Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements
<p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol ma...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Y. Chen [verfasserIn] M. Takeuchi [verfasserIn] T. Nah [verfasserIn] L. Xu [verfasserIn] M. R. Canagaratna [verfasserIn] H. Stark [verfasserIn] K. Baumann [verfasserIn] F. Canonaco [verfasserIn] A. S. H. Prévôt [verfasserIn] L. G. Huey [verfasserIn] R. J. Weber [verfasserIn] N. L. Ng [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2020 |
|---|
| Übergeordnetes Werk: |
In: Atmospheric Chemistry and Physics - Copernicus Publications, 2003, 20(2020), Seite 8421-8440 |
|---|---|
| Übergeordnetes Werk: |
volume:20 ; year:2020 ; pages:8421-8440 |
| Links: |
Link aufrufen |
|---|
| DOI / URN: |
10.5194/acp-20-8421-2020 |
|---|
| Katalog-ID: |
DOAJ036444901 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | DOAJ036444901 | ||
| 003 | DE-627 | ||
| 005 | 20230307231328.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 230227s2020 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.5194/acp-20-8421-2020 |2 doi | |
| 035 | |a (DE-627)DOAJ036444901 | ||
| 035 | |a (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 050 | 0 | |a QC1-999 | |
| 050 | 0 | |a QD1-999 | |
| 100 | 0 | |a Y. Chen |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| 264 | 1 | |c 2020 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 520 | |a <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< | ||
| 653 | 0 | |a Physics | |
| 653 | 0 | |a Chemistry | |
| 700 | 0 | |a M. Takeuchi |e verfasserin |4 aut | |
| 700 | 0 | |a T. Nah |e verfasserin |4 aut | |
| 700 | 0 | |a T. Nah |e verfasserin |4 aut | |
| 700 | 0 | |a L. Xu |e verfasserin |4 aut | |
| 700 | 0 | |a L. Xu |e verfasserin |4 aut | |
| 700 | 0 | |a M. R. Canagaratna |e verfasserin |4 aut | |
| 700 | 0 | |a H. Stark |e verfasserin |4 aut | |
| 700 | 0 | |a H. Stark |e verfasserin |4 aut | |
| 700 | 0 | |a K. Baumann |e verfasserin |4 aut | |
| 700 | 0 | |a F. Canonaco |e verfasserin |4 aut | |
| 700 | 0 | |a A. S. H. Prévôt |e verfasserin |4 aut | |
| 700 | 0 | |a L. G. Huey |e verfasserin |4 aut | |
| 700 | 0 | |a R. J. Weber |e verfasserin |4 aut | |
| 700 | 0 | |a N. L. Ng |e verfasserin |4 aut | |
| 700 | 0 | |a N. L. Ng |e verfasserin |4 aut | |
| 700 | 0 | |a N. L. Ng |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i In |t Atmospheric Chemistry and Physics |d Copernicus Publications, 2003 |g 20(2020), Seite 8421-8440 |w (DE-627)092499996 |x 16807324 |7 nnns |
| 773 | 1 | 8 | |g volume:20 |g year:2020 |g pages:8421-8440 |
| 856 | 4 | 0 | |u https://doi.org/10.5194/acp-20-8421-2020 |z kostenfrei |
| 856 | 4 | 0 | |u https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c |z kostenfrei |
| 856 | 4 | 0 | |u https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf |z kostenfrei |
| 856 | 4 | 2 | |u https://doaj.org/toc/1680-7316 |y Journal toc |z kostenfrei |
| 856 | 4 | 2 | |u https://doaj.org/toc/1680-7324 |y Journal toc |z kostenfrei |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_DOAJ | ||
| 912 | |a GBV_ILN_381 | ||
| 951 | |a AR | ||
| 952 | |d 20 |j 2020 |h 8421-8440 | ||
| author_variant |
y c yc m t mt t n tn t n tn l x lx l x lx m r c mrc h s hs h s hs k b kb f c fc a s h p ashp l g h lgh r j w rjw n l n nln n l n nln n l n nln |
|---|---|
| matchkey_str |
article:16807324:2020----::hmclhrceiainfeodrognceooaauastiteotesensnihsrmiutnosiheouinieflgteoomssetoeehtfmad |
| hierarchy_sort_str |
2020 |
| callnumber-subject-code |
QC |
| publishDate |
2020 |
| allfields |
10.5194/acp-20-8421-2020 doi (DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c DE-627 ger DE-627 rakwb eng QC1-999 QD1-999 Y. Chen verfasserin aut Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< Physics Chemistry M. Takeuchi verfasserin aut T. Nah verfasserin aut T. Nah verfasserin aut L. Xu verfasserin aut L. Xu verfasserin aut M. R. Canagaratna verfasserin aut H. Stark verfasserin aut H. Stark verfasserin aut K. Baumann verfasserin aut F. Canonaco verfasserin aut A. S. H. Prévôt verfasserin aut L. G. Huey verfasserin aut R. J. Weber verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut In Atmospheric Chemistry and Physics Copernicus Publications, 2003 20(2020), Seite 8421-8440 (DE-627)092499996 16807324 nnns volume:20 year:2020 pages:8421-8440 https://doi.org/10.5194/acp-20-8421-2020 kostenfrei https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c kostenfrei https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf kostenfrei https://doaj.org/toc/1680-7316 Journal toc kostenfrei https://doaj.org/toc/1680-7324 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 AR 20 2020 8421-8440 |
| spelling |
