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Indian Journal of Materials Science
Volume 2014 (2014), Article ID 675417, 7 pages
Influence of Rare Earth Doping on Microstructure and Luminescence Behaviour of Sodium Sulphate
Department of Physics, Bangalore University, Jnana Bharathi Campus, Bangalore 560 056, India
Received 12 October 2013; Accepted 1 December 2013; Published 6 January 2014
Academic Editors: S. Binetti, F. Gourbilleau, and M. K. Jayaraj
Copyright © 2014 Y. S. Vidya and B. N. Lakshminarasappa. 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.
Na2SO4, Na2SO4: Li, and Na2SO4: Li, Eu, Dy phosphors were prepared by using slow evaporation technique followed by subsequent calcination at 400°C for 4 h. Doping with Li+ ion stabilized the thenardite phase of host matrix, while codoping with RE3+ stabilized the phase transformation from stable thenardite to metastable mirabilite crystal structure. The microstructure and morphology were studied by using scanning electron microscopy and transmission electron microscopy. The thermoluminescence studies revealed that isovalent doping of Li+ served as a quencher and addition of codopant introduces the additional trap sites in the host matrix. The room temperature emission spectra of Li-doped, RE3+-codoped, and undoped Na2SO4 were studied under ultraviolet radiation. For pure Na2SO4 the two peaks which appeared are at 364 and 702 nm, respectively. The emission intensities of RE3+-codoped samples increase with increase in dopant concentration.
Alkali sulphates have been known for a long time as versatile and excellent phosphor materials. These sulphates have attracted the attention of many workers in view of their potential applications in radiation dosimetry, TV screens, cathode ray tubes, and so forth. A variety of defect centres are likely to be formed in sulphate based phosphors [1–6]. Sulphate based radiation dosimeter materials doped with rare earth (RE) ions have been extensively investigated due to their high luminescence sensitivity . Significant advancements have been made in thermoluminescence (TL) and photoluminescence (PL) experiments during the last couple of decades [8–10]. Up to date, sodium sulphate is extensively investigated from the prospect of phosphor material attributed to its simple chemical composition and defect rich crystal. Na2SO4 exhibits a variety of phase transitions between its five anhydrous polymorphs (labelled I–V). The phase transformation sequence among the Na2SO4 polymorphs can be described as Na2SO4 forms two naturally occurring minerals: mirabilite (Na2SO4·10H2O) and thenardite (Na2SO4). Both are in thermodynamic equilibrium at 32°C which may be lowered to 18°C in the presence of foreign ions . At room temperature, phase V (thenardite) is reported to be stable while phase III is metastable. Phases I and II are high-temperature polymorphs; however, phase II is reported to have a narrow stability zone. Phase IV is considered to be metastable and its phase relation and structure have yet to be well established [12–15]. Correcher et al.  observed the spectra of infrared-stimulated luminescence (IRSL), radioluminescence (RL), and TL of thenardite. Sidike et al.  studied the photoluminescence (PL) spectra, excitation spectra, and decay curves of natural, heat-treated, and -irradiated thenardite from Ai-Diang salt lake and concluded that crystal defects were responsible for observed luminescence. Reliable studies on the PL and TL properties of thenardite are very few till to date, to the best of our knowledge. In order to develop new dosimetric materials and to obtain a better understanding of the physical mechanism of radiation effects, Na2SO4 is doped and codoped with activators.
In the present work, fading TL and PL behaviour of pure and RE3+-codoped Na2SO4 matrix are explained in detail. The host matrix shows the existence of bicrystalline phase after codoping with hypervalent ion. The codoped and pure Na2SO4 samples have been well characterized by powder X-ray diffraction (PXRD), scanning electron microscopy (SEM), and transmission electron microscopy (TEM) techniques.
2.1. Materials Preparation
Na2SO4 and Li2SO4 (0.5 mol%) were stoichiometrically dissolved in double-distilled deionized water (A). A known quantity of RE2O3 (RE = Eu and Dy) was dissolved in concentrated H2SO4 (B) and added to solution (A) to get RE/Na mole ratio in the concentration range of 0.08 to 0.5 mol%. The solution is then dried in an oven. The sample thus obtained in powder form was crushed and calcined at 400°C for 4 h in furnace. After natural cooling to RT, it is crushed to fine powder and pressed into pellets (80 kg/cm2).
