2003年2月24日新疆巴楚-伽师Ms6.8级地震加速度记录简介     

艾买提·乃买提 《内陆地震》2004,18(3):254-259

2003年2月24日新疆巴楚—伽师地区发生了Ms6．8级地震，极震区地震烈度Ⅸ度．布设在西克尔水库、伽师、巴楚强震固定地震台获取了该震的加速度记录。各地震台震中距分别为25km,47km、113km，记录到最大水平加速度峰值分别为85．39cm／8／8、50．71cm／s／s、76．03cm/s/s，反应谱的卓越周期为0．45—0．51s．对一次余震也作了介绍，同时提出几个问题供地震学者、地质学家及地震工程人员进一步探讨．  相似文献   

利用测震台网记录获得加速度波形的方法研究   总被引：3，自引：0，他引：3  

姚兰予  聂永安  赵靖华  卞真付 《中国地震》2004,20(1):39-46

研究了从测震台网速度记录获得高质量加速度波形的方法，并以天津蓟县台安装的CTSI-EDAS24速度型甚宽带地震仪和EST-Q4128型强。震仪对同一地震记录的处理分析为例，对计算步骤和处理方法进行了详细论述。处理结果的对比分析表明，该方法简单有效，拓宽了数字测震台网波形记录的服务应用范围。  相似文献   

Approximate representation of thep-norm distribution     

Sun Haiyan Ph.D 《地球空间信息科学学报》2001,4(3):1-5

［1］Liu D J,Shi W Z,Tong X H,et al.Precision analysis and quality cont rol of GIS spatial data.Shanghai:Shanghai Publishing House of Scientific Documen ts,1999 ［2］Chen X R,Fang Z B,Li G Y,et al.Non_parameter statistics.S hanghai:Shanghai Publishing House of Science and Technology,1989 ［3］Li Q H,Tao B Z.Application of probability statistical theory in survey ing.Beijing:Beijing Publishing House of Surveying and Mapping,1982 ［4］Sun H Y.p_norm distribution theory and its application in surveyin g data processing:[Ph.D Thesis].Wuhan:Wuhan Technical University of Surveying and Mapping,1995  相似文献   

高空急流加速与低层锋生   总被引：27，自引：10，他引：27  

高守亭  陶诗言 《大气科学》1991,15(2):11-22

本文从动力学上找到了低层锋生函数同急流区内纬向平均风加速的关系,指出高空急流加速有利于大气低层锋生,并从天气学的角度给出了高空急流加速同低层大气锋生的环流形态特征。即高空波的动量和热量通量在急流区的辐合,促使高空急流加速,并引起急流入口区上下层之间的质量调整,在急流轴高度以下出现一个反环流,反环流的上升支同其下原有的弱锋前的上滑爬升气流发生耦合,造成上滑气流加强,低层锋面坡度变陡,冷暖对比明显,引起大气低层锋生。  相似文献   

软土地基上土工结构物的离心模拟试验     

张师德  陈绪禄 《上海国土资源》1988,(4)

由于离心模拟试验所提供的高加速度可以模拟重力加速度,而引起土工结构物的稳定性和地基变形问题,主要原因正是由于地基不能适应上部结构物的自重,因而土工离心试验能最大限度地逼近现场试验,试验结果已为设计工程师所采用。本文主要介绍4个沿海工程如何利用离心模拟试验来检验这些工程的稳定和变形。  相似文献   

Relative Efficiency of Single-Outlier Discordancy Tests for Processing Geochemical Data on Reference Materials and Application to Instrumental Calibrations by a Weighted Least-Squares Linear Regression Model     

Surendra P. Verma  Lorena Díaz-González  Rosalinda González-Ramírez 《Geostandards and Geoanalytical Research》2009,33(1):29-49

Numerous studies report geochemical data on reference materials (RMs) processed by outlier-based methods that use univariate discordancy tests. However, the relative efficiency of the discordancy tests is not precisely known. We used an extensive geochemical database for thirty-five RMs from four countries (Canada, Japan, South Africa and USA) to empirically evaluate the performance of nine single-outlier tests with thirteen test variants. It appears that the kurtosis test (N15) is the most powerful test for detecting discordant outliers in such geochemical RM databases and is closely followed by the Grubbs type tests (N1 and N4) and the skewness test (N14). The Dixon-type tests (N7, N8, N9 and N10) as well as the Grubbs type test (N2) depicted smaller global relative efficiency criterion values for the detection of outlying observations in this extensive database. Upper discordant outliers were more common than the lower discordant outliers, implying that positively skewed inter-laboratory geochemical datasets are more frequent than negatively skewed ones and that the median, a robust central tendency indicator, is likely to be biased especially for small-sized samples. Our outlier-based procedure should be useful for objectively identifying discordant outliers in many fields of science and engineering and for interpreting them accordingly. After processing these databases by single-outlier discordancy tests and obtaining reliable estimates of central tendency and dispersion parameters of the geochemical data for the RMs in our database, we used these statistical data to apply a weighted least-squares linear regression (WLR) model for the major element determinations by X-ray fluorescence spectrometry and compared the WLR results with an ordinary least-squares linear regression model. An advantage in using our outlier procedure and the new concentration values and uncertainty estimates for these RMs was clearly established.  相似文献   

