Comparison of Digital Mapping Methods for the Thickness of Black Soil Layer of Cultivated Land in Typical Black Soil Area of Songnen Plain

被引:0
|
作者
Guo J. [1 ,2 ]
Liu F. [1 ,2 ]
Xu S. [1 ,2 ]
Gao L. [1 ]
Zhao Z. [1 ,4 ]
Hu W. [2 ,3 ]
Yu D. [1 ,2 ]
Zhao Y. [1 ,2 ]
机构
[1] State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing
[2] University of Chinese Academy of Sciences, Beijing
[3] Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing
[4] School of Geomatics, Anhui University of Science and Technology, Huainan
基金
中国国家自然科学基金;
关键词
digital soil mapping; machine learning; optimal covariates; random forest-regression kriging; spatial differentiation characteristics; stacking generalization model; thickness of black soil layer; variable selection;
D O I
10.12082/dqxxkx.2024.230682
中图分类号
学科分类号
摘要
The thickness of black soil layer is closely related to the soil fertility and quality of agricultural soils. Accurately describing the spatial distribution of the thickness of the cultivated black soil layer in the typical black soil area of Songnen in Northeast China is of great significance. It contributes to the protection of black soil and promotes the sustainable development of agriculture. However, the commonly used predictive models are difficult to apply when trying to map digital soils in flat areas. How to accurately predict the spatial distribution characteristics of the thickness of black soil layer is an urgent problem that needs to be solved. The typical black soil area of Songnen in Northeast China was selected as the research area. Based on the basic data of 106 profile points and 45 environmental factors in the study area, the variables were screened by factor importance ranking and correlation elimination method. Multiple Linear Regression (MLR), Random Forest (RF), Gradient Boosting Decision Tree (GBDT), Extreme Gradient Boosting (XGBoost), Random Forest-Regression Kriging (RF-RK), and Stacking methods were used to predict the thickness of black soil layer. The predictive accuracy of different models was evaluated and the optimal covariates influencing the spatial distribution of the thickness of black soil layer were studied. Based on the best model, the black soil layer thickness classification map of farmland in the black soil area of northeast China was drawn. Our results showed that the Stacking method combined the advantages of several models, and its prediction performance was the best (R2=0.47, MAE=21.02 cm, RMSE=27.12 cm), followed by RF- RK and RF. After eliminating the environmental variables with low contribution through variable screening, the R2 of different models increased by an average of 0.11, with a maximum increase of 0.32 in MLR. The spatial distribution trend of the thickness of black soil layer predicted by different models was generally consistent. The black soil layer above 60 cm was mainly distributed in the northeast and southeast of the study area, while the black soil layer below 30 cm was mainly distributed in the southwest of the study area. In the plain area, RF- RK and Stacking can be used as effective methods for predicting the thickness of black soil layer. Gross Primary Productivity (GPP), Slope Length and Steepness Factor(LS), and Land Surface Temperature Maximum (LSTm) were the most important explanatory variables in the model. The spatial distribution information of the thickness of black soil layer can provide data support for black soil protection and agricultural sustainable development in the black soil region. © 2024 Science Press. All rights reserved.
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页码:1452 / 1468
页数:16
相关论文
共 62 条
  • [1] Han X.Z., Li N., Research progress of black soil in Northeast China[J], Scientia Geographica Sinica, 38, 7, pp. 1032-1041, (2018)
  • [2] Zhang X.Y., Sui Y.Y., Song C.Y., Degradation process of arable mollisols[J], Soils and Crops, 2, 1, pp. 1-6, (2013)
  • [3] Li B.G., Liu Z., Huang F., Et al., Ensuring national food security by strengthening high- productivity black soil granary in Northeast China[J], Bulletin of Chinese Academy of Sciences, 36, 10, pp. 1184-1193, (2021)
  • [4] Liu D.G., Zhang X.C., Cui Y., Et al., Investigation report on the issue of black soil protection[J], Chinese Journal of Agricultural Resources and Regional Planning, 25, 4, pp. 16-19, (2004)
  • [5] Liu K., Wei M.H., Dai H.M., Et al., Spatiotemporal variation of black soil layer thickness in black soil region of Northeast China[J], Geology and Resources, 31, 3, pp. 434-442, (2022)
  • [6] Zhang X.Y., Liu X.B., Key issues of mollisols research and soil erosion control strategies in China[J], Bulletin of Soil and Water Conservation, 40, 4, pp. 340-344, (2020)
  • [7] Zhu A.X., Yang L., Fan N.Q., Et al., The review and outlook of digital soil mapping[J], Progress in Geography, 37, 1, pp. 66-78, (2018)
  • [8] Zhang G.L., Shi Z., Zhu A.X., Et al., Progress and perspective of studies on soils in space and time[J], Acta Pedologica Sinica, 57, 5, pp. 1060-1070, (2020)
  • [9] Chabala L.M., Mulolwa A., Lungu O., Application of ordinary kriging in mapping soil organic carbon in Zambia [J], Pedosphere, 27, 2, pp. 338-343, (2017)
  • [10] da Silva Chagas C., de Carvalho W., Bhering S.B., Et al., Spatial prediction of soil surface texture in a semiarid region using random forest and multiple linear regressions [J], Catena, 139, pp. 232-240, (2016)