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Article

Characterization, Kinetic Using Deconvolution Techniques and Thermodynamic Study of Synthetic MgHPO4·3H2O

by
Saifon Kullyakool
1,2,
Somphob Thompho
3,
Banjong Boonchom
1,2,* and
Pesak Rungrojchaipon
1
1
Material Science for Environmental Sustainability Research Unit, Department of Chemistry, School of Science, King Mongkut’s Institute of Technology Ladkrabang, Bangkok 10520, Thailand
2
Municipal Waste and Wastewater Management Learning Center, School of Science, King Mongkut’s Institute of Technology Ladkrabang, Bangkok 10520, Thailand
3
Pharmaceutical Research Instrument Center, Faculty of Pharmaceutical Sciences, Chulalongkorn University, Pathumwan, Bangkok 10330, Thailand
*
Author to whom correspondence should be addressed.
Crystals 2023, 13(4), 567; https://doi.org/10.3390/cryst13040567
Submission received: 2 March 2023 / Revised: 19 March 2023 / Accepted: 22 March 2023 / Published: 27 March 2023
(This article belongs to the Special Issue Recent Developments of Inorganic Crystalline Materials)

Abstract

:
MgHPO4·3H2O was synthesized via a simple wet reaction and transformed to its final decomposed product, Mg2P2O7 at 873 K. The thermal properties, vibrational modes of block units, and solid phases of the synthetic compounds have been investigated by TG/DTG/DTA, FTIR, and XRD techniques. The temperature dependence of thermodynamic properties estimated from the DSC data occurred in two regions (before and after the dehydration reaction) indicating a characteristic of the prepared MgHPO4·3H2O sample. The dehydration reactions of 3.5 mol of water molecules in the structure overlapped in the temperature of 363–823 K and showed the phase transition at 921 K as revealed by TG/DTG/DTA. The deconvolution technique using the newly modified co-mathematical functions was used to separate the overlapped dehydration steps in the DTG curve, which obtained the three steps. Only the first and second steps were estimated using kinetic triplet parameters (Ea, A, and model), which indicate the single dehydration mechanism with the A1.25 model and the multi-step of a parallel mechanism with the A1.6 model, respectively. The data of kinetics and thermodynamics play key points in theoretical study, application development, and industrial production of magnesium phosphates as a theoretical basis.

