ISSN 1000-3665 CN 11-2202/P

    基于FBG技术的土体含水率测量方法试验

    A study of soil moisture content measurement based on FBG technology

    • 摘要: 亲水橡胶是一种水敏性高分子聚合物,具有吸水膨胀、失水收缩的特性,同时其弹性、强度和持水能力保持不变。通过胶黏封装方法,将亲水橡胶与光纤耦合,利用FBG光纤传感技术,精确测量由于亲水橡胶吸水膨胀、失水收缩导致的光纤拉伸和压缩形变,当橡胶与土体含水率达到动态平衡时,可以通过测量光纤形变得到土体含水率。通过试验验证了亲水橡胶体变与其含水率之间的线性相关性,且在反复试验中亲水橡胶吸水、失水的能力基本保持不变,表明亲水橡胶可以作为含水率感测的换能材料;建立了FBG传感器中心波长与亲水橡胶含水率之间的对应关系;通过对黏土含水率的测试,发现该含水率传感器的FBG中心波长与黏土试样含水率呈分段线性关系,表明利用该传感器监测土体含水率的方法具有可行性,不仅可以实现含水率的原位监测,而且还能得到含水率的空间分布及其随时间的实时变化情况,为土体工程性质的评价、地质灾害的预测预报提供依据,具有广泛的应用前景。

       

      Abstract: Hydrophilic rubber is a sort of water-sensitive polymers. It is characterized by water swelling and shrinkage, while its elasticity, strength and water holding capacity remain unchanged. In this paper, hydrophilic rubber is coupled with the fiber with the adhesive packaging method. FBG (fiber Bragg grating) sensing technology is used to accurately measure the fiber tensile and compressive deformation, which are caused by water swelling and shrinkage. When the moisture content of rubber and the moisture content of soil are in a dynamic equilibrium, soil moisture content can be obtained by measuring the deformation. Firstly, the linear correlation between the hydrophilic rubber volume and its moisture content is verified by experiments. The ability of water swelling and shrinkage for hydrophilic rubber in repeated tests still remains unchanged, indicating that the hydrophilic rubber can be used as the energy exchange material for moisture content sensing. Then we establish the corresponding relationship between the central wavelength of FBG sensor and the moisture content of hydrophilic rubber. Finally, this moisture sensor is used to test the moisture content of clay. The piecewise linear relationship between the central wavelength of FBG sensor and the moisture content of clay sample shows that this moisture sensor has the feasibility of monitoring the soil moisture content. Not only can the sensor realize the in situ monitoring of moisture content, but also can get the spatial distribution of moisture content and its real-time changes. It can provide the basis for the evaluation of the engineering properties of soil and the prediction of geological hazard, which has wide application prospect.

       

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