Masters Theses

Abstract

"Classical considerations of the evaporation of a homogeneously nucleated droplet in an atmosphere of low humidity, indicates complete evaporation of the drop. Experimental results however, show that there is left behind a residual nucleus that is quite stable. Condensation occurs on these nuclei at comparatively low supersaturations. Using a specially instrumented cloud chamber, experimental procedures are described which attempt to investigate some of the properties of these nuclei. Various possibilities causing this stability are examined and compared to the experimental results obtained"--page [ii].

Advisor(s)

Kassner, James L.

Committee Member(s)

Russell, Robert R.
Rivers, Jack L.
Pyron, Howard D.

Department(s)

Physics

Degree Name

M.S. in Physics

Sponsor(s)

National Science Foundation (U.S.)

Publisher

University of Missouri at Rolla

Publication Date

1965

Pagination

xi, 90 pages

Note about bibliography

Includes bibliographical references (page 70).

Rights

© 1965 Ronald Dawbarn, All rights reserved.

Document Type

Thesis - Open Access

File Type

text

Language

English

Subject Headings

Atmospheric nucleationCloud chamberDropsEvaporation

Thesis Number

T 1724

Print OCLC #

5966875

Electronic OCLC #

805986622

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