Graphical Abstract

1. Introduction

The magnesium phosphate compounds are always stable in various hydrated forms such as struvite (MgNH4PO6H2O) [1], newberyite (MgHPO43·H2O) [2], bobierite (Mg3(PO4)2·8H2O) [3], and hannayite (Mg3(NH4)2H4(PO4)4·8H2O) [4] and they can be obtained from mineral resources or produced by humans [5]. Under the heat treatment, these magnesium phosphate hydrates can change into magnesium phosphate anhydrous compounds (Mg3(PO4)2), magnesium cyclophosphate (Mg2P4O12), and magnesium pyrophosphate (Mg2P2O7) [6,7,8,9,10,11]. The magnesium phosphate anhydrous compounds are attractively used as heterogeneous catalysts for many organic syntheses [12,13,14], anti-corrosive ceramic pigments [15], and as fillers for bioactive materials [16] because they are temperature-resistant, structurally and chemically stable, and insoluble in water [17]. Aramendía et al. reported that the mix-phase of Mg3(PO4)2 and Mg2P2O7 consisting of acidic and basic site plays a role as a catalyst in the dehydration-dehydrogenation reaction of 2-hexane [13]. In 1999, the catalytic activity of Mg2P2O7, Mg3(PO4)2, and NaMg4(PO4)3 in the gas-phase conversion of 2-hexanol was reported by Aramendía et al. [18]. Sadiq et al. reported the catalytic activity of pure Mg3(PO4)2 and Mg3(PO4)2 modified by Co-Mo, in 3,3-dimethylbut-1-ene isomerization reaction as a gas/solid interface reaction [19]. The results showed that Mg3(PO4)2 has high catalytic activity in skeleton isomerization due to strong acid sites of Lewis and Brônsted acid centers [19]. In 2015, Sadiq et al. studied the catalytic activity of Mg3(PO4)2 and Mg2P2O7 in the skeletal isomerization of 3,3-dimethylbut-1-ene and the result exhibits the Mg2P2O7 catalyst, which has high number of active acid sites and is more active than Mg3(PO4)2 catalyst [14]. Moreover, Mg2P2O7 is an alternative non-toxic and color stable ceramic over high temperature [15]. Newberyite, a constituent of human and animal calculi, has been used as additive in bioactive material [5]. Sugiyama et al. reported the use of MgHPO4 to remove aqueous ammonium from wastewater [20]. Mohammad et al. prepared MgHPO4 bound by ethyl cellulose that can be used in the sensory, pharmaceutical, and biomedical sectors [21]. Based on the above-mentioned reports, newberyite and Mg2P2O7 are particularly interesting and are the joint focus of this study.
Newberyite belongs to the orthorhombic space group Pbca with eight molecules in a unit cell [2,7]. The MgHPO4·3H2O structure has a strong hydrogen bond of the pair of HPO 4 2 molecules resulting in the complex vibrational bands of PO 4 3 ground [2,7]. Its final decomposition product, Mg2P2O7, belongs to the monoclinic system in P21/n space group [2,7]. Aramendía et al. have synthesized magnesium phosphate by varying the reactant sources (Mg and P) and mole ratios of Mg to P [13]. The study found that the different sources and the ratios of Mg to P resulted in different stoichiometric compounds. Mesíková et al. synthesized MgHPO4·3H2O in an ice bath from a suspension of magnesium hydroxide and a solution of phosphoric acid within a short period time (1 h) [2]. The pH effect on the synthesized product was studied and the results showed that when increasing the pH value, the growth of particle size distribution also increased, while the specific surface area decreased [2]. Boonchom studied the decomposition kinetics of the commercial MgHPO4·3H2O and found that the decomposition occurred in one step as a single dehydration process with F1/3 model controlling mechanism [7]. Based on previous study results, the different synthetic routes for obtaining one material showed that differences in thermal behavior and other properties [16,17] might be affected to apply in a specific field, e.g., catalytic.
In this work, MgHPO4·3H2O was synthesized using a simple wet chemical reaction at ambient temperature. The thermal decomposition from MgHPO4·3H2O into Mg2P2O7 was analyzed. The deconvolution technique using co-mathematical functions was used to separate the covering decomposition step. The activation energy and pre-exponential factor were determined using the modified iterative from Kissinger, Akahira and Sonose (KAS) equations [22,23]. The mechanism function of the decomposition was confirmed by three methods; (1) the roughly observed g(α) by plotting of dα/dT versus α and the g(α) was identified by curve shape, (2) the exhaustive g(α) was evaluated using the modified master plots combined with the non-linear curve fitting, (3) checking of the correction of the g(α) evaluated from (2) by using the basic master plotting equation [24,25]. Additionally, the temperature dependence of the standard thermodynamic functions (the change in entropy, enthalpy, and Gibbs free energy) was evaluated from DSC results using the cubic polynomial curve fitting [26,27]. Studies on the thermodynamics, mechanisms and kinetics of thermally-decomposed reactions are challenging, with sophistication affecting the large diversity of factors, with diverse effects such as the rebuilding of solid state crystal lattices, setting-up and growth of new crystallization nuclei, diffusion of gaseous agents or reaction products, materials heat conductance, the static or dynamic feature of the environment, the physical state of the reagents, that is, dispersity, layer thickness, specific surface area and porosity, the kind, quantity, and distribution of the active centers on solid state surface, etc. [28,29,30,31,32]. The results obtained from such studies can be straightforward and practical in materials science for both academics and industrialists who are interested in the preparation of various metals and alloys, cement, ceramics, glasses, enamels, glazes, catalysts, and polymer and composite materials [31,33]. The key factor in obtaining MgHPO4·3H2O and Mg2P2O7 with different properties has been used in different preparative methods, which could play a large role in industrial applications [31,32].

2. Materials and Methods

2.1. Synthesis and Characterization

MgHPO4·3H2O powder was synthesized by a simple wet chemical reaction. A MgCl2·6H2O solid sample was dissolved in 85% w/w H3PO4 in the ratio of Mg:P at 1:1 and then controlled at 313 K for 2 h. After that, the resulting solution was adjusted to pH 6 by 1.0 M NaOH, and a precipitate then appeared. The white powder was isolated by filtration, then washed with deionized water and dried in open air. The synthesized hydrate was calcined at 500 and 973 K. The synthesized hydrate and the thermal treatment products were characterized using Fourier-transform infrared spectroscopy (FTIR, Perkin Elmer Spectrum GX; UK) in the wavenumber range of 4000–370 cm−1 by KBr pellet technique (spectroscopy grade of KBr, Merck; Germany), thermogravimetry, derivative thermogravimetry, and differential thermal analysis (TG/DTGDTA, Perkin Elmer Pyris Diamond; Waltham, MA, USA), and X-ray powder diffraction (XRD, Phillips 3710; UK) technique with CuKα radiation (λ = 1.5406 nm) over the 2θ range of 5° < 2θ < 70°.

2.2. The Temperature Dependence of the Thermodynamic Functions

Heat capacity (Cp) of MgHPO4·3H2O and Mg2P2O4 were determined using DSC (Perkin-Elmer Pyris1) technique measuring within the temperature range from 323 to 823 K at heating rate of 10 K min−1 under N2 atmosphere with sample mass of 4.5 mg (accurate). The isobaric molar heat capacity, Cp(T), derived from the ratio of the actual DSC heat flow (ΔP/mW) and applied heating rate (β/K min−1) is expressed as the equation [34].
C p T = 1 m dH dT = 1 m dH / dt dT / dt = 1 m P β
where, m is the sample mass (g). The temperature dependence of Cp(T) can be evaluated from non-linear regression using cubic polynomial curve fitting. Moreover, the temperature dependence of standard thermodynamic functions such as entropy, enthalpy and Gibbs free energy can be estimated from Cp(T) with the following Equations (1)–(3) [16].
S ° = S T ° S 298.15 ° = 298.15 T C p T T dT + H t T t + T t T m C p T T dT + H m T m + T m T T C p T T dT
H ° = H T ° H 298.15 ° = 298.15 T t C p T dT + H t + T t T m C p T dT + H m + T m T T C p T dT
G ° = G T ° G 298.15 ° = H T ° H 298.15 ° T S T ° S 298.15 °

