50 GPa下NiO等温状态方程的高压X光研究

 本文采用在位的（in situ）高压X光衍射方法研究了近50 GPa和室温下三方结构NiO的等温压缩行为，并用Murnaghan状态方程对实验值进行了最小二乘法拟合，得到的NiO室温状态方程的相应参量分别为：B₀=223 GPa，B₀'=4.21。在室温压力范围内没有观察到第一类结构相变。NiO在六方指标下的轴比c/a随压力的变化在实验压力范围内可用c/a=2.450~1.569×10^-3（GPa）近似描述。     

Hg1-xCdxTe在高压下的结构、状态方程与相变

 利用X射线粉末衍射方法,在室温高压下观察到了Hg_1-xCd_xTe（x=0.19）的相变。实验是在DAC高压装置上完成的,压力从0逐步加至10.1 GPa。在常温常压下Hg_1-xCd_xTe（x=0.19）具有闪锌矿结构。从实验结果看到,在压力为3 GPa和6.8～8.3 GPa之间有两个结构相变存在。初步认为,后一个相变与Hg_1-xCd_xTe（x=0.19）的金属化有密切关系。通过计算,得到了它在相变前的状态方程,并且与二元HgTe化合物在相变规律上进行了比较。     

金刚石压砧内单轴应力场对物质状态方程测量的影响

金刚石压砧的几何结构使得在高压下封垫内的样品通常处于单轴应力场中：压砧轴向加载应力最大,径向应力最小.由于金刚石压砧内非静水压单轴应力场的影响,用传统的高压原位X射线衍射方法测得的物质压缩曲线一般位于理想静水压压缩曲线之上.利用金刚石压砧径向X射线衍射技术以及晶格应变理论,结合最近的钨、金刚石和硼六氧样品的高压原位同步辐射径向X射线衍射实验结果,从宏观差应力、样品强度、标压物质和待测物质强度的关系三个方面分析讨论了金刚石压砧内单轴应力场对物质状态方程测量的影响及解决方案. 关键词： 金刚石压砧 单轴应力场 高压原位X射线衍射 状态方程     

γ-Ce中的高压纵波声子模软化和状态方程描述

利用同步辐射角散X射线衍射技术测量了室温条件下0---0.74 GPa 压力范围内Ce的等温压缩线.发现γ-Ce的室温等温压缩线呈外凸形, 这是由其纵波声子模软化所致.利用超声测量得到的体弹性模量随压力变化的规律, 对实验所得到的压力与体积数据, 用二阶和三阶Murnaghan 方程、 二阶和三阶Birch 方程、 三阶Xu方程以及二阶Vinet方程进行比较, 并且对这些状态方程得到的体弹性模量随压力的变化规律与超声实验的结果相对比, 发现三阶Murnaghan 方程和三阶Xu方程对γ-Ce最适用.     

天青石的等温状态方程和拉曼振动研究

利用金刚石对顶砧（DAC）装置产生高压,在室温下、0～32 GPa压力范围,对天青石（SrSO4）进行了原位高压X射线衍射和拉曼光谱研究. 根据高压X射线衍射的数据,测定了天青石的等温状态方程,得到天青石的零压体弹模量KT0＝83GPa（K'T0＝4）, 在所研究压力范围内没有观察到相变的发生. 高压拉曼光谱的数据显示,在5GPa左右,SO4四面体弯曲振动峰发生劈裂,这是由SO4四面体畸变引起的;同时,所有的拉曼振动峰都随着压力的增加而增加, 并且,高频模的平均压力导数要高于低频模的,根据以上数据获得了模格林奈森参数.     

同步辐射X射线光源在高压科学研究中的应用

同步辐射X射线光源已经成功地应用到高压科学研究的诸多领域.文章简要回顾了同步辐射高压技术的发展历史,简要介绍了同步辐射X射线衍射技术在高压状态方程、强关联体系、地球内部物质以及早期生命起源等研究中的应用.介绍了同步辐射X射线光谱技术(包括晶格振动声子谱的测量)在高压研究中的应用,此外,还介绍了时间分辨的同步辐射技术在冲击压缩研究中的应用,最后展望了未来先进光源应用于高压科学研究的前景.     

百吉帕超高压下Ag的X光衍射实验和研究

 详细地介绍了百吉帕超高压实验的方法和步骤。实验是在具有杠杆式的金刚石对顶压砧（DAC）高压装置上完成的。以Ag为样品，进行百吉帕超高压下X光衍射的实验研究。最高压力达121 GPa，并获得了若干有意义的实验曲线和结果。     

室温高压下天然锡石状态方程研究

 利用金刚石压腔同步辐射X射线就位衍射技术,在室温、最高压力达13 GPa条件下,对采自云南个旧锡矿的天然锡石做了X衍射测量。结果表明,在实验压力范围内锡石未发生相变,其晶胞参数随压力增大而逐渐减小。与前人合成锡石实验结果相比,本次实验测定的晶胞参数偏大。由Birch状态方程对实验结果p-V进行最小二乘法拟合,得出锡石的K_T(0)＝228 GPa。分析认为,在天然矿物晶体中,Zr对Sn的类质同象置换是晶胞参数偏大的主要原因。     

原位高压微米氧化锌电学性质的研究

利用集成有金属薄膜电极的金刚石对顶砧,对微米氧化锌样品进行了原位高压电导率测量.结果表明,在919 GPa时样品电导率达到最小值,在919—1122 GPa时样品电导率急剧增大,说明此时样品从纤锌矿结构向岩盐矿结构转变直至完全相变,1122　GPa为相变点.通过测量不同条件下高温退火处理的样品电导率,明显看到氧空位对电导率的影响. 关键词： 高压 微米氧化锌 电导率 金刚石对顶砧     

