橡胶基复合靶抗贯穿特性的近似分析方法

采用体积含量加权的方法确定了复合靶等效状态方程参数,采用纤维含量平方外推的方法确定了复合靶的等效强度。然后利用球腔膨胀和柱腔贯穿相结合的方法提出了一种分析计算钢球贯穿橡胶基复合靶的近似分析模型。计算方法简明、高效,而且对剩余速度和临界穿透速度等的计算结果与已有实验有良好的符合。     

Dewar瓶内液体晃动的近似计算方法

本文研究Dewar瓶内液体的晃动特征问题，将液体晃动的微分方程边值问题转换为具有积分形式的泛函极值问题，在此基础上建立了旋转对称容器液体晃动特征问题的有限元数值计算方法和通用程序，并计算了Dewar球，球腔，圆柱腔液体的晃动固有频率，结果显示了Dewar瓶综合了球腔和圆柱腔液体晃动的特征，它将液体晃动频率控制在一窄带范围之内。利用该程序，本文又计算了Dewar瓶液体晃动的单摆模型，为了便于工程应用，本文提出了一种对Dewar瓶建立等效圆柱容器液体晃动模型的方法，给出了模型的参数变换公式，从而可以通过对圆柱窝器液体晃动的解析计算得到Dewar瓶的液体晃动结果。利用数值计算结果，本文验算了近似计算方法的有效性和近似程序。     

Heat conduction in a rock mass with an annular hot water store

Vast subterranean caverns may be used for hot water storage in distinct heating schemes; such caverns can be annular, with a central pillar. This paper considers the quasi-steady solution of the heat conduction equation for this geometry with periodic temperature variations     

海域水流及水质之综合智慧型系统

本文研究之目的为将近年来先进的人工智能技术与现有的数学模型互相结合，开发一套有关海域水流及水质之综合智能型系统。其应用之技术包括智能型系统、人工神经网络及模糊推理系统。此系统可作辅助设计或训练之工具，能帮助水力及环境工程师熟习最先进的海域水流及水质模型，以期使科研与实际执行者之间的距离缩小。其结果可导致对各种不同方式数学模型之好处、应用或限制，有更透彻的了解，甚至从而达成突破及贡献。随着环境可持续性愈来愈被重视，对开发此类综合系统之需求亦逐渐增加，正好可辅助决策者迅速地达成决定，并同时可向公众提供方便及公开的水质信息。     

SiC粒子非均布引起铝基复合材料的损伤分析

 根据电镜断面考察结果，以Gurson模型为本构方程的有限单元 法对包体模型及三维非均匀模型进行了详细分析. 为了评价应力-应变 关系及损伤的主要因素，考虑了基体中SiC粒子的体积率和径比的非均 匀分布. 其结果表明，用这种非均匀模型能很好地仿真铝基体在大量塑 性变形之后所发生的韧窝破坏过程. SiC粒子体积率、径比及其位置的 非均匀性，对局部和整体损伤过程与应力-应变关系的影响相当大. 当 Sic粒子径比为1.0，并在基体中均匀分布时，断裂应变会大幅度增大.     

Boussinesq方程的发展形式与Airy波理论差异性研究

应用势流理论，采用递推函数方法推导出一个新形式的Ｂｏｕｓｉｎｅｓｑ方程。通过对新方程的参数设置，可以讨论出Ｂｏｕｓｓｉｎｅｓｑ方程发展趋势和不同的发展形式。对浅水波动的描述方程，Ｂｏｕｓｓｉｎｅｓｑ方程的发展趋势为适用水深范围的拓展。拓展应用范围的大小则由其方程频散特征向Ａｉｒｙ波频散解逼近程度来决定。而Ｂｏｕｓｉｎｅｑ方程又不同于Ａｉｒｙ波，主要原因是Ｂｏｕｓｓｉｎｅｓｑ方程中含有线性频散项，Ａｉｒｙ波则只是长波首项近似，无线性频散项。其频散特征为精确的线性频散解。对实际水波传播而言，Ａｉｒｙ波理论的局限性是不言而喻的。     

The “decaying springs” model for irreversibility in polymer melts

In this work, entanglements in a polymer melt are modeled as a system of parallel springs which form and decay spontaneously. The springs are assumed to be nonlinear, and a certain fraction of them is torn apart by a certain strain.Based on these assumptions, a model of behavior in simple shear is developed. This model is shown to predict a behavior comprising that of a Wagner fluid, and is generalized to a tensorial model of single integral type. The integrand depends on a product of a material function, modeling reversible behavior, and a material functional which takes irreversible processes into account.Irreversibility of network disentanglement, which may occur when deformation changes or reverses direction, can be modeled in this way. It is shown that the two well-known Wagner constitutive equations with and without irreversibility assumptions are special cases of the model developed. In case of a deformation which does not change directions, the new material function and the material functional are multiplied to yield Wagner's damping function.When the rate of spring formation is a function of temperature, the developed model is shown to predict thermorheologically simple behavior. A constitutive equation for non-isothermal flow of polymers is developed with this assumption.     

Pore-scale network model for drainage-dominated three-phase flow in porous media

Drainage displacements in three-phase flow under strongly wetting conditions are completely described by a simple generalisation of well understood two-phase drainage mechanisms. As in two-phase flow, the sequence of throat invasions in three-phase flow is determined by fluid connectivity and threshold capillary pressure for the invading interface. Flow through wetting and intermediate spreading films is important in determining fluid recoveries and the progress of the displacement in three-phase flow. Viscous pressure drops associated with flow through films give rise to multiple filling and emptying of pores. A three-phase, two-dimensional network model based on the pore-scale fluid distributions and displacement mechanisms reported by Øren et al. and which accounts for flow through both wetting and intermediate fluid films is shown to correctly predict all the important characteristics of three-phase flow observed in glass micromodel experiments.