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In situ high-pressure spectroscopic studies using moissanite (4H-SiC) anvils

机译:使用莫桑石(4H-SiC)砧的原位高压光谱研究

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We examined the Raman scattering and IR absorption spectroscopy of 4H-SiC and its performance as an anvil material for high-pressure UV-visible absorption spectroscopic measurements. The first- and second-order Raman peaks of 4H-SiC and diamond do not coincide. 4H-SiC does not have obvious signals from 2330-5000 cm-1, suggesting that 4H-SiC anvils are beneficial for high-pressure studies of samples whose Raman signals locate in the region of diamond. Above 1800 cm-1, the transmitted signal of 4H-SiC in the IR absorption spectra, measured through 4.6 mm thickness is much higher than that of type IIa diamond. An in situ high-pressure UV-visible absorption spectroscopy study on CdI2 was carried out up to 28.0 GPa using 4H-SiC anvil cells (4H-SAC) with a 400 μm culet and the acquired band gap narrowed with increasing pressure. These results show that 4H-SiC has an excellent performance in high-pressure spectroscopic studies.
机译:我们研究了4H-SiC的拉曼散射和IR吸收光谱及其在高压UV-可见吸收光谱测量中作为砧材的性能。 4H-SiC和金刚石的一阶和二阶拉曼峰不一致。 4H-SiC在2330-5000 cm -1 处没有明显的信号,这表明4H-SiC砧对拉曼信号位于金刚石区域的样品的高压研究很有帮助。在1800 cm -1 以上,通过4.6 mm厚度测得的4H-SiC在红外吸收光谱中的透射信号远高于IIa型金刚石。使用具有400μm底尖和获得的带隙的4H-SiC砧室(4H-SAC)对高达28.0 GPa的CdI 2 进行了原位高压紫外-可见吸收光谱研究随着压力的增加而缩小。这些结果表明4H-SiC在高压光谱研究中具有优异的性能。

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