3.1. Mechanochemical Synthesis of Mg-HA
Figure 3 shows the XRD patterns of the products prepared from different magnesium-based reagents according to reactions (1–3). As seen, all the XRD patterns of the samples produced from magnesium oxide have reflections of the initial MgO at 2θ = 43.03° and HA phases (
Figure 3a). At
x = 2 there is also a reflex at 2θ = 31.25
o, which belongs to the β-Ca
3(PO
4)
2 (TCP) phase. The XRD patterns of the samples synthesized using Mg(OH)
2 and Mg(H
2PO
4)
2·2H
2O contain only the apatite phase reflections (
Figure 3b,c). This leads to the conclusion that reactions 2 and 3 proceed entirely to completion, i.e. all the reagents participate in the formation of the Mg-HA structure, which is not the case for reaction 1.
Table 1 shows that the concentration of MgO in the resultant products is about two times less than that introduced into the initial mixture. Therefore, only a part of magnesium oxide reacts with the other components to form Mg-HA by reaction 1.
The changes in the cell and volume parameters in the substituted samples depending on the concentration of the introduced magnesium oxide confirm the presence of magnesium cations in the structure of the as-synthesized Mg-HA (
Figure 4). As seen, the most significant decrease in these values is observed for the samples prepared by reaction 2, with magnesium hydroxide used as the Mg source. This can be attributed to the different ionic radii of calcium and magnesium cations: R(Ca
2+) = 1.00 Å, R(Mg
2+) = 0.72 Å [
41]. In the case of MgO, a decrease in these parameters is not so marked because not all the magnesium has reacted, as mentioned above. In the case of monomagnesium phosphate, the larger changes in the parameters at large values of x, unlike the case of magnesium hydroxide, can be explained by the influence of a large number of water molecules released during the chemical interaction of this mixture of the reactants (reaction 3), which can increase the lattice parameter values. An interesting fact is that the concentration of the released water does not affect the crystallite size (
Figure 4c). Although the dopant concentration affects it; thus, the larger
x, the smaller the average crystallite size is.
The low reactivity of magnesium oxide in mechanochemical synthesis may be due to its high mechanical strength and strong abrasive resistance (periclase has a Mohs hardness value of 5.5, calcium oxide – 3.5), unlike the other reactants of the reaction mixture that are prone to hydration. The authors of study [
42] reported that, in the first minutes of the mechanochemical treatment of the initial mixture in a planetary ball mill, the grinding of the reagents occurs followed by the neutralization reaction with the formation of HA crystallites. The different degree of grinding of the reagents, resulted from their different hardness, does not allow the particles to be efficiently distributed over the volume of the reaction mixture. Therefore, only a small part of the surface layer of MgO particles is involved in Reaction (1). In this case, magnesium-deficient apatite with low (Са+Mg)/P ratio (< 1.67) is formed. With a deficiency of calcium ions in the HA cationic sublattice, the so-called "acidic" apatite Са
10–у(НРО
4)
у(РО
4)
6–у(ОН)
2–у is formed during mechanochemical synthesis [
43]. In our case, since a part of magnesium can be incorporated into the apatite crystal structure, the possible composition of the as-synthesized apatite is Са
10–xMg
x–y(НРО
4)
y(РО
4)
6–у(ОН)
2–y, where у < x. Consequently, reaction (1) can be re-written as follows:
The presence of (НРО
4)
2– groups in the structure of Mg-HA prepared from magnesium oxide is confirmed by the FTIR spectra (
Figure 5), which show a corresponding absorption band at 880 cm
-1 [
43], which is not observed in the spectra of the samples synthesized using magnesium hydroxide (
Figure 5b). The absorption bands of the phosphate anion (572, 602, 960, 1048, 1090 cm
-1) and the bands of stretching (3572 cm
-1) and libration (630 cm
-1) vibrations of the hydroxyl group in the HA structure appear in both spectra [
4]. The broad bands at 1640 and 3430 cm
-1 belong to adsorbed water, while the low-intensity bands at 1420 and 1470 cm
-1 correspond to the low carbonate ion content [
4].
