活塞圆筒装置压力盘样品组装的温度测定和热结构分析

活塞圆筒是目前使用最广泛的固体介质高温高压装置,样品组装方式和组装件的材料类型决定了高压腔体内部的热结构特征。在0.5、1.0、1.5GPa压力下、800~1 400℃范围内,采用改进的双热电偶法、尖晶石反应测温法对QUICKpress型活塞圆筒的13mm压力盘的样品组装进行了温度测定,通过获得的实验数据并结合傅里叶热传导模拟结果进行了热结构分析。实验结果表明:(1)热峰位置均位于有效石墨炉中心以下,即靠近钢塞一侧,20℃温差范围的热点区轴向分布区域大小介于2.8~5.2mm,其热梯度为7.7~13.0℃/mm,而非热点区热梯度为42~83℃/mm;(2)随着温度或压力升高,热峰倾向于朝有效石墨炉中心靠拢,同时伴随着炉内热梯度增大和热点区变小,温度的影响更为显著。还对活塞圆筒压力组装的热结构的影响因素及相关问题进行了探讨。     

First-order character of the displacive structural transition in BaWO₄

Nearly all displacive transitions have been considered to be continuous or second order,and the rigid unit mode(RUM) provides a natural candidate for the soft mode.However,in-situ X-ray diffraction and Raman measurements show clearly the first-order evidences for the scheelite-to-fergusonite displacive transition in BaWO 4:a 1.6% volume collapse,coexistence of phases,and hysteresis on release of pressure.Such first-order signatures are found to be the same as the soft modes in BaWO 4,which indicates the scheelite-to-fergusonite displacive phase transition hides a deeper physical mechanism.By the refinement of atomic displacement parameters,we further show that the first-order character of this phase transition stems from a coupling of large compression of soft BaO 8 polyhedrons to the small displacive distortion of rigid WO 4 tetrahedrons.Such a coupling will lead to a deeper physical insight in the phase transition of the common scheelite-structured compounds.     

Raman Investigation of BaWO4-II Phase under Hydrostatic Pressures up to 14.8GPa

The BaW04-17 phase is synthesized at 5.0 GPa and 610~C with a cubic-anvil apparatus and identified by XRD. Raman scattering measurement is carried out to investigate the phase behaviour of a pure BaW04-Ⅱ phase （space group P21/n, Z = 8） under hydrostatic pressures up to 14.8 GPa at ambient temperature. In each spectrum recorded for this phase, 27 Raman modes are observed, and all bands shift toward higher wavenumber with a pressure dependence ranging from 3.8 to 0.2 cm- 1/GPa. No pressure-driven phase transition occurs in the entire pressure range in this study. Our results indicate that the previously reported high pressure phase of Ba WO4 at pressure above about 10 GPa and room temperature （Errandonea et al. Phys. Rev. B 73（2006）224103） is not the BaW04-Ⅱ phase.     

First-order character of the displacive structural transition in BaWO4

Nearly all displacive transitions have been considered to be continuous or second order, and the rigid unit mode （RUM） provides a natural candidate for the soft mode. However, in-situ X-ray diffraction and Raman measurements show clearly the first-order evidences for the scheelite-to-fergusonite displacive transition in SaWO4： a 1.6% volume collapse, coexistence of phases, and hysteresis on release of pressure. Such first-order signatures are found to be the same as the soft modes in BaWO4, which indicates the scheelite-to-fergusonite displacive phase transition hides a deeper physical mechanism. By the refinement of atomic displacement parameters, we further show that the first-order character of this phase transition stems from a coupling of large compression of soft BaOs polyhedrons to the small displacive distortion of rigid WO4 tetrahedrons. Such a coupling will lead to a deeper physical insight in the phase transition of the common scheelite-structured compounds.     

江西岩背火山侵入杂岩的地球化学特征和成因

本文对江西岩背火山侵入杂岩作了较详细的同位素和微量元素研究。它们具有相似的结晶年龄,较高的(~(87)Sr/~(86)Sr)_i和δ~(18)O值,高的~(207)Pb/~(204)Pb值,低的ε_(Nd)值和古老的Nd模式年龄。同时,它们还具有高的Rb/Sr和F/Cl值,弱的铈负异常和强的铕负异常。这些特征清楚表明,岩背火山侵入杂岩是同源岩浆演化的产物,其初始岩浆是由早、中元古代变质沉积岩经部分熔融形成的。