2.3. Kinetic Study of Thermal Transformation

The kinetic study of MgHPO4·H2O was carried out by TG/DTG/DTA at four heating rates (10, 15, 20, and 25 K min−1) over the temperature range of 303–1073 K. The mathematical deconvolution method was used to separate the covered DTG peaks and then the kinetic parameters in each step were determined [25].
Mathematical Deconvolution. The mathematical deconvolution technique as a popular technique was used to separate the covering peaks [24,25]. The numerous mathematical functions were used to separate the unclearly divided peaks as shown below.
  • Gaussian Function: Ref. [25] There Are Many Versions of Gaussian Functions:
Normal Gaussian peak function
y = 1 σ 2 π exp x x c 2 2 σ 2
Amplitude version of Gaussian peak function
y = A   exp x x c 2 2 σ 2
A = a 2 σ π 2
Bi-Gausssian peak function
y = H   exp   x x c 2 2 σ 1 2 ,   ( x < x c )
y = H   exp   x x c 2 2 σ 2 2 ,   x x c
H = a σ 2 π
Constrained Gaussian peak function
y = A σ 1 + σ 2 x c 2 π exp x x c 2 2 σ 1 + σ 2 2
2.
Amplitude Version of Weibull Peak Function
y = A σ 2 1 σ 2 1 σ 2 σ 2 S σ 2 1 exp S σ 2 + σ 2 1 σ 2
S = x x c σ 1 + σ 2 1 σ 2 1 / σ 2
A = a σ 1 σ 2 π 2
3.
Fraser-Suzuki Peak Function
y = H exp ln 2 S ln 1 + 2 S   x x c 2 2 σ 2
where the peak parameters such as σ, A, H, xc, and S are standard deviation, amplitude, peak high, center, and asymmetric parameters (dimensionless), respectively.
The Gaussian and Fraser-Suzuki functions are the most popular ones to use to separate the covering peak [24,25,35]. In this work, the co-mathematical functions combining the deconvolution technique were performed. Equations (4)–(14) were tested to separate the covering DTG curve and the suitable functions were selected by minimizing the residual sum of square (RSS) and R2 close to 1.000.
Kinetic parameters determination. The activation energy (E) and pre-exponential factor (A) were determined after deconvolution treatment. The E and A values were evaluated using the iterative modified KAS method as the following equation [22,23].
ln β T 2 = ln A R g α E E R T
Equation (15) was modified to be
ln β h x T 2 = ln A R g α E E R T
where x = E/RT and h(x) is expressed by the 4th-order of Senum-Yang approximation formula as following the equation [36].
h x = x 4 + 18 x 3 + 86 x 2 + 96 x x 4 + 20 x 3 + 120 x 2 + 240 x + 120
The iterative procedure can be performed by following steps:
(i)
Assume h(x) = 1 to estimate the initial value of E1. The isoconversional methods stop the calculation at this step.
(ii)
Using E1, calculate a new value of E2 from the plot of ln [β/h(x)T2] versus 1000/T.
(iii)
Repeat step (ii), replacing E1 with E2. When Ei − Ei−1 < 0.1 kJ mol−1, the last value of Ei was considered to be the exact value of the activation energy of the reaction.
The pre-exponential factor A was calculated using Equation (15) by substituted g(α).
Moreover, the Kissinger equation was used to calculate the kinetic parameters, E and A of the fourth step.
ln β T p 2 = ln A R E E R T p
According to Equation (18), plotting of ln(β/Tp2) versus 1000/Tp in four heating rates then the E and A can be calculated from slope and y-intercept, respectively.
Mechanism function determination. The mechanism function of the dehydration step in this work was determined using the non-linear method accepted from ICTAC Kinetics Committee recommendations in 2011 appropriating for evaluation of the kinetic parameters whether that of single-step or multi-step reaction [37,38].
From the rate equation
d α d T = A β e E α / R T f α
where f(α) is the differential form of the mechanism function. Integrating Equation (19) yields the integral form of the mechanism function g(α) as following the equation:
g α = 0 1 f d α = A E α β R p x
where,
p x = x e x x 2 d x
p x = e x x 2 h x
From Equation (19), referring to α = 0.5, the master plots equation is obtained as follows:
g α g 0.5 = p x p x 0.5
Y e x p = p x p x 0.5
Y T h e o r y = g α g 0.5
The theoretical plots of g(x)/g(0.5) can be obtained for the different kinetic mechanism functions at the reported 35 functions [24,25,35]. Based on Equation (24), the plots of p(x)/p(x0.5) versus α are the experimental plots [39]. In this work, the modified master plots combined with the non-linear curve fitting method are used to evaluate the correct g(α) and the general equation as following the equations:
F   models :   g α = 1 n 1 1 α 1 n 1
R   models : g α = 1 1 α 1 / n
P   models :   g α = α 1 / n
A   models :   g α = ln 1 α 1 / n
From the Equations (8) and (10)–(12), the nonlinear master plots curve fitting equations can be expressed following the equations.
F   models : g α g 0.5 = 1 α 1 n 1 0.5 1 n 1
R   model :   g α g 0.5 = 1 1 α 1 / n 1 0.5 1 / n
P   models :   g α g 0.5 = α 1 / n 0.5 1 / n
A   models : g α g 0.5 = ln 1 α 1 / n ln 0.5 1 / n
Equations (29)–(32) are tested by the fitting of the n-order according to 35 (Table S1) reported functions and the results show that the R2 is equal to 1.000. The mechanism functions evaluated from the modified master plots combined with the non-linear curve fitting method were double-checked using Equation (20) by comparing the g(α) from the experimental and that of theoretical (Table S1) by minimization of the residual sum of square (RSS) [25,38].
R S S = g α e x p g α T h e o 2