The STA data confirm the presence of adsorbed and lattice water in the synthesized samples, which is released in the temperature range of 50–600
oС (
Figure 6). The amount of water in the samples is different and consistent with the stoichiometry of reaction equations (1)–(3). When MgO, Mg(OH)
2, and Mg(Н
2PO
4)
2·2Н
2О are used as the Mg sources, the amount of water released from the samples is 4.1, 7.1, and 7.2 wt.% respectively. The endoeffects observed in the DTA curves at higher temperatures are obviously related to the decomposition of the substituted apatite structure.
The data shown in
Table 2 indicate that the removal of adsorbed water does not change the phase composition of the samples synthesized with the addition of magnesium hydroxide and monomagnesium phosphate. They remain single phase in contrast to the samples synthesized with the incorporation of magnesium oxide. Heating of the samples obtained with MgO led to an increase in the MgO concentration and the formation of the TCP phase at
x = 1.5.
Figure 7 shows the changes in the unit cell parameters of the Mg-HA phase in the samples after heating at 500 °C. Comparing the data shown in this figure with those shown in
Figure 4, it is evident that, after heating, the parameters keep changing with increasing
x but not that much. At the same time, after the removal of water, the lattice parameters and cell volumes of the samples synthesized using Mg(OH)
2 and Mg(Н
2PO
4)
2·2Н
2О are nearly the same and keep decreasing with increasing
x. This suggests that the samples with the same
x are of comparable magnesium concentrations in the Mg-HA lattice. As for the samples synthesized using magnesium oxide, the change in the parameter
c is very similar to that for the samples obtained using both Mg(OH)
2 and Mg(Н
2PO
4)
2·2Н
2О, although the parameter
a increases with an increase in
x. The different trend in changing the parameter
a for the samples obtained with MgO may be caused by an increase in the number of vacancies of the OH groups in the Mg-HA structure [
4] in accordance with Formula (4). The decrease of the parameter
c in this case is due to the increase in the number of substitutions of the calcium positions with both the magnesium and hydrogen ion of the group (HPO
4)
2-, located also in the region of the vacant position of the calcium cation. After the water has been removed from the Mg-HA samples, the crystallite size of the apatite phase gradually decreases with increasing
x for all series of samples (
Figure 7d).
3.2. Lattice Parameters Predicted by DFT
The purpose of this section is to provide a theoretical insight on the incorporation of Mg2+ in the HA crystal lattice, since it is not possible to refine experimentally the structure of the substituted apatite in this case due to its small crystallite size and the low electron density of the substituent cation.
Figure 8 shows the calculated cell parameters for models containing different amount of Ca1 and Ca2 substitutions. As can be seen, the general tendency is the decrease of the unit cell size with the addition of Mg cations. However, the differences of the positions of the substituted Ca cations have significant effect on the cell parameters at high
x. In particular, at
x > 1, the cell parameters
a and
b decrease noticeably if magnesium is located in the Ca1 position, while the parameter
c increases only slightly. In the case of the Ca2 substitutions all parameters decreases but slower, than in the case of Ca1, so that the unit cell volumes at the same
x in both substitutions have comparable values in the whole range of magnesium concentrations and they decrease almost linearly with the increasing of the number of substitutions in the cell.
Comparison of the results of modeling (
Figure 8) with the experimental data (
Figure 4) suggests that during the synthesis of Mg-HA, the substitution of calcium by magnesium predominantly occurs in the Ca2 position. This is also indicated by the calculated values of the formation energy (E
f) of the substitutions of calcium for magnesium in the positions Ca1 and Ca2 shown in
Figure 9.
Figure 9 shows that the dependence of E
f on the magnesium concentration in Ca1 position has a parabolic shape with a minimum at
x = 1. The E
f values for substitutions in Ca2 position change irregularly as the concentration
x increases. As seen, all the values except for those at
x = 1 are below the E
f values for substitutions in Ca1 position, i.e., E
f(Ca1) > E
f(Ca2). At a concentration
x = 1, the formation energy values for both Mg substitutions are close, which means that the magnesium cation can coexist at the positions Ca1 and Ca2.
From the above, we can conclude that for almost all values of x, Mg substitution in the Ca2 position is energetically more favorable than in the Ca1 position, hence, the substitution in the Ca2 position mainly occurs during Mg-HA synthesis.
3.3. Thermal Stability of Mg-HA
The thermal stability of the Mg-HA samples synthesized using Mg(Н
2PO
4)
2·2Н
2О was investigated.
