Laboratory studies on optical properties of secondary organic aerosols generated during the photooxidation of toluene and the ozonolysis of α -pinene: OPTICAL PROPERTIES OF SOAS

By T. Nakayama, Y. Matsumi, Kei Sato, T. Imamura, A. Yamazaki, A. Uchiyama. 2010

136 citations recorded by the source corpus.

Subfields: Atmospheric Science, Health, Toxicology and Mutagenesis

View Paper: https://www.semanticscholar.org/paper/fdbcf989392f0016367bd9395eb86fcdf469b209

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The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. K. Naumann
2. Neel Kotra
3. Jiu-meng Liu
4. Julia Laskin
5. Martin Gysel
6. A. Laskin
7. E. Edgerton
8. M. Laborde

In Health, Toxicology and Mutagenesis

1. Martin Gysel
2. M. Laborde
3. Joshua P. Schwarz
4. M. Schnaiter
5. B. Weinzierl

Citations in the corpus

• Optical properties and aging of light-absorbing secondary organic aerosol (2016, result): “Nakayama et al. (2013) has reported that light absorption of SOA has a dependence on NOx , that MAC increases with NOx , which likely also explains the higher k values reported by earlier work from the same group (Nakayama et al., 2010).”
• Size-resolved measurements of brown carbon in water and methanol extracts and estimates of their contribution to ambient fine-particle light absorption (2013, background): “Brown carbon also has secondary sources (e.g., Andreae and Gelencser, 2006; Chakrabarty et al., 2010; Chen and Bond, 2010; Nakayama et al., 2010; Sareen et al., 2010; Shapiro et al., 2009; Bones et al., 2010; Bate-man et al., 2011; Nguyen et al., 2012; de Haan et al., 2009; Zhang et al., 2011,…”
• A global simulation of brown carbon: Implications for photochemistry and direct radiative effect (2015, methodology): “In addition to the primary source above, we also consider SOC produced from aromatic oxidation as a secondary source of BrC (Hecobian et al., 2010; Jaoui et al., 2008; Lin et al., 2015; Nakayama et al., 2010; Nakayama et al., 2013; Zhong and Jang, 2011).”
• Single Particle Soot Photometer intercomparison at the AIDA chamber (2012, result): “This value is consistent with values reported by Nakayama et al. (2010) (n = 1.41−0i at λ = 532 nm andn = 1.458−0i atλ = 355 nm) but is lower than the one reported by Schnaiter et al. (2005), both for SOA fromα-pinene ozonolysis.”