扩大SM-3KV短周期地震仪的工作频率范围

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS
A. N. Besedina, N. V. Kabychenko, S. G. Volosov, A. G. Goev, N. L. Konstantinovskaya, R. A. Reznichenko
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引用次数: 0

摘要

本文介绍了一种利用SM-3KV短周期地震仪将传感器的频带扩展到低频区的仪器解决方案。校正电路建立在运算放大器上的两级积分器上。开发的原型SM-3KV-cor在实验室和现场条件下进行了测试。对爆炸和地震记录的分析表明,所开发的方案可用于进行频率高于0.06 Hz的地震监测。通过与宽频带地震仪数据的对比,表明SM-3KV-cor可以基于接收函数的构造重建地震台站安装点附近的地壳速度特征。在分析P-S转换波总记录时,在约660 km深度的上地幔相变带下边界处识别出一个相位,这表明SM-3KV-cor传感器也可以用于分析相变带特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Expanding the Operating Frequency Range of SM-3KV Short-Period Seismometers

Expanding the Operating Frequency Range of SM-3KV Short-Period Seismometers

The article provides an example of an instrumental solution for expanding the frequency band of the sensor into the low-frequency region using the SM-3KV short-period seismometer. The correction circuit is built on two stages of integrators on operational amplifiers. The developed prototype SM-3KV-cor was tested in laboratory and field conditions. Analysis of records of explosions and earthquakes showed that the developed scheme can be used when conducting seismic monitoring at frequencies above 0.06 Hz. When compared with data from a broadband seismometer, it is shown that the SM-3KV-cor can be used to reconstruct the velocity features of the Earth’s crust near the installation site of a seismic station based on the construction of receiver functions. When analyzing the total records of P-S converted waves, a phase was identified from the lower boundary of the phase transition zone of the upper mantle at a depth of about 660 km, which suggests the possibility of using the SM-3KV-cor sensor also to analyze the features of the phase transition zone.

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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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