Institut Charles Gerhardt Montpellier, UMR 5253, CNRS-UM2-ENSCM-UM1, C2M, Université Montpellier 2, CC 1504, Place Eugène Bataillon, 34095 Montpellier Cédex 5 (France), Fax: (+33) 467144290.
Chemphyschem. 2014 Jan 13;15(1):118-25. doi: 10.1002/cphc.201300793. Epub 2013 Dec 2.
From high-precision Brillouin spectroscopy measurements, six elastic constants (C11, C33, C44, C66, C12, and C14) of a flux-grown GeO2 single crystal with the α-quartz-like structure are obtained in the 298-1273 K temperature range. High-temperature powder X-ray diffraction data is collected to determine the temperature dependence of the lattice parameters and the volume thermal expansion coefficients. The temperature dependence of the mass density, ρ, is evaluated and used to estimate the thermal dependence of its refractive indices (ordinary and extraordinary), according to the Lorentz-Lorenz equation. The extraction of the ambient piezoelectric stress contribution, e11, from the C'11-C11 difference gives, for the piezoelectric strain coefficient d11 , a value of 5.7(2) pC N(-1), which is more than twice that of α-quartz. As the quartz structure of α-GeO2 remains stable until melting, piezoelectric activity is observed until 1273 K.
从高精度布里渊光谱测量中,获得了具有α-石英类似结构的通量生长 GeO2 单晶在 298-1273 K 温度范围内的六个弹性常数(C11、C33、C44、C66、C12 和 C14)。收集高温粉末 X 射线衍射数据以确定晶格参数和体积热膨胀系数随温度的变化。评估质量密度 ρ 的温度依赖性,并根据洛伦兹-洛伦兹方程估算其折射率(寻常光和非常光)的热依赖性。从 C'11-C11 差值中提取环境压电应力贡献 e11,给出压电应变系数 d11 的值为 5.7(2)pC N(-1),是α-石英的两倍多。由于α-GeO2 的石英结构在熔化之前保持稳定,因此直到 1273 K 仍观察到压电活性。