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Article

Medium- and High-Entropy Rare Earth Hexaborides with Enhanced Solar Energy Absorption and Infrared Emissivity

1
College of Chemistry and Materials Science, Fujian Normal University, Fuzhou 350117, China
2
Fujian Institute of Research on the Structure of Matter, Chinese Academy of Sciences, Fuzhou 350002, China
3
Xiamen Institute of Rare Earth Materials, Haixi Institute, Chinese Academy of Sciences, Xiamen 361021, China
4
Fujian Science & Technology Innovation Laboratory for Optoelectronic Information of China, Fuzhou 350108, China
5
Xiamen Key Laboratory of Rare Earth Photoelectric Functional Materials, Xiamen Institute of Rare Earth Materials, Haixi Institute, Chinese Academy of Sciences, Xiamen 361021, China
6
Key Laboratory of Rare Earths, Ganjiang Innovation Academy, Chinese Academy of Sciences, Ganzhou 341000, China
*
Authors to whom correspondence should be addressed.
Materials 2024, 17(8), 1789; https://doi.org/10.3390/ma17081789
Submission received: 5 March 2024 / Revised: 10 April 2024 / Accepted: 10 April 2024 / Published: 12 April 2024
(This article belongs to the Special Issue Design, Processing and Properties of High Entropy Ceramics)

Abstract

:
The development of a new generation of solid particle solar receivers (SPSRs) with high solar absorptivity (0.28–2.5 μm) and high infrared emissivity (1–22 μm) is crucial and has attracted much attention for the attainment of the goals of “peak carbon” and “carbon neutrality”. To achieve the modulation of infrared emission and solar absorptivity, two types of medium- and high-entropy rare-earth hexaboride (ME/HEREB6) ceramics, (La0.25Sm0.25Ce0.25Eu0.25)B6 (MEREB6) and (La0.2Sm0.2Ce0.2Eu0.2Ba0.2)B6 (HEREB6), with severe lattice distortions were synthesized using a high-temperature solid-phase method. Compared to single-phase lanthanum hexaboride (LaB6), HEREB6 ceramics show an increase in solar absorptivity from 54.06% to 87.75% in the range of 0.28–2.5 μm and an increase in infrared emissivity from 76.19% to 89.96% in the 1–22 μm wavelength range. On the one hand, decreasing the free electron concentration and the plasma frequency reduces the reflection and ultimately increases the solar absorptivity. On the other hand, the lattice distortion induces changes in the B–B bond length, leading to significant changes in the Raman scattering spectrum, which affects the damping constant and ultimately increases the infrared emissivity. In conclusion, the multicomponent design can effectively improve the solar energy absorption and heat transfer capacity of ME/HEREB6, thus providing a new avenue for the development of solid particles.

