TY - JOUR
T1 - Direct Comparison of the Submicron Aerosol Hygroscopicity of Water-Soluble Sugars
AU - Dawson, Joseph Nelson
AU - Malek, Kotiba A.
AU - Razafindrambinina, Patricia N.
AU - Raymond, Timothy M.
AU - Dutcher, Dabrina D.
AU - Asa-Awuku, Akua A.
AU - Freedman, Miriam Arak
N1 - Funding Information:
U.S. National Science Foundation Award (NSF) 1255832, 1723290, 1723874.
Funding Information:
M.A.F. and J.N.D. acknowledge support from the NSF: AGS-1723290 and E. -J. E. Ott for her work on the measurement of sucrose surface tension. J.N.D. acknowledges funding from the NSF GRFP (NSF 1255832). A.A.-A. and P.N.R. acknowledge support from the NSF: 1723920. D.D.D., T.M.R., and K.A.M. acknowledge support from the NSF: 1723874 and thank H. Jacoby for her contributions to the first field campaign, as well as, K. Nguyen, L. Romano, and B. King for their software.
PY - 2020
Y1 - 2020
N2 - Water-soluble organic compounds (WSOCs) readily uptake water and form atmospheric droplets. Understanding the water-uptake ability of these WSOCs can improve our understanding of their radiative effects and thus can improve current climate models. In this study, we measure the subsaturated and supersaturated droplet growth of four WSOCs: levoglucosan, sucrose, raffinose, and trehalose. Specifically, we use three distinct nanoscale droplet growth methods: cavity ring-down spectroscopy (CRDS), hygroscopic tandem differential mobility analysis (H-TDMA), and cloud condensation nuclei (CCN) counting and report optical growth factor (fRH), growth factor (Gf), refractive indices, and critical activation diameters (dp50) for each aerosol system. Köhler theory (assuming a droplet surface tension equal to that of pure water) is applied to all droplet growth measurements, and the single-parameter hygroscopicity, κ, is reported for the four WSOCs measured on the different platforms. The three experimental methods measure decreased hygroscopicity with an increase in WSOC molecular weight. When assuming the droplets are dilute, κ values from measurements are consistent with known values. The three experimental methods have comparable precision with systematic deviations in the average κ for each method. Few studies have employed fRH data to obtain κ values. The current two methods to estimate κ from fRH data produce similar results, are dry aerosol size-dependent, and agree with κ values that assume dilute solution behavior. Thus, the presented measured data set and analysis contribute to the comparison of subsaturated and supersaturated data from optical and geometric methods for organic aerosol.
AB - Water-soluble organic compounds (WSOCs) readily uptake water and form atmospheric droplets. Understanding the water-uptake ability of these WSOCs can improve our understanding of their radiative effects and thus can improve current climate models. In this study, we measure the subsaturated and supersaturated droplet growth of four WSOCs: levoglucosan, sucrose, raffinose, and trehalose. Specifically, we use three distinct nanoscale droplet growth methods: cavity ring-down spectroscopy (CRDS), hygroscopic tandem differential mobility analysis (H-TDMA), and cloud condensation nuclei (CCN) counting and report optical growth factor (fRH), growth factor (Gf), refractive indices, and critical activation diameters (dp50) for each aerosol system. Köhler theory (assuming a droplet surface tension equal to that of pure water) is applied to all droplet growth measurements, and the single-parameter hygroscopicity, κ, is reported for the four WSOCs measured on the different platforms. The three experimental methods measure decreased hygroscopicity with an increase in WSOC molecular weight. When assuming the droplets are dilute, κ values from measurements are consistent with known values. The three experimental methods have comparable precision with systematic deviations in the average κ for each method. Few studies have employed fRH data to obtain κ values. The current two methods to estimate κ from fRH data produce similar results, are dry aerosol size-dependent, and agree with κ values that assume dilute solution behavior. Thus, the presented measured data set and analysis contribute to the comparison of subsaturated and supersaturated data from optical and geometric methods for organic aerosol.
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U2 - 10.1021/acsearthspacechem.0c00159
DO - 10.1021/acsearthspacechem.0c00159
M3 - Article
AN - SCOPUS:85096635003
JO - ACS Earth and Space Chemistry
JF - ACS Earth and Space Chemistry
SN - 2472-3452
ER -