2.2. Material Characterization
The PXRD pattern of sample is obtained using Philips PW/1050/70/76 X-ray diffractometer which was operated at 30 KV and 20 mA using CuKα radiation as the source with a nickel filter at a scan rate of 2°/min. The size, shape, and distribution of the grains were examined by SEM analysis using Quanta 200 FEI SEM. TEM measurement was carried out using a Philips CM 200 microscope having 2.4 Å resolutions.
TL glow curves were measured with system in the temperature range from 25 to 300°C operating with linear heating rates of 5 K s−1. Prior to the TL measurements, samples (pellets of 1 mm thickness with 5 mm in diameter are used for TL measurements) were exposed to irradiation from a 60Co source to a total dose of 0.02 to 2 kGy at the sample cavity. Photoluminescence emission and excitation spectra were registered in identical experimental conditions, using Yvon Fluorometer, Jobspectrometer with Xenon lamp source at an excitation wavelength of 340 nm at SAIF, IIT, Chennai, India.
3. Results and Discussion
3.1. Powder X-Ray Diffraction Analysis
Figure 1 shows the PXRD of Na2SO4, Na2SO4: Li0.5%, and Na2SO4: Li0.5%, Eu0.5%, . The undoped and Li+-doped Na2SO4 exhibited stable thenardite, while codoping of RE3+ to Na2SO4 resulted in the phase transformation from stable thenardite to metastable mirabilite phase. The mirabilite content in the sample showed critical dependence on RE3+ concentration.
The average crystallite size () and matrix distortion are calculated from FWHM of the most intense PXRD peak using the following, respectively [18, 19]: where “” is the average grain size of the crystallites, “” is the incident wavelength, “” is the Bragg angle, “” is the stress factor, and “” is the diffracted full width at half maximum (in radians) caused by the crystallites.
The higher ionic radius of the RE3+ ion can possibly act as an interstitial impurity in the host matrix. The introduction of substitutional dopant metal ions with a higher ionic size would induce cationic vacancies at the surface of thenardite grains, which favours the bond rupture, ionic rearrangement, and structure reorganization for the formation of mirabilite phase. The thenardite to mirabilite phase is generally considered as a nucleation growth process during which the mirabilite nuclei are formed within the thenardite phase. The thenardite grain size decreases with an increase in the Dy3+ concentration (Table 1).
With an increase in the Dy3+ content, the variation in the lattice parameter was reflected in the elongation of the -axis (Table 2). Since only the dimension changes while -axis and -axis remain almost constant for the range of dopant concentration, it can be concluded that with increase in Dy3+ concentration the crystal growth proceeds along -axis. The extent of matrix distortion was nearly ~200 times higher for doped samples compared to bare samples due to the higher ionic radius of RE3+ compared to host Na+. It is well known that the incorporation of RE3+ ions within the host crystal introduces lattice strains as a result of size mis match.
Due to smaller ionic radius, the stress associated with Li+ is dominated by lattice contraction. It is interesting to note that stress factor associated with Li+ doping (lattice contraction) is larger compared to RE3+ doping (lattice expansion).
3.2. Scanning Electron Microscopy Studies
The surface morphological features of the Na2SO4, Na2SO4: Li0.5%, and Na2SO4: Li0.5%, Eu0.5%, Dy0.5% samples are shown in Figure 2. The pure, Li+-doped, and RE3+-codoped Na2SO4 showed the uniform distribution of generalized hexagonal habit of grains corresponding to orthorhombic prisms and pyramids without any agglomeration. The codoping leads to noticeable changes on the grain size of the sample.
3.3. Transmission Electron Microscopy Studies
The shape and size of these particles were also determined by TEM (Figures 3 and 4). TEM images and selected area electron diffraction (SAED) of Na2SO4 and Na2SO4: Li0.5% showed that the crystals are hexagonal-shaped particles with almost no amorphous constituents and are weekly aggregated. SAED patterns of these samples were neither regular diffraction spots nor whole diffraction rings, indicating that the number of polycrystalline grains in the selected area was finite.
Results revealed that, in pure Na2SO4, these spots might belong to the -values of 3.636, 3.18, 3.07, and 2.78 Å which corresponds to (200), (131), (040), and (311) planes of thenardite. In Na2SO4: Li+, Eu3+, Dy3+ these spots correspond to -values 4.166, 3.77, 2.85, and 2.01 Å which correspond to (112), (220), , and (151) planes. Among them (220) and (151) belong to thenardite and (112) and belong to mirabilite content of Na2SO4.
3.4. Thermoluminescence Studies
3.4.1. TL Studies of Na2SO4 and Na2SO4: Li+
TL property of host sample was investigated at different γ-ray dose levels. The pristine orthorhombic phosphor has only one glow main peak at ~180°C. The intensity of these glow peaks increases with irradiation and shifts towards higher temperature region (Figure 5).
