Abstract
Nanostructured powders of Sr1.96MgSi2O7:Eu 2+0.01 , R 3+0.01 (R3+ = Er3+, Tm3+ and Tb3+) have been fabricated via urea combustion technique. XRD results implied that tetragonal Sr2MgSi2O7 was the major phase whereas monoclinic Sr2SiO4 and SrSiO3 were the minor phases. Meanwhile, field emission SEM textures showed the hollow spherical network-like shape structures filled with fused interconnections for the Sr1.96MgSi2O7:Eu 2+0.01 sample. It has been recognized that the replacement of Sr2+ with co-dopant R3+ ions e.g. Er3+, Tm3+ and Tb3+ considerably help obtaining homogeneous structure as well. The values of band gap energy and calculated refractive index were ultimately dependant on the ionic radius of R3+ co-doping ion. It has been suggested that the divalent activator ion (Eu2+) was responsible for the number of PL emission spectra, while the trivalent co-activator ions (R3+) were the key reasons for variations in the broadening and intensity of PL emission spectra.
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1 Introduction
Alkaline earth silicate based phosphors have attracted much attention as host materials than can display distinguished luminescence properties compared with aluminate and sulphide based phosphors (Yu et al. 2004; Fu et al. 2005; Clabau et al. 2005; Gong et al. 2012). In this context, Eu2+-activated strontium magnesium silicate (SMS) phosphors have been potentially utilized for various applications such as decorative paints, traffic and emergency signs, photo-sensitizers, biological probes and medical diagnostics (Chen et al. 2006; Wu et al. 2011; Maldiney et al. 2013). The most commonly Eu2+, Dy3+-codoped strontium magnesium silicate material has been extensively considered, suggesting excellent properties of chemical stability, high quantum efficiency and long afterglow brightness (i.e. phosphorescence) (Pan et al. 2008; Song et al. 2008; Wu et al. 2010, 2011; Ishizaki et al. 2012; Ye et al. 2013). Basically, the co-activator (codopant ion) plays a crucial role in harnessing the emission extent and prolonging the decay time by trapping the free holes and allowing multiple electronic 4f–5d transitions between the produced successive energy levels (Chen et al. 2006; Dorenbos 2005; Aitasalo et al. 2006; Shi et al. 2007). In this regard, a lot of research has been accomplished during the last few years concentrated on exploring the effect of different divalent activators such as Eu2+, Mn2+ and trivalent co-activators such as Dy3+, Tm3+, La3+ and Nd3+, … etc. on the luminescence emission properties of alkaline earth silicate based host materials (Aitasalo et al. 2005; Liu et al. 2005; Wu et al. 2009, 2010; Alvani et al. 2005). Moreover, various preparation methods have been introduced for synthesis of the long persistent activated strontium magnesium silicate phosphors including solid state (Gong et al. 2012; Song et al. 2008; Li et al. 2009), co-precipitation (Pan et al. 2008), combustion (Bhatkar and Bhatkar 2011) and spinning processes (Ye et al. 2013; Jun et al. 2014). Otherwise, there is a significant lack in the research studies concerning the impact of co-dopant (i.e. co-activator) ions rather than Dy3+ ion which are mainly responsible for the afterglow phenomena of all photoluminescence materials. The recent study of different co-activators e.g. Er3+, Tm3+ and Tb3+ on Eu2+-SrAl2O4 has confirmed the fundamental differences in the photoluminescence effect with each lanthanide cations (Sanad and Rashad 2016). For these reasons, this work aims at monitoring the principal changes in the crystallographic, morphological, optical and photoluminescence properties of Eu2+-Sr2MgSi2O7 samples and the Eu2+, R3+co-activated samples with different lanthanide cations including Er3+, Tm3+ and Tb3+. Accordingly, nano-structured phosphors powders have been synthesized via simple urea combustion method. Alongside, different parameters such as cell parameters, particle size, band energy gap as well as refractive index and emission spectrum maxima have determined from the obtained results.