1. Introduction

The efficient utilization of solar energy has become a key means of achieving the goals of “carbon neutrality” and “carbon peak” [1]. Concentrated solar power (CSP) is a type of electricity generation that captures solar energy and uses it directly as a heat source for the electricity cycle. For third-generation CSP, molten salts, solid particles, and gases are candidates for the capture of solar energy [2,3]. As a key component of a solid particle solar receiver (SPSR) [4,5], solid particles not only heat themselves from concentrated sunlight but also act as a heat transfer medium to transfer heat to the back-end for power generation. Direct solar absorption based on solid particles and their use as heat transfer mediums (HTMs) has attracted increased interest as potential high-temperature CSP. The ideal particles should have high solar absorptivity (0.28–2.5 μm) and high infrared emissivity (1–22 μm) [6,7,8,9]. The absorption of solar radiation is an important part of the photothermal conversion process. High absorption in the visible and near-infrared spectra is essential for ensuring the efficient operation of solar concentrators. Moreover, high emissivity in the infrared range is necessary to exchange the absorbed energy of the falling particles with the fluid in the form of infrared radiation in the thermal exchanger. This approach simplifies the complexity of concentrated solar power systems and achieves the integration of heat absorption and thermal radiation in the particulate medium. Currently, various solid particles, including mullite [10], sand [11], quartz [9], silica sand [6,12,13], alumina [6,14,15], and olivine [16], can be used as heat transfer mediums (HTMs) in receivers [17]. However, current conventional particulate heat absorbers suffer from low heat absorption and heat transfer performance. Therefore, new materials with high solar absorptivity and high infrared emissivity need to be developed to solve the problems of heat absorption and transfer.
Rare-earth hexaborides (REB6) have a special crystal structure of the CsCl-type. On the one hand, the special boron network structure and the dominance of strong B–B bonds provide excellent properties of a low work function, high thermal stability, high mechanical strength, and high melting point [18,19,20,21]. On the other hand, the thermal, electrical, magnetic, and optical properties are significantly influenced by the presence of La metal atoms embedded within a stable boron octahedron network [22]. Elisa Sani et al. investigated the spectral reflectance and thermal emissivity of single-phase LaB6 and LaB6-ZrB2-SiC composites and found that LaB6 had the potential to be used as a high-temperature direct solar absorber [23]. LaB6 particles possess excellent optical properties and high thermal stability; thus, they are a suitable choice for SPSRs. However, the lower emissivity of LaB6 [23] does not meet the requirements of heat transfer mediums (HTMs). In order to simultaneously possess solar absorption and back-end heat dissipation, it is necessary for the material to have a high solar absorptance and infrared emittance. Therefore, the solar absorptance and infrared emittance of LaB6 need to be increased by other means.
In recent years, high-entropy ceramics (HECs), which are novel materials with no less than five equimolar metal cations or anions [24], have been the focus of much research. Various HECs have been successively designed and developed [21,25,26,27,28,29,30,31,32,33]. The use of highentropy provides a new strategy for tailoring materials properties. This approach is an effective means of modulating the emissivity of materials. Zhou et al. synthesized (La0.2Nd0.2Gd0.2Sm0.2Pr0.2)MgAl11O9 and found that it had a much higher infrared emissivity than LaMgAl11O9 [34]. Wang et al. synthesized La(Fe0.2Co0.2Ni0.2Cr0.2Mn0.2)O3 ceramics, which exhibited an emissivity of up to 92% in the range from 0.76 to 2.50 μm [35]. Song et al. designed and synthesized high-entropy transition metal disilicides and the higher infrared emissivity was due to the increase in phonon scattering caused by lattice distortion; this reduced the thermal and electrical conductivity of the lattice and ultimately increased its infrared emissivity [36]. Consequently, to control infrared emissivity and solar absorptivity, the high-entropy strategy is an effective method. However, the application of HEREB6 ceramic particles for solar energy absorption has not been reported. Therefore, the high-entropy design is expected to improve the solar absorptivity and infrared emissivity of LaB6, providing a new strategy for the development of SPSRs.
In this study, we aimed to improve the solar absorptivity and infrared emissivity by designing and synthesizing two ME/HEREB6 of (La0.25Sm0.25Ce0.25Eu0.25)B6 (MEREB6) and (La0.2Sm0.2Ce0.2Eu0.2Ba0.2)B6 (HEREB6) by a high-temperature solid phase method using a multicomponent design strategy. The phase composition and morphology of these HEREB6 were analyzed and the effects of composition and lattice distortion on their solar absorptivities and infrared emissivities were systematically investigated. Their solar absorptivity and infrared emissivity were systematically compared with those of single-phase LaB6. High entropy was found to be an effective means of overcoming the shortcomings of LaB6. The results show that ME/HEREB6 exhibited high infrared emissivity and high solar absorptivity; thus, a multicomponent design provides a novel approach to the development of solar energy materials.

2. Experimental

2.1. Composition Design

To demonstrate the influence of the multicomponent design on the solar absorption and infrared emissivity of metal hexaborides, using LaB6 as the base, MEREB6 and HEREB6 were designed and synthesized via a high-temperature solid-phase method based on the atomic size difference as the primary criterion. The choice of Ce is due to the small difference between the atomic radius and La, while the selection of Sm, Eu, and Ba is made to reduce the free electron concentration by introducing variable-valence ions or divalent ions.
The average size difference between medium- and high-entropy rare earth hexaborides can be expressed as Equation (1)
δ r = i = 1 n r i 1 - r i / ( i = 1 n x i r i ) 2
where n is the number of metal components, xi is the molar fraction of the ith component of the metal, and ri represents the atomic radius of the ith component of the metal.
The configuration entropy of medium- and high-entropy rare earth hexaborides can be expressed as Equation (2)
Δ S c o n f = R i = 1 n x i ln x i
where R is the gas constant, n is the number of metal components, and xi is the molar fraction of the ith component of the metal.
The average size difference and configuration entropy are shown in Table 1, the average size differences between MEREB6 and HEREB6 are 2.58% and 3.95%, respectively. Moreover, the entropy values of MEREB6 and HEREB6 are 1.3863R and 1.6094R, respectively.

