基于OFDR技术的土体含水率模型研究

    STUDY ON THE SOIL WATER CONTENT MODEL BASED ON OFDR TECHNOLOGY

    • 摘要: 土体含水率是影响土体工程性质的重要因素,因此对土体含水率进行测定具有重要的工程意义。本文采用主动加热光纤法,通过光频域反射(OFDR)技术进行土体含水率测定试验,以最大升温值法(ΔTmax)标定土体含水率,得到土体含水率与光纤温度特征值之间的函数模型,并基于试验结果建立了土体光纤温度特征值随土体含水率、电加热功率和加热时间变化的BP神经网络预测模型。研究结果表明:基于试验结果得到的4个含水率函数模型,在电加热功率越大且加热时间越长条件下,函数模型拟合效果较好;借助含水率函数模型,可通过土体光纤温度特征值得到土体含水率预测值,但是函数模型预测精度有限;而本文建立的土体含水率神经网络预测模型具有较高的预测精度,对土体含水率预测的平均相对误差仅为0.18%。结果表明,土体含水率神经网络预测模型相对于土体含水率函数模型精度更高且稳定性更好。

       

      Abstract: Soil water content is an important factor affecting the engineering properties of soil. It is of great engineering significance to measure soil water content. In this paper, the active heating optical fiber method is used to measure the soil water content through optical frequency domain reflection(OFDR)technology. The maximum temperature rise value method(ΔTmax) is used to calibrate the soil water content. The functional model between soil water content and the optical fiber temperature characteristic value is obtained. Based on the test results, the BP neural network prediction model of the soil fiber temperature characteristic value changing with soil water content, electric heating power, and heating time is established. The results show that the four soil water content function models were found to have better fitting performance under the conditions of higher electric heating power and longer heating time based on the experimental results. With the help of the soil water content function model, the predicted value of soil water content can be obtained through the temperature characteristics of fiber for soil; however, the prediction accuracy of the function model is limited. The neural network prediction model of soil water content established in this paper has high prediction accuracy, and the average relative error of soil water content prediction is only 0.18%.The results show that the neural network prediction model of soil water content has higher accuracy and better stability than the soil water content function model.

       

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