云南强震的动力探讨

本文应用近年来多种地球物理方法对东亚及云南地区应力场、地壳上地幔构造研究成果，探讨了造成云南多震及大震空间分布特征的动力来源。由于印度板块与亚欧板块的碰撞挤压及青藏高原的高差作用使高原物质向东漫流，受到扬子准古陆及华南地块的阻挡，于是沿其焊接边界应力集中产生大震。加之本、非稳态热、介质的化学组成及物理状态等因素的综合作用造就了云南大震的空间分布特征。     

Seismic wave scattering effects under different canyon topographic and geological conditions

Based on our numerical model for wave scattering problems due to P and SV wave incidences and the frequency domain analysis procedure, the effect of canyon topographic and geologic conditions on ground motion due to P and SV earthquake wave incidences has been extensively studied in this paper. The numerical results from this research illustrated that: (1) canyon topographic and geologic conditions can dramatically affect both peak value and frequency contents of the free field motion along the canyon surface during an earthquake; (2) a canyon may be subjected to stronger ground motion when its predominant frequency is in coincidence with the predominant frequency of the incident earthquake wave; (3) a stronger wave mode conversion effect can be induced by a steeper canyon bank or a softer weathered stratum on the canyon surface in the case of an earthquake wave incidence; (4) compared with harmonic wave incidences, the amplification effect of a canyon on the incident earthquake wave is a little weaker due to the average self-healing effect of the earthquake wave.     

Local high-temperature phenomena within magnetic clouds

In this study,three methods were used to analyze 17 large-scale local high-temperature regions with durations exceeding 2 h within magnetic clouds(MCs)observed by advanced composition explorer from 1998 to 2008.Results show that five of these large-scale regions may have been caused by flare heating;seven of the regions may have been caused by nonuniform expansion when MCs propagated in the solar-terrestrial space;four large-scale high temperature regions may likely result from combined non-uniform expansion and flare heating;and only one large-scale local high-temperature region was not related to either flare heating nor non-uniform expansion.No evidence indicated that magnetic reconnection occurred or had occurred within the high-temperature regions.Based on our results,we infer that such local high-temperature phenomena within MCs are caused primarily as a result of flare heating and non-uniform expansion,either separately or jointly,and that magnetic reconnection plays only a minor role in the formation of high-temperature regions.     

2009年世界地震活动性和地震灾情概要

2009年地震频度较高,强度较低;地震灾情一般较轻,较重的地区一是印度尼西亚地区,其次是意大利地区。     

基于小波变换与小波包变换的降噪方法比较

在模拟地震记录信号中加入信噪比为17的高斯白噪声,然后分别采用小波降噪和小波包降噪方法,对含噪信号进行降噪处理。在不同降噪阈值下,比较降噪后信号的信噪比。结果表明:在同一降噪阈值下,小波包降噪后信号的信噪比高于小波降噪后信号的信噪比,而且采用wbmpen方法给定的阈值明显可以提高降噪后信号的信噪比。     

超大跨度斜拉桥考虑行波效应的地震动随机响应研究

斜拉桥地震反应不同于其它桥型,具有明显的空间耦合效应.利用有限元理论对苏通长江公路大桥的空间抗震性能进行分析,重点研究行波效应对结构响应的影响,并与一致激励计算的结果进行比较,为大跨度斜拉桥抗震分析采用随机方法提供了一定的参考依据.研究结果表明,行波效应对斜拉桥结构内力有显著的影响,大跨度斜拉桥抗震性能分析必须考虑行波效应.而行波效应的影响与结构自身动力特性、视波速、构件位置及研究响应类型(位移与内力)相关.     

应用神经网络建立加速度峰值衰减规律

在假定了加速度峰值衰减规律的形式后，本采用人工神经网络拟合实际加速度峰值观测资料来求取方程中的待定系数。为加速神经网络的训练，本设计了基于ＢＰ学习算法的目标分段网络训练法。     

大同阳高震区及其邻区壳幔速度结构与深部构造

利用通过本区６条宽角反射／折射剖面资料对大同阳高震区及邻区地壳上地幔速度结构与构造进行了详细的研究。结果表明,地壳上地幔速度结构与构造在纵向和横向上具有明显的不均一性。浅部基底断裂发育,而在其深部,根据波组特征、壳内界面及速度等值线起伏变化和低速异常体的边界等推测有３处地壳深断裂带。本区最明显的上地壳低速体位于大同—阳原附近,其南界存在地壳深断裂,大同阳高地震群与该低速异常体和深断裂有关。     

Burst strain disturbance — A new test study on fracture precursor

A multi-functional high-frequency seismometer, a new instrumental system, is used for recording multi-point strain variations of rock samples in the process of fracture development. The results indicate that strain in each point appears burst disturbance synchronously besides a tendency variation before main fracture. The burst disturbance could probably be one of the short-impending precursors before great earthquake.     

中国地震网格试验系统中资源管理与作业调度研究-资源管理和作业动态分配模型ProRMJS的建立me

通过分析与研究建立资源管理和作业动态分配ProRMJS模型,解决了中国地震灾害仿真网格试验系统（CEDAGrid）中网格科学计算平台在初期建设中存在的一些资源管理方面的问题. 针对网格科学计算平台默认各个计算节点均能提供计算服务的问题,ProRMJS通过ldquo;计算池rdquo;这一虚拟组织为调度器分发作业提供支撑;而调度器则根据计算池中各个节点的计算能力和状态,动态分配任务,这样就保证了计算平台的稳定性. 针对默认各个计算节点均能完成任务的问题, ProRMJS通过监控各个节点所负担作业的运行进度和设定作业时间阈值来管理作业运行. 对于各个节点计算能力大小的区别, ProRMJS通过对各个节点计算性能的权值量化,实行按ldquo;需rdquo;分配作业. 对各个节点计算性能的权值量化, ProRMJS是通过综合考虑各个因素对机器计算能力大小的影响后通过加权计算的方式完成的,从而提高了整个计算平台的工作效率. 最后通过实现地震应力触发科学计算实例验证了方案的有效性,为网格技术在地震领域内的进一步应用作了有意义的探索.