2.2. Materials and Methods

Three ceramic materials, LaB6, (La0.25Sm0.25Ce0.25Eu0.25)B6 (MEREB6), and (La0.2Sm0.2Ce0.2Eu0.2Ba0.2)B6 (HEREB6), were synthesized by a high-temperature solid-state reaction method. Commercially available lanthanum oxide (La2O3, ≥99.99%), samarium oxide (Sm2O3, ≥99.99%), cerium oxide (CeO2, ≥99.5%), europium oxide, (Eu2O3, ≥99.99%), barium carbonate (BaCO3, ≥99.95%), and boron carbide (B4C, ≥98%, ≥200 mesh) were purchased from Aladdin (Aladdin Biochemical Technology Co., Ltd., Shanghai, China) as raw materials. ME/HEREB6 powder was prepared by mixing four rare earth oxide powders and barium carbonate powder with B4C powder in the desired stoichiometric ratio. The initial stage of the boron carbide reduction process leads to the formation of rare earth borates as an intermediate phase with the reaction equation shown in Equations (3)–(8) [37], where RE denotes La, Sm, Ce, and Eu.
4 RE 2 O 3 + 7 B 4 C = 4 REBO 3 + REB 6 + 7 C
4 REBO 3 + 7 C + 5 B 4 C = 4 REB 6 + 12 CO
( 3 ) + ( 4 ) : 4 RE 2 O 3 + 12 B 4 C = 5 REB 6 + 12 CO
6 CeO 2 + 4 B 4 C = 4 CeBO 3 + 2 CeB 6 + 4 C
4 CeBO 3 + 4 C + 5 B 4 C = 4 CeB 6 + 9 CO + 3 2 O 2
( 6 ) + ( 7 ) : 6 CeO 2 + 9 B 4 C = 6 CeB 6 + 9 CO + 3 2 O 2
However, Ba, as a neighboring element of La, was prepared in this study using the same mechanism as REB6. Since BaO reacts readily with water and carbon dioxide in the air to form BaCO3, BaCO3 was chosen as the Ba source for the experiment. Therefore, the initial stage of its reaction may also form an alkaline earth borate [38] intermediate phase and the reaction equation is shown in Equations (9)–(11):
2 BaCO 3 + 2 B 4 C = BaB 2 O 4 + BaB 6 + 2 C + 2 CO
BaB 2 O 4 + 2 C + B 4 C = BaB 6 + 3 CO + 1 2 O 2
( 9 ) + ( 10 ) : 2 BaCO 3 + 3 B 4 C = 2 BaB 6 + 5 CO + 1 2 O 2
In particular, the molar ratio of reactants is listed in Table 2.
These powders were weighed and transferred to an agate mortar in a stoichiometric ratio according to the composition of the target. Then, the mixture was ground by hand for 1 h until it was thoroughly mixed. The mixture obtained was kept at a pressure of 5 MPa for 30 s and then pressed into green bodies 20 mm in diameter. The green bodies were then placed in a graphite crucible in a tube furnace and argon gas was passed through the crucible for a period to ensure air removal. The green bodies were then heated to 1600 °C in an argon atmosphere at a heating rate of 5 °C/min and held for 2 h. The samples were cooled to 1000 °C (again at a rate of 5 °C/min) and then cooled in the furnace. Finally, all calcined samples were ground once again to obtain a fine powder.

