黏弹性流体驱替微孔道中残余油滴的水动力学机制

选取上随体Maxwell本构方程建立黏弹性流体在微孔道中的流动方程,运用控制体积法和交替方向隐式(ADI)方法得到流场的数值解,计算流动的速度场和应力场,分析不同弹性驱替液作用在残余油滴上的驱替力,以及不同弹性驱替液驱替时残余油滴的变形,从水动力学角度探索聚合物溶液所具有的弹性驱替残余油滴的水动力学机制.结果表明:与无...     

延长油田长7致密油储层流体可动用性特征

为准确评价延长油田长7致密油储层流体可动用性,利用核磁共振结合高速离心对延长油田长7致密油储层T2截止值进行标定,对可动流体百分数和不同级别大小孔隙中流体控制量进行深入分析。对比了中国典型致密油区的可动流体百分数分布特征。通过CT、高压压汞、恒速压汞,从微观孔隙结构角度详细分析了流体可动用性的内在控制因素。研究表明:延长油田长7致密油储层饱和水状态T2图谱可分为4类,T2截止值介于1.7~11 ms之间。可动流体主要来自亚微米空间,储层60%以上的流体控制于纳米级空间。0.05×10-3μm2以下储层可动流体百分数低于30%,储层难以动用。延长致密油可动用性好于大庆和大港致密油储层。储层致密是影响储层流体可动用性的关键因素。     

水平环缝内低温工质自然对流传热实验装置的研发

针对工业领域中常见的低温工质自然对流传热现象,该文研发了一套用于水平环缝内低温工质自然对流传热实验的装置,介绍了实验装置的结构和原理,并进行了初步的性能测试。结果表明,利用该装置测得的实验数据精度较高,能够满足相关实验要求。该装置可同时用于水平同心和偏心环缝内低温工质自然对流传热实验研究。     

基于流体力学理论的全尾砂浆管道输送流变性能

为研究充填料浆流变性能,利用流体力学原理,通过L型管道自流输送实验对其在管道中流动的力学特性进行了分析. 结果表明:料浆浓度、流量和管径对料浆管输阻力和充填倍线大小的作用程度不同,其中料浆浓度影响尤为显著. 在能够实现自流输送的充填倍线合理条件下,采场充填时,当结合充填能力确定流量和管径后,可通过充填站调节制浆浓度以使充填材料在管道输送、采场中沉降、抗离析、脱排水、固结硬化和力学性能等方面表现良好.     

Anisotropic thermal conductivity of magnetic fluids

Considering the forces acting on the particles and the motion of the particles, this study uses a numerical simulation to investigate the three-dimensional microstructure of the magnetic fluids in the presence of an external magnetic field. A method is proposed for predicting the anisotropic thermal conductivity of magnetic fluids. By introducing an anisotropic structure parameter which characterizes the nonuniform distribution of particles suspended in the magnetic fluids, the traditional Maxwell formula is modified and extended to calculate anisotropic thermal conductivity of the magnetic fluids. The results show that in the presence of an external magnetic field the magnetic nanoparticles form chainlike clusters along the direction of the external magnetic field, which leads to the fact that the thermal conductivity of the magnetic fluid along the chain direction is bigger than that along other directions. The thermal conductivity of the magnetic fluids presents an anisotropic feature. With the increase of the magnetic field strength the chainlike clusters in the magnetic fluid appear to be more obvious, so that the anisotropic feature of heat conduction in the fluids becomes more evident.     

川东北下三叠统飞仙关组白云岩成因——来自岩石结构的证据

以岩石结构分析为基础,结合自云石有序度和Sr含量及Sr同位素等资料,对川东北下三叠统飞仙关组广泛发育的白云岩成因进行研究,从中识别出准同生白云岩和埋藏白云岩两种成因类型.其中具有储集意义的仅为多期次埋藏交代成因的成岩白云岩,包括鲕粒白云岩和晶粒白云岩两种主要结构类型.综合成岩埋藏白云岩的结构与有序度和Sr含量及Sr同位素地球化学特征,可将埋藏白云化过程划分为早、中、晚三个成岩阶段.各阶段储层白云岩的岩石结构虽然有显著的差别,但微量元素Sr含量和Sr同位素地球化学特征具有明显的相似性与周源性,不仅显示了埋藏白云化流体为具备早三叠世海水Sr同位素组成特征的海源地层水而与大气淡水无关,同时反映了多期次的埋藏白云化作用是发生在继承性发展演化的过程中的和相对封闭的体系中,因此,对储层的发育和天然气的聚集成藏都非常有利.     

黑龙江鹿鸣钼矿床流体包裹体特征

鹿鸣钼矿床位于小兴安岭-张广才岭成矿带中南部.钼矿体产于二长花岗岩与花岗斑岩的接触带内,钼矿化主要载体为石英脉,呈脉状、网脉状分布于矿体的内部.研究了主要含矿石英脉体中流体包裹体的特征,结果表明:包裹体相态类型主要为气液两相,矿床的成矿温度峰值分别为400,220℃,盐度为19%~144%,成矿压力平均为18MPa,成矿深度为09~28km,成矿流体成分富含CO2,H2O,CH4等多种气态组分,以及Na+,Ca2+,SO2-4,Cl-液态组分;矿床初始流体来源于岩浆热液,成矿后期受大气降水的混入.矿床成因类型应划归为与中酸性侵入岩浆活动有关的中高温斑岩型钼矿床.     

偶极硬球流体第二维里系数的计算

在《热力学与统计物理》中,往往涉及到原子流体的维里系数的计算.作为研究偶极流体相行为的一个补充,同时为了加强学生对理论推导能力的训练,研究了偶极硬球流体的第二维里系数.首先把偶极硬球流体粒子间的各向异性势能写成旋转不变的形式,进而把相应的玻尔兹曼因子作泰勒展开,代入第二维里系数的公式中进行逐项积分计算,最后得到了偶极硬球流体第二维里系数的解析表达式.     

Coexisting brittle-ductile fracturing mechanisms in fault zones of the upper crust level

Microstructural and sub-microstructural studies are conducted on calcite marble taken from the Autseib fault zone, Damara region, Namibia, SW Africa. The characteristic microstructural styles of rocks deformed in the upper crust are analyzed, including mainly the two microstructural contrasts in the tectonites: (i) coarse grains (centimeter scale) in primary rocks and in deformed clasts and extremely fine grains (micron scale) in the matrix; and (ii) macroscopic cataclastic (brittle) and microscopic mylonitic (ductile) textures. The coexistence of the macroscopic brittle and microscopic ductile textures is better explained by deformation through a comprehensive association of intragranular twinning and kinking, intraand intergranular ductile fracturing, and pressure solution along grain boundaries. Ductile fracturing, i.e. fracturing triggered and accommodated by twinning and fluid-enhanced dislocation creep and dynamic recrystallization, is among the most important mechanisms of rock deformation in the shallow crust, while grain size reduction and dynamic recrystallization are primarily nucleated and distributed due to the incoherencies along some boundaries, e.g. kink band boundaries, fractures and grain boundaries in the deformed grains.     

具阀门梯度的平面流体的径向流动

研究了具阀门梯度的平面径向流动卢的一类自由边值问题，首先给出了问题的数学模型，接着用等价折舅物拟变分不等式的研究，得出了该自由边值问题的古典解的存在唯一性。