椭圆型缓坡方程的一个有效的有限元解

将海绵层消波的方法用于有限元方法中,提出了缓坡方程的一种有效的有限元求解方法.在应用有限元法求解椭圆型缓坡方程时,通过在方程中加摩阻项,并在入射边界(波浪由此边界进入计算域)处使用不连续单元,将绕射势从总势中分离出来,在边界上利用海绵层进行消波处理,有效地消除了由于引用放射边界条件引起的误差和数值反射现象.     

雨生红球藻(Haematococcus pluvialis)基因工程选择试剂的筛选

采用细胞计数法，研究了重要经济微藻——雨生红球藻对10种基因工程常用选择试剂的敏感性。结果表明，雨生红球藻对除草剂草丁膦和抗生素Zeocin比较敏感，50μg／ml的草丁膦和25μg／ml的Zeocin可明显地抑制雨生红球藻生长，尤其是50μg／ml的草丁膦能导致细胞两周内全部死亡；高浓度的卡那霉素和硫酸链霉素也可抑制雨生红球藻的生长；雨生红球藻对包括氯霉素和G418在内的其他6种试剂不敏感，即使处理浓度高达1000μg／ml。本文结果提示草丁膦可能是雨生红球藻基因工程适宜的选择试剂，其相应的抗性基因bar可能成为雨生红球藻遗传转化的选择标记基因。     

基于网络GIS的海洋功能区划管理信息系统

在分析海洋功能区划信息特征的基础上,结合网络GIS集成技术,提出了海洋功能区划管理信息系统的三层结构框架和系统研制的关键性技术,并应用实例详细说明了系统的实用功能。     

Improvements on Mean Free Wave Surface Modeling

Some new results of the modeling of mean free surface of waves or wave set-up are presented. The stream funetion wave theory is applied to incident short waves. The limiting wave steepness is adopted as the wave breaker indcx in the calculation of wave breaking dissipation. The model is based on Roelvink (1993), but the numerical techniques used in the solution are based on the Weighted-Average Flux (WAF) method (Watson et al. , 1992), with Time-Operator-Split-ting (TOS) used for the treatment of the source terms. This method allows a small number of eomputational points to be used, and is particularly efficient in modeling wave set-up. The short wave (or incident primary wave) energy equation is solved by use of a traditional Lax-Wendroff technique. The present model is found to be satisfactory compared with the measurements conducted by Stive (1983).     

开孔沉箱在斜向入射波作用下受力研究

应用透空壁内流体速度与壁两侧的压力差成正比的线性模型,研究了斜向波与无限多个开孔沉箱的相互作用.依照结构物的几何形状,把整个流域分成无限多个子域,在每个子域内应用特征函数展开法对速度势进行展开.对于沉箱内的波浪运动,引入相位差概念;在构造反射波模型时,考虑了结构物的几何形状影响.列举出物理模型实验结果与数值实验结果的比较,可以看出两者吻合较好.进一步的数值计算验证表明,当孔隙系数无限大时,开孔墙前后的速度非常接近.在低频入射波作用下,垂直于沉箱的水平力随角度的变大而减小,平行于沉箱排列方向的力则变大.     

利用有限元方法求解双曲型缓坡方程

本文提出了一种双曲型缓坡方程的有限元计算方法 ,在建立有限元积分方程时通过在造波线处加入脉动源项来实现内部造波 ,并在开边界处利用阻尼层吸波 ,减少了在边界处由于数值处理引起的误差。数值计算结果与实测值吻合良好。本方法可用于大区域波浪场的计算中     

Application of A Fast Multipole BIEM for Flow Diffraction from A 3D Body

A Fast Multipole Method (FMM) is developed as a numerical approach to the reduction of the computational cost and requirement memory capacity for a large in solving large-scale problems. In this paper it is applied to the boundary integral equation method (BIEM) for current diffraction from arbitrary 3D bodies. The boundary integral equation is discretized by higher order elements, the FMM is applied to avoid the matrix/vector product, and the resulting algebraic equation is solved by the Generalized Conjugate Residual method (GCR). Numerical examination shows that the FMM is more efficient than the direct evaluation method in computational cost and storage of computers.     

Reflection of Oblique Incident Waves by Breakwaters with Partially-Perforated Wall

The reflection of oblique incident waves from breakwaters with a partially-perforated front wall is investigated. The fluid domain is divided into two sub-domains and the eigenfunction expansion method is applied to expand velocity poten-tials in each domain. In the eigen-expansion of the velocity potential, evanescent waves are included. Numerical results of the present model are compared with experimental data. The effect of porosity, the relative chamber width, the relative water depth in the wave absorbing chamber and the water depth in front of the structure are discussed.     

基于格子Boltzmann方法的饱和冻土孔隙成冰介观尺度模拟

路基冻胀问题严重影响寒区高速铁路的安全服役,而成冰相变过程是解释冻胀机制的关键。基于介观尺度的格子Boltzmann方法,将修正的孔隙水冻结温度算法与焓法固液相变格子Boltzmann模型相结合,模拟了悬浮液滴冻结和冻土孔隙水成冰两个过程,分别揭示了液态水在自由状态和孔隙束缚状态下冰水相变的细观机制。计算结果表明：土体孔隙中冰晶由中心向外生长的过程与悬浮在空气中的液滴冻结过程截然不同,并且孔隙水越接近颗粒表面,其冻结温度越低。相同粒径颗粒按照不同排列方式得到的冻结特征曲线（soil freezing characteristic curves,简称SFCC）具有明显差异;不同粒径的SFCC随着颗粒增大残余水含量逐渐变少,形态更加陡峭。通过与文献试验结果对比,验证了格子Boltzmann方法的有效性,表明该方法能够为研究多孔介质水气迁移与相变过程提供介观尺度的新手段。     

西伯利亚板块东南缘晚古生代伸展体制新证据：东乌旗角闪辉长岩年代学及地球化学研究

为研究西伯利亚板块东南缘晚古生代板内伸展开始时间及地幔属性。基于1∶5万野外宏微观调查,采用LA-MC-ICP-MS锆石U-Pb定年法对分布于东乌旗西部的角闪石辉长岩进行了年龄测定和岩石地球化学测试。结果表明:角闪辉长岩主要由斜长石、角闪石和单斜辉石组成,锆石U-Pb年龄为280.8±1.5Ma,属早二叠世。地球化学数据显示:岩石具较高SiO2(48.87%~53.70%)、TiO2(0.73%~2.27%)、Al2O3(15.05%~16.69%)的含量,中等至较高的MgO(4.84%~9.25%)、FeOT(6.91%~10.47%)和较低的CaO(5.80%~7.94%)。富Na2O(2.75%~3.90%),贫K2O(1.01%~1.90%),为铁质—富铁质碱性和拉斑玄武岩系列岩石组合。稀土总量较高(∑REE为97.50×10-6~251.16×10-6),轻重稀土分异程度中等[(La/Yb)N=4.23~7.12],Eu异常不明显(δEu=0.85~0.98)。岩石富集大离子亲石元素(LILE)Ba、Sr、K等,相对亏损高场强元素(HFSE)Nb、Ta、Th等,高的Zr(87×10-6~289×10-6)和Zr/Y(4.03~7.66)比值,与板内幔源岩浆作用的产物一致。综上,我们认为角闪辉长岩为板内伸展构造体制下富集型地幔橄榄岩部分熔融形成的玄武质岩浆岩浆经分离结晶作用后形成的,标志着~280 Ma西伯利亚板块东南缘晚古生代造山过程进入到板内非造山阶段。