3. Results and Discussion

3.1. Characterization

The synthesized hydrate and the calcined products at 723 and 923 K (4 h in air atmosphere) were characterized by TG/DTG/DTA, FTIR, XRD, and DSC techniques.
TG/DTG/DTA results. The TG/DTG/DTA curves are shown in Figure 1. The loss weight exhibited in the TG curve in the range of 363–823 K was found to be 35.79%, which is equal to 3 molecules of water of crystallization and 0.5 molecules of water of constituent. The corresponding peak observed at 435 K in DTG and DTA curves was related to the endothermic reaction. This confirms that the dehydration reactions of 3.5 molecules of water in the structure have overlapped. Moreover, there was an exothermic DTA peak at 921 K attributing that to be due to the phase transition from lower to higher crystallinities as confirmed by the FTIR (Figure 2) and XRD (Figure 3) results, and the thermal transformation reaction of MgHPO4·3H2O is shown in the Equation (35). The thermal behavior of the synthesized MgHPO4·3H2O compound in this work differed from that of the commercial MgHPO4·3H2O compound reported in previous work [7].
MgHPO 4 3 H 2 O   ( s ) 363 573   K MgHPO 4   s + 3 H 2 O   ( g )   573 823   K   1 2 Mg 2 P 2 O 7 s ;   low   crystallinity + 1 2 H 2 O   g   921   K   1 2 Mg 2 P 2 O 7 s ; high   crystallinity
FTIR result. The FTIR spectra of the synthesized hydrate and the calcined products at 773 and 973 K are illustrated in Figure 2. The spectrum of the hydrate (Figure 2a) exhibits the vibrational bands of water at around 3500–3200 cm−1, 1700–1600 cm−1, and 700 cm−1. The vibrational bands of HPO 4 2 are demonstrated to be the complex character such as A-B-C trio bands of the two forming components due to the stretching of the strongly H-bonded hydrogenphosphate [2,4,7]. Normally, the B band (2900 cm−1) is stronger than A and C bands (2400 cm−1), while the C band is covered up by the vibrational (banding) band of water appearing at around 1600 cm−1. In the case of the calcined products at 773 and 973 K (Figure 2b,c), the spectra are quite similar, which do not appear in the vibrational bands of water and exhibit the vibration frequencies at low regions indicating the character of [P2O7]4− anion. The fundamental vibrational modes of [P2O7]4− anion containing the P-O stretching, symmetric PO2 stretching (νsym, PO2), asymmetric PO2 stretching (νasym, PO2), symmetric (νsym, POP), asymmetric stretch (νasym, POP) bridge, and PO3 deformation and rocking modes, the POP deformations and the torsional and external modes are known to appear in the ranges of 1150–960, 954, 1082, 649, 737, 580–420 cm−1, respectively [15,18].
XRD result. The XRD patterns of the hydrate, the calcined product at 773 and 973 K (4 h in air atmosphere) are shown in Figure 3 and the results show that the hydrate and the calcined products (773 and 973 K) are MgHPO4·3H2O and Mg2P2O7, respectively. The XRD pattern of the calcined product at 773 K observed low intense peaks points to the character of amorphous phase or low crystallinity of Mg2P2O7. The pattern of the hydrate (Figure 3a) agrees with the standard PDF #72-0023 (MgHPO4·3H2O) crystallizing in the orthorhombic system with space group Pbca. The patterns of calcined product at 973 K (Figure 3c) °C agrees with the PDF #32-0626 crystallizes in the monoclinic system with space group P21/n [2,5,7,13]. These results agree well with the results from TG/DTG/DTA and FTIR. The final decomposition product, Mg2P2O7 completely occurs after the temperature of 921 K as an exothermic temperature attributed to being due to phase transition from lower to higher crystallinity [13].

