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基于经验小波变换的鄱阳湖CODMn预测

陈伟 金柱成 俞真元 王晓丽 彭士涛 魏燕杰

陈伟,金柱成,俞真元,等.基于经验小波变换的鄱阳湖CODMn预测[J].环境工程技术学报,2023,13(1):180-187 doi: 10.12153/j.issn.1674-991X.20210592
引用本文: 陈伟,金柱成,俞真元,等.基于经验小波变换的鄱阳湖CODMn预测[J].环境工程技术学报,2023,13(1):180-187 doi: 10.12153/j.issn.1674-991X.20210592
CHEN W,KIM J S,YU J W,et al.Forecasting CODMn of Poyang Lake based on empirical wavelet transform[J].Journal of Environmental Engineering Technology,2023,13(1):180-187 doi: 10.12153/j.issn.1674-991X.20210592
Citation: CHEN W,KIM J S,YU J W,et al.Forecasting CODMn of Poyang Lake based on empirical wavelet transform[J].Journal of Environmental Engineering Technology,2023,13(1):180-187 doi: 10.12153/j.issn.1674-991X.20210592

基于经验小波变换的鄱阳湖CODMn预测

doi: 10.12153/j.issn.1674-991X.20210592
基金项目: 中央级公益性科研院所基本科研业务费专项(TKS190202,TKS20200405);天津市科技计划项目(20JCQNJC00100)
详细信息
    作者简介:

    陈伟(1997—),男,硕士研究生,主要研究方向为生态修复,tjutcw1997@163.com

    通讯作者:

    王晓丽(1972—),女,教授,主要研究方向为污染修复技术,tjutwxl@163.com

  • 中图分类号: X524

Forecasting CODMn of Poyang Lake based on empirical wavelet transform

  • 摘要:

    高锰酸盐指数(CODMn)是衡量水质状况的最重要参数之一,能反映水体受还原性物质污染的程度。结合经验小波变换(EWT)和双向长短期记忆(BLSTM)神经网络,提出了一种先利用EWT将原始的CODMn时间序列分解成若干成分,然后利用BLSTM神经网络对分解出来的每个成分进行预测,最后将所有成分的预测结果重建获得最终CODMn预测值的新的混合模型EWT-BLSTM;并以2017年8月—2020年4月鄱阳湖CODMn监测数据为研究对象,进行模型性能验证。结果表明:EWT-BLSTM模型具有良好的预测性能,预测未来1 d以后的CODMn时,EWT-BLSTM模型的平均绝对百分比误差为2.25%,与单一BLSTM神经网络模型相比降低了10.53%;预测未来7 d以后的CODMn时,EWT-BLSTM模型的平均绝对百分比误差为8.36%,与单一BLSTM神经网络模型相比降低了16.16%。在CODMn峰值处,该模型依然保持较高稳定的预测性能,说明在数据相对复杂、极端的情况下,该模型依然适用。

     

  • 图  1  2017年8月1日—2020年4月30日鄱阳湖CODMn数据分布

    Figure  1.  CODMn data distribution of Poyang Lake from August 1, 2017 to April 30, 2020

    图  2  LSTM神经网络和BLSTM神经网络的对比

    注:x(1),x (2),···,x(t)为数据输入;y(1),y (2),···,y (t)为数据输出。

    Figure  2.  Comparison between LSTM and BLSTM neural networks

    图  3  地表水体CODMn预测流程

    Figure  3.  Flow chart of CODMn prediction of surface water

    图  4  EWT对鄱阳湖CODMn时间序列的数据分解

    Figure  4.  Data decomposition of CODMn time series by EWT in Poyang Lake

    图  5  鄱阳湖测试阶段CODMn预测值和实测值之间的相关性 (P<0.01)

    Figure  5.  Correlation between predicted and measured CODMn values of Poyang Lake in test stage (P < 0.01)

    图  6  鄱阳湖测试阶段CODMn预测值和实测值对比

    Figure  6.  Comparision of predicted and measured CODMn values of Poyang Lake in test stage

    表  1  参与比较的模型的结构

    Table  1.   Structure of the competitor models

    模型数据分解算法神经网络算法
    BLSTM不使用BLSTM
    WD-BLSTMWDBLSTM
    EMD-BLSTMEMDBLSTM
    EWT-SVREWTSVR
    EWT-ELMEWTELM
    EWT-LSTMEWTLSTM
    下载: 导出CSV

    表  2  ICEEMDAN分解成分的样本熵

    Table  2.   Sample entropy calculation of ICEEMDAN modes

    成分类型样本熵
    原始数据0.85
    MODE10.81
    MODE20.72
    MODE30.57
    MODE40.45
    MODE50.19
    MODE60.09
    MODE70.04
    MODE80.00
    下载: 导出CSV

    表  3  CODMn时间序列以分解成分的预测模型的时间滞后值

    Table  3.   Time lags of the prediction model of the decomposition components of CODMn time series

    成分类型1 d以后预测7 d以后预测
    MODE14741
    MODE25246
    MODE34943
    MODE43630
    MODE55448
    MODE64135
    MODE75448
    MODE85650
    下载: 导出CSV

    表  4  BLSTM神经网络的超参数

    Table  4.   Hyperparameters of BLSTM neural network

    参数数值
    BLSTM层数2
    第一层的神经元数输入大小×2
    第二层的神经元数输入大小
    最小批量大小16
    学习率0.01
    最大迭代次数100
    下载: 导出CSV

    表  5  测试阶段EWT-BLSTM模型的预测性能

    Table  5.   Forecast performance of EWT-BLSTM model in the testing stage

    预测类型MAE/(mg/L)RMSE/(mg/L)MAPE/%
    1 d以后预测0.050.072.25
    7 d以后预测0.200.328.36
    下载: 导出CSV

    表  6  各模型的预测性能比较

    Table  6.   Comparison of the prediction performance of different models

    模型1 d以后预测7 d以后预测
    MAE
    /(mg/L)
    RMSE
    /(mg/L)
    MAPE
    /%
    MAE
    /(mg/L)
    RMSE
    /(mg/L)
    MAPE
    /%
    BLSTM0.320.6212.780.600.8724.52
    WD-BLSTM0.170.356.770.280.4611.72
    EMD-BLSTM0.190.239.330.340.5214.70
    EWT-SVR0.300.512.490.490.6723.75
    EWT-ELM0.230.369.790.290.4911.69
    EWT-LSTM0.050.082.340.250.3511.42
    EWT-BLSTM0.050.072.250.200.328.36
    下载: 导出CSV
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  • 收稿日期:  2021-10-19

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