Open Access Article
Abdelrhman
Yousif
*ab,
Andrey
Turshatov
*a,
Dmitry
Busko
a,
Krishnan
Rajagopalan
a,
Elizabeth
Coetsee-Hugo
c and
Bryce S.
Richards
*ad
aInstitute of Microstructure Technology, Karlsruhe Institute of Technology (KIT), Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, Germany. E-mail: abdelrhman.mohmmed@kit.edu
bDepartment of Physics, Faculty of Education, University of Khartoum, P.O. Box 321, Omdurman 11115, Sudan. E-mail: abdelrhman.yousif@uofk.edu
cDepartment of Physics, University of the Free State, Bloemfontein ZA9300, South Africa
dLight Technology Institute, Karlsruhe Institute of Technology, Engesserstrasse 13, 76131 Karlsruhe, Germany
First published on 30th March 2026
In this work, Bi3+-doped CaYGaO4 phosphors were synthesised through solid-state reaction and systematically optimised using lithium-based fluxes to enhance their photoluminescence quantum yield (PLQY) in the blue region. Comparative studies between Li2O and Li2CO3 fluxes revealed distinct structural and optical impacts. Rietveld refinement confirmed effective Bi3+ incorporation, with samples treated using 2% Li2CO3 and 1% Li2O exhibiting superior crystallinity. SEM analysis showed molten-like particle morphologies and increased porosity in Li2CO3-treated samples features absent in those treated with Li2O. XPS results highlighted a notable reduction in oxygen-related defects in Li2CO3-modified phosphors, correlating with improved PLQY performance. Photoluminescence measurements demonstrated strong blue emission at 430 nm under 330 nm excitation, alongside additional red (720 nm) and near-infrared (780 nm) emissions from stabilised Bi2+ species, attributed to lithium-induced lattice rearrangements. The sample treated with Li2CO3 achieved a PLQY of 70%, surpassing flux-free and Li2O-assisted counterparts, reinforcing the pivotal role of flux chemistry in fine-tuning emission efficiency. In particular, lithium carbonate flux profoundly influences Bi3+-doped CaYGaO4 phosphors, establishing flux chemistry as a versatile tool for engineering efficient blue emitters for photonic applications.
Recent studies have also highlighted alternative blue-emitting candidates including Bi3+-doped halide nanocrystals,9 Cd-based coordination complexes,10 nitrogen-doped carbon dots, and organic dyes such as violanthone derivatives that offer promising PLQY and spectral tunability,11 yet remain underrepresented in current reviews.
This study focuses on Bi3+-doped phosphors due to their favourable combination of high PLQY, robust thermal and chemical stability, emission wavelengths that closely align with the blue peak of the PAR spectrum, and relatively low toxicity compared to other heavy-metal-based emitters; while factors such as particle size and mixed-valence behaviour remain complex, they offer additional avenues for tuning luminescent performance.
Bi3+-activated oxide hosts stand out among the underexplored materials due to their broad emission profiles and strong near-UV absorption.2,12 These properties stem from the adaptable 6s2 electronic configuration of Bi3+ ions,3 which allows transitions from the 1S0 ground state to excited 3P0, 3P1, 3P2, and 1P1 levels. The dipole-allowed 1S0 → 3P1 transition predominantly drives intense blue luminescence.2,13
CaYGaO4 doped with Bi3+ has garnered considerable interest as a versatile luminescent material, distinguished by its pronounced absorption in the near-UV region and efficient blue emission. These attributes enable its deployment in multiple photonic applications, including persistent luminescence in elevated temperature conditions,14 energy transfer investigations within Bi3+/Mn4+ (ref. 15) and Bi3+/Tb3+ (ref. 16) co-doped systems, and spectral optimization for near-UV-pumped white-light-emitting diodes.3
Fu et al.2 demonstrated that Bi3+-activated CaYGaO4 synthesised with partial Y3+ substitution and Li2CO3 flux exhibited a broad emission centred at 435 nm and a PLQY of 47.5%.2 Considering the minimal difference in ionic radii between Ca2+ (1.00 Å) and Bi3+ (1.03 Å), it is plausible that Bi3+ may also occupy Ca2+ sites within the crystal lattice. Based on this assumption, the present study adopts a targeted substitution approach by introducing Bi3+ at a fixed concentration of 0.5%, yielding the Ca0.995YGaO4:0.5%Bi3+ phosphor. Unlike the approach taken by Fu et al.,2 the present synthesis was performed under Ca2+ stoichiometric deficiency rather than Y3+ deficiency, offering new insight into site occupancy and its influence on luminescent behaviour.
