Influence of the Mineralogical Composition of Clays and of Exchange Cations on the Catalytic Oxidation of Ethyl Alcohol in the Vapour Phase*

Clay Minerals ◽  
1954 ◽  
Vol 2 (11) ◽  
pp. 107-110
Author(s):  
Jose M. Albareda
1925 ◽  
Vol 22 (5) ◽  
pp. 738-750 ◽  
Author(s):  
F. H. Constable

(1) An apparatus has been devised in which the composition of the vapour phase passing over the catalyst can be varied at will, or two vapours can be used alternately as reactants.(2) By using ethyl alcohol, and amyl alcohol from fusel oil alternately as reactants, the poisoning of a very active copper gauze catalyst has been followed and the temperature coefficient of the dehydrogenation of ethyl alcohol by the copper has been measured during the poisoning.(3) The activity of the catalyst, poisoned by amyl alcohol, fell in accordance with the simple logarithmic law(4) Confirmation was obtained that the rates of dehydrogenation of ethyl and amyl alcohols were equal.(5) The temperature coefficient of dehydrogenation on the catalyst was unchanged throughout the poisoning, though the reaction velocity was reduced 30 times.(6) The temperature coefficient was also shown to be unchanged during sintering, the reaction-velocity having been reduced 10 times.(7) Equations are derived for the rate of poisoning of an exponential distribution of centres of activity when the poison attacks the more active centres selectively.(8) The relation deducedcannot usually be distinguished (except with special relations between the constants) from the simple logarithmic law of poisoning.(9) Thus the exponential distribution normally poisons like a surface composed of homogeneous centres, the temperature coefficient being unchanged by the poisoning.(10) The equationdescribes the reaction-velocity as a function of time, and temperature, and gives adequate explanation of previous experimental results on the forms of the heating and cooling curves with “poisonous” alcohols.(11) Frenkel has shown , where τ0 is the vibration frequency of the molecule perpendicular to the surface, and μ0 is the heat of desorption of one gram molecule. Thus if the heat of desorption is not small compared with the energy necessary to cause chemical disruption of the molecule, the previous equation becomesthe form of the equation being unaltered.


1957 ◽  
Vol 15 (1) ◽  
pp. 39-41
Author(s):  
Shinpachiro KATO ◽  
Yasuhiro OISHI

1931 ◽  
Vol 35 (11) ◽  
pp. 3272-3279 ◽  
Author(s):  
A. R. Day

2007 ◽  
Vol 25 (5) ◽  
pp. 335-345
Author(s):  
Narayandas Ganguly ◽  
Kallakuri Janakiram ◽  
Nabinkrishna Nag ◽  
Sudhirkumar Bhattacharyya

1967 ◽  
Vol 10 (6) ◽  
pp. 342-347
Author(s):  
Masashi Ikeda ◽  
Shigeru Mizukami ◽  
Yukio Nakayama ◽  
Yuji Takayama

1934 ◽  
Vol 26 (12) ◽  
pp. 1276-1279 ◽  
Author(s):  
John A. Patterson ◽  
Allan R. Day

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