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基于協(xié)同克里金插值的土壤耕作層含水率反演方法
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陜西省重點研發(fā)計劃項目(2024NC-ZDCYL-05-02)


Inversion of Soil Tillage Layer Moisture Content Based on Co-Kriging Interpolation
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    摘要:

    土壤耕作層是作物生長發(fā)育的基礎(chǔ),準確監(jiān)測土壤耕作層含水率并對作物進行精準灌溉能提高作物產(chǎn)量和水資源利用率。為實現(xiàn)高效監(jiān)測土壤耕作層含水率,提出一種基于協(xié)同克里金插值的土壤耕作層含水率反演方法。首先以能夠獲取土壤表層信息的Sentinel-1衛(wèi)星數(shù)據(jù)為本文數(shù)據(jù)源,與具有可靠運算能力的XGBoost(Extreme gradient boosting)模型結(jié)合可以高效反演土壤表層含水率;將其大范圍土壤含水率反演結(jié)果作為協(xié)變量,把115個實測土壤耕作層含水率作為主變量,利用土壤表層與耕作層變量間的協(xié)同關(guān)系,采用協(xié)同克里金方法插值得到土壤耕作層含水率;協(xié)同克里金法可以很好地利用土壤表層與耕作層變量間的協(xié)同關(guān)系提升插值精度,并且在一定程度上可解決土壤耕作層含水率實測數(shù)據(jù)量不足的問題。將土壤耕作層含水率克里金插值和利用表層與耕作層含水率線性擬合進行對比,結(jié)果表明,采用協(xié)同克里金插值反演土壤耕作層含水率能夠大幅提高預測準確性,決定系數(shù)R2分別提高0.25和0.20,均方根誤差(RMSE)分別降低0.029、0.014cm3/cm3,平均絕對誤差(MAE)分別降低0.028、0.015cm3/cm3,精度顯著提高。

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    The soil tillage layer is the foundation of crop growth and development. Accurately monitoring the moisture content of the soil tillage layer and providing precise irrigation to crops can improve crop yield and water resource utilization efficiency. To achieve efficient monitoring of soil tillage layer moisture content, a soil tillage layer moisture content inversion method based on collaborative Kriging interpolation was proposed. Firstly, Sentinel-1 satellite data, which can obtain soil surface information, was used as the data source. Combined with the reliable XGBoost (extreme gradient boosting) model, it can efficiently invert soil surface moisture content. Using the large-scale soil moisture inversion results as covariates and 115 measured soil tillage layer moisture contents as main variables, the synergistic relationship between soil surface and tillage layer variables was utilized to interpolate the soil tillage layer moisture content using the collaborative Kriging method. The collaborative Kriging method can effectively utilize the synergistic relationship between soil surface and tillage layer variables to improve interpolation accuracy, and to some extent solve the problem of insufficient measured data on soil tillage layer moisture content. Comparing the Kriging interpolation of soil tillage layer moisture content with the linear fitting of surface and tillage layer moisture content, the results showed that using collaborative Kriging interpolation to invert soil tillage layer moisture content can significantly improve prediction accuracy. The coefficient of determination R2 was increased by 0.25 and 0.20, the root mean square error (RMSE) was decreased by 0.029cm3/cm3 and 0.014cm3/cm3, and the average absolute error (MAE) was decreased by 0.028cm3/cm3 and 0.015cm3/cm3, respectively. The accuracy was significantly improved.

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郭交,朱哲,項詩雨,鄺曉飛,尉鵬亮.基于協(xié)同克里金插值的土壤耕作層含水率反演方法[J].農(nóng)業(yè)機械學報,2025,56(6):457-467. GUO Jiao, ZHU Zhe, XIANG Shiyu, KUANG Xiaofei, WEI Pengliang. Inversion of Soil Tillage Layer Moisture Content Based on Co-Kriging Interpolation[J]. Transactions of the Chinese Society for Agricultural Machinery,2025,56(6):457-467.

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  • 收稿日期:2024-12-18
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  • 在線發(fā)布日期: 2025-06-10
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