In addition, this study also explores the emergence of Bi2+-related luminescence in the far red as a secondary phenomenon, offering deeper insight into possible mixed-valence states and charge compensation mechanisms within the Ca0.995YGaO4:0.5%Bi3+ system.
Flux-assisted synthesis plays a critical role in optimizing crystallographic quality and luminescent behaviour, particularly in cases involving aliovalent substitution (Bi3+ → Ca2+). Lithium-based fluxes, e.g. Li2CO3, have demonstrated success in promoting phase purity and suppressing oxygen-related defects, thereby enhancing PLQY and overall emission performance.2,17 The choice of flux agent is thus a key parameter in material synthesis.18
Lithium-based fluxes have not been widely employed in CaYGaO4 and related layered gallates due to their volatility, pronounced chemical reactivity, and tendency to induce secondary phases or unpredictable defect states. However, recent studies by Fu et al.2 demonstrate that, when carefully optimized, Li-based fluxes can significantly enhance crystallinity and reduce oxygen-related defects, thereby improving photoluminescence efficiency.
While Li2CO3 is widely adopted, Li2O remains comparatively underexplored in the context of oxide phosphor development. Its distinct chemical properties may influence phase formation, particle morphology, and defect dynamics in ways not yet fully understood warranting further investigation into its role as an alternative flux.
Its inclusion may influence phase formation, particle morphology, and defect behaviour. Exploring the use of Li2O as an alternative flux to Li2CO3 provides a valuable opportunity to enhance our understanding of flux chemistry and its impact on photophysical properties.
Although lithium flux–assisted enhancement of Bi3+ emission has been reported before, our work is novel in revealing that lithium fluxes not only improve crystallinity but also suppress oxygen-related defects, stabilize Bi3+/Bi2+ coexistence, and promote Bi3+ substitution at Ca2+ sites, thereby unlocking dual emissions and record-high photoluminescence efficiency in CaYGaO4.
Therefore, this work aims to determine whether Ca0.995YGaO4:0.5%Bi3+ phosphors synthesised using Li2CO3 and Li2O exhibit distinct differences in crystal structure, PLQY, and emission intensity. Specifically, it examines how flux agents affect structural refinement, defect states, and particle morphology through charge compensation and substitution mechanisms. To this end, the samples were synthesised via a conventional solid-state reaction method. Their structural and optical properties were systematically investigated using X-ray diffraction (XRD) combined with Rietveld refinement, X-ray photoelectron spectroscopy (XPS), and scanning electron microscopy (SEM). Photoluminescence characterization, including measurements of the absolute PLQY, was also performed to evaluate the emission efficiency.
Surface morphology and particle size were analysed using SEM – Zeiss SUPRA 60VP system equipped with a secondary electron detector (SE-II). Prior to imaging, samples were sputter-coated with a thin gold layer to improve conductivity and minimise charging effects.
XPS measurements were performed using a PHI Quantes Scanning Dual X-ray Microprobe equipped with a monochromatic Al Kα source (hν = 1486.6 eV). Spectra were acquired under ultra-high vacuum conditions (base pressure: 8.4 × 10−10 Torr) with a pass energy of 26 eV, yielding a photoelectron energy resolution of ≤0.4 eV. The analysis focused on the O 1s core level to assess changes in oxygen-related defects and electronic environments. Peak fitting for excitation spectra and XPS data was performed using Origin 2023 software, applying a Gaussian function for spectral fitting.
