Abstract

Analyzing the soil near crop roots may reveal limitations to growth and yield even in a no-tillage system. The purpose of the present study was to relate the chemical and physical properties of soil under a no-tillage system to soybean root growth and plant yield after five years of use of different types of limestone and forms of application. A clayey Oxisol received application of dolomitic and calcitic limestones and their 1:1 combination in two forms: surface application, maintained on the soil surface; and incorporated, applied on the surface and incorporated mechanically. Soil physical properties (resistance to mechanical penetration, soil bulk density and soil aggregation), soil chemical properties (pH, exchangeable cations, H+Al, and cation exchange capacity) and plant parameters (root growth system, soybean grain yield, and oat dry matter production) were evaluated five years after setting up the experiment. Incorporation of lime neutralized exchangeable Al up to a depth of 20 cm without affecting the soil physical properties. The soybean root system reached depths of 40 cm or more with incorporated limestone, increasing grain yield an average of 31 % in relation to surface application, which limited the effect of lime up to a depth of 5 cm and root growth up to 20 cm. It was concluded that incorporation of limestone at the beginning of a no-tillage system ensures a favorable environment for root growth and soybean yield, while this intervention does not show long-term effects on soil physical properties under no-tillage. This suggests that there is resilience in the physical properties evaluated.

Highlights

  • The deleterious effects of acidity on soil chemical properties and plant productivity are well known in several agroecosystems, which justifies lime application on acid soils

  • Higher Ca contents were found in the calcitic limestone treatment than in the dolomitic limestone treatment and control, they were similar to Cal:Dol treatment in all depths

  • Regardless of the kind, is determinant for improving soil chemical quality, allowing for greater soil availability of Ca or Mg according to the composition of the lime; 2

Read more

Summary

Introduction

The deleterious effects of acidity on soil chemical properties and plant productivity are well known in several agroecosystems, which justifies lime application on acid soils. Either before NT or when the system is already consolidated, is generally performed periodically to eliminate soil reacidification (Rheinheimer et al, 2000; Caires et al, 2008). In this case the effects of soil amendment in depth are limited and dependent on the lime neutralization depth limits (Rheinheimer et al, 2000) and lime particle migration (Amaral et al, 2004). The neutralization rate depends on various factors, such as the lime application rate, soil type, the presence of compacted layers, environmental conditions and the amount of plant residues in the NT system, among others

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call