Monitoring Ice Nucleation in Pure and Salty Water via High-Speed Imaging and Computer Simulations

Sigurd Bauerecker*, Peter Ulbig, Victoria Buch#, Luboš Vrbka§ and Pavel Jungwirth*§
Institut für Physikalische and Theoretische Chemie, Technische Universität Braunschweig, D-38106 Braunschweig, Germany, Fachbereich Analytische Messtechnik and Druck, Physikalisch Technische Bundesanstalt, D-38116 Braunschweig, Germany, Fritz Haber Institute for Molecular Dynamics, Hebrew University, Jerusalem, Israel 91904, and Institute of Organic Chemistry and Biochemistry, Academy of Sciences of the Czech Republic and Center for Biomolecules and Complex Molecular Systems, 16610 Prague 6, Czech Republic
J. Phys. Chem. C, 2008, 112 (20), pp 7631–7636
DOI: 10.1021/jp711507f
Publication Date (Web): May 15, 2008
Copyright © 2008 American Chemical Society
* To whom correspondence should be addressed. For computational materials, E-mail: pavel.jungwirth@uochb.cas.cz. Phone: +420-220 410 314 . Fax: +420-220 410 320 (P.V.). For experimental issues, E-mail: s.bauerecker@tu-bs.de (S.B.).
,

Technische Universität Braunschweig.

,

Physikalisch Technische Bundesanstalt.

,
#

Hebrew University.

,
§

Academy of Sciences of the Czech Republic and Center for Biomolecules and Complex Molecular Systems.

Abstract

High-speed monitoring of the freezing process of freely suspended supercooled pure and salty water droplets is reported for the first time. Combined visual (VIS) and infrared (IR) imaging directly delivers three-dimensional and surface temperature information about the proceeding freezing front with up to 2000 frames per second. The freezing behavior changes gradually up to 1 M and dramatically above a 1 M NaCl concentration. To capture the initial stage of the nucleation molecular dynamics (MD), calculations with atomistic and femtosecond resolution have been performed, and homogeneous ice nucleation in a salt solution has been successfully simulated. A combination of experimental imaging and calculations allows one to unravel structural (e.g., preferred bulk or surface location of the ice nucleus and final ion distribution) and dynamical (time scales for nucleation and freezing) aspects of the freezing process in water and salt solutions. While the thermodynamic consequence of added salt, that is, lowering of the freezing point, is well-known, here, we elucidate the kinetic antifreeze effect of added salt and the molecular origin of the corresponding slow-down of ice nucleation and freezing.

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History

  • Published In Issue May 22, 2008
  • Article ASAPMay 15, 2008
  • Received: December 6, 2007
    Revised: February 7, 2008

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