Harvard University School of Engineering and Applied Sciences  Environmental Sciences and
Engineering (ESE) Program
Atmospheric Sciences Seminar
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Current Projects
 
  • Phase Transitions of
       Atmospheric Particles


     - Crystallization of SNAP
        Particles
     - 1×3TDMA
     - Atmospheric Nanoparticles
     - Modeling Aerosol Phase
        Transitions and Radiative
        Effects


  • Dissolution and
       Precipitation of Minerals
       in Aquatic Environments

     
  • Chemical Oxidation
       Reactions and Hydrophobic
       -to-Hydrophilic Aging of OAs


     - Aerodyne AMS analysis
     - CCN properties of OAs

  • Origins of Life:
       Mineral Surface Photo-
       Electrochemistry


  • Harvard Environmental Chamber

    AMAZE-08


    Closed Projects

      - Crystallization of Sulfate and
       Nitrate Coatings on
       Tropospheric Mineral Particles

     
      - Tropospheric Mineral
       Particles as Ice Nuclei

     
      - Building Structures at
       the Nanoscale



     

    Crystallization of Sulfate-Nitrate-Ammonium
    -Proton Particles

    Aerosol particles exhibit hysteresis in their interaction with water vapor. Crystalline particles uptake liquid water when the ambient relative humidity (RH) reaches the deliquescence relative humidity (DRH) of the particles. However, aqueous particles of the same composition do not crystallize at the DRH, but become highly supersaturated until the RH reaches the crystallization relative humidity (CRH) and the particles crystallize. Predictions of aerosol particle phase thus require knowledge of the DRH, the CRH, and the ambient relative humidity (RH) history. Although the DRH values of aerosol particles can be predicted based on thermodynamic models, there is currently no physical model that can successfully predict CRH values.

    Hysteresis

    DRH and CRH also depend on chemical composition. Particles composed of sulfate, nitrate, ammonium, and proton (SNA) are especially important because, on a global basis, they make the largest anthropogenic contribution to the aerosol mass budget.

    In our first report, we experimentally determined the CRH values of SNA particles as a function of composition, providing polynomials that can be used in chemical transport models to determine the physical state of particles. Subsequent reports have focused on identifying the specific solids formed when particles crystallize. We are currently interested in determining the morphology of crystalline particles and how morphology depends on relative humidity history.


    People Involved

    Publications

    1. T. Rosenoern, J.C. Schlenker, and S.T. Martin, "Hygroscopic Growth of Multicomponent Aerosol Particles Influenced by Several Cycles of Relative Humidity," Journal of Physical Chemistry A, 2008, 112, 2378-2385. PDF File. Errata.

    2. Schlenker, J.C., and Martin, S.T., "Crystallization Pathways of Sulfate-Nitrate-Ammonium Aerosol Particles," The Journal of Physical Chemistry A, 2005, 109, 9980-9985. PDF File.

    3. Schlenker, J.C., Malinowski, A., Martin, S.T., Hung, H.M., Rudich, Y., "Crystals Formed at 293 K by Aqueous Sulfate-Nitrate-Ammonium-Proton Aerosol Particles," Journal of Physical Chemistry A, 2004, 108, 9375-9383. PDF File.

    4. Martin, S.T., Schlenker, J.C., Malinowski, A., Hung, H.M., and Rudich, Y., "Crystallization of atmospheric sulfate-nitrate-ammonium particles," Geophysical Research Letters, 2003, 30, 2102. PDF File. Movie File.

     

     



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    Environmental Chemistry Group