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首页> 外文期刊>Geophysical Research Letters >Strong-Motion Seismogeodesy by Deeply Coupling GNSS Receivers with Inertial Measurement Units
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Strong-Motion Seismogeodesy by Deeply Coupling GNSS Receivers with Inertial Measurement Units

机译:通过具有惯性测量单元的GNSS接收器深度耦合GNSS接收器的强运动地震

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摘要

Global navigation satellite system (GNSS) displacements at near-source stations can be biased in both amplitude and phase due to fierce earthquake strike. We propose to inject inertial measurement unit (IMU)-recorded ground motions into GNSS receivers to compensate their phase-lock loops (PLLs) for seismic motion stress, aiming at keeping steady carrier-phase tracking. We use a shake table to replay an acceleration record (0.5-2.0 g) from the 2008 Mw7.9 Wenchuan earthquake to test this IMU-augmented PLL: It achieves a 1.9-mm amplitude error (RMS) and an 8.0-ms phase lag against the shake table's recordings, while the conventional PLL languishes to 6.0 mm and 56.5 ms, respectively. Moreover, the IMU-augmented PLL enables a six-degree-of-freedom integration among the GNSS and IMU data, where the displacement amplitude error and phase lag decline further to 0.9 mm and 3.5 ms, respectively. We believe that the IMU-augmented GNSS receivers are ideal strong-motion seismograph to capture trustworthy broadband displacements in the near fields.
机译:近源站的全球导航卫星系统(GNSS)位移可以在激烈的地震撞击引起的幅度和相位中偏置。我们建议注入惯性测量单元(IMU)-recorded地面运动到GNSS接收器用于震动应力补偿他们的锁相回路(PLL),旨在保持稳定的载波相位跟踪。我们使用摇桌重放2008 MW7.9汶川地震的加速度记录(0.5-2.0g)来测试该IMU增强的PLL:它达到了1.9毫米幅度误差(RMS)和8.0-MS阶段滞后针对摇动台的录音,而传统的PLL分别萎缩至6.0毫米和56.5毫秒。此外,IMU - 增强的PLL能够在GNSS和IMU数据之间实现六程度自由的集成,其中位移幅度误差和相位滞后分别进一步下降至0.9mm和3.5ms。我们认为,IMU - 增强的GNSS接收器是理想的强运动地震仪,以捕捉在近场的可信赖的宽带位移。

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