基于ArcGIS的三维闪电数据图形显示系统

针对三维闪电探测仪大规模组网后,接收和解算的定位数据大幅增加,国内缺少专用于三维闪电数据监测显示与处理制作方面的软件,使用B/S(Browser/Server)架构结合ArcGIS地理信息平台,Oracle、 SQLite数据库等技术方法,开发了三维闪电数据图形显示系统。利用状态数据接收与解析入库、探测仪实时状态统计等功能模块设计出状态监控子系统;利用定位数据实时统计、历史查询、三维显示等功能模块设计出实时显示子系统,联合具有数据服务产品生成功能的产品制作子系统组成图形显示系统,以国家三维闪电探测网为实际应用背景验证系统功能和运行状况。结果表明,三维闪电数据图形显示系统直观友好、监控及时、功能齐备、产品丰富,是雷电科研领域的有益工具。     

基于GIS的配网抢修指挥业务关键技术研究

配网故障抢修作为配电生产常规性重要工作，具有全天候故障响应、直接面对用户、故障情况多样、作业环境复杂等特点，如何快速地安排检修，使停电损失降到最小，有力地保证用电安全和供电可靠性，这是供电企业的重要工作。该文研究基于GIS的配网抢修指挥业务关键技术，从企业的实际应用出发，利用GIS的拓扑信息以及相关业务系统实时数据信息分析客户报修内容，定位故障点，并利用地理图形调度抢修资源，安排最快的抢修驻点的抢修队伍去进行故障抢修，并利用GPS定位在GIS图形上实时跟踪抢修车辆的出发、到达现场的现场抢修进程，达到快速、准确地进行故障抢修处理，提高企业的供电服务水平。     

水泥机械立窑温度图形监测系统研制

水泥机械立窑温度图形监测系统是将微机实时监测窑内温度引进水泥机械立窑,用检测到的窑壁有限点温度值,结合窑内的传热数学模型在ＣＲＴ上显示出窑内工况,使操作人员可在控制室内监测窑运行,实现闭门烧窑,既保证煅烧质量又可改善劳动强度和生产环境,实现文明生产,提高劳动效率。     

CAPP系统中输入子系统的图形技术

本文论述了ＣＡＰＰ系统中输入子系统的图形处理技术。系统采用型面要素分解法输入，并对零件图形实时显示，较好地解决了零件信息描述，在图形处理及菜单技术有一定特色，本文还论述了图形实时显示的原理和方法。     

飞机结构静强度试验虚拟显示中的CAE图形可视化关键技术

近年来,虚拟显示作为飞机结构静强度虚拟试验中的重要功能之一,在航空结构试验领域获得了广泛应用,促进了虚实融合试验新模式的发展。系统梳理了当前航空虚拟试验中的关键问题,基于自主CAE图形引擎SABRE.visual,从试验数据实时监控处理、三维云图快速绘制、试验应变片快速定位及关联显示及支持多镜头的用户界面设计等4个方面总结了在虚拟显示领域的关键技术探索,形成了一款虚拟显示软件,具备试验应变数据三维云图实时显示和试验应变片快速定位及关联显示功能,并在航空型号试验现场进行了应用,结果表明效果显著。     

快速Phong明暗处理算法的研究

研究了Ｐｈｏｎｇ模型的快速明暗处理问题，并在前人研究的基础上提出一种近似最佳一致逼近的明暗处理算法。与已有的各种算法相比，该算法具有在不影响图形显示速度的前提下，既能提高又能控制图形显示精度的优点。     

实时监控图形生成系统

图形生成系统是实时监控系统的重要组成部分．运用图形生成系统来生成在线显示画面,可以有效地提高监控系统开发效率和系统的通用性．本文介绍了一种利用面向对象技术和可视化技术研制开发的实时监控图形生成系统,该系统具有友好的用户界面、强大的图元类库支持、两级系统扩充接口及动态连接等功能．     

煤矿井下WiFi人员定位GIS系统设计与实现

按GIS软件工程的思想和UML统一建模语言对煤矿井下人员定位与考勤系统进行需求分析、用例分析、领域建模和动态建模。利用空间数据库分类描述井下巷道的图形和属性信息,借助WiFi无线定位,实时确定井下各类人员的空间位置、分布和动态变化,并显示在电子地图上。研发成果对煤矿安全生产具有指导意义。     

