独山子台跨断层垂直形变观测资料干扰消除研究

doi:10.11867/j.issn.1001-8166.2009.05.0523

地球科学进展 ›› 2009, Vol. 24 ›› Issue (5): 523 -531. doi: 10.11867/j.issn.1001-8166.2009.05.0523

刘冠中 ¹,王建军 ¹,王在华 ²,蒋靖祥 ²,谢周敏 ¹,李秦 ³

1.中国地震局地壳应力研究所，北京 100085; 2. 新疆维吾尔自治区地震局，新疆乌鲁木齐 830011;
3.新疆维吾尔自治区气象信息中心，新疆乌鲁木齐 830002

收稿日期:2008-09-01 修回日期:2009-03-19 出版日期:2009-05-10
通讯作者: 刘冠中 E-mail:bjyanjiu@163.com
基金资助:
中国地震局地壳应力研究所基本科研业务费专项“新疆跨断层形变观测资料与地震活动的关系研究”（编号：ZDJ2007-31）资助.

Research on Interference Elimination for Vertical Deformation Data at Dushanzi Station in Xinjiang

Liu Guanzhong ¹,Wang Jianjun ¹,Wang Zaihua ²,Jiang Jingxiang ²,Xie Zhoumin ¹,Li Qin ³

1. Institute of Crustal Dynamics, China Seismological Bureau, Beijing 100085,China;
2. Seismological Bureau of Xinjiang Uygur Autonomous Region, Urumqi 830011, China;
3. Meteorological Information Center of Xinjiang Uygur Autonomous Region, Urumqi 830002,China

Received:2008-09-01 Revised:2009-03-19 Online:2009-05-10 Published:2009-05-10
Contact: LIU Guan-Zhong E-mail:bjyanjiu@163.com

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结合多参考自适应噪声对消和小波模极大值去噪理论，研究了新疆独山子台跨断层垂直形变观测数据的干扰因素及消除方法，结果表明：利用气象温度数据和断层两盘温差数据作为两个噪声参考输入进行自适应噪声对消，可有效消除信号中的年周期变化;利用小波模极大值去噪方法，可以抑制信号中的高频白噪声成分，使信号畸变更加明显。仿真结果及实际应用均验证了此方法的有效性与实用性，消除干扰后的垂直形变数据与台站100 km范围内4级以上地震有较好的对应性，反映了独山子台对周边地区4级以上地震的映震能力。

关键词: 断层形变, 干扰消除, 独山子, 自适应噪声对消, 模极大值

Based on the theory of multiple-reference adaptive noise cancellation and wavelet transform modulus maxima, this paper studied the method of interference cancellation for vertical deformation data from Dushanzi. The results indicate that: The annual variation in vertical deformation data is produced by seasonal variety of near-surface temperature and the temperature difference between fault′s hanging wall and foot wall, and the data is also influenced by white noise and other random noise. By using the data of meteorological temperature and auxiliary temperature to carry out adaptive noise cancellation, we can eliminate the effect of annual variation. Furthermore, by means of wavelet transform modulus maxima denoising on the data which has been ruled out the effect of annual variation, the white noise is inhibited, and the signal′s distortion is clearer and more accurate. Simulation testing and practical application demonstrate the denoise effect of the said method is effective and practical. The vertical deformation data that eliminated the effect of interference is found in good correspondence to the earthquakes of M_s≥4 within the radius of 100km from the station, and that reflects the station′s ability to response earthquake of M_s≥4 for surrounding area.

Key words: Fault deformation, Interference elimination, Dushanzi, Adaptive noise cancellation, Modulus maxima.

中图分类号:

