Assessment of pedotransfer functions for estimating soil water retention curves for the amazon region
01/Jun/2014
Knowledge of the soil water retention curve (SWRC) is essential for understanding and modeling hydraulic processes in the soil. However, direct determination of the SWRC is time consuming and costly. In addition, it requires a large number of samples, due to the high spatial and temporal variability of soil hydraulic properties. An alternative is the use of models, called pedotransfer functions (PTFs), which estimate the SWRC from easy-to-measure properties. The aim of this paper was to test the accuracy of […]
Least limiting water range for the assessment of soil physical degradation
01/Dec/2013
The effects of soil use and management on soil physical quality have been largely discussed due to its environmental and agronomic impacts. The least limiting water range (LLWR) is a modern indicator of soil physical quality that can indicate processes and mechanisms linked to soil physical degradation caused by soil use and management. The aim of this work was to quantify the influence of different land uses and soil tillage on the LLWR of an Oxisol (170, 40 and 790 […]
Least limiting water range in a typic haplorthox after the first continuous grazing period of brachiaria ruziziensis in integrated crop-livestock system
01/Jun/2013
The least limiting water range (LLWR) is one of the best indicators of soil physical quality in intensive production systems. The objective of this study was to evaluate the physical quality of a Typic Haplorthox by the LLWR after three crop growing seasons and the first year of crop-livestock integration in Xambrê, northwestern Paraná, Brazil. The experiment was established in a randomized block design with three replications. Treatments consisted of four brachiaria heights before grazing (0.10; 0.20; 0.30, and 0.40 […]
Influence of soil bulk density in a dystroferric red ultisol moisture estimated by time domain reflectometry
01/Oct/2011
Among the techniques for soil moisture evaluation, the use of Time Domain Reflectometry (TDR) stands out, which consists of an indirect, non-destructive, fast and accurate method less dependent on environmental factors. However, works carried out after its applications suggest the influence of factors related to soils structural and mineralogical characteristics, which makes necessary the site calibration for the TDR proper functioning. The aim of this work was to study the influence of bulk density (Ds) on the volumetric soil water […]
Least limiting water range in soil under crop rotations and chiseling
01/Jun/2011
Soil water availability to plants is affected by soil compaction and other variables. The Least Limiting Water Range (LLWR) comprises soil physical variables affecting root growth and soil water availability, and can be managed by either mechanical or biological methods. There is evidence that effects of crop rotations could last longer than chiseling, so the objective of this study was to assess the effect of soil chiseling or growing cover crops under no-till (NT) on the LLWR. Crop rotations involving […]
Physical-hydric attributes of an oxisol from the cerrado region under coffee plantation as affected by the sampling position
01/Dec/2008
The soil compaction, induced by different traffic intensities, can cause damage in the soil structure, reducing the coffee plantation production. The objectives of this study was to develop a model of load support capacity for a Red Latosol (Oxisol) under Cerrado and under coffee and to investigate the effect of coffee plantation management on soil pore distribution and soil water retention, in different sampling positions in the coffee plantation. The stud site is located at 18 º 59 ‘ 15 […]
Physiological responses of orange trees to permanent groundcover vegetation types
01/Jun/2008
The presence of a groundcover in-between tree rows in orange orchards can affect the water uptake and physiology of the orange trees. The objective of this study was to characterize the relationships between the physiological variables of orange leaf and soil water content in a Paleudults in groundcover management systems with bahiagrass (Paspalum notatum), leguminous perennial peanut (Arachis pintoi) and spontaneous vegetation. The study was performed in in an experimental “Pêra” orange orchard established in 1993 in Alto Paraná, northwestern […]
Quantifying soil physical degradation through the soil penetration resistance curve
01/Jun/2008
Soil resistance to penetration (PR) frequently reduces plant root growth. PR increases with soil bulk density (Bd) and decreases with soil moisture (θ), and the mathematical description of the relationships of PR with Bd and θ determines the soil penetration resistance curve (SRC). The objective of this study was to quantify the SRC of an Oxisol under different land use practices and to use it to describe soil physical degradation. Four areas were selected: (a) native forest; (b) pasture cultivated […]
Criteria for pot capacity determination
01/Feb/2008
The field capacity, or its equivalent for soils in pots, the “pot capacity”, is an important parameter for irrigation management. We aimed to determine both water content and water loss as a function of time in pots filled with material of a clayey and a medium-textured soil. From these data the pot capacity water content was estimated using different criteria. It was concluded that the final water content extrapolated from the observed q-t curve is a good estimator of the […]
Vertical and horizontal spatialization of quality indicators of a typic haplortox under citrus
01/Feb/2007
The objective of this report was to verify the form of vertical and horizontal spatialization of chemical, physical and water quality indicators of a Typic Haplortox cultivated with citrus. The ‘Valencia’ orange grove on ‘Rangpur’ lime was planted in 1995, in the county of Alto Paraná, northwestern Paraná, Brazil. In August 2002, undisturbed and disturbed samples were collected for chemical, physical and water analysis. Twenty-four transects were sampled perpendicular to the tree trunk, in two layers (0-0.20 and 0.20-0.40 m depth) […]
