Abstract

The physical properties and fertility of the soil are important factors in the formation and establishment of pasture. Changes in physical properties affect the movement of water, air, nutrients and roots, which, in turn, affect the productivity and longevity of pastures. The objective of this study was to evaluate the physical properties of the soil and the dry matter yield of a pasture with signalgrass cv. Basilisk (Brachiaria decumbens cv. Basilisk), fertilized with increasing nitrogen doses (N), on a dystrophic Red-Yellow Latosol. The experiment was conducted on the Fazenda Rio Manso of the Universidade Federal dos Vales do Jequitinhonha e Mucuri, in Couto de Magalhães de Minas, State of Minas Gerais, Brazil. To evaluate the annual forage yield, a split plot scheme in a randomized block design with four replications was used, with N doses (0, 50, 100, 150, and 200 kg/ha/year) in the plots and growing seasons (first and second) in the subplots. For soil evaluation, a split plot scheme was used with N doses (0, 25, 50, 75 and 100 kg/ha/cut) in the plots and three sampling times (prior to the experiment, at the end of the first growing season and at the end of the second growing season) in the subplots in a randomized block design with four replications. This analysis was performed separately at two soil depths (0-3 and 10-13 cm). Forage samples were analyzed for the annual dry matter yield (DMY), and soil samples were analyzed for pre-consolidation pressure (σp), initial soil bulk density (Bd), total pore volume (TPV) and void index (Vd). Higher nitrogen doses increased the dry matter yield of signalgrass pasture and the pre-consolidation pressure of the soil. The total pore volume and void index decreased, and the initial soil bulk density increased, though without promoting soil compaction.

Highlights

  • The physical properties and fertility of the soil are important factors involved in the formation and establishment of pasture

  • The results of dry matter yield for signalgrass are shown in table 4

  • Reductions in the P levels were observed; these reductions may be related to a higher extraction of soil P in the second year resulting from the higher production of plant dry matter (Table 4)

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Summary

Introduction

The physical properties and fertility of the soil are important factors involved in the formation and establishment of pasture. Changes in physical properties affect the movement of water, air, nutrients and roots growth, which, in turn, influence the productivity and longevity of pastures. The low productivity and quality of the forages and the degradation of large pasture areas due to improper management of grazing and fertilization are partly responsible for this situation (Costa et al, 2008). Soil compaction can result in a reduction in the productivity and longevity of pastures (Imhoff et al, 2000) and accelerate erosion processes (Oliveira et al, 2004)

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