正庚烷相变序列的高压拉曼光谱研究

在室温条件下, 利用金刚石对顶砧超高压实验技术, 对液态的正庚烷进行了原位高压拉曼光谱研究, 采用红宝石荧光压标测压, 实验的最高压力为20.78 GPa。实验中发现, 当压力达到1.2 GPa左右时, 原本透明的样品腔内有小晶粒形成, 此时测量的拉曼谱上发现有许多新的拉曼峰出现。因此, 我们判断正庚烷在此压力下发生了一次相变; 当压力增加到3 GPa左右时, 在92.42 cm-1和2913.6 cm-1处又出现了2个新的拉曼峰, 并且拉曼频移随压力变化的曲线出现拐点, 我们推测在此压力下正庚烷可能又发生第二次相变; 当压力高于14.5 GPa时, 正庚烷发生了第三次压致相变; 而当压力介于7.5~14.5 GPa之间正庚烷处于两相共存的状态。我们给出了液体正庚烷在高压下的相变序列为: 液相-旋转相Ⅲ-旋转相Ⅳ-结晶相。该研究结果为进一步理解和研究其他正烷烃在高压下的结构、物理和化学特性提供了理论基础。     

正辛烷的高压拉曼光谱研究

 采用金刚石对顶砧高压装置,在室温下对正辛烷（C₈H₁₈）进行了原位高压拉曼光谱研究,实验的最高压力为13GPa。在实验的压力范围内,正辛烷的拉曼峰位随压力的升高均向高频移动,峰强逐渐减弱,峰形变宽。常态为液态的正辛烷在0.8 GPa时,拉曼频移随压力的变化曲线出现了拐点,发生了液－固相变;在6.8 GPa时,伴随着原拉曼峰的消失或劈裂,以及新拉曼峰的出现,此时正辛烷可能发生了固－固相变。该相变压力低于已有的低碳数正烃烷的压致相变结果。正烃烷的压致相变压力点,具有随着结构链长的增加,其相变压力降低的规律。     

叠氮化钡的高压拉曼光谱研究

在室温条件下,利用金刚石对顶砧高压技术,对叠氮化钡进行了原位高压拉曼光谱研究,采用红宝石荧光压标测压,实验的最高压力为10 GPa。实验压力范围内拉曼光谱随压力增加发生了丰富的变化。由于多处拉曼峰的出现和消失并伴随频移有拐点,我们判断叠氮化钡在3 GPa左右时发生了第一次结构相变;随着压力继续增加,在3.5~6.5 GPa范围内拉曼光谱仍不断变化,我们判断可能是相变或者是N=N=N键角和两个键长的非对称压缩导致的;压力继续增加,在8 GPa左右,多处新峰出现和峰的劈裂表明又发生了一次结构相变,并且判断叠氮化钡向着更复杂的结构转变。通过实验可以确定,实验压力范围内N=N=N离子并未被破坏。其实验结果有待高压同步辐射实验的进一步确认。     

氨的半水合物的高压拉曼光谱研究

在室温条件下, 利用金刚石对顶砧超高压技术, 对氨的半水合物(2NH3·H2O) 进行了原位高压拉曼光谱研究, 采用红宝石荧光压标测压, 实验的最高压力为41.0 GPa。装入金刚石对顶砧样品腔的初始样品为液态的氨的半水合物, 当压力达到3.5 GPa时, 显微镜下观察到整个样品腔内均匀的出现块状晶体, 同时, 测量到的拉曼谱上出现许多新的拉曼峰。因此, 我们判断在此压力下液态的2NH3·H2O发生了液固相变。当压力增加到19.0 GPa左右时, 2NH3·H2O的拉曼频移随压力变化的曲线有拐点, 并且具有软化特性的N-H伸缩振动模式消失。我们分析这是因为在高压下, 通过O-H…N成键的II型氨分子发生了旋转, 所以2NH3·H2O在此压力下发生了一次固固相变。     

叠氮化钠原位高压拉曼光谱研究

在室温条件下,利用金刚石对顶砧高压技术对叠氮化钠进行了原位高压拉曼光谱研究,采用红宝石荧光压标测压,实验的最高压力为37.7GPa。实验压力范围内拉曼光谱随压力增加发生了丰富的变化。由于多处拉曼峰的出现和消失并伴随频移有拐点,我们判断叠氮化钠在0~0.4GPa时发生了第一次结构相变,在相变过程中叠氮根的天平振动模式(Eg)出现了振动模式分裂为Ag和Bg,并且伴随着叠氮根离子之间的电荷转移。随着压力继续增加,在14.1GPa和27.3GPa分别发生了第二次和第三次结构相变。压致相变的路径为β-NaN_3→α-NaN_3→γ-NaN_3→δ-NaN_3。我们的拉曼散射研究,证实了此前的XRD研究。此外,结合计算,我们对常压下β-NaN_3的拉曼振动进行了指认。     

