求解二维扩散方程的加权平均隐式多重网格方法

提出了数值求解二维扩散方程两种精度分别为O(τ^2 h^2)和O(τ^2 h^4)的无条件稳定的加权平均隐格式，并采用多重网格方法进行求解，从而克服了传统迭代法在求解隐格式时收敛速度慢的缺陷，提高了求解效率．数值实验验证了该方法的精确性和可靠性．     

三维水动力学模型高精度差分格式和解法研究

采用高精度差分格式对三维水动力学问题的时均化Navier-Stokes方程进行了数值模拟，进而采用广义共轭剩余法（GCR方法）求解压力泊松方程，并采用显式三级二阶Runge-Kutts格式模拟了时间步进过程。傅立叶分析表明，文中所采用的三阶迎风紧致差分格式具有较高的精度，数值实验进一步验证了上述数值模型的准确性和有效性。     

基于语义网络的方案设计过程表达与推理

从基于机械运动方案设计的表达方法必须能支持概念设计全过程的思想出发，提出计算机辅助概念设计系统必须能够表达设计方案、产生方案、产生多个方案和确定最优方案．根据方案表达方法应具备的基本功能要求，选用语义网络技术表达设计方案过程、工艺动作、机构及其相互间的关系，通过对设计方案中机构时间配合及其影响的表达和调整实现了方案设计运动循环图表达的计算机辅助化．利用基于语义网络表示的不确定性推理技术构造待求问题的语义网络片断，通过已有设计实例与设计要求的属性值与属性值、属性值与属性值域、属性值域与属性值域三者的匹配比较构造贴近度计算公式，并对工业平缝机中的挑线机构进行了机构选型．实例证明了击模型的正确、实用性．     

基于二维提升方案的可逆双正交小波变换在渐进性无损图像压缩中的应用

分析了一维(基于行、列分解和重构)提升方案的特点，从理论上指出了一维提升方案的不足之处，提出了二维(基于子带分解和重构)提升方案，并给出了CDF(1，3)双正交小波二维提升方案的具体形式，改进的提升方案弥补了一维提升方案的不足之处，不需作‘√2’因子和归一化处理，整个小波变换是可逆的、基于整数运算的、能量守恒的，减少了误差传递的机会，用该小波变换实现了快速的、渐进性的直至无损图像压缩。     

百色盆地百49块百岗组三段高分辨率层序地层学分析

以高分辨率层序地层学理论为指导，通过地表露头、岩芯、测井资料的综合研究，并结合地震剖面资料，分析了百色盆地塘寨油田百49块古近系百岗组三段不同级别的层序界面和湖泛面特征及识别标志，划分出1个长期、3个中期、14个短期基准面旋回层序。在此基础上，详细讨论了各级次基准面旋回层序的垂向序列、岩性岩相组合、结构类型及更加样式等特征，并探讨了高分辨率层序地层学的研究成果在区块油气开发工程中的应用前景。     

Inhibitory effect of the adenovirus type 5 E1A protein expressed in the yeast system

The human adenovirus type 5 E1A, a tumor- suppressor gene[1], codes for two major related proteins of 243 amino acids (12S) and 289 amino acids (13S) by al-ternative splicing in two exons[2]. Studies have been shown that E1A can regulate expression of many genes and cell cycle[3]. Both in vitro and in vivo experiments indicated that E1A could induce tumor cells differentia-tion, convert tumor cells into an epithelial phenotype, in-hibit tumor cell growth and metastasis and strongly en-ha…     

Shift visual cryptography scheme of two secret images

A new visual cryptography scheme of two secret images, which is named the shift visual cryptography of two secret images, is given. The compound function family of a general construction model is also introduced. The uniqueness and validity of this model are proved, and the minimum rows and columns for realizing the scheme are obtained. Compared with visual cryptography of one secret image, the shift visual cryptography scheme can share two secret images with the same size of pixels expansion without losing the contrast. It has randomness and various forms, and furthermore, we can also visually recover two secret images even if the two shares are different in form and color.     

A model for assessing effects of climate change on runoff in China

A model is established for assessing the effects of climate change on runoff in China based on the land surface parameterization scheme variable infiltration capacity (VIC). The entire area of China is represented by 2604 cells with a resolution of 60 km×60 km for each cell. Forcing data, soil and vegetation parameters needed by the VIC model for the entire area of China are prepared. Daily forcing data, which are obtained from 740 stations between 1980 and 1990, are interpolated to the 60 km×60 km grid system. The VIC model is run on every grid cell over the whole China, and a routing scheme is run offline with daily input of surface runoff and drainage from the VIC to get hydrograph at basin outlets. The spatial patterns of simulated runoff and mean annual precipitation are consistent very well. The results of monthly streamflow simulations over the Huaihe and Weihe River basins indicate that there is a good agreement between the observed and simulated values, and also initially indicate the rationality and feasibility of the evaluation model.     

Compact difference approximation with consistent boundary condition

For simulating multi-scale complex flow fields it should be noted that all the physical quantities we are interested in must be simulated well. With limitation of the computer resources it is preferred to use high order accurate difference schemes. Because of their high accuracy and small stencil of grid points computational fluid dynamics (CFD) workers pay more attention to compact schemes recently. For simulating the complex flow fields the treatment of boundary conditions at the far field boundary points and near far field boundary points is very important. According to authors' experience and published results some aspects of boundary condition treatment for far field boundary are presented, and the emphasis is on treatment of boundary conditions for the upwind compact schemes. The consistent treatment of boundary conditions at the near boundary points is also discussed. At the end of the paper are given some numerical examples. The computed results with presented method are satisfactory.     

东营凹陷沙三段-沙二下亚段T-R层序特征及成因

将东营凹陷古近系沙三段沙二下亚段划分为 3个三级层序 ,即沙三下层序 (SSⅠ )、沙三中层序 (SSⅡ )和沙三上沙二下层序 (SSⅢ )。SSⅠ和SSⅡ层序由湖进体系域和湖退体系域组成T R旋回 ,其特征是代表层序边界的不整合分布局限 ,湖进体系域厚度小 ,主要为细粒沉积物 ,退积式叠加 ;湖退体系域较厚 ,由进积式叠加的砂岩、砾岩和泥岩组成。T R层序的形成主要是由于层序形成早期的构造沉降和气候起主导作用 ,其基底快速沉降 ,湖水供应充分 ,湖平面快速上升。在层序形成晚期 ,沉积物供给和气候起主导作用 ,沉积物供给多 ,快速向前推进 ,湖平面下降。构造沉降和沉积物供给因素对层序控制作用的转换促使其形成层序和体系域的边界。T R层序与三分层序之间的转换是由于层序形成的不同阶段的主控因素不同而引起的