2 Experimental
2.1 Materials and methods
Anhydrous strontium nitrate Sr(NO3)2 (Sigma-Aldrich 99.9%), magnesium acetate tetrahydrate Mg(OAc)2.4H2O (Sigma-Aldrich 99.9%), TEOS SiC8H20O4 (Sigma-Aldrich 99.9%), europium nitrate hexahydrate Eu(NO3)3.6H2O (Alfa Aesar 99.9%), erbium acetate tetrahydrate Er(OAc)3.4H2O (Alfa Aesar 99.9%), thulium acetate hydrate Tm(OAc)3.xH2O (Sigma-Aldrich 99.9%), terbium nitrate pentahydrate Tb(NO3)3.5H2O (Sigma-Aldrich 99.9%) and urea N2H4CO (Sigma-Aldrich 99.5%) were employed as raw materials. Deionized water was used in the whole work. Strontium magnesium silicate phosphors of four chemical compositions Sr1.99MgSi2O7:Eu 2+0.01 (SMS1), Sr1.98MgSi2O7:Eu 2+0.01 , Er 3+0.01 (SMS2), Sr1.98MgSi2O7:Eu 2+0.01 , Tm 3+0.01 (SMS3) and Sr1.98MgSi2O7:Eu 2+0.01 ,Tb 3+0.01 (SMS4) micropororous samples were synthesized via urea combustion method. In typical synthesis, Sr, Mg, Si and Eu (1%wt.) salts of stoichiometric amounts were dissolved in 0.5 M urea solution which act as a combustion fuel and complexing agent. Then, about 1%wt of R3+ (Er3+, Tm3+ or Tb3+) salts was also added for precursor preparation of the codoped strontium magnesium silicate phosphors Sr1.98MgSi2O7: Eu2+, R3+. The solutions were mixed for 30 min then boiled to evaporate the excess water. Thereafter, the resulting viscous liquid started to undergo auto-combustion after putting the glass beaker directly in a muffle furnace (at 400 °C) yielding grayish dark fluffy precursor powders. Finally, the obtained combustion precursors were pre-calcined at 1000 °C for 6 h in an air atmosphere to remove the residual carbon. Finally, these powders were calcined again at 1200 °C for 3 h with heating rate (5° min−1) in presence of gas mixture (argon 95% and hydrogen 5%). The reducing H2 gas of 5% was injected in order to ensure complete conversion of activator ion Eu3+ into Eu2+ ion.
2.2 Sample characterization
X-ray powder diffraction (XRD) was executed on a model Bruker AXS diffractometer (D8-ADVANCE Germany) with Cu Kα (λ = 1.54056 Å) radiation, operating at 40 kV and 40 mA. The diffraction data were recorded for 2θ values between 20° and 60° and the scanning rate was 3° min−1 or 0.02°/0.4 s). The particle morphology was inspected by a field emission scanning electron microscopy FE-SEM (JEOL-JSM-5410 Japan). The optical measurements were implemented using (Jasco-V-570 spectrophotometer, Japan) using integrating sphere reflectance unit. The diffuse reflectance and absorption spectrum measurements of all phosphors have been accomplished in the wavelength range 200-2000 nm at room temperature. Photoluminescence (PL) spectra were obtained at room temperature using fluorescence spectrophotometer (SHIMADZU RF-5301PC Japan) with xenon discharge lamp (150 W) as excitation source.
3 Results and discussion
3.1 Crystal structure
Figure 1a shows the XRD patterns of Eu2+-doped and Eu2+, R3+ -codoped samples calcined at 1200 °C for 3 h. The Sr2MgSi2O7 tetragonal crystal structure is clearly identified as the major phase (PDF card no. 75-1736) with P-421m space group. Minor diffraction peaks are also detected for two phase impurities including Sr2SiO4 (PDF card no. 39-1256) and SrSiO3 (PDF card no. 24-1230) phases where they could be obtained as a result of replacing Sr2+ with two types of rare earth ions. Therefore, the crystallinity and peaks intensities of the main phase are quite depressed in case of SMS3 and SMS4 codoped samples. It is also noticed that the peaks of the main phase are slightly shifted which considered a true evidence of rare earth ions introduction in the crystallite sites of Sr2+ ions as shown in Fig. 1b. The detected broadening for most of XRD peaks suggests the nano-sized crystals of the prepared powders. Evidently, the crystallite size of Sr2MgSi2O7 phase in the as-prepared nanocomposites can be estimated by applying Scherrer’s equation (Sanad et al. 2014) based on the average of the highest two reflections (211) at 2θ = 30.5° and (212) at 2θ = 43.3° using the full width at half maximum (FWHM). It is found that the Eu2+, R3+-codoped samples have smaller crystallite sizes than that of Eu2+-doped sample. This might be explained by the crystallinity quenching with rare earth elements which has a direct impact on the crystal growth rate.
