PDF file - Facultatea de Chimie şi Inginerie Chimică
PDF file - Facultatea de Chimie şi Inginerie Chimică
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MATHEMATICAL MODELING FOR THE CRYSTALLIZATION PROCESS OF HYDROXYAPATITE …<br />
Table 1. The experimental results of the transformation gra<strong>de</strong> of beta-whitlockite<br />
in time and at 20 0 C and 50 0 C for different pH values<br />
pH<br />
Time<br />
[s]<br />
η<br />
0 3600 7200 10800 14400 18000 21600 25200 28800 32400<br />
8.5<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.003<br />
0.005<br />
0.009<br />
0.025<br />
0.021<br />
0.052<br />
0.042<br />
0.090<br />
0.063<br />
0.142<br />
0.092<br />
0.190<br />
0.120<br />
0.250<br />
0.158<br />
0.328<br />
0.191<br />
0.390<br />
9.1<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.055<br />
0.092<br />
0.215<br />
0.330<br />
0.415<br />
0.590<br />
0.620<br />
0.800<br />
0.775<br />
0.910<br />
0.880<br />
0.971<br />
0.945<br />
0.990<br />
0.981<br />
1.000<br />
0.991<br />
-<br />
9.7<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.068<br />
0.102<br />
0.240<br />
0.340<br />
0.470<br />
0.610<br />
0.670<br />
0.815<br />
0.820<br />
0.920<br />
0.920<br />
0.977<br />
0.962<br />
0.990<br />
0.980<br />
1.000<br />
1.000<br />
-<br />
10.2<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.101<br />
0.136<br />
0.350<br />
0.450<br />
0.620<br />
0.740<br />
0.820<br />
0.910<br />
0.940<br />
0.978<br />
0.981<br />
0.996<br />
0.996<br />
1.000<br />
1.000<br />
-<br />
-<br />
-<br />
11.3<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.110<br />
0.157<br />
0.370<br />
0.490<br />
0.650<br />
0.790<br />
0.840<br />
0.931<br />
0.950<br />
0.982<br />
0.986<br />
0.997<br />
0.996<br />
1.000<br />
1.000<br />
-<br />
-<br />
-<br />
12<br />
20ºC<br />
50ºC<br />
0<br />
0<br />
0.119<br />
0.187<br />
0.400<br />
0.560<br />
0.680<br />
0.840<br />
0.860<br />
0.960<br />
0.960<br />
0.995<br />
0.989<br />
1.000<br />
1.000<br />
-<br />
-<br />
-<br />
-<br />
-<br />
From the slope were <strong>de</strong>termined the numerical values of the K<br />
constants, presented in Table 2.<br />
Tablel 2. The values of K constant<br />
20 0 C 50 0 pH<br />
C<br />
K1 K2 K3 K1 K2 K3<br />
8.5 6.583E-06 2.032E-10 1.920E-19 1.513E-05 4.671E-10 4.412E-19<br />
9.1 1.510E-04 4.649E-09 4.392E-18 2.480E-04 7.655E-09 7.232E-18<br />
9.7 1.740E-04 5.372E-09 5.075E-18 2.620E-04 8.089E-09 7.641E-18<br />
10.2 2.410E-04 8.356E-09 9.915E-18 3.340E-04 1.158E-08 1.374E-17<br />
11.3 2.600E-04 9.036E-09 1.072E-17 3.830E-04 1.329E-08 1.577E-17<br />
12 2.450E-04 9.728E-09 1.494E-17 3.980E-04 1.579E-08 2.425E-17<br />
In or<strong>de</strong>r to i<strong>de</strong>ntify the mathematical mo<strong>de</strong>l which <strong>de</strong>scribes the<br />
process the process simulation was nee<strong>de</strong>d. For this purpose the numerical<br />
values of the K1, K2 and K3 from Table 2 were used and different times were<br />
calculated relating to the transformation gra<strong>de</strong> of beta-whitlockite in HAP and<br />
compared with the experimental results. The results obtained at 20 0 C and<br />
50 0 C for pH=9.7 are presented in Figure 3 (the simulations were ma<strong>de</strong> for all<br />
pH values, but in this article are presented only the relevant simulation results).<br />
The analysis of the results show a very good fit of the experimental<br />
results with those calculated for equation (16), where the errors for the majority<br />
of the results don’t exceed 2%. In the mathematical mo<strong>de</strong>ls expressed by<br />
equations (14) and (18) the <strong>de</strong>viations from the experimental values are high.<br />
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