10.5194/acp-20-8421-2020 doi (DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c DE-627 ger DE-627 rakwb eng QC1-999 QD1-999 Y. Chen verfasserin aut Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< Physics Chemistry M. Takeuchi verfasserin aut T. Nah verfasserin aut T. Nah verfasserin aut L. Xu verfasserin aut L. Xu verfasserin aut M. R. Canagaratna verfasserin aut H. Stark verfasserin aut H. Stark verfasserin aut K. Baumann verfasserin aut F. Canonaco verfasserin aut A. S. H. Prévôt verfasserin aut L. G. Huey verfasserin aut R. J. Weber verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut In Atmospheric Chemistry and Physics Copernicus Publications, 2003 20(2020), Seite 8421-8440 (DE-627)092499996 16807324 nnns volume:20 year:2020 pages:8421-8440 https://doi.org/10.5194/acp-20-8421-2020 kostenfrei https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c kostenfrei https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf kostenfrei https://doaj.org/toc/1680-7316 Journal toc kostenfrei https://doaj.org/toc/1680-7324 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 AR 20 2020 8421-8440 |
| allfields_unstemmed |
10.5194/acp-20-8421-2020 doi (DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c DE-627 ger DE-627 rakwb eng QC1-999 QD1-999 Y. Chen verfasserin aut Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< Physics Chemistry M. Takeuchi verfasserin aut T. Nah verfasserin aut T. Nah verfasserin aut L. Xu verfasserin aut L. Xu verfasserin aut M. R. Canagaratna verfasserin aut H. Stark verfasserin aut H. Stark verfasserin aut K. Baumann verfasserin aut F. Canonaco verfasserin aut A. S. H. Prévôt verfasserin aut L. G. Huey verfasserin aut R. J. Weber verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut In Atmospheric Chemistry and Physics Copernicus Publications, 2003 20(2020), Seite 8421-8440 (DE-627)092499996 16807324 nnns volume:20 year:2020 pages:8421-8440 https://doi.org/10.5194/acp-20-8421-2020 kostenfrei https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c kostenfrei https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf kostenfrei https://doaj.org/toc/1680-7316 Journal toc kostenfrei https://doaj.org/toc/1680-7324 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 AR 20 2020 8421-8440 |
| allfieldsGer |
10.5194/acp-20-8421-2020 doi (DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c DE-627 ger DE-627 rakwb eng QC1-999 QD1-999 Y. Chen verfasserin aut Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< Physics Chemistry M. Takeuchi verfasserin aut T. Nah verfasserin aut T. Nah verfasserin aut L. Xu verfasserin aut L. Xu verfasserin aut M. R. Canagaratna verfasserin aut H. Stark verfasserin aut H. Stark verfasserin aut K. Baumann verfasserin aut F. Canonaco verfasserin aut A. S. H. Prévôt verfasserin aut L. G. Huey verfasserin aut R. J. Weber verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut In Atmospheric Chemistry and Physics Copernicus Publications, 2003 20(2020), Seite 8421-8440 (DE-627)092499996 16807324 nnns volume:20 year:2020 pages:8421-8440 https://doi.org/10.5194/acp-20-8421-2020 kostenfrei https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c kostenfrei https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf kostenfrei https://doaj.org/toc/1680-7316 Journal toc kostenfrei https://doaj.org/toc/1680-7324 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 AR 20 2020 8421-8440 |
| allfieldsSound |
10.5194/acp-20-8421-2020 doi (DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c DE-627 ger DE-627 rakwb eng QC1-999 QD1-999 Y. Chen verfasserin aut Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< Physics Chemistry M. Takeuchi verfasserin aut T. Nah verfasserin aut T. Nah verfasserin aut L. Xu verfasserin aut L. Xu verfasserin aut M. R. Canagaratna verfasserin aut H. Stark verfasserin aut H. Stark verfasserin aut K. Baumann verfasserin aut F. Canonaco verfasserin aut A. S. H. Prévôt verfasserin aut L. G. Huey verfasserin aut R. J. Weber verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut N. L. Ng verfasserin aut In Atmospheric Chemistry and Physics Copernicus Publications, 2003 20(2020), Seite 8421-8440 (DE-627)092499996 16807324 nnns volume:20 year:2020 pages:8421-8440 https://doi.org/10.5194/acp-20-8421-2020 kostenfrei https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c kostenfrei https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf kostenfrei https://doaj.org/toc/1680-7316 Journal toc kostenfrei https://doaj.org/toc/1680-7324 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 AR 20 2020 8421-8440 |
| language |
English |
| source |
In Atmospheric Chemistry and Physics 20(2020), Seite 8421-8440 volume:20 year:2020 pages:8421-8440 |
| sourceStr |
In Atmospheric Chemistry and Physics 20(2020), Seite 8421-8440 volume:20 year:2020 pages:8421-8440 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Physics Chemistry |
| isfreeaccess_bool |
true |
| container_title |
Atmospheric Chemistry and Physics |
| authorswithroles_txt_mv |
Y. Chen @@aut@@ M. Takeuchi @@aut@@ T. Nah @@aut@@ L. Xu @@aut@@ M. R. Canagaratna @@aut@@ H. Stark @@aut@@ K. Baumann @@aut@@ F. Canonaco @@aut@@ A. S. H. Prévôt @@aut@@ L. G. Huey @@aut@@ R. J. Weber @@aut@@ N. L. Ng @@aut@@ |