In Na2SO4: Li0.5%, Li+ quenches the TL intensity of Na2SO4 and shifts the TL glow curves position towards lower temperature (Figure 6).
3.4.2. TL Studies of Na2SO4: Li+, Eu3+, Dy3+
The glow curve of Na2SO4: , , consists of a single glow peak ranging from 382 to 424 K (Figure 7). The TL intensity increases with increase in the -ray exposure and lies between that of Na2SO4: , and that of Na2SO4: , . This suggests that an increasing number of traps responsible for these glow peaks were getting filled with an increase in radiation dose. These traps release the charge carriers on thermal stimulation to finally recombine with their counterparts, thus giving rise to different glow peaks. However, the TL intensity still remains higher compared to host sample.
3.4.3. Calculation of Kinetic Parameters
The trap parameters, such as activation energy and order of kinetics , were calculated for the different concentration TL glow peak of the Na2SO4: Li0.5% and Na2SO4: Li0.5%, , ( 0.1, 0.2, and 0.5) phosphor irradiated with a gamma dose of 2 kGy at RT using Chen’s set of empirical formulae for the shape of glow curve (Figure 8) .
In the present study, geometrical form factor value is very close to 0.52, suggesting that the TL emission involves retrapping of charges. Table 3 lists the peak parameters as obtained for deconvoluted peaks for different RE3+ concentration where, , , , where is the Boltzmann constant .
3.4.4. TL Fading
The effect of fading was studied up to 90 days by irradiating samples with a gamma dose of 2 kGy. The extent of fading was maximum for Na2SO4 compared to codoped Na2SO4, suggesting that introduced by addition trap sites favouring the intensification of TL signal (Figure 9). About 1.4%, 1.16%, and 1.19% of fading were observed for Na2SO4, Na2SO4: Li0.5%, and Na2SO4: Li0.5%, Eu0.5%, Dy0.5%, respectively, during the first five days, but thereafter the intensity remained almost constant up to 20 days; afterwards fading becomes maximum. However, it is suggested that the irradiation of nanocrystalline phosphor at high doses results in the formation of deep traps which resulted in the fading of TL signal.
3.5. Photoluminescence Studies
3.5.1. PL Studies of Na2SO4 and Na2SO4: Li+
The PL emission spectra of host sample consist of a strong peak at 364 nm for pure thenardite and are attributed to band-to-band PL phenomenon due to the band gap excitation (Figure 10).
In addition, low intense peak at ~702 nm is attributed to excitonic PL arising from intrinsic defects of thenardite Na2SO4 powders. The emission band with the most intense peak at approximately 702 nm showed a distinct vibronic structure. The vibronic structure characteristic of S2− centre was observed in the red region.
The -ray irradiated thenardite did not change the feature of PL but reduced the luminescence efficiency. This suggests that -ray irradiation of thenardite may generate a killer centre for luminescence in thenardite. We could not find any dip due to absorption by the killer centre. It seems that -ray irradiation has an annealing effect although mechanism was not yet clear.
The PL emission spectra of Na2SO4: Li0.5% are the same as that of the host sample (Figure 11).
3.5.2. PL Studies of Na2SO4: Li+, Eu3+
The PL emission spectra of Na2SO4: Li+, Eu3+, Dy3+ for 340 nm excitation showed bands at 481, 490, 575, and 711 nm. The first three peaks are assigned to Dy3+ and the peak arising at 711 nm was assigned to Eu3+ emission (Figure 12).
Pure and codoped phosphors have been prepared at RT by slow evaporation technique. PXRD pattern confirmed the phase transformation from stable thenardite to metastable mirabilite after codoping with RE3+ ions. SEM studies showed the presence of uniform distribution of prisms and pyramids. The codopant introduces additional trap sites favouring the intensification of TL signal. Therefore, up to a given irradiation dose, this phosphor has potential candidate for use in radiation dosimetry. The PL intensities of codoped Na2SO4 samples were found to be dependent on the RE3+ concentration.
Y. S. Vidya is thankful to “ISRO-ISEC, advanced devices and radiation cell, Bangalore” for providing facilities for -irradiation. The author also wishes to thank Dr. S. Girish Kumar, PDF Scholar, Department of Physics, IISc, Bangalore, and Department of Physics, Lal Bahadur Shastri Government First Grade College, R. T. Nagar, Bangalore, for their support.
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