2.3. Analysis and Characterization

The phase structures of LaB6 and ME/HEREB6 were identified with an X-ray diffractometer (XRD, Miniflex 600, Rigaku, Japan) over the range of 15–105° (2θ degree) with Cu Kα radiation (λ = 1.5406 Å) at a scanning rate of 1°/min and a step size of 0.02. Rietveld refinement was used to extract the phase structure information from the XRD data with the aid of Fullprof software 2024 [39]. The microstructure and elemental distribution of the samples were analyzed using field emission transmission electron microscopy (FTTEM, Talos F200s, Thermo Fisher Scientific, Waltham, MA, USA) in combination with an energy dispersive spectroscopy (EDS) system. The Raman spectra of the samples were collected with a LabRAM Aramis (Horiba Jobin Yvon S.A.S., Palaiseau, France) automated scanning confocal Raman microscope excited using a laser wavelength of 532 nm. The optical reflectance properties were measured with a UV–vis–NIR spectrophotometer (Carry 5000, Agilent Technologies Ltd., Santa Clara, CA, USA) equipped with a 110 mm InGaAs integrating sphere in the wavelength range from 0.28 to 2.5 μm; barium sulfate was used as a reference. The normal infrared emissivity of all of the samples in the range of 1–22 μm was measured using a dual-band infrared emissivity meter (IR-2, Chengbo Optoelectronics Technology Co., Ltd., Shanghai, China).

3. Results and Discussion

3.1. Phase Composition and Microstructure

As shown in Figure 1, the crystal structure of CsCl-type rare earth hexaborides (REB6) is cubic with a space group of Pm-3 m (No. 221), the Wyckoff sites of rare earth in 1a (0, 0, 0), and boron elements in 6f (0.5, 0.5, z); here, the position parameter z of the B atom is related to the lattice parameter (a) and the B-B bond lengths [40]. Furthermore, the structure of REB6 is a compound consisting of ionic and covalent bonds, where the RE-RE bond is ionic, the RE-B bond is intermediate between ionic and covalent bonds, and the B-B bond is covalent [41]. Moreover, the strength of the σ-bonds between the octahedra (B-Binter) exceeds that of the τ-bonds within octahedra (B-Bintra) [42]. In addition, the lattice parameters can be modified by varying the length of the inter-octahedral σ bonds (B-Binter) and intra-octahedral τ bonds (B-Bintra) [43]. Changes in the B-B bond length can have a significant effect on the optical properties, resulting in an improvement in the infrared emissivity. The variations in the B-Binter and B-Bintra distance spacings significantly impact on the optical properties, resulting in enhanced infrared emissivity. The optical properties of high-entropy REB6 are excellent and this improvement may be attributed to changes in the lattice distortion [36,44] and the free electron concentration. However, the boron sublattice in hexaborides is charge deficient and the number of deficient electrons has been experimentally and theoretically determined to be 2 [45]. Therefore, a metal cation with at least a +2 charge must be present to maintain electronic stability. However, the REB6 compound family includes trivalent rare earth ions such as La, Ce, Pr, and Nd, mixed-valent ions such as Sm (approximately 2.7), divalent ions such as Eu, and divalent alkaline earth elements such as Ca, Sr, and Ba [46,47,48]. Therefore, the free electron concentration can be reduced by introducing divalent or variable valence ions.
Figure 2a shows the XRD patterns of the synthesized LaB6, MEREB6, and HEREB6 powders together with the Standard ICDD/JCPDS cards of LaB6. No significant difference was observed between the XRD patterns of ME/HEREB6 and LaB6. The X-ray diffraction pattern of ME/HEREB6 shows a single solid solution phase. Figure 2b shows the partial enlargement of the (110) peak at 2θ values of 28.5–31.5°. Compared to the peak position of LaB6, the peaks of MEREB6 shifted toward higher 2θ values and HEREB6 shifted toward lower 2θ values. Thus, the lattice constant decreases or increases and these results are consistent with the data in Table 2, which show a reduction in cell parameters after refinement. Variations in the lattice parameters can be attributed to different group element designs, resulting in different degrees of lattice distortion. In addition, the broadening of the main peak of the XRD pattern is also observed, which may be due to grain refinement caused by elemental doping.
The Rietveld method of crystal structure refinement [39] uses a whole-pattern profile fitting technique, which allows the crystal structure information to be obtained from powder X-ray diffraction data. Figure 3a–c displays the XRD Rietveld refinement results for LaB6, MEREB6, and HEREB6. Evidently, the calculated XRD patterns are in good agreement with the experimental patterns. The difference curves (Yobs-Ycal) in Figure 3b,c are smoothed and the χ2 values are less than 4%, indicating that the refinement results are reliable [49]. The difference curves (Yobs-Ycal) in Figure 3a are smoothed and have a slightly higher χ2 value (5.91%) because of the very high precision of the data collected [50]. Therefore, the results from this refinement are also reliable. Moreover, the refined unit-cell parameters and bond lengths for LaB6, MEREB6, and HEREB6 are listed in Table 3.
Figure 4a,d shows the selected region electron diffraction (SAED) plots; here, the clear and regular diffraction spots confirm that MEREB6 and HEREB6 have a CsCl-type crystal structure and high crystallinity. Figure 4b,e shows the typical (110) and (100) lattice plane of the MEREB6 and HEREB6 powders with D-spacings of 0.2972 nm and 0.4236 nm, respectively. These values are similar to the values of 0.2938 nm (110) and 0.4158 nm (100) calculated from the XRD images. Figure 4c, f shows the inverse fast Fourier transforms (IFFTs) of the MEREB6 and HEREB6 images from the dislocations in the white boxed area in Figure 4b,e, respectively. Furthermore, linear dislocation lines, which exist alone or intertwined to form dislocation networks (as shown in Figure 4c,f), are observed [51,52]. The dislocations potentially occur due to the lattice distortion caused by the multi-component design. The MEREB6 and HEREB6 powders were further characterized by HR-TEM. Figure 5a,b shows the high-angle annular dark-field (HAADF) images and corresponding elemental distribution maps of MEREB6 and HEREB6. No apparent segregation of any of the elements was observed and this result provides further evidence of the formation of a uniform single-phase solid solution.

