Dergiler / Atmospheric Pollution Research / 2018 / Cilt: 9 - Sayı: 6

Potential role of intraparticle diffusion in dynamic partitioning of secondary organic aerosols T

Sayfa
1131–1136
DOI
—
🏛️Bu makalenin bibliyografik verileri ve tam metin bağlantısı DergiPark üzerinden sağlanmıştır.
DergiPark Kaydı ↗
✨

Yapay Zeka Hızlı Bakış & Çıkarımlar

AI Insight
⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

Dynamic partitioning framework might be therefore necessary for SOA parameterization and photochemical models such as CMAQ.

📌 3 Maddede Bu Makale

🎯
Amaç & Hipotez:Dynamic gas-particle partitioning for secondary organic aerosols (SOA) is modeled by incorporating all the three processes: external mass transfer from bulk air to particle surfaces, intraparticle diffusion (characterized by diffusion coefficient, D p ), and particle-phase reaction (characterized by first-order rate constant, k c ).
📊
Temel Bulgular & Veri:Sensitivity analysis shows that for a fast reaction case (k c = 10 −1 /s), intraparticle diffusion can be reasonably neglected for D p higher than 10 −19 m 2 /s and gas-particle partition coefficient (K part ) higher than 10 9 .
💡
Sonuç & Katkı:Dynamic partitioning framework might be therefore necessary for SOA parameterization and photochemical models such as CMAQ.
🔬Tür:Modelleme & Sayısal Simülasyon
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Alan Parametreleri

Özet

Dynamic gas-particle partitioning for secondary organic aerosols (SOA) is modeled by incorporating all the three processes: external mass transfer from bulk air to particle surfaces, intraparticle diffusion (characterized by diffusion coefficient, D p ), and particle-phase reaction (characterized by first-order rate constant, k c ). A fully analytical solution to this model is provided to examine role of intraparticle diffusion. Based on the solution, a criterion is provided to judge whether intraparticle diffusion can be neglected or not with particle-phase reaction accounted for. Results indicate that taking particle-phase reaction into consideration allows a wider range to neglect intraparticle diffusion. Sensitivity analysis shows that for a fast reaction case (k c = 10 −1 /s), intraparticle diffusion can be reasonably neglected for D p higher than 10 −19 m 2 /s and gas-particle partition coefficient (K part ) higher than 10 9 . For a slow reaction case (k c = 10 −5 /s), intraparticle diffusion becomes negligible for D p higher than 10 −19 m 2 /s and K part higher than 10 11 . For 12 semi-volatile species used in a regional Community Multiscale Air Quality (CMAQ) model, D p is roughly approximated by their surrogates in various polymers. Species with relatively small K part and slow particle-phase reaction are more likely to be impacted by in- traparticle diffusion, besides small D p . Dynamic partitioning framework might be therefore necessary for SOA parameterization and photochemical models such as CMAQ.

🔖

Bu Makaleye Atıf Yap

LIU, C., CAO, J. (2018). Potential role of intraparticle diffusion in dynamic partitioning of secondary organic aerosols T. Atmospheric Pollution Research, Cilt: 9 - Sayı: 6, 1131–1136. https://ajindex.com/articles/214261

📄 Tam Metin PDF Okuyucu

📄

PDF görüntüleyici hazırlanıyor...

Kaynakça (8)

  1. Bateman, A.P., Gong, Z., Liu, P., Sato, B., Cirino, G., Zhang, Y., Artaxo, P., Bertram, A.K., Manzi, A.O., Rizzo, L.V., Souza, R.a.F., Zaveri, R.A., Martin, S.T., 2016. Sub-micro- metre particulate matter is primarily in liquid form over Amazon rainforest. Nat. Geosci. 9, 34–37.
  2. Brook, R.D., Rajagopalan, S., Pope, C.A., Brook, J.R., Bhatnagar, A., Diez-Roux, A.V., Holguin, F., Hong, Y., Luepker, R.V., Mittleman, M.A., Peters, A., Siscovick, D., Smith, S.C., Whitsel, L., Kaufman, J.D., 2010. Particulate matter air pollution and cardio- vascular disease: an update to the scientific statement from the American heart as- sociation. Circulation 121, 2331–2378.
  3. Carlton, A.G., Bhave, P.V., Napelenok, S.L., Edney, E.O., Sarwar, G., Pinder, R.W., Pouliot, G.A., Houyoux, M., 2010. Model representation of secondary organic aerosol in CMAQv4.7. Environ. Sci. Technol. 44, 8553–8560.
  4. Donahue, N.M., Robinson, A.L., Stanier, C.O., Pandis, S.N., 2006. Coupled partitioning, dilution, and chemical aging of semivolatile organics. Environ. Sci. Technol. 40, 02635–02643.
  5. Hall, W.A., Johnston, M.V., 2011. Oligomer content of α-pinene secondary organic aerosol. Aerosol Sci. Technol. 45, 37–45.
  6. Hallquist, M., Wenger, J.C., Baltensperger, U., Rudich, Y., Simpson, D., Claeys, M., Dommen, J., Donahue, N.M., George, C., Goldstein, A.H., Hamilton, J.F., Herrmann, H., Hoffmann, T., Iinuma, Y., Jang, M., Jenkin, M.E., Jimenez, J.L., Kiendler-Scharr, A., Maenhaut, W., Mcfiggans, G., Mentel, T.F., Monod, A., Prévôt, A.S.H., Seinfeld, J.H., Surratt, J.D., Szmigielski, R., Wildt, J., 2009. The formation, properties and impact of secondary organic aerosol: current and emerging issues. Atmos. Chem. Phys. 9, 5155–5236. Ipcc, 2013. Climate Change 2013: the Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press,
  7. Cambridge, United Kingdom and New York, NY, USA, pp. 1535. Isaacman-Vanwertz, G., Yee, L.D., Kreisberg, N.M., Wernis, R., Moss, J.A., Hering, S.V., De Sá, S.S., Martin, S.T., Alexander, M.L., Palm, B.B., Hu, W., Campuzano-Jost, P., Day, D.A., Jimenez, J.L., Riva, M., Surratt, J.D., Viegas, J., Manzi, A., Edgerton, E., Baumann, K., Souza, R., Artaxo, P., Goldstein, A.H., 2016. Ambient gas-particle partitioning of tracers for biogenic oxidation. Environ. Sci. Technol. 50, 9952–9962.
  8. Jimenez, J.L., Canagaratna, M.R., Donahue, N.M., Prevot, A.S.H., Zhang, Q., Kroll, J.H., Decarlo, P.F.