The lattice parameters a and c of the samples was calculated using following equation (Rashad et al. 2015):
where a and c are lattice parameters, d is the interplanar distance and (h k l) are the Miller indices.
It is clear that the values of cell parameters and lattice volumes of Eu2+, R3+-codoped samples are decreased than those of Eu2+-doped sample of as a result of the shrinkage in the M–O bonds. This behavior could be explained by the differences of radius of substituted metal ions (i.e. Sr2+ < R3+), which also certifies the measured reduction in the crystallite size of Eu2+, R3+-codoped samples. The variations in the crystallographic parameters and phases are collected in Table 1.
3.2 Crystal morphology
Figure 2 reveals the FE-SEM images of SMS1, SMS2, SMS3 and SMS4 phosphors at two different magnifications × 2000 (a, c, g, e) and × 5000 (b, d, f, h). The microstructure of Eu2+-doped sample (SMS1) appears with hierarchical -like texture. The particles have spherical shape of fused interconnections and their size ranges from 1 to 3 µm. The second sample SMS2 displays sponge-like structure. The particle size average slightly decreases which encourages higher diffusion among the interconnected particles. However, the Tm3+ ion addition in the third sample SMS3 forms a homogenous surface of small agglomeration and regularly distributed pores. The particle size average ranges from 0.5 to 1.5 µm. Meanwhile, the fourth sample SMS4 indicated different particles shape and dimensions. This could be assigned to the presence of mixed phases creating intrinsic allotropic like structure. Therefore, both the porosity and particle size average are clearly decreased in comparison with other samples. These obtained particle size results are found to be in a good agreement with the calculated crystallographic parameters from XRD data. The specific surface area SBET was 10.138 m2/g whereas the mean pore diameter and pore volume were 10.4129 nm and 5.27 × 10−3 cm3/g, respectively Eu2+-doped SMS1 sample phosphors calcined at 1200 °C for 3 h. The low surface area was attributed to the absorption of some organic species results from the combustion of urea on the surface of the samples (Rashad et al. 2016).
3.3 Optical properties
3.3.1 Diffuse reflectance and absorption spectra
The UV–Vis diffuse reflectance and absorption spectra of Eu2+-doped and Eu2+, R3+ (Er3+, Tm3+ or Tb3+) codoped samples calcined at 1200 °C for 3 h were displayed in Fig. 3. All samples was characterized by a relatively high reflectivity ~ 72% for sample SMS1 above 500 nm, and the highest was ~ 75% for sample SMS4 above 320 nm as shown in Fig. 3a. As clearly visible, the absorbance spectrum shows absorbance values of about 0.15 for samples SMS1 and SMS2, 0.13 at wavelengths above 500 nm as well as samples SMS3 and SMS4 as shown in Fig. 3b.
3.3.2 Band gap energy
In the limiting case of an infinitely powder samples, thickness and sample holder have no influence on the value of reflectance (R). In this case, the Kubelka–Munk equation at any wavelength becomes (Elseman et al. 2016):
F (R∞) is the so-called remission or Kubelka–Munk function which is proportional to absorption, S called K–M scattering and K absorption coefficients. In the parabolic band structure, the band gap Eg, and absorption coefficientα, of a direct band gap semiconductor are related through the well known equation (Sanad et al. 2016):
where α is the linear absorption coefficient of the material, hν is the photon energy and A is proportionality constant. When the material scatters in perfectly diffuse manner (or when it is illuminated at 60 ± incidence), the K–M absorption coefficient (K) becomes equal to 2α (K = 2α). In this case, considering the K–M scattering coefficient (S) as constant with respect to wavelength, and using the remission function in Eq. (2) we obtain the expression (Elseman et al. 2016):
Therefore, obtaining F (R∞) from Eq. (3) and plotting the [F (R∞)hν]2 against hν, the band gap Eg of a powder sample can be extracted easily. It is found that Sr1.98MgSi2O7: Eu 2+0.01 , Tm 3+0.01 sample posses the lowest Eg value among those of the other samples as illustrated in Fig. 4. For instance, it is also seen that the ionic radius of the rare earth dopants are in the following order [Tm3+ (230 pm) < Er3+ (232 pm) < Tb3+ (237 pm) < Eu2+ (240 pm)]. Therefore, our band gap energy measurements are in good agreement with the fact of increasing Eg value with decreasing ionic radius of doping ion and vices versa (Mote et al. 2013; Manikandan et al. 2013; Huse et al. 2013; Viswanath et al. 2014).
