并列双圆柱涡激振动的经验性模型研究

建立一种新的预报并列双圆柱涡激振动响应的经验性模型,根据特定间距比条件下旋涡脱落频率出现分支的现象,提出以两个具有不同固有频率的尾流振子来共同描述结构的近壁尾涡动力特性,同时两个振子均满足van der Pol方程,进而得到结构振子和流体振子的耦合方程组。使用该模型分别对中高质量比和低质量比的并列圆柱涡激振动问题进行数值计算,结果表明,结构的位移响应和最大振动幅值等变化规律与实验结果趋势一致,数值基本吻合。     

2013年德令哈郊区ML4.5震群特征及发震背景研究

2013年3月底至4月初青海省德令哈郊区连续发生了数次ML4.5左右的地震,市区震感强烈.利用双差定位法对该震群进行重新定位,发现震群空间分布呈近NS向,深度集中于4～10 km的地表浅层,纵向深度剖面呈“斗状”断层特征;利用CAP(Cut and Paste)方法反演了震群中ML≥3.3地震的震源机制解,结果为走滑类型,震群特征与附近的主构造宗务隆山断裂带性质不符.地质勘探发现凹陷或盆地边缘主构造附近通常存在横向伴生断裂,这些断裂规模不大,以走滑性质为主.本次震群位于柴达木盆地北边缘,通过相似构造的对比,认为该区附近同样满足横向断裂存在的条件.由于本次震群各项特征与横向断层的构造理论十分相符,推断出该震群应该是这种微小断裂活动的结果,横向断裂通常规模不大,因此可判断出震群震源区未来发生强震的可能性较小.     

安装粘弹性转角阻尼器的海洋平台—摇摆墙体系抗震性能分析

在海洋平台摇摆墙体系基础上,在摇摆墙底部的铰接点处安装一粘弹性转角阻尼器,进行被动消能结构振动控制,利用ANSYS进行地震荷载作用下的抗震性能验算,并对阻尼器的刚度和阻尼参数进行了分析。结果表明,在摇摆墙底部施加的转角阻尼器能显著降低结构的地震反应。     

近车站地铁运行引起的环境振动的实验与分析

选取上海地铁交通9号线沿线近车站典型区段为对象,以基于LabVIEW2010开发平台的振动测试系统进行数据采集。根据现场实测数据,分析了地铁运行时隧洞中心线对应的地表处3个方向,以及距中心线不同距离地表处垂直地面方向的振动响应实况和振动特性及传播规律。结果表明,地面振动以垂直地表方向振动为主,振动幅值距离隧洞中心线越远越小,在15m左右存在放大区,且放大的敏感频率为15~25Hz。本次实验地点靠近9号线某车站,实验数值具有一定的典型性和特殊性,可为完善该领域的研究提供借鉴和参考。     

基于结构动力特征的小损伤识别方法研究

为了获取基于结构动力特征的小损伤识别方法,组织实施了钢直管、钢壳及5层钢框架结构的损伤识别试验。试验结果表明,以"频率比"作为结构损伤诊断指标对于识别均匀、规整的一维(杆、索)、二维(板、壳)以及三维钢框架结构的损伤十分敏感;该指标对识别钢直管纵向大损伤及3mm横向切口的小损伤;对钢壳径向损伤及环向损伤,对5层钢框架结构的节点螺栓脱落损伤均敏感有效。     

非均质土中桩端扩散虚土桩法的桩基纵向振动研究

根据桩端土应力扩散的规律,建立了桩端扩散虚土桩模型。基于该模型对非均质土中桩-土纵向耦合振动进行研究。利用复刚度传递多圈层平面应变模型,得到桩与虚土桩桩侧土的剪切复刚度。结合边界条件、初始条件和连续条件,对扩散虚土桩和实体桩动力方程从底层往顶层逐层进行求解,得到桩顶动力响应的频域解析解和时域半解析解。通过对桩端扩散虚土桩扩散角、扩散层厚度、桩侧土非均质性和桩长的影响进行计算分析,得到基于扩散虚土桩法桩-土纵向振动响应特性。研究结论可为桩基础动力设计和动态检测提供理论依据。     

