金和铂的室温等温物态方程及其压标的意义

 在对Grüneisen系数高温高压特性不作任何假设的前提下,由冲击雨贡纽数据直接确定了材料零温零压体积、等温体模量及其对压力的一阶偏导。基于上述参数,计算了两种常用压标材料金和铂压缩比至0.5~0.6的0 K物态方程,并通过相应的热压修正得到了金和铂的室温等温物态方程。计算结果与准静水压条件下静高压实验结果具有非常好的吻合性,缩小了早期不同金和铂压标之间的差异。独立来源实验数据和理论计算结果的交叉检验表明,金和铂的室温等温物态方程计算结果可以用于今后静高压实验的压标。     

百吉帕压力下固态氩的状态方程

 利用最新的X光衍射实验数据和Ar原子的弹性散射实验结果，得到了Ar原子间的相互作用和350 GPa下的固态氩的状态方程。这个状态方程可以作为超高压力下的压标。在150 GPa以上的压标，是目前高压研究中急需的。固态氩既可作为准静水压传压介质，又可作为高压X光衍射中的压标使用。本文计算了固态氩的Grüneisen参数、Debye特征参数、定容比热和等温体模量随压力的变化，压力范围为0~150 GPa。     

纤锌矿氮化硼及其应用的研究（Ⅱ）——纤锌矿型氮化硼的等温状态方程

 使用两种不同的高压在位X光衍射法，研究了用爆炸法合成的纤锌矿型氮化硼（wBN）在室温下的等温状态方程。一种方法是用转靶X光角色散粉末衍射法，研究了它在0~40 GPa压力范围内的等温压缩行为。结果表明，wBN在0~40 GPa的压力范围内是稳定的，没有发生结构相变。通过p-V数据对Murnaghan方程拟合，得到wBN在p=0时的等温体模量B₀=(335±34) GPa及其对压力的一阶导数B₀'=4.21；另一种是用同步辐射X光能量色散衍射法，研究了它在0~25 GPa压力范围内的等温状态方程。实验中，使用了改进的自动加压的DAC高压装置，此装置保证了实验中衍射角θ₀固定不变。将获得的p-V数据仍用Murnaghan方程拟合，得到wBN在p=0时等温体模量B₀=(280±56) GPa，及其B₀'=4.39。     

准静水压条件下SrF2的X射线衍射

利用同步辐射能量色散X射线衍射技术对SrF₂进行了高压相变实验研究. 实验以Ar作为传压介质, 以获得准静水压条件. 实验用红宝石荧光法标定样品压力, 得到的最高压力为44.2GPa. 在实验压力范围内, SrF₂在11.2GPa时发生了从立方晶系到正交晶系的相变, 通过拟合相变前后的P-V状态 方程, 得到立方SrF₂的体弹模量为70.0(5.0)GPa, 正交SrF₂的体弹模量为198.3(15.2)GPa. 卸压到零压时, SrF₂回到立方相结构.     

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。     

冲击加载下NaCl单晶高压声速与温度的同步测量

基于二级轻气炮和多通道辐射高温计,测量了45~85GPa压力范围内NaCl单晶的B2相区、B2-液相混合相区和液相区的高压声速和温度。通过高压声速数据,确定了NaCl单晶的冲击熔化压力区间为58~67GPa。当压力为67GPa时,NaCl单晶的冲击熔化温度为3 740K。计算了NaCl单晶的等熵体模量、Grüneisen系数和定容比热容,对比分析了多种模型对Grüneisen系数高压演化特性的描述。结果显示,根据吴强模型计算的Grüneisen系数不但在液相区与冲击压缩实验结果吻合得非常好,而且在低压区也与金刚石压砧实验结果及有限应变计算结果吻合得非常好。     

固氖高压物态方程的量子理论计算

 运用Hartree-Fock计算方法和原子团簇理论,研究了高压下面心立方晶体氖中的二体相互作用、三体相互作用对中心原子势能及冷能的贡献。结合零点振动能,计算得到了固氖在4~208 GPa压强范围内的等温物态方程。结果表明,在较高压强区域内,等温压缩线与高压实验数据符合得非常好;在压强超过100 GPa的区域内,计算得到的等温压缩线较目前已有的理论研究结果系统地改善并提高了3%~5%,精确地解释了固氖的高压实验数据。     

