Advances in Materials Science and Engineering

Volume 2012 (2012), Article ID 968396, 4 pages

doi:10.1155/2012/968396

Research Article

Rapid Synthesis of Dittmarite by Microwave-Assisted Hydrothermal Method

Lai zhenyu,1,2 Qian Jueshi,² Lu Zhongyuan,¹ Li Qian,¹ and Zou Qiulin¹

¹School of Materials Science and Engineering, Southwest University of Science and Technology, Sichuan, Mianyang 621010, China

²School of Materials Science and Engineering, Chongqing University, Chongqing 400030, China

Received 9 April 2012; Revised 29 June 2012; Accepted 29 June 2012

Academic Editor: Markku Leskela

Copyright © 2012 Lai zhenyu et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract.

Dittmarite was obtained using MgO and (NH₄)₂HPO₄ as raw materials via microwave-assisted hydrothermal method for 3 min at 120°C. The resulting samples were investigated by X-ray powder diffraction, scanning electron microscopy, Fourier transform infrared spectroscopy, and thermogravimetry-differential thermal analysis. The results indicate that dittmarite can be rapidly synthesized by microwave-assisted hydrothermal method. With higher temperature and longer reaction time, highly crystallized dittmarite can be obtained. Pure dittmarite can be synthesized for 3 min at 120°C, which is faster than with the use of any other reported methods.

1. Introduction

Dittmarite was first discovered at Skipton Caves by MacIvor in Australia [1]. The mineral has gained interest because of its strongly defined layered crystal structures. Many researchers have studied a series of compounds, MIMIIPO₄·H₂O (MI = NH₄, K; MII = Mn, Fe, Co, Ni), related to dittmarite for their synthesis [2] and application in shape-selective redox catalysts, ionic exchange, ionic conductivity, magnetic properties, and so on [3–6].

The present study focuses on the rapid synthesis of pure dittmarite via microwave-assisted hydrothermal method. MgO was used as the source of magnesium and (NH₄)₂HPO₄ was used as the source of phosphate and ammonium. The phases of the samples were identified by X-ray powder diffraction (XRD). The microstructure, infrared spectrum, and thermal properties of the samples were measured by scanning electron microscopy (SEM), Fourier transform infrared spectroscopy, and thermogravimetry-differential thermal analysis (TG-DTA), respectively.

2. Experiment

The MgNH₄PO₄·H₂O compound was prepared by a microwave-assisted hydrothermal method using Ethos A (Milestone, Italy). Analytical reagents MgO and (NH₄)₂HPO₄ were added in a half-filled Teflon container, keeping the solution pH by adding KOH at approximately 8. The solutions were microwaved for 3, 5, and 10 min at 50, 80, and 120°C. The resulting precipitate was separated by filtration, washed with deionized water and ethanol, and then dried for 24 h at 80°C.

The as-prepared samples were identified by XRD analysis on D/max-RB diffractometer (Rigaku, Japan) using CuKα radiation () in the range of 5° to 70°. Differential thermal analysis and thermogravimetry were traced using STA 449 C Jupiter (NETZSCH, Germany). Using TM-1000 (HITACHI, Japan), the SEM images of the samples were visualized. The infrared absorption spectrum of the sample was measured by a Thermo Scientific Nicolet 380 FT-IR spectrometer (Thermo Fisher Scientific, USA).

3. Results and Discussion

Figure 1 shows the powder XRD patterns of the synthetic samples with various temperatures and reaction times. Figure 1(a) illustrates the XRD patterns of samples prepared under 50°C for 3, 5, and 10 min. The main phase is MgO, but many reflections with lower intensity which represent dittmarite can also be found. In Figure 1(b), dittmarite and MgO still coexist in the samples, but the peak intensity of dittmarite increases with longer reaction times. Meanwhile, the peak intensity of MgO decreases with longer reaction times. The XRD patterns shown in Figure 1(c) match closely with the published pattern for dittmarite (JCPDF 36-1491). Thus, they are considered as single-phase materials. This result indicates that dittmarite can be easily synthesized by microwave-assisted hydrothermal method under 120°C within a 3 min reaction time.

(a) 50°C

(b) 80°C

(c) 120°C

Figure 1: XRD patterns of the samples.

The SEM micrograph of dittmarite is shown in Figure 2. The sample is mainly composed of plate-like dittmarite. The particles of dittmarite are in agglomeration state with a flower-like shape, the result is similar with the SEM morphgraph of dittmarite-type compound KMnPO₄·H₂O prepared by Koleva et al. [7].

Figure 2: SEM morphgraph of dittmarite.

The FT-IR absorption spectrum for dittmarite is shown in Figure 3. The phosphate ion vibrations are at about 1,061, 979, and 576 cm⁻¹. All the bands between 3250 and 2400 cm⁻¹ belong to the stretching modes The bands at 3500 and 1641 cm⁻¹ appear as a result of the stretching and bending H₂O vibrations, respectively, and around 1470 cm⁻¹ belong to the bending vibrations. The H₂O bending mode band is expected to appear at 1500 cm⁻¹ whereas the vibration at 633 cm⁻¹ represents the Mg–O bond. This spectrum is in accordance with previous studies [8–10].

Figure 3: FT-IR spectrum of the as-prepared dittmarite.

