Spatial variability effects of ground motions on cable-stayed bridges   总被引：3，自引：0，他引：3  

K. Soyluk  A. A. Dumanoglu 《Soil Dynamics and Earthquake Engineering》2004,24(3):241-250

In this paper, stochastic analysis of a cable-stayed bridge subjected to spatially varying ground motions is performed. While the ground motion is described by power spectral density (PSD) function, the spatial variability of ground motions is taken into account with the incoherence and the wave-passage effects. The incoherence effect is examined by taking into account two extensively used models. As the effect of the wave-passage effect is investigated by using various wave velocities, the effect of local soil conditions where the bridge supports are constructed is outlined by using homogeneous firm, medium and soft soil conditions. Solutions obtained for the spatially varying ground motions are compared with those of the specialised cases of the ground motion model. Stationary as well as the transient response analyses are performed for the considered bridge model. It is concluded that spatial variability and propagation effects of ground motions have important effects on the dynamic behaviour of the bridge and the variability of the ground motions should be included in the stochastic analysis of cable-stayed bridges.  相似文献   

Non-singular time domain BEM with applications to 3D inertial soil–structure interaction     

Dimitris L. Karabalis   《Soil Dynamics and Earthquake Engineering》2004,24(3):281-293

A direct time domain boundary element method is presented based on the Stokes fundamental solutions, discretized in both time and space, and an efficient time step-by-step solution that minimizes the accumulation of errors. A non-singular numerical integration procedure, in the Cauchy sense, is proposed for the generation of the associated influence matrices. This methodology is shown to be efficient for the solution of a number of computationally intensive problems in the area of soil–structure interaction. In addition, an algorithm for the direct calculation of the response of massive foundations to externally applied forces and/or obliquely incident seismic waves is introduced. The accuracy and computational efficiency of the proposed methodologies is established through a number of comparison studies.  相似文献   

在耀斑-电流片坐标系中——研究耀斑-激波的传播特性（Ⅰ）          下载免费PDF全文

魏奉思  张剑虹 《地球物理学报》1990,33(2):125-134

本文提出一种用于研究太阳瞬变扰动在日球空间传播的新坐标系--瞬变源-日球电流片坐标系,并运用该坐标系以瞬变源耀斑为例,分析研究了由地球近空飞船观测到的277个耀斑-激波事件,发现:1.引起行星际激波和地球物理事件的大耀斑（H_α≥2,持续时间>半小时）的频数在耀斑-日球电流片坐标系中呈高斯分布,极值在电流片附近,那种在日面坐标系中随日面纬度呈双峰形的分布看不到了;2.当地球观测者和耀斑位于日球电流片同侧时,耀斑事件频次明显高于它们分处不同侧时的情形;3.激波参数（速度、磁场、密度和温度）呈现了同侧高于异侧,强激波多在同侧观测到;4.激波沿日球电流片方向的传播具有一定优势.上述结果表明,日球电流片的存在对瞬变扰动,如耀斑-激波在日球空间,特别是近太阳的传播可能具有重要影响.  相似文献   

高温超导磁强计研制及在瞬变电磁法中的应用   总被引：1，自引：0，他引：1  

陈晓东  赵毅  邓晓红  吕国印  张杰  赵敬洗 《物探与化探》2006,30(3):229-232

高温超导磁强计具有直接测量磁场、低噪声、高灵敏度、动态范围大、频带宽低频响应好的特点,可以取代感应线圈作瞬变电磁法的接收传感器。在理论上,高温超导磁强计应用在瞬变电磁法中具有优势。以高温超导磁强计作收传感器和以感应线圈作收传感器,在瞬变电磁法上进行了大量的野外对比试验,结果表明:把高温超导磁强计应用于瞬变电磁法(TEM)勘探上,能够加大勘探深度。  相似文献   

波包传播特征与西太平洋副热带高压移动的关系   总被引：5，自引：0，他引：5  

宋燕  缪锦海  琚建华 《气象学报》2006,64(5):576-582

利用波包传播诊断方法,研究高频波波包传播特征与瞬变波和副热带高压北进南退的关系。波包传播的初步特征为冬季波包传播生命史长,一般为7—10 d,传播速度为2—10 m/s,中心强度可超过0.4,在中高纬度地区传播路径一般为先向东南移,后向东北移;夏季比冬季的生命史短,中心强度也弱,传播路径与冬季相同。热带地区的波包传播路径先向西南,后向北移。一般波包强中心增强时,有利于槽发展,当强中心明显减弱时,有利于槽的衰减。当波包强中心持续地叠加在脊上时,脊将减弱。副热带高压的明显北跳常与南海特征区(0°—20°N,100°—120°E)持续5 d及以上的无波包强中心活动有关,并且在2次季节性北跳之后,又持续5 d以上出现波包强中心;副热带高压南移过程都与持续5 d及以上的南亚区域波包强中心、台风强中心或温带波包强中心活动有关。  相似文献   

