Abstract:Soil mapping demands large-scale surveys that are costly and time consuming. It is necessary to identify strategies with reduced costs to obtain detailed information for soil mapping. We aimed to compare multispectral satellite image and relief parameters for the quantification and mapping of clay and sand contents. The Temporal Synthetic Spectral (TESS) reflectance and Synthetic Soil Image (SYSI) approaches were used to identify and characterize texture spectral signatures at the image level. Soil samples wer… Show more
“…For our study, SySI represents the soils surface of agriculture areas and other natural surfaces with low vegetation cover and rock outcrops, when the vegetation was absent or almost absent, typical for savanas. The GEOS3 has also been implemented in different regions in Brazil for mapping soil variables [11,12,47]. Similar approaches were developed to produce bare soil composites based on Landsat data and accurately employed for soil mapping and management in Germany [9] and the Swiss Plateau and Europe [8].…”
The Midwest region in Brazil has the largest and most recent agricultural frontier in the country where there is no currently detailed soil information to support the agricultural intensification. Producing large-extent digital soil maps demands a huge volume of data and high computing capacity. This paper proposed mapping surface and subsurface key soil attributes with 30 m-resolution in a large area of Midwest Brazil. These soil maps at multiple depth increments will provide adequate information to guide land use throughout the region. The study area comprises about 851,000 km2 in the Cerrado biome (savannah) in the Brazilian Midwest. We used soil data from 7908 sites of the Brazilian Soil Spectral Library and 231 of the Free Brazilian Repository for Open Soil Data. We selected nine key soil attributes for mapping and aggregated them into three depth intervals: 0–20, 20–60 and 60–100 cm. A total of 33 soil predictors were prepared using Google Earth Engine (GEE), such as climate and geologic features with 1 km-resolution, terrain and two new covariates with 30 m-resolution, based on satellite measurements of the topsoil reflectance and the seasonal variability in vegetation spectra. The scorpan model was adopted for mapping of soil variables using random forest regression (RF). We used the model-based optimization by tuning RF hyperparameters and calculated the scaled permutation importance of covariates in R software. Our results were promising, with a satisfactory model performance for physical and chemical attributes at all depth intervals. Elevation, climate and topsoil reflectance were the most important covariates in predicting sand, clay and silt. In general, for predicting soil chemical attributes, climatic variables, elevation and vegetation reflectance provided to be the most important of predictive components, while for organic matter it was a combination of climatic dynamics and reflectance bands from vegetation and topsoil. The multiple depth maps showed that soil attributes largely varied across the study area, from clayey to sandy, suggesting that less than 44% of the studied soils had good natural fertility. We concluded that key soil attributes from multiple depth increments can be mapped using Earth observations data and machine learning methods with good performance.
“…For our study, SySI represents the soils surface of agriculture areas and other natural surfaces with low vegetation cover and rock outcrops, when the vegetation was absent or almost absent, typical for savanas. The GEOS3 has also been implemented in different regions in Brazil for mapping soil variables [11,12,47]. Similar approaches were developed to produce bare soil composites based on Landsat data and accurately employed for soil mapping and management in Germany [9] and the Swiss Plateau and Europe [8].…”
The Midwest region in Brazil has the largest and most recent agricultural frontier in the country where there is no currently detailed soil information to support the agricultural intensification. Producing large-extent digital soil maps demands a huge volume of data and high computing capacity. This paper proposed mapping surface and subsurface key soil attributes with 30 m-resolution in a large area of Midwest Brazil. These soil maps at multiple depth increments will provide adequate information to guide land use throughout the region. The study area comprises about 851,000 km2 in the Cerrado biome (savannah) in the Brazilian Midwest. We used soil data from 7908 sites of the Brazilian Soil Spectral Library and 231 of the Free Brazilian Repository for Open Soil Data. We selected nine key soil attributes for mapping and aggregated them into three depth intervals: 0–20, 20–60 and 60–100 cm. A total of 33 soil predictors were prepared using Google Earth Engine (GEE), such as climate and geologic features with 1 km-resolution, terrain and two new covariates with 30 m-resolution, based on satellite measurements of the topsoil reflectance and the seasonal variability in vegetation spectra. The scorpan model was adopted for mapping of soil variables using random forest regression (RF). We used the model-based optimization by tuning RF hyperparameters and calculated the scaled permutation importance of covariates in R software. Our results were promising, with a satisfactory model performance for physical and chemical attributes at all depth intervals. Elevation, climate and topsoil reflectance were the most important covariates in predicting sand, clay and silt. In general, for predicting soil chemical attributes, climatic variables, elevation and vegetation reflectance provided to be the most important of predictive components, while for organic matter it was a combination of climatic dynamics and reflectance bands from vegetation and topsoil. The multiple depth maps showed that soil attributes largely varied across the study area, from clayey to sandy, suggesting that less than 44% of the studied soils had good natural fertility. We concluded that key soil attributes from multiple depth increments can be mapped using Earth observations data and machine learning methods with good performance.
