Response of irrigated wheat cultivars to different nitrogen rates and sources
01/Oct/2009
High wheat yields require good N fertilization management. The objective of this study was to evaluate the effects of different N applications at sowing using Entec (N source with nitrification inhibitor) and urea (traditional N source) at covering, on four wheat cultivars. The experiment was conducted in a randomized block design in a factorial scheme, with four replications, at the Experimental Station of the Faculdade de Engenharia de Ilha Solteira – UNESP, on a dystrophic, epi-eutrophic alic Red Latosol with […]
The use of total luminescence spectroscopy in the investigation of the effects of different rice management practices on humic substances of a planosol
01/Oct/2009
In the Earth’s carbon cycle, C stocks in the soil are higher than in vegetation and atmosphere. Maintaining and conserving organic C concentrations in the soil by specific management practices can improve soil fertility and productivity. The aim of this study was to evaluate the impact of agricultural management techniques and influence of water regime (flooded or drained) on the structure of humic substances by excitation/emission matrix fluorescence. Six samples of a Planosol (Planossolo by the Brazilian System of Soil […]
Bulk density of an alfisol under cultivation systems in a long-term experiment evaluated with gamma ray computed tomography
01/Oct/2009
The sustainability of irrigated rice (Oryza sativa L.) in lowland soils is based on the use of crop rotation and succession, which are essential for the control of red and black rice. The effects on the soil properties deserve studies, particularly on soil compaction. The objective of this study was to identify compacted layers in an Albaqualf under different cultivation and tillage systems, by evaluating the soil bulk density (Ds) with Gamma Ray Computed Tomography (TC). The analysis was carried […]
Specific surface área and porosity of the clay fraction and phosphorus adsorption in two rhodic ferralsols
01/Oct/2009
The porosity of the clay fraction is very important for the understanding of the physicochemical phenomena which are relate to the specific surface area of solid particles. The specific surface area (SBET) and porosity of clay fractions of two Rhodic Ferralsols in the state of Mato Grosso do Sul, Brazil, natural kaolinite (KGa2), synthetic goethite (Gt) and hematite (Hm) were evaluated through adsorption and desorption isotherms of N2.. Results concerning SBET and particle porosity were related to the maximum P […]
Peat bogs in the Serra do Espinhaço Meridional – Minas Gerais, Brazil. II – influence of drainage on elemental humus composition and substances
01/Oct/2009
Peat bogs are Organosols formed under ideal ecological conditions in terms of the accumulation of organic material, controlled by geomorphological and geological processes and climate. The physical, chemistry and biological constitution of peat bogs is largely unknown. In this study the peat bogs of the Southern Serra do Espinhaço (Minas Gerais, Brazil) were described and sampled from three profiles at 1,250 m (P1), 1,350 m (P4) and 1,800 m (P2) above sea level. The three profiles were characterized morphologically, the […]
Rice growth as affected by combined ammonium and nitrate supply
01/Oct/2009
In rice cultivated under flooded conditions, the anaerobic condition favors the formation of NH4+ in the soil, and is therefore considered the main available N source for this crop. However, the process of O2 transport through the aerenchyma and its release by roots, create a favorable environment for nitrification in the plant rizosphere. Nitrification intensity determines the proportions between available NH4+ and NO3– . In this case, it is believed that the presence of NO3– can favor rice growth and […]
Growth and mineral nutrition of (Gliricidia sepium (Jacq.) Kunth ex Steud) seedlings in nutrient solution under saline stress
01/Oct/2009
Salinity is one of the most limiting factors to plant growth and development. Plant survival in saline environments depends on adaptive processes involving uptake, transport, and distribution of ions in plant organs. To evaluate growth and mineral nutrition of Gliricidia sepium seedlings under saline conditions, an experiment was carried out under nylon-mesh protection, at the Federal University of Campina Grande, in Patos – PB. Seeds were sown in pots containing Hoagland & Arnon nutrient solution with four NaCl levels (0, […]
Morphology and classification of luvisols and planosols developed on metamorphic rocks in semiarid northeastern Brazil
01/Oct/2009
The Semiarid Region of Northeast Brazil covers around 750,000 km2 and the Pre-Cambrian areas are dominated by shallow and poorly developed soils. According to the Brazilian System of Soil Classification the soils of the region are predominantly classified as Lithic Neosols, Luvisols and Planosols. This study aimed to characterize and classify 12 soil profiles in four toposequences representative of the common occurrence of Luvisolics in the Semiarid Region of Northeast Brazil by the Brazilian System of Soil Classification. Two sequences […]
Phosphorous forms in cultivated indian black earth (anthrosols) of varying texture in the brazilian Amazon
01/Oct/2009
Despite the agricultural importance of Indian Black Earth (IBE) in the Amazon region, there are few studies that report on the relation between soil texture and chemical fertility of IBE. These soils of pre-Colombian origin, with high contents of P, Ca and other nutrients are found across the Amazon valley. IBE profiles were studied to evaluate the total contents of P, its primary chemical forms and the P transformation phases in areas with IBE soils of variable texture and in […]
Chemical composition of soil solution in different soil pore classes
01/Oct/2009
The chemistry of the soil solution can be regarded as an indicator of the presence of nutrients or contaminants in the soil. To evaluate the variation of this chemical composition in the soil pores, a sequential system of extraction of the soil solution from the different soil pore classes was used. Soil columns were constructed and filled with air-dried fine soil of a Dystrophic Ultisol, and irrigated with: distilled water (T1), treated wastewater (T2) and treated wastewater + 1.2 g […]
