Formation of nanoparticles of blue haze enhanced by anthropogenic pollution

The molecular processes leading to formation of nanoparticles of blue haze over forested areas are highly complex and not fully understood. We show that the interaction between biogenic organic acids and sulfuric acid enhances nucleation and initial growth of those nanoparticles. With one cis-pinoni...

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Bibliographic Details
Main Authors: Zhang, Renyi (Author), Wang, Lin (Author), Khalizov, Alexei F. (Author), Zhao, Jun (Author), Zheng, Jun (Author), McGraw, Robert L. (Author), Molina, Luisa Tan (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: National Academy of Sciences, 2010-09-17T13:51:00Z.
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Online Access:Get fulltext
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100 1 0 |a Zhang, Renyi  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences  |e contributor 
100 1 0 |a Molina, Luisa Tan  |e contributor 
100 1 0 |a Molina, Luisa Tan  |e contributor 
700 1 0 |a Wang, Lin  |e author 
700 1 0 |a Khalizov, Alexei F.  |e author 
700 1 0 |a Zhao, Jun  |e author 
700 1 0 |a Zheng, Jun  |e author 
700 1 0 |a McGraw, Robert L.  |e author 
700 1 0 |a Molina, Luisa Tan  |e author 
245 0 0 |a Formation of nanoparticles of blue haze enhanced by anthropogenic pollution 
260 |b National Academy of Sciences,   |c 2010-09-17T13:51:00Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/58580 
520 |a The molecular processes leading to formation of nanoparticles of blue haze over forested areas are highly complex and not fully understood. We show that the interaction between biogenic organic acids and sulfuric acid enhances nucleation and initial growth of those nanoparticles. With one cis-pinonic acid and three to five sulfuric acid molecules in the critical nucleus, the hydrophobic organic acid part enhances the stability and growth on the hydrophilic sulfuric acid counterpart. Dimers or heterodimers of biogenic organic acids alone are unfavorable for new particle formation and growth because of their hydrophobicity. Condensation of lowvolatility organic acids is hindered on nano-sized particles, whereas ammonia contributes negligibly to particle growth in the size range of 3-30 nm. The results suggest that initial growth from the critical nucleus to the detectable size of 2-3 nm most likely occurs by condensation of sulfuric acid and water, implying that anthropogenic sulfur emissions (mainly from power plants) strongly influence formation of terrestrial biogenic particles and exert larger direct and indirect climate forcing than previously recognized. 
520 |a Robert A. Welch Foundation (A-1417) 
520 |a National Natural Science Foundation (China) (40728008) 
520 |a Department of Energy Atmospheric Sciences Program 
546 |a en_US 
690 |a aerosol 
690 |a biogenic 
690 |a climate 
690 |a nucleation 
690 |a forest 
655 7 |a Article 
773 |t Proceedings of the National Academy of Sciences of the United States of America