| 研究生: |
廖勿渝 Liao, Wu-Yu |
|---|---|
| 論文名稱: |
基於深度學習和地球物理的震源監測 Integration of deep-learning and earthquake physics for seismic sources monitoring |
| 指導教授: |
李恩瑞
Lee, En-Jui |
| 學位類別: |
博士 Doctor |
| 系所名稱: |
理學院 - 地球科學系 Department of Earth Sciences |
| 論文出版年: | 2024 |
| 畢業學年度: | 113 |
| 語文別: | 英文 |
| 論文頁數: | 182 |
| 中文關鍵詞: | 地震學 、深度學習 、地震監測 |
| 外文關鍵詞: | Seismology, Deep learning, Seismic monitoring |
| 相關次數: | 點閱:121 下載:70 |
| 分享至: |
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地震波形包含了關於震源、傳遞介質及相關孕震地體構造的寶貴訊息。近年來,密集地震網的部署增強了偵測微震活動的能力,包括天然地震和地貌改變之過程,如山崩和落石。一般來說,地表震動事件之確認基於辨識單一測站記錄到的訊號並與測網內其他測站的辨識結果進行關聯性分析(association)。然而,大量收集而來的數據為手動數據處理和分析帶來了挑戰,尤其是像地震預警這樣的即時應用。開發可靠且高效率的地震監測算法對於研究孕震構造和減災至關重要。地震監測大致可以分為地震目錄編纂和地震預警。這兩者在反應時間上有所不同,取決於是否需要等待並使用地震S波的資訊。地震目錄編纂可以幫助探索微震活動及其與孕震構造的關係,其中地震S波的資訊有助於提高震源深度之解算精度。地震預警系統則僅使用地震P波到時的觀測數據發佈地震警報,在具有致災性的地震S波到達之前提供資訊給社會大眾,以減輕潛在的地震災害。當我開始攻讀博士學位時,深度學習已經成為解決地震偵測問題的主要算法之一,例如去除訊號背景噪音、挑選體波到時、事件確認的關聯性分析、規模與震度預估等。然而,地球物理的知識尚未整合到決策過程中,無法限制深度學習演算法潛在的錯誤輸出,因而使其說服力較低。我在地震監測中專注於三個方向,旨在結合深度學習與地球物理並探索其在地震學中的應用。首先,對於地震目錄編纂,我開發了一個用於挑選地震P和S波相到時的深度學習模型,並將其與基於已知速度模型解算之理論走時的反投影法(back projection)結合進行相位連結。其次,通過簡單的數據增強策略,我研究了深度學習算法在不完整地震波形(少於1到3秒)中即時辨識P波波相的方法,以用於地震預警。第三,我探索了在從單測站到多個測站的記錄中同時使用時間域與時頻域資料辨識落石事件的遷移學習(transfer learning)方法。訓練落石訊號辨識模型的問題在於落石波形的觀測和人工標記結果較少。然而,如果應用了適當的遷移學習技術,深度學習模型可以從大量標記的地震數據中學習如何解讀並辨識落石訊號。總結,深度學習應用在地震學中的發展在地震監測任務中顯示出其可靠並強大的能力。地震物理的整合可以進一步約束深度學習的輸出,並具有極大的潛力來改進常態性地震監測工作流程。
Seismic waveforms embody valuable information about seismic sources, propagation media, and source-induced structures. In recent years, the growth of dense seismic networks has enhanced the capability to detect microseismicity, including earthquakes and geomorphological processes like landslides and rockfalls. Generally, an event confirmation is based on signal identification at a single station and its association with multiple station observations. However, the massive amount of collected data poses manual data processing and analysis challenges, especially for real-time use cases such as earthquake early warning. Developing reliable and efficient algorithms for seismic monitoring is thus crucial for studying seismic-induced structures and hazard mitigation. Earthquake monitoring can be roughly separated into earthquake cataloging and earthquake early warning, which differ in reaction period and whether to wait for and utilize the S phase information. Earthquake cataloging could help explore microseismicity and its relationship with seismic-induced structures, in which the S phase information puts constraints to help solve focal depth precisely. The earthquake early warning system mitigates the potential hazard by reporting earthquake alerts with solely the observations of P arrivals preceding the most destructive S waves. When I started my Ph.D. program, deep learning emerged as one of the dominating algorithms in solving earthquake detection problems, such as signal denoising, body wave arrival-time picking, event determination, magnitude and ground motion prediction, etc. However, earthquake physics had not been integrated into the decision-making process, making it less convincing since there are no constraints for the potential error outputs from deep learning algorithms. I focused on three directions in seismic source monitoring to solve the problem and explore the utility of deep learning applications in seismology. First, for earthquake cataloging, I developed an advanced model for picking seismic P and S arrivals and integrated it with the back-projection algorithm for phase association. The back-projection algorithm sticks to the physics of theoretical travel time based on the known velocity model. Second, with a simple data augmentation strategy, I examined the deep learning algorithms' utility in identifying P arrivals with incomplete earthquake waveforms (less than 1 to 3 seconds) for earthquake early warning. Third, I explored the transfer learning method in identifying rockfall events from single to multiple-station recordings using time-series and time-frequency domain data. The problem is that the rockfall waveform is poorly observed and labeled. However, if the appropriate transfer learning technique has been applied, the deep learning model can recognize the rockfall waveform from the massively labeled earthquake data. In summary, the developments of deep learning applications in seismology hold promising results in earthquake monitoring tasks. Integrating earthquake physics could further constrain the deep learning outputs and has great potential to improve regular seismic monitoring workflow.
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