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An Experimental Study on Thermal State Monitoring for Permafrost Roadbed of Qinghai-Tibet Railway Using DTS

机译:DTS监测青藏铁路多年冻土路基温度状态的试验研究

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The free water content in frozen soil is greatly influenced by its thermal state. Once the ice in frozen soil starts to thaw out, the soil structure will be loosed and its strength will greatly decrease. A distributed temperature sensing (DTS) system is suggested to monitor the thermal state of permafrost roadbed of Qinghai-Tibet railway in order to prevent the non-homogeneous thaw settlement of permafrost roadbed in this paper. An experimental study using DTS based on Raman optic time domain reflectometry (RODTR) was carried out to investigate the application feasibility of DTS for thermal state monitoring for permafrost roadbed. The experimental results indicate that the distributed temperature field of frozen soil along the optical fiber can be easily monitored in real time between the temperature of -24.6℃ and 27.2℃, and the temperature rising event along the cable can be clearly distinguished by DTS. It is expected that DTS based on ROTDR has great potential in thermal state monitoring for permafrost roadbed of Qinghai-Tibet Railway.
机译:冻土中的自由水含量受其热态的影响很大。一旦冰冻的土壤中的冰开始融化,土壤结构就会松弛,强度会大大降低。为了防止多年冻土路基的非均匀融化沉降,建议采用分布式温度传感(DTS)系统监测青藏铁路多年冻土路基的热状态。进行了基于拉曼光学时域反射仪(RODTR)的DTS实验研究,以研究DTS在多年冻土路基热状态监测中的应用可行性。实验结果表明,在-24.6℃和27.2℃之间的温度范围内,可以方便地实时监测沿光纤的冻土分布温度场,并且通过DTS可以清楚地识别沿电缆的温度升高事件。预计基于ROTDR的DTS在青藏铁路多年冻土路基热状态监测中具有巨大的潜力。

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