1) inelastic attenuation value Q
非弹性衰减Q值
1.
According to 437 horizontal-component seismograms recorded at 21 stations of Gansu Digital Seismic Network,we used Genetic Algorithm and Atkinson s method to study the inelastic attenuation value Q of the northeastern margin of Qinghai-Tibet plateau and the site response of each station based on the trilinear geometrical spreading model.
根据甘肃数字地震台网21个子台的437条波形记录,采用三段几何衰减模型,利用Atkinson方法和遗传算法,研究了青藏高原东北缘地区的非弹性衰减Q值和各台站的场地响应,得到该地区非弹性衰减Q值与频率f的关系为:Q(f)=564。
3) anelastic attenuation
非弹性衰减
1.
The combined effects of soft rock sites and anelastic attenuation factor have been separated and determined respectively by(using) this method.
采用该方法,分离软基岩场地联合效应和非弹性衰减的影响,并把二者分别确定出来。
4) inelastic attenuation
非弹性衰减
1.
The inelastic attenuation model of media in the Sichuan Basin region has been studied by using the joint conversion of genetic algorithm based on the waveform data recorded by Sichuan Digital Seismic Network.
利用四川数字地震台网记录的地震波形资料,采用遗传算法联合反演方法研究了四川盆地地区的介质非弹性衰减模型。
2.
In this paper, according to the relationship of observation spectrum with source spectrum, travel-path attenuation factor and site effect, we use the digital seismic data of moderate-small earthquakes to invert the soft rock site effect and S wave inelastic attenuation under the constraint of site effect, and determine the parameters of path and site.
采用中小地震的数字观测资料,依据地震观测谱和震源谱、传播路径衰减因子及场地效应的关系式,在对场地效应约束的条件下,反演S波非弹性衰减和软基岩场地效应,确定研究区路径、场地参数。
3.
Using 487 pieces of digital oscillograms of 19 seismic events recorded at 32 seismologic stations located on Ordos massif and its surroundings, we calculate the parameters of three segments attenuation and the relation of inelastic attenuation Q value with frequency in the crust of Ordos Massif, the site responses of 32 stations and the source parameters of 19 events by the genetic algorithm.
采用分布于鄂尔多斯地块及其周缘的32个地震台站记录到的19次地震事件共487条数字化波形记录,利用遗传算法反演得到了整个鄂尔多斯地块地壳内S波的三段几何扩散参数、S波非弹性衰减Q值随频率变化的关系式、32个台站的场地响应以及19次地震的震源参数。
5) inelastic attenuation coefficient
非弹性衰减系数
1.
5 earthquakes from Fujian digital seismic station network since 1998, the inelastic attenuation coefficient, geometric diffusion coefficient, site response and seismic source parameters of seismic waves of Fujian area are calculated based on the algorithms proposed by Atkinson et al.
5级以上地震的波形资料,采用Atkinson等提出的方法计算了福建地区地震波非弹性衰减系数、几何扩散系数和台站场地响应。
补充资料:弹性散射和非弹性散射
弹性散射和非弹性散射 elastic scattering and inelastic scattering 使用粒子间碰撞来研究粒子的性质、相互作用和内部结构的两种情况。如果碰撞过程中两粒子间只有动能的交换,粒子类型、其内部运动状态和数目并无变化,则称为弹性散射或弹性碰撞。如果碰撞过程中除了有动能交换外,粒子的数目、类型和内部状态有所改变或转化为其他粒子,则称为非弹性散射或非弹性碰撞。 散射过程的研究对于了解许多物理现象具有很重要的意义。例如E.卢瑟福对a粒子被物质散射的研究,提出原子的有核模型;J.弗兰克和G.L.赫兹的电子与原子碰撞实验证实了N.玻尔的定态假设;建造高能加速器就是利用被加速粒子的散射过程来研究粒子的性质、相互作用和相互转化的规律。60年代末到70年代初利用高能轻子对质子和中子的深度非弹性散射的实验,发现质子和中子内部存在点状结构。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条