Jorge Tadeu Fim Rosas , José A.M. Demattê , Nícolas Augusto Rosin , Raul Roberto Poppiel , Nélida E.Q. Silvero , Merilyn Taynara Accorsi Amorim , Heidy S. Rodríguez-Albarracín , Letícia Guadagnin Vogel , Bruno dos Anjos Bartsch , José João Lelis Leal de Souza , Lucas de Carvalho Gomes , Danilo César de Mello
{"title":"利用地球观测策略绘制巴西粘土氧化物分馏图","authors":"Jorge Tadeu Fim Rosas , José A.M. Demattê , Nícolas Augusto Rosin , Raul Roberto Poppiel , Nélida E.Q. Silvero , Merilyn Taynara Accorsi Amorim , Heidy S. Rodríguez-Albarracín , Letícia Guadagnin Vogel , Bruno dos Anjos Bartsch , José João Lelis Leal de Souza , Lucas de Carvalho Gomes , Danilo César de Mello","doi":"10.1016/j.geoderma.2025.117425","DOIUrl":null,"url":null,"abstract":"<div><div>The major oxides in the clay fraction of tropical soils are iron (Fe2O3), aluminum (Al2O3), and silicon (SiO2) oxides, which are responsible for the soil’s capacity to provide multiple ecosystem services. Therefore, they are used to classify the soils into different pedological classes. Despite their importance of these oxides, quantifying them on a large scale presents significant challenges. The most common method is laboratory sulfuric acid digestion, which is expensive, complex, and environmentally detrimental. To overcome these issues and provide faster results, we developed a satellite technique associated with machine learning (ML) to map Fe<sub>2</sub>O<sub>3</sub>, Al<sub>2</sub>O<sub>3</sub>, and SiO<sub>2</sub> in all agricultural areas in Brazil at 30 m resolution. Additionally, we tested the feasibility of the generated maps to infer soil weathering, and assist in the construction of pedological maps. A dataset, comprising 5,330 sites (0–20 cm and 80–100 cm) across all 27 states was employed in prediction. Six spectral variables obtained from the historical Landsat series (bare soil) and seven terrain attributes derived from a digital elevation model were employed to generate the Fe<sub>2</sub>O<sub>3</sub>, Al<sub>2</sub>O<sub>3</sub>, and SiO<sub>2</sub> maps, using the Random Forest algorithm. The predicted maps of oxides covered nearly 3.48 million km<sup>2</sup> (∼40 % of the national territory). The best predictions were observed for Fe<sub>2</sub>O<sub>3</sub> in the 0–20 cm layer (RMSE = 49.8 <span><span>g.kg</span><svg><path></path></svg></span><sup>−1</sup>, RPIQ = 1.82, and R<sup>2</sup> = 0.62), while the worst predictions were for SiO<sub>2</sub> in the 80–100 cm layer (RMSE = 65.3 <span><span>g.kg</span><svg><path></path></svg></span><sup>−1</sup>, RPIQ = 1.50 and R<sup>2</sup> = 0.22). It was possible to infer soil weathering using the Ki index. Despite the models not showing such high R<sup>2</sup> values, the results are aligned with legacy maps, highly weathered soils were observed in the plateaus of the Cerrado biome, while younger soils were observed in the arid Caatinga biome and waterlogged soils in the Pantanal biome. The generated maps also demonstrated a high potential for grouping pedological soil classes. They also revealed a relationship between oxide contents and the NDVI of sugarcane crops, indicating potential applications in crop management. Moreover, this satellite-based technique, supported by ML, presents a plausible approach to predict oxide fraction at high spatial resolution for large areas.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117425"},"PeriodicalIF":6.6000,"publicationDate":"2025-07-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Mapping clay fraction oxides in Brazil using Earth observation strategy\",\"authors\":\"Jorge Tadeu Fim Rosas , José A.M. Demattê , Nícolas Augusto Rosin , Raul Roberto Poppiel , Nélida E.Q. Silvero , Merilyn Taynara Accorsi Amorim , Heidy S. Rodríguez-Albarracín , Letícia Guadagnin Vogel , Bruno dos Anjos Bartsch , José João Lelis Leal de Souza , Lucas de Carvalho Gomes , Danilo César de Mello\",\"doi\":\"10.1016/j.geoderma.2025.117425\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The major oxides in the clay fraction of tropical soils are iron (Fe2O3), aluminum (Al2O3), and silicon (SiO2) oxides, which are responsible for the soil’s capacity to provide multiple ecosystem services. Therefore, they are used to classify the soils into different pedological classes. Despite their importance of these oxides, quantifying them on a large scale presents significant challenges. The most common method is laboratory sulfuric acid