The traffic of agricultural machinery and soil compaction occur near the canopy of citrus trees, which increases soil physical restrictions to root growth. Soil management strategies include the use of permanent groundcover in the interrows of orange tree plantations, although the effects of these practices on the soil physical quality are largely unknown. The objective of this study was to assess the impact of groundcover management systems on some indicators of soil physical quality for orange tree orchards. The study […]

Soil structure (type, size and development) defines the total soil porosity and macro and microporosity distribution, and is considered to be one of the most important agricultural soil properties. The aim of this work was to study the effect of the clay fraction mineralogy, including the crystallographic mineral characteristics, in the soil physical properties of two Oxisols developed from the basaltic rocks, in different landscape positions (toposequence) in Paraná State, Brazil. With this objective, the soil profile was morphologically described […]

Agricultural machinery traffic may lead to a restrictive state of soil compaction for crop yields in no-tillage systems. This study was conducted at the University of Cruz Alta, in Cruz Alta, State of Rio de Janeiro, Brazil. The main objective was to evaluate the effects of soil management systems and compaction states on selected soil physical properties and on yield of six soybean cultivars. The experiment was conducted on an Oxisol with 427 g kg-1 of clay, prior under no-tillage. The experimental […]

The understanding and quantification of the impact caused by soil use and management on the physical soil quality are fundamental for the development of sustainable agricultural systems. The objective of this research was to quantify some physical soil properties to evaluate the physical quality of a dystrophic Red Latosol (Rhodic Ferralsol) in the northwest of the State of Paraná, Brazil. Undisturbed soil samples were collected from two contiguous areas on an Experimental Farm of the State University of Maringá. One […]

The soil water retention curve plays a fundamental role in the development of studies on the dynamics of soil water, modeling of physical soil processes and plant growth. The retention curve is usually obtained by simultaneously measuring water content (θ) and soil water potential (ψ) in a single sample. An alternative procedure is to use several samples per ψ to describe the retention curve. The use of this procedure requires that the variation factors which exist among the samples are […]

The porosity characteristics of a Red-Yellow Podzolic was evaluated after 10 years of cultivation, under the following soil management treatments: no-tillage, moldboard plowing + disking, disk plowing + disking, off-set disk harrowing followed by moldboard plowing + disking, off-set disk harrowing followed by disk plowing + disking and off-set disk harrowing followed by disking. Undisturbed 15 cm high and 15 cm deep soil blocks, were sampled for morphometric analysis of the soil porosity. Results indicated the presence of surface sealing […]

The study of the effects of soil tillage systems on some physical and chemical properties of a Typic Paleudal and on cassava yield (Manihot esculenta, Crantz) was carried out in the northwest of the state of Paraná, Brazil in 1994/95 and 1996/97. Three soil tillage systems were used: (a) no-tillage; (b) minimum tillage (field cultivator and disc harrowing); and, (c) conventional tillage (mouldplowing and disc harrowing). A randomized complete block experimental design with six replications was used. Higher macroporosity values in the 0.10 m […]

Aiming to evaluate the influence of the clay fraction mineralogy on the physical properties of Latosols (Oxisols) from southeastern Brazil, seven Latosols, representative of this group, were selected from the states of Minas Gerais and Espírito Santo, having distinct morphological features associated with soil structure. The sampling of soils was performed in the latossolic B horizon, with disturbed and undisturbed samples being collected. Chemical, physical and mineralogical characterizations were performed in the laboratory. Regression and correlation analyses taking into account […]