一个方便实用的粉末衍射数据处理和结构分析程序

重点介绍了最近开发的粉末Ｘ射线衍射数据处理和结构分析软件“ＰｏｗｄｅｒＸ”．“ＰｏｗｄｅＸ在Ｗｉｎｄｏｗｓ９５／９８平台下工作,有使用方便的图形界面和连机帮助,具有数据平滑、扣除背景、扣除α２、寻峰、指标化、晶格参数精修等多种功能,可以输入多种格式的衍射数据,可以方便地进行数据格式转换,非常适合多晶结构分析和精修的需要,程序中包含有独特的衍射仪零点、样品偏心系统误差样正功能和精确ＣｕＫα２扣除功能     

High pressure studies up to 50GPa of CuO

Abstract

Copper oxide has been studied at high pressure up to 50 GPa. A monoclinic structure was compatible with the measurements at all pressures, and no phase change was observed. A bulk modulus, B₀, = 98 GPa, and its pressure derivative B′₀ = 5.6 was obtained.     

High pressure X-ray diffraction experiments on NpS and PUS up to 60 GPa

Abstract

Neptunium and plutonium monosulfides were studied under high pressure up to ～60 GPa using a diamond anvil cell in an energy dispersive X-ray diffraction facility. The compounds, of cubic rock salt structure type at ambient pressure, do not show any crystallographic phase transition in the domain of investigation. From the pressure-volume relationship, we determined bulk moduli of 92 and 120 GPa with pressure derivatives of 4.6 and 4.1 for NpS and PUS respectively.     

High resolution X-ray diffraction studies at high pressures

Abstract

The principal sources of systematic error in high-pressure x-ray structure determination with a diamond anvil cell have been studied in detail. The results of these studies have been used to develop techniques to minimise or correct for these effects.     

Static strength of gold compressed up to 127 GPa

Gold powder is compressed non-hydrostatically up to 127 GPa in a diamond anvil cell(DAC),and its angle dispersive X-ray diffraction patterns are recorded.The compressive strength of gold is investigated in a framework of the lattice strain theory by the line shift analysis.The result shows that the compressive strength of gold increases continuously with the pressure up to 106 GPa and reaches 2.8 GPa at the highest experimental pressure(127 GPa) achieved in our study.This result is in good agreement with our previous experimental result in a relevant pressure range.The compressive strength of gold may be the major source of the error in the equation-of-state measurement in various pressure environments.     

Phase transitions in PbTe under quasi-hydrostatic pressure up to 50 GPa

PbTe has been investigated using synchrotron X-ray diffraction (XRD) in a diamond anvil cell under quasi-hydrostatic pressures up to 50 GPa. Upon compression to 6.6 GPa, the initial NaCl phase transforms to an intermediate phase, which is confirmed to be an orthorhombic structure with a space group Pnma. At 18.4 GPa, the intermediate Pnma phase undergoes a phase transition to the CsCl structure. The systemic analysis of the crystal structures between the NaCl and intermediate phases indicates that the structure of the Pnma phase could be derived from the distortion of the NaCl structure. The bulk modulus of the CsCl phase is B₀=52(2) GPa with V₀=60.8(4) ų and B′₀=4.0 (fixed), slightly larger than the NaCl phase (B₀=44(1) GPa) and the intermediate phase (B₀=49(3) GPa).     

High-pressure Raman study of solid hydrogen up to 300 GPa

The high-pressure behavior of solid hydrogen has been investigated by in situ Raman spectroscopy upon compression to 300 GPa at ambient temperature. The hydrogen vibron frequency begins to decrease after it initially increases with pressure up to 38 GPa. This softening behavior suggests the weakening of the intramolecular bond and the increased intermolecular interactions. Above 237 GPa, the vibron frequency softens very rapidly with pressure at a much higher rate than that of phase III, corresponding to transformation from phase III into phase IV. The phase transition sequence has been confirmed from phase I to phase III and then to phase IV at 208 and 237 GPa, respectively. Previous theoretical calculations lead to the proposal of an energetically favorable monoclinic C2/c structure for phase III and orthorhombic Pbcn structure for phase IV. Up to 304 GPa, solid hydrogen is not yet an alkali metal since the sample is still transparent.     

Diamond-anvil cell high pressure X-ray studies on thorium to 100 GPa

Abstract

High pressure crystal structural changes and volume compression for thorium were investigated to 100 GPa in a diamond-anvil cell apparatus using the energy-dispersive X-ray diffraction technique. No structural change was observed in this pressure range. However, a slope change in the P-V curve was observed between 20 and 30 GPa. We surmise that this break in the slope may be due to an electronic transformation.     

顽火辉石的高温高压同步辐射研究

 采用同步辐射能量色散X射线衍射技术、激光加热技术和金刚石对顶砧（DAC）高压装置,在温度为2 000 K和压力为23 GPa的范围内,对采自地幔二辉橄榄岩中的顽火斜方辉石,进行了原位的高温高压能量色散X射线衍射（EDXRD）测量。实验结果表明：当压力为15.3 GPa、温度为1 600 K时（相当于地球内部410 km处的地震波不连续界面的温压环境）,顽火斜方辉石转变为橄榄石的β相——瓦兹利石（Wadsleyite）相;继续加温加压至2 000 K、23 GPa时（相当于地球内部670 km处的地震波不连续界面的温压环境）,顽火斜方辉石相变为钛铁矿（Ilmenite）结构和钙钛矿（Perovskite）结构的混和相。实验结果进一步证明,在地幔中存在的两个地震波不连续界面是由橄榄石、顽火斜方辉石等矿物的相变引起的。