valoración física comparativa del muestreador uhland y el proctor en un suelo franco arenoso de sabana del estado monagas, venezuela comparative physical evaluation of uhland and proctor samplers on a sandy savanna soil in the state of monagas in venezuela

valoración física comparativa del muestreador uhland y el proctor en un suelo franco arenoso de sabana del estado monagas, venezuela comparative physical evaluation of uhland and proctor samplers on a sandy savanna soil in the state of monagas in venezuela

;Américo J. Hossne García;Omar Guerra
medical mycology journal 2013 Vol. 23 pp. 3-13
157
garca2013actavaloracin

Abstract

Es común la obtención de muestras de suelos agrícolas mediante el equipo Uhland. El ín­dice crítico de compactación del suelo se establece con la prueba Proctor. El objetivo fue la comparación física del muestreador Uhland, con caída libre y forzada del martillo, con el aparato Proctor para valorar la alteración mecánica de la muestra. Se utilizaron los Proctor estándar y modificado, el Uhland a caída libre y forzada del martillo, un diseño estadístico completamente aleatorizado con diez repeticiones y cuatro tratamientos, Análisis de Va­rianza, Mínima Diferencia Significativa y regresión polinómica. Se concluyó que el Uhland produjo resultados similares al Proctor. La energía penetrante del Uhland resultó superior a la compactante del Proctor. La humedad del suelo influyó sobre la densidad aparente seca. La relación de solidez y la porosidad aerífera identificaron mejor el proceso.


It is common to obtain agricultural soil samples using the Uhland sampler. The critical index of soil compaction is obtained with the Proctor test. The objective of this work was to perform a physical comparison between the Uhland sampler, with free and forced fall of the hammer, and the Proctor apparatus to assess mechanical alterations of the sample. Standard and modified Proctor instruments were used, as well as the Uhland with free and forced hammer fall. A completely randomized statistical design with ten replicates and four treatments was performed along with the analysis of variance, Minimum Significant Differ­ence and polynomial regression. It was concluded that Uhland and Proctor instruments pro­duced similar results. The penetrating energy of the Uhland was higher than the compacting energy of the Proctor. Humidity in the soil had an influence of the apparent dry density. The solidity ratio of the soil and the air porosity were the parameters that best identified the compaction process for the Proctor and Uhland instruments.

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