L. Gianfreda et al., KINETIC-BEHAVIOR OF SYNTHETIC ORGANO-COMPLEXES AND ORGANO-MINERAL-UREASE COMPLEXES, Soil Science Society of America journal, 59(3), 1995, pp. 811-815
A study was conducted for characterizing the properties and the cataly
tic behavior of enzymatic complexes that are considered analogues of t
hose usually present in soil. Active enzymatic complexes were formed a
t 10 degrees C by interaction for 1 h of urease and tannic acid with a
nd without Fe ions and OH-Al polymers. The enzymatic complexes obtaine
d in the presence of Fe3+ ions and OH-Al species showed higher activit
y levels than urease-tannate complexes. The pH optimum of immobilized
urease did not differ significantly from that of free urease, except f
or the tannate complexes, which showed a pH optimum slightly shifted u
pwards by approximate to 0.5 units. Immobilized urease displayed the h
ighest activity in a wider range of temperatures (60-80 degrees C) com
pared with the free enzyme. The free enzyme showed a marked reduction
in activity above 70 degrees C. Higher values of energy of activation
(E(a)), enthalpy of activation (Delta H-a), and the kinetic parameter
(K-m) were obtained for urease immobilized on tannate molecules. On th
e contrary, the complexes obtained with Fe3+ and OH-Al species display
ed kinetic and thermodynamic parameters similar to those of the free e
nzyme. Immobilized urease showed a catalytic behavior similar to the f
ree enzyme, when the interaction with tannic acid occurred in the pres
ence of Fe3+ ions and OH-Al polymers. Evidently, both Fe ions and OH-A
l species favored the formation of enzymatic complexes in which confor
mational and catalytic features of the enzyme remained practically unc
hanged.