| publishDateDaySort_date |
2020-01-01T00:00:00Z |
| hierarchy_top_id |
092499996 |
| id |
DOAJ036444901 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ036444901</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230307231328.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230227s2020 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/acp-20-8421-2020</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ036444901</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QC1-999</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QD1-999</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Y. Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Physics</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Chemistry</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. Takeuchi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">T. Nah</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">T. Nah</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. R. Canagaratna</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">H. Stark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">H. Stark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Baumann</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">F. Canonaco</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">A. S. H. Prévôt</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. G. Huey</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">R. J. Weber</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Atmospheric Chemistry and Physics</subfield><subfield code="d">Copernicus Publications, 2003</subfield><subfield code="g">20(2020), Seite 8421-8440</subfield><subfield code="w">(DE-627)092499996</subfield><subfield code="x">16807324</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:20</subfield><subfield code="g">year:2020</subfield><subfield code="g">pages:8421-8440</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/acp-20-8421-2020</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1680-7316</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1680-7324</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">20</subfield><subfield code="j">2020</subfield><subfield code="h">8421-8440</subfield></datafield></record></collection>
|
| callnumber-first |
Q - Science |
| author |
Y. Chen |
| spellingShingle |
Y. Chen misc QC1-999 misc QD1-999 misc Physics misc Chemistry Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| authorStr |
Y. Chen |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)092499996 |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut |
| collection |
DOAJ |
| remote_str |
true |
| callnumber-label |
QC1-999 |
| illustrated |
Not Illustrated |
| issn |
16807324 |
| topic_title |
QC1-999 QD1-999 Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| topic |
misc QC1-999 misc QD1-999 misc Physics misc Chemistry |
| topic_unstemmed |
misc QC1-999 misc QD1-999 misc Physics misc Chemistry |
| topic_browse |
misc QC1-999 misc QD1-999 misc Physics misc Chemistry |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
cr |
| hierarchy_parent_title |
Atmospheric Chemistry and Physics |
| hierarchy_parent_id |
092499996 |
| hierarchy_top_title |
Atmospheric Chemistry and Physics |
| isfreeaccess_txt |
true |
| familylinks_str_mv |
(DE-627)092499996 |
| title |
Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| ctrlnum |
(DE-627)DOAJ036444901 (DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c |
| title_full |
Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| author_sort |
Y. Chen |
| journal |
Atmospheric Chemistry and Physics |
| journalStr |
Atmospheric Chemistry and Physics |
| callnumber-first-code |
Q |
| lang_code |
eng |
| isOA_bool |
true |
| recordtype |
marc |
| publishDateSort |
2020 |
| contenttype_str_mv |
txt |
| container_start_page |
8421 |
| author_browse |
Y. Chen M. Takeuchi T. Nah L. Xu M. R. Canagaratna H. Stark K. Baumann F. Canonaco A. S. H. Prévôt L. G. Huey R. J. Weber N. L. Ng |
| container_volume |
20 |
| class |
QC1-999 QD1-999 |
| format_se |
Elektronische Aufsätze |
| author-letter |
Y. Chen |
| doi_str_mv |
10.5194/acp-20-8421-2020 |
| author2-role |
verfasserin |
| title_sort |
chemical characterization of secondary organic aerosol at a rural site in the southeastern us: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (hr-tof-ams) and figaero chemical ionization mass spectrometer (cims) measurements |
| callnumber |
QC1-999 |
| title_auth |
Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| abstract |
<p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< |
| abstractGer |
<p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< |
| abstract_unstemmed |
<p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p< |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_381 |
| title_short |
Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements |
| url |
