High temperature reaction kinetics
Description:
During the last year the dependence of the apparent rate of OD + CO on water pressure was measured at 305, 570, 865 and 1223 K. An explanation was found and tested for the H/sub 2/O dependence of the apparent rate of OH(OD) + CO at high temperatures. The isotope effect for OH(D) with CO was determined over the temperature range 330 K to 1225 K. The reason for the water dependence of the rate of OH(OD) + CO near room temperatures has been investigated but no clear explanation has been found. 1 f…
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Date:
January 1, 1985
Creator:
Jonah, C. D.; Beno, M. F.; Mulac, W. A. & Bartels, D.
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Partner:
UNT Libraries Government Documents Department