2015
DOI: 10.20502/rbg.v16i3.765
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Estudo Das Coberturas Superficiais Na Interface Cerrado-Vereda No Norte De Minas Gerais

Abstract: Resumo:Embora sejam contempladas por pesquisas que abordam seus diversos aspectos naturais, com ênfase biológica, as veredas carecem de estudos sobre suas geocoberturas e das encostas associadas, incluindo os solos. Este estudo buscou analisar essas coberturas e suas relações com a dinâmica do canal fl uvial, tendo como área de investigação a vereda/rio Peruaçu, afl uente do Rio São Francisco, localizada no norte de Minas Gerais. Estudos dessa natureza podem elucidar mecanismos hidrogeomorfológicos presentes n… Show more

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Cited by 5 publications
(4 citation statements)
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“…The values are close to those Nascimento et al (2015) found in palm swamps around Uberlândia-MG. Similar results were also found in the Palm Swamps of Peruaçu State Park, west of Minas Gerais, by Neves et al (2015). In this area, the soils were acidic and dystrophic, both laterally and vertically.…”
Section: Description Of the Physicochemical Attributes In Soil Horizo...supporting
confidence: 82%
“…The values are close to those Nascimento et al (2015) found in palm swamps around Uberlândia-MG. Similar results were also found in the Palm Swamps of Peruaçu State Park, west of Minas Gerais, by Neves et al (2015). In this area, the soils were acidic and dystrophic, both laterally and vertically.…”
Section: Description Of the Physicochemical Attributes In Soil Horizo...supporting
confidence: 82%
“…4200 cal a bp , is characterised by clastic sediment input (coarse and fine sand, silt and clay). A sedimentological study conducted by Neves et al (2015) in palm swamps of northern Minas Gerais State, located ca. 70 km north of the Pandeiros wetland, identified that sediment remobilisation through the hillsides by superficial flows is the main source of clastic sediment input in the palm swamps.…”
Section: Discussionmentioning
confidence: 99%
“…Tal característica do relevo limita a prática de atividades agrícolas, assim como a pouca profundidade deste solo e presença de pedregosidade e rochosidade. Os afloramentos rochosos, que constituem tipos de terreno, não sendo classificáveis como solos, possuem um relevo bastante variado, desde plano até escarpado, com o predomínio daqueles acidentados: escarpado, montanhoso e forte ondulado (NEVES et al, 2015;GONÇALVES et al, 2017).…”
Section: Methodsunclassified