共查询到20条相似文献，搜索用时 78 毫秒
1.
RESPONSE OF TRANSMISSION TOWER SYSTEM TO HORIZONTAL AND ROCKING EARTHQUAKE EXCITATIONS 总被引：1，自引：0，他引：1
理论分析和震害经验表明，地震动的转动分量对某些工程结构的影响是重要的。本文提出了高压输电塔－导线耦联体系在水平和摇摆地震动作用下更一般的分析方法，推导出耦联体系的运动方程，给出了数值算例，结果表明，地震动摇摆分量对输电塔耦联体系的影响是重要的。 相似文献
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MR阻尼器耦联的带裙房高层建筑的半主动逻辑控制方法 总被引：3，自引：1，他引：3
针对MR阻尼器耦联的带裙房高层建筑的特点，提出了一种MR阻尼器耦联的带裙房高层建筑的半主动逻辑控制方法，并用此方法对12层带3层裙房的高层建筑进行了试验控制。结果表明，此种方法简单，工程实现容易。 相似文献
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理论分析和震害经验表明，地震动的转动分量对某些工程结构的影响是重要的。本文提出了高压输电塔－导线耦联体系在水平和摇摆地震动作用下更一般的分析方法，推导出耦联体系的运动方程，给出了数值算例，结果表明，地震动摇摆分量对输电塔耦联体系的影响是重要的。 相似文献
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振动台实时耦联动力试验系统构建解决方案 总被引：2，自引：1，他引：1
实时耦联动力试验(RTDHT)是一种将物理模型试验和数值求解计算实时耦联在一起进行整体结构动力反应分析的新型结构动力试验方法。构建实时耦联动力试验系统将面临数值子结构实时计算、数据实时传输、加载器精确加载等问题。本文首先以清华大学新近建成的一套基于振动台的实时耦联动力试验系统为例,对试验系统构建中面临的问题以及相应的解决方案进行了阐述,对构建实时耦联动力试验系统提出了一些指导性的建议。随后简要介绍了利用该系统已经进行的一些实时耦联动力试验,并对实时耦联动力试验可能的应用前景进行了探讨。 相似文献
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平扭耦联隔震体系的简化模型及有关参数变化的计算分析 总被引：5，自引：1，他引：5
李向真 《地震工程与工程振动》2005,25(3):163-166
本文根据隔震结构的动力学特点，提出了空间平扭耦联隔震结构简化计算模型，该模型仅有四个自由度，做定性分析和近似计算十分方便，力学概念明确可靠，文中并对这种体系的动力特性和反应，采用反应谱方法进行分析计算。还对平扭耦联隔震结构的重要特征参数对结构的动力特性和动力反应的影响，进行了较为全面的分析研究。 相似文献
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输电塔—线耦联体系地震反应分析方法（Ⅱ）：纵向 总被引：2，自引：1，他引：2
在地震作用下、由输电塔和导线组成的耦联体系的精确分析是非常复杂的，工程中需要的一种合理的抗震计算简图。文献「１」和「２」提出了该种耦联体系的简化抗震计算方法，本文进一步发展了这种方法，建立了该种耦联体系在纵向地震作用下更一般的力学模型，导出了相应的运动方程和求解方法。 相似文献
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偏心结构非线性地震反应分析的一种简化方法 总被引：1，自引：1，他引：1
本文建立了基于结构状态方程和偏心结构体系的层剪力-扭矩等效屈服EYST面概念的求解平扭耦联非线性地震反应的分离-予估-修正递推算法，编制了相应的计算程序。通过与三个单层偏心结构模型的破坏性地震模拟试验结果的对比，验证了小变形阶段平-扭耦联地震反应算法的实用性和可靠性。算例表明，该程序数据处理量小，运算快捷，便于应用。 相似文献
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双向偏心结构扭转耦联地震反应的序列最优控制 总被引：1，自引：0，他引：1
本文分析了不对称建筑结构平移-扭转耦联振动的动力特性及地震作用下的响应;根据地震动输入结构的过程,推导出一种更为一般的最优控制算法,所获得的控制力表达式同时包括地震响应和地震激励。通过对一非规则四层框架结构的扭转耦联地震反应控制分析表明,该算法不仅能有效地控制结构的平移地震反应,而且更有效地抑制结构的扭转耦联地震反应。 相似文献
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本文用二维有限元法,将弹性多孔介质中应力-孔隙压耦联理论应用于新丰江水库诱发地震机制的研究。计算中,不仅考虑了均匀、非均匀模型的耦联,还考虑了断层的性质、产状对耦联作用的影响及库水位随时间的变化。 结果表明:附加应力与孔隙压耦联作用是诱发水库地震的重要因素。新丰江水库地震不仅与库区存在的断裂、高密度基底有关,还与库水的加、卸载方式有关。 相似文献
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大跨越输电塔-线体系动力特性分析 总被引：20，自引：0，他引：20
大跨越输电塔-线体系的动力特性评估是其抗风、抗震设计的重要环节。本文在有关文献的基础上，建立了大跨越输电塔-线体系耦联振动动力特性分析的多自由度体系计算方法，并对大跨越输电塔-线体系工程实例的动力特性进行了分析，计论了塔-线耦联振动对塔，线各自动力特性的影响，得到了若干结论。 相似文献
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常规τ值法假设应力松弛时间与应变延迟时间近似相等, 造成了常Q模型拟合精度低. 本文利用精确的广义流变体模型Q值计算公式, 研究改进的τ值法求解常Q模型参数. 根据地震波散射理论, 推导了基于广义流变体模型的黏滞性介质一阶波恩近似方程, 结合位移-速度关系得到了含卷积完全匹配层边界条件的黏滞性介质应力-速度方程的一阶波恩近似表达式. 通过数值实验验证并对比了黏滞性介质中全波波动方程、 一阶波恩近似方程以及单程波波动方程的波场特征, 讨论了基于流变体模型的黏滞性介质一阶波恩近似方程对速度扰动和Q扰动的适应性, 以及对旅行时和振幅精度的影响. 相似文献
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常规Alkhalifah动校正公式精度低，不能精确描述各向异性介质长偏移距地震反射同相轴的时距关系.本文以提高VTI介质长偏移距地震资料动校正公式的精度为目标，在分析VTI介质常规动校正方程的基础上，根据误差最小原理建立优化校正系数图版，实现对常规动校正公式大偏移距误差的修正，建立最优化校正Alkhalifah动校正方程,实现了对VTI介质长偏移距地震资料常规动校正方程的改进.之后由Fomel群速度公式导出高精度VTI模型长偏移距时距函数，提出了高精度VTI介质长偏移距地震资料动校正方程.将以上的动校正方程用于各向异性参数反演，模型计算表明最优化校正Alkhalifah动校正方程的反演精度是常规长偏移距动校正方程反演精度的2～4倍，高精度动校正方程的反演精度是常规动校正方程反演精度的2～8倍. 相似文献
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Vertical mixing beneath the bed surface and its effect on sediment composition has long been underestimated. This paper proposes a mixing equation to illustrate the temporal and spatial variations of bed material composition for bed form dominant rivers. A continuous mass conservation equation for elevation-specific nonuniform bed material composition is initially presented. A vertical mixing equation is finally derived as a diffusion-type partial differential equation with a source term charact... 相似文献
