Construction of Realistic Scene in Virtual Turning Based on Global Illumination Model and Chip Simulation

With the rapid development of manufacturing technology, the traditional simulation of machining can not meet the people‘s need. Research on virtual machining environment is one of the key parts of virtual manufacturing technology. According to the features of virtual turning, this paper proposes a simplified Whitted lighting model based on analysis of Phong and other local illumination model. This model takes the material and roughness of workpiece into account to calculate the roughness coefficient D, geom...     

采用触发测头进行曲面自动跟踪测量

介绍触发测头的工作特点,并提出一种新的采用触发测头进行曲面自动跟踪测量的方法,该方法采集速度快,精度高,可以应用在数控机床上实现工件的数字化采集,尤其适用于薄壁受易变形工件的数据采集。     

曝气处理甲苯的传质机理

曝气技术(AS)是处理地下水中石油污染的修复技术，具有低成本、高效率和原位操作等显著优势．通过自行设计安装的二维砂箱，结合AS的流型，对其进行了去除甲苯的传质研究．采用乙炔示踪法对AS的流型研究表明，在0．15m^3／h的乙炔曝气流量下，气体在地下水区域中分布非常均匀，形状近似为对称U字形．AS甲苯传质研究表明，在曝气过程中，空气可达到的区域是AS修复的主要区域，且甲苯的去除时间受空气含量的影响极大．曝气源附近的区域．其去除效率很高。经400min曝气后，甲苯去除效率达80％．     

关于f×f与f的动力性质间关系的研究

利用伪轨跟踪性质和一些其他方法,研究了紧系统(X×X,f×f)和(X,f)的动力性质间的关系,有些结果推广了文献[1～5]、[7～9]中的相应结果.     

一种新的矩形网格生成等值线算法

提出了一种利用数据关联表生成矩形网格等值线的算法。该算法的优点是计算效率高，避免了以往等值线追踪算法起始点选取困难、网格出口边判断复杂的问题。算法的追踪结果精度取决于等值点的计算方法，其精度是可控的。这种算法原理可以扩展应用到三角网格的等值线方法中。     

数字图像处理在测井曲线矢量化中的应用

针对测井曲线的矢量化问题，在讨论频域和空域的测井曲线图像预处理优缺点的基础上，采用了矢量跟踪的方法来处理测井曲线、对不同油田的20多种测井图纸样本进行了测试，实验表明矢量化的精度可达98％。     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6～1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.     

自动绘制沉积微相图算法设计

成功地给出了沉积微相边缘追踪算法和边缘线生成算法。根据相带连通边界井之间的位置关系 ,将每一口边界井的周围生成的一系列单元控制线连接起来就可以画出沉积边缘线 (相带线 )。单元相带线的形状是由 3个控制点的位置决定的。针对沉积微相图上各种错综复杂的微相叠合及接触关系 ,系统地归纳和设计了 2 0 0多条规则。应用这些规则和算法 ,可以准确地求出相带线的位置。特别是运用控制线单元的生成技术 ,用户通过鼠标在屏幕上拾取控制线单元的控制点就可以实现人机交互功能。同时 ,向量成图技术使得成果图件的复用、修改和再生成为可能。实际应用结果表明 ,计算机自动绘制沉积微相图软件的绘图效果能够满足地质工作的需求。