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81.
Stressrelaxationandattenuationoffluid-saturatedsandstoneatlowfrequencyDao-YingXI(席道瑛),Ai-WenLIU(刘爱文)andWeiLIU(刘卫)(Universityo... 相似文献
82.
The analysis and interpretation of coda waves have received increasing attention since the early seventies. In the past few years interest in this subject has spread worldwide, and the study of high-frequency seismic coda waves has become a very important seismological topic. As a conclusion of the studies accomplished in this time, coda waves are considered the result of scattering processes caused by heterogeneities acting on seismic waves.P andS waves play a particularly important role in this interaction. The process introduces an attenuation which, added to the intrinsic absorption, gives the observed apparent attenuation. Therefore, coda waves constitute a thumbprint left by the heterogeneities on the seismograms. Coda waves offer decisive information about the mechanism of how scattering and attenuation take place. This review describes coda waves in detail, and summarizes the work done in this subject to 1986. The relation between coda waves and attenuation in the context of research on seismic scattering problems is stressed. Particular attention has been given to the application of coda waves to estimate source and medium parameters. The state-of-the-art of the temporal variations of coda wave shape, and the possible use of these variations as an earthquake precursor also are presented. Care has been taken to introduce the statistical models used to deal with the heterogeneities responsible for scattering. 相似文献
83.
中小震近场地震动估计中地震动衰减关系的适用性分析 总被引:9,自引:1,他引:9
核工程场地设计基准地震动确定中涉及弥散地震的地震动估计,这导致中小震近场地震动估计成为被关注的研究课题。本文基于一些中小震近场地震动记录资料,分析和探讨了国内外多种地震动衰减关系对中小震近场地震动估计的适用性问题,并结合我国几个核工程地震问题研究工作的实践对中小震近场地震动衰减关系确定的思路和原则提出了建议。 相似文献
84.
安徽地区地震波衰减、场地响应及震源新参数的测定 总被引:5,自引:2,他引:5
根据安徽数字地震台网7个地震台的143条波形资料,研究了安徽地区的衰减模型和各台站的场地响应。采用三段几何衰减模型拟合,得到了安徽及邻近地区的几何衰减函数,得到安徽地区非弹性衰减Q值随频率f的关系为Q(f)=235.3×f0.616;7个台站的场地响应均无明显的放大效应,这与它们均处于岩石地基相符;并在本地区地震预测研究中尝试使用新参数,进行了初步的应用。 相似文献
85.
86.
Izmir Bay is one of the most polluted estuaries in the whole Mediterranean Sea. The inner part of the Bay (Inner Bay) is heavily
affected by domestic and industrial discharge. As a result of these loads, strong eutrophication occurs in the Inner Bay,
which is temporally anaerobic. The ecologically sensitive approach of the local authorities during the last decade has given
rise to a wide variety of monitoring and research studies on this bay. On the other hand, the municipality of Izmir started
to operate wastewater treatment facilities since January 2000. The Institute of Marine Sciences and Technology — Izmir (IMST)
with its research vessel R/V K Piri Reis has been conducting an intensive monitoring program since 1988 and especially during
the recent few years. These investigations provide an opportunity for the evaluation of the performance of the wastewater
treatment plant in terms of the change in the optical properties of Izmir Bay water in a positive manner. The turbidity values
measured in these monitoring studies indicate that the values have changed drastically after January 2000. Their spatial variation
indicates that the values decrease from the Inner Bay towards the Aegean Sea. The turbidity (light transmission) values are
measured with an automatic CTD (conductivity, temperature and depth) system during each cruise. The seiche disc depth measurement
is carried out only occasionally. The accuracy of the seiche disc depth is dependent on certain daylight conditions and depends
on the operator. The seiche disc depth (D
s) is an important parameter to estimate primary production of organic matter (hereafter called production). A relation between
light transmission (turbidity) value and seiche disc depth (D
s) is found with very good agreement. The correlations are very high (approximately 0.94) with slight seasonal variation. 相似文献
87.
88.
89.
3-D S-waveQ structure in Jiashi earthquake region is inverted based on the attenuation of seismic waves recorded from earthquakes in
this region in 1998 by the Research Center of Exploration Geophysics (RCEG), CSB, and a rough configuration of deep crustal
faults in the earthquake region is presented. First, amplitude spectra of S-waves are extracted from 450 carefully-chosen
earthquake records, called observed amplitude spectra. Then, after instrumental and site effect correction, theoretical amplitude
spectra are made to fit observed amplitude spectra with nonlinear damped least-squares method to get the observed travel time
overQ, provided that earthquake sources conform to Brune’s disk dislocation model. Finally, by 3-D ray tracing method, theoretical
travel time overQ is made to fit observed travel time overQ with nonlinear damped least-squares method. In the course of fitting, the velocity model, which is obtained by 3-D travel
time tomography, remains unchanged, while onlyQ model is modified. When fitting came to the given accuracy, the ultimateQ model is obtained. The result shows that an NE-trending lowQ zone exists at the depths of 10–18 km, and an NW-trending lowQ zone exists at the depths of 12–18 km. These roughly coincide with the NE-trending and the NW-trending low velocity zones
revealed by other scientists. The difference is that the lowQ zones have a wider range than the low velocity zones.
Foundation item: Joint Seismological Science Foundation of China (957-07-414) and State Key Basic Research Development and Programming Project
(95-13-02-02).
Contribution No. RCEG200105, Research Center of Exploration Geophysics, China Seismological Bureau. 相似文献
90.
In recent years, more and more studies are focused on the performance in seismic design instead of the strength of structures. People have realized that the structure deformation (displacement) can describe the damage more properly and directly than the strength (force). The displacement design spectra need to be constructed within more wide range of the period and the damping for the displacement-based seismic design. 相似文献