Particle size distribution was measured using a Fritsch Analysette 22 NeXT Nano laser particle sizer, with a measurement range of 0.01 to 3800 µm.
The absolute PLQY was measured using a custom-built optical setup incorporating an integrating sphere (LabSphere Inc), similar to that described previously.19 Samples were excited with low-power UV LEDs (325 nm and 365 nm, Roithner GmbH), and the emitted light was collected with a spectrometer (AvaSpec-ULS2048 × 64TEC-EVO, Avantes BV) via an optical fibre (BFY200MS02, Thorlabs Inc.). The PLQY system was irradiance-calibrated using a deuterium–halogen lamp (AvaLight DH-S, Avantes BV) and wavelength-calibrated with a Mercury–Argon calibration light source (HG-1, Ocean Optics). Samples were mounted in a quartz sheet holder (QGA33, Aireka Scientific) to avoid parasitic UV absorption. Data acquisition and spectral integration were semi-automated using a LabVIEW routine, and PLQY values were calculated following the DeMello procedure.20 Replicate measurements were not performed; values are therefore reported as single calibrated determinations.
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Given the potential for Bi3+, Bi2+, and Li+ to occupy various polyhedral sites within the Ca0.995YGaO4 lattice, substitutional feasibility was assessed for Ca2+, Y3+, and Ga3+ positions. As summarised in Table 1, substitutions at Ca2+ and Y3+ sites fall within the acceptable mismatch threshold (Dr < 30%), indicating favourable lattice integration. In contrast, Ga3+ site substitutions exhibit excessive mismatch, suggesting likely lattice disruption. Li+ ions similarly favour Ca2+ and Y3+ sites due to more compatible ionic radii.
| Host cation (CN) radii (Å) | Dopant (CN) radii (Å) | D r (%) |
|---|---|---|
| Ca2+ (6) 1.00 | Bi3+ (6) 1.03 | 3.0 |
| Bi2+ (6) 1.17 | 17 | |
| Li+ (6) 0.76 | 24 | |
| Y3+ (6) 0.90 | Bi3+ (6) 1.03 | 14.4 |
| Bi2+ (6) 1.17 | 30 | |
| Li+ (6) 0.76 | 15 | |
| Ga3+ (4) 0.47 | Bi3+ (4) 0.96 | 51 |
| Bi2+ (4) 1.31 | 101.5 | |
| Li+ (4) 0.73 | 55 | |
For the charge-compensation mechanism in CaYGaO4, substitution of Bi2+/Bi3+ ions at Ca2+ sites introduce a charge imbalance that must be compensated to preserve electrostatic neutrality. Several compensation pathways have been reported in the literature (e.g., Wang et al.3 for CaYGaO4; Puchalska et al.23 for Bi substitution in SrAl4O7; Yousif et al. for Bi substitution in CaO12). The dominant mechanisms can be summarised as follows. Substitution of Bi3+ at Ca2+ sites generate a +1-excess charge, which may be compensated either by Ca vacancies
or by oxygen interstitials
. Bi3+ substitution at Y3+ sites are isovalent and therefore does not require charge compensation. In contrast, Bi2+ can replace Ca2+ directly in an isovalent manner, and the emergence of Bi2+-related red/NIR emission in our samples supports the presence of such centres. The O 1s XPS analysis further shows that Li2CO3 suppresses vacancy-related oxygen species, indicating that Li+ assists charge compensation and stabilises mixed Bi3+/Bi2+ incorporation, consistent with the enhanced PLQY.
Although our present work is experimentally focused with a fixed Bi3+ doping concentration of 0.5%, previous density functional theory (DFT) studies have demonstrated that Bi3+/Bi2+ site occupation and flux chemistry strongly influence band structure, band gap, and charge density Ogawa et al.,24 Ahmed et al.25 These reports provide theoretical precedent supporting our interpretation of flux-assisted site substitution and defect compensation.
