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基于平均影响值算法和BP神经网络的根区土壤湿度估算
引用本文:袁玲,方秀琴,郭晓萌,杨露露,张晓祥,任立良.基于平均影响值算法和BP神经网络的根区土壤湿度估算[J].科学技术与工程,2022,22(17):6911-6919.
作者姓名:袁玲  方秀琴  郭晓萌  杨露露  张晓祥  任立良
作者单位:河海大学水文与水资源学院;河海大学水文与水资源学院;河海大学海岸灾害及防护教育部重点实验室
基金项目:国家重点研发计划项目(2019YFC1510601);国家自然科学基金(42071040)
摘    要:为了探讨基于地表特征信息应用人工神经网络计算根区土壤湿度的可行性,本研究利用中国境内四个典型区域的农田生态系统野外台站的地表和根区土壤水分实测数据,结合6种气象数据和2种植被指数数据构建了不同深度根区土壤湿度的BP神经网络计算模型,采用决定系数(R2)、均方根误差(RMSE)和平均绝对误差(MAE)三个指标来评估四个站点不同土层深度的模型性能,并使用平均影响值算法(MIV)得到9个地表特征变量的重要性。结果表明:在20~90/100cm深度,模型的平均R2值分别为0.79、0.69、0.66、0.56、0.51和0.47;RMSE为1.91%、2.17%、2.51%、2.71%、2.82%和3.08%;MAE为1.44%、1.61%、1.75%、1.89%、2.04%和2.35%,表明BP神经网络模型能够较好地拟合不同气候和土壤类型区域站点的根区土壤湿度,但模型性能和对土壤湿度的估算精度随土壤深度的增加而降低。地表特征信息的重要性计算结果表明,表层土壤湿度是根区土壤湿度计算模型中最为重要的特征,多个地面特征之间的相互作用为辅助条件,且不同特征在不同气候区和土壤类型区对RZSM的影响情况也不一致。

关 键 词:土壤湿度  时序变化  BP神经网络  MIV算法
收稿时间:2021/9/17 0:00:00
修稿时间:2022/5/27 0:00:00

Calculation of Root Zone Soil Moisture Using MIV-BP Neural Networks
Yuan Ling,Fang Xiuqin,Guo Xiaomeng,Yang Lulu,Zhang Xiaoxiang,Ren Liliang.Calculation of Root Zone Soil Moisture Using MIV-BP Neural Networks[J].Science Technology and Engineering,2022,22(17):6911-6919.
Authors:Yuan Ling  Fang Xiuqin  Guo Xiaomeng  Yang Lulu  Zhang Xiaoxiang  Ren Liliang
Institution:College of Hydrology and Water Resources, Hohai University
Abstract:In order to explore the feasibility of using the artificial neural network method to calculate the RZSM based on the surface information, the BP neural network models were constructed to estimate the RZSM at different soil depths using the measured soil moisture data, meteorological data and vegetation index data at four typical sites in China. The coefficient of determination (R2), the root mean square error (RMSE) and the mean absolute error (MAE) were used to evaluate the performance of the models at different soil depths. The mean impact value (MIV) was used to obtain the importance of the input variables. The results show that at depths of 20~90/100cm, the average R2 values of the model are 0.79, 0.69, 0.66, 0.56, 0.51 and 0.47, respectively; RMSE is 1.91%, 2.17%, 2.51%, 2.71%, 2.82% and 3.08%; MAE is 1.44%, 1.61% 1.75%, 1.89%, 2.04%, and 2.35%, which indicated that the BP Neural Networks method was able to fit the RZSM variability at different stations with different climates and soil type, but the performance and accuracy of RZSM decrease with the increase of soil depth. The results also indicated the model capability of RZSM calculation decreased as the increase of soil depth. The MIV results showed that SSM is the most important feature in the model and the interaction between multiple ground features is an auxiliary condition, also, the effects of different features on RZSM in different climate zones and soil types are inconsistent.
Keywords:soil moisture  time series change  BP neural network  MIV
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