2023 Volume 64 Issue 5 Pages 945-949
Owing to the quasiperiodic order, one independent term in the elasticity of quasicrystals (phonon–phason coupling) is characteristic of quasicrystals. It is not seen in conventional crystals and has continued to be a significant subject in the research field of quasicrystals. Recently, a novel method was applied to a Mackay-type Al–Pd–Mn icosahedral quasicrystal to prove the existence of phonon–phason coupling and to evaluate its strength based on the elasticity of quasicrystals. This study applied the method to a Tsai-type Ag–In–Yb icosahedral system to evaluate its phonon–phason coupling strength. We applied phonon strain to the quasicrystal at a temperature with active phason, and the induction of phason strain was successfully detected and evaluated using powder X-ray diffraction. We evaluated the phonon–phason coupling elastic constant of the Ag–In–Yb icosahedral quasicrystal to be 0.17 ± 0.04 GPa by quantitatively comparing the measured induced phason strain with our calculation results.
Fig. 2 Phason momentum (|G⊥|) dependence of the full width at half maximum of the X-ray diffraction peaks ((Δq)FWHM) for the as-grown sample, the samples with the compressed stress of 75 and 100 MPa, and the sample subjected to the same heat treatment but without compression (0 MPa). Reciprocal vector (|G|||) dependences of (Δq)FWHM for these samples are shown in the inset.
Quasicrystals (QCs) have a unique type of ordered structure characterized by disallowed crystallographic rotational symmetry and quasiperiodic translational order.1–3) Owing to the quasiperiodic translational order, QCs have a peculiar type of elastic degrees of freedom called phason degrees of freedom, in addition to phonon degrees of freedom. With the lowest-order approximation, the elastic free energy (fel) of the QCs per unit volume can be expressed as a function of the phonon (conventional) strain uij and phason strain wij, fel comprising the following three independent terms:
\begin{equation} f_{\text{el}}(u_{ij},w_{ij}) = f_{u - u}(u_{ij}) + f_{w - w}(w_{ij}) + f_{u - w}(u_{ij},w_{ij}), \end{equation} | (1) |
Koschella et al.7) and Zhu et al.8) evaluated the elastic coupling constant of fu−w for the model QC structures of decagonal and icosahedral systems. They introduced phason strain into QCs to construct a series of crystal approximants (CAs) and measured their phonon strain to evaluate the coupling constant. Edagawa et al.9–11) applied this method to real QC alloys for experimental evaluation. However, CAs are generally different phases from the QCs; therefore, the method using CAs cannot directly probe the fel of QCs. This indicated that the estimated values may not be accurate. Recently, a new approach, which directly probes the fel of QCs, was proposed for the quantitative evaluation of the coupling constant and was applied to a single crystal of the Al–Pd–Mn icosahedral QC, by which the existence of fu−w was demonstrated.12) The icosahedral QC phases discovered so far can be classified into three groups based on the type of atomic cluster that constitutes the QC structure: Mackay-type, Bergman-type, and Tsai-type. The Al–Pd–Mn icosahedral QC belongs to the Mackay type.
In this paper, this approach was applied to a Tsai-type Ag–In–Yb icosahedral system. Phonon strain was applied to single crystals of the Ag–In–Yb icosahedral QC at an elevated temperature with active phason. The induction of phason strain was successfully observed by powder X-ray diffraction, and the X-ray diffraction peaks were simulated based on the elasticity of the QCs. The magnitude of the induced phason strain was quantitatively determined by comparing the measured X-ray diffraction peaks with the simulated results, from which the coupling constant of fu−w was evaluated.
