The principle of detecting seepage anomalies in water-retaining earthen structures through temperature monitoring has yet to gain extensive acceptance in modern field applications. As such, this study demonstrated the practical detection of seepage anomaly from fiber optic distributed temperature sensing (DTS) through physical and numerical modeling. A high-resolution DTS, capturing temperature at a sub-cm interval, was embedded in a laboratory-scale earth dam featuring normal and anomalous seepage conditions (induced by artificial defect). Then, a fluctuating reservoir thermal load was applied, and the internal temperature of the dam was monitored. Evaluation of the temperature lag time showed a quicker detection of temperature changes on the DTS sensing locations traversed by the anomalous seepage flow. The disparity in temperature lag times across the DTS increased significantly when a severe seepage anomaly was induced by systematically channeling the reservoir water directly into the artificial defect through a small tube tapping into the reservoir. Further insight into the heat-seepage interaction was achieved through coupled hydrothermal numerical modeling using COMSOL Multiphysics.
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Bekele et al. (2024) studied this question.
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