3.2. The Temperature Dependence of the Thermodynamic Functions

The result from the measurement of DSC carrying out over the temperature range of 323–823 K at a heating rate of 10 K min−1 under N2 atmosphere exhibits three endothermic peaks of the transitions as shown in Figure 4. The transition temperatures on the DSC curve appearing at a higher temperature than that on TG/DTG/DTA curves may be due to the high sensitivity of DSC technique [26,27]. However, the results from DSC and TG/DTG/DTA techniques agree with each other. Figure 4a illustrates the Cp(T) curve divided into two regions consisting of; region I (323–383 K) and region II (518–583 K), a region after dehydration. It can be seen that the Cp(T) equations of both regions show the fine cubic polynomial relationships with temperature from 323 to 383 and 518 to 583 K, which confirm the correlation coefficient of fitting R2 as 0.9995 and 0.998, respectively. Although the observed temperature is from 323 to 383 and 518 to 583 K, the equations of Cp(T) are stable and continuous, which can serve as a guide for the application of the studied compound in the temperature. The entropy ΔS°(T), enthalpy ΔH°(T), and Gibbs free energy ΔG°(T) changes from two temperature ranges (323–383 and 518–583 K) taking 298.15 as the benchmark temperature were calculated by Equations (1)–(3). The results are shown in Equations (36)–(43).
Region I; T1 = 323–383 K
C p T 1 = 133.39 1.28 T + 4.20 × 10 3 T 2 4.50 × 10 6 T 3   k J   K 1 m o l 1 ; R 2 = 0.9995
S ° T 1 = 519.94 + 133.39 ln T 1.28 T + 2.10 × 10 3 T 2 1.50 × 10 6 T 3   k J   K 1 m o l 1
H ° T 1 = 33270 + 133.39 T 1.14 T 2 + 1.40 × 10 3 T 3 1.12 × 10 6 T 4     k J   m o l 1
G ° T 1 = 33270 + 653.33 T 133.39 T ln T + 0.14 T 2 7.00 × 10 4 T 3 + 3.80 × 10 7 T 4     k J   m o l 1
Region II; T2 = 518–583 K
C p T 2 = 72.16 + 0.3511 T 2.46 × 10 4 T 2 + 2.37 × 10 7 T 3   k J   K 1 m o l 1 ;   R 2 = 0.9998
S ° T 2 = 315.56 72.16 ln T + 0.3511 T 1.23 × 10 4 T 2 + 7.90 × 10 8 T 3     k J   K 1 m o l 1
H ° T 2 = 7728.85 72.16 T + 0.1756 T 2 8.2 × 10 5 T 3 + 5.92 × 10 8 T 4   k J   m o l 1
G ° T 2 = 7728.85 387.72 T + 72.16 T ln T 0.1755 T 2 + 4.10 × 10 5 T 3 1.98 × 10 8 T 4     k J   m o l 1
The dependence of thermodynamic properties on temperatures is shown in Equations (36)–(43), which are characteristic of the prepared MgHPO4·3H2O samples, which occurred in two regions: the first (I) region is before the dehydration (hydrate being transformed) reaction and the second (II) region is after the dehydration (occurred anhydrous form) process. However, Equations (41)–(43) used for estimation will give slightly inaccurate due to the covered peaks of the DSC curve resulting in the unrealistic ΔH and Tp (peak temperature). When calculated in the individual temperature ranges, the values of ΔS°(T), ΔH°(T), and ΔG°(T) increase with the rise in temperature. The calculated results showed that the equations of the entropy and Gibbs free energy changes exhibit logarithmic temperature dependence, while the enthalpy change has a non-linear relationship with temperature. These results can give valuable information for both theory and applications of magnesium phosphate materials, which are used to consider its phase transformation affecting the catalytic application.