P542

[1] Wang Jianjun.Technique study of across-fault deformation measurement and its application[J].Chinese Journal of Rock Mechanics and Engineering，2004，23（2）：261-266.［王建军．跨断层形变自动化观测技术的研究与应用[J].岩石力学与工程学报，2004，23(2)：261-266.］
[2] Gao Fuwang，Li li，Niu Anfu，et al．Study on the identification and elimination of the disturbance in crustal strain record[J].Earthquake，2004，24：91-97.［高福旺，李丽，牛安福,等.对体应变干扰因素的识别及排除［J］.地震，2004，24：91-97.］
[3] Zhang Wenlai，Luo Hongjiang，Su Ping．The interferential analysis on air pressure change toward observational daily change curve of SS-Y tensometer［J］．Inland Earthquake，2006，20(3)：266-270.[张文来，罗宏江，苏萍．气压变化对SS-Y伸缩仪观测日变曲线的干扰分析［J］．内陆地震，2006，20(3)：266-270.]
[4] Liu Shijin，Yang Guang，Li Xuechuan．Interfering recognization in the digitize data of deformation observation in Guza seismic station［J］．Earthquake Research in Sichuan，2007，123：31-35.［刘仕锦，阳光，李学川．姑咱地震台数字化形变观测资料干扰识别［J］．四川地震，2007，123：31-35.]
[5] Li Jie．Analysis of main interference of leveling survey in Gaoya,Shandong［J］．Earthquake Research in Shanxi，1998，92：47-50.［李杰．山东高崖水准主要干扰的分析［J］．山西地震，1998，92：47-50.］
[6] Zhao Shuping，Zhang Zhaodong．A study on the elimination of interference in the observed data of pressure solution differential stress at Taianstation,Shandong province［J］．North China Earthquake Sciences, 1996，14(1)：47-50.［赵淑平，张昭栋．山东省泰安台压容差应变观测排除干扰研究［J］．华北地震科学,1996，14(1)：47-50.］
[7] Bo Wanju．Development and Application of the eliminating interference method by Frequency-band division［J］．Earthquake Research in Shanxi，1993，74：24-29.［薄万举．分频段排除干扰方法的建立与应用［J］．山西地震，1993，74：24-29.］
[8] Zhu Xiaofang，Chen Yaguang．Application of noise cancellation in signal processing system［J］．Modern Electronics Technique，2006，24：86-88.［朱小芳，陈亚光．噪声对消在信号处理系统中的应用［J］．现代电子技术，2006，24：86-88.］
[9] Liu Guanzhong，Jiang Jingxiang，Wang Jianjun，et al．“Rate cumulative analysis” on across-fault fixed deformation data and preliminary anomaly extraction method［J］．Inland Earthquake，2007，21(3)：230-237.［刘冠中，蒋靖祥，王建军,等．跨断层定点形变观测资料“速率累加分析”及其异常初步提取方法［J］．内陆地震，2007，21(3)：230-237.］
[10] Jiao Qing，Zhang Hongxu，Song Guangfu，et al．A preliminary study on the cross-fault displacement variation at Dushanzi station in Xinjiang,China,before the M7.8 earthquake in Pakistan［J］．Earthquake，2007，27(1)：77-84.［焦青，张鸿旭，宋光甫,等．巴基斯坦7.8级地震前新疆独山子台跨断层位移变化初析［J］．地震，2007，27(1)：77-84.］
[11] Jing Yan，Zhang Shizhong，Li Hong, et al．Response of vertical deformation on faults to remote strong earthquakes［J］.Acta Seismologica Sinica，2007，29(2)：165-172.［荆燕，张世中，李宏,等．断层垂直形变对强远震的响应［J］．地震学报，2007，29(2)：165-172.］
[12] Zhang Yiguang，Zhang Ruiyun．The annual variation rule of the data observed by type DSJ fault-crossing levellers in Xinjiang［J］．Inland Earthquake，1998，12(2)：142-146.［张毅光，张瑞云．新疆DSJ型水平断层活动测量仪年变规律的研究［J］．内陆地震，1998，12(2)：142-146.］
[13] Wang Zaihua，Kong Defeng，Song Guangfu．Relative analysis between fault deformation observational datum and auxiliary temperature observational datum［J］．Inland Earthquake，2005，19(2)：188-191.［王在华，孔德峰，宋光甫．断层形变测量资料与辅助温度观测资料相关分析［J］．内陆地震，2005，19(2):188-191]
[14] Li Jie，Liu Xiqiang，Li Hong，et al．Analyses on normal background characteristics about deformation observation data on the basis of wavelet transform method［J］．Acta Seismologica Sinica，2005，27(1)：33-41.［李杰,刘希强，李红,等．利用小波变换方法分析形变观测资料的正常背景变化特征［J］．地震学报，2005，27(1)：33-41.］
[15] He Zhenya．Adaptive Signal Processing［M］.Beijing：Science Press, 2002:247-249.［何振亚．自适应信号处理［M］．北京：科学出版社，2002:247-249.］
[16] Simon Haykin．Adaptive Filter Theory Fourth Edition［M］.Zheng Baoyu, translated．Beijing：Publishing House of Electronics Industry，2003:185-202.［Simon Haykin. 自适应滤波器原理［M］．郑宝玉译．北京：电子工业出版社，2003:185-202.］
[17] Mallat S，Hwang W L．Singularity detection and processing with wavelets［J］．IEEE Transactions on Information Theory，1992，38(2)：617-643.］
[18] Meng Qinghua，Zhao Wenli．Study on signal denoising of modulus maximum based on optimal wavelet package decomposition[J].Chinese Journal of Sensors and Actuators，2006，19(6)：2 582-2 584.[孟庆华，赵文礼．基于最优小波包基的模极大值法信号消噪研究［J］．传感技术学报，2006，19(6)：2 582-2 584.］
[19] Fan Jichang，Liu Mingjun，Wang Fuyun，et al. Analysis on maximum wavelet decomposition level from theory and application[J].Review Science & Technology，2008，26(10)：40-42.[樊计昌，刘明军，王夫运,等.浅析小波最大分解层[J]．科技导报，2008,26(10): 40-42.]
[20] Dimitris G Manolakis,Vinay K Ingle,Stephen M Kogon．Statistical and Adaptive Signal Processing[M].Zhou Zheng，et al. translated.Beijing：Publishing House of Electronics Industry，2003:499-521.[Dimitris G Manolakis, Vinay k Ingle, Stephen M Kogon.统计与自适应信号处理[M].周正等译．北京：电子工业出版社，2003:499-521.]

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