2005
DOI: 10.1590/s0100-06832005000200015
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Incremento da exatidão da análise granulométrica do solo por meio da coleta da suspensão (Silte + Argila)

Abstract: RESUMOA análise granulométrica do solo é realizada em três etapas: aplicação de pré-tratamentos para remoção de agentes cimentantes e floculantes, dispersão da amostra de solo e quantificação das frações do solo. Para quantificar as frações do solo, há necessidade de separá-las previamente. Dependendo do tamanho, utiliza-se o peneiramento, para as frações areia grossa e areia fina, e a sedimentação, para as frações silte e argila. Algumas propostas metodológicas calculam a proporção da fração silte no sistema … Show more

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Cited by 168 publications
(96 citation statements)
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“…For physical characterization, soil samples were collected at depths of 0.0-0.30 m and 0.30-0.60 m, for particle size analysis, using the pipette method and 0.1 mol L -1 of NaOH (Ruiz 2005). The clay fraction was separated by sedimentation, total sand by sieving, and silt was calculated based on the difference between them.…”
Section: Methodsmentioning
confidence: 99%
“…For physical characterization, soil samples were collected at depths of 0.0-0.30 m and 0.30-0.60 m, for particle size analysis, using the pipette method and 0.1 mol L -1 of NaOH (Ruiz 2005). The clay fraction was separated by sedimentation, total sand by sieving, and silt was calculated based on the difference between them.…”
Section: Methodsmentioning
confidence: 99%
“…A fração silte foi obtida por diferença entre duas pipetagens, sendo na primeira recolhido silte + argila e, na segunda, apenas argila, considerando o tempo de sedimentação segundo a equação de Stokes, levando-se em conta a densidade de partículas (Embrapa, 1997) de cada solo em estudo. As frações texturais foram calculadas conforme proposta apresentada por Ruiz (2005).…”
Section: Methodsunclassified
“…Physical and chemical soil properties are listed in table 1. Particle-size analysis was performed with the pipette method adapted by Ruiz (2005) and the C content determined by dichromate oxidation (Yeomans & Bremner, 1988); the total soil N was determined by the Kjehdal method; available P and exchangeable K were extracted by Mehlich-1; Ca, Mg and Al were extracted by 1 mol L -1 KCl and the pH measured in water, at a ratio of 1: 2.5. The P content was determined by colorimetry of the phosphomolybdic complex, as described by Braga & Defelipo (1974); K was determined by flame photometry; Ca and Mg by atomic absorption; and Al by titration (Defelipo & Ribeiro, 1981).…”
Section: Methodsmentioning
confidence: 99%