基于集群的影像并行OPTA算法研究

并行计算是提高海量遥感影像细化处理速度的有效途径.基于对OPTA细化算法的分析,深入研究OPTA细化并行算法中数据划分和数据通信优化等关键问题,提出一种适合集群并行处理的通信优化并行算法,实验证明该算法具有良好的加速比,适合集群计算环境下海量遥感影像的细化处理.     

GPS软件接收机精确载波频率捕获算法分析与实现

采用基于快速傅里叶变换（FFT）的并行码相位搜索捕获算法实现GPS信号的捕获,根据相位关系对载波频率进行精化,使其满足跟踪模块的需求。在分析算法的基础上,通过对模拟信号和实测数据进行捕获实验,实现了对载波频率的精化,获得精确频率可直接用于后续跟踪环路。     

利用流水线技术的遥感影像并行处理

针对现有的OpenMP和直接的线程并行法难以对遥感影像处理链进行加速的问题,引入流水线概念对复杂的功能链进行并行加速,提出了基于流水线技术的遥感影像并行处理方法。影像处理实验验证了流水线在遥感影像多级连续处理方面的优势。     

地震前兆数据多线程采集与多目标入库应用研究

利用可实例化的智能线程池技术,通过两个线程池分别实现了前兆数据的并行数据采集与数据的多目标入库,可自动实现对最近巧天内的数据进行检测与采集,采集仪器的数量由原来的几台、十几台提高到上千台,大大提高了地震前兆数据的采集效率;通过数据的多目标入库,数据由台站到区域中心以及国家台网中心的同步速度也得到很大提高.     

可调节经线收敛度和经纬线间隔的伪圆柱投影

令纬度ψ<,j>转换为ψ<,j>后,中央经线方程用一个ψ<,j>的7次幂方程表示,中央经线方程的系数关联着纬线间隔.令经度λ<,i>转换为ξ<,i>后,赤道方程用一个ξ<,i>的7次幂方程表示,赤道方程的系数关联着经线间隔.经线的收敛度由经线方程的收敛系数调节.由此构建可调节经线收敛度和经纬线间隔的伪圆柱投影.用一实例...     

Comparison of the Ordovician-Carboniferous Boundary Between Korea and NE China: Implications for Correlation and Tectonic Evolution

There is a great hiatus between Ordovician and Carboniferous strata in the Northeast China and Korean Peninsula. In order to understand geology and tectonic evolution, and to find out the similarities and differences in both regions, two sections in the Western Hill near Beijing in NE China and several sections in the Korean Peninsula were selected to examine their geologic boundaries between Lower and Upper Paleozoic strata to compare their characteristic features. At four sites in the two sections in the Western Hill near Beijing were examined their contact relations. The Hui Yu section is the same horizon where one site is top of a quarry hill and the other of down hill. Mid-Carboniferous Qingshuijian Formation rests on the Ordovician Majiagou Formation. Limestone beds are more commonly intercalated with shale and sandstone at site 2 of the Hui Yu section, while at site 1, conglomerate beds are dominant. Site 1 of the Se Shu Fen section shows eroded and concealed karst topography and conglomerate beds are intercalated within shale beds. Silurian and Devonian strata are absent in these areas. In the Korean Peninsula, most O-C contacts occur between Ordovician limestone formation and Carboniferous strata, although Silurian strata occur beneath the Carboniferous strata in the Jeongseon area and Pyeongnam Basin. Most contact relations are parallel unconformity and angular unconformity is rarely seen. The O-C relations in both regions are similar to each other, and these indicate that the Korean Peninsula was located near or belonged to the Sino-Korean paraplatform during Paleozoic time.     

并行网络电法在煤层覆岩破坏监测中的应用

并行网络电法勘探现场观测数据表明,随着开采煤层上覆岩体破坏程度的加剧,其电阻率值呈上升趋势:当煤层上覆岩层视电阻率值相对于背景电阻率值增大1~2倍时为裂隙发育带;当增大3倍以上时为离层冒落带。对于全空间电阻率观测,其视电阻率值的变化主要是以突出异常为主。应用结果表明,利用并行网络电法进行煤层顶板视电阻率动态监测,可以直观反映“三带”的发育形态以及开采产生矿山压力的显现规律,为矿井安全提供有效的探测手段。      

Spectral element analysis on the characteristics of seismic wave propagation triggered by Wenchuan <Emphasis Type="Italic">M</Emphasis><Subscript>s</Subscript>8.0 earthquake

The 2008 Wenchuan earthquake occurred in an active earthquake zone, i.e., Longmenshan tectonic zone. Seismic waves triggered by this earthquake can be used to explore the characteristics of the fault rupture process and the hierarchical structure of the Earth’s interior. We employ spectral element method incorporated with large-scale parallel computing technology, to investigate the characteristics of seismic wave propagation excited by Wenchuan earthquake. We calculate synthetic seismograms with one-point source model and three-point source model respectively. The AK135 model is employed as a prototype of our numerical global Earth model. The Earth’s ellipticity, Earth’s medium attenuation, and topography data are taken into consideration. These wave propagation processes are simulated by solving three-dimensional elastic wave governing equations. Three-dimensional visualization of our numerical results displays the profile of the seismic wave propagation. The three-point source, which is proposed from the latest investigations through field observation and reverse estimation, can better demonstrate the spatial and temporal characteristics of the source rupture process than the one-point source. We take comparison of synthetic seismograms with observational data recorded at 16 observatory stations. Primary results show that the synthetic seismograms calculated from three-point source agree well with the observations. This can further reveal that the source rupture process of Wenchuan earthquake is a multi-rupture process, which is composed by at least three or more stages of rupture processes. Supported by National Basic Research Program of China (Grant No. 2004CB418406), National Natural Science Foundation of China (Grant Nos. 40774049 and 40474038), and Computer Network Information Center, Chinese Academy of Sciences (Grant No. INF105-SCE-02-12)     

空孔直眼掏槽成腔模型理论与实践分析

空孔直眼掏槽是隧道或井巷掘进的主要方法之一。基于典型空孔掏槽炮眼布置,分析了掏槽眼爆破形成空腔的物理力学过程;建立了空腔形成的物理和力学模型;研究了腔内碎石在高压爆生气体作用下的抛射过程;得出了空腔尺寸的理论计算方法。槽腔岩石介质破碎和外端部漏斗形成取决于掏槽眼装药爆炸动作用;碎石的抛出率与炸药性质、岩石性质和爆破参数有关。理论分析与在某矿进行的48次试验结果有较好的吻合性。     

基于三维非线性有限元的边坡稳定分析方法

刚体极限平衡法不能反映岩体中实际的应力分布,而基于有限元的强度折减系数法在判断收敛性方面存在一些问题。为了解决这些问题,采用多重网格法,分别建立用于有限元计算的结构网格和用于计算滑面稳定安全系数的滑面网格,可以方便地获得任意滑面或滑块的稳定安全系数,从而将非线性有限元和极限平衡分析结合起来。为了提高计算规模和计算精度,采用有限元并行计算程序TFINE.Pfem进行计算,分析了网格密度对计算结果精度的影响,并应用于锦屏高边坡的稳定分析中。与刚体极限平衡法结果的对比分析表明,由于考虑了计算过程中的非线性应力调整,该方法的计算结果比刚体极限平衡法偏大,而且更符合实际情况。