Frequency spectrum characteristic of quartz sandstone rock mass with GPR
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摘要: 經過巖土體介質反射回的地質雷達波特征攜帶了所穿透的巖土體內部的相關信息,其中地質雷達波頻譜主頻值可以作為判斷巖土體結構特征的一個定量指標.以圍巖為石英砂巖的公路隧道工程為依托,采用MALA地質雷達配100 MHz屏蔽天線,對隧道掌子面前方的石英砂巖體進行超前地質探測試驗,分析典型的Ⅴ級、Ⅳ級和Ⅲ級石英砂巖圍巖的雷達波形圖圖像特征和雷達波在巖體介質中傳播的傅里葉頻譜特征.通過分析現場試驗數據,得出巖體介質的雷達波主頻值因自身結構特征和周邊環境變化而在一定的敏感頻率區間內的規律.對比分析研究結果與工程開挖實際,表明通過分析超前地質探測獲得的雷達波傅里葉頻譜主頻值特征來反演識別圍巖結構特征是切實可行的.Abstract: Ground penetrating radar(GPR) electromagnetic waves which penetrate through rock and soil mediums and are reflected back carry internal information about the target objects. The GPR basic frequency values of Fourier spectra can be used as a quantitative index of judgment for the structure characteristic of rock and soil mediums. Based on a highway tunnel project with the surrounding rock of quartz sandstone,advanced geological exploration test was carried out in front of the tunnel face with MALA GPR and a 100 MHz shielded antenna. Typical Class Ⅴ,Class Ⅳ and Class Ⅲ quartz sandstone surrounding rock mass were chosen to analyze their waveform graph information characteristic and the Fourier spectrum frequency characteristic during electromagnetic wave propagation in rock mass mediums. The regularity of GPR wave basic frequency values corresponding to the quartz sandstone rock mass medium in a certain sensitive frequency range due to its structure and surrounding environment changes was obtained through field test data analysis. A comparison between the research results and engineering excavation practices shows that it is feasible to invert the basic frequency value characteristic of GPR waves derived from advanced geological exploration for determining the structure characteristics of surrounding rock.
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