全光纤安防系统模式识别混合编程的实现

介绍了宽域全光纤监控预警系统及光纤扰动信号模式识别算法.利用小波包分解对信号进行分解与重构,并提取各频段内信号分量能量谱作为特征向量;应用综合考虑观测数据和确定性先验知识的BVC-RBF神经网络实现信号分类,提高了网络的泛化能力.利用Matlab引擎、动态链接库(DLL)、组件对象模型(COM)3种混合编程方法将Mat...     

不连续问题的无网格分域算法

提出一种无网格方法中采用分域的思想处理材料和位移不连续问题的方法。该方法将求解域沿不连续面进行分域,通过使用两种转换矩阵使子域交界面上的位移连续性得到满足;采用分块矩阵法计算转换后的刚度矩阵,所得刚度矩阵仍具有稀疏、带状性。可采用与有限元耦合的方式施加本质边界条件。编制了该算法的计算程序,通过对材料不连续悬臂梁弯曲问题的分析和单边裂纹板裂纹张开位移的计算,验证了该算法的正确性和有效性。     

基于DTD元素树的XML与RDB的双向映射算法研究

分析了XML文档到关系数据库的映射方法,并提出了元素树和元素树节点与其他类型数据之间的映射算法.在此基础上建立了XML模式和关系模式之间的双向映射模型,并给出了双向映射模型算法,从而完成了XML与RDB数据转换.     

弦方程密度函数的确定性

利用Liouville变换,得到弦方程密度函数的1/4次幂的朗斯基行列式与弦方程特征函数之间的关系,从而确定了弦方程的密度函数.     

区间删失数据函数的均值估计

运用无偏转换思想构造了区间删失数据函数的均值估计,并在此基础上对所构造的估计量方差进行了研究.针对Ⅰ型区间删失情况和Ⅱ型区间删失情况,找到了估计量方差有限的条件.     

分形数集自相似新异类型

按照集合特征把分形自相似划分为4类,以前分形数集中出现的自相似可归为第Ⅰ、Ⅱ、Ⅲ类,未见第Ⅳ类.发现一种新的三元数集,具有Ⅳ类自相似性.数集整体外观像3叶片叶轮,叶边有序排列着无数芽枝.芽枝上结有两种不同形状的自相似子集,结在枝梢段的子集具有全集形,结在枝干段的子集具有Mandelbrot集形,呈现一棵树结两种果的现象.两种子集各带有自己的自相似后代,自相似传递方式迥异.Mandelbrot集形子集的后代都是Mandelbrot集形:全集形子集的后代也分两种形,像全集那样遵循枝干段与枝梢段不同的规则.芽枝干梢两段有可辨的交接处,却是无穷精致的极限点.比较多种分形数集的运算规则和形象,得出数算规则小差别可以导致数集形态和自相似特性大差别的结论,也推测分形数集或有自相似的趋向性.文中给出了该三元数集的定义、样集参数和空间位置,附图21幅展示了整体三维形象、两种子集的剖面形态以及局部复杂的自相似结构.     

基于真彩切片的MRI图片颜色迁移及三维重构分析

借助于可视人工程的真彩图片作为常用MRI、CT等灰度图片彩色化的颜色迁移的彩色特性源本,以MRI切片和真彩图片的亮度、纹理和几何作为映射间的配准参数而进行合理的颜色转换,以弥补医学灰度图片伪彩色方案中各组织非对应的彩色映射关系.通过真彩图片与灰色图片的亮度分布曲线的调整和纹理特征关系的调整和配准而到有效和符合真实人体器...     

重组GATA4腺病毒的构建及心肌细胞感染

利用AdEasy腺病毒表达系统构建了GATA4基因过表达腺病毒.编码大鼠GATA4基因的目的片段克隆入pAdTrackcmv质粒,pAdTtrackcmv-GATA4穿梭质粒经PmeⅠ线性化后转入含pAdEasy-1的BJ5183菌进行同源重组.pAdEsay-GATA4重组质粒经卡那霉素抗性筛选及PacⅠ酶切鉴定.pAdEsay-GATA4转入293A细胞进行包装,产生具有感染性的重组病毒.Ad-GATA4重组病毒感染HeLa及乳鼠心肌细胞,通过免疫印迹及实时定量聚合酶链反应(Real-time PCR)检测GATA4表达及促心肌肥大效应.Ad-GATA4重组病毒感染乳鼠心肌细胞后,诱导心肌细胞表面积明显增加,ANF表达明显增强.结果表明,Ad-GATA4腺病毒成功感染心肌细胞并诱导了大鼠心肌肥大表型的出现.     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.