6 results

Effect of conservation practices on soil moisture and maize (Zea mays L.) cropping in the semi-arid northeast of Brazil

Tatyana Keyty de Souza Borges, Abelardo Antônio de Assunção Montenegro, Thaís Emanuelle Monteiro dos Santos, Demetrius David da Silva, Valdemir de Paula e Silva Junior

01/Dec/2014

The Brazilian semi-arid region has limited production capacity, due to its intrinsic characteristics in relation to vegetation, climate, and soil. Soil cover, a recommended practice for this region, increases infiltration, providing for better use of rainwater, and contributing to crop development by reducing water loss through runoff. In this context, the aim of this study was to evaluate the effects of different types of soil cover in maintaining soil moisture under natural rainfall conditions, as well as to evaluate the […]

Time-space analysis of water balance components in an Oxisol

Neilo Bergamin Moreira, Paulo Leonel Libardi, Monica Martins Silva Salvador, Helon Hébano de Freitas Sousa

01/Feb/2014

Monitoring the variables that constitute the soil water balance equation in a farmed field is important for reliably evaluating water deficit periods during the crop cycle, managing irrigation and estimating nutrient losses through leaching. Components of the water balance equation may vary in space and time, and the study of the temporal stability of the spatial variability of these components is essential for determining the observation points in the field (sites) for monitoring soil moisture accurately with reduced effort in […]

Spatial and temporal evaluation of gravimetric and volumetric water storage in an Oxisol under citrus

Dolorice Moreti, Paulo Leonel Libardi, Genelício Crusoé Rocha, Márcio José Lovatti, Laura Ianello Giassetti Aguiar

01/Dec/2007

Temporal stability is described as the temporal persistence of a spatial pattern and is evaluated through correlation analysis of successive measurement data. In this study, the soil water storage was evaluated along two 76 m transects, each of them sampled at 20 points. The soil is an Oxisol (Yellow Red Latosol) under an 11- year-old citrus orchard, in Piracicaba-SP, Brazil. Soil water content, for the calculation of soil water storage in the layer 0.0-1.10 m, was obtained from weekly neutron probe readings at […]

Actual evapotranspiration of a productive orange plantation on an Oxisol in southeastern Brazil

Antonio Carlos Rodrigues Cruz, Paulo Leonel Libardi, Genelício Crusoé Rocha, Laércio Alves de Carvalho

01/Oct/2005

Water and nutrient availability in the soil at suitable times and in adequate amounts, as related to edaphic and climatic conditions, are undeniably relevant for crop yields. The objective of this work was to evaluate the actual evapotranspiration of an orange plantation, analyze its variability and verify the influence of the soil water loss on crop productivity. The experiment was carried out in Piracicaba County (SP), Brazil, on an Oxisol. The actual evapotranspiration was evaluated by a soil water balance […]

Temporal stability of the spatial distribution of water storage in a soil under citrus cultivation

Genelício Crusoé Rocha, Paulo Leonel Libardi, Laércio Alves de Carvalho, Antônio Carlos Rodrigues Cruz

01/Feb/2005

The objective of this work was to quantify and characterize the spatio-temporal variability and the temporal stability of water storage in a yellow Latosol under citrus cultivation. The experimental plot was installed on a soil under a 10 years old citrus crop, consisting of 40 observation points along two transects in a 4 m x 7 m spacing, that is, two parallel transects 1 and 2 (two plant rows) spaced 7 m with 20 points each 4 m apart, encompassing a 80 x 14 m land area (40 plants). Each point […]

Parameter variability of the equation relating hydraulic conductivity to soil water content using the instantaneous profile method

Q. de Jong van Lier, P. L. Libardi

01/Dec/1999

Hydraulic conductivity is one of the most important soil properties for studies dealing with infiltration, water movement within the soil profile and to plant roots and internal drainage. The availability of the function hydraulic conductivity x soil water content (K(θ)) is essential to these studies. However, little is known about the variability of the empirical parameters of this function. Aiming to contribute with information on the variability of these parameters, a study is described in which observations of hydraulic conductivity […]