Time probabilistic evaluation of seismically induced landslide hazard in Irpinia (Southern Italy)   总被引：2，自引：0，他引：2  

V. Del Gaudio  J. Wasowski 《Soil Dynamics and Earthquake Engineering》2004,24(12):915-928

A recently proposed method, which incorporates the Newmark model to evaluate the earthquake-induced landslide hazard at regional scale, was applied to Irpinia, one of the most seismically active regions of Italy. The method adopts a probabilistic approach to calculate values of critical acceleration a_c representing the minimum strength required for a slope not to fail at a fixed probability level in a given time interval. Regional probabilistic hazard maps were generated for the two failure types most common in Irpinia (slump–earthflows and rock falls). The results suggest that quite moderate critical acceleration (0.05–0.08 g) could suffice to keep the slope failure probability low. However, the available data indicate that potential slide surfaces with a_c below these values could be common in Irpinia, where, perhaps in relation to particular geo-environmental conditions, a relative large number of marginally stable slopes might survive other destabilising actions and fail even on occasion of not particularly strong earthquake shaking.  相似文献   

Geomagnetic diurnal-variation anomalies and their relation to strong earthquakes     

Ding Jian-hai  Liu Jie  Yu Su-rong  Xiao Wu-jun 《地震学报(英文版)》2004,17(1):85-93

The diurnal-variation anomalies of the vertical-component in geomagnetic field are mainly the changes of phase and amplitude before strong earthquakes. On the basis of data recorded by the network of geomagnetic observatories in China for many years, the anomalous features of appearance time of the minima of diurnal variations (i.e, low-point time) of the geomagnetic vertical components and the variation of their spatial distribution (i.e, phenomena of low-point displacement) have been studied before over 30 strong earthquakes with M _S≥6.6 such as Kunlunshan M _S=8.1 earthquake on November 14, 2001; Bachu-Jashi M _S=6.8 earthquake on February 24, 2003; Xiaojin M _S=6.6 earthquake on September 22, 1989, etc. There are good relations between such rare phenomena of geomagnetic anomalies and the occurrence of earthquakes. It has been found that most earthquakes occur in the vicinity of the boundary line of sudden change of the low-point displacement and generally within four days before and after the 27th or 41st day counting from the day of appearance of the anomaly. In addition, the anomalies of diurnal-variation amplitude near the epicentral area have been also studied before Kunlunshan M _S=8.1 earthquake and Bachu-Jiashi M _S=6.8 earthquake. Foundation item: National Science Technology Tackle Key Project during the Tenth Five-year Plan (2001BA601B01-05-04)  相似文献   

工业测量中平行光管定向法的试验研究     

李欣  冯文灏  张志华 《测绘信息与工程》2005,30(5):47-49

介绍平行光管法的有关概念,利用实验室内的稳固水泥测墩及控制点,研究平行光管法确定起始方向线的误差及其引起的点位位移与图形变形间的关系,指出在高精度工业测量中,使用平行光管法及图形变形理论可提高工业目标测量精度。  相似文献   

3-D rheologic model of earthquake preparation (I) — Displacement field     

Song Zhi-ping  Yin Xiang-chu  Mei Shi-rong 《地震学报(英文版)》2003,16(6):588-597

Based on the three-dimensional ela stic inclusion model proposed by Dobrovolskii, we developed a three-dimensional rheologic inclusion model and theory to study the earthquake preparation process. By using correspondence principle in the theory of rheologic mechanics, we derived the analytic expression of the viscoelastic displacement at an arbitrary point (x, y, z) in three directions of x, y and z-axes (i.e., U(r, t), V*(r, t) and W(r, t)) produced by a three-dimension inclusion in the semi-infinite rheologic medium defined by the standard linear rheologic model. Foundation item: Chinese Joint Seismological Science Foundation (101105)  相似文献   

Digital photogrammetry as a tool in analogue modelling: applications to volcano instability     

F. Donnadieu  K. Kelfoun  B. van Wyk de Vries  E. Cecchi  O. Merle 《Journal of Volcanology and Geothermal Research》2003,123(1-2):161

Three techniques of digital photogrammetry have been applied successfully to laboratory analogue models to study surface displacements caused by various volcano deformation types. Firstly, side-perspective videos are used to differentiate profile displacements between cryptodome intrusion models and models deforming by ductile inner-core viscous flow. Both models show similar morphologic features including a bulged flank and an asymmetric upper graben. However, differences in displacement trajectories of the bulge crest reflect upward intrusion push contrasting with essentially downward displacement vectors of weak core models. The other two techniques use vertical views correlated automatically either as time-sequence monoscopic views or as coeval stereoscopic pairs. This exploits to a maximum the method’s potential by imaging surface displacements over the whole model. Successive monoscopic photograms, because they suffer only moderate numerical processing for topographic effect removal, can detect very small displacements occurring early in deformation processes. As illustrated by analysis of intrusion models, the monoscopic method allows prediction of fault locations and main displacement locations. It can also anticipate the principal strain directions, and separate different deformation stages. On the other hand, the stereo-photogrammetry technique, although more complicated, provides topography and volume changes, as well as pictures of surface displacements in three dimensions. Results are presented for the spreading of volcano models on a ductile substratum and viscous cored cones. We have found digital photogrammetry to be a useful tool for analogue modelling, because it provides quantitative data on surface displacements, including movement invisible to the eye, as well as topographic changes. It is a good method for investigating and comparing different deformation mechanisms. It is especially useful for interpretation of displacement patterns obtained from monitoring of natural active volcanoes. In fact, results of the methods used in the laboratory can be directly compared with field data from geodetic or photogrammetric surveys, as at Mount St. Helens in 1980.  相似文献   