For Li2CO3-treated samples, the CaYGaO4 phase persists up to 2.0 wt%. At 2.5 wt%, a new diffraction peak emerges near 29.6° marked with a red asterisk in Fig. 1(a) attributed to CaCO3 based on ICSD PDF no. 01-070-0095 (see Fig. S1). This phase may be stabilised or modified by Bi2+ incorporation under CO2-rich synthesis conditions, potentially contributing to deep red luminescence (see Luminescence section).
The Li2O-treated samples displayed in Fig. 1(b) retain well-defined crystalline patterns at 0.5 wt% and 1.0 wt%. At higher Li2O levels, diffraction peaks shift slightly toward higher 2θ angles, indicating possible Li+ incorporation via interstitial sites or cation substitution in oxide phosphor hosts (lanthanum oxycarbonate,17 rare-earth oxides such as Y2O3:Eu3+,18 and related oxides26).
A distinct peak at 30.15° appears at 1.5 wt% Li2O (marked with a red asterisk), matching ICSD PDF no. 121813, corresponding to the (Ca12Ga14O33)1.667 phase (Fig. S3).
The divergence in secondary phase formation between Li2CO3 and Li2O likely reflects their distinct chemical behaviour. Li2CO3 decomposes at higher temperatures than CaCO3 and releases CO2; however, due to its relatively low concentration and delayed decomposition onset, it is unlikely to significantly stabilise CaCO3 during calcination. In contrast, Li2O being carbonate-free and strongly basic favours oxygen-rich environments that promote the formation of complex oxides such as (Ca12Ga14O33)1.667.
To further evaluate the crystal structure, Rietveld refinement was performed. Representative refinement profiles for 2.0 wt% Li2CO3 and 1.0 wt% Li2O-treated samples are shown in Fig. 1(c) and (d), respectively. The models demonstrate excellent agreement between experimental and calculated patterns, confirming structural fidelity and phase purity. The extracted lattice parameters and reliability indices are provided in Table S1 of the SI.
The crystal structure of CaYGaO4, is illustrated in Fig. 2, featuring three distinct cationic sites occupied by Ca2+, Y3+, and Ga3+. The Ca2+ and Y3+ ions reside in separate octahedral environments (A1 and A2), while Ga3+ occupies tetrahedral A3 sites. The distorted CaO610− octahedra form infinite edge-sharing chains along the b-axis, whereas corner-sharing YO69− octahedra extend perpendicular to the a-axis, producing puckered layers. Interstitial GaO45− tetrahedra fill voids between octahedra but remain spatially isolated, lacking direct connectivity. Energetically, low-valent cations like Ca2+ favour edge-sharing sites due to shorter A–A distances, minimizing Coulombic repulsion and stabilizing the lattice.27 In contrast, smaller trivalent cations such as Y3+ are stabilised in corner-sharing environments, consistent with crystallographic ordering based on ionic radius and charge differentiation.1,2
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| Fig. 2 The crystal structure of CaYGaO4 adopts an olivine-type framework with orthorhombic symmetry (space group Pnma, no. 62). Ca2+ and Y3+ ions occupy octahedral sites, each coordinated by six oxygen atoms to form [CaO6] and [YO6] units, respectively. Ga3+ ions reside in tetrahedral sites, coordinated by four oxygen atoms to form [GaO4] units.1 | ||
Fig. 4 presents SEM images of Ca0.995YGaO4:0.5%Bi3+ samples synthesised under flux-free conditions and with lithium-based flux treatments. The particle morphologies show a clear dependence on flux type, with mixtures of small and large irregular agglomerates exhibiting varied grain compactness and generally smooth surfaces. As indicated by blue markers, no pores or molten spherical particles are observed in flux-free samples. In contrast, soft, molten-like spherical particles and visible pores are evident in samples treated with Li2CO3 flux, suggesting distinct microstructural modifications. These features are absent in samples synthesised using Li2O flux, underscoring a flux-specific influence on particle formation. Pore formation may result from a secondary phase, associated with CaCO3 stabilised by Bi3+ and Li2CO3, migrating to the surface. Alternatively, it may be caused by the evaporation of lithium and other volatile species during high-temperature synthesis.