Figure 6 shows the changes in the XRD patterns of Mg-HA samples at different concentrations
x of magnesium after heat treatment at different temperatures. As seen, the substituted samples are less stable than unsubstituted HA. Upon decomposition of Mg-HA, the reflections of β-TCP and MgO appear in the XRD patterns, which was also reported by Moreira et al. [
44].
Figure 10.
XRD patterns of the Mg-HA samples with magnesium concentration x = 0.25 (a), x = 0.5 (b), x = 1.0 (c), and x = 2.0 (d) after heat treatment at different temperatures. Unmarked reflections belong to the HA phase.
Figure 10.
XRD patterns of the Mg-HA samples with magnesium concentration x = 0.25 (a), x = 0.5 (b), x = 1.0 (c), and x = 2.0 (d) after heat treatment at different temperatures. Unmarked reflections belong to the HA phase.
The results of the quantitative phase analysis of the XRD patterns by modeling their profiles showed that the decomposition of Mg-HA proceeds in two stages and the starting temperature of this process depends on the concentration of magnesium in the Mg-HA structure. As can be seen from
Table 3, at a concentration
x = 0.25, the sample remains single-phase up to 700 °C inclusive, whereas at 800 °C, a nanosized phase of magnesium oxide is formed. At higher values of
x, the MgO phase appears already at 700 °C. A further increase in the temperature up to 800 °C results in the formation of the second impurity phase, β-TCP, whereas the concentration of MgO increases. The amounts of MgO and β-TCP increase as the magnesium concentration in Mg-HA increases.
Figure 8a,b shows that, unlike the samples heated at 500 °C, the unit cell parameters and volume of the HA phase, annealed at 900 °C with the formation of the impurity phases MgO and β-TCP, almost do not change (
Figure 8c,d) (
Figure 5a-c). This implies that the HA structure after the formation of the impurity phases does not contain magnesium cations. At the same time, the unit cell parameter values of the β-TCP phase are
a = 10.34 Å and
c = 37.20 Å, which is much smaller than those reported by Bohner et al. [
45]. Consequently, the β-TCP phase contains magnesium cations, which agrees with the data reported in studies [13,32].
Figure 12.
Variation of the parameters a and c (a), and unit cell volume (b) of the HA phase in the samples with different concentrations of the introduced magnesium after annealing at 900 °С.
Figure 12.
Variation of the parameters a and c (a), and unit cell volume (b) of the HA phase in the samples with different concentrations of the introduced magnesium after annealing at 900 °С.
Taking into account that the decomposition of Mg-HA proceeds in two stages with the formation of MgO in the first stage and the substituted β-TCP and MgO in the second stage, the decomposition of Mg-HA can be described by Reactions (6)–(7):
where y ≤ 0.5
At the first stage of the decomposition proceeding by Reaction (6), Mg-HA, which contains a small concentration of cationic vacancies and magnesium oxide, is formed. At the second stage of the decomposition proceeding by Reaction (7) at a slightly higher temperature, the number of hydroxyl groups in the apatite structure decreases to less than 1, so the crystal lattice of the substituted apatite becomes unstable and decomposes into the substituted β-TCP and MgO. Magnesium substitution for calcium cations in the structure of β-TCP was also reported in studies [
21,
23,
32].
The significant difference between ionic radii of calcium and magnesium may be the reason for the decomposition of Mg-HA. In this case, the magnesium cations, which partially occupy the calcium positions, are located at a much larger distance from their nearest neighboring oxygen anions than the calcium cations in the same position. The thermal expansion of the crystal lattice upon heating resulting in a further increase in the ion-ion distances lead to the destruction of the ionic crystal at the sites of localization of the magnesium cations followed by the formation of β-TCP and MgO phases. It is noteworthy that, for all concentrations of the introduced magnesium, the behavior of the crystallite size of the substituted apatite phase after cooling and unsubstituted HA (
Figure 7), which does not undergo any structural transformations in this temperature range, have the same dynamic. Even at x = 2, when the Mg-HA structure is almost completely decomposed (only 6 % HA remains), the changes in the crystallite sizes have the same dynamics. Consequently, the Mg-HA structure decomposes upon heating.
Figure 11.
Evolution of the apatite crystallite size with temperature upon heating Mg-HA containing different magnesium concentrations.
Figure 11.
Evolution of the apatite crystallite size with temperature upon heating Mg-HA containing different magnesium concentrations.