Optimal soil organic matter mapping using an ensemble model incorporating moderate resolution imaging spectroradiometer, portable X-ray fluorescence, and visible near-infrared data

被引:10
作者
Yan, Yang [1 ]
Li, Baoguo [1 ,2 ]
Rossel, Raphael Viscarra [3 ]
Sun, Fujun [4 ]
Huang, Yuanfang [1 ,2 ]
Shen, Chongyang [1 ,2 ]
Shi, Zhan [1 ]
Ji, Wenjun [1 ,2 ,5 ]
机构
[1] China Agr Univ, Coll Land Sci & Technol, Beijing 100193, Peoples R China
[2] Minist Nat Resources, Key Lab Agr Land Qual, Beijing 100193, Peoples R China
[3] Curtin Univ, Sch Mol & Life Sci, Soil & Landscape Sci, GPO Box U1987, Perth, WA 6845, Australia
[4] Shenyang Agr Univ, Coll Land & Environm, Shenyang 110866, Peoples R China
[5] Chinese Acad Sci, Aerosp Informat Res Inst, State Key Lab Remote Sensing Sci, Beijing 100101, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金;
关键词
Soil organic matter; Portable X-ray fluorescence; Visible near-infrared; Ensemble model; Uncertainty analysis; CARBON; SPECTROMETRY;
D O I
10.1016/j.compag.2023.107885
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
Digital soil mapping of soil organic matter (SOM) is necessary because of its importance for carbon sequestration, soil health, and food security. However, large-scale digital soil mapping of SOM remains a challenge to improve accuracy and provide more local information. To address this knowledge gap, a strategy that incorporates remote and proximal sensing data into an ensemble model for the digital soil mapping is proposed. In this study, moderate resolution imaging spectroradiometer, portable X-ray fluorescence, and visible near-infrared spectroscopy data from 402 soil samples were used to map the SOM at a resolution of 90 m, model the SOM with random forest, cubist, and ensemble models, and evaluate its environmental factors in the northeastern and northern Chinese plains, a typical agricultural plain (approximately 66,000,000 ha). The digital maps of the SOM were derived along with their uncertainties. The results show that the visible near-infrared and portable X-ray fluorescence data play an important role in the SOM distribution. Inclusion of these data in the model, improved the R-p(2) by 6.25-35.42 %, and reduced the root mean square error of the prediction by 0.30-1.54 g kg(-1). The ensemble model, which included remote and proximal sensing variables, outperformed the results of previous studies with a root mean square error of 6.68 g kg 1 and provided more detailed information. Thus, this study confirmed the effectiveness of the proposed strategy. The SOM product obtained by this strategy was able to accurately control soil management, and the structural equation model showed that human activities exerted a direct influence on SOM comparable to the overall effect of natural factors on SOM. The contribution of straw mulching to human activities was great with path coefficient >0.50. This suggests that land management, especially straw mulching, should be improved in this area. In summary, this study proposed a novel strategy for accurately and efficiently obtaining SOM products for agricultural decision-making, terrestrial carbon cycling, and carbon stock estimation. Future advancements will focus on more accurate and detailed global SOM maps or carbon storage by integrating multiple models with remote sensing data and proximal sensing data from available soil spectral libraries.
引用
收藏
页数:12
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