3.2. Lattice Distortion Analysis

In theory, lattice distortion refers to the extent to which the positions of the constituent atoms deviate from the ideal lattice punctures [53]. In addition, fluctuations in the nature of chemical bonding in the crystal structure can also be considered part of the lattice distortion, such as the magnitude of changes in bond angles and bond lengths [54]. The variation in the B-B bond lengths is shown in Table 1. It has been reported that there is a relationship between the infrared emission properties of a material and its lattice strain; thus, to quantify the extent of the lattice distortion [44], the lattice strain of the samples was calculated using the Williamson–Hall formula (Equation (12)) [55]
β cos θ = k λ D + 4 ε sin θ
where β is the half-peak height and width, θ is the diffraction angle, D is the grain size, λ is the wavelength of the Cu Kα radiation source (λ = 1.5406 Å), and ε is the lattice strain. A straight line of βcosθ versus 4sinθ for the samples was fitted from the XRD data. The lattice strains (ε) of the samples were determined from the positive slopes. Figure 6 shows the calculated lattice strains based on Williamson–Hall analysis. A gradual increase in the lattice strain for LaB6, MEREB6, and HEREB6 was observed with values of 0.0299%, 0.0682%, and 0.1550%, respectively, as shown in Figure 6. Clearly, the lattice strain trend is in agreement with the lattice constants listed in Table 1.
Lattice distortion of the major factors influencing the properties of high-entropy materials. In addition, Raman spectroscopy can also verify lattice distortion [56]. The hexaborides of the rare earth elements have a cubic CsCl-type structure with a Pm-3 m space group. According to group theory, a set of allowed vibrational modes of the crystals in the Pm-3m structure is given by Equation (13) [57]:
Γ = A 1 g + E g + T 1 g + T 2 g + 2 T 1 u + T 2 u
where A1g, Eg, and T2g denote the Raman active modes. Figure 7a shows the Raman spectrum of LaB6, where three main peaks were observed at 671.37 cm−1(T2g), 1111.37 cm−1(Eg), and 1234.25 cm−1(A1g); the results were in agreement with previous reports [58,59]. The eigenvectors of these three intramolecular vibrations of the B6 molecules are shown in the inset of Figure 7a. In addition, Eg and A1g correspond to B–B stretching modes and the T2g mode is a B–B–B valence angle bending mode of the boron lattice [57,58,60]. Simultaneously, the T2g peak is blueshifted, the Eg peak is redshifted, and the A1g peaks are initially blueshifted and then redshifted, as shown in Figure 7b. Compared to single-phase LaB6, high-entropy hexaboride powders show a broadening of the Raman peak shape due to the lattice distortion and internal stress.

