acp-9-6685-2009
– ident: ref1
  doi: 10.1029/2007JD009365
– ident: ref53
  doi: 10.1029/2003JD003736
– ident: ref12
  doi: 10.5194/acp-9-1431-2009
– ident: ref49
  doi: 10.1071/EN14186
– ident: ref20
  doi: 10.1007/s004420050122
– ident: ref52
  doi: 10.1126/science.1221520
– ident: ref17
  doi: 10.1016/j.atmosenv.2005.10.023
– ident: ref16
  doi: 10.5194/acp-9-3331-2009
– ident: ref22
– ident: ref41
  doi: 10.1002/2013JD020713
– ident: ref19
– ident: ref68
  doi: 10.1029/2010JD014130
– ident: ref34
  doi: 10.1038/nature11917
– ident: ref45
  doi: 10.1016/0304-4203(94)90005-1
– ident: ref40
  doi: 10.5194/acp-11-3037-2011
– ident: ref32
  doi: 10.1029/2009JD013323
– ident: ref65
  doi: 10.5194/bg-11-5675-2014
– ident: ref15
  doi: 10.1007/s10533-004-0370-0
– ident: ref25
  doi: 10.1098/rstb.2013.0115
– ident: ref46
  doi: 10.1021/jp8078293
– ident: ref54
  doi: 10.1016/j.atmosenv.2004.08.026
– ident: ref3
  doi: 10.1029/92JD00411
– ident: ref28
– ident: ref11
  doi: 10.1126/science.1150369
– ident: ref13
  doi: 10.5194/acp-10-2663-2010
– ident: ref64
  doi: 10.1021/es1001117
– ident: ref58
  doi: 10.5194/acp-13-1927-2013
– ident: ref29
  doi: 10.1002/2014GL059665
– ident: ref71
  doi: 10.1016/j.atmosenv.2007.12.015
– ident: ref57
  doi: 10.1016/S0883-2927(01)00061-0
– ident: ref36
  doi: 10.1029/2002JD003051
– ident: ref33
  doi: 10.1021/es803456n
– ident: ref10
– ident: ref9
  doi: 10.1029/2005GB002672
– ident: ref23
  doi: 10.1021/es902476f
– ident: ref69
  doi: 10.1029/2001JD000870
– ident: ref6
  doi: 10.4319/lo.2002.47.3.0713
SSID ssj0025014
Score 2.3860033
Snippet To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in...
SourceID doaj
proquest
gale
crossref
SourceType Open Website
Aggregation Database
StartPage 9883
SubjectTerms Aerosols
Ageing
Aging
Air pollution
Atmospheric chemistry
Autumn
Biogeochemistry
Biological
Biomass
Biomass burning
Burning
Carbon
Carbonyl compounds
Carbonyls
Combustion
Emissions
Formations
Fossil fuels
Fuel combustion
Gases
Hydrocarbons
Isotope ratios
Nitrates
Nitrogen
Nitrogen (Chemical element)
Nitrogen isotopes
Organic nitrogen
Pollution sources
Ratios
Seasonal variation
Seasonal variations
Seasonality
Spring
Spring (season)
Summer
Suspended particulate matter
Terrestrial environments
Tracers
Water chemistry
Winter
SummonAdditionalLinks – databaseName: Directory of Open Access Journals
  dbid: DOA
