纳米SiO2形成柯石英的p-T相图

 使用纳米SiO₂粉体为原料,在2.0～4.2 GPa、150～1200 ℃范围内进行了一系列的高压高温实验研究,得到了该压力温度范围内晶化产物α-石英与柯石英的p-T相图,而且该相图中的相边界在650 ℃以下斜率为负,在650 ℃以上基本水平。通过X射线衍射仪（XRD）、Raman光谱仪（Raman）、傅立叶红外光谱仪（FT-IR）、DSC-TGA差热分析仪（TG-DTA）-等表征手段,发现纳米SiO₂原粉中水分（包含Si－OH和吸附水）的存在能显著降低合成柯石英的温度和时间,在4.2 GPa压力下得到了目前合成柯石英的最低温度190 ℃。常压下,合成的柯石英在800 ℃以下能够稳定存在,在1 000 ℃以上转化为α-方石英。     

高压下α-石英和柯石英的相变行为

利用金刚石压腔和同步辐射X射线衍射技术,对α-石英和柯石英在常温高压下的相变行为进行了研究。实验结果表明:α-石英在约23 GPa开始发生结构相变,在约44 GPa相变完成,直至59 GPa仍能观察到结晶态;柯石英在约22 GPa转变为柯石英-Ⅱ相,高于36 GPa时,继续发生结构转变,直至59 GPa仍有结晶态;氖气和氩气所提供的不同静水压条件对α-石英和柯石英的高压相变行为影响不大。实验结果为进一步厘清二氧化硅物相的压致相变行为和相变机制提供了实验支撑。     

非晶态SiO2的高温高压转变研究

利用金刚石对顶砧高压装置和激光双面加热技术, 以经700°C热处理后的吉林长白山硅藻土作为非晶态SiO₂样品,在0—4GPa, 1000—1300K温压条件下开展同步辐射X射线衍射原位测试(EDXD方法), 研究非晶态SiO₂在高温高压条件下的结晶转变方式. 测试结果表明, 在0.8—2.4GPa, 1000—1300K温压条件下, 非晶态SiO₂转变成α-石英而非β-石英或方石英, 其结晶温度较常压下非晶态SiO₂晶化所需温度明显较低, 表明压力有利于降低非晶态SiO₂转变的活化能, 并与常压下的结晶产物不同. 在3—4GPa, 1300K温压条件下, 非晶态SiO₂和石英均转变成了柯石英.     

应用于扫描探针显微镜的石英音叉机械模型研究

石英音叉作为力传感器广泛地应用于各种扫描探针显微镜,主要涉及石英音叉的同相振动和反相振动两种振动模式.通过实验方法和有限元仿真方法对石英音叉的两种振动模式进行研究,发现石英音叉的双臂之间以及双臂与音叉的基部之间都存在耦合作用,双臂之间的耦合使音叉的反相共振频率升高,双臂与基部之间的耦合使音叉的同相共振频率降低.针对两种振动模式的动态特性建立了石英音叉的机械模型并进行合理简化.简化模型是一个四弹簧三质点系统,计算了简化模型的参数.通过一个音叉臂等效质量变化与音叉反相共振频率变化之间的定量关系证明了简化机械模 关键词： 扫描探针显微镜 石英音叉 振动模式 机械模型     

VISAR条纹常数的检测方法

 提出了4种可检测VISAR条纹常数的方法。在这4种方法中,DISAR和VISAR的混合测试系统对VISAR条纹常数的测定精度高,适用范围广,是一种普适方法。在不具备DISAR仪器以及DISAR、VISAR混合测试技术的条件下,也可以通过VISAR延迟时间的测定、加窗熔石英对称碰撞产生的相对标准速度源以及标检过的VISAR仪器对VISAR条纹常数进行检测。     

密集波分复用石英光纤通信系统中受激Raman散射的稳态分析模型

假设石英光纤的Raman增益谱为线性谱,并给出了拟合直线.以此为基础,得到了前向N信道 受激Raman散射稳态耦合波方程的解析解.这个解析解是在考虑了N个信号光之间串话下得到 的,它适用于任意功率大小的信号光和任意信道间隔排列的情况.N个信号光在石英光纤中经 过受激Raman散射作用后,具有以下特点：在传输过程中,任意两信道的信号光光子通量的比 值随光纤的有效互作用长度、总的输入光子通量和两信道频率间隔按指数规律变化.解析解 与数值解进行了比较,两者取得了很好的一致. 关键词： 受激Raman散射 密集波分复用 石英光纤 Raman放大     

熔石英棒-光纤组合型相位共轭镜的研究

提出了一种由大口径的熔石英棒和较大芯径的光纤组成的相位共轭镜.在光纤中产生的斯托克斯(Stokes)种子光经由熔石英棒放大后输出.该相位共轭镜可以用于高重复频率激光系统中以改善激光光束质量.实验中,在重复频率100 Hz的情况下,最大获得了42.05%的受激布里渊散射反射率,光束质量从3降低到1.6;在重复频率400 Hz的情况下,光束质量从4降到了1.7.根据实验条件建立的理论模型经数值求解后与实验结果拟合较好,并由理论推导提出了一种提高该复合型相位共轭镜工作状态的有效方法.     