“…Since then, these application of random theory functions are extremely used for spatialisation of georeferenced data and as it has been performed for agricultural purposes (Dowd, 1991;Shannon et al, 2018;Wackernagel, 2014). The machine learning approach estimates soil spatial arrangements using ancillary variables such as digital elevation models (DEM) and its covariates, and remote sensing data such as satellite images from Landsat 5 Thematic Mapper (McBratney et al, 2003;Fongaro et al, 2018;Gallo et al, 2018;Castro-Franco et al, 2018).…”
Applying the upcoming technologies in agriculture has been a major economic, environmental and social challenge for scientists and farmers. In order to overcome such challenge, this study evaluated the advantages and limitations of using geostatistics and machine learning for soil mapping in agricultural practices and soil surveys. The study occurred in Tocantins State, Brazil, and consisted into seven areas with a total extension of 17.24 km 2 , 222 meters regular gridded resulting in one-point sampling per 0.0493 km 2 of five randomly sampled cores within a 1 m circle radius. It was collected 332 georeferenced soil samples at 0-20 cm depth using an auger and then, soil laboratory analyses performed. Afterward, liming rate maps were originated from the predicted soil attributes clay, cation exchange capacity and base saturation comparing four methods: ordinary kriging, random forest, cubist, support vector machine and the best model results of each soil attribute. Evaluating the methods, the Pearson's index presented strong results for soil attributes predicted by random forest and ordinary kriging. Machine learning methods can be successfully applied for soil mapping in agricultural practices and soil surveys using less soil samples rather than geostatistical framework.
“…A partir dos estudos de (Neto, 2017) Era esperado que o teor de argila fosse determinante nessa diferenciação, decorrente dos processos da evolução da vertente já trabalhado e explicado por outros estudos (Obi Redy et al, 2004;Pissarra et al, 2004;Demattê et al, 2011). Da mesma maneira a cor também era esperada ter uma relação com os compartimentos, sendo totalmente influenciada pela drenagem dos solos que é diferente em cada compartimento (Campos e Demattê, 2004 Assim como em outros estudos, a argila nos horizontes superficiais tem sido utilizada para o mapeamento digital de solos, tendo em vista sua alta correlação com os parâmetros do relevo (Fongaro et al, 2018;Poppiel et al, 2018). Assim, com a identificação da variação do e 11 continuou representada pelo atributo em questão, apresentando baixa variação de solos nas áreas (Tabela 5).…”
Section: Relação Entre Atributos Do Solo E Rede De Drenagemunclassified
Rede de drenagem 2. Compartimentação automática da paisagem 3. Mapeamento digital de solos 4. Estereoscopia digital I. Título AGRADECIMENTOS Agradeço primeiramente à Deus pelo sustento e por sempre me surpreender com sua bondade. Sem isso seria impossível caminhar. Agradeço imensamente à minha família, pois sempre me apoiaram e deram suporte em todos os momentos desse caminho. Agradeço em especial ao meu Pai, Nilton. Todo o seu esforço valeu a pena. Reconheço que se não fossem os seus finais de semana perdidos eu não estaria aqui. Serei eternamente grato e sei que está orgulhoso. Agradeço à minha mãe pelo amor e carinho. A condição de fazer esse curso era você estar bem e hoje está curada. O tempo passou mas a saudade ainda aperta. Obrigado por me incentivar sempre. Agradeço à meu irmão Luccas. Nunca se contente com pouco, seja o melhor que puder em tudo. Você vai mais longe do que pode imaginar. Agradeço à Ana, minha noiva, meu amor. Você deixou a caminhada mais leve e mais bela. Obrigado pelo apoio e compreensão nos tempos difíceis. Você é uma mulher incrível! Te amo! Agradeço à minha segunda família, Nivaldo e Hilda. Obrigado por me tratarem como filho e não pouparem esforços para ajudar quando preciso. Vocês também tornaram a caminhada muito mais facil. Viva o vinho! Agradeço aos novos irmãosTaís, Pedro e Sara. A caminhada está só começando. Agradeço aos amigos e a Igreja no Jupiá.
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