3.3.3 Refractive index and dielectric constant
The refractive index (n) of semiconducting materials is very important in determining the optical properties of the material. Knowledge of n is essential to design heterostructure lasers in the optoelectronic devices as well as in the solar cell applications.
The refractive index (n) of the samples can be calculated using Herve and Vandamme relation (Herve and Vandamme 1994). Where Eg is the energy band gap.
Where A and B are numerical constants with values of 13.6 and 3.4 eV, respectively. The calculated averages of the refractive index for Eu3+-doped and R3+, Eu3+-doped samples are recorded in Table 2. Figure 5 evinces the variation in the refractive indices against the band gap energies. It is indicated that the minimum refractive index (n) was 1.93 at 4.82 eV for Sr1.98MgSi2O7: Eu 2+0.01 , Tm 3+0.01 sample. Moreover, it can also be implied that the refractive indices are shifted towards lower values at higher Eg values.
On the other hand, both static and high frequency dielectric constants are determined for all the samples as listed in Table 2. The high frequency dielectric constant (εα) is calculated using the relation (Herve and Vandamme 1994):
The static dielectric constant (ε0) of the samples is calculated using the relation (Herve and Vandamme 1994):
Such obtained results emphasized that the change in the refractive indices and dielectric constants are mainly relied on the absorption features of these phosphors.
3.3.4 Photoluminescence (PL) properties
Figure 6 reveals the typical PL emission spectrum of the as-prepared phosphors after excitation at different wavelengths (365, 380, 390 and 410 nm). The PL results of SMS1 sample show two broad convoluted emission bands which are centered around 460 and 555 nm. The deconvolution of the bands increases with increasing excitation wavelength. The collected signals are different in the band width and intensity. The existence of two types of luminescent centers is due to the difference of coordination number of Sr from 6 to 8 in the Sr2MgSi2O7 crystal structure (He et al. 2010; Dutczak et al. 2012). Therefore, the Eu2+ ions replaces Sr2+ ion and located two different sites (Eu 1 and Eu 2) (Ochi 2006; Fei et al. 2005; Zhang et al. 2010). Consequently, the emission bands at 460 and 555 nm are attributed to the excitation transitions of different Eu2+ centers 4f6–4f15d7. The Eu2+ ion becomes an excited Eu+ after the capture of the excited electrons in the conduction band. Meanwhile, the codopant ions R3+ (Er3+, Tm3+ or Tb3+) act as trap levels for the created free holes and turn into R4+. After the termination of excitation source, the hole is thermally released to the valence band again and migrates to the excited Eu+ ion where it is captured. As a result recombination takes place, i.e. the excited Eu+ returns to the Eu2+ ground state, which gives rise to the persistent luminescence properties (Pan et al. 2008; Sabbagh Alvani et al. 2005; Shirakura et al. 2005). It is clear that the SMS1 showed higher performance than the reported results at the same excitation wavelengths (Song et al. 2008; Zhang et al. 2010). Meanwhile, SMS2, SMS3 and SMS4 samples displayed similar performance to the previous published co-doped phosphors (Pan et al. 2008; Jun et al. 2014).
Eventually, Er3+, Eu2+-codoped sample reveals the maximum intensity and broadening of PL emission peaks in comparison with other co-doped phosphors. This behavior could be explained by the largest ionic radii difference between Eu2+ and Er3+ ions which leads to creating the largest number of trapping and releasing effects, thus strong and weak emission bands are easily recorded (Sanad and Rashad 2016).
