Abstract

The physical properties of soils are important for proper monitoring of soil functions. In order to evaluate soil resistance to agricultural equipment, a study was carried out on the four main soil types (ferralitic, ferruginous, hydromorphic and vertisol) in the eight agroecological zones of Benin. The objective of this work was to determine the physical and mechanical parameters of the soils. A sampling of soil types by agroecological zone was carried out in 36 localities in Benin to record vertical and horizontal soil strengths using a compactometer and a penetrometer. These data were complemented by measurements of texture, density and water content of the soil samples. Ananalysis of variance, polynomial regressions and Pearson correlation were performed between the parameters studied. It is noted that majority of soils assessed were sandy loam. The high sand content in most soils would be due to the depth considered (20 cm). The bulk densities range from 1.21 to 1.73gcm-3 and water contents from 4.9 to 35.11%. Vertical resistances range from 3.89 to 16.36 kg cm-2 and horizontal resistances from 1.03 to 4.44 kg cm-2. Strong soil resistances (vertical and horizontal) are recorded in the northern part of Benin where large proportions of the gravelswere observed in the samples taken. A positive correlation was observed between vertical resistance and horizontal soil resistance. It can be concluded that soil resistance in Benin vary from one agro-ecological zone to another, but the linking of soil properties is less significant between zones.Keywords: Soil compaction, soil resistance, penetrometer, agroecological zones, Benin

Highlights

  • Soil occupies a special position because of its agronomic and environmental functions in the preservation of natural resources

  • The presence of gravels were observed in most samples collected in agroecological zones of northern Benin

  • The results of this study showed a small variation in soil bulk density

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Summary

Introduction

Soil occupies a special position because of its agronomic and environmental functions in the preservation of natural resources. Soil compaction, characterized by reduction of macrospores, available water and productivity (Birkas et al 2008) can be evaluated by measuring soil density and penetrometer resistance When these properties exceed critical values, plant growth is severely restricted (Medeiros et al 2010). Experimental results studied variations of crop yield as a function of the level of subsidence of the surface horizons (Richard, 2008) but the influence of soil stress on the strength of agricultural equipment has been less studied. To study these constraints, two approaches could be adopted: laboratory methods or in situ methods. It is true that all intrinsic properties and mechanical parameters of soils are never known with a high degree of precision or reliability, because of the natural variability of the materials constituting the soil

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