![]() | (2) |
Samples exhibiting higher area ratios indicative of a lower concentration of vacancy-related oxygen species tend to demonstrate enhanced PLQY, as will be discussed in the luminescence section. This correlation underscores the critical role of oxygen-related defects in governing the optical performance of the material.
Fig. 6(a)–(c) shows the O 1s spectra of the Li2O flux samples, and Fig. 6(d) presents the corresponding lattice to defect oxygen area ratios. The 0.5% and 1.0% Li2O samples exhibit low ratios, indicating a high concentration of oxygen related defects. In contrast, the 1.5% Li2O sample shows a marked increase in this ratio, reflecting a substantial reduction in defect density. This improvement is likely linked to enhanced mass transport and crystallization at higher Li2O loading particularly as samples above 1.5% Li2O begin to show partial melting which promotes more complete oxygen incorporation and suppresses vacancy formation. The secondary phase detected by XRD at 1.5% Li2O may further stabilize oxygen stoichiometry.
When comparing the O 1s area-ratio trends of the Li2O and Li2CO3 flux samples, the behaviour differs: low Li2O concentrations lead to higher defect levels, whereas Li2CO3 at low concentration effectively suppresses defects.
At higher Li2O loading the defect density decreases, while for Li2CO3 the defect-related oxygen component increases again at higher flux concentration.
In summary, the O 1s XPS analysis demonstrates that both Li2CO3 and Li2O fluxes modulate oxygen-related defects, but through distinct concentration dependent mechanisms. In the Li2CO3 system, defect suppression is most effective at moderate loading (1.5%), whereas higher concentrations lead to a resurgence of vacancy-related oxygen species. By contrast, the Li2O system exhibits a high defect density at low loadings (0.5–1.0%), followed by a pronounced reduction at 1.5%, consistent with flux-mediated partial melting and enhanced mass transport that promote more complete oxygen incorporation. The observed decrease in vacancy-related oxygen components at these optimal concentrations correlates directly with the enhancement in PLQY, confirming that the suppression of non-radiative recombination centres particularly oxygen vacancies is a key mechanism by which lithium-based fluxes improve the luminescence efficiency of CaYGaO4:Bi3+ phosphors.
Fig. 7(b) illustrates the impact of lithium-based fluxes Li2O and Li2CO3 on the blue emission intensity of Ca0.995YGaO4:0.5%Bi3+ phosphors under 330 nm excitation. Both fluxes enhance emission up to an optimal concentration, beyond which a decline is observed. This behaviour indicates that moderate flux concentration promotes improved crystallinity and favourable local coordination, while excessive flux leads to defect formation and emission quenching, as evidenced by the structural insights presented in Section 3.4 based on XPS analysis. The optimal enhancement concentration differs between the fluxes, reflecting distinct fluxing efficiencies and lattice interactions.
Fu et al.2 reported a comparable enhancement in photoluminescence (PL) intensity with the use of Li2CO3 flux, demonstrating its effectiveness in boosting blue PL emission in CaY0.995GaO4:0.5%Bi3+ phosphors under near-UV excitation.2 Their findings showed a ∼1.5-fold increase in emission intensity over the pristine sample at optimal Li2CO3 content, attributed to reduced surface defects, improved crystallinity, and enhanced Bi3+ incorporation into the host lattice. In the present study, a distinct synthesis approach based on calcium deficiency yields a significantly greater PL enhancement. Specifically, the inclusion of 1 wt% Li2O results in a 1.9-fold increase in emission intensity, and 2 wt% Li2CO3 leads to an even more notable ∼2.2-fold improvement relative to the pristine sample. These results indicate a synergistic effect between Ca-deficient synthesis and lithium flux, surpassing earlier PL enhancement reports and offering a promising new strategy for optimizing Bi3+-activated phosphors. This contrast highlights the varying fluxing capacities of Li2O and Li2CO3, and underscores their distinct roles in modulating the luminescence properties of Ca0.995YGaO4:0.5%Bi3+. This enhancement is attributed to lattice modification and charge compensation, where Li+ ions facilitate Bi3+ substitution at Ca2+ lattice sites and mitigate non-radiative recombination by correcting aliovalent charge imbalance.29
Lithium carbonate flux profoundly influence Bi3+-doped CaYGaO4 phosphors, with Li2CO3 enabling record-high PLQY and Li2O promoting alternative oxide phases. These findings highlight flux chemistry as a versatile tool for engineering efficient blue emitters.
