• 沒有找到結果。

第二章 文獻回顧

5.2 建議

1. 本研究顯示在將訊號轉換至時頻譜上能明顯發現其各頻率訊號能量隨 時間變化情形,例如 P 波頻率較高,到時較早,S 波次之,頻率也相對 較低,而施測資料也可能受到水波或管波之雜訊影響,即可以在低頻處 看到大範圍之時間影響。因為有時頻譜如此清楚的變化情形,藉由時窗 函數前處理的輔助,選定適當之頻率範圍,未來也能朝向 P 波之初達到 時判釋方向邁進。

2. 本研究提出之半自動化挑波方法對於時頻譜解析度之依賴性高,雖然透 過時頻分析法的參數調整即可解決,但治根的辦法還是需要同時獲取高

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頻率與高時間解析度。故未來建議嘗試以希爾伯特-黃轉換(Hilbert Huang Transform)利用經驗模態分解(Empirical Mode Decomposition, EMD)方法將訊號分解為本質模態函數(Intrinsic Mode Functions, IMF), 然後將 IMF 作希爾伯特轉換(Hilbert Transform),正確地獲得資料的瞬 時頻率,以繪製高頻率、高時間解析度之時頻譜(Huang et al., 1998)並以 此時頻譜作為半自動化挑波方法之判釋基礎。

3. 從時間演進回顧所提出的自動化挑波方法可以發現,其自動化方法越來 越多元,並沒有一種單一方法適用所有訊號,往往結合不同面向之評判 標準或分析方法。同樣概念,未來建議本研究提出的半自動方法能結合 其他現有的挑波機制,以期達到擁有多適應性之全自動化挑波方法。

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