Accurately determining the freezing state and non-closure distances of artificial frozen walls is crucial for evaluating their development effectiveness. However, under complex field conditions, traditional thermometer hole monitoring methods have limitations such as a limited number and fixed positions, leading to difficulties in detection or inaccurate results. This study conducted laboratory bidirectional freezing tests, integrating temperature and water content monitoring with NM-4A non-metallic ultrasonic testing technology to systematically analyze the evolutionary patterns of ultrasonic time-frequency parameters during the freezing process of loess with different water contents. The results show that phased sharp increases in P-wave velocity (Vp) and head wave amplitude (Ah), the transition of the frequency spectrum from multi-peak to single-peak, and abrupt changes in centroid frequency (fc) and kurtosis of the frequency spectrum (KFS) can serve as key criteria for judging frozen wall closure. Dynamic changes in the reflection coefficient (rI), transmission coefficients (tP, tI), and acoustic impedance field are the main mechanisms affecting ultrasonic propagation characteristics. Based on ray acoustics theory, a prediction equation for non-closure distances was established. Validation demonstrated high accuracy, with error ranges of 0.001–6.293 mm for laboratory tests and the accuracy range is 76.82% ∼ 91.56% for field measurements. Incorporating the four parameters (Vp, Ah, fc, KFS) into radar charts enables qualitative evaluation of the frozen wall closure state. The ultrasonic testing method formed by combining this qualitative evaluation with the prediction equation provides an efficient and reliable technical means for judging the closure and quantifying the non-closure distance of bidirectionally frozen loess walls.
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