Pure metallic elements with a nominal composition of Ag42In42Yb16 were placed in a conical-bottom alumina crucible with a diameter of 16 mm and sealed in a silica tube under an argon atmosphere. The silica tube was slowly pulled down in the furnace at a tube speed of 0.8 mm/h. In this way, large single crystals of the Ag–In–Yb icosahedral QC were grown by using the Bridgman method. The crystallographic orientation of the grown single crystals were characterized using back-scattering X-ray Laue diffraction measuring instruments, and 2 × 2 × 5 mm3 rectangular samples were formed with the long axis of the sample along one of the 2-fold axes of the icosahedral QC. Compression tests were performed at 573 K using an automatic material-testing machine equipped with a heating furnace. Constant elastic stress was maintained along the long axis of the sample over time. The samples were then quenched to room temperature while maintaining the same stress. Subsequently, the stress was removed. Finally, the samples were powdered and subjected to X-ray diffraction measurements using Cu Kα radiation at 40 kV and 200 mA.
The calculation method is described in detail in our previous work.12) We summarize the equations used in our calculation as follows. Based on the generalized elasticity of the icosahedral QC, when an elastic stress σ is applied along [001] (one of the 2-fold axes of the icosahedral QC), the applied phonon strain $u_{ij}^{\text{appl}}$ can be expressed as follows:
\begin{equation} u_{ij}^{\text{appl}} = \begin{bmatrix} - \nu \varepsilon & 0 & 0\\ 0 & - \nu \varepsilon & 0\\ 0 & 0 & \varepsilon \end{bmatrix} , \end{equation} | (2) |
\begin{align} & w_{ij}^{\text{ind}} = M \begin{bmatrix} \tau & 0 & 0\\ 0 & -\dfrac{1}{\tau} & 0\\ 0 & 0 & - 1 \end{bmatrix} ,\\ & M = K_{3}\varepsilon (1 + \nu)/(K_{1} - 4K_{2}/3) \end{align} | (3) |
Figure 1 shows the X-ray diffraction spectrum at scattering angles 2θ from 20 to 80° for the as-grown sample of Ag–In–Yb icosahedral QC, where the Cu Kα2 component was numerically removed from the raw data. All peaks can be indexed as icosahedral phase. These peak widths are close to the X-ray instrumental resolution limit, indicating that the single-phase samples’ structural quality is excellent.
X-ray diffraction spectrum at scattering angles 2θ from 20° to 80° for the as-grown sample of Ag–In–Yb icosahedral quasicrystal, where the Cu Kα2 component was removed numerically from the raw data.
Figure 2 shows |G⊥| (the magnitude of the phason momentum) dependences of the full width at half maximum intensities of the X-ray diffraction peaks (Δq)FWHM for the as-grown sample, the samples with compressed stresses of 75 and 100 MPa for 1 h at 573 K, and the sample processed with the same heat treatment as compressed samples at 573 K but without compression (0 MPa). No clear |G⊥| dependence of (Δq)FWHM can be exhibited for the as-grown sample and the sample without compression at 573 K. In contrast, the (Δq)FWHM of samples with compressed stresses of 75 and 100 MPa at 573 K have a clear upward trend with increasing |G⊥|, where the slope becomes more significant with increasing stresses. Because no oxidation or phase changes can be detected in all compressed samples, the broadening of X-ray peaks is attributable to the induction of the phason strain. Meanwhile, there is no noticeable |G||| (the magnitude of the reciprocal vector, that is, scattering vector q-value (q ≡ 4π sin θ/λ)) dependence of (Δq)FWHM for all these samples, as shown in the inset. These results indicate that when applying phonon strain to the Ag–In–Yb icosahedral QC, the phason strain was induced successfully, and the induced phason strain was positively dependent on the applied phonon strain, proving the existence of fu−w. We note here that the phonon strain was removed upon the removal of the compressed stresses on samples and that the phason one was “frozen” at room temperature.
Phason momentum (|G⊥|) dependence of the full width at half maximum of the X-ray diffraction peaks ((Δq)FWHM) for the as-grown sample, the samples with the compressed stress of 75 and 100 MPa, and the sample subjected to the same heat treatment but without compression (0 MPa). Reciprocal vector (|G|||) dependences of (Δq)FWHM for these samples are shown in the inset.