金刚烷的高压拉曼光谱研究

对金刚烷(C_(10)H_(16))进行了常温原位高压拉曼光谱研究,最高压力为25 GPa。通过分析高压拉曼光谱,结合拉曼频移随压力的变化情况,得出在实验压力范围内C_(10)H_(16)发生了多次相变。0.6 GPa时,C_(10)H_(16)由常温常压下的无序相(α相)转变为有序相(β相);继续加压至1.7 GPa时,第2次结构相变开始,直至3.2 GPa,第2次相变完全结束;第3次相变开始于6.3 GPa,结束于7.7 GPa;22.9 GPa时发生了第4次结构相变。另外,首次在拉曼光谱上探测到第3次相变过程中晶格振动峰的变化,说明第3次相变并非前人报道的等结构相变。     

巨磁阻材料Sr2CrWO6高压下的结构稳定性和电学特性

 采用金刚石压砧高压装置，研究了双钙钛矿结构化合物Sr₂CrWO₆在室温下、34.5 GPa压力内的同步辐射X射线衍射谱，发现在9.6 GPa的压力点样品的结构有所变化。结合室温下20 GPa内电阻和电容随压力的变化，证明样品在9 GPa附近发生了晶体结构相变，而在2~5 GPa的压力范围内样品发生了电子结构相变。     

微区Raman光谱在TiO_2高压结构相变研究中的应用

本文以金红石单晶TiO2和锐钛矿多晶TiO2为研究对象,应用金刚石小压机和原位拉曼光谱测量技术,系统研究了室温高压下TiO2的结构相变。原位拉曼测量表明,金红石单晶TiO2在压力达到12.91GPa时开始发生由金红石结构向斜锆石结构(MI)的相变,当压力达到14.16 GPa时,相变完成;继续加压到21.65 GPa,没有发现进一步的相变;卸压时由斜锆石结构转变为PbO2结构,相变发生在大约7.11 GPa处。锐钛矿多晶TiO2在压力达到4.26 GPa时开始向PbO2结构转变,当压力达到8.34 GPa时相变完成;继续加压到12.94 GPa,样品开始发生由PbO2结构向斜锆石结构的相变,当压力达到18.74 GPa时相变完成;继续加压到21.39 GPa,没有发现进一步的相变;卸压时也由斜锆石结构转变为PbO2结构,起始相变压力点应高于8 GPa。     

绿柱石的原位高压X射线研究

 采用同步辐射光源和金刚石对顶砧（DAC）技术,对绿柱石进行了室温下的原位高压能散X射线衍射（EDXD）研究,实验的最高压力为19.2 GPa。在实验压力范围内,未观察到绿柱石发生相变,轴压缩率c大于a;在小于9.3 GPa的压力范围内,其体积压缩率符合二阶Murnaghan状态方程,而压力在9.3～19.2 GPa范围内时,其体积压缩率有所增加,且体积-压力关系近乎线性变化。     

斜锆石（ZrO2）高温高压相变的Raman光谱研究

 以Ar作压力介质，在0~23 GPa压力范围内，利用金刚石压腔装置（DAC）和激光加温技术，采用显微拉曼光谱进行原位测试，对处于准静水压力条件下的斜锆石开展高温高压相变研究。研究结果表明：室温下斜锆石ZrO₂于3.4 GPa时开始发生相变，到10.4 GPa时其明显转变成一个空间群为Pbca的斜方相。此新相随着压力升高，直到15.3 GPa，仍稳定存在。通过研究，首次获得了Pbca相的拉曼谱图。随后在15.3 GPa压力下进行了激光加温后淬火，结果发现，加热前的Pbca相又转变成了空间群为Pnam的PbCl₂结构类型的高压相，该相直到实验最高压力23 GPa仍稳定存在。     

Pressure-Effect on Anatase Titanium Dioxide

Pressure-induced phase transition of anatase titanium dioxide was investigated by Raman, absorption spectroscopy and X-ray diffraction. The change in Raman and absorption spectra with pressure revealed that the transition from anatase to high pressure phase with f -PbO 2 structure (TiO 2 -II) occurred in the pressure range of 4.0-4.6 GPa for a single crystal. The X-ray powder diffraction patterns indicate the presence of superstructural lattice of anatase at pressures more than 3 GPa. The superstructure of anatase disappears on the release of the pressure. A sluggish transition to the high pressure phase is also observed. The anatase coexists with the high pressure phase at 5.2 GPa. The difference in the results between optical spectroscopy (single crystal) and X-ray diffraction (powder) will be due to crystalinity of the sample.     