钙钛矿(CaTiO_3)高压相变及等温压缩

高温高压条件下对钙钛矿(Perovstsite)多晶进行了研究,在金刚石压砧设备上压力条件最高达38GPa,YAG莱塞加热温度近1000℃以上,用红宝石萤光校压系统进行压力标定。实验结果表明静水压条件X射线就位测量,CaTiO_3(Ⅰ)由斜方晶系在10GPa时直接向六方CaTiO_3(Ⅱ)结构相变,体积变化为1.6％;1000℃加热及非静水压条件下,CaTiO_3(Ⅰ)由斜方晶系首先转变为四方晶系CaTiO_3(Ⅲ)转变压力为8.5GPa,体积变化0％,继续增加压力到15GPa,CaTiO_1(Ⅲ)向CaTiO_3(Ⅱ)转化成六方晶系,体积变化亦为1.6％。三种高压相,在压力降到一个大气压时都会消失,所以是逆转化的非淬火相。 等温压缩在标准静水压条件下进行,压力应小于10.4GPa,K_0~'=5.6时,X_o=210±7GPa,此数据是根据Birch-Murnaghan状态方程求得的体模重。     

钙钛矿（GaTiO3）高压相变及等温压缩

 高温高压条件下对钙钛矿（Perovstsite）多晶进行了研究，在金刚石压砧设备上压力条件最高达38 GPa，YAG莱塞加热温度近1 000 ℃以上，用红宝石荧光校压系统进行压力标定。实验结果表明静水压条件X射线就位测量，GaTiO₃(Ⅰ)由斜方晶系在10 GPa时直接向六方GaTiO₃(Ⅱ)结构相变，体积变化为1.6％；1 000 ℃加热及其非静水压条件下GaTiO₃(Ⅰ)由斜方晶系首先转变为四方晶系GaTiO₃(Ⅲ)转变压力为8.5 GPa，体积变化为0％，继续增加压力导15 GPa，GaTiO₃(Ⅲ)向GaTiO₃(Ⅱ')转化成六方晶系，体积变化亦为1.6％。三种高压相，在压力降到一个大气压时都会消失，所以是逆转化的非淬火相。等温压缩在标准静水压条件下进行，压力应小于10.4 GPa，K₀'=5.6时，K₀=(210±7)GPa，此数据是根据Birch-Murnaghan状态方程求得的体模量。     

天然绿帘石原位高压同步辐射X射线衍射研究

在金刚石压腔高压装置(DAC)上采用同步辐射角度色散X射线衍射技术,在室温、最高压力9.16GPa条件下,对天然绿帘石进行了状态方程研究。在实验压力范围内,未观察到绿帘石发生相变。通过Birch-Murnaghan状态方程,对所获得的实验数据进行了状态方程拟合,获得了天然绿帘石的体弹模量值为116(7)GPa,体弹模量的压力导数值为7.8(8),若将体弹模量的压力导数值固定为4,获得绿帘石的体弹模量值为132(4)GPa。另外,绿帘石存在较为明显的轴向压缩各向异性:c轴方向压缩系数最大,b轴方向压缩系数最小,说明天然绿帘石在c轴方向更易于压缩,而b轴方向最抗压。     

Equations of state for Cu,Ag, and Au and problems with shock wave reduced isotherms

Thermophysical data at low pressure are used to constrain a thermodynamic model for equations of state and all the other thermophysical properties in wide ranges of pressure and temperature. Comparisons with shock wave reduced isotherms show strong deficiencies in the models used in the data reductions. A revision in the evaluation of static high-pressure X-ray diffraction data for Cu and Au together with data for ruby luminescence line shifts from the literature lends further support to some recent refinements of the ruby pressure scale.     

Equal compressibility structural phase transition of molybdenum at high pressure

We have studied the high-pressure compression behavior of molybdenum up to 60 GPa by synchrotron radial x-ray diffraction (RXRD) in a diamond anvil cell (DAC). It is found that all diffraction peaks of molybdenum undergo a split at around 27 GPa, and we believe that a phase transition from a body-centered cubic structure to a rhombohedral structure at room pressure has occurred. The slope of pressure-volume curve shows continuity before and after this phase transition, when fitting the pressure-volume curves of the body-centered cubic structure at low pressure and the rhombohedral structure at high pressure. A bulk modulus of 261.3 (2.7) GPa and a first-order derivative of the bulk modulus of 4.15 (0.14) are obtained by using the nonhydrostatic compression data at the angle ψ = 54.7° between the diffracting plane normal and stress axis.     

