远程浅层爆破震源的微震信号频谱能量消散衰减规律研究OA
Attenuation Laws of Spectral Energy Dissipation in Microseismic Signals from Remote Shallow Blasting Sources
基于江西省地震局赣州地震监测中心站测震台网监测数据,通过对赣州铁山垅钨矿不同位置、不同炸药量的爆破进行多方位、远距离实时监测,得到爆破振动微震信号,对数据进行识别与分析处理得到中远爆区爆破振动信号的传播规律.针对爆破振动信号受复杂环境条件的影响,采用Butterworth滤波器消除趋势分量,结合小波去噪、HHT去噪两者优势进行去噪,分析同一爆破不同监测基站与同一监测基站不同爆破下的时频特性、频带能量特性、地表环境对微震信号频谱能量传播的影响.研究表明,萨道夫斯基经验公式仍适用于爆破振动信号在32~120 km中远爆区的传播规律,其中:1)在中远爆区,信号能量在低频带高度集中,并随爆心距(R)的增大频带下移;2)当爆心距固定时,信号能量随炸药量(Q)增大显著增大,能量集中频带波动处于正常范围;3)爆破振动信号的衰减也受传播路径上地表环境的影响.
Based on the seismic monitoring data from the Ganzhou Earthquake Monitoring Center Sta-tion of the Jiangxi Seismological Agency,real-time monitoring of blasting vibrations from different lo-cations and explosive quantities at the Ganzhou Tieshanlong Tungsten Mine was conducted from mul-tiple directions and long distances.The microseismic signals generated by blasting were obtained and analyzed to identify the propagation patterns of blasting vibration signals in medium and far blasting zones.Considering the influence of complex environmental conditions on blasting vibration signals,a Butterworth filter was used to eliminate trend components,and a combination of wavelet denoising and HHT denoising was applied to analyze the time-frequency characteristics,frequency band energy characteristics,and the impact of terrestrial environment on the spectral energy propagation of micro-seismic signals under different monitoring base stations and different blasting events.The study shows that the Sadovsky empirical formula is still applicable to the propagation patterns of blasting vibration signals in the medium and far blasting zones(32-120 km),where:1)in the medium and far blasting zones,signal energy is highly concentrated in the low-frequency band and shifts downward with in-creasing distance from the blast center(R);2)when the distance from the blast center is fixed,sig-nal energy increases significantly with the increase in explosive quantity(Q),and the concentrated frequency band fluctuates within a normal range;3)the attenuation of blasting vibration signals is al-so affected by the surface environment along the propagation path.
谢斌;续伟;肖孟仁;冯亮
赣州地震监测中心站,赣州,341000江西理工大学资源与环境工程学院,赣州,341000赣州地震监测中心站,赣州,341000江西理工大学资源与环境工程学院,赣州,341000
天文与地球科学
爆破振动时频分析能量分布地表影响
blasting vibrationtime-frequency analysisenergy distributionsurface effects
《大地测量与地球动力学》 2026 (1)
78-85,8
国家自然科学基金(4210071309)江西省自然科学基金(20224BAB203040)中国地震局"三结合"课题(3JH-202401050)江西省地震局"2111"孵化基金(FD2111-202404).
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