Rheological Parameters as Affected by Water Tension in Subtropical Soils
06/Jun/2016
ABSTRACT Rheological parameters have been used to study the interaction between particles and the structural strength of soils subjected to mechanical stresses, in which soil composition and water content most strongly affect soil resistance to deformation. Our objective was to evaluate the effect of water tension on rheological parameters of soils with different mineralogical, physical, and chemical composition. Surface and subsurface horizons of four Oxisols, two Ultisols, one Alfisol, and one Vertisol were physically and chemically characterized; their rheological parameters […]
Quantification of the least limiting water range in an oxisol using two methodological strategies
01/Dec/2014
The least limiting water range (LLWR) has been used as an indicator of soil physical quality as it represents, in a single parameter, the soil physical properties directly linked to plant growth, with the exception of temperature. The usual procedure for obtaining the LLWR involves determination of the water retention curve (WRC) and the soil resistance to penetration curve (SRC) in soil samples with undisturbed structure in the laboratory. Determination of the WRC and SRC using field measurements (in situ […]
Soil resistance to penetration and forage and root production at different grazing intensities
01/Jun/2012
Soil fertilization may be a sustainable strategy for the intensification of grazing, considering that the effects of cattle trampling that are deleterious for the soil physical quality do not affect the productivity and the sustainability of pasture production systems. The purpose of this study was to evaluate the effect of grazing at different intensities of N-fertilized pasture on the soil physical quality and impact on forage and root yield of Panicum maximum cv. IPR-86 Milênio. The experiment was conducted in […]
Modeling the water retention curve in Oxisols using the Double Van Genuchten Equation
01/Feb/2011
The clay fraction mineralogy and the granular structure of Oxisols in the Cerrado (Brazilian savanna) are the reason for the great volume of large pores as well as of extremely small pores, but no significant medium pore volume, resulting in low available water for plants. This study aimed to characterize and model the behavior of water retention in Oxisols with different texture classes of the Cerrado region. Samples were collected from the Bw horizon of 10 Oxisols under native vegetation. […]
Influence of sampling type on the dielectric constant and calibration of TDR probes
01/Apr/2010
The technique of TDR (time-domain reflectometry) is an important tool for the study of soil water content. For a correct use of this technique, models that relate the volumetric water content in soil with the soil dielectric constant must be calibrated, considering the characteristics of each soil. The purpose of this study was to evaluate the influence of soil type and sampling form (disturbed and undisturbed samples) on the dielectric constant (Ka) of the soil and the performance of models […]
Soil compaction and yield of corn hybrids in an oxisol. II – least limiting water range and root system
01/Aug/2009
The objective of this study was to evaluate, under field conditions, in Colina-SP, Brazil, the response of two corn cultivars to six soil compaction levels of an Oxisol regarding the root system development, and to characterize soil compaction by the least limiting water range (LLWR). The experiment was arranged in a randomized complete block design, with strip plots and four replications. The corn hybrids DKB 390 and DAS 2B710 were used. After corn sowing, undisturbed soil samples were collected to determine physical […]
Soil compaction and yield of corn cultivars in an oxisol: I – plant characteristics, soil and S index
01/Aug/2009
The purpose of this study was to evaluate, under field conditions, in Colina-SP, Brazil, the response of two genetically different corn cultivars to six compaction levels of an Oxisol. The experiment was arranged in a randomized complete block design, with strip plots and four replications. The corn hybrids DKB 390 and DAS 2B710 were used. After corn seeding, non-deformed soil samples were collected from the layers 0-0.10, 0.10-0.20 and 0.20-0.30 m to determine soil physical properties and the S index. At the seed […]
Least limiting water range to evaluate soil compaction and physical quality of an oxisol cultivated with soybean
01/Dec/2007
Soil physical quality is essential for plant growth and sustainable agricultural systems. This study aimed to evaluate the efficiency of the least limiting water range (LLWR) to monitor soil compaction and soil physical quality for soybean, without and with irrigation. The study was carried out in an clayer Red Latosol (Oxisol) (21 ° 14 ‘ 53 ” S; 48 ° 17 ‘ 20 ” W; 540 m asl). The experiment was entirely randomized, in a 6 x 2 factorial scheme, with four repetitions. The compaction treatments were: T1 = without compaction; T2 = 1 pass of a 4 t […]
Effect soil compaction on root growth and maize yield
01/Aug/2007
The structural soil modifications caused by different tillage systems can result in more or less intense compaction, which interferes with soil penetration resistance, bulk density and porosity, influencing root growth and crop yields. The objective of this work was to evaluate the effect of compaction on particular characteristics of a Red Latosol and associate them with root growth and maize yield. The main treatments consisted of six compaction levels, induced by controlled tractor traffic and the secondary treatments of two […]
Exploratory analysis and variability of hydraulic conductivity equation parameters, in an instantaneous profile experiment
01/Apr/2006
In agriculture and environmental studies, the hydraulic conductivity equation, that is, the hydraulic conductivity (K) as a function of soil-water content (q), plays an important role in the resolution of practical problems related to irrigation, drainage, and leaching of nutrients and pollutants. In order to quantify and characterize this hydric soil property it is essential to obtain representative values that can be safely used in a number of applications. With the objective of characterizing the statistical behavior and of quantifying […]