Steven Neshyba

Scanning Electron Microscopy of Pure Ice

Micrograph of a roughened prismatic facet of pure water ice obtained by variable-pressure scanning electron microscopy. The horizontal corrugations, called "trans-prismatic strands", are characteristic of the prismatic facet, and are thought to be pyramidal microfacets. Roughened pyramidal facets are seen at the bottom of this micrograph.

More Information

Steven NeshybaProfessor, Chemistry

BA, Reed College, 1981
PhD, Yale University, 1990

Physical, atmospheric

 

 


Teaching

Spring 2013: Chemistry 120


Research

Collaborators:

Ivan Gladich, Martina Roeselova, and Pavel Jungwirth, UOCHB

Penny Rowe and Von Walden, University of Idaho

Research page


 

CONTACT INFORMATION

Thompson 355D
253.879.3379
nesh@pugetsound.edu