Sieve analysis studies depend on obtaining suspensions of fully-dispersed and stable samples to facilitate the quantification of the fractions of soil aggregates. The aim of this study was to compare the percentage of fractions obtained with four chemical dispersants and two methods of mechanical dispersion. To carry out this investigation, nine soils were selected from the departments of Cordoba and Sucre and four methodologies using chemical dispersions: ((NaPO3)6 + Na2CO3), (NaOH) 1M, (Na4P2O7) 0.1M pH 10, and CH3COONa 1M, and two methodologies of mechanical dispersion were evaluated: a slow one at 60 rpm for 6 hours and another at 4000 rpm for 15 minutes. The results were analyzed using a correlation test and contrasts. It was verified...
Abstract: Knowledge of the physical properties of soils, including the clay content, is of utmost im...
The use of dispersants in particle size analysis is a common practice, but this could cause bias on ...
A study has been made of the intensity of the forces binding soil particles together, when the soil ...
Sieve analysis studies depend on obtaining suspensions of fully-dispersed and stable samples to faci...
An adequate individualization of particles is required for a correct granulometric analysis in order...
The dispersion of the samples in soil particle-size analysis is a fundamental step, which is commonl...
The dispersion of the samples in soil particle-size analysis is a fundamental step, which is commonl...
Uma das condições essenciais para a realização da análise textural é a individualização completa das...
El fraccionamiento granulométrico de la materia orgánica (MO) se basa en que las fracciones asociada...
Knowledge of the soil physical properties, including the clay content, is of utmost importance for a...
O conhecimento a respeito das propriedades físicas do solo, incluindo os teores de argila é de suma ...
A method for the experimental determination of the amount of clay dispersed from soil into water is ...
The aim of this study was to evaluate the Bouyoucos method, at different stirring times and using tw...
The use of dispersants in particle size analysis is a common practice, but this could cause bias on ...
The purpose of dispersion is to destroy all aggregates without affecting the size of the individual ...
Abstract: Knowledge of the physical properties of soils, including the clay content, is of utmost im...
The use of dispersants in particle size analysis is a common practice, but this could cause bias on ...
A study has been made of the intensity of the forces binding soil particles together, when the soil ...
Sieve analysis studies depend on obtaining suspensions of fully-dispersed and stable samples to faci...
An adequate individualization of particles is required for a correct granulometric analysis in order...
The dispersion of the samples in soil particle-size analysis is a fundamental step, which is commonl...
The dispersion of the samples in soil particle-size analysis is a fundamental step, which is commonl...
Uma das condições essenciais para a realização da análise textural é a individualização completa das...
El fraccionamiento granulométrico de la materia orgánica (MO) se basa en que las fracciones asociada...
Knowledge of the soil physical properties, including the clay content, is of utmost importance for a...
O conhecimento a respeito das propriedades físicas do solo, incluindo os teores de argila é de suma ...
A method for the experimental determination of the amount of clay dispersed from soil into water is ...
The aim of this study was to evaluate the Bouyoucos method, at different stirring times and using tw...
The use of dispersants in particle size analysis is a common practice, but this could cause bias on ...
The purpose of dispersion is to destroy all aggregates without affecting the size of the individual ...
Abstract: Knowledge of the physical properties of soils, including the clay content, is of utmost im...
The use of dispersants in particle size analysis is a common practice, but this could cause bias on ...
A study has been made of the intensity of the forces binding soil particles together, when the soil ...