陶瓷ZrO2晶粒的透射电镜研究

运用透射电子显微镜中的暗场技术,观察和研究了陶瓷ZrO2多晶试样的晶粒形貌特征。在暗场像下能清楚观察到其晶粒呈六方片状,尺寸在305nm到410nm之间。与明场像相比,暗场像中晶粒的取向衬度更加明显,暗场技术是研究和观察多晶颗粒形态和尺寸的有力工具之一。     

岩心磁组构分析古水流方向的原理与应用

目的针对鄂尔多斯盆地天环拗陷南段延长组开展磁组构古水流研究。方法通过测量岩心样品的磁化率各向异性,分析磁组构特征,结合矿物岩石学特征综合开展岩心古水流方向判识。结果延长组碎屑岩的古水流方向为NE—SW,NW—SE和NS向,分别代表西南、西北和北部3个方向的物质供给。结论磁组构分析古水流方向与轻重矿物组合法判断的物源方向一致,表明应用磁组构分析钻井岩心古水流方向的方法是可行、可靠的,利用磁组构分析方法恢复古水流方向,判识物源具有较好的应用前景。     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

The equilibrium between diagenetic calcites and dolomites and its impact on reservoir quality in the sandstone reservoir of Kela 2 gas field

Based on the equilibrium theory of chemical reactions between water and rocks,this paper establishes a thermodynamic phase relationship diagram among calcites,dolomites and water solution under the condition of diagenesis based on the thermodynamic database of related minerals and fluids and dolomite's degree of order parameters.It has been discovered that the equilibrium between calcites and dolomites in the diagenetic environment is strongly impacted by temperature and the Ca/Mg ratios in groundwater,and that the dolomite's degree of order in the diagenetic environment is a function of crystallization temperature and time,not controlled by water solution.Hereby,the authors make a further analysis of the close relationship of chemical reaction between carbonate cements and pore water in the sandstone reservoirs of Kala 2 gas field in Kuche sag.It can be seen that there are different impacts on sandstone reservoir quality among the equilibrium system of calcites,dolomites and pore water at different depths of reservoirs.     

磁场中弱电离气体二维平板超音速边界层扰动演化研究

数值模拟了6种不同外加磁场下M∞=4．5、弱电离的二维平板边界层的基本流场及边界层中第二模态不稳定波的非线性演化。发现：外加磁场使边界层附近同—γ处的流向速度减小从而使边界层的厚度增加；很大程度地改变法向速度；壁面摩擦系数减小；很大程度地抑制第二模态不稳定波的增长。这些影响主要决定于外加磁场的强度，而对外加磁场的产生方式不很敏感。外加磁场的存在还使得压力产生波动，在边界层内，压力波峰的位置与流向磁场力绝对值极大的位置基本一致；在边界层外，压力波峰的位置滞后于流向磁场力绝对值极大的位置，并且离边界层越远，这种滞后就越明显。     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

Exchange-coupling interaction, effective anisotropy and magnetic property of nano-magnetic materials

The theories and models of exchange-coupling interaction between grains in nanocrystalline magnetic materials are introduced here. Their insufficiencies and distinctions from the experimental results are pointed out, and some revisions are made. The effects of the phase component ratio, the grain size and microstructure on the effective anisotropy and magnetic properties in the nanocomposite permanent materials and the improved models are discussed in detail.     

环流循环除尘系统分离柱内旋风流场分析

由柱坐标系下的Navier-Stokes方程出发,建立了环流循环除尘系统分离柱内流速场新的数学模型,利用具有成熟使用经验的加权残值法对流场进行求解,并与实验结果进行了比较。结果表示,所采用的数学模型和计算方法是可行的。     

乌五井区克拉玛依组油藏开发效果分析

目的提高乌5井区克拉玛依组油藏注水开发效果。方法在充分认识油藏静态地质特征的基础上,利用压力测试、油井产液剖面、注水井吸水剖面等测试结果,结合注水井和采油井生产数据的动态分析,认识各种地质及生产动态因素对注水效果的影响和控制作用。结果注入水在地质上主要受构造、沉积微相和储层物性3方面控制,工程上主要受注水时机、注水方式和注水强度的影响。结论有益的为开发同类油藏提供了该研究经验和借鉴。     

基于声线跟踪法的稳态声场空间分布计算

使用一种新的声线跟踪模型来预测稳态声场的能量分布,声场空间分布能通过一次仿真就得到预测并成像.接收球在这种方法中没有被使用,因为预测的目标不是一个点而是整个三维空间.首先建立一个三维的能量数组以模拟整个声空间,该数组的行数,列数和层数分别与声空间的宽,长和高成正比.能量数组中的每一个元素被用于记录声空间中某一个小立方体的声强,而该元素在数组中的位置与该立方体在声空间中的位置相同.每根声线的传播路径都被跟踪,其传播路径将被离散化为一系列均匀分布而又密集的节点,每个节点的坐标都被计算出来以找到能量数组中位置相同的元素,该节点的声强将被记录在它所对应的数组元素中.当全部声线都被跟踪完毕时,声强空间分布就已经建立在能量数组中了.某一个平面内或某一条线上的声强级和声压级分布都可以直接根据能量数组中的值计算出来并成像.在进行的实验中对稳态声场的声压级进行测量和预测,发现预测结果与实验结果吻合很好,因此这种新的声线跟踪模型的有效性得到证明.