[1]番绍辉,王光明,刘克骧,等.龙陵邦腊掌测震台数据质量及背景噪声分析[J].华南地震,2026,46(06):147-153.[doi:10.13512/j.hndz.2026.06.14]
 FAN Shaohui,WANG Guangming,LIU Kexiang,et al.Data Quality and Background Noise Analysis of Longling Banglazhang Seismic Station[J].,2026,46(06):147-153.[doi:10.13512/j.hndz.2026.06.14]
点击复制

龙陵邦腊掌测震台数据质量及背景噪声分析()

华南地震[ISSN:1006-6977/CN:61-1281/TN]

卷:
46
期数:
2026年06期
页码:
147-153
栏目:
地震科学研究
出版日期:
2026-10-23

文章信息/Info

Title:
Data Quality and Background Noise Analysis of Longling Banglazhang Seismic Station
文章编号:
1001-8662(2026)06-0147-07
作者:
番绍辉; 王光明; 刘克骧; 马志刚; 杨铭昌
云南省地震局,昆明 650051
Author(s):
FAN Shaohui; WANG Guangming; LIU Kexiang; MA Zhigang; YANG Mingchang
Yunnan Earthquake Agency, Kunming 650051, China
关键词:
邦腊掌地震台; 数据质量; 背景噪声; 功率谱密度; 异常信号
Keywords:
Banglazhang Seismic Station;  Data quality;  Background noise;  Power spectral density;  Abnormal signal intensity
分类号:
P315
DOI:
10.13512/j.hndz.2026.06.14
文献标志码:
A
摘要:
基于龙陵新建邦腊掌测震台2024年2月—2025年12月的连续地震波形数据,采用噪声功率谱密度(PSD)、概率密度函数(PDF)和1~20Hz频段噪声均方根RMS值计算方法,分析其数据质量、背景噪声变化特征及噪声异常原因。结果表明:1Hz以上高频段噪声无显著日变化,人类活动干扰较弱,但其受附近小溪湍急水流、泥沙及河床相互作用产生的持续高频噪声干扰显著;0.05~0.5Hz微震频段仅观测到0.1~0.5Hz频段的次级微震频段噪声峰值,该频段呈现显著的季节性变化特征,秋冬季噪声水平较春夏季高2~3dB,且秋冬季噪声峰值出现频率低于春夏季;0.05Hz以下长周期频段无显著季节性变化,但水平向的噪声水平较垂直分量大,表明水平分量更易受温度扰动和大气压变化的影响。邦腊掌测震台背景噪声异常源于地震计脉冲标定、施工干扰,仪器故障及地震信号等。本研究成果为台站堪选、背景噪声水平与数据质量评估及异常信号识别提供重要参考依据。
Abstract:
Based on the continuous seismic waveform data from February 2024 to December 2025 at the newly-built Banglazhang Seismic Station in Longling, the data quality, background noise variation characteristics and noise anomaly causes were analyzed by using noise power spectral density(PSD), probability density function(PDF) and noise root mean square (RMS) value calculation method in 1-20 Hz frequency band. The results show that there is no significant diurnal variation of high-frequency noise above 1 Hz, and the interference of human activities is weak, but it is significantly disturbed by the continuous high-frequency noise generated by turbid current, sediment and riverbed interations of the nearby stream. In the 0.05-0.5 Hz microseismic frequency band, only the peak noise of the secondary microseismic frequency band in the 0.1-0.5 Hz frequency band is observed, which shows signifi‐cant seasonal variation characteristics. The noise level in autumn and winter is 2-3 dB higher than that in spring and summer, and the frequency of peak noise in autumn and winter is lower than that in spring and summer. There is no significant seasonal variation in the long-period frequency band below 0.05 Hz, but the horizontal noise level is larger than the vertical component, indicating that the horizontal component is more susceptible to temperature dis‐turbance and atmospheric pressure change. The background noise anomaly of Banglazhang Seismic Station is de‐rived from seismometer pulse calibration, construction interference, instrument failure and seismic signal. The re‐search results provide an important reference for station site selection, background noise level and data quality as‐sessment, and abnormal signal recognition.