High-pressure study of NaAlH4 by Raman spectroscopy up to 17 GPa

A high-pressure Raman study was carried out on NaAlH₄ up to 17 GPa using the diamond anvil cell method. In the pressure region 2–5 GPa, several of the original modes split. Although this might be a sign of some structural change, the spectral changes do not allow us to claim the existence of a clear phase transition in this pressure range. The spectra revert to their ambient pressure forms on decreasing pressure below<3.0–1.4 GPa. A phase transition to β-NaAlH₄ was found at 14–16 GPa. This phase transition is also reversible with an unusually strong hysteresis: the β-NaAlH₄ can be followed upon decompression down to 3.9 GPa. Analysis of Raman data shows that this phase transition is compatible with a theoretical prediction of a strong volume collapse.     

石膏的高压原位Raman光谱和相变研究

 利用金刚石对顶砧（DAC）高压装置产生高压,在0~35 GPa压力范围,对石膏（Gypsum,CaSO₄·2H₂O）晶体进行了高压原位Raman光谱研究。根据高压Raman光谱的实验数据,给出了石膏晶体Raman振动频率与压力的依赖关系;在4.5 GPa附近,在对称性伸缩振动范围,发现新的Raman峰1 012  cm^-1出现,这个峰的强度随压力升高逐渐增强,据此断定在4.5 GPa 附近,石膏晶体发生了压力导致的结构相变。     

Dynamics of the BiTeI lattice at high pressures

Raman measurements of the phonon spectrum of BiTeI at pressures of up to 20 GPa have been performed. A decrease in the linewidth of E² vibration by almost a factor of 2 with an increase in the pressure to 3 GPa has been detected. The frequencies of all four Raman active modes increase monotonically with the pressure. These lines are observed in spectra up to ～8 GPa. Sharp change in the spectrum occurs at pressures of 8–9 GPa, indicating a transition to the high-pressure phase, which holds up to 20 GPa. This transition is reversible and hardly has any hysteresis. A sample in the high-pressure phase is single crystal.     

硼酸锂系列晶体的高压拉曼散射研究

本文进行了硼酸锂系列晶体的高压拉曼散射及其压致相变的研究。对于三硼酸锂（ＬｉＢ３Ｏ５），我们发现在５．０ＧＰａ有一可逆的晶态到晶态的相变，在２７．０ＧＰａ有一不可逆的晶态到非晶态的相变。二硼酸锂（Ｌｉ２Ｂ４Ｏ７）不可逆压致非晶相变发生在３２．０ＧＰａ附近。对于一硼酸锂，我们研究了０—５５．８ＧＰａ范围内的高压拉曼光谱，只在２．０ＧＰａ发现了一个晶态到晶态的相变，但未发现不可逆压致非晶化现象。在硼酸锂系列晶体中，不可逆压致非晶化的压力随Ｌｉ２Ｏ的含量的增加而升高。硼酸锂晶体中Ｌｉ２Ｏ的含量越高，压致非晶化越不容易发生，这与熔体急冷法制备硼酸锂玻璃的规律是一致的。     

Raman spectroscopic study of the phase transitions induced by hydrostatic pressure in a Rb2KScF6 crystal

The Raman spectra of Rb₂KScF₆ elpasolite crystals are studied in the pressure range up to 7 GPa. A phase transition is revealed at a pressure of approximately 1 GPa. Analysis of the changes in the spectral parameters shows that the phase transition is accompanied by a doubling of the volume of the primitive cell in the initial cubic phase. Judging from the character of the variations in the pressure dependences of the frequency of the observed vibrations, there can exist another transition to the phase with a lower symmetry at a pressure of approximately 2.1 GPa.     

A high pressure Raman study of TeO2 to 30 GPa and pressure-induced phase changes

The effect of pressure on the Raman modes in TeO₂ (paratellurite) has been investigated to 30GPa, using the diamond cell and argon as pressure medium. The pressure dependence of the Raman modes indicates four pressure-induced phase transitions near 1 GPa, 4.5 GPa, 11 GPa and 22 GPa. Of these the first is the well studied second-order transition fromD ₄ ⁴ symmetry toD ₂ ⁴ symmetry, driven by a soft acoustic shear mode instability. The remarkable similarity in the Raman spectra of phases I to IV suggest that only subtle changes in the structure are involved in these phase transitions. The totally different Raman spectral features of phase V indicate major structural changes at the 22GPa transition. It is suggested that this high pressure-phase is similar to PbCl₂-type, from high pressure crystal chemical considerations. The need for a high pressure X-ray diffraction study on TeO₂ is emphasized, to unravel the structure of the various high pressure phases in the system.