钨合金的高压本构研究

通过静高压实验、动高压实验及理论计算相结合的方法，确定了钨合金的一种高压本构方程 （Steinberg模型方程）中的各参数.用数值模拟计算方法，采用几种不同的本构模型进行了 计算，并与实测结果进行了比较.结果显示，确定的高压本构方程计算值与实测值符合最好. 关键词： 高压本构方程 Steinberg 模型 数值模拟计算 粒子速度波形     

熔石英棒-光纤构成的新型复合相位共轭镜的实验和理论研究

提出了一种新型的由熔石英棒和石英光纤组成的复合型相位共轭镜,其可运用于高重复频率激光输入系统中以改善光束质量.该复合相位共轭镜具有较高的受激布里渊散射反射率和受激布里渊散射损伤阈值以及较低的受激布里渊散射阈值等优点.实验中,在100 Hz重复频率下,最大获得了42.05%的受激布里渊散射反射率.根据实验条件,由耦合波方程及边界条件得到的物理模型,经数值求解后得到的结果和实验符合较好.且由理论结果提出了一种提高该复合型相位共轭镜工作状态的有效方法. 关键词： 复合型相位共轭镜 受激布里渊散射 熔石英 耦合波方程     

单模石英光纤中连续波泵浦SRS谱的演化

利用连续波掺Yb双包层光纤激光器为泵浦源,对单模石英光纤中受激Raman散射谱的形成过程进行了实验研究结果表明,由自发Raman散射向受激Raman散射演化的过程中Stokes谱宽度不断变窄当Stokes波信号功率较强时,在Raman光谱内部会出现能量红移现象,使Stokes光谱峰值相对于泵浦波的频移量从440cm^-1转化到490cm^-1.     

α-β石英相变的应变参数计算及其地质意义

 利用已有的α和β石英压缩性、热膨胀性、弹性及相变温度压力资料，计算了α-β石英相转变时，α和β石英的晶胞参数。依据虎克定律以及高压下β石英的弹性参数，估算了α-β石英相转变时的应变、应力和应变能。结果表明，在0~1.1 GPa条件下，随压力升高，α-β石英相变的线应变介于-0.006~0.005之间，体应变介于-0.016~0.012之间，应力介于-0.46~0.14 GPa之间；应变能介于965~2 760 kJ/m³之间。压力为0.5 GPa左右时，α-β石英相变的应变、应力和应变能均达到最小值。在此基础上，讨论了壳内大规模酸性岩浆活动引起的α-β石英相变对壳内岩石的作用。     

Brillouin scattering of vitreous silica under high pressure

The pressure dependence of Brillouin spectra of vitreous silica exhibits a maximum in the hypersonic absorption and a minimum in the sound velocity at about 2 GPa almost independent of temperature. The results are discussed on the basis of relaxing defects residing in double-well potentials with a Gaussian distribution of barrier heights and a Lorentzian distribution in the asymmetry. Our analysis suggests that both the distribution functions are strongly changed at higher pressures. It is striking that a phase boundary between α-quartz and coesite exists just at the pressure where absorption and sound velocity of vitreous silica pass their extremum. This might be a hint that a corresponding structural change also occurs in the glass.     

Luminescence of polymorphous SiO2

The luminescence of self-trapped exciton (STE) was found and systematically studied in tetrahedron structured silica crystals (α-quartz, coesite, cristobalite) and glass. In octahedron structured stishovite only host material defect luminescence was observed. It strongly resembles luminescence of oxygen deficient silica glass and γ or neutron irradiated α-quartz. The energetic yield of STE luminescence for α-quartz and coesite is about 20% of absorbed energy and about 5(7)% for cristobalite. Two types of STE were found in α-quartz. Two overlapping bands of STEs are located at 2.5–2.7 eV. The model of STE is proposed as Si–O bond rupture, relaxation of created non-bridging oxygen (NBO) with foundation of a bond with bridging oxygen (BO) on opposite side of c or x,y channel. The strength of this bond is responsible for thermal stability of STE. Similar model of STE was ascribed for coesite and cristobalite with difference related to different structure. STE of Silica glass is strongly affected by disordered structure.     