3.3. Solar Energy Absorption

Figure 8a displays the reflectance and solar irradiance spectra of LaB6, MEREB6, and HEREB6. The reflectance spectra gradually decrease with the doping of rare earth and alkaline earth ions, indicating an increase in absorption. This is due to the change in the plasmon resonance with the free electron concentration. According to the literature, the plasma frequencies of LaB6, SmB6, CeB6, EuB6, and BaB6 are 4.94 eV, 2.61 eV, 4.90 eV, 1.32 eV, and 0.60 eV [61,62], respectively. With the exception of the divalent REB6 (EuB6 and YbB6), the divalent alkaline earth hexaborides (BaB6, SrB6, CaB6, etc.) and SmB6, the number of conduction band electrons per unit cell in trivalent rare-earth hexaborides is one and the Boron-2p bonding bands are filled with two electrons per mole [45]. The conduction band is formed by the rare-earth 5d-Boron 2p bonding band. On the other hand, SmB6 has only 0.6 to 0.7 electrons per mole due to a change in Sm valence, while divalent hexaborides have only a few conduction electrons [63]. Elemental doping reduces the free electron concentration and plasma frequency, resulting in a redshift of the absorbance band. This effectively regulates the near-infrared absorption of the material and enhances its solar energy absorption capacity. In addition, from the room temperature hemispherical reflectance R(λ), the total solar absorptance α can be calculated by Equation (14):
α = λ min λ max ( 1 R ( λ ) ) S ( λ ) d λ λ min λ max S ( λ ) d λ
where λmin = 0.28 μm, λmax = 2.5 μm, and S(λ) is the Sun emission spectrum, which is the standard solar spectral irradiance obtained from ISO Standard 9845-1(2022), AM1.5 [64]. The solar absorption rate calculated according to eq 1 is shown in Figure 8b. With the doping of rare earth and alkaline earth ions in the multicomponent design, the solar absorption rate of the samples gradually increased. The average solar absorption rate increased from 54.05% to 87.75%.

3.4. Infrared Emissivity

The infrared emissivity of a material is one of the most important indicators of its application value providing its ability for infrared radiation emission. According to Kirchhoff’s law [65], the following can be said:
α + r + τ = 1
where α is the absorptivity, τ is the transmittance, and r is the reflectance. Since the sample powders prepared for the test are dark purple and dark blue, they hardly transmit any light radiation, so their transmittance τ is zero, so Equation (16) can be simplified as follows:
α + r = 1
According to Kirchhoff’s law, the emissivity is equal to the absorbance when the material is in thermal Equation (17) as follows:
α = ε
where ε is the infrared emissivity. It can therefore be deduced that for the infrared emissivity ε, the following is true:
ε = 1 r
As shown in Figure 9a, HEREB6 exhibits an average infrared emissivity of 88.76% in the range of 0.76–2.5 μm. Notably, this improvement is remarkable and the emissivity is 1.65 times greater than that of LaB6 (53.64%). Moreover, the high-entropy design effectively addressed the low emissivity limitations of boride ceramics in this band. Figure 9b shows the normal infrared emissivity in the range of 1–22 μm. The infrared emittance of the sample surface at room temperature from 1 to 22 μm was measured by an active blackbody radiation source and the normal reflectance R of the sample surface was determined. According to Kirchhoff’s law, the absorptivity of the object is numerically equal to the emissivity, that is, σ = ε and the normal emissivity ε of the measured object in the infrared band was obtained. The infrared emissivity of the multicomponent design is significantly greater in the 1–22 μm band, with the highest emissivity for the HEREB6 samples reaching 89.96% in the range of 1–22 μm. Moreover, the emissivity of LaB6 is as high as 76.19%. These results indicate that LaB6 has an inherently high infrared emission capability. Clearly, the emissivity increases from 76.19% to 89.96% after the multicomponent design strategy with the rare earth and alkaline earth ions.
REB6 compounds are metal-like conducting ceramic materials with a high concentration of free electron gas containing bound and free electrons and their optical properties in the infrared region are determined by the in-band dielectric function of the dielectric function [36]. The intraband dielectric function is represented using Equation (19)
ε int r a ( ω ) = 1 ω D 2 ω ( ω + i η )
where ωD is the plasma frequency for intraband transitions (Equation (20)) and η is the damping constant of electrons.
ω D 2 = n e e 2 m e f f
where ne is the concentration of the free carrier, e is the elementary charge, and meff is the effective mass of the carrier.
In addition, the electrical conductivity is expressed as (Equation (21)) according to the Drude model for an electron gas.
σ = n e 2 τ m e
where n denotes the electron density, e is the electron charge, me is the electron mass, and τ is the relaxation time. The damping constant of the electrons, the reciprocal of the relaxation time τ, is determined by the electron scattering mechanism, which limits the electrical conductivity. In particular, the electrical conductivity exhibits a negative correlation with η [36,66]. However, much research has shown that high-entropy strategies reduce the conductivity of a material. Moreover, lattice distortion induces changes in the B–B bond length, leading to significant changes in the Raman scattering spectrum, which affects the damping constant. Therefore, high-entropy can be used to change the infrared emissivity through modulation of the damping constant.