Exploring the compression behavior of HP-BiNbO_4 under high pressure

In the present work, a third form, the so-called HP-BiNbO_4 synthesized at high pressure and high temperature is investigated with the in-situ angle-dispersive x-ray diffraction(ADXRD) measurements under high pressure. We explore the compression behavior and phase stability of HP-BiNbO_4. The structure of HP-BiNbO_4 is first determined. The x-ray diffraction data reveal that the structure HP-BiNbO_4 is stable under pressures up to 24.1 GPa. The ADXRD data yield a bulk modulus K_o = 185(7) GPa with a pressure derivative K_o'= 2.9(0.8). Furthermore, the data are compared with those of other ABO_4 compounds. The results show that the bulk modulus of HP-BiNbO_4(about 185 GPa) is slightly higher than that of tetragonal BiVO_4 and significantly greater than those of the tungstates and molybdates.     

High pressure X-ray diffraction study of SrMnO3 perovskite

Using a diamond anvil cell device and synchrotron radiation, the in-situ high-pressure structure of SrMnO3 has been investigated. At pressure up to 28.6 GPa, no pressure-induced phase transition is observed. The lattice parameters as a function of pressure is reported, and the relationship of the axial compression coefficients is β<,a>> β<,c>. The isothermal bulk modulus K<,298>=266(4) GPa is also obtained by fitting the pressure- volume data using the Murnaghan equation of state.     

High pressure X-ray diffraction study of CaMnO3 perovskite

Using a diamond anvil cell device and synchrotron radiation,the in-situ high-pressure structure of CaMnO3 has been investigated.In the pressure up to 36.5 GPa,no pressure-induced phase transition is observed.The pressure dependence on the lattice parameters of CaMnO3 is reported,and the relationship of the axial compression coefficients is βa >βc > βb.The isothermal bulk modulus K298=224(25)GPa is also obtained by fitting the pressure-volume data using the Murnaghan equation of state.     

Volume compression of CuCl to 7 GPa

The unit cell volume of CuCl as a function of pressure has been measured up to 7 GPa (giga Pascals). The compression behaviour is quite normal. The analysis of the compression data gives 40·3±1·5 GPa for the bulk modulus of the zinc blende phase. The zinc blende phase transforms to a tetragonal phase at 5·5 GPa, the volume change associated with the transformation being 12%. A comparison of the bulk modulus of CuCl with those of CuBr and CuI indicates that an anomaly exists in this group.     

Equation of state for technetium from X‐ray diffraction and first-principle calculations

The ambient temperature equation of state (EoS) of technetium metal has been measured by X-ray diffraction. The metal was compressed using a diamond anvil cell and using a 4:1 methanol-ethanol pressure transmitting medium. The maximum pressure achieved, as determined from the gold pressureEquation of state for technetium from X-ray diffraction and first-principle calculations scale, was 67 GPa. The compression data shows that the HCP phase of technetium is stable up to 67 GPa. The compression curve of technetium was also calculated using first-principles total-energy calculations. Utilizing a number of fitting strategies to compare the experimental and theoretical data it is determined that the Vinet equation of state with an ambient isothermal bulk modulus of B_0T=288 GPa and a first pressure derivative of B′=5.9(2) best represent the compression behavior of technetium metal.     

High-pressure radial X-ray diffraction study of osmium to 58 GPa

Nonhydrostatic compression behavior of osmium (Os) was investigated up to 58.2 GPa using radial X-ray diffraction (RXRD) together with lattice strain theory in a diamond-anvil cell. The apparent bulk modulus of Os derived from RXRD data varies from 262 GPa to 413 GPa, depending on Ψ, the orientation of the diffraction planes with respect to the loading axis. Fitting to the third-order Birch-Murnaghan equation of state, the RXRD data obtained at Ψ = 54.7° yields a bulk modulus K₀ = 390 ± 6 GPa with pressure derivative K^′ ₀ fixed at 4. The ratio of differential stress to shear modulus t/G ranges from 0.024 to 0.029 at the pressures of 15.7–58.2 GPa. The yield strength was observed to increase with compression and reach the value of 11.7 GPa at the highest pressure. This confirms that Os is the strongest known pure metallic material compared with the reported stiff elemental metals such as W, Mo and Re. It was found that the apparent c/a ratio changed with the nonhydrostatic compression, as well as the orientation Ψ in our experiments. Moreover, the aggregate moduli of Os at high pressure were determined from the RXRD measurements.