基于MPDI时间序列特征的平原区土壤质地数字制图

Digital Mapping of Soil Texture in Plain Areas Based on MPDI Time Series Features

  • 摘要:
    目的 探究利用改进垂直干旱指数(MPDI)的时间序列特征提升平原区土壤质地数字制图精度,为平原区土壤质地数字制图提供新的见解。
    方法 本研究以河南省封丘县为研究区,将基于地表动态反馈(LSDF)方法构建的MPDI时间序列特征变量与地形因子、气候因子、植被因子常规变量相结合作为协变量,借助普通克里格、支持向量机、随机森林和卷积神经网络模型预测模型对土壤质地(黏粒、粉粒、砂粒质量百分比)进行数字制图,并运用SHAP方法解释变量重要性。
    结果 研究结果显示,引入MPDI时间序列特征后,支持向量机、随机森林和卷积神经网络模型预测精度均有所提升。其中卷积神经网络模型预测结果最优,黏粒、粉粒、砂粒含量的平均绝对误差(MAE)、均方根误差(RMSE)、相对均方根误差(RRMSE)最低,分别为4.937、6.344、0.296;5.363、6.677、0.266;10.007、12.215、0.228。黏粒、粉粒、砂粒质量百分比一致相关性系数(CCC)和决定系数(R2)最高,分别为0.343、0.227,0.268、0.143,0.312、0.189。同时SHAP重要性排序结果显示,MPDI时间序列特征变量在模型预测中具有重要作用,是土壤质地预测的关键变量。
    结论 引入MPDI时间序列特征后,不同模型预测误差在不同程度上均有所降低,提高了土壤质地数字制图预测精度。

     

    Abstract:
    Objective The aim was to explore the application of the improved vertical drought index (MPDI) in extracting time series features to enhance the accuracy of digital mapping of soil texture in plain areas, in order to provide new insights for the digital mapping of soil texture in plain regions.
    Methods Taking Fengqiu County in Henan Province as the research area, the combining MPDI time series feature variables were constructed based on the Land Surface Dynamic Feedback (LSDF) method with conventional variables such as terrain factors, climate factors, and vegetation factors as covariates. The ordinary kriging, support vector machine, random forest, and convolutional neural network models were used to perform digital mapping of soil texture (percentages of clay, silt, and sand), and the SHAP method was applied to interpret variable importance.
    Results The research results showed that the prediction accuracy from support vector machine, random forest, and convolutional neural network models were all improved after introducing MPDI time series features. Among them, the convolutional neural network model achieved the best prediction results, with the lowest mean absolute error (MAE), root mean square error (RMSE), and relative root mean square error (RRMSE) for clay, silt, and sand content, which were 4.937, 6.344, 0.296 in MAE; 5.363, 6.677, 0.266 In RMSE; and 10.007, 12.215, 0.228 in RRMSE, respectively. The concordance correlation coefficient (CCC) and coefficient of determination (R2) were also the highest, showing 0.343, 0.227 in clay; 0.268, 0.143 in silt; and 0.312, 0.189, in sand, respectively. At the same time, the SHAP importance ranking results indicated that MPDI time series feature variables played an important role in model prediction and were key variables for soil texture prediction.
    Conclusion The introduction of MPDI time series features reduces prediction errors to varying degrees across different models, improves prediction accuracy, which will propose a new environmental variable, and provide new insights for digital mapping of soil texture in plain areas.

     

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