Abstract

Soil compaction and fertilization affect soybean development. This study evaluated the effects of soil compaction and fertilization on soybean (Glycine max cv. Embrapa 48) productivity in a Typic Haplustox under field conditions in Jaboticabal, SP, Brazil. A completely randomized design with a 5 x 2 factorial layout (compaction vs. fertilization), with four replications in each treatment, was employed. Each experimental unit (replicate) consisted of a 3.6 m² useful area. After the soil was prepared by cultivation, an 11 Mg tractor passed over it a variable number of times to create five levels of compaction. Treatments were: T0= no compaction, T1= one tractor pass, T2= two, T4= four, and T6= six passes, and no fertilizer and fertilizer to give soybean yields of 2.5 to 2.9 Mg ha-1. Soil was sampled at depths of 0.02-0.05, 0.07-0.10, and 0.15-0.18 m to determine macro and microporosity, penetration resistance (PR), and bulk density (Db). After 120 days growing under these conditions, the plants were analyzed in terms of development (plant height, number of pods, shoot dry matter per plant and weight of 100 seeds) and seed productivity per hectare. Soil compaction decreased soybean development and productivity, but this effect was decreased by soil fertilization, showing that such fertilization increased soybean tolerance to soil compaction.

Highlights

  • Since the 1970s, investments in studies on the genetic improvement of cultivars, fertilizers and pesticides for soybean production in Brazil have increased and improved productivity

  • Soil compaction usually has been evaluated from traits such as porosity, bulk density (Db) and penetration resistance (PR) (Tormena et al, 2002; Silva et al, 2004)

  • PR is directly related to root growth (Letey, 1985) and has been preferred as an indicator for soil compaction

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Summary

Introduction

Since the 1970s, investments in studies on the genetic improvement of cultivars, fertilizers and pesticides for soybean production in Brazil have increased and improved productivity. The demand for studies on the effects of soil compaction on soybean has increased since negative effects on yield have been shown (Hakansson & Voorhees, 1998; Ralisch & Tavares Filho, 2002). PR is directly related to root growth (Letey, 1985) and has been preferred as an indicator for soil compaction. Considering these soil parameters, critical values have been determined for adequate root growth such as: aeration porosity = 10% (Gupta & Allmaras, 1987), Db = 1.55 Mg m-3 for clay loam soils Agric. (Piracicaba, Braz.), v.61, n.6, p.626-631, Nov./Dec. 2004

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