Effect of causal and acausal filters on elastic and inelastic response spectra     

David M. Boore  Sinan Akkar 《地震工程与结构动力学》2003,32(11):1729-1748

With increasing interest in displacement spectra and long‐period motions, it is important to check the sensitivity of both elastic and inelastic response spectra to the filtering that is often necessary to remove long period artifacts, even from many modern digital recordings. Using two records of very different character from the M=7.1, 1999 Hector Mine, California, earthquake, we find that the response spectra can be sensitive to the corner periods used in causal filtering, even for oscillator periods much less than the filter corner periods. The effect is most pronounced for inelastic response spectra, where the ratio of response spectra computed from accelerations filtered at 25 and 200 sec can be close to a factor of 2 for oscillator periods less than 5 sec. Published in 2003 by John Wiley Sons, Ltd.  相似文献   

基于性态的砌块砌体结构极限性态目标位移确定方法的研究   总被引：7，自引：0，他引：7  

屈成忠  谢礼立 《地震工程与工程振动》2003,23(2):18-25

对砌块砌体结构进行Push—over分析，其结果准确与否和结构的极限性态目标位移的可靠确定关系很大。本文基于大量的配筋砌块砌体墙片试验结果，对直接基于位移的抗震设计法进行改进，使之能够用于砌块砌体结构的极限性态目标位移的确定。用改进的方法求解一座1／4比例的10层砌块砌体模型结构的极限性态目标位移，并与该模型结构的振动台试验结果进行比较。结果说明本文提出的改进方法是可以应用于求解砌块砌体结构的极限性态目标位移的。  相似文献   

钢筋混凝土结构倒塌分析的前沿研究   总被引：13，自引：1，他引：13  

张雷明  刘西拉 《地震工程与工程振动》2003,23(3):47-52

结构倒塌分析主要涉及三个难点，即不连续位移场的描述、接触碰撞分析以及结构倒塌过程中大位移、大转动的描述。本文就国内外研究现状针对结构倒竭的评定标准以及上述三个难点做出评述，同时介绍了作者近期工作，并对今后研究工作做了展望，以供参考。  相似文献   

Active blocks and their deformations derived from the velocity field in North China   总被引：1，自引：0，他引：1  

黄立人  杨国华  王敏 《地震学报(英文版)》2003,16(1):79-91

Based on the horizontal movement velocities and their error estimations of 144GPS stations in North China de-duced from the results obtained from multiple GPS measurements carried out in the period of 1992-2001,the horizontal deformation in the area is stuklied.The movements,entire deformations,local deformations,activeity patterns and intensities along the boundary zones are derived.And then the risk of strong earthquake in the area is estimated.In the research,the horizontal displacement observations can be considered as the sum of three parts.The first part is the entire motion following Eurasian plate,which can be derived from NUVAL-IA model;the second part is the relative motions and deformations between the sub-tectonic blocks in the studied area,which can be derived from a set of displacement observations determined by the expanded QUAD method in the paper;the third part is the local deformations and errors in the sub-tectonic blocks,which can be described as the inhomoge-neous strains of the block.The method and results are introduced in detail in the paper.  相似文献   

南天山库车秋里塔格褶皱带三维构造分析   总被引：17，自引：3，他引：17  

管树巍 汪新杨树锋  赵卫东徐峰 雷刚林 《地质论评》2003,49(5):464-473

笔者利用库车秋里塔格地区3000km的二维地震反射资料，结合地表构造测量成果，分段叙述秋里塔格褶皱带的构造几何学和运动学性质，说明构造交汇部位断层和褶皱的叠加过渡关系，并通过二维构造剖面的组合，建立秋里塔格褶皱带的三维构造几何模型。研究发现秋里塔格褶皱带为浅部断层传播褶皱与深部断层转折褶皱叠加形成的复合型背斜带，深部台阶状逆断层的叠加作用、叠加断层位移量的转换、断层断坡高度的变化造成地表背斜沿走向发生变化，笔者通过测量断层叠加方式、断层位移量转换、断层断坡高度，说明秋里塔格褶皱带背斜叠加、扭曲、分叉现象的构造机理，并且给出了秋里塔格褶皱带断层的滑移量。  相似文献