FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2318404116> ?p ?o ?g. }

• W2318404116 abstract "Abstract. In our previous works, it was demonstrated that the combined use of quantitative energy-dispersive electron probe X-ray microanalysis (ED-EPMA), which is also known as low-Z particle EPMA, and attenuated total reflectance FT-IR (ATR-FT-IR) imaging has great potential for a detailed characterization of individual aerosol particles. In this study, individual Asian Dust particles collected during an Asian Dust storm event on 11 November 2011 in Korea were characterized by the combined use of low-Z particle EPMA and ATR-FT-IR imaging. The combined use of the two single-particle analytical techniques on the same individual particles showed that Asian Dust particles had experienced extensive chemical modification during long-range transport. Overall, 109 individual particles were classified into four particle types based on their morphology, elemental concentrations, and molecular species and/or functional groups of individual particles available from the two analytical techniques: Ca-containing (38%); NaNO3-containing (30%); silicate (22%); and miscellaneous particles (10%). Among the 41 Ca-containing particles, 10, 8, and 14 particles contained nitrate, sulfate, and both, respectively, whereas only two particles contained unreacted CaCO3. Airborne amorphous calcium carbonate (ACC) particles were observed in this Asian Dust sample for the first time, where their IR peaks for the insufficient symmetric environment of CO32− ions of ACC were clearly differentiated from those of crystalline CaCO3. This paper also reports the field observations of CaCl2 particles converted from CaCO3 for the Asian Dust sample collected in the planetary boundary layer. Thirty three particles contained NaNO3, which are the reaction products of sea-salt and NOx/HNO3, whereas no genuine sea-salt particles were encountered, indicating that sea-salt particles are more reactive than CaCO3 particles. Some silicate particles were observed to contain nitrate, sulfate, and water. Among 24 silicate particles, 10 particles contained water, the presence of which could facilitate atmospheric heterogeneous reactions of silicate particles including swelling minerals, such as montmorillonite and vermiculite, and non-swelling ones, such as feldspar and quartz. This paper provides detailed information on the physicochemical characteristics of individual Asian Dust particles that experienced extensive chemical modification during long-range transport through the combined use of the two single-particle analytical techniques." @default.
• W2318404116 created "2016-06-24" @default.
• W2318404116 creator A5002246850 @default.
• W2318404116 creator A5042762809 @default.
• W2318404116 creator A5049263275 @default.
• W2318404116 creator A5066578495 @default.
• W2318404116 creator A5068100868 @default.
• W2318404116 creator A5070465686 @default.
• W2318404116 date "2012-10-17" @default.
• W2318404116 modified "2023-10-16" @default.
• W2318404116 title "Observation of chemical modification of Asian Dust particles during long-range transport by the combined use of quantitative ED-EPMA and ATR-FT-IR imaging" @default.
• W2318404116 cites W1661141144 @default.
• W2318404116 cites W1664291249 @default.
• W2318404116 cites W1906416366 @default.
• W2318404116 cites W1922663536 @default.
• W2318404116 cites W1965158560 @default.
• W2318404116 cites W1972384340 @default.
• W2318404116 cites W1973728267 @default.
• W2318404116 cites W1978859451 @default.
• W2318404116 cites W1981920792 @default.
• W2318404116 cites W1993373772 @default.
• W2318404116 cites W1998779579 @default.
• W2318404116 cites W1999868042 @default.
• W2318404116 cites W2000510490 @default.
• W2318404116 cites W2004244427 @default.
• W2318404116 cites W2006407068 @default.
• W2318404116 cites W2007230074 @default.
• W2318404116 cites W2013526692 @default.
• W2318404116 cites W2018024014 @default.
• W2318404116 cites W2018499373 @default.
• W2318404116 cites W2018730602 @default.
• W2318404116 cites W2019577728 @default.
• W2318404116 cites W2019900533 @default.
• W2318404116 cites W2021250814 @default.
• W2318404116 cites W2026795369 @default.
• W2318404116 cites W2028959227 @default.
• W2318404116 cites W2029157867 @default.
• W2318404116 cites W2032127570 @default.
• W2318404116 cites W2037825859 @default.
• W2318404116 cites W2038624089 @default.
• W2318404116 cites W2041033720 @default.
• W2318404116 cites W2041485177 @default.
• W2318404116 cites W2041735804 @default.
• W2318404116 cites W2041987850 @default.
• W2318404116 cites W2043339911 @default.
• W2318404116 cites W2051161175 @default.
• W2318404116 cites W2054959591 @default.
• W2318404116 cites W2057089681 @default.
• W2318404116 cites W2061636889 @default.
• W2318404116 cites W2061916782 @default.
• W2318404116 cites W2064670849 @default.
• W2318404116 cites W2065264826 @default.
• W2318404116 cites W2065352925 @default.
• W2318404116 cites W2080219468 @default.
• W2318404116 cites W2085364201 @default.
• W2318404116 cites W2087838164 @default.
• W2318404116 cites W2087859936 @default.
• W2318404116 cites W2095535725 @default.
• W2318404116 cites W2096049379 @default.
• W2318404116 cites W2103719236 @default.
• W2318404116 cites W2105463749 @default.
• W2318404116 cites W2112531993 @default.
• W2318404116 cites W2113670949 @default.
• W2318404116 cites W2127680170 @default.
• W2318404116 cites W2133544629 @default.
• W2318404116 cites W2162923152 @default.
• W2318404116 cites W2164988561 @default.
• W2318404116 cites W2318150963 @default.
• W2318404116 cites W2318186751 @default.
• W2318404116 cites W2322569073 @default.
• W2318404116 cites W2335180093 @default.
• W2318404116 cites W4238855760 @default.
• W2318404116 cites W4302083512 @default.
• W2318404116 doi "https://doi.org/10.5194/acpd-12-27297-2012" @default.
• W2318404116 hasPublicationYear "2012" @default.
• W2318404116 type Work @default.
• W2318404116 sameAs 2318404116 @default.
• W2318404116 citedByCount "1" @default.
• W2318404116 countsByYear W23184041162013 @default.
• W2318404116 crossrefType "posted-content" @default.
• W2318404116 hasAuthorship W2318404116A5002246850 @default.
• W2318404116 hasAuthorship W2318404116A5042762809 @default.
• W2318404116 hasAuthorship W2318404116A5049263275 @default.
• W2318404116 hasAuthorship W2318404116A5066578495 @default.
• W2318404116 hasAuthorship W2318404116A5068100868 @default.
• W2318404116 hasAuthorship W2318404116A5070465686 @default.
• W2318404116 hasBestOaLocation W23184041161 @default.
• W2318404116 hasConcept C107872376 @default.
• W2318404116 hasConcept C111368507 @default.
• W2318404116 hasConcept C113196181 @default.
• W2318404116 hasConcept C127313418 @default.
• W2318404116 hasConcept C138411078 @default.
• W2318404116 hasConcept C159985019 @default.
• W2318404116 hasConcept C160529264 @default.
• W2318404116 hasConcept C178790620 @default.
• W2318404116 hasConcept C185592680 @default.
• W2318404116 hasConcept C192562407 @default.
• W2318404116 hasConcept C193024070 @default.
• W2318404116 hasConcept C199289684 @default.
• W2318404116 hasConcept C204323151 @default.

• next