快速Phong明暗处理算法的研究

研究了Ｐｈｏｎｇ模型的快速明暗处理问题，并在前人研究的基础上提出一种近似最佳一致逼近的明暗处理法。与已有的各种算法相比，该算法具有在不影响图形显示速度的前提下，既能提高又能控制图形显示精度的优点。     

基于GPS和GPRS的高速公路车速实时检测系统设计

本课题采用了GPS卫星定位和GPRS通用无线分组业务相结合的技术思路,很好的发挥了两者的长处：定位及时准确、大量的数据传输高效快速、硬件电路设计简单、串口手法控制合理化。采用ATMEGA128单片机作为系统的处理中心,其速度快,接口多,功耗小。主要的信息处理显示部分由LabVIEW应用图形编程系统来完成。基于以上三点来完成对高速公路车速实时检测。     

Near-field postseismic deformation along the rupture of 2008 Wenchuan earthquake and its implications

At first time, we observed the postseismic deformation, which actually is a kind of creep after slip, along the intra-plate active fault associated with the Wenchuan earthquake. To understand the near-field postseismic deformation following 2008 Wenchuan earthquake in Sichuan Province of China, we compared the fault scarp or flexure scarp profiles measured in different campaigns. Our result shows that among total 19 observation sites, on 13 sites (68% of 19) fault scarps fall back with an average about 9.7% decrease; on 5 sites (26% of 19) fault scarps present no change; and on one site (6% of 19) fault scarp continues to uplift with 12.8% increase. The variety of fault scarp we observed results mainly from near-field postseismic deformation, after slip occurred in shallow. Based on our observations, the following are demonstrated: except for the southwestern end near Yingxiu Town where coseismic slip deficit and some elastic energy residue exist there, fall back (68%) or non-changing (26%) of fault scarp shows energy balance or energy deficit due to overthrust, implying that the likelihood of occurrence of strong aftershocks of ≥ M7 becomes very small in these energy-released areas. Moreover, we suggest that a minimum of 10% error due to near-field postseismic deformation should be considered when evaluating the magnitude of historic and paleoearthquake or slip rate based on the fault scarp dis-placement, even though the error caused by erosion has been accounted already.     

The M S7.1 Yushu earthquake surface rupture and large historical earthquakes on the Garzê-Yushu Fault

As revealed by field investigations, the co-seismic surface rupture zone of the 2010 M_S7.1 Yushu earthquake, Qinghai is a char-acteristic sinistral strike-slip feature consisting of three distinct sinistral primary ruptures, with an overall strike of 310°–320° and a total length of 31 km. In addition, an approximately 2-km-long en-echelon tensile fissure zone was found east of Longbao Town; if this site is taken as the north end of the rupture zone, then the rupture had a total length of ~51 km. The surface rupture zone is composed of a series of fissures arranged in an en-echelon or alternating relationship between compressive bulges and tensile fissures, with a measured maximum horizontal displacement of 1.8 m. The surface rupture zone extends along the mapped Garzê-Yushu Fault, which implicates it as the seismogenic fault for this earthquake. Historically, a few earthquakes with a magnitude of about 7 have occurred along the fault, and additionally traces of paleoearthquakes are evident that characterize the short-period recurrence interval of large earthquakes here. Similar to the seismogenic process of the 2008 Wenchuan earthquake, the Yushu earthquake is also due to the stress accumulation and release on the block boundaries resulting from the eastward expansion of Qinghai-Tibet Plateau. However, in contrast with the Wenchuan earthquake, the Yushu earthquake had a sinistral strike-slip mechanism resulting from the uneven eastward extrusion of the Baryan Har and Sichuan-Yunnan fault blocks.     

GPS monitoring of the crustal motion in southwestern China

Through GPS carrier phases observation in southwestern China during 1991–1997, the velocity field within eastern Qinghai-Xizang (Tibet) and its neighbour regions has been established. The velocity of those sites in and west of Chuan-Dian block is mostly 5–10 mm · a^™1 relative to the fiduciary station CHDU (Chengdu), and the motion in Chuan-Qing and Yangtze blocks east of the Xianshuihe-Xiaojiang fault is weak with a velocity of about 0–7 mm · a⁻¹. The velocity vector in these areas indicates a clockwise rotation vortex rather than the so-called intensive eastward pushing or eastward escape. The main pattern of the crustal deformation is a clockwise rotation vortex structure and a differential slip along the boundary fault between different blocks.     