3.3. Kinetic Study

The kinetic study of MgHPO4·H2O was carried out by measuring TG/DTG/DTA at four heating rates (10, 15, 20, and 25 K min−1). The three steps of the dehydration reactions are not clearly separated difficult to determine the kinetic parameter. Therefore, the mathematical deconvolution method was used to separate into the DTG peaks to further determine the kinetic parameters in each step.
Mathematical Deconvolution. The DTG curve was separated to three steps by co-functions of the deconvolution method by using Equations (4)–(14) and the suitable functions consist of Bi-Gaussian, Amplitude version of Gaussian, and Fraser-Suzuki peak functions for the first (I), second (II), and third (III) steps, respectively [24,25,29,39]. The deconvolution of DTG curves and the dα/dT vs. T curves of the I and II steps of four heating rates are shown in Figure 5 with the minimizing of RSS and R2 close to 1.000, which is a factor used to confirm the realistic of the deconvolution method. For the third step, the deconvolution method is not applied because the reason for the realistic is caused. The comparison between the simulated TG curves and the experimental TG curves of four heating rates exhibited in Figure 6 shows no significant difference.
Activation energy determination. After the three covering steps were separated, the percentages of weight loss of each step were simulated by integrating the deconvolution treated curves (Figure 5 and Figure 6). The modified iterative from KAS equation was used to determine the activation energy as shown in Table 1. The % relative error values of the first step, which are less than 10%, illustrate the independence of activation energies on the conversion fractions, α, and confirm that the dehydration step is the single step mechanism. The second step consists of more than 10% of the relative error values contributed to the multi-step mechanism of the decomposition presumed due to the parallel of the two mechanisms [22,23,37]. The third step shows the widely distributing activation energy values contributed that the mechanism consists of many processes such as the physical and chemical processes of the changes, therefore the realistic of the kinetic parameters are difficult to determine. This result is consistent with the deconvolution method for the third step. The average activation energies for the three steps obtained in this work are different from those of the single step reported in previous work found to be about 100 kJ/mol−1 calculated by Ozawa, KAS, and iterative methods [7]. The obtained Ea values of the first separated peak are higher than that for the second separated peak, which could be due to a stronger H-bond in first water molecules than that of the H-bond in second water molecules. In order to break the H-bond, the dehydration process of the starting compound (MgHPO4·3H3O) requires higher Ea values than that of the dehydration process of MgHPO4·nH3O (0 < n < 2) supporting the stability of the hydrate formula form.
The Mechanism Function Evaluation. The g(α) can be roughly observed by plotting of dα/dT versus α illustrated in Figure 7. The shapes of dα/dT versus α curve of the first and the second steps are the same as the shapes of the A or R models and the A or F models, respectively. The correct g(α) models were evaluated by the master plots combined with the non-linear curve fitting (Equations (29)–(32)). Figure 8 illustrates the master plots fitted non-linear curves of the first and the second steps and the most probable mechanism functions are according to A1.25 for the first step and A1.61 for the second step. The most probable mechanism functions are according to A1.25 for the first step and A1.61 for the second step, that is the dehydrations of both steps are controlled by the random nucleation and consequent growth, A models with the different n-order. The correction of the mechanism functions fitted from the modified master plots method is double-checked using Equation (19). The g(α) evaluated from the experiment is compared with the theoretical by minimizing the RSS (Equation (33)) and the results are shown in Figure 9 and Figure 10. The results evaluated from Equation (19) agree well with the results fitting from the modified master plots method. The obtained results are shown more credible in the kinetics. Both function models obtained indicate a similar mechanism of sigmoid rate equations or random nucleation and subsequent growth. The models obtained in this work are different from one step as a single dehydration process with the F1/3 model controlling mechanism estimated by the Coats–Redfern method reported previously [7], which indicates that the different synthetic routes showed different thermal behavior and kinetic parameters [16,17].

4. Conclusions

MgHPO4·3H2O was successfully synthesized by the simple precipitation for a short time (2 h) and thermally decomposed into a single dehydration process resulting from three overlapped steps in the range of 373–823 K. The final product showed thermal stability at above 773 K and the excellent crystallinity was recorded at about 921 K obtained from the complete exothermic DTA peak. The prepared sample and their final products obtained from heating at 773 and 973 K were analyzed by FTIR and XRD techniques. The temperature dependence of the standard ΔS°(T), ΔH°(T), and ΔG°(T) determined using the cubic polynomial curve fitting was found that ΔH°(T) exhibits non-linear dependence of temperature, while ΔS°(T) and ΔG°(T) are logarithmic dependence of temperature, created from DSC data. The three steps of the dehydration process showed the overlapped peak in the DTG curve and the deconvolution technique using co-mathematical functions was used to separate individual peaks. The iterative modified KAS equation was used to calculate the E values independence on the conversion fraction with r2 (the correlation coefficient of linear regression) and the % relative error, which offer to discuss the physical meaning of kinetics. The first step shows the % relative errors are less than 10% indicating from the E dependent with the conversion fraction, while the second step is opposite and the third step is hard to explain on kinetics because of very low r2 values. Consequently, mechanisms of the first, second, and third steps are the single dehydration process, the multi-step, and the parallel of the physical and chemical processes, respectively. The g(α) models of the first and the second dehydration steps were determined by three methods (the roughly observed g(α) by the plotting of dα/dT versus α, the exhaustive g(α) evaluated using the modified master plots combined with the non-linear curve fitting and then the corrective g(α) checked using the basic master plot equation), which obtained the results with good consistency. The random nucleation and consequent growth, A models with the different n-order, are the mechanism controlling the dehydration process of the first (A1.25) and the second (A1.61) steps. The results of the thermodynamics and kinetics of thermal decomposition of MgHPO4·3H2O for the synthesized Mg2P2O7 are mandatory for researchers (academic scientists and industrialists) to refine the technology and make magnesium phosphate, which may be useful for potential applications as enamels, glazes, catalysts, etc.

Supplementary Materials

The following supporting information can be downloaded at: https://www.mdpi.com/article/10.3390/cryst13040567/s1, Table S1: Mathematical expressions for nucleation rates law [40]. Table S2. Algebraic expressions of kinetic functions and its corresponding mechanism [37]. Figure S1. One-dimensional diffusion through a flat plane [40]. Figure S2. Schematic representation of a spherical reaction [40].

