基于硬件加速的反射和折射场景的辐射度方法

镜面反射、折射场景的辐射度计算是非常耗时的过程。通过引入光学映射虚物体的概念,并且提出了统一创建反射和折射虚物体的方法,在非漫射环境辐射度计算时,采用处理实际物体一样的方法处理虚物体,这样,形状因子和附加形状因子的计算都可以借助图形硬件加速来完成。基于同样的通过引入虚物体而利用图形硬件加速的思想,利用支持OpenGL的图形硬件加速卡,实现了具有镜面反射和折射效果的辐射度场景的实时绘制。结果表明,利用图形硬件是提高真实感图形绘制速度的有效手段。     

三维空间线性规划问题的图解法

本文着重论述怎样利用几何作图,并通过计算,求三维空间线性规划问题的最优解。     

浅析邯郸农行金库盗窃案涉案巨款追缴

倍受关注的河北省邯郸市农业银行支行金库被盗案近期有了一审结果,任晓峰、马向景二人以贪污罪被判处死刑。任、马二人非法获取四千多万元巨款用于购买彩票,案件受害方邯郸农业银行能否向当地体彩中心索回任晓峰等人用于买彩票而支付的巨款?善意取得能否适用于该案?本文通过分析善意取得制度基本理论,结合新出台的物权法规定,指出此案不适用善意取得,巨款应予追缴返还给邯郸农业银行。     

双参数量子代数SUqs（1,1）的表示：正离散序列

本文通过构造双参数量子群ＳＵｑｓ（１，１）生成元的ｑｓ－Ｂｏｓｏｎ实现，给出了ＳＵｑｓ（１，１）的正离散序列表示。     

A model for carbon isotope distribution of methane during diagenesis

The evolution of methane carbon isotope with depth has been discussed based on diagenetic reaction kinetics and isotopic Rayleigh fractionational theory. A mathematical model to describe data of methane carbon isotope for the Liaohe oil field has been established.     

确定隐函数中参数的最小二乘法

将最小二乘法推广到了隐函数情形，简化了一些实际问题的处理。文中给出了插值和非线性回归两种情况下的最小二乘法原理，并讨论了具体的算例。     

ZrO2陶瓷材料在水环境中的疲劳断裂特性

采用断裂力学中的四点弯曲试验法 ,对 Zr O_2 陶瓷材料分别在大气、水环境中的静疲劳和循环疲劳破坏特性进行研究 ,通过扫描电子显微镜 (SEM)对试验片断裂面的微细组织进行观察 ,分析并阐明了造成材料疲劳断裂的机理 .结果表明 ,相同应力条件下 ,材料在水环境中的疲劳寿命比大气环境中低以及循环疲劳对材料的疲劳寿命起到劣化作用 ,该劣化作用可以认为是由于循环应力使得微裂纹增加和扩展造成的 .     

皖西大别山区野生攀援观赏植物资源与应用研究

通过对皖西大别山区野生攀援观赏植物资源的调查研究,本区有野生攀援植物157种具有较高观赏价值。根据其攀援特性分为缠绕类75种、吸附类17种、卷须类27种、蔓生类38种。探讨了其在园林绿化中的应用形式,对本区野生攀援观赏植物进行了总体评价,并对其开发利用提出了建议。     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.