Early stages of glacial clustering in supercooled triphenyl phosphite

Birgit Effey Schwickert, Steven R. Kline, H. Zimmermann, K. M. Lantzky, J. L. Yarger

Research output: Contribution to journalArticle

21 Scopus citations

Abstract

Glacial phase clustering and growth in triphenyl phosphite is observed in the temperature interval of 210 K to 214 K by small angle neutron scattering performed at the NIST Center for Neutron Research. Presented are the radius, volume fraction, and polydispersity of clusters of glacial phase surrounded by a supercooled liquid. The data can be interpreted in a four-step model of (I) cluster formation, (II) rapid nucleation, (III) agglomeration, and finally (IV) saturation. Two schemes of cluster growth can be identified. The first one is a region of radius stagnation (II), which is followed by a region of volume stagnation (III). Competition between the increase in cluster size and the increase in the number of clusters is deduced from this behavior.

Original languageEnglish (US)
Article number045410
Pages (from-to)454101-454106
Number of pages6
JournalPhysical Review B - Condensed Matter and Materials Physics
Volume64
Issue number4
StatePublished - Jul 15 2001
Externally publishedYes

ASJC Scopus subject areas

  • Electronic, Optical and Magnetic Materials
  • Condensed Matter Physics

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    Schwickert, B. E., Kline, S. R., Zimmermann, H., Lantzky, K. M., & Yarger, J. L. (2001). Early stages of glacial clustering in supercooled triphenyl phosphite. Physical Review B - Condensed Matter and Materials Physics, 64(4), 454101-454106. [045410].