Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
672924 | Thermochimica Acta | 2015 | 8 Pages |
Abstract
In this study, we have reinvestigated the thermal decomposition kinetics of iron(III) phosphate dihydrate FePO4â2H2O in air atmosphere by TG/DTG and DTA techniques using non-isothermal experiments. The apparent activation energy Eα was determined by the differential and integral isoconversional methods and suggested that the decomposition reaction is complex and follows multi-step processes. A mathematical deconvolution technique using Fraser-Suzuki equation was applied to the DTG curves and allowed the separation of two distinct processes. The apparent activation energies determined by the isoconversional Friedman's method were 93.05 ± 3.80 kJ molâ1 and 73.41 ± 3.14 kJ molâ1 for the first and second process respectively. Using Malek's procedure for each process, the characteristics of y(α) and z(α) functions showed that the kinetic reaction follows the Johnson-Mehl-Avrami model (JMA(n)). One-dimensional nucleation and growth mechanism occurred firstly with f(α1) = 1.272(1 â α1)[âln(1 â α1)](1 â 1/1.272) and pre-exponential factor A1 = 9.11 Ã 1010 minâ1. After 27% of total conversion, a two-dimensional nucleation and growth mechanism becomes predominant with f(α2) = 2.306(1 â α2)[âln(1 â α2)](1 â 1/2.306) and A2 = 1.28 Ã 108 minâ1. It was concluded that the two decomposition processes of FePO4â2H2O are closely interrelated and thus neglected the first process leads to incoherent results.
Keywords
Related Topics
Physical Sciences and Engineering
Chemical Engineering
Fluid Flow and Transfer Processes
Authors
Mariam Khachani, Adnane El Hamidi, Mohammed Kacimi, Mohammed Halim, Said Arsalane,