|Table of Contents|

Co-seismic Response Characteristics of Water Level in Well Tangshan of Hebei, China Based on EEMD(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2024年第02期
Page:
252-268
Research Field:
应用地球物理
Publishing date:

Info

Title:
Co-seismic Response Characteristics of Water Level in Well Tangshan of Hebei, China Based on EEMD
Author(s):
XU Ying-xia1 DING Jun-ke2 MA Chuan-bi23GUO Jian-fang3 YIN Bao-jun4 CAO Chong2 ZUO Wen-zhe5
(1. Department of Earth Science and Engineering, Shanxi Institute of Technology, Yangquan 045000,Shanxi, China; 2. School of Emergency Management and Safety Engineering, North China University of Science and Technology,Tangshan 063210, Hebei, China; 3. Tangshan SeismicMonitoring CenterStation, Hebei EarthquakeAgency, Tangshan 063003, Hebei, China; 4. Tangshan EmergencyManagement,Tangshan 063099, Hebei, China; 5. College of Mining Engineering, North China University of Science and Technology,Tangshan 063210, Hebei, China)
Keywords:
co-seismic response well Tangshan EEMD second valueof observation data natural frequency seismic orientation fracture orientation seismic energy density
PACS:
P315
DOI:
10.19814/j.jese.2023.11002
Abstract:
Ensemble empirical mode decomposition(EEMD)can objectively and truly extract useful information from nonlinear and non-stationary signals, and the waveform signal characterized by water level in seismic observation well is also a typical nonlinear and non-stationary signal, so that EEMD has important application potential in obtaining the co-seismic response information ofwell water level. Taking well Tangshanin Hebei as an example, the advantages and disadvantages of EEMD for well water level analysis and processing through its co-seismic response of multiple well water levels from 2016 to 2023 were analyzed, the co-seismic response characteristics of well Tangshan were identified to teleseismic and near-seismic well water levels, and the seismic recording ability of well Tangshan was inferred by using the empirical formula of seismic energy density. The results show that after EEMD processing, the reconstruction of appropriate high-frequency components can suppress noise interference, which is more conducive to observing the co-seismic response characteristics of well water level. The oscillating co-seismic response caused by far-field large earthquakes can be identified and extracted objectively and truly. For the study of step-varying co-seismic response caused by near-field earthquakes, it is necessary to combine the original data to identify through high-frequency components. The second valueof well water levelobservation data is more conducive to revealing the change of regional stress field. Due to the improvement of the recording accuracy of second valueofobservation data, the earthquake with energy density of 1.77×10-7 J?m-3could be record by water level of well Tangshan. The sensitivity of observation wells to earthquakesin different orientations can be used to study the orientation ofthefracture in which they are located. For far-field earthquakes over a certain distance, the co-seismic response frequency ofwellwater level recorded by the well-aquifer system can calculate the natural vibration frequency of observation well within a certain range, and the natural vibration frequency of well Tangshan is close to the seismic Rayleigh wave.

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Last Update: 2024-04-10