  link: http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwrV1Lb9QwELZQT1wQjyICBZkKgThEjV-JzW2pqFqkcgAq9WY5fqCVilMl6f9nJsmuuhKUS4-JJ1biGXu-icffEPKOJe1TkLyEQA0CFHBxpQEvVFa6jcwxHvxUDuj8W316Ib9eqstbpb4wJ2ymB54H7qiKbW0AWxnvnIwmaNaExsfkhZChDTN7aWU2wdQSauFuGYZata5KrM00b1ACWpFHzl-XTJVGawEmguVwbzmkibf_X6vz5HJOHpNHC1akq_kdn5AHMT8lxTnA3K6f_obT9_T4ag2Yc7p6RvJq_N0NSBSw9tRvSrnRLlGYuH0387FSF-FFuquBrjPNuG2D5Xtin-lqWLtPdKZlQt3R-c8-PJEDHTByDg6625533CcXJ19-Hp-WS0GF0kPUNpYpeS5VFK032rcpKM1T4DIK5Wpo4jx5L4OLeCLBRNUaaVxbeVe7UIvKCfGc7OUuxxeENqmtQShFnwATBOiPxUpKJbiK2tS-IB83o2qvZ94MC_EGasCCBixTFjVgUQMF-YzDvpVDxuvpBtiBXezA_s8OCnKISrPIaZExaeaXuxkGe_bju10hIQ04a90U5MMilLqxd94tZxDgm5AGa0fyYEcSFOZ3mze2YZdJP1jWQKwMa5ys_toMWAnRquJ1Qd5um7FjzHPLESwAugA4hwuruUtGCaQ9ZPwOGYMJRAwU_PI-BvcVeYiKmnLr-AHZG_ub-BrA2Ni-mebdHyV1M-Y
  priority: 102
  providerName: Directory of Open Access Journals
Title Atmospheric chemistry of nitrogenous aerosols in northeastern Asia: biological sources and secondary formation
URI https://www.proquest.com/docview/1709451040
https://www.proquest.com/docview/2414561526
https://search.proquest.com/docview/1717500409
https://search.proquest.com/docview/1753509412
https://search.proquest.com/docview/1919971582
https://doaj.org/article/0eb6981b9caa4e9d817d7cefc334dbd5
Volume 15
hasFullText 1
inHoldings 1
isFullTextHit
isPrint
link http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV3db9MwELdY98IL4lMEtsogBOIhWuLYic0L6qaVgdQJBhN7sxx_TJVG0iXZ_89dkhYqQZ-q1JdTkrPvy-ffEfImDdIGx1kMgRoEKGDiYgVWKE5k6VOTMmf7dkCL8_zskn-5Eldjwq0dyyrXOrFX1K62mCM_AkuDtl6w_OPqNsauUbi7OrbQ2CP7DCKFZEL2j0_Pv15sQi7cNcOQK5dJjD2aho1K8Fr4kbGrOBWxkjKDqYJtcf8yTD1-__-0dG965g_Jg9FnpLNByI_IPV89JtEC3N266bPi9C09uVmC79lfPSHVrPtVtwgYsLTUrlu60TpQWMBNPeCyUuPhQeqbli4rWuH2Dbbx8U1FZ-3SfKADPBPKkA4ZfrijcrTFCNoZYLc59_iUXM5Pf5ycxWNjhdhC9NbFIVjGhc9Kq6QtgxOSBce4z4TJYYixYC13xuPJBOVFqbgyZWJNblyeJSbLnpFJVVf-OaFFKHMgCt4G8A0c8Et9wrnImPBS5TYi79dfVa8G_AwNcQdKQIMEdCo0SkCjBCJyjJ99Q4fI1_0fdXOtx4WkE1_mCnxtZY3hXjmZFq6wPtgs4650wOQ1Ck0jtkWFxTPX5q5t9efvF3qGwDRgtGURkXcjUai7xlgznkWAd0I4rC3Kgy1KEJjdHl7PDT0u_lanBcTMoOt48s_hPzM5Iq82w8gY690qDzMAWIBbhwpW7aIRGcIfpmwHjcJCohQE_GL3o7wk91EEffUcOyCTrrnzh-BudeWU7Mn5p-m4svB3vvj2c9onL34DH94uhQ
link.rule.ids 315,783,787,867,2109,12777,21400,27936,27937,33385,33386,33756,33757,43612,43817,74363,74630
linkProvider ProQuest
