2015
DOI: 10.5897/ajar2015.9983
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Soil attributes in agricultural uses and in the Semiarid RN-Brazil in eutrophic Cambisol

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Cited by 3 publications
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“…According to the distribution of the particle size that shows the physical attributes of the profiles (Table 2), the highest clay contents in the surface layer were found in the profiles NFA1, NFA2, NFA3, and COA (Cambissolos Haplicos), ranging from 360 g kg -1 to 408 g kg -1 , and in the PPA (Neossolo Fluvico) (550 g kg -1 ), which is in an area of sediment deposition and groundwater oscillations and present sandy clay, and clay loam to clay textures. Souza et al (2015) evaluate physical and chemical properties of a Cambissolo Eutrofico under different agricultural uses in the Chapada do Apodi and found predominance of the clay fraction in areas with native forests, and Spondia sp., with similar values ranging from 373 to 478 g kg -1 . However, the clay fraction increased in depth, mainly in the Argissolo (CCA), presenting accumulation of clay of 422 g kg -1 in the 25-50 cm layer, denoting the evolution to a textural B horizon (Bt) formed by the pedogenic process of argiluviation ( Table 2).…”
Section: Physical Attributesmentioning
confidence: 99%
“…According to the distribution of the particle size that shows the physical attributes of the profiles (Table 2), the highest clay contents in the surface layer were found in the profiles NFA1, NFA2, NFA3, and COA (Cambissolos Haplicos), ranging from 360 g kg -1 to 408 g kg -1 , and in the PPA (Neossolo Fluvico) (550 g kg -1 ), which is in an area of sediment deposition and groundwater oscillations and present sandy clay, and clay loam to clay textures. Souza et al (2015) evaluate physical and chemical properties of a Cambissolo Eutrofico under different agricultural uses in the Chapada do Apodi and found predominance of the clay fraction in areas with native forests, and Spondia sp., with similar values ranging from 373 to 478 g kg -1 . However, the clay fraction increased in depth, mainly in the Argissolo (CCA), presenting accumulation of clay of 422 g kg -1 in the 25-50 cm layer, denoting the evolution to a textural B horizon (Bt) formed by the pedogenic process of argiluviation ( Table 2).…”
Section: Physical Attributesmentioning
confidence: 99%