4. Conclusions

In this study, LaB6 and two medium- and high-entropy hexaborides of (La0.25Sm0.25Ce0.25Eu0.25)B6 (MEREB6) and (La0.2Sm0.2Ce0.2Eu0.2Ba0.2)B6 (HEREB6) were designed and synthesized via a high-temperature solid-state reaction method with argon gas at 1600 °C. The XRD results provided evidence that the phases of these ME/HEREB6 ceramics were pure with no detectable impurity phase. XRD and EDS showed that ME/HEREB6 formed a homogeneous single phase solid solution. By analyzing the phase composition and microstructure, we showed that the ME/HEREB6 powder had a CsCl-type structure with Pm-3m space group with high crystallinity. The solar absorptivity of MEREB6 and HEREB6 is significantly increased in the range of 0.28–2.5 μm. The increase in solar absorptivity is mainly due to the decrease in free electron concentration and plasma frequency. Moreover, the emissivities of MEREB6 and HEREB6 in the ranges of 0.76–2.5 μm and 1–22 μm were also improved. The increase in emissivity was mainly caused by the multicomponent design, the induced lattice distortion, and the lower conductivity, resulting in an increase in the damping constant. In summary, both ME/HEREB6 ceramics had solar absorptivities greater than 80% and infrared emissivities close to 90%. Finally, in this study, ME/HEREB6 was synthesized, had high solar absorptivity and high infrared emissivity, and is expected to be used in solid particle solar receivers. Our study provides a new strategy for the development of solid particle solar receivers.

Author Contributions

Conceptualization, F.Y. and H.C.; methodology, H.W. and Y.P.; formal analysis, H.W. and J.Z.; investigation, H.W., Y.L. and H.C.; data curation, K.W., M.H. and L.X.; writing—original draft preparation, H.W.; writing—review and editing, H.C.; supervision, F.Y. and K.W.; project administration, Y.L.; funding acquisition, F.Y. and H.C. All authors have read and agreed to the published version of the manuscript.

Funding

The work was supported by the Lingchuang Research Project of China National Nuclear Corporation, the National Key Research and Development Program of China (No. 2022YFB3504302), the Fujian Provincial Natural Fund Project (Grant No. 2021J05101), the Young Elite Scientists Sponsorship Program by CAST (Grant No. YESS20210336), and the XIREM autonomously deployment project (Grant No. 2023GG03).

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

Data are contained within the article.

Conflicts of Interest

The author declares no conflicts of interest.