linkToHtml http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV1Lb9NAEF5BOcAFlZcwFFgQAnGw6n3ZXi4oVIQUmh6glXpbrfdRRSp2aqf_nxnbCUSCHJOdjBx_u_PYnf2GkLcsli56yVNI1CBBAReXavBCaVZWgVnGvevbAc1P89m5_HahLsYNt24sq1zbxN5Q-8bhHvkheBr09Yrnn5bXKXaNwtPVsYXGbXJHCvDVeFN8-nWTcOGZGSZceZml2KFpOKaEmEUeWrdMmUp1WQqYKNgU9y-31LP3_89G945nuk_ujxEjnQwQPyC3Qv2QJHMIdpu23xOn7-jR1QIiz_7TI1JPVr-aDukCFo66dUM32kQKy7dtBlZWagM8SHPV0UVNazy8wSY-oa3ppFvYj3QgZ0IE6bC_D7-oPe0wf_YW1G1uPT4m59MvZ0ezdGyrkDrI3VZpjI5LFUTldOmq6FXJo-cyCGVzGOI8Oie9DXgvQQdVaaltlTmbW5-LzArxhOzVTR2eElrEKgehGFyEyMCDPhYyKZXgKpQ6dwn5sH6rZjmwZxjIOhABAwgYpgwiYBCBhHzG176RQ97r_oumvTTjMjJZqHINkbZ21sqgfckKX7gQnRDSVx6UvEHQDDJb1Fg6c2lvus4c__xhJkhLAy67LBLyfhSKzaq1zo43EeA_IRnWluTBliQA5raH13PDjEu_M6yAjBksncz-OfxnHifk9WYYFWO1Wx1gBoAKCOrQvOpdMkog-SHjO2Q0lhExAPjZ7kd5Re7OzuYn5uT49Ptzcg_h6Ovo-AHZW7U34QUEXqvqZb-6fgPjHSyV
linkToPdf http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV3db9MwELegkxAviE8RGGAQAvEQNXHsJOYFdWPVBqyaBpP2Zjn-mCqNpCTZ_89d4hYqQR8TX0-p73wf9vl3hLxNfWm85SyGRA0SFHBxsQQvFCdl5VKdMmuGdkCni_z4gn-5FJeh_qkLZZVrmzgYatsY3COfgqdBXy9YPvWhLOLs8_zT6leMHaTwpDW007hN9gqeZ8mE7B0cLc7ON-kXnqBh-pWXSYz9msZDS4hg-FSbVZyKWJZlBmqDLXL_clIDlv__LPbghub3yb0QP9LZKPAH5JarH5LoFELfph12yOk7eni9hDh0eHpE6ln_s-kQPGBpqFm3d6ONp7CY22bEaKXawYc01x1d1rTGoxxs6ePams66pf5IR6gmlCcdd_vhF7WlHWbTVgO7zR3Ix-RifvTj8DgOTRZiA5lcH3tvGBcuq4wsTeWtKJm3jLtM6ByGGPPGcKsd3lKQTlSSS10lRufawiTrLHtCJnVTu6eEFr7Kgcg74yFOsMAvdQnnImPClTI3EfmwnlW1GrE0FOQgKAEFElCpUCgBhRKIyAFO-4YOUbCHF017pcKiUomrcglxtzRacydtmRa2MM6bLOO2ssDkDQpNIc5FjRpzpW-6Tp18P1czBKkBB14WEXkfiHzTt9rocC8B_hNCY21R7m9RgsDM9vBaN1QwBJ1KC8ifwe7x5J_Df7Q6Iq83w8gYa99qBxoALCDEQ2Mrd9GIDKEQU7aDRmJRUQoCfrb7U16RO7C01LeTxdfn5C5KYyiqY_tk0rc37gVEYX31Miyv3x8pMjI
openUrl ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Atmospheric+chemistry+of+nitrogenous+aerosols+in+northeastern+Asia%3A+biological+sources+and+secondary+formation&rft.jtitle=Atmospheric+chemistry+and+physics&rft.au=Pavuluri%2C+C+M&rft.au=Kawamura%2C+K&rft.au=Fu%2C+P+Q&rft.date=2015-09-02&rft.issn=1680-7316&rft.eissn=1680-7324&rft.volume=15&rft.issue=17&rft.spage=9883&rft.epage=9896&rft_id=info:doi/10.5194%2Facp-15-9883-2015&rft.externalDBID=NO_FULL_TEXT
thumbnail_l http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=1680-7324&client=summon
thumbnail_m http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=1680-7324&client=summon
thumbnail_s http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=1680-7324&client=summon