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A Broadband Accelerometer for Studying High Frequency Noise Produced by the Earth

机译:用于研究地球产生的高频噪声的宽带加速度计

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This article considers a physical and mathematical model of an accelerometer for recording ultrasmall surface vibrations (10-10-10-11 m) in the frequency range of tens of hertz that operates on the basis of the S-mode of bending vibrations. The simulation results made it possible not only to compare the basic design characteristics with the experimental parameters of the available prototype of the accelerometer but also to study the change in the properties of the accelerometer with changing mechanical and electrical parameters of the structure. The ability to turn on a sequential series of bimorphic elements makes it possible to increase the sensitivity at the converter output to 10 V s2/m in the working frequency band of 10-100 Hz, which is more than an order of magnitude higher than the sensitivity of the currently available broadband systems based on piezoceramic transducers. The resonance frequency of the accelerometer is 520 Hz, while the transverse sensitivity is 1% or less. The methodology and features of the experimental recording of seismic noise by an accelerometer at the Nachiki seismic station in Kamchatka are described. The efficiency of using the registration system for observing tidal effects in seismic noise is shown.
机译:本文考虑加速度计的物理和数学模型,用于在弯曲振动的S-模式下操作数十赫兹的频率范围内记录超大表面振动(10-10-10-11 m)。模拟结果使得不仅可以将基本设计特性与加速度计的可用原型的实验参数进行比较,而且还可以研究加速度计的性能变化,改变结构的机械和电气参数。打开连续系列的黑芯元素的能力使得可以在10-100Hz的工作频带中增加转换器输出到10V S2 / M的灵敏度,这比大于高于的数量级基于压电陶瓷传感器的目前可用宽带系统的敏感性。加速度计的共振频率为520Hz,而横向灵敏度为1%或更少。描述了Kamchatka中Nachiki地震站的加速度计的地震噪声实验记录的方法和特征。示出了使用用于观察地震噪声中潮汐效应的使用注册系统的效率。

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