Emissions from the laboratory combustion of wildland fuels: Particle morphology and size

By Rajan K. Chakrabarty, Hans Moosmüller, Mark A. Garro, W. P. Arnott, J. Walker, R. Susott, R. Babbitt, Cyle E. Wold, E. Lincoln, W. Hao. 2006

218 citations recorded by the source corpus.

How researchers see this paper

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

Cloud condensation nucleation activity of biomass burning aerosol (2009, background): “: CCN ACTIVITY OF BIOMASS BURNING AEROSOL 2 of 16 D22205 [Chakrabarty et al., 2006; Lewis et al., 2009] and the system is described further by Petters et al. [2009a].”
Ice nuclei emissions from biomass burning (2009, background): “[7] The soot fraction of fresh combustion particles consists of fractal-like chain aggregates with a threedimensional mass fractal dimension of 1.75, and their aerodynamic size can vary significantly from their geometric size [Chakrabarty et al., 2006].”
Transmission electron microscopy study of aerosol particles from the brown hazes in northern China (2009, background): “Some spherical particles were referred to as tar ball from biomass burning [Po´sfai et al., 2004; Hand et al., 2005; Chakrabarty et al., 2006 ].”
Strong spectral variation of biomass smoke light absorption and single scattering albedo observed with a novel dual-wavelength photoacoustic instrument (2008, background): “Soot optics can vary strongly with the number of monomers, monomer size, fractal dimension, and refractive index [Chakrabarty et al., 2006, 2007; Liu et al., 2008].”