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  Home > JCE Print > Journal of Chemical Education > Issues > 1997  > August  >
In the Laboratory
Convection in a Continuously Stratified Fluid
Richard M. Heavers
Department of Chemistry and Physics, Roger Williams University, One Old Ferry Road, Bristol, RI 02809-2921

Cover
August 1997
Vol. 74 No. 8
p. 965

Abstract
This paper begins by commemorating Count Rumford's observations of convection in 1797. Rumford investigated the effects of stewed apples, eiderdown, and other fibrous materials on retarding vertical circulation in liquids. In contrast to Count Rumford's historic experiments, the present paper describes a simple, visually instructive, physical chemistry experiment for demonstrating how a mathematical model can be applied to free convection in a vertically stratified salt solution. In the first part of the experiment, a linear salt concentration profile is created in a beaker of water at room temperature. The salt concentration (and density) is greatest at the bottom of the liquid. When the beaker containing the salt solution is then heated on a hot plate, a well defined convecting bottom layer forms almost immediately. The measured rate of growth in thickness of this convecting layer is compared to that predicted from a model based on density differences. The temperature of the liquid above the bottom convecting layer remains close to its initial value, illustrating that heat from the hot plate is confined to the bottom layer by the salt (density) stratification.
More Information
*  Citation
Heavers, Richard M. J. Chem. Educ. 1997 74 965.
*  Keywords
Demonstrations, History/Philosophy, Laboratory Instruction, Laboratory Equipment/Apparatus, Liquids
*  History
Created:
Last Updated:
July 28, 1999
June 23, 2005
  Home > JCE Print > Journal of Chemical Education > Issues > 1997 > August > Page 965


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