Soft Fault Diagnosis for Analog Circuits Based on Slope Fault Feature and BP Neural Networks

Fault diagnosis is very important for development and maintenance of safe and reliable electronic circuits and systems. This paper describes an approach of soft fault diagnosis for analog circuits based on slope fault feature and back propagation neural networks (BPNN). The reported approach uses the voltage relation function between two nodes as fault features; and for linear analog circuits, the voltage relation function is a linear function, thus the slope is invariant as fault feature. Therefore, a unified fault feature for both hard fault (open or short fault) and soft fault (parametric fault) is extracted. Unlike other NN-based diagnosis methods which utilize node voltages or frequency response as fault features, the reported BPNN is trained by the extracted feature vectors, the slope features are calculated by just simulating once for each component, and the trained BPNN can achieve all the soft faults diagnosis of the component. Experiments show that our approach is promising.     

Crustal P-wave velocity structure in Lower Yangtze region： Reinterpretation of Fuliji-Fengxian deep seismic sounding profile

A deep seismic sounding profile in this paper, from Fuliji in Anhui Province to Fengxian of Shanghai City, is located at eastern China (Fig. 1). The field work was jointly accomplished by the Chinese Geological and Mineral Bureau, the China Seismological …     

Chwa & Hakimi故障模型的方程诊断算法

对于一般情形下的Chwa ＆ Hakimi模型,在不以“t-可诊断性”和“相信大多数”作前提假设的情况下,找到了求全体相容故障模式的具体方法——方程诊断算法,实践证明,诊断效果理想。     

The 3-D structure of shear wave in South China and the southward extension of Tanlu fault

By processing the CSND Rayleigh wave data with the matched filter FTAN technique, Rayleigh wave disper- sion for southeast China is obtained. The 4°×4°S wave dispersion of the pure path is calculated using random inversion scheme, and 3-D S wave velocity structure is set up. Incorporating the above-mentioned results with wide angle seismic sounding data, we studied structure framework and the extending of faults in this area, which demonstrates that the depth of Moho in South China varies from 30 to 40 km, shallower from west to east. The depth of Moho varies from 25 to 28 km for the offshore. The depth of the asthenosphere in upper mantle varies from 60 to 100 km. The depth difference of layers at the two sides of Tanlu fault is more than 10 km at the south part of the Yangtze River, and the fault extends downward more than 170 km. The fault exceeds the main land at Hainan Island and slips into the southern China Sea. Both Tanlu fault and the huge bend of gravity gradient anomaly are influenced by deep latent tectonics.     

基于EMD关联维的齿轮箱齿轮状态振动辨识

论述了经验模式分解(EMD)的理论和特性,以及关联维数及其特性,并根据实际齿轮箱振动信号的非平稳特征和简单监测征兆的需要,引入分别适于非线性非平稳信号分析和表征系统观测序列非线性、不规则程度的经验模式分解和关联维数,提出用EMD关联维来辨识齿轮箱振动信号,结果表明：当齿轮处于不同状态时,与齿轮故障密切相关的内在模式函数的关联维数明显不同,EMD关联维方法可以作为齿轮故障的特征提取工具。     

楼宇自动控制专用开关电源的BIT设计

针对消防自动报警控制系统对电源的基本要求,设计一种单端反激式的开关电源,分析提出实现国家标准所规定的电源各种故障机内检测(BIT)方法,它只需要占用一个单片机口线实现对电源各种故障信号的机内检测,特别是直流故障的检测方法,其不仅能完成相应的检测功能,对保护和延长蓄电池的寿命有十分重要的意义。     

复式半背斜及其形成的动力学初探

作者于1980年提出了《复式半背斜》术语。根据近年来研究,可以断定,它是一个广泛存在的构造型。它具有一系列特征,如:1.连续发育的褶皱呈束状,褶皱束的中部略向前突出呈一弧形;2.物质水平运动具有明显定向性;3.复式半背斜为一巨型断裂限制,在此断裂的一侧离开限制性断裂的距离越大,复式半背斜所暴露的地层带的年龄就越年轻,在另一侧不存在与复式半背斜相应的地质构造,而出现花岗岩带、地槽褶皱带或古老的基岩,等等。笔者划分出复式半背斜的五种动力学类型:1.重力滑动型;2.深断裂挤压型;3.重力滑动与深断裂挤压复合型;4.早期重力滑动与晚期断裂深部挤压复合型;5.深断裂挤压与重力扩张复合型。