Aa. Christy et al., DETERMINATION OF KINETIC-PARAMETERS FOR THE DEHYDRATION OF CALCIUM-OXALATE MONOHYDRATE BY DIFFUSE-REFLECTANCE FT-IR SPECTROSCOPY, Applied spectroscopy, 48(5), 1994, pp. 561-568
Variable-temperature diffuse reflectance infrared spectroscopy was use
d to study the reaction kinetics of the dehydration of calcium oxalate
monohydrate. The kinetic analysis of the dehydration process indicate
s that there are two reactions taking place, as well as the presence o
f two different equimole water molecular environments in the crystal s
tructure of calcium oxalate monohydrate. Partial least-squares calibra
tion of the dehydration profiles was carried out to identify the evolu
tion sequence of the two different types of water molecules in the cry
stal structure of calcium oxalate monohydrate. The results indicate th
at the water molecules in the crystal structure which are responsible
for the stretching absorptions at 3428 and 3336 cm-1 are eliminated fi
rst at a higher rate, during the first part of the reaction, and the o
thers responsible for the absorptions at 3486 and 3058 cm-1 are elimin
ated at a later stage. The unexpected and unidentified band arising fr
om bending modes of one of the types of water molecules is shown to ar
ise from the same water molecules that are responsible for the stretch
ing absorptions at 3486 and 3058 cm-1. Kinetic parameters were determi
ned for the dehydration step, and the overall activation energy calcul
ated for the dehydration step is in agreement with values reported in
the literature. However, the clear presence of two distinct reactions
invalidates all previous determinations of reaction order.