Genesis and transformation of basic rock-derived soils with shiny ped faces under tropical conditions

• Autor(a) principal: Marcos Gervasio Pereira
• Data de Publicação: 2022
• Outros Autores: Rafael Cipriano da Silva, Miguel Cooper, Lúcia Helena Cunha Dos Anjos, Deyvid Diego Carvalho Maranhão, Fábio Soares de Oliveira
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: Repositório Institucional da UFMG
• Texto Completo: http://dx.doi.org/10.36783/18069657rbcs20220028; http://hdl.handle.net/1843/59871; https://orcid.org/0000-0002-1402-3612; https://orcid.org/0000-0002-4392-0275; https://orcid.org/0000-0003-4922-4657; https://orcid.org/0000-0003-0063-3521; https://orcid.org/0000-0003-1709-3752; https://orcid.org/0000-0002-1450-7609
• topic: Pedogenesis; Soil classification; Ferralitization; Nitidization; Textural pedofeatures; Solos - formação; Solos - classificação

Soil evolves in landscapes in a natural process in which soil properties are gradually transformed. However, the transformation of argic to ferralic horizons in basic rock-derived soils under tropical conditions is poorly understood. Depending on the position of the soil profiles in landscape, evidence of pedogenetic transformation between different horizons might indicate the formation and destruction of aggregates with shiny faces. This study aimed to determine pedogenetic changes in basic rock-derived profiles in a toposequence, because soils derived from mafic rocks are not abundant in the study region (Pinheiral, Rio de Janeiro State, Brazil). Trenches were dug at the summit (P1), upper (P2), middle (P3), and lower (P4) thirds along the toposequence. The morphological, physical, chemical, mineralogical, and micromorphological properties of the profiles were characterized, and a weathering index was calculated from X-ray fluorescence element values. All profiles had chemical and physical properties indicating an advanced degree of weathering resulting from the parent material and tropical climate conditions. In P1 and P4 that were classified as Nitossolos, the most evident pedogenetic processes were ferralitization and nitidization, due to the advanced degree of weathering, accumulation of oxyhydroxides and kaolinite in the horizons, and formation of textural pedofeatures by mechanical-hydric stress and evidence of the illuviation process. Profiles P2 and P3 revealed a ferralitization process and were classified as Latossolos. Absence of shiny macromorphological ped faces in some Bw horizons, and their micromorphological coexistence in Bt and Bw horizons within the same profile were associated with the transformation of the blocky into a granular microstructure, suggesting argic-ferralic horizon transformation.