digestion, which is expensive, complex, and environmentally detrimental. To overcome these issues and provide faster results, we developed a satellite technique associated with machine learning (ML) to map Fe<sub>2</sub>O<sub>3</sub>, Al<sub>2</sub>O<sub>3</sub>, and SiO<sub>2</sub> in all agricultural areas in Brazil at 30 m resolution. Additionally, we tested the feasibility of the generated maps to infer soil weathering, and assist in the construction of pedological maps. A dataset, comprising 5,330 sites (0–20 cm and 80–100 cm) across all 27 states was employed in prediction. Six spectral variables obtained from the historical Landsat series (bare soil) and seven terrain attributes derived from a digital elevation model were employed to generate the Fe<sub>2</sub>O<sub>3</sub>, Al<sub>2</sub>O<sub>3</sub>, and SiO<sub>2</sub> maps, using the Random Forest algorithm. The predicted maps of oxides covered nearly 3.48 million km<sup>2</sup> (∼40 % of the national territory). The best predictions were observed for Fe<sub>2</sub>O<sub>3</sub> in the 0–20 cm layer (RMSE = 49.8 <span><span>g.kg</span><svg><path></path></svg></span><sup>−1</sup>, RPIQ = 1.82, and R<sup>2</sup> = 0.62), while the worst predictions were for SiO<sub>2</sub> in the 80–100 cm layer (RMSE = 65.3 <span><span>g.kg</span><svg><path></path></svg></span><sup>−1</sup>, RPIQ = 1.50 and R<sup>2</sup> = 0.22). It was possible to infer soil weathering using the Ki index. Despite the models not showing such high R<sup>2</sup> values, the results are aligned with legacy maps, highly weathered soils were observed in the plateaus of the Cerrado biome, while younger soils were observed in the arid Caatinga biome and waterlogged soils in the Pantanal biome. The generated maps also demonstrated a high potential for grouping pedological soil classes. They also revealed a relationship between oxide contents and the NDVI of sugarcane crops, indicating potential applications in crop management. 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Mapping clay fraction oxides in Brazil using Earth observation strategy
The major oxides in the clay fraction of tropical soils are iron (Fe2O3), aluminum (Al2O3), and silicon (SiO2) oxides, which are responsible for the soil’s capacity to provide multiple ecosystem services. Therefore, they are used to classify the soils into different pedological classes. Despite their importance of these oxides, quantifying them on a large scale presents significant challenges. The most common method is laboratory sulfuric acid digestion, which is expensive, complex, and environmentally detrimental. To overcome these issues and provide faster results, we developed a satellite technique associated with machine learning (ML) to map Fe2O3, Al2O3, and SiO2 in all agricultural areas in Brazil at 30 m resolution. Additionally, we tested the feasibility of the generated maps to infer soil weathering, and assist in the construction of pedological maps. A dataset, comprising 5,330 sites (0–20 cm and 80–100 cm) across all 27 states was employed in prediction. Six spectral variables obtained from the historical Landsat series (bare soil) and seven terrain attributes derived from a digital elevation model were employed to generate the Fe2O3, Al2O3, and SiO2 maps, using the Random Forest algorithm. The predicted maps of oxides covered nearly 3.48 million km2 (∼40 % of the national territory). The best predictions were observed for Fe2O3 in the 0–20 cm layer (RMSE = 49.8 g.kg−1, RPIQ = 1.82, and R2 = 0.62), while the worst predictions were for SiO2 in the 80–100 cm layer (RMSE = 65.3 g.kg−1, RPIQ = 1.50 and R2 = 0.22). It was possible to infer soil weathering using the Ki index. Despite the models not showing such high R2 values, the results are aligned with legacy maps, highly weathered soils were observed in the plateaus of the Cerrado biome, while younger soils were observed in the arid Caatinga biome and waterlogged soils in the Pantanal biome. The generated maps also demonstrated a high potential for grouping pedological soil classes. They also revealed a relationship between oxide contents and the NDVI of sugarcane crops, indicating potential applications in crop management. Moreover, this satellite-based technique, supported by ML, presents a plausible approach to predict oxide fraction at high spatial resolution for large areas.
期刊介绍:
Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.