高压下β-FeOOH纳米固体结构转变的研究

 以化学水解法合成的β-FeOOH纳米微粉（平均粒径在12 nm左右）为原料，分别在0.0~4.5 GPa和200~350 ℃的压力和温度范围进行冷压和热压处理。实验结果表明，冷压对β-FeOOH纳米固体的结构没有明显影响，但却使它的热致相变（从β-FeOOH相到α-Fe₂O₃相）温度从常压下的203.8 ℃提高到4.5 GPa压力下的274 ℃，接近常规体相材料的相变温度。而在一定的热压条件处理下，首次发现了从β-FeOOH相到α-FeOOH相的结构转变，并在4.5 GPa、200 ℃的热压条件下得到了转变过程中的一个新的亚稳相。从压力和温度对纳米微粒的作用角度，对上述实验结果进行了讨论。     

Crystallization of mesoporous silica SBA-15 in a high pressure hydrothermal environment

Mesoporous silica SBA-15 (with ～6?nm pore size and ～6?nm wall thickness) was exposed to a hydrothermal environment at 2 and 5?GPa. The p,T quenched products were investigated by powder X-ray diffraction and transmission electron microscopy. Infrared spectroscopy and thermogravimetric analysis of a sample subjected to 5?GPa at room temperature suggests functionalization of both inner and outer pore surface by silanol. Partial transformation to nano-sized (20–50?nm) coesite crystals with nonfaceted morphology was observed during short equilibration times of 2?h at 125°C, which is significantly below the melting point of water (～250°C). Untransformed SBA-15 maintained intact pore structure. At 175°C and during 8?h, SBA-15 transformed completely into faceted coesite crystals with dimensions 100–300?nm, suggesting Ostwald ripening and thus significant mass transport in the solid water environment. At 2?GPa the melting point of water is near 70°C. Partial transformation to nano-sized α-quartz was observed at 65°C and during 2?h. Untransformed SBA-15 partially pore collapsed. The reduced pore stability of SBA-15 at 2?GPa is attributed to the presence of liquid water in the pores due to melting point depression of confined water.     

Temperature-induced phase transition in quartz nanocrystals dispersed in pseudotachylite

The size and concentration of α-quartz nanocrystals dispersed in samples of pseudotachylite and the internal stresses in these nanocrystals have been determined using infrared spectroscopy in the temperature range 300–800 K. Pseudotachylite is a product of intense crushing of granite that undergoes in the Earth’s crust faults. It has been found that the size of the nanocrystals is ～20 nm and does not depend on temperature. As the temperature increases, their concentration decreases monotonically and tends to zero at ～650 K. This process is paralleled by a growth of the concentration of β-quartz nanocrystals. The α-quartz nanocrystal concentration regains its initial level with decreasing temperature. Thus, the α → β phase transition in quartz nanocrystals in pseudotachylite starts at temperatures lower by ～500 K than that in the bulk of the macrocrystal (846 K), and is stretched by ～350 K. At room temperature, the unit cell of nanocrystals is compressed by surface tension forces. These forces retard the α → β phase transition. The thermal expansion coefficient of nanocrystals is larger than that of macrocrystals, which entails a decrease of compression and a monotonic decrease of the concentration of α-quartz nanocrystals with increasing temperature.     

Ionic liquid; possibility of protein-preserving solvent under high pressure

We have investigated the pressure-induced phase transition behavior (～3.0 GPa) of aqueous 1-butyl-3-methylimidazolium chloride ([bmim][Cl]) solutions with N-methylacetamide (NMA), which is a simple protein model compound, using Raman spectroscopy. From Raman spectral changes and optical observation in the sequence of elevated pressure, we found that the aqueous [bmim][Cl] solution with NMA in the water-rich condition induces the high pressure crystallization at 2.6 GPa. On the other hand, in the [bmim][Cl]-rich condition, high pressure crystalline phase was not observed even up to 3.0 GPa. Our results show that the aqueous [bmim][Cl] solution in the ionic liquid-rich condition along with the use of pressure has a potential for protein-preserving solvent.     

High pressure induced phase transformation of SiO2 and GeO2: difference and similarity

We report high pressure polymorphism of SiO₂ and GeO₂ at room and high temperatures. It was found that kinetics has a large effect on pressure induced phase transitions of SiO₂ and GeO₂. The high pressure behavior of SiO₂ and GeO₂ polymorphs depends on the starting material and pressure–temperature history. Our studies show that SiO₂ and GeO₂ have a common sequence of high pressure, high temperature structural transformations when the same type of starting material (amorphous or α-quartz) was used: (amorphous or α-quartz)⇒d-NiAs⇒rutile⇒CaCl₂⇒α-PbO₂⇒pyrite (Pa-3) types. In the case of cristobalite as starting material, the α-PbO₂-type phase can be synthesized directly from the high pressure room temperature phase omitting rutile- or CaCl₂-type structure. The crystallization of the d-NiAs phase in a narrow temperature interval 1000–1300 K can be used as an indicator of presence of a cation disordered network in both SiO₂ and GeO₂ materials at high pressure before heating.