Author Contributions

S.K.: investigation, experiment, data curation, writing—original draft, review and editing. S.T.: data curation, writing—review and editing. B.B.: conceptualization, investigation, writing—review and editing, supervision. P.R.: conceptualization, data curation, writing—review and editing. All authors have read and agreed to the published version of the manuscript.

Funding

King Mongkut’s Institute of Technology Ladkrabang, [KREF145907].

Data Availability Statement

All data that support the findings of this study are available from the corresponding author upon reasonable request.

Acknowledgments

We thank the Department of Chemistry, Faculty of Science, Khon Kaen University for providing research facilities. The financial support from the Advance Phosphate Material and Alternative Fuel Energy Research Unit, Department of Chemistry, Faculty of Science, King Mongkut’s Institute of Technology Ladkrabang, [KREF145907], is gratefully acknowledged. The authors would like to thanks the Scientific Instruments Center KMITL for supporting TGA, FTIR, XRD, and SEM techniques.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. TG/DTG/DTA curves of MgHPO4·3H2O at over the temperature range of 303–1073 K at a heating rate of 10 K min−1 under N2 atmosphere.
Figure 1. TG/DTG/DTA curves of MgHPO4·3H2O at over the temperature range of 303–1073 K at a heating rate of 10 K min−1 under N2 atmosphere.
Crystals 13 00567 g001
Figure 2. FTIR spectra: (a) the synthesized hydrate, (b) the calcined products at 773 K, and (c) the calcined products at 973 K.
Figure 2. FTIR spectra: (a) the synthesized hydrate, (b) the calcined products at 773 K, and (c) the calcined products at 973 K.
Crystals 13 00567 g002
Figure 3. XRD patterns: (a) MgHPO4·3H2O, (b) the calcined products at 773 K, and (c) the calcined products at 973 K (4 h in air atmosphere).
Figure 3. XRD patterns: (a) MgHPO4·3H2O, (b) the calcined products at 773 K, and (c) the calcined products at 973 K (4 h in air atmosphere).
Crystals 13 00567 g003
Figure 4. DSC result: (a) heat capacity curve of MgHPO4·3H2O and (b) heat flow curve.
Figure 4. DSC result: (a) heat capacity curve of MgHPO4·3H2O and (b) heat flow curve.
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Figure 5. Four deconvoluted DTG peaks were observed from overlapped DTG peaks from modified co-mathematical functions for the experimentally observed DTG curve of the studied thermal solid-state reaction.
Figure 5. Four deconvoluted DTG peaks were observed from overlapped DTG peaks from modified co-mathematical functions for the experimentally observed DTG curve of the studied thermal solid-state reaction.
Crystals 13 00567 g005
Figure 6. The comparison between the weight loss from experimental and simulated by deconvolution curves fitting method at four heating rates.
Figure 6. The comparison between the weight loss from experimental and simulated by deconvolution curves fitting method at four heating rates.
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Figure 7. The dα/dT versus α curves of (a) the first and (b) the second steps.
Figure 7. The dα/dT versus α curves of (a) the first and (b) the second steps.
Crystals 13 00567 g007
Figure 8. The fitted non-linear curves of (a) the first and (b) the second steps from the master plots combined with the non-linear curve fitting method. Comparative results between the experimental and model plots for (a) the first and (b) the second individual peaks obtained from Y(α) plots of the studied thermal solid-state reaction.
Figure 8. The fitted non-linear curves of (a) the first and (b) the second steps from the master plots combined with the non-linear curve fitting method. Comparative results between the experimental and model plots for (a) the first and (b) the second individual peaks obtained from Y(α) plots of the studied thermal solid-state reaction.
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Figure 9. The experimental and the theoretical plots (a,b) of the explored g(α) versus α curves using the reaction models for the first step.
Figure 9. The experimental and the theoretical plots (a,b) of the explored g(α) versus α curves using the reaction models for the first step.
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Figure 10. The experimental and the theoretical plots (a,b) of the explored g(α) versus α curves using the reaction models for the second step.
