K-rich lamellar exsolution in clinopyroxene： Constraint on the depth of peridotite source at Zhimafang

The oriented lamellar K-rich exsolutions within clinopyroxene host were recognized in garnet peridotite massif at Zhimafang in the Sulu ultrahigh pressure metamorphic terrane, eastern China. EMP and TEM analyses revealed that the composition and the index of electron diffraction for this exsolution are corresponding with phlogopite, and the shape is the lamellae with 1 μm in width and 5 to 30 μm in length. Moreover, the topotaxy is that the (001) of K-rich exsolution parallels to (I00) of the clinopyroxene host. The electron diffraction analyzing shows the exsolution is of a 1M polymorphism. The high-resolution lattice fringe image displays the stack features along [001], which only a layer mineral shows. We conclude that the clinopyroxene with IM and K-rich exsolution was probably derived from mantle depths over 240 km, thus resulting from decompressional exsolution in the initial stage of slab exhumation.     

A new model for analyzing laminar forced convective enhanced heat transfer in latent functionally thermal fluid

In this paper, a new model to analyze laminar forced convective enhanced heat transfer in latent functionally thermal fluid is developed. The main characteristics of the model are- i) a new formula of the specific heat at constant pressure is used; ii ) a real heat transfer process is considered; that is, heat transfer processes occur not only between working fluid and microcapsules, but also between the mixture and tube wall; iii) the new method, which combines the newly developed axisymmetrical dual reciprocity boundary element method (DRBEM) with finite difference method (FDM), is used to solve the control equations of this problem. The new model is validated by experimental data. Some new physical results on the variational characteristics of the specific heat at constant pressure with space and time during phase-change process, the time-marching history of the phase-change interfaces and so on are obtained. Several main physical factors that affect enhanced heat transfer in latent functionally thermal fluid are numerically analyzed. Some new understandings for the mechanism of enhanced heat transfer in the functionally fluid are obtained.     

用分段回归方法计算孔隙结构的分形维数

储层岩石的孔隙空间具有良好的分形特征,孔隙结构的分形维数可以用来定量描述孔隙结构的复杂程度。应用分形几何的原理,推导了储层岩石不同孔隙分布和毛细管压力曲线的分形几何模型。根据毛管压力曲线资料,用分段回归的方法计算了不同孔隙结构的分形维数。计算结果表明,用分段回归方法计算孔隙结构的分形维数能更好地反映孔隙结构的实际情况。若孔隙大小相差不大,孔隙结构的分形维数相等或比较接近;若孔隙大小相差较大、非均质性较强,得到的孔隙结构分形维数不同。     

Research on effects of hydrostatic pressure on the dielectric property of Pb(Zn<Subscript>1/3</Subscript>Nb<Subscript>2/3</Subscript>)O<Subscript>3−</Subscript>BaTiO<Subscript>3−</Subscript> PbTiO<Subscript>3</Subscript> relaxor ferroelectric ceramics

The dielectric properties of Pb(Zn1_1/3Nb_2/3)O₃₋ BaTiO₃₋PbTiO₃ relaxor ferroelectric ceramics near the rhombohedral and tetragonal phase boundary were investigated under hydrostatic pressure. It was found that hydrostatic pressure made their phase transition temperature T _c and the peak temperature T _m decreased, and the frequency dispersion and relaxor behavior enhanced. In these disorder systems of composite pervoskite structures, there appeared polar clusters or nanodomains. The unique physical characteristics, which made the relaxor behavior enhanced, is that the correlation length among these nanodomains decreases greatly with the pressure increasing.     

微重力条件下气／液两相流压降实验研究

利用俄罗斯IL-76失重飞机对微重力条件下方形截面管道内的水/气两相流压降进行了实验研究．利用本次微重力气／液两相流压降实验结果对一些目前常用的基于地面常重力实验结果的两相流压降预测模型(均相模型、Lockhart-Martinelli—Chisholm模型和Friedel模型)在微重力条件下的适用性进行了评估．比较发现,均相模型和Lockhart-Martinelli—Chisholm模型预测结果和实验数据差异很大;而Friedel模型的预测结果尽管也与实验数据有着明显的差别,但在这些模型中是误差最小的．因此,可以利用Friedel模型来对微重力气／液两相流压降进行初步预估,而新的、更精确的模型将依赖于更有物理意义的分析方法及不同重力条件下气／液两相流压降实验的结果．     

大坝背管裂缝宽度计算公式的改进

指出了用现有裂缝理论计算钢衬钢筋混凝土压力管道裂缝宽度的局限性.进一步完善了"外部管壁”的力学模型,并据此导出了精确度更高的半理论半经验公式,该公式考虑了混凝土保护层内外的裂缝宽度差异.最后给出了算例.     

岩石单轴与三轴CT尺度裂纹演化过程观测

结合使用专用三轴压力仪与CT扫描仪,对砂岩和粉砂岩分别进行压缩试验并获得了系列CT图像。发现单轴压缩和三轴压缩时岩石试件均经历压密、扩容、CT尺度裂纹萌生、扩展、扩张、贯通和岩石宏观破坏阶段。在压密阶段和扩容阶段,CT图像无明显变化。采用密度损伤增量定量描述细观裂纹演化的集合效应。在CT尺度裂纹演化阶段,从CT图像出发描述裂纹的空间位置、形态、运动方向分析CT尺度裂纹演化对于岩石变形和强度的影响。裂纹模式图可揭示CT裂纹演化的规律。CT裂纹演化的基本特点是扩展与扩张的交替性。三轴条件下CT裂纹与主应力夹角较大,裂纹面较平直,裂纹扩张困难,呈现剪切破坏特点。     

Structural stability of infinite-layer CaCuCO<Subscript>2</Subscript> under high pressure

Since the discovery of high temperature supercon-ductivity by Bednorz et al. in 1986[1], many series of cu- prate superconductors have been synthesized. Critical temperature has been improved continuously. But no verdict has been given upon what mechanism causes su- perconductivity. CaCuO2 conductive layers are the parent structure of the high Tc cuprate superconductors, such as Cu-12 (n-1)n[2], Tl-12(n-1)n[3] and Hg-12(n-1)n[4,5] super- conductor families. In 1988, infinite-layer (Ca0.86S…     

浅谈普通箱式压滤机技术改造

介绍了一种经济、有效地将隔膜式压滤机的压滤过滤技术嫁接到现用普通箱式压滤机上的方法,在一定程度上克服了普通箱式压滤机对入料性质变化适应性差的问题。     

兰州地区某工程垃圾地基土处理方法研究

对兰州地区某工程垃圾地基土进行了表层开挖、灰土紧密和换填夯实的综合技术处理.利用原位现场静载荷试验,研究了垃圾土处理前后的变形性能、承载力和变形机理,为工程基础选型提供了依据.