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  5. The Absorption of Gaseous Iodine by Water Droplets
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The Absorption of Gaseous Iodine by Water Droplets

Date Issued
March 1, 1985
Author(s)
Albert, Michael F.
Advisor(s)
Jack S. Watson
Additional Advisor(s)
Joseph J. Perona
H. L. Dodds Jr.
Permanent URI
https://trace.tennessee.edu/handle/20.500.14382/39101
Abstract

A new model has been developed for predicting the rate at which gaseous molecular iodine is absorbed by water sprays. The model is a quasi-steady state mass transfer model that includes the iodine hydrolysis reactions. The parameters of the model are spray drop size, initial concentration of the gas and liquid phases, temperature, pressure, buffered or unbuffered spray solution, spray flow rate, containment diameter and drop fall height. The results of the model were studied under many values of these parameters. Plots of concentration of iodine species in the drop versus time have been produced by varying the initial gas phase concentration of molecular iodine over the range of 1 x 10-10 moles/liter and a drop size of 1000 microns.


Results from the model are compared to results available from the Containment Systems Experiments at Pacific Northwest Laboratory. The difference between the model predictions and the experimental data ranges from -120.5% to 68.0% with the closest agreement 7.7%. The new spray model is also compared to previously existing spray models. At high concentrations of gaseous molecular iodine, the new spray model is considered to be less accurate but at low concentrations, the new model predicts results that are closer to the experimental data. Inclusion of the iodine hydrolysis reactions is shown to be a feature important to a model intended for determining the removal of molecular iodine over a wide range of conditions.

Disciplines
Chemical Engineering
Degree
Master of Science
Major
Chemical Engineering
Embargo Date
March 1, 1985
File(s)
Thumbnail Image
Name

AlbertMichaelF_1985_OCRed.pdf

Size

25.73 MB

Format

Adobe PDF

Checksum (MD5)

16ff7f5ce20b41320808c32f388d1bee


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