Solar wind influence on atmospheric processes in winter Antarctica     

O. Troshichev   《Journal of Atmospheric and Solar》2008,70(18):2381-2396

Galactic cosmic rays (GCRs) altered by solar wind are traditionally regarded as the most plausible agent of solar activity influence on the Earth's atmosphere. However, it is well known that severe reductions in the GCRs flux, known as Forbush decreases (FDs), are caused by solar wind of high speed and density, which sweeps away the GCRs on its way. Since the FD beginnings are registered at the Earth's orbit simultaneously with dramatic disturbances in the solar wind, the atmospheric effects, assigned to FDs, can be, in reality, the results of the solar wind influence on the atmospheric processes. This paper presents a summary of the experimental results demonstrating the strong influence of the interplanetary electric field on atmospheric processes in central Antarctica, where the large-scale system of vertical circulation is formed during winter seasons. The influence is realized through acceleration of the air masses, descending into the lower atmosphere from the troposphere, and the formation of cloudiness above the Antarctic Ridge, where the descending air masses enter the surface layer. The acceleration is followed by a sharp increase of the atmospheric pressure near-pole region, which gives rise to the katabatic wind strengthening above the entire Antarctica. The cloudiness formation results in the sudden warmings in the surface atmosphere, since the cloud layer efficiently backscatters the long wavelength radiation from the ice sheet, but does not affect the adiabatic warming process of the descending tropospheric air masses. When the drainage flow strengthening the circumpolar vortex around the periphery of the Antarctic continent decays, the surface easterlies typical of the coast stations during the winter season are replaced by southerlies and the cold Antarctic air masses flow out to the Southern ocean.  相似文献   

汶川8.0级地震强震动特征初步分析   总被引：19，自引：3，他引：16  

于海英  王栋  杨永强  卢大伟  解全才  张明宇  周宝峰  江纹乡  程翔  杨剑 《震灾防御技术》2008,3(4):321-336

本文对国家强震动台网中心收集的2008年5月12日14时28分04秒汶川8．0级地震中获取的420组三分量加速度记录进行了处理和初步分析。在这次地震中布设在龙门山断裂带及其周围地区的50多个台站获得了大于100gal的加速度记录,有46组三分量加速度记录的断层距小于100km,使中国大陆近断层区域所获得的强震动加速度记录的数量成倍增加。本文依据这批数据,对汶川大地震强震动特性进行了初步分析,给出了此次地震断层附近地区的PGA衰减规律,并利用此规律模拟了断层附近的加速度峰值,绘制了PGA分布图、竖向PGA与水平向PGA比值图;给出了汶川地震断层附近的加速度反应谱、上盘效应、竖向效应、速度大脉冲效应等地震动特征,这些特征可作为抗震设计规范修订的依据并供灾区重建时参考。  相似文献   

福建地区中小地震加速度与仿真加速度记录的反应谱特征分析     

林建生  叶雯燕  谢文杰  施关荣  吴淑美  陈新兴 《华南地震》2009,29(3):33-42

利用福建省区域数字强震动和数字地震台网历年的地震记录,通过资料选取、数据处理,计算了其地震反应谱,并分析了Ⅰ、Ⅱ、Ⅲ类场地反应谱谱形参数的统计关系及反应谱特征．有关研究结果对合理地利用福建地区现有台网观测资料具有实际意义。  相似文献   

Errors in velocities and displacements deduced from accelerographs: An approach based on the theory of error propagation   总被引：3，自引：0，他引：3  

Stathis C. Stiros   《Soil Dynamics and Earthquake Engineering》2008,28(5):415-420

Based on the theory of errors, and in particular on the law of error propagation and approximation techniques, we present some simple formulae for random errors of velocities and displacements computed on the basis of numerical integration of accelerometer records. These errors are regarded as function of the characteristic errors of accelerometers and of the duration of the signal for velocities, and of the square of the duration of the signal for displacements. Instabilities in the sampling rate introduce additional noise, which is proportional to the sum of the squares of measurements of acceleration, mostly influenced by high peaks. Because of uneven weighting, however, peaks at early stages of the record are more important than in their later stages.  相似文献