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Source forensics of n-alkanes and n-fatty acids in urban aerosols using compound specific radiocarbon/stable carbon isotopic composition
n -Alkanes and fatty acids are important molecular markers for the source apportionment of organic matter in the atmosphere. Traditional approaches to date have mostly relied upon the source-specific differences in their molecular distributions and carbon preference index. Alternatively, we demonstrate here the use of stable carbon and radiocarbon isotopic composition ( δ ^13 C and Δ ^14 C, respectively) of n -alkanes and n -fatty acids in aerosols from two urban receptor sites (Beijing and Tianjin) in Northeast China to assess their sources in autumn. The Δ ^14 C _n _-alkanes of C _19 –C _24 and C _26 –C _32 even-carbon homologs (−851 to −708‰) indicate their dominance from fossil fuel combustion. In contrast, the Δ ^14 C of most abundant palmitic acid (C _16:0 ) and stearic acid (C _18:0 ) suggest a larger contribution from nonfossil sources (∼91%–94%), mainly due to inputs from cooking, biomass burning and microorganisms. Compared with lower Δ ^14 C of C _27 and C _31 n -alkanes (−449‰), C _29 n -alkane (−241‰) and C _20 –C _30 n -fatty acids (−263‰) showed more contemporary likely due to significant contribution from plant litter and biomass burning that contain more fresh biogenic material. Fossil character of C _27 –C _31 n -alkanes (40%) and C _20 –C _30 n -fatty acids (30%) could be from soil resuspension and/or loess deposits in upwind regions through long-range atmospheric transport.
Source forensics of n-alkanes and n-fatty acids in urban aerosols using compound specific radiocarbon/stable carbon isotopic composition
n -Alkanes and fatty acids are important molecular markers for the source apportionment of organic matter in the atmosphere. Traditional approaches to date have mostly relied upon the source-specific differences in their molecular distributions and carbon preference index. Alternatively, we demonstrate here the use of stable carbon and radiocarbon isotopic composition ( δ ^13 C and Δ ^14 C, respectively) of n -alkanes and n -fatty acids in aerosols from two urban receptor sites (Beijing and Tianjin) in Northeast China to assess their sources in autumn. The Δ ^14 C _n _-alkanes of C _19 –C _24 and C _26 –C _32 even-carbon homologs (−851 to −708‰) indicate their dominance from fossil fuel combustion. In contrast, the Δ ^14 C of most abundant palmitic acid (C _16:0 ) and stearic acid (C _18:0 ) suggest a larger contribution from nonfossil sources (∼91%–94%), mainly due to inputs from cooking, biomass burning and microorganisms. Compared with lower Δ ^14 C of C _27 and C _31 n -alkanes (−449‰), C _29 n -alkane (−241‰) and C _20 –C _30 n -fatty acids (−263‰) showed more contemporary likely due to significant contribution from plant litter and biomass burning that contain more fresh biogenic material. Fossil character of C _27 –C _31 n -alkanes (40%) and C _20 –C _30 n -fatty acids (30%) could be from soil resuspension and/or loess deposits in upwind regions through long-range atmospheric transport.
Source forensics of n-alkanes and n-fatty acids in urban aerosols using compound specific radiocarbon/stable carbon isotopic composition
Lujie Ren (author) / Yiyun Wang (author) / Kimitaka Kawamura (author) / Srinivas Bikkina (author) / Negar Haghipour (author) / Lukas Wacker (author) / Chandra Mouli Pavuluri (author) / Zhimin Zhang (author) / Siyao Yue (author) / Yele Sun (author)
2020
Article (Journal)
Electronic Resource
Unknown
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