Figure 10. The experimental and the theoretical plots (a,b) of the explored g(α) versus α curves using the reaction models for the second step.
Crystals 13 00567 g010
Table 1. The calculated E, A, and % relative error of the three dehydration steps from the iterative modified KAS equation.
Table 1. The calculated E, A, and % relative error of the three dehydration steps from the iterative modified KAS equation.
αStep IStep IIStep III
E/kJ mol−1%ErrorR2A/s−1E/kJ mol−1%ErrorR2A/s−1E/kJ mol−1%ErrorR2A/s−1
0.10106.840.620.99478.18 × 101380.987.770.98194.97 × 101053.3538.190.4372-
0.12105.880.490.99665.25 × 101381.078.750.97724.16 × 101051.9038.550.4307-
0.14104.980.380.99803.51 × 101380.999.540.97303.38 × 101052.2737.110.4570-
0.16104.320.280.99892.56 × 101380.8410.210.96912.73 × 101051.7137.290.4537-
0.18103.880.180.99962.02 × 101380.6510.780.96552.22 × 101051.1937.480.4502-
0.20103.080.090.99991.44 × 101380.4511.260.96231.81 × 101051.0836.800.4628-
0.22102.340.070.99991.06 × 101380.2311.680.95931.49 × 101050.8836.980.4595-
0.24101.720.130.99988.11 × 101280.0112.050.95661.23 × 101050.6837.180.4558-
0.26101.020.220.99936.10 × 101279.7912.380.95411.03 × 101050.4837.400.4517-
0.28100.400.290.99884.72 × 101279.5712.670.95178.62 × 10950.1737.130.4568-
0.3099.760.360.99823.64 × 101279.3412.940.94957.25 × 10950.0837.360.4524-
0.3299.020.430.99752.74 × 101279.1213.190.94736.13 × 10949.9837.620.4477-
0.3498.440.500.99652.17 × 101278.9113.440.94525.23 × 10949.8937.890.4427-
0.3697.790.560.99561.68 × 101278.6913.650.94334.47 × 10949.6137.940.4419-
0.3897.120.620.99461.30 × 101278.4813.850.94143.83 × 10949.4938.160.4377-
0.4096.470.680.99351.02 × 101278.2514.030.93963.27 × 10949.3738.410.4333-
0.4295.810.750.99237.92 × 101178.0314.210.93782.81 × 10949.2538.670.4286-
0.4495.140.800.99116.16 × 101177.8014.380.93602.41 × 10949.1438.940.4238-
0.4694.480.860.98994.82 × 101177.5514.540.93432.06 × 10949.0339.220.4187-
0.4893.820.910.98863.78 × 101177.3014.690.93271.76 × 10948.9239.510.4135-
0.5093.120.960.98722.94 × 101177.0414.830.93101.51 × 10948.8239.820.4081-
0.5292.431.020.98582.28 × 101176.7714.970.92941.28 × 10948.7240.140.4026-
0.5491.731.070.98441.78 × 101176.4815.090.92771.09 × 10948.6240.460.3969-
0.5691.021.120.98301.38 × 101176.1815.220.92619.19 × 10848.5340.800.3911-
0.5890.301.170.98151.07 × 101175.8615.340.92447.73 × 10848.4441.140.3852-
0.6089.571.210.98008.24 × 101075.5115.430.92296.46 × 10848.3541.500.3791-
0.6288.821.260.97846.34 × 101075.1415.540.92125.36 × 10848.2641.850.3731-
0.6488.051.300.97694.86 × 101074.7415.630.91964.41 × 10848.1742.240.3666-
0.6687.251.350.97533.69 × 101074.3215.720.91793.60 × 10848.1042.610.3605-
0.6886.411.390.97372.77 × 101073.8715.790.91622.92 × 10848.0243.010.3539-
0.7085.511.440.97212.04 × 101073.3715.880.91432.33 × 10847.9543.430.3471-
0.7284.531.480.97051.47 × 101072.8215.960.91231.83 × 10847.9043.830.3407-
0.7483.491.520.96881.04 × 101072.1716.020.91031.40 × 10846.9544.770.3257-
0.7682.371.560.96707.21 × 10971.5416.050.90851.07 × 10845.3046.350.3016-
0.7881.171.610.96534.87 × 10970.8616.070.90678.06 × 10745.7744.630.3280-
0.8079.891.650.96333.22 × 10970.0916.100.90455.91 × 10747.4144.900.3238-
0.8278.561.710.96112.09 × 10969.1416.150.90164.10 × 10749.0945.180.3194-
0.8477.211.770.95831.35 × 10968.1316.170.89882.80 × 10750.8145.480.3148-
0.8675.661.790.95738.19 × 10867.0716.140.89621.86 × 10752.5845.790.3101-
0.8874.051.830.95524.88 × 10865.8716.100.89331.19 × 10754.3846.120.3051-
0.9072.321.900.95212.79 × 10864.5516.070.88977.28 × 10646.8352.080.2233-
average91.861.310.96285.98 × 10975.8516.060.8168.27 × 10749.4522.220.63-
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Kullyakool, S.; Thompho, S.; Boonchom, B.; Rungrojchaipon, P. Characterization, Kinetic Using Deconvolution Techniques and Thermodynamic Study of Synthetic MgHPO4·3H2O. Crystals 2023, 13, 567. https://doi.org/10.3390/cryst13040567

AMA Style

Kullyakool S, Thompho S, Boonchom B, Rungrojchaipon P. Characterization, Kinetic Using Deconvolution Techniques and Thermodynamic Study of Synthetic MgHPO4·3H2O. Crystals. 2023; 13(4):567. https://doi.org/10.3390/cryst13040567

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Kullyakool, Saifon, Somphob Thompho, Banjong Boonchom, and Pesak Rungrojchaipon. 2023. "Characterization, Kinetic Using Deconvolution Techniques and Thermodynamic Study of Synthetic MgHPO4·3H2O" Crystals 13, no. 4: 567. https://doi.org/10.3390/cryst13040567

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