2005
DOI: 10.14295/ras.v19i1.1352
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Análise De Bacia Aplicada Às Unidades Mesozóicas Do Triângulo Mineiro (Sudeste Do Brasil): Uma Estratégia Na Prospecção De Recursos Hídricos Subterrâneos

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Cited by 8 publications
(8 citation statements)
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“…The geology is mainly in the northeast portion of the Paraná Sedimentary basin, under the geological features of the Central Plateau, formed by the Uberaba formation (k2bub), Marília formation (k2bm), and Serra Geral formation (k1 delta sg) (Figure 3A), [44][45][46]. The soil is formed by organic and inorganic compounds, formed by horizons and change according to climatic influences in a pedological differentiation concerning the source material and the pedogenetic processes [46][47][48][49][50]. The soils were identified in three types, as can be seen in Figure 3B: Red Latosol (Oxisols), Red Yellow Latosol, and Red Yellow Argisol [48].…”
Section: Study Areamentioning
confidence: 99%
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“…The geology is mainly in the northeast portion of the Paraná Sedimentary basin, under the geological features of the Central Plateau, formed by the Uberaba formation (k2bub), Marília formation (k2bm), and Serra Geral formation (k1 delta sg) (Figure 3A), [44][45][46]. The soil is formed by organic and inorganic compounds, formed by horizons and change according to climatic influences in a pedological differentiation concerning the source material and the pedogenetic processes [46][47][48][49][50]. The soils were identified in three types, as can be seen in Figure 3B: Red Latosol (Oxisols), Red Yellow Latosol, and Red Yellow Argisol [48].…”
Section: Study Areamentioning
confidence: 99%
“…The soils were identified in three types, as can be seen in Figure 3B: Red Latosol (Oxisols), Red Yellow Latosol, and Red Yellow Argisol [48]. The geomorphology of the EPA of the Uberaba River basin is characterized by four compartments, which are identified by the tops of the Pediplano, the headwaters, smooth-wavy surface with the convex top, and wavy surface with the sharp top [44][45][46][47][48][49][50] (Figure 3C), occupying 11.13%, 6.56%, 66.68%, and 15.63% of the area, respectively. The main land use of land cover are: agriculture, forestry (eucalyptus), natural landscape (native forest), mining, and urban areas (Figure 3D).…”
Section: Study Areamentioning
confidence: 99%
“…O arcabouço hidrogeológico da área é representado pelo SAB que é um aquífero sedimentar com ocorrência nos estados de São Paulo, Minas Gerais, Paraná, Mato Grosso do Sul e Goiás, cobrindo uma área de aproximadamente 330.000 km² (Batezalli et al 2005 Devido às características geológicas do SAB em Minas Gerais, com intensa cimentação carbonática, as vazões de produção tendem a ser baixas, sendo seus poços somente utilizados para suprir pequenas demandas de até 20 m³/h. No Triângulo Mineiro, a espessura dessa unidade pode chegar a 180 metros na região de Iturama, com espessuras médias de 30 a 40 metros (Batezelli et al 2005).…”
Section: Caracterização Da áReaunclassified
“…O Sistema Aquífero Bauru (SAB) é um dos principais aquíferos do Brasil, com grande extensão territorial, entretanto, é muito pouco estudado na região do Triângulo Mineiro, sua área de ocorrência em Minas Gerais, com destaque para os trabalhos de Oliveira e Campos (2004); Batezelli et al (2005); Velásquez et al (2008), dentre outros. O SAB é um importante aquífero intergranular na região do Triângulo Mineiro, onde suas águas subterrâneas desempenham uma importante função estratégica na manutenção das vazões das drenagens na época de estiagem, exatamente devido ao fato de ser um aquífero livre, que lhe confere conexão hidráulica com os rios da região (Bertol et al 2006).…”
Section: Introductionunclassified
“…The eastern area limit encompasses part of the administrative region of the Alto Paranaíba (BATEZELLI et al, 2005;IBGE, 2016). The region landscape is characterized by tabular surfaces with gradual reduction of elevations to the west, varying between 750m and 350m.…”
Section: Study Areamentioning
confidence: 99%