铂纳米粒子和锰卟啉修饰的聚苯胺新材料的制备及表征

借助循环伏安电化学聚合制备了聚苯胺(PANi)/MnT1239卟啉复合材料,再利用还原恒电位沉积法负载铂纳米粒子(Pt NP),最终制备了聚苯胺/MnT1239卟啉/铂纳米粒子复合材料.电沉积铂之后聚苯胺/MnT1239卟啉材料发生明显样貌变化,棒状结构平均直径从90 nm增加到200 nm,材料具有较大的表面积,空间可负载性好.铂纳米粒子平均尺寸在20 nm,附着均匀,氧化峰电流在0.2 V处达到7.4 mA,电化学性能优良.     

Phase Transition and EOS of Marmatite （Zn0.76Fe0.23S） up to 623K and 17 GPa

In situ energy dispersive x-ray diffraction for natural marmatite （Zn0.76Fe0.23S） is performed up to 17. 7 GPa and 623 K. It is fit, ted by the Birch-Murnaghan equation of state （EOS） that Ko and α0 for marmatite are 85（3）GPa and 0.79（16）＊10^-4 K^-1, respectively. Fe^2＋ isomorphic replacing to Zn^2＋ in natural crystal is responsible for high bulk modulus and thermal expansivity of marmatite. Temperature derivative of bulk modulus （OK/OT）p for marmatite is fitted to be -0.044（23） GPaK^-1. The unambiguous B3-B1 phase boundaries for marmatite are determined to be Pupper（GPa）= 15.50 - 0.016T（℃） and Plower （GPa）=9.94-0.012T（℃） at 300-623K.     

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。     

纳米级无机聚钼酸盐“二级有序聚集体”

介绍了纳米级水溶性无机聚钼酸盐分子的逐步生长合成, 对近年来水溶液中纳米级无机聚钼酸盐分子的奇特自聚集行为进行了简述, 从两亲分子“有序聚集体”概念的角度, 提出了水溶性纳米级无机聚钼酸盐“二级有序聚集体”的概念.     

Phase Transition and EOS of Cinnabar （α-HgS） at High Pressure and High Temperature

Phase relations and equation of state （EOS） of natural cinnabar （α-HgS） are investigated by high-pressure and high-temperature synchrotron x-ray powder diffraction. The unambiguous cinnabar-rocksalt structure phase boundaries are determined to be PI （GPa）=15.54- 0.014T（℃） and Pupper（GPa）= 23.84- 0.014T（℃） at 300-623K. With K1 fixed at 4, we obtain K0 = 37（4） GPa, （aK/aT）p= -0.025（2） GPaK-1, and α0 = 3.79（20） × 10-5 K-1 for the cinnabar phase of α-HgS. The （aK/aT）p and α0 of cinnabar phase are obtained for the first time. A nearly isotropic compression of cinnabar phase is observed by linear regressions.     

石榴子石族矿物状态方程研究进展

石榴子石是重要的造岩矿物,是上地幔、地幔转换带以及(超)高压变质岩中最重要的造岩矿物之一,研究其状态方程对于约束地球内部物质组成和状态、正确理解大洋岩石圈俯冲板块和地幔动力学过程具有重要意义。文中综述了20世纪70年代以来石榴子石p-V(压强-晶胞体积)和p-V-T(压强-晶胞体积-温度)状态方程的研究进展,重点讨论高温高压条件下石榴子石的稳定性以及组分变化和含水对热弹性参数的影响。最后简略概括石榴子石状态方程研究存在的问题,并指出发展方向。     

Synchrotron X-ray diffraction study of phenacite at high pressure

We report the results of a natural phenacite from 0 to 30.9 GPa using in situ angle-dispersive X-ray diffraction and a diamond anvil cell at the National Synchrotron Light Source, Brookhaven National Laboratory. Over this pressure range, no phase change or disproportionation has been observed. The isothermal equation of state was determined. The values of V₀, K₀, and K₀′ refined with a third-order Birch-Murnaghan equation of state are V₀=1116.1±1.2 ų, K₀=223±9 GPa, and K₀′=5.5±0.8. Furthermore, we confirm that the linear compressibilities (β) along a and c directions of phenacite are elastically isotropic (β_a=1.50×10^-3 and β_c=1.34×10^-3 GPa^-1). Consequently, it can be concluded that the compressibility of phenacite under high pressures has been accurately constrained.     

Phase Relations and Pressure-Volume-Temperature Equation of State of Galena

The phase relations and pressure volume dependences of galena （PbS） under high pressure and high temperature are investigated by means of in situ observation using resistance heating in a diamond anvil cell and synchrotron radiation. The phase transition from NaCl type to TII type takes place at approximately 2.4 GPa. A fit to the high temperature third-order Bireh-Murnaghan equation of state yields an isothermal bulk modulus Ko = 37（3） GPa, and its pressure derivative K＇0 = 3.6（3）, the temperature derivative of the bulk modulus （ K/ T）p = -0.022（9） GPaK^-1, and the thermal expansion coeffeient α0 = 2.2（5） × 10^-5 K^-1 for TII-type galena. The linear compressibilities j3 along a, b and c directions of TII type is elastically anisotropic （βa = 3.4 × 10^-3 GPa^-1, βb = 1.4× 10^-4 GPa^-1 and βc = 1.6 × 10^-3 GPa^-1）. We obtain the temperature derivative of the bulk modulus （ K/ T）p and thermal expansion coefficient α0 for TlI-type galena for the first time.     

An in situ high-pressure X-ray diffraction experiment on hydroxyapophyllite

The compression behavior of a natural hydroxyapophyllite is investigated up to about 10.01 GPa at 300 K using in situ angle-dispersive X-ray diffraction and a diamond anvil cell at the High Pressure Experiment Station, Beijing Synchrotron Radiation Facility (BSRF). Over this pressure range, no phase change or disproportionation is observed. The isothermal equation of state is determined for the first time. The values of zero-pressure volume V0 , isothermal bulk modulus K0 , and K0 refined with a third-order Birch-Murnaghan equation of state are V0 = 1276.3±0.9  3 , K0 = 71±3 GPa, and K0 = 8±1. Furthermore, we confirm that the values of linear compressibility β along the a and c directions of hydroxyapophyllite are elastically anisotropic.