Then, based on the elasticity of the QCs, we simulated the powder X-ray diffraction peaks, in which the phason strain $w_{ij}^{\text{ind}}$ in eq. (3) is induced. The simulation method was described in detail in our previous paper12) and is reviewed in the following section. The induced phason strain $w_{ij}^{\text{ind}}$ leads to the shifting of Bragg spots in the 3D reciprocal space: $\mathbf{G}_{\| } \to \mathbf{G}'_{\| }$, as follows:
\begin{equation} \mathbf{G}'_{\|} = \mathbf{G}_{\|} - \mathbf{G}_{\bot} \cdot w_{ij}^{\text{ind}}. \end{equation} | (4) |
Phason momentum (|G⊥|) dependence of the full width at half maximum of the X-ray peaks ((Δq)FWHM) for simulated X-ray diffraction peaks for various |M|.
The comparison of the measured and simulated X-ray diffraction peaks for the 100 MPa (top), 75 MPa (middle) compressed samples, and the as-grown sample (bottom) are shown in Fig. 4, while M = −0.02, −0.015 and 0 were used in our simulations, respectively. The consistency between the measured and simulated peaks was quite good. For the Tsai-type Ag–In–Yb icosahedral system, the values of E and ν have never been reported. However, the Ag–In–Yb icosahedral QC is isostructural with the Tsai-type Cd–Yb icosahedral QC, and their melting points are nearly equal. Thus, it may be assumed that the Lamé constants λ and μ of the Ag–In–Yb icosahedral QC are approximately equal to those of the Cd–Yb icosahedral QC, which have been previously reported to be 35.28 and 25.28 GPa, respectively.13) Therefore, we obtain E = μ(3λ + 2μ)/(λ + μ) ≈ 65 GPa and ν = λ/2(λ + μ) ≈ 0.29, respectively. Then, the values of K1 and K2 for Ag–In–Yb icosahedral QC have been previously reported to be 24 MPa and 5.7 MPa, respectively.14) For our compressed stress σ = 100 MPa and ε = −σ/E ≈ −1.53 × 10−3, substituting K1, K2, ε, ν, and M = −0.02 into the M = K3ε(1 + ν)/(K1 − 4K2/3) in eq. (3), we obtain the absolute value of the phonon–phason coupling constant, |K3| ≈ 0.17 ± 0.04 GPa. The value of |K3| is in good agreement with previous results of internal friction measurements. It quantitatively explains the internal friction peaks previously observed for the Ag–In–Yb icosahedral phase.14) The absolute value of the evaluated phonon–phason coupling constant |K3| for the Ag–In–Yb icosahedral QC in the present study and other previously reported |K3| of icosahedral QCs are presented in Table 1.
Measured (black) and simulated (red) X-ray diffraction peaks for the 100 MPa (top), 75 MPa (middle) compressed samples, and as-grown sample (bottom), while M = −0.02, −0.015, and 0 were used in our simulations, respectively.
The method used in our previous work to evaluate the phonon–phason coupling strength of a Mackay-type Al–Pd–Mn icosahedral system12) was applied to evaluate the coupling strength of a Tsai-type Ag–In–Yb icosahedral system. In our experiment, phonon strain was applied to single crystals of Ag–In–Yb icosahedral QC at a temperature with active phason. The induced phason strain was successfully observed and measured by X-ray diffraction measurements, providing clear evidence of phonon–phason coupling in the Tsai-type Ag–In–Yb icosahedral system. The powder X-ray diffraction peaks were simulated based on the elasticity of the QCs. The induced phason strain was quantitatively evaluated by comparing the measured X-ray peaks with our simulated peaks. The absolute value of the phonon–phason coupling elastic constant |K3| was determined to be 0.17 ± 0.04 GPa. The value of |K3| is in good agreement with previous results of internal friction experiments for an Ag–In–Yb icosahedral QC.
This work was supported by JST, CREST Grant Number JPMJCR22O3 Japan, and KAKENHI Grant-in-Aid (No. JP19H05821) from the Japan Society for the Promotion of Science (JSPS). This work was also supported by the Light Metal Educational Foundation, Inc., under funds for the Encouragement and Promotion of Research, Study, and Education.