https://doi.org/10.5194/acp-20-8421-2020 https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 |
| remote_bool |
true |
| author2 |
M. Takeuchi T. Nah L. Xu M. R. Canagaratna H. Stark K. Baumann F. Canonaco A. S. H. Prévôt L. G. Huey R. J. Weber N. L. Ng |
| author2Str |
M. Takeuchi T. Nah L. Xu M. R. Canagaratna H. Stark K. Baumann F. Canonaco A. S. H. Prévôt L. G. Huey R. J. Weber N. L. Ng |
| ppnlink |
092499996 |
| callnumber-subject |
QC - Physics |
| mediatype_str_mv |
c |
| isOA_txt |
true |
| hochschulschrift_bool |
false |
| doi_str |
10.5194/acp-20-8421-2020 |
| callnumber-a |
QC1-999 |
| up_date |
2024-07-03T20:37:08.602Z |
| _version_ |
1803591644462710784 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ036444901</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230307231328.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230227s2020 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/acp-20-8421-2020</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ036444901</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ8cc59c29dece4a0b935863a04c80de3c</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QC1-999</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QD1-999</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Y. Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Chemical characterization of secondary organic aerosol at a rural site in the southeastern US: insights from simultaneous high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and FIGAERO chemical ionization mass spectrometer (CIMS) measurements</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<The formation and evolution of secondary organic aerosol (SOA) were investigated at Yorkville, GA, in late summer (mid-August to mid-October 2016). The organic aerosol (OA) composition was measured using two online mass spectrometry instruments, the high-resolution time-of-flight aerosol mass spectrometer (AMS) and the Filter Inlet for Gases and AEROsols coupled to a high-resolution time-of-flight iodide-adduct chemical ionization mass spectrometer (FIGAERO-CIMS). Through analysis of speciated organics data from FIGAERO-CIMS and factorization analysis of data obtained from both instruments, we observed notable SOA formation from isoprene and monoterpenes during both day and night. Specifically, in addition to isoprene epoxydiol (IEPOX) uptake, we identified isoprene SOA formation from non-IEPOX pathways and isoprene organic nitrate formation via photooxidation in the presence of <span class="inline-formula"<NO<sub<<i<x</i<</sub<</span< and nitrate radical oxidation. Monoterpenes were found to be the most important SOA precursors at night. We observed significant contributions from highly oxidized acid-like compounds to the aged OA factor from FIGAERO-CIMS. Taken together, our results showed that FIGAERO-CIMS measurements are highly complementary to the extensively used AMS factorization analysis, and together they provide more comprehensive insights into OA sources and composition.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Physics</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Chemistry</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. Takeuchi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">T. Nah</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">T. Nah</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. R. Canagaratna</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">H. Stark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">H. Stark</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Baumann</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">F. Canonaco</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">A. S. H. Prévôt</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. G. Huey</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">R. J. Weber</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">N. L. Ng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Atmospheric Chemistry and Physics</subfield><subfield code="d">Copernicus Publications, 2003</subfield><subfield code="g">20(2020), Seite 8421-8440</subfield><subfield code="w">(DE-627)092499996</subfield><subfield code="x">16807324</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:20</subfield><subfield code="g">year:2020</subfield><subfield code="g">pages:8421-8440</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/acp-20-8421-2020</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/8cc59c29dece4a0b935863a04c80de3c</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.atmos-chem-phys.net/20/8421/2020/acp-20-8421-2020.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1680-7316</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1680-7324</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">20</subfield><subfield code="j">2020</subfield><subfield code="h">8421-8440</subfield></datafield></record></collection>
|
| score |
7.400549 |