The PL emission spectrum at excitation λEX = 380 nm of Eu2+-doped and Eu2+, R3+ (Er3+, Tm3+ or Tb3+) co-doped samples annealed at 1200 °C for 3 h were displayed in Fig. 6b were seen Eu2+-doped Sr1.98MgSi2O7 (SMS1) at around 461 nm (2.69 eV) with a broad line shape with FWHM of 58 nm, whereas in Eu2+, Er3+ doped (SMS2) it is seen at around 462 nm (2.68 eV) with FWHM of 67 nm, Eu2+, Tm3+ (SMS3) it is seen at around 477 nm (2.60 eV) with FWHM of 148 nm and Eu2+, Tb3+ (SMS4) it is seen at around 485 nm (2.56 eV) with FWHM of 133 nm, as listed in Table 2.
Figure 7 illustrates band deconvolution of the photoluminescence spectra of R3+ (Er3+, Tm3+ or Tb3+) co-doped Sr2MgSi2O7:Eu2+ phosphor annealed at 1200 °C for 3 h. Figure 7a shows under the near UV excitation of 380 nm, deconvolution of Sr2MgSi2O7:Eu2+ phosphor three broads blue emission band centered around 430–495 nm and several sharp lines in the orange–red region peaking at about 522, 592, 616, 632, and 658 nm. The broad blue emission band, it is known that Eu2+ presents three broads emission band peaking at around 430–495 nm due to the 4f 5d1 to 4f7 transition of Eu2+(8S7/2-7Fj, j = 0, 1, 2, 3, and 4) (Hao Tam et al. 2016). The red emission lines should be ascribed to the transitions within the 4f6 configuration of Eu3+ which these lines corresponds to the 5D0 → 7F0, 5D0 → 7F1, 5D0 → 7F2, 5D0 → 7F3 and 5D0 → 7F4 transitions of Eu3+, respectively (Hao Tam et al. 2016; Yao et al. 2011). It could be possible that, co-doping R3+ ions e.g. Er3+, Tm3+ and Tb3+ considerably a small amount of Eu3+ ions and R3+ were decreased Eu2+ ions that leads to the blue emission which can diminish this ions transformation. It can also be seen from Fig. 7 that while the PL intensity of the red emissions increased with different rare earth co-doped R3+ (Er3+, Tm3+ or Tb3+), the peak position and the shape of the blue band change arbitrary with different rare earth doping. However, the blue emission bands related to Eu2+ ions is sensitive to the host lattice environment, the change of the blue emission band with different rare earth co-doped R3+ (Er3+, Tm3+ or Tb3+) may indicate the change of the crystalline phases in the sample as observed from XRD results. Furthermore, the increase of the PL intensity of the red emission is related to the higher content of the Sr2MgSi2O7 phase upon to different rare earth co-doped R3+ (Er3+, Tm3+ or Tb3+).
4 Conclusion
Different samples of lanthanides co-activated strontium magnesium silicate based phosphors have been successfully prepared using simple urea combustion technique. The changes in the crystal structure and the morphology of the formed particles have been investigated in the presence and the absence of trivalent co-doping ions including Er3+, Tm3+ or Tb3+. Clearly, tetragonal Sr2MgSi2O7 phase was the dominant phase while Sr2SiO4 and SrSiO3 were the minor phases with monoclinic crystal structures, respectively. FE-SEM results established the decrease of particle size with uniform microstructure with lanthanide co-doping were exhibited. Nevertheless, Sr1.98MgSi2O7:Eu 2+0.01 sample displayed the hierarchical sponge-like morphologies with the few interconnected particles. The Sr1.99MgSi2O7:Eu 2+0.01 sample demonstrated the minimum band gap energy ~ 4.67 eV, whereas Sr1.98MgSi2O7:Eu 2+0.01 , Tm 3+0.01 achieved the maximum band gap energy ~ 4.82 eV. The photoluminescence emission spectrum show two broad convoluted emission bands which were centered around 460 and 555 nm as well as the deconvolution of the bands raised with rising the excitation wavelength. Er3+, Eu2+-co-doped sample revealing the maximum intensity and broadening PL emission peaks in comparison with other co-doped phosphors.
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Sanad, M.M.S., Rayan, D.A. & Rashad, M.M. Optical and photoluminensce properties of Eu2+-activated strontium magnesium silicate phosphors using different rare earth co-activators. Opt Quant Electron 51, 192 (2019). https://doi.org/10.1007/s11082-019-1913-x
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DOI: https://doi.org/10.1007/s11082-019-1913-x