To elucidate the behaviour of the excitation bands, the normalized excitation spectra were decomposed into Gaussian components for all synthesis conditions, including the two lithium-based fluxes and the flux-free sample. Fig. 7(a) shows the Gaussian fitting for the flux-free sample, while Fig. 7(b) illustrates the variation in peak areas as a function of lithium-flux concentration. Fig. 8(c)–(f) display the corresponding decomposed components for the samples synthesized with lithium-based fluxes. The area of each peak was calculated and normalized to the total integrated area of all three peaks, allowing a direct comparison of the relative contributions of the deconvoluted components.
In these figures, the red dotted line represents the cumulative fit obtained from the superposition of the three Gaussian components, which closely reproduces the experimental spectrum shown in black. Based on the fitted peaks, the following assignments are proposed:
peak 1 (4.0 eV): 1S0 → 3P1 transition of Bi3+ ions in low-symmetry environments, likely corresponding to Bi3+ substituting Y3+ sites.2
Peak 2 (3.7 eV): dipole-allowed 1S0 → 3P1 transition associated with Bi3+ ions occupying Ca2+ lattice sites.2
Peak 3 (3.4 eV): excitation involving defect-related localized states near Bi3+ ions. This region may also overlap with Bi2+ excitation, as experimental result represented in Fig. 8(a), which will be discussed later.
As shown in Fig. 8(b), the flux-free sample is dominated by peaks 1 and 3, indicating that excitation primarily involves Bi3+ ions on Y3+ sites and defect-mediated localized states. Upon the introduction of Li2CO3 flux, the relative area of peak 1 decreases, while peak 2 becomes increasingly dominant, suggesting that Li+ promotes the incorporation of Bi3+ into Ca2+ lattice sites where the local symmetry favors efficient dipole-allowed transitions. This behaviour is attributed to the ability of Li+ ions to provide charge compensation, thereby reducing cation vacancies and facilitating the incorporation of additional Bi3+ ions into the host lattice, consistent with the findings of Wang et al.3
The area of peak 3 initially decreases, reaching a minimum at the Li2CO3 concentration corresponding to the highest photoluminescence (PL) intensity, indicating reduced defect-mediated excitation. At higher Li2CO3 concentrations, however, peak 3 increases again, implying that excess Li+ introduces additional defects that promote non-radiative pathways or trap-state formation.
In the case of Li2O flux, Li2O concentrations above 1.5 wt% could not be employed due to sample melting. Within the accessible Li2O concentration range, peak 1 shows a decreasing normalized area as Li2O concentration increases up to 1 wt%, after which it begins to rise, indicating the Li2O flux-induced enhancement of luminescent centers where Bi3+ occupies Y3+ lattice sites. Peak 2 exhibits a strong increase in normalized area at 1 wt% Li2O, followed by a decrease, suggesting that Li+ promotes the incorporation of Bi3+ into Ca2+ lattice sites at lower Li2O concentrations compared with Li2CO3. The area of peak 3 shows a slight decrease with increasing Li2O concentration, indicating a modest reduction in the defect-mediated excitation band in Li2O samples as concentration rises.
