Interference analysis of the extensometer observation at Xuzhou seismic station
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摘要: 徐州地震台伸缩仪运行至今主要受降雨及气压干扰,分析研究了降雨及气压对伸缩仪的影响,并进行了定量分析。结果表明,EW分量降雨的响应较为灵敏;观测数据短时间大幅加速上行的主要原因是仪器传感器铁芯在差动变压传感器中未居中,偏置的传感器铁芯在差动变压传感器中的感应面积增加,使得感应电压在观测中大幅增加。Abstract: The extensometer of Xuzhou seismic station is mainly disturbed by rainfall and atmospheric pressure. The influence of rainfall and atmospheric pressure on extensometer is quantitatively analyzed. The results show that the response of EW component rainfall is more sensitive. The main reason for the rapid acceleration of observation data in a short time is that the sensor core is not centered in the differential voltage transformer sensor. The induced area of the biased sensor core in the differential voltage transformer sensor increases greatly, leading to an increase of the induced voltage in the observation.
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Key words:
- extensometer /
- typical interference /
- anomalous change /
- rainfall change
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表 1 徐州台伸缩仪潮汐因子及精度表
Table 1. Factor and precision table of telescopic instrument of Xuzhou seismic station
时间
(年-月)潮汐因子 精度 NS EW NS EW 2020-01 0.8304 0.3899 0.0018 0.0181 2020-02 0.8420 0.3268 0.0018 0.0129 2020-03 0.8417 0.3563 0.0392 0.2171 2020-04 0.8318 0.3722 0.0024 0.0135 2020-05 0.8309 0.3825 0.0034 0.0212 2020-06 0.8220 0.5484 0.0064 0.1678 2020-07 0.8404 0.2877 0.0392 0.2171 2020-08 0.8874 0.4100 0.0054 0.0188 2020-09 0.8277 0.3663 0.0326 0.1453 2020-10 0.8367 0.3347 0.0034 0.0163 2020-11 0.8353 0.3555 0.0040 0.0127 2020-12 0.8326 0.3535 0.0052 0.0124 表 2 伸缩仪降雨响应表
Table 2. Rainfall response table of telescopic instrument
日期
(年-月-日)降雨量(W)
/mm降雨持续时间
(△t)/h应变量增量/10−10 变化时间/h 降雨效率 NS(△a1) EW(△a2) NS(t1) EW(t2) NS($\eta_{1} $) EW($\eta_{2} $) 2020-01-07 33.10 24.73 439 1430 20.83 8.67 0.54 1.75 2020-02-14 23.60 12.58 − 288 − 41.56 − 0.97 2020-06-27 33 15 566 3243 32.13 39.01 1.14 6.55 2020-08-08 28.20 4.90 − 1367 − 32.00 − 9.89 2021-05-15 26.30 23.40 1016 2933 43.06 54.2 1.84 5.31 2021-06-16 61.20 29.40 1202 1962 30.40 24.48 0.67 1.09 2021-07-03 26.40 6.50 913 3626 31.87 34.93 5.32 21.13 2021-07-28 136.40 36.20 8720 4467 6.15 22.24 1.77 0.91 2021-08-02 102.50 5.58 1036 851 7.40 2.70 1.81 1.49 2021-09-04 60.90 26 1261 1342 10.00 8.20 0.80 0.85 2021-09-19 57 14 599 3836 19.00 46.20 0.75 4.81 -
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