Measuring thermal conductivity of frozen soil using fiber optic sensors

Bing Wu, Hong-hu Zhu, Cao Dingfeng
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引用次数: 2

Abstract

The thermal conductivity is crucial for determining heat transfer in frozen soil. However, it is a challenge to obtain accurate measurement values due to the instability of soil properties. Recently, the fiber optic sensing technologies has enabled accurate and distributed in-situ monitoring of a variety of geotechnical parameters. This paper aims to explore the feasibility of actively heated fiber Bragg grating (AH-FBG) method in measuring thermal conductivity of frozen soil. A series of laboratory experiments were performed on frozen soil samples at different initial temperatures from −16 to 5 ℃. The theoretical upper and lower limits of thermal conductivity were used to evaluate the AHFBG measurements. The thermal conductivity recorded by a heat transfer analyzer was used to identify the measurement accuracy. The experimental results that the AH-FBG method can accurately measure the thermal conductivity of frozen soil when the initial temperature is below −6 ℃, and the measurement error is within acceptable range of 0.8%. When the soil temperature is between −6 and 0 ℃, significant measurement errors were observed due to the disturbance of heating to the frozen soil.
利用光纤传感器测量冻土热导率
导热系数是决定冻土传热的关键。然而,由于土壤性质的不稳定性,获得准确的测量值是一个挑战。近年来,光纤传感技术已经能够对各种岩土参数进行精确和分布式的原位监测。本文旨在探讨主动加热光纤布拉格光栅(AH-FBG)测量冻土导热系数的可行性。在- 16 ~ 5℃不同初始温度条件下,对冻土样品进行了一系列室内实验。热导率的理论上限和下限被用来评价AHFBG测量结果。用传热分析仪记录的热导率来确定测量精度。实验结果表明,AH-FBG法在初始温度低于- 6℃时能够准确测量冻土的导热系数,测量误差在0.8%的可接受范围内。当土壤温度在- 6 ~ 0℃之间时,由于加热对冻土的扰动,测量误差较大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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