参考文献/References:

[1]立凯,陈浩,张朋,等.江苏省测震台网背景噪声特征[J].华北地震科学,2021,39(3):66-71+76.
[2]唐浩,徐金银,何秋菊,等.宁夏区域地震观测背景噪声特征[J].大地测量与地球动力学,2024,44(11):1199-1206.
[3] McNamara D E, Buland R P. Ambient noise levels in the Continental United States[J]. Bulletin of the Seismological Society of America, 2004, 94(4): 1517-1527.
[4] Peterson J. Observations and modeling of seismic background noise[J]. USGS Open File Report, 1993, 18(12): 93-322.
[5]吴丽慧,廖武林,黎金玲,等.黄石市地震台背景噪声特征分析[J].地震工程学报,2025,47(1):152-159.
[6]谢江涛,林丽萍,赵敏,等.四川地区地震背景噪声特征分析[J].地震学报,2021,43(5):533-550.
[7]陈阳,侍田宏,朱涛,等.利用背景噪声功率谱曲线变化判断备选台站台基质量[J].华南地震,2025,45(3):35-41.
[8]立凯,瞿旻,秦磊,等.连云港地震台台基噪声与干扰源分析[J].地震地磁观测与研究,2022,43(3):60-64.
[9]陈家樑,巫立华,戴丽金,等.福建测震台网数据质量监管与评估[J].华南地震,2025,45(2):24-30.
[10]李凤英,张天继,李文涛,等.基于噪声水平分析的云南地震台网数据质量评估[J]. 地震研究,2026,49(2):214-223.
[11]游秀珍,林彬华,李军,等.福建地震预警台网观测数据质量评估[J].地球物理学进展,2024,39(4):1330-1342.
[12]安全,韩晓明,包文超,等.内蒙古地区强震动台站背景噪声与数据质量分析[J]. 地震学报,2024,46(3):490-501.
[13]林彬华,金星,廖诗荣,等.地震噪声异常实时监测[J].中国地震,2015,31(2):281-289.
[14] GB/T 19531.3—2004 地震台站观测环境技术要求[S].
[15]谢江涛,林丽萍,谌亮.九寨沟MS7.0地震应急流动台站噪声水平分析[J].大地测量与地球动力学,2020,40(9):962-969.
[16] Burtin A, Bollinger L, Vergne J, et al. Spectral analysis of seismic noise induced by rivers: A new tool to monitor spatiotemporal changes in stream hydrodynamics[J]. Journal of Geophysical Research: Solid Earth, 2008, 113(B5):B05301.
[17]王芳,王伟涛,龙剑锋,等.中国大陆地区宽频带地震台网台基噪声特征[J].地震学报,2019,41(5):569-584.
[18]包文超,赵铁锁,申影,等.内蒙古地震预警台站异常数据检测与分析[J].高原地震,2023,35(2):50-55.
[19]安全,赵艳红,苏日亚,等.内蒙古区域背景噪声特征分析[J].华北地震科学,2021,39(1):89-96.
[20] Wolin E, Van der Lee S, Bollmann T A, et al. Seasonal and diurnal variations in long-period noise at SPREE Stations:The Influence of soil characteristics on Shallow Stations’ performance[J]. Bulletin of the Seismological Society of America, 2015, 105(5): 2433-2452.
[21]葛洪魁,陈海潮,欧阳飚,等.流动地震观测背景噪声的台基响应[J].地球物理学报,2013,56(3):857-868.
[22] Evangelidis C P, Melis N S. Ambient noise levels in Greece as recorded at the Hellenic Unified Seismic Network[J]. Bulletin of the Seismological Society of America, 2012, 102 (6): 2507-2517.
[23]巫立华,张宝剑,黄鹤凌,等.福建地区地震背景噪声特征分析[J].华南地震,2026,46(1):9-17.
[24]荆涛,孙艺,崔政东.辽宁地区低频背景噪声特征分析及模型建立[J].华南地震,2023,43(1):61-69.
[25] Demuth A, Ottem?ller L, Keers H. Ambient noise levels and detection threshold in Norway[J]. Journal of Seismology, 2016, 20(3): 889–904.
[26]杨千里,郝春月,田鑫.新疆和田台阵PSD与PDF分析[J].地球物理学报,2019,62(7):2591-2606.
[27] Marzorati S, Bindi D. Ambient noise levels in north central Italy[J]. Geochemistry, Geophysics, Geosystems, 2006, 7 (9): 1-14.

相似文献/References:

[1]陈家樑,巫立华,戴丽金,等.福建测震台网数据质量监管与评估[J].华南地震,2025,(02):24.[doi:10.13512/j.hndz.2025.02.04]
 CHEN Jialiang,WU Lihua,DAI Lijin,et al.Seismic Data Quality Management and Evaluation of Fujian Seismic Monitoring Network[J].,2025,(06):24.[doi:10.13512/j.hndz.2025.02.04]

备注/Memo

备注/Memo:
收稿日期:2026-01-23
基金项目:云南省地震局青年地震科学基金资助项目(2025K04);云南省地震局创新团队(CXTD202508);腾冲深部构造活动云南省野外科学观测研究站项目联合资助。
作者简介:番绍辉(1993-),男,工程师,主要从事地震监测与研究。E-mail: 250336803@qq.com
通信作者:王光明(1990-),男,高级工程师,主要从事地震研究等工作。E-mail: 609979407@qq.com
更新日期/Last Update: 2026-10-21