Matches in SemOpenAlex for { <https://semopenalex.org/work/W1485303913> ?p ?o ?g. }
- W1485303913 endingPage "1203" @default.
- W1485303913 startingPage "1192" @default.
- W1485303913 abstract "Deokjeok Island is located off the west coast of the Korean Peninsula and is a suitable place to monitor the long-range transport of air pollutants from the Asian continent. In addition to pollutants, Asian dust particles are also transported to the island during long-range transport events. Episodic transport of dust and secondary particles was observed during intensive measurements in the spring (March 31-April 11) and fall (October 13-26) of 2009. In this study, the chemical characteristics of long-range-transported particles were investigated based on highly time-resolved ionic measurements with a particle-into-liquid system coupled with an online ion chromatograph (PILS-IC) that simultaneously measures concentrations of cations (Li+, Na , NH4+, K+, Ca2+, Mg2+) and anions (F-, C1-, NO3-, SO42-). The aerosol optical thickness (AOT) distribution retrieved by the modified Bremen Aerosol Retrieval (M-BAER) algorithm from moderate resolution imaging spectroradiometer (MODIS) satellite data confirmed the presence of a thick aerosol plume coming from the Asian continent towards the Korean peninsula. Seven distinctive events involving the long-range transport (LRT) of aerosols were identified and studied, the chemical components of which were strongly related to sector sources. Enrichment of acidic secondary aerosols on mineral dust particles, and even of sea-salt components, during transport was observed in this study. Backward trajectory, chemical analyses, and satellite aerosol retrievals identified two distinct events: a distinctively high [Ca2++Mg2]/[Na+] ratio (>2.0), which was indicative of a preprocessed mineral dust transport event, and a low [Ca2++Mg2+]/[Na+] ratio (<2.0), which was indicative of severe aging of sea-salt components on the processed dust particles. Particulate C1- was depleted by up to 85% in spring and 50% in the fall. A consistent fraction of carbonate replacement (FCR) averaged 0.53 in spring and 0.55 in the fall. Supporting evidences of C1- enrichment on the marine boundary layer prior to a dust front were also found. Supplemental materials are available for this article. Go to the publisher's online edition of the Journal of the Air & Waste Management Association for sector and air mass classifications of clean and LRT cases." @default.
- W1485303913 created "2016-06-24" @default.
- W1485303913 creator A5000165857 @default.
- W1485303913 creator A5001416971 @default.
- W1485303913 creator A5008816933 @default.
- W1485303913 creator A5030755601 @default.
- W1485303913 creator A5031326827 @default.
- W1485303913 creator A5044134935 @default.
- W1485303913 creator A5045513930 @default.
- W1485303913 creator A5052351431 @default.
- W1485303913 creator A5061907930 @default.
- W1485303913 creator A5066497556 @default.
- W1485303913 creator A5090060290 @default.
- W1485303913 date "2011-10-31" @default.
- W1485303913 modified "2023-10-09" @default.
- W1485303913 title "Observed Chemical Characteristics of Long-Range Transported Particles at a Marine Background Site in Korea" @default.
- W1485303913 cites W1973728267 @default.
- W1485303913 cites W1975518279 @default.
- W1485303913 cites W1975697764 @default.
- W1485303913 cites W1978859451 @default.
- W1485303913 cites W1980883613 @default.
- W1485303913 cites W1985187959 @default.
- W1485303913 cites W1989324384 @default.
- W1485303913 cites W1999599573 @default.
- W1485303913 cites W2008585672 @default.
- W1485303913 cites W2014082902 @default.
- W1485303913 cites W2014107246 @default.
- W1485303913 cites W2019458363 @default.
- W1485303913 cites W2023145721 @default.
- W1485303913 cites W2027023520 @default.
- W1485303913 cites W2028904249 @default.
- W1485303913 cites W2034931535 @default.
- W1485303913 cites W2045465826 @default.
- W1485303913 cites W2045967893 @default.
- W1485303913 cites W2051302314 @default.
- W1485303913 cites W2054119472 @default.
- W1485303913 cites W2060108973 @default.
- W1485303913 cites W2062275317 @default.
- W1485303913 cites W2062432057 @default.
- W1485303913 cites W2065422988 @default.
- W1485303913 cites W2068036296 @default.
- W1485303913 cites W2069276124 @default.
- W1485303913 cites W2084998902 @default.
- W1485303913 cites W2131565340 @default.
- W1485303913 cites W2135327894 @default.
- W1485303913 cites W2153242329 @default.
- W1485303913 cites W2156404109 @default.
- W1485303913 cites W2162923152 @default.
- W1485303913 cites W2164840653 @default.
- W1485303913 cites W2166286846 @default.
- W1485303913 cites W2172217559 @default.
- W1485303913 cites W43316755 @default.
- W1485303913 doi "https://doi.org/10.1080/10473289.2011.604001" @default.
- W1485303913 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/22168103" @default.
- W1485303913 hasPublicationYear "2011" @default.
- W1485303913 type Work @default.
- W1485303913 sameAs 1485303913 @default.
- W1485303913 citedByCount "5" @default.
- W1485303913 countsByYear W14853039132014 @default.
- W1485303913 countsByYear W14853039132015 @default.
- W1485303913 countsByYear W14853039132017 @default.
- W1485303913 countsByYear W14853039132018 @default.
- W1485303913 crossrefType "journal-article" @default.
- W1485303913 hasAuthorship W1485303913A5000165857 @default.
- W1485303913 hasAuthorship W1485303913A5001416971 @default.
- W1485303913 hasAuthorship W1485303913A5008816933 @default.
- W1485303913 hasAuthorship W1485303913A5030755601 @default.
- W1485303913 hasAuthorship W1485303913A5031326827 @default.
- W1485303913 hasAuthorship W1485303913A5044134935 @default.
- W1485303913 hasAuthorship W1485303913A5045513930 @default.
- W1485303913 hasAuthorship W1485303913A5052351431 @default.
- W1485303913 hasAuthorship W1485303913A5061907930 @default.
- W1485303913 hasAuthorship W1485303913A5066497556 @default.
- W1485303913 hasAuthorship W1485303913A5090060290 @default.
- W1485303913 hasBestOaLocation W14853039131 @default.
- W1485303913 hasConcept C107872376 @default.
- W1485303913 hasConcept C121332964 @default.
- W1485303913 hasConcept C127313418 @default.
- W1485303913 hasConcept C1276947 @default.
- W1485303913 hasConcept C153294291 @default.
- W1485303913 hasConcept C159985019 @default.
- W1485303913 hasConcept C160529264 @default.
- W1485303913 hasConcept C178790620 @default.
- W1485303913 hasConcept C185592680 @default.
- W1485303913 hasConcept C192562407 @default.
- W1485303913 hasConcept C19269812 @default.
- W1485303913 hasConcept C193024070 @default.
- W1485303913 hasConcept C204323151 @default.
- W1485303913 hasConcept C205649164 @default.
- W1485303913 hasConcept C2775840915 @default.
- W1485303913 hasConcept C2777007095 @default.
- W1485303913 hasConcept C2777517185 @default.
- W1485303913 hasConcept C2778343803 @default.
- W1485303913 hasConcept C2778804858 @default.
- W1485303913 hasConcept C2779345167 @default.
- W1485303913 hasConcept C39432304 @default.
- W1485303913 hasConcept C91586092 @default.
- W1485303913 hasConceptScore W1485303913C107872376 @default.