一种面向非规则数据的阶段预取策略

传统数据预取技术在处理结构复杂的非规则数据应用程序时,其有效性明显下降.为解决该问题,基于程序运行时的数据访问阶段性特征,提出一种面向非规则数据的阶段预取策略,研究应用程序的访存规律和预取调度机制.该策略通过在线剖析应用程序的访存行为,识别出数据访问性能指标表现稳定的数据访问阶段和具有特定访存行为特征的预取阶段,实现在数据访问阶段内依据预取阶段的访存规律动态调整预取操作.实验结果表明,与传统的基于访存流模型的数据预取技术相比较,阶段预取策略能够减少无用预取,更加有效地改善非规则数据应用程序性能.     

Analysis of the System of Wavy and Ring Deformation in Draping

The paper analyzes the principle of positioning of waves by notching at the bottom of the waves hi garment draping from the dynamic perspective, and search for the best molding effect under 45?to fabric grain as the model baseline. Wavy and ring deformation laws are proved by the sample photographs.     

周期系的非规则性

本文根据一些实验事实和数据,从四个方面阐述了元素周期系的非规则性。     

波动方程基准面法在深层勘探中的可应用性

波动方程基准面技术一直作为解决不规则的地表而受到人们的重视 .波动方程基准面方法也是解决深层勘探问题的一种有效的途径 .通过基准面的下移 ,可以使深部的信号增强 ,变多值走时为单值走时 ,从根本上消除了上覆层速度横向不均匀的影响 .使依赖近双曲线的分频叠加的去噪技术有可能用于深层资料 ,也可以在基准面上做深度偏移 ,既能提高计算效率 ,又能改善深层成像效果 .本文以大庆的“陆相断陷模型”为例 ,利用波动方程基准面有限差分法做的各种实例证明上述论断     

Elastic Wave Propagation Simulation in Heterogeneous Anisotropic Media on Non-uniform Grids

A finite-difference method with spatially non-uniform grids was developed to simulate elastic wave propagation in heterogeneous anisotropic media. The method is very simple and requires less compution time. Complicated geometric structures, such as low-velocity layers, cased boreholes and nonplanar interfaces, are treated with fine non-uniform grids. Unlike the multi-grid scheme, this method does not require interpolation between the fine and coarse grids and all grids are Computed in the same spatial iteration. Planar or nonplanar surfaces including underground lens and cased boreholes are easily treated in a way similar to regular grid points. The Higdon‘s absorbing boundary condition was used to eliminate boundary reflections. Numerical simulations show that the method has satisfactory stability and accuracy. The proposed scheme more efficiently simulates wave propagation in heterogeneous anisotropic media than conventional methods using regular rectangular grids of equal accuracy.     

双层压电板的180°畴中传播的SH型电声表面波研究

本文从一般的压电方程出发,给出了在双层压电板的180°畴中传播的SH型电声表面波波解,着重讨论了两层的厚度相等时的情况,并给出了其色散关系及波场的空间分布.理论分析和实验测试均表明等厚双层压电板与铁电畴层波波导具有相似的传输特性,且更有利于低频信号的传输.     

WIND observations of plasma waves inside the magnetic cloud boundary layers

Based on the WIND observational data for the plasma waves from thermal noise receptor （TNR） working on the frequency 4-256 kHz and the solar wind and the magnetic fields, we analyze the plasma wave activities in the 60 magnetic cloud＇s boundary layers （BLs） and find that there are often various plasma wave activities in the BLs, which are different from those in the adjacent solar wind （SW） and the magnetic clouds （MC）. The basic characteristics are that： （1） the enhancement of the Langmuir wave near the electronic plasma frequency （fpe） is a dominant wave activity, which occupies 75% investigated samples; （2） the events enhanced both in the langmuir and ion acustic （f〈fpe） waves are about 60% of investigated samples; （3） broadband, continuous enhancement events in the plasma wave activities were observed in the whole frequency band of TNR, and about 30% of the 60 samples, however, were not observed in the SW and the MC investigated events; （4） although the ratio of the temperatures between the electon and proton, Te/Tp ≤1, the ion caustic wave enhancement activities are still often observed in the BLs, which makes it difficult to explain them by the traditional plasma theory. New results reported in this paper further show that the magnetic cloud＇s BL is an important dynamic structure, which could provide useful diagnosis for understanding the cloud＇s BL physics and could expand a space developing space plasma wave theory.     

热解产物MgO颗粒形貌对收率的影响

热解工艺制备的MgO颗粒形貌各异,粒径分布不均.传统的数值模拟过程假设产物为同粒径的标准球形颗粒,与实验结果存在一定的误差.因此, 以射流热解制备MgO过程为研究对象,引入伸缩因子等参数,研究了几种特殊的非规则MgO颗粒在射流热解反应器出口的分布,对比标准球形颗粒的分布结果进行讨论.结果表明:收缩因子α、丰满指数k及放缩径比β共同作用影响着MgO的收率.当α=-0.25,k=1,β=1时,MgO的收率较高,为96.88%;当α=0.25,k=2,β=1.5时,MgO的收率较低,为80.39%.     

平流层全球重力波活动的COSMIC观测研究

本文利用从2007年1月到2013年2月的COSMIC（Constellation Observation system for Meteorology,Ionosphere and Climate)温度数据,分析了平流层（20-35 km）的全球重力波活动及其随纬度、高度和季节的变化特征,揭示了平流层不同纬度重力波活动的中期变化规律。以及重力波振荡周期随纬度的变化。赤道地区重力波全年活动很强,且存在明显的准两年振荡(quasi-biennial oscillation,简称QBO)。在 〖20〗^° S-〖20〗^° N 的重力波势能极大值区与强对流区域保持一致。中高纬地区重力波都主要表现为冬季强夏季弱。中纬地区,两个半球冬季陆地上重力波活动强于海洋,且南美洲南部安第斯山每年除夏季外都有较明显的重力波活动。高纬地区,南半球冬季重力波分布保持稳定,而北半球则在某些区域增强,某些区域较弱,这一现象可能是与SSW（Stratospheric Sudden Warming）相关。通过LS谱图分析,我们发现QBO主要出现在平流层低纬地区,AO（annual oscillation,简称AO）和SAO（semiannual oscillation,简称SAO）则主要出现在平流层中高纬地区。     

船舶兴波流场mj求解的边界元计算方法

船舶前进定常兴波对非定常水动力问题的影响，在物面边界条件中通过所谓的mj项体现出来。由于mj项含有定常兴波势的二阶导数，给实际计算带来困难。本文将边界元方法求解叠模流场mj项的技术进一步扩展到定常兴波流场mj项的计算。并以潜体为例给出计算结果。