Digital mapping of soil parent material in a heterogeneous tropical area

被引:28
作者
Bonfatti, Benito R. [1 ]
Dematte, Jose A. M. [1 ]
Marques, Karina P. P. [1 ]
Poppiel, Raul R. [1 ]
Rizzo, Rodnei [1 ]
Mendes, Wanderson de S. [1 ]
Silvero, Nelida E. Q. [1 ]
Safanelli, Jose L. [1 ]
机构
[1] Univ Sao Paulo, Luiz de Queiroz Coll Agr, Dept Soil Sci, Ave Padua Dias 11,Postal Box 09, BR-13416900 Piracicaba, SP, Brazil
基金
巴西圣保罗研究基金会;
关键词
Parent material; Soil formation factors; Bare soil image; Machine learning; REGION; CLASSIFICATION; REFLECTANCE; GOETHITE; HEMATITE; BASIN;
D O I
10.1016/j.geomorph.2020.107305
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Parent material is one of the five factors in soil formation. Studies on parent material allow interpreting soil genesis processes and improve our knowledge of specific soil attributes. However, soil parent material maps at detailed cartographic scale (finer than 1:100,000) are rare in tropical areas and it is usually inferred from poorly detailed geological data, which generally group different lithologies into single units. Thus, we propose a methodology to map soil parent material based on remote sensing and machine learning in a geologically very complex area. The study site covers 1378 km(2) in Sao Paulo State, Brazil. Prediction models used data from 280 geological observation points, a digital elevation model (spatial resolution of 5 m, upscale to 30 m) and multitemporal Landsat images in a range of 30 years. We evaluated six classification algorithms, namely random forest, decision tree, support vector machine, multinomial logistic regression, K-means (unsupervised classification), and object-based image analysis with maximum likelihood classification. Environmental covariates were grouped to create different scenarios combining terrain derivatives, hydrologic covariates, topsoil spectral reflectance, and spatial coordinates. A bare soil image, elaborated using 30 years of Landsat data, was evaluated as a covariate to predict soil parent material. Predictions were validated using three different strategies: crossvalidation, separate validation dataset (20%), and comparison with legacy geological maps (information from two areas with geological maps at fine scale). We also assessed the correspondence between the map of predicted soil parent material and data of soil particle size from 571 soil sampling points. Random forest algorithm presented the best validation performance, whereas the group of terrain derivatives and hydrologic covariates explained most of model variation. The produced parent material map was coherent with the spatial distribution of soil particle size across the study area. (C) 2020 Elsevier B.V. All rights reserved.
引用
收藏
页数:17
相关论文
共 71 条
[1]  
Al-Khaier F., 2003, SOIL SALINITY DETECT, P1
[2]   Koppen's climate classification map for Brazil [J].
Alvares, Clayton Alcarde ;
Stape, Jose Luiz ;
Sentelhas, Paulo Cesar ;
de Moraes Goncalves, Jose Leonardo ;
Sparovek, Gerd .
METEOROLOGISCHE ZEITSCHRIFT, 2013, 22 (06) :711-728
[3]   Mineralogy and factors controlling charge development of three Oxisols developed from different parent materials [J].
Anda, Markus ;
Shamshuddin, J. ;
Fauziah, C. I. ;
Omar, S. R. Syed .
GEODERMA, 2008, 143 (1-2) :153-167
[4]  
[Anonymous], 2014, ArcGIS Desktop Help 10.2 - GIS Dictionary
[5]  
[Anonymous], 2006, REMOTE SENSING DIGIT
[6]  
Birkeland P.W., 1999, Soils and Geomorphology, P1, DOI DOI 10.1016/S0169-555X(00)00019-2
[7]  
Bjornberg S., 1966, B SOC BRASILEIRA GEO, V15
[8]   Mapping soil organic matter in the Baranja region (Croatia): Geological and anthropic forcing parameters [J].
Bogunovic, Igor ;
Trevisani, Sebastiano ;
Pereira, Paulo ;
Vukadinovic, Vesna .
SCIENCE OF THE TOTAL ENVIRONMENT, 2018, 643 :335-345
[9]  
Caetano-Chang M. R., 2003, GEOCIENCIAS, V22, P33
[10]  
Carvalho A.M.V., 1954, B SOC BRASILEIRA GEO, V3