Describing near surface, transient flow processes in unconfined aquifers below irrigated lands: A deforming finite element model for heterogeneous aquifers     

D.R. Purkey  W.W. Wallender  Nazrul Islam  G.E. Fogg  B. Sivakumar 《Journal of Hydrology》2006,330(3-4):435-443

Hydrologic models of irrigated lands generally adopt either a basin-scale or a root-zone perspective. While basin-wide macro-scale models rely on the aggregation of important spatial and temporal data across large areas, micro-scale root-zone models depend on the definition of rigid boundaries around the zone of plant–soil–water interaction. In reality, irrigation management decisions are made on a field by field basis and can interact across field boundaries. This paper first describes a shallow water table model, based on deforming finite element (DFE) framework, to characterize the near-surface field-to-field hydrologic response to various irrigation and drainage management regimes along a gently sloping alluvial fan. The model is then enhanced through changing geometry of a fluctuating water table below a series of irrigated fields. Such an enhancement also offers computational flexibility relative to the saturated–unsaturated models commonly used in micro-scale studies. The model is designed with the alluvial fan aquifers of California’s western San Joaquin Valley as reference systems.  相似文献   

A semi-analytical model in time domain for moving loads     

T. Bierer  C. Bode 《Soil Dynamics and Earthquake Engineering》2007,27(12):1073-1081

A model for investigations of ground motions due to continuously moving loads with constant and time-varying amplitudes is presented. The vertical displacements excited by moving load areas are obtained at a fixed observation point at the surface of the three-dimensional halfspace in time domain. The load is moving along a straight line with constant speed. To solve this nonaxisymmetric, initial boundary value problem a semi-analytical, discretized model is developed. It is based on Green's functions for a suddenly applied, stationary surface point load with Heaviside time dependency. These functions, also called influence functions of the halfspace, are valid for any homogeneous, isotropic and linear-elastic medium. The principle of superposition is used. Results are shown for the transient and the steady-state ground motions, and they are compared with analytical solutions. The load speed is varied in the subcritical range up to the propagation velocity of Rayleigh-waves.  相似文献   

Forward Lagrangian stochastic simulation of a transient source in the atmospheric surface layer     

E. H. Shadwick  J. D. Wilson  T. K. Flesch 《Boundary-Layer Meteorology》2007,122(2):263-272

We show that a forward Lagrangian stochastic (LS) model simulates well the ensemble-averaged concentration transient due to a short time (5 min) point source in the uniform atmospheric surface layer. In LS models, computational particles, which may not descend below ground level, are necessarily reflected at an imposed (artificial) boundary above ground. Model results were rather insensitive to the placing of the lower reflection boundary, and no definite benefit stemmed from including a parametrization for unresolved delays/displacements beneath the lower boundary.  相似文献   

TEM法斜坡函数断电效应的修正及正反演计算     

胡建德 《煤田地质与勘探》1995,23(1):51-54

介绍了层状大地上水平共平面共心线框在阶跃函数或矩形脉冲激发时使用Gaver-Stehfest算法计算互阻抗的方法以及斜坡函数断电效应的修正、给出了重叠回线装置时全时域视电阻率的计算方法和TEM资料的反演算法。   相似文献   

瞬变电磁法中心回线装置资料解释方法的改进   总被引：11，自引：1，他引：10       下载免费PDF全文

石显新  闫述  傅君眉  陈明生 《地球物理学报》2009,52(7):1931-1936

中心回线装置是瞬变电磁勘探中最常用的装置之一.中心回线装置的视电阻率一般从回线中心点场的公式出发导出.在现场实际施工中,为提高工作效率,把发射回线中部三分之一的区域作为观测范围.通过对场分布特征的分析研究表明,与中心点相比,观测区边缘处的感应电动势数值偏离达15%~25%,这与广泛存在于华北型煤系中赋存深度为400~1000 m的陷落柱、导水小断层等引起的异常相比,已经不可忽略.大定源回线公式可以准确地表示任意场点的感应电动势,由此导出视电阻率无边缘效应影响;观测按照中心回线方式并保持在近区进行,可使感应电动势和视电阻率之间的转换简单而直接.理论和实际应用结果表明,这些措施进一步提高了瞬变电磁探测中心回线方法的探测精度.在有上覆低阻屏蔽层的情况下,对埋深500~700 m的陷落柱给出了明显的异常反映,并被井下掘进所验证.  相似文献