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基于人工神经网络的复杂介质中波的传播不确定性分析方法

程曦 张志勇

程曦, 张志勇. 基于人工神经网络的复杂介质中波的传播不确定性分析方法[J]. 电子与信息学报, 2021, 43(12): 3662-3670. doi: 10.11999/JEIT200755
引用本文: 程曦, 张志勇. 基于人工神经网络的复杂介质中波的传播不确定性分析方法[J]. 电子与信息学报, 2021, 43(12): 3662-3670. doi: 10.11999/JEIT200755
Xi CHENG, Zhiyong ZHANG. An Uncertainty Analysis Method of Wave Propagation in Complex Media Based on Artificial Neural Network[J]. Journal of Electronics & Information Technology, 2021, 43(12): 3662-3670. doi: 10.11999/JEIT200755
Citation: Xi CHENG, Zhiyong ZHANG. An Uncertainty Analysis Method of Wave Propagation in Complex Media Based on Artificial Neural Network[J]. Journal of Electronics & Information Technology, 2021, 43(12): 3662-3670. doi: 10.11999/JEIT200755

基于人工神经网络的复杂介质中波的传播不确定性分析方法

doi: 10.11999/JEIT200755
基金项目: 国家自然科学基金(61701427)
详细信息
    作者简介:

    程曦:女,1986年生,讲师,研究方向为计算电磁学、人工神经网络

    张志勇:男,1984年生,讲师,研究方向为计算电磁学、人工神经网络、农业信息化

    通讯作者:

    张志勇 jsjzzy@xjau.edu.cn

  • 中图分类号: TN959; O441.4

An Uncertainty Analysis Method of Wave Propagation in Complex Media Based on Artificial Neural Network

Funds: The National Natural Science Foundation of China (61701427)
  • 摘要: 土壤在物理系统的工作频率范围内可能表现出较强的色散性,色散物质的不确定参数在波传播的仿真结果中引入了不确定性。在考虑这些仿真结果的可接受性时,量化仿真结果中的不确定性至关重要。针对传统不确定性分析法计算效率低、运算量大的问题,该文以探地雷达建模仿真中的不确定性分析为例,提出一种基于人工神经网络的不确定性分析模型,阐述了模型的构建过程,及克服过拟合问题的策略。作为探地雷达全波仿真的替代模型能够预测仿真结果,进而得到仿真结果的统计信息,如均值、标准差。经比较,在相同的数值模型、不确定性输入参数个数,以及参数变化范围为10%的前提条件下,对任意一组输入参数,输出得到1000组结果时,该方法所得预测结果统计特性与执行全波仿真所得具有较好的一致性,且显著降低运算量,计算时间效率提升79.82%。
  • 图  1  ANN替代模型的训练过程与测试过程

    图  2  4种不同激活数属分别应用于ANN替代模型隐藏层后训练损失函数与验证损失函数随Epochs的变化关系(未应用DropOut方法)

    图  3  探地雷达系统及其应用场景模拟模型

    图  4  基于MCS方法的电场强度$ {E_z} $变化规律

    图  5  土壤中含有金属块以及花岗岩,输入不确定性参数个数为7且变化波动范围均为10%时,$ {R_x} $处电场强度$ {E_z} $统计特性

    图  6  土壤中含有金属块以及花岗岩,输入不确定性参数个数为7且变化波动范围均为10%时,$ {R_x} $处电场强度$ {E_z} $统计特性

    图  7  土壤中含有金属块,输入不确定性参数个数为7且变化波动范围均为10%时,$ {R_x} $处电场强度$ {E_z} $统计特性

    表  1  应用DropOut方法前后,不同激活函数作用时ANN替代模型的损失函数值

    激活函数网络是否应用
    DropOut方法
    训练数据损失
    (×10–5)
    验证数据损失
    (×10–5)
    ReLU函数0.7636.98
    3.7304.28
    LReLU函数2.7805.50
    3.7204.36
    PReLU函数0.9537.65
    3.7304.30
    ELU函数3.7404.30
    //
    下载: 导出CSV

    表  2  色散土壤模型参数

    土壤湿度(%)$ {\varepsilon _\infty } $$ {\sigma _{\text{s}}} $(mS/m)$ {A_1} $$ {A_2} $$ {\tau _1} $(ns)$ {\tau _1} $(ns)
    2.53.200.3970.750.302.710.108
    54.151.1101.800.603.790.151
    106.002.0002.750.753.980.251
    下载: 导出CSV

    表  3  ANN替代模型超参数设置

    神经网络Batch SizeEpochs数量隐藏层数量及各层
    神经元数量
    ANN替代模型2550001000,1000,1000
    下载: 导出CSV

    表  4  传统MCS不确定分析法和ANN替代模型进行数值模拟的CPU耗时

    数值模拟方法仿真次数CPU耗时(s)
    MCS10001125663.71
    ANN替代模型2002011.21(训练耗时)+1.80(预测耗时)
    下载: 导出CSV
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出版历程
  • 收稿日期:  2020-08-26
  • 修回日期:  2021-09-11
  • 网络出版日期:  2021-10-28
  • 刊出日期:  2021-12-21

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