The thermal stability and acidity of 12-tungstophosphoric acid (HPW) a
nd its salts, both fresh and postreaction, have been studied by in sit
u and ex situ infrared and thermal analytical methods. The relationshi
p between acidity and the lifetime and deactivation behavior in the hi
gh-pressure oligomerization of propene has also been investigated as h
as been the location of the active sites in heteropoly anions. These s
tudies have confirmed a correlation between structural stability and t
he salt cation, with the potassium salt of HPW being the most thermall
y stable. A correlation has also been established between salt Type (A
or B) and the nature of coke deposits formed during reaction. Type A
salts produced only Type I(aliphatic) coke during butene isomerisation
, butane cracking and short time-on-stream isothermal propene oligomer
isation reactions but both Type I and Type II (aromatic) coke in long
time-on-stream and/or nonisothermal oligomerisation operation. Type B
(high surface area) salts always formed both Type I and Type II coke.
In all cases the formation of Type II coke was responsible for catalys
t deactivation. This coke blocking of acidic sites Cas confirmed by NH
3 adsorption/desorption studies of postreaction heteropoly anions. On
the basis of shifts in IR bands, it is proposed that the coke deposits
responsible for deactivation are formed in the so-called cup M-O-M ed
ge sites of the Keggin Unit. A mechanism is proposed to describe the t
hermal decomposition of HPW. (C) 1995 Academic Press, Inc.