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Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol

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Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. / Huff Hartz, K.E.; Rosenørn, Torben; Ferchak, S.R. et al.

In: Journal of Geophysical Research F: Earth Surface, Vol. 110, No. 14, 2005, p. D14208-15.

Research output: Contribution to journal/Conference contribution in journal/Contribution to newspaper › Journal article › Research › peer-review

Harvard

Huff Hartz, KE, Rosenørn, T, Ferchak, SR, Raymond, TM, Bilde, M, Donahue, NM & Pandis, SN 2005, 'Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol', Journal of Geophysical Research F: Earth Surface, vol. 110, no. 14, pp. D14208-15. https://doi.org/10.1029/2004JD005754

APA

Huff Hartz, K. E., Rosenørn, T., Ferchak, S. R., Raymond, T. M., Bilde, M., Donahue, N. M., & Pandis, S. N. (2005). Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. Journal of Geophysical Research F: Earth Surface, 110(14), D14208-15. https://doi.org/10.1029/2004JD005754

CBE

Huff Hartz KE, Rosenørn T, Ferchak SR, Raymond TM, Bilde M, Donahue NM, Pandis SN. 2005. Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. Journal of Geophysical Research F: Earth Surface. 110(14):D14208-15. https://doi.org/10.1029/2004JD005754

MLA

Huff Hartz, K.E. et al. "Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol". Journal of Geophysical Research F: Earth Surface. 2005, 110(14). D14208-15. https://doi.org/10.1029/2004JD005754

Vancouver

Huff Hartz KE, Rosenørn T, Ferchak SR, Raymond TM, Bilde M, Donahue NM et al. Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. Journal of Geophysical Research F: Earth Surface. 2005;110(14):D14208-15. doi: 10.1029/2004JD005754

Author

Huff Hartz, K.E. ; Rosenørn, Torben ; Ferchak, S.R. et al. / Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. In: Journal of Geophysical Research F: Earth Surface. 2005 ; Vol. 110, No. 14. pp. D14208-15.

Bibtex

@article{d0361517d9f24e6d8e4be6ea9814d8f9,

title = "Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol",

abstract = "The ability of biogenic secondary organic aerosol (SOA) to contribute to the concentration of cloud condensation nuclei (CCN) in the atmosphere is examined. Aerosol is generated by the ozonolysis reaction of monoterpenes (α-pinene, β-pinene, 3-carene, and limonene) and sesquiterpenes (β-caryophyllene, α-humulene, and α-cedrene) in a 10 m temperature-controlled Teflon smog chamber. In some cases, a self-seeding technique is used, which enables high particle concentrations with the desired diameters without compromising particle composition and purity. The monoterpene SOA is excellent CCN material, and it activates similarly (average activation diameter equals 48 ± 8 nm at 1% supersaturation for the species used in this work) to highly water-soluble organic species. Its effective solubility in water was estimated to be in the range of 0.07-0.40 g solute/g HO. CCN measurements for sesquiterpene SOA (average activation diameter equals 120 ± 20 nm at 1% supersaturation for the species used in this work) show that it is less CCN active than monoterpene SOA. The initial terpene mixing ratio (between 3 and 100 ppb) does not affect the CCN activation for freshly generated SOA.",

author = "{Huff Hartz}, K.E. and Torben Rosen{\o}rn and S.R. Ferchak and T.M. Raymond and M. Bilde and N.M. Donahue and S.N. Pandis",

year = "2005",

doi = "10.1029/2004JD005754",

language = "English",

volume = "110",

pages = "D14208--15",

journal = "Journal of Geophysical Research",

issn = "0148-0227",

publisher = "American Geophysical Union",

number = "14",

}

RIS

TY - JOUR

T1 - Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol

AU - Huff Hartz, K.E.

AU - Rosenørn, Torben

AU - Ferchak, S.R.

AU - Raymond, T.M.

AU - Bilde, M.

AU - Donahue, N.M.

AU - Pandis, S.N.

PY - 2005

Y1 - 2005

N2 - The ability of biogenic secondary organic aerosol (SOA) to contribute to the concentration of cloud condensation nuclei (CCN) in the atmosphere is examined. Aerosol is generated by the ozonolysis reaction of monoterpenes (α-pinene, β-pinene, 3-carene, and limonene) and sesquiterpenes (β-caryophyllene, α-humulene, and α-cedrene) in a 10 m temperature-controlled Teflon smog chamber. In some cases, a self-seeding technique is used, which enables high particle concentrations with the desired diameters without compromising particle composition and purity. The monoterpene SOA is excellent CCN material, and it activates similarly (average activation diameter equals 48 ± 8 nm at 1% supersaturation for the species used in this work) to highly water-soluble organic species. Its effective solubility in water was estimated to be in the range of 0.07-0.40 g solute/g HO. CCN measurements for sesquiterpene SOA (average activation diameter equals 120 ± 20 nm at 1% supersaturation for the species used in this work) show that it is less CCN active than monoterpene SOA. The initial terpene mixing ratio (between 3 and 100 ppb) does not affect the CCN activation for freshly generated SOA.

AB - The ability of biogenic secondary organic aerosol (SOA) to contribute to the concentration of cloud condensation nuclei (CCN) in the atmosphere is examined. Aerosol is generated by the ozonolysis reaction of monoterpenes (α-pinene, β-pinene, 3-carene, and limonene) and sesquiterpenes (β-caryophyllene, α-humulene, and α-cedrene) in a 10 m temperature-controlled Teflon smog chamber. In some cases, a self-seeding technique is used, which enables high particle concentrations with the desired diameters without compromising particle composition and purity. The monoterpene SOA is excellent CCN material, and it activates similarly (average activation diameter equals 48 ± 8 nm at 1% supersaturation for the species used in this work) to highly water-soluble organic species. Its effective solubility in water was estimated to be in the range of 0.07-0.40 g solute/g HO. CCN measurements for sesquiterpene SOA (average activation diameter equals 120 ± 20 nm at 1% supersaturation for the species used in this work) show that it is less CCN active than monoterpene SOA. The initial terpene mixing ratio (between 3 and 100 ppb) does not affect the CCN activation for freshly generated SOA.

UR - http://www.scopus.com/inward/record.url?scp=24944547338&partnerID=8YFLogxK

U2 - 10.1029/2004JD005754

DO - 10.1029/2004JD005754

M3 - Journal article

AN - SCOPUS:24944547338

VL - 110

SP - D14208-15

JO - Journal of Geophysical Research

JF - Journal of Geophysical Research

SN - 0148-0227

IS - 14

ER -