Skip to main content
Article
Hygroscopic growth and CCN activity of HULIS from different environments
Journal of Geophysical Research
  • Thomas B. Kristensen, University of Copenhagen, Copenhagen
  • Heike Wex, Leibniz Institute for Tropospheric Research
  • Bettina Nekat, Leibniz Institute for Tropospheric Research
  • Jacob K. Nøjgaard, Aarhus University
  • Dominik van Pinxteren, Leibniz Institute for Tropospheric Research
  • Douglas H. Lowenthal, Desert Research Institute, Reno
  • Lynn Mazzoleni, Michigan Technological University
  • Katrin Dieckmann, Leibniz Institute for Tropospheric Research
  • Christian Bender Koch, University of Copenhagen, Copenhagen
  • Thomas F. Mentel, Institute for Energy and Climate Research
  • Hartmut Herrmann, Leibniz Institute for Tropospheric Research
  • A. Gannet Hallar, Desert Research Institute, Reno
Document Type
Article
Publication Date
11-27-2012
Disciplines
Abstract

[1] Humic-like substances (HULIS) constitute a significant fraction of aerosol particles in different environments. Studies of the role of HULIS in hygroscopic growth and cloud condensation nuclei (CCN) activity of aerosol particles are scarce, and results differ significantly. In this work the hygroscopic growth and CCN activity of water extracts (WE) and HULIS extracted from particulate matter (PM) collected at a polluted urban site (Copenhagen, Denmark), a rural site (Melpitz, Germany) and the remote site Storm Peak Laboratory (Colorado, USA) were investigated. Measurements of inorganic ions, elemental carbon, organic carbon and water soluble organic carbon (WSOC) within the PM confirmed that the sources of aerosol particles most likely differed for the three samples. The hygroscopic properties of the filtered WE were characterized by hygroscopicity parameters for subsaturated conditions (κGF) of 0.25, 0.41 and 0.22, and for supersaturated conditions κCCN were 0.23, 0.29 and 0.22 respectively for the urban, rural and remote WE samples. The measured hygroscopic growth and CCN activity were almost identical for the three HULIS samples and could be well represented by κGF = 0.07 and κCCN = 0.08–0.10 respectively. Small amounts of inorganic ions were present in the HULIS samples so the actual values for pure HULIS are expected to be slightly lower (κGF* = 0.04–0.06 and κCCN* = 0.07–0.08). The HULIS samples are thus less hygroscopic compared to most previous studies. To aid direct comparison of hygroscopic properties of HULIS from different studies, we recommend that the fraction of inorganic species in the HULIS samples always is measured and reported.

Publisher's Statement

©2012. American Geophysical Union. Publisher's version of record: https://dx.doi.org/10.1029/2012JD018249

Version
Publisher's PDF
Citation Information
Thomas B. Kristensen, Heike Wex, Bettina Nekat, Jacob K. Nøjgaard, et al.. "Hygroscopic growth and CCN activity of HULIS from different environments" Journal of Geophysical Research Vol. 117 Iss. D22 (2012)
Available at: http://works.bepress.com/l-mazzoleni/38/