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Introduction The phenomenon of water level tide was discovered at Duchort diggings, Czech in 1879. By 1939, Theis, an America hydrogeologist, confirmed that periodical wave of the well water level is caused by the solid tide. In 1964, Melchior, a Belgium geophysist, began to make research on this phenomenon. Then Cooper (1965), Bredehoeft (1967) and WANG, et al (1988) followed. In China the study on water level tide began with 1970s, and the study on well water level phase lagging began … 相似文献
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Second-order exact ensemble averaged equation for linear stochastic differential equations with multiplicative randomness and random forcing is obtained by using the cumulant expansion ensemble averaging method and by taking the time dependent sure part of the multiplicative operator into account. It is shown that the satisfaction of the commutativity and the reversibility requirements proposed earlier for linear stochastic differential equations without forcing are necessary for the linear stochastic differential equations with forcing when the cumulant expansion ensemble averaging method is used. It is shown that the applicability of the operator equality, which is used for the separation of operators in the literature, is also subjected to the satisfaction of the commutativity and the reversibility requirements. The van Kampen’s lemma, which is proposed for the analysis of nonlinear stochastic differential equations, is modified in order to make the probability density function obtained through the lemma depend on the forcing terms too. The second-order exact ensemble averaged equation for linear stochastic differential equations with multiplicative randomness and random forcing is also obtained by using the modified van Kampen’s lemma in order to validate the correctness of the modified lemma. Second-order exact ensemble averaged equation for one dimensional convection diffusion equation with reaction and source is obtained by using the cumulant expansion ensemble averaging method. It is shown that the van Kampen’s lemma can yield the cumulant expansion ensemble averaging result for linear stochastic differential equations when the lemma is applied to the interaction representation of the governing differential equation. It is found that the ensemble averaged equations given for one the dimensional convection diffusion equation with reaction and source in the literature obtained by applying the lemma to the original differential equation are restricted with small sure part of multiplicative operator. Second-order exact differential equations for the evolution of the probability density function for the one dimensional convection diffusion equation with reaction and source and one dimensional nonlinear overland flow equation with source are obtained by using the modified van Kampen’s lemma. The equation for the evolution of the probability density function for one dimensional nonlinear overland flow equation with source given in the literature is found to be not second-order exact. It is found that the differential equations for the evolution of the probability density functions for various hydrological processes given in the literature are not second-order exact. The significance of the new terms found due to the second-order exact ensemble averaging performed on the one dimensional convection diffusion equation with reaction and source and during the application of the van Kampen’s lemma to the one dimensional nonlinear overland flow equation with source is investigated. 相似文献