Taken together, these trends show that the two lithium fluxes modulate Bi3+ site occupancy and the defect landscape in distinct ways, thereby controlling the balance between radiative and non-radiative excitation pathways. The behaviour of peak 3, associated with defect-related excitation, aligns with the XPS findings in Section 3.4. Overall, the results indicate that lithium-based fluxes tune the excitation dynamics by altering Bi3+ site occupancy and the local lattice environment. Gaussian deconvolution is used here only as a phenomenological aid; the mechanistic interpretation is supported by the combined evidence from PL, XPS, PLQY, and the literature rather than deconvolution alone.
As shown in Fig. 9(b), the intensity of the 780 nm emission depends on the lithium flux content. Notably, phosphors treated with 1 wt% Li2O and 2 wt% Li2CO3 exhibit enhancements of approximately 2.8-fold and 2.5-fold, respectively, compared to the pristine sample. The second component, centred at 720 nm, emerges under excitation at 360 and 480 nm, suggesting that Bi2+ ions in alternative coordination environments also contribute to the luminescence. This interpretation is further supported by the appearance of an additional XRD diffraction peak, tentatively attributed to a secondary phase such as CaCO3:Bi2+,Li+, implying partial segregation or stabilization of Bi2+ within a carbonate-rich environment promoted by lithium flux incorporation.
Although the emission from Bi2+ as a red and NIR emitter under appropriate excitation conditions has been well documented across various host matrices and excitation sources (see Table 2). However, this behaviour has not yet been reported for the CaYGaO4 host.
For our sample with an absorptance measured in the integrating sphere of 17%, the PLQY error was estimated following the method of Madirov et al.19 For this absorbance, the relative error is expected to be ∼5%, which is also consistent with relative uncertainty of 3.4% for replicated measurements reported by Bhiri et al. for YPO4:Yb3+,Er3+ phosphors with a slightly higher absorptance of ∼30%.32
The PLQY of the 2.5% Li2CO3 sample was measured to be 45% (Fig. 5), consistent with the earlier explanation that higher flux concentrations promote defect formation. Beyond the 1.5% level, further increases in Li2CO3 resulted in a progressive decline in PLQY, most likely due to the generation of additional non-radiative defects and flux-induced quenching effects. This behaviour highlights the critical importance of maintaining an optimal flux concentration to balance defect passivation with luminescence efficiency. The PLQY improvement associated with Li2CO3 is attributed to enhanced crystallinity and a reduced density of non-radiative defects, as confirmed by XRD and XPS analyses discussed earlier. In contrast, Li2O appears to induce lattice distortions and promote defect states that act as quenching centres, thereby suppressing PLQY. This disparity likely arises from the higher defect concentration introduced during flux-assisted synthesis. Although direct crystallographic evidence of Bi site substitution and Bi2+ formation is challenging, complementary PL, XPS, and PLQY observations converge to support these mechanisms. Our results show that Li2CO3 uniquely suppresses oxygen defects, stabilises Bi3+/Bi2+ coexistence, and enables dual emission, whereas Li2O fails to achieve these effects. This establishes a previously unreported mechanistic link between flux chemistry and photophysical behaviour in CaYGaO4. The beneficial role of lithium fluxes, particularly Li2CO3, is well supported in the literature for other host systems. Notably, Kim et al. demonstrated that Li2CO3 acts as a self-purifying flux, significantly improving crystallinity in Ba2SiO4:Eu2+ phosphors by removing impurities from low-grade starting materials.33
A comparative summary of PLQY values for Bi3+-doped gallates is presented in Table 3, highlighting the superior performance of the current material. Reported PLQY values for Bi3+-activated gallate phosphors exhibiting structural similarity to CaYGaO4 including BaLaGaO4, SrLaGaO4, and CaLaGaO4 further underscore the relevance of host lattice design. These compounds are known to exhibit blue-region luminescence, and their PLQY benchmarks provide a meaningful context for evaluating the efficiency of CaYGaO4-based systems.
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