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Figure 1. Crystal structure of REB6.
Figure 1. Crystal structure of REB6.
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Figure 2. (a) XRD pattern of ME/HEREB6 and (b) partial enlargement of the (110) plane.
Figure 2. (a) XRD pattern of ME/HEREB6 and (b) partial enlargement of the (110) plane.
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Figure 3. (ac) Rietveld refinement of the XRD patterns.
Figure 3. (ac) Rietveld refinement of the XRD patterns.
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Figure 4. Samples of (ac) MEREB6 and (df) HEREB6, with their electron diffraction patterns and corresponding inverse fast Fourier transform (IFFT) patterns.
Figure 4. Samples of (ac) MEREB6 and (df) HEREB6, with their electron diffraction patterns and corresponding inverse fast Fourier transform (IFFT) patterns.
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Figure 5. Compositional maps from EDS of (a) MEREB6 and (b) HEREB6.
Figure 5. Compositional maps from EDS of (a) MEREB6 and (b) HEREB6.
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Figure 6. Lattice strains calculated based on Williamson–Hall analysis.
Figure 6. Lattice strains calculated based on Williamson–Hall analysis.
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Figure 7. (a) Raman spectra of LaB6 and (b) Raman spectra of LaB6, MEREB6, and HEREB6.
Figure 7. (a) Raman spectra of LaB6 and (b) Raman spectra of LaB6, MEREB6, and HEREB6.
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Figure 8. (a) Reflectance and solar irradiance spectra and (b) solar absorption rates of the LaB6, MEREB6, and HEREB6.
Figure 8. (a) Reflectance and solar irradiance spectra and (b) solar absorption rates of the LaB6, MEREB6, and HEREB6.
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Figure 9. (a) Spectrum of the sample emissivity in the range of 0.76–2.5 μm and (b) the normal infrared emissivity in the range of 1–22 μm.
Figure 9. (a) Spectrum of the sample emissivity in the range of 0.76–2.5 μm and (b) the normal infrared emissivity in the range of 1–22 μm.
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Table 1. Calculated atomic size differences (δr) and configuration entropy of medium- and high-entropy rare earth hexaborides.
Table 1. Calculated atomic size differences (δr) and configuration entropy of medium- and high-entropy rare earth hexaborides.
Composition Codeδr (%)ΔSconf
MEREB62.581.3863 R
HEREB63.951.6094 R
Table 2. Constituent of raw materials of LaB6, MEREB6, and (HEREB6).
Table 2. Constituent of raw materials of LaB6, MEREB6, and (HEREB6).
Composition CodeMolar Ratio of Raw Materials
LaB61La2O3:3B4C
MEREB61La2O3:1Sm2O3: 2CeO2:1Eu2O3:12B4C
HEREB61La2O3:1Sm2O3:2CeO2:1Eu2O3:2BaCO3:15B4C
Table 3. Lattice parameters and refined bond lengths (Å).
Table 3. Lattice parameters and refined bond lengths (Å).
SamplesLattice ParametersInteratomic Distances (Å)
a (Å) = b (Å) = c (Å)B–Binter MeanB-Bintra MeanM-B Mean
LaB64.15761.647 (14)1.775 (10)3.0531 (18)
MEREB64.155461.672 (10)1.756 (7)3.0550 (13)
HEREB64.160051.677 (11)1.756 (8)3.0588 (15)
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Wang, H.; Pan, Y.; Zhang, J.; Wang, K.; Xue, L.; Huang, M.; Li, Y.; Yang, F.; Chen, H. Medium- and High-Entropy Rare Earth Hexaborides with Enhanced Solar Energy Absorption and Infrared Emissivity. Materials 2024, 17, 1789. https://doi.org/10.3390/ma17081789

AMA Style

Wang H, Pan Y, Zhang J, Wang K, Xue L, Huang M, Li Y, Yang F, Chen H. Medium- and High-Entropy Rare Earth Hexaborides with Enhanced Solar Energy Absorption and Infrared Emissivity. Materials. 2024; 17(8):1789. https://doi.org/10.3390/ma17081789

Chicago/Turabian Style

Wang, Hongye, Yanyu Pan, Jincheng Zhang, Kaixian Wang, Liyan Xue, Minzhong Huang, Yazhu Li, Fan Yang, and Heng Chen. 2024. "Medium- and High-Entropy Rare Earth Hexaborides with Enhanced Solar Energy Absorption and Infrared Emissivity" Materials 17, no. 8: 1789. https://doi.org/10.3390/ma17081789

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