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A quasi three-dimensional (QUASI 3-D) model is presented for simulating the subsurface water flow and solute transport in the unsaturated and in the saturated zones of soil. The model is based on the assumptions of vertical flow in the unsaturated zone and essentially horizontal groundwater flow. The 1-D Richards equation for the unsaturated zone is coupled at the phreatic surface with the 2-D flow equation for the saturated zone. The latter was obtained by averaging 3-D flow equation in the saturated zone over the aquifer thickness. Unlike the Boussinesq equation for a leaky-phreatic aquifer, the developed model does not contain a storage term with specific yield and a source term for natural replenishment. Instead it includes a water flux term at the phreatic surface through which the Richards equation is linked with the groundwater flow equation. The vertical water flux in the saturated zone is evaluated on the basis of the fluid mass balance equation while the horizontal fluxes, in that equation, are prescribed by Darcy law. A 3-D transport equation is used to simulate the solute migration. A numerical algorithm to solve the problem for the general quasi 3-D case was developed. The developed methodology was exemplified for the quasi 2-D cross-sectional case (QUASI2D). Simulations for three synthetic problems demonstrate good agreement between the results obtained by QUASI2D and two fully 2-D flow and transport codes (SUTRA and 2DSOIL). Yet, simulations with the QUASI2D code were several times faster than those by the SUTRA and the 2DSOIL codes. 相似文献
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J. J. Westerink 《Advances in water resources》1987,10(4)
A finite element method formulation for solving the harmonic shallow water equations in their primitive or unmodified form is developed and analysed. The scheme, referred to as the Primitive Pseudo Wave Equation Formulation (PPWE), involves developing a weak weighted residual form of the continuity equation and furthermore forming a pseudo wave equation by substituting the discretized form of the momentum equation into the discretized form of the continuity equation. The final set of equations to be solved, the pseudo wave equation and the primitive momentum equations, deceptively resemble the discretized equations of the wave equation formulation of Lynch and Gray. Despite this resemblance, Fourier analysis indicates that the PPWE scheme is still fundamentally primitive.However, application of the PPWE scheme to a set of stringent test problems results in very good solutions with well controlled nodal oscillations. It is shown that this low degree of spurious oscillations is due to the treatment of the boundary conditions such that elevation is taken as an essential condition and normal flux is taken as a natural condition. This particular boundary condition treatment is suggested by the formation of the pseudo wave equation. Furthermore, even though the equation re-arrangement does not in itself effect the solutions, it does make the scheme much more efficient. 相似文献
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The galvanic problem is frequently solved by a Fredholm integral equation of the second kind based on a single layer source formulation. At higher conductivity contrasts between the model and its surroundings the homogeneous part of the integral equation approaches an eigenvalue equation. With infinite contrast the solution of this limiting integral equation is non-unique, but in the subspace of zero total charge the solution is unique. This mathematical property of the integral equation is reflected in its numerical solution with the result that large numerical errors may appear and convergence of the solution becomes very slow. Errors are, for the most part, related to the computed excess charge generated in the numerical solution. The effect is studied by comparing the results computed from the solution of the integral equation alone with those computed from a particular solution where the requirement of zero total charge is used as a constraint. The model examples clearly show that the use of the constraint condition significantly improves the accuracy of the results. 相似文献