The TG and DTA curves of the obtained dittmarite at a rate of 10°C/min from ambient temperature to 800°C are presented in Figure 4. The thermal decomposition study shows the endothermic steps in the temperature range from 165°C to 370°C, and the experiment value is 34.9 wt%, which corresponds to the mass loss of water and ammonia molecules present in the structure.

Figure 4: TG-DTA curves for the as-prepared dittmarite.

Based on the above results, the formation mechanism of dittmarite can be discussed as follows. Due to heating by microwave irradiation, the samples result in homogeneous nucleation within a very short time and the nucleation and crystal growth occur simultaneously. For the past few years, many researchers have posited that the kinetics of material synthesis may be significantly accelerated using microwave-assisted hydrothermal methods [11–14]. In the current study, the rapid synthesis of dittmarite by microwave-assisted hydrothermal methods was found to have the potential for saving energy and cost of production.

4. Conclusions

In the current paper, dittmarite was rapidly synthesized by microwave-assisted hydrothermal methods at 120°C for 3 min using MgO and (NH₄)₂HPO₄ as raw materials. Microwave irradiation can significantly accelerate the reaction. The anticipated materials can be prepared at lower temperature and shorter reaction time using microwave heating.

Acknowledgments

Financial support from the National Natural Science Foundation of China (10976023), the Key Subject Laboratory of National Defense for Radioactive Waste and Environmental Security (08ZXNP05), the Key Project of Southwest University of Science and Technology (06ZX2148), and the Opening Project of Key Laboratory for Advanced Building Materials of Sichuan Province (07XZJ002) is gratefully acknowledged.

References

B. P. Onac and P. Forti, “Minerogenetic mechanisms occurring in the cave environment: an overview,” International Journal of Speleology, vol. 40, pp. 78–98, 2011.

H. Basset and W. Bedwell, “Studies of phosphates. Part I. Ammonium magnesium phosphate and related compounds,” Journal of the Chemical Society, pp. 854–871, 1933.

A. Pujana, J. L. Pizarro, L. Lezama, A. Goñi, M. I. Arriortua, and T. Rojo, “Synthesis, crystal structure, and magnetic properties of NH₄CuPO₄·H₂O,” Journal of Materials Chemistry, vol. 8, no. 4, pp. 1055–1060, 1998.

Y. Ding, D. J. Jones, P. M. Torres, and J. Roziere, “Two-dimensional nanocomposites: alternating inorganic-organic polymer layers in zirconium phosphate,” Chemistry of Materials, vol. 7, no. 3, pp. 562–571, 1995.

A. Pujana, J. L. Pizarro, L. Lezama, A. Goni, M. I. Arriortua, and T. Rojo, “Hydrothermal synthesis, structural, spectroscopic and magnetic studies of the NH₄Mn(AsO₄)·H₂O arsenate type dittmarite,” Materials Research Bulletin, vol. 34, no. 10-11, pp. 1545–1555, 1999.

V. G. Koleva, “Metal-water interactions and hydrogen bonding in dittmarite-type compounds M′M″PO₄·H₂O (M′ = K⁺, ⁺; M″ = Mn²⁺, Co²⁺, Ni²⁺): correlations of IR spectroscopic and structural data,” Spectrochimica Acta—Part A, vol. 62, no. 4-5, pp. 1196–1202, 2005.

V. Koleva, E. Zhecheva, and R. Stoyanova, “Facile synthesis of LiMnPO₄ olivines with a plate-like morphology from a dittmarite-type KMnPO₄·H₂O precursor,” Dalton Transactions, vol. 40, no. 28, pp. 7385–7394, 2011.

A. K. Sarkar, “Hydration/dehydration characteristics of struvite and dittmarite pertaining to magnesium ammonium phosphate cement systems,” Journal of Materials Science, vol. 26, pp. 2514–2518, 1991.

B. Šoptrajanov, V. Stefov, I. Kuzmanovski, G. Jovanovski, H. D. Lutz, and B. Engelen, “Very low H–O–H bending frequencies. IV. Fourier transform infrared spectra of synthetic dittmarite,” Journal of Molecular Structure, vol. 613, no. 1–3, pp. 7–14, 2002.

V. G. Koleva, “Vibrational behavior of the phosphates ions in dittmarite-type compounds M′M″PO₄·H₂O (M′ = K⁺, ⁺; M″ = Mn²⁺, Co²⁺, Ni²⁺),” Spectrochimica Acta—Part A, vol. 66, no. 2, pp. 413–418, 2007.

S. Ifrah, A. Kaddouri, P. Gelin, and D. Leonard, “Conventional hydrothermal process versus microwave-assisted hydrothermal synthesis of La1−xAgxMnO3+δ (x = 0, 0.2) perovskites used in methane combustion,” Comptes Rendus Chimie, vol. 10, no. 12, pp. 1216–1226, 2007.

Y. Hu, C. Liu, Y. Zhang, N. Ren, and Y. Tang, “Microwave-assisted hydrothermal synthesis of nanozeolites with controllable size,” Microporous and Mesoporous Materials, vol. 119, no. 1–3, pp. 306–314, 2009.

Y.-Z. Wang and Y. Fu, “Microwave-hydrothermal synthesis and characterization of hydroxyapatite nanocrystallites,” Materials Letters, vol. 65, no. 23-24, pp. 3388–3390, 2011.

L. Zhenyu, X. Guangliang, and Z. Yalin, “Microwave assisted low temperature synthesis of MnZn ferrite nanoparticles,” Nanoscale Research Letters, vol. 2, no. 1, pp. 40–43, 2007.