Abstract

Abstract: The objective of this work was to evaluate the effect of different farm systems on clay dispersion and its relationship with soil chemical properties and the no-tillage system participatory quality index (IQP), in watershed areas in the west of the state of Paraná, Brazil. The farm systems evaluated were: no-tillage; no-tillage with crop succession; no-tillage with soil disturbance; and conventional system. In addition, the farm systems were evaluated for their IQP. Soil samples were collected at 0.0-0.20-m soil depth, in 40 agricultural areas and in 6 native forests considered as references. The degree of clay dispersion, total organic carbon, pH (CaCl2), exchangeable potassium (K+), available phosphorus (P), exchangeable calcium and magnesium (Ca2++Mg2+), and potential acidity (H+Al3+) were determined. A linear multiple regression model was fitted by the method of least squares. The averages of clay dispersion degree per watershed were compared at 5% probability. The farm systems were compared by Scott-Knott’s test. Soil chemical properties showed a higher influence on clay dispersion than the different farm systems assessed. The no-tillage system alone showed the highest content of organic carbon, which was similar to those of the native areas. The conventional system and the no-tillage system with soil disturbance showed a lower IQP and a higher degree of clay dispersion than the areas with the no-tillage system alone. The IQP allows distinguishing the conventional system from the no-tillage system.

Highlights

  • The use of the soil and its management change the agricultural productivity and sustainability

  • All evaluated areas have their soil with heavy clay, except for one area, which fits into a clay textural class (FAO, 1988)

  • There was a significant difference for clay dispersion (CD) in the two areas evaluated in the Sanga Mineira watershed between the no-tillage with crop succession (NT) and no-tillage with soil disturbance (NTD) farm systems

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Summary

Introduction

The use of the soil and its management change the agricultural productivity and sustainability. Together with other soil properties, waterdispersible clay is used to understand the stability of the soil microstructure and its relationship with erosive processes (Igwe & Obalum, 2013), since the released particles can clog the pores, reducing the water flows and gases (Chaves et al, 2001; Nguetnkam & Dultz, 2014). These particles are transported in flowing streams to waterbodies (Demarchi & Zimback, 2014), favoring their contamination (Martin et al, 2015). It is not always completely implemented, which results in the reduction of its benefits as a conservation practice (Silva et al, 2014)

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