考虑累积损伤效应的围岩变形特性研究

隧道爆破开挖诱发的动力扰动作用范围往往远大于其开挖进尺,同一部位围岩受到循环爆破开挖的多次扰动普遍存在累积损伤。对乌东德水电站左岸导流洞爆破开挖过程中的爆破振动和围岩变形监测进行了监测和数值分析,基于累积损伤理论,通过引入损伤判据及损伤变量,考虑计算中产生的不同程度的损伤区域的岩体参数劣化,并将劣化后的参数引入相应损伤单元进行后续开挖爆破数值模拟计算,从而对岩体爆破开挖累积损伤效应进行模拟。通过比较乌东德水电站导流洞的实测数据以及数值模拟计算结果发现,考虑累积损伤的计算结果无论是爆破振动速度还是围岩变形均更接近于实测值。对爆破开挖的分析模拟中应考虑围岩的多次循环爆破累积损伤效应。     

A comparison between magnetic shear and flare shear in a well-observed M-class flare

We give an extensive multi-wavelength analysis of an eruptive M1.0/1N class solar flare, which occurred in the active region NOAA 10044 on 2002 July 26. Our empha-sis is on the relationship between magnetic shear and flare shear. Flare shear is defined as the angle formed between the line connecting the centroids of the two ribbons of the flare and the line perpendicular to the magnetic neutral line. The magnetic shear is computed from vector magnetograms observed at Big Bear Solar Observatory (BBSO), while the flare shear is computed from Transition Region and Coronal Explorer (TRACE) 1700A images. By a detailed comparison, we find that: 1) The magnetic shear and the flare shear of this event are basically consistent, as judged from the directions of the transverse mag-netic field and the line connecting the two ribbons' centroids. 2) During the period of the enhancement of magnetic shear, flare shear had a fast increase followed by a fluctuated decrease. 3) When the magnetic shear stopped its enhancement, the fluctuated decreasing behavior of the flare shear became very smooth. 4) Hard X-ray (HXR) spikes are well correlated with the unshearing peaks on the time profile of the rate of change of the flare shear. We give a discussion of the above phenomena.     

月球引潮力振动与大气潮汐的周期变化

在天气学中,当复杂而开放的气候系统处于远离平衡的临界状态时,任何微小的外力扰动都有可能带来一场雪崩式的"蝴蝶效应";而天气系统的演变尽管错综复杂,其实质却主要是冷暖气团的强弱与进退,再就是月球引潮力的周期变化还能引发周期大气潮。据此推想,在月球的周期运行过程中,是交点月南、升、北、降水平引力拐点所产生的引潮力振动(方向、大小的改变),通过大气内部的动力过程,对不稳定气团可产生激发作用,从而引导冷暖空气南北进退和天气系统演变,便出现了周期大气潮和转折天气周循环。     

Q Vector Analysis of Torrential Rainfall from Meiyu Front Cyclone： A Case Study

Following similar derivation of quasi-geostrophic Q vector （Q^C）, a new Q vector （Q^N） is constructed in this study. Their difference is that the geostrophic wind in quasi-geostrophic Q vector is replaced by the wind in Q^N vector. The diagnostic analysis of Q^N vector is compared with that of Q^G vector in the case study of a typical Meiyu front cyclone （MYFC） occurred over Changjiang-Huaihe regions during 5-6 July 1991. The results show that the Q^N vector has more diagnostic advantages than Q^G vector does. Convergence of Q^N vector at 700 hPa is found to be a good indicator to mimic the horizontal distribution of precipitation. Q^N vector is further partitioned into four components： Q^Nalst （along-stream stretching）,Q^Ncurv （curvature）,Q^Nshdv （shear advection）, and Q^Ncrst （cross-stream stretching） in a natural coordinate system with isohypse （PG partitioning）. The application of Q^N PG partitioning in the MYFC torrential rain indicates that PG partitioning of Q can identify dominant physical processes. The horizontal distribution of 2V·Q^Nalst is similar to that of 2V·Q^N and mainly accounts for 2V·Q^N during the entire period of Meiyu. The effects of Q^Ncurv on rainfall enhancement fade from the mature stage to decay stage. Qshdv enhances precipitation significantly as the MYFC develops, and the effect weakens rapidly when the MYFC decays during its eastward propagation. Q^Ncrst shows little impacts on rainfall during the onset and mature phases whereas it displays significant role during the decay phase.Q^N alst and Q^Nshdv and Q^Ncrst show cancellation only during the decay period.