Soybean and eucalyptus response to increased soil density and phosphorus doses
01/Aug/2010
Agriculture and soil management in the Cerrado can cause soil compaction, resulting in decreased porosity and water and nutrient availability, with a negative impact on plant growth and development. The objective of this study was to evaluate the effect of soil density and phosphorus doses (P) on soybean and eucalyptus grown in two Cerrado oxisols with different texture: one (LV) with 610 g kg-1 clay and the other (LVA), with 190 g kg-1 clay. Three soil densities (0. 90, 1. 10 and 1. 30 Mg m-3) […]
Availability of a soluble phosphorus source applied to soil samples with different acidicity levels
01/Aug/2010
Considerations on the interactions of P in the soil-plant system have a long history, but are still topical and not yet satisfactorily understood. One concern is the effect of liming before or after application of soluble sources on the crop yield and efficiency of available P under these conditions. The aim of this study was to evaluate the effect of soil acidity on availability of P from a soluble source, based on plant growth and chemical extractants. Nine soil samples […]
Effect of El Niño/Southern Oscillation on rainfall erosivity in Santa Maria (RS)
01/Aug/2010
El Niño/Southern Oscillation (ENSO) affects the weather and climate of several locations, causing changes in the atmospheric circulation and climate variables, mainly rainfall, in all regions of Brazil. In southern Brazil, during El Niño years (the positive phase of ENSO), rainfall is often above normal whereas during La Niña years (the negative phase of ENSO), rainfall is often below normal. Some rainfall properties are affected by ENSO, such as frequency, intensity and amount. These properties are important to define erosive rainfall events. […]
Use of spatial representation to calculate the topographic factor in the revised universal soil loss equation in watersheds
01/Aug/2010
Methods of spatial representation to calculate the topographic factor (LS) of the Revised Universal Soil Loss Equation (USLE) have been used to estimate soil erosion and sediment yield of watersheds. These procedures are based on equations traditionally used to determine the LS factor and information that characterize the hillslope forms and processes, derived from the Digital Elevation Model (DEM). Two computational methods commonly used to calculate LS factor in soil erosion and sediment yield models were analyzed in this study. […]
Maximum phosphorus adsorption capacity as related to iron and aluminum forms in subtropical soils
01/Aug/2010
Phosphorus is among the macronutrients the least absorbed by plants. Nevertheless, the amount of P-containing fertilizers applied to humid tropical and subtropical soils in relatively high. The reason is the strong interaction between of P and Fe and Al oxides, which are abundant in these soils. The study of these interactions is fundamental to know more about the relations between phosphorus adsorption and soil constituents. The objective of this study was to evaluate how the minerals in the clay fraction, […]
Physical properties of a typic paleudalf under long-term no-tillage and cropping systems
01/Aug/2010
No-tillage associated to cover crops may maintain soil quality, improving or preserving favorable soil physical conditions for plant growth. This study assessed soil bulk density, porosity, penetration resistance, and water infiltration of a PALEUDALF, in the Experimental Area of the Soil Science Department of the Federal University of Santa Maria, in Santa Maria, RS, Brazil, in an experiment started in 1991, with the following crop successions and rotations: (1) Corn/Soybean – Jackbean – MFP; (2) Bare soil – SDES; (3) […]
Soil characterization along a climatic gradient in the triunfo mountain range, semi-arid region of pernambuco state, Brazil
01/Aug/2010
Highland forests in mountains of Northeast Brazil are islands of humid Atlantic forest in the midst of the semi-arid region. The climatic conditions are rather atypical, improved by the occurrence of orographic rainfall, which can reach 1,200 mm per year. In the state of Pernambuco, most of the scientific studies in these humid highland forests are focused on botanical and zoological aspects only, with very little information about soils. Aiming to study the soils of the humid mountains in the semi-arid […]
Soil genesis and classification in the environment “mar de morros” in the mid-valley of the river Paraiba do Sul, RJ
01/Aug/2010
Brazilian tropical soils are generally regarded as highly weathered, which is attributed to the climatic conditions (high temperatures and rainfall). However, in the “Mar de Morros” environment the intensity of pedogenic processes can be affected by the erosional removal of material, due to the hilly relief, which rejuvenates the surfaces. The objective of this study was to characterize and classify soil profiles in a toposequence developed from muscovite-biotite gneiss, located in the municipality of Pinheiral (Rio de Janeiro State). The […]
Contribution of humic substances from different composts to the synthesis of humin in a tropical soil
01/Aug/2010
The contribution of humic substances of different composts to the synthesis of humin in a tropical soil was evaluated. Increasing doses (0, 13, 26, 52, and 104 Mg ha-1) of five different composts consisting of agroinpowderrial residues were applied to a Red-Yellow Latosol. These composts were chemically characterized and 13C NMR determined and the quantity of the functional alkyl groups of humic acids applied to the soil as compost was estimated. Thirty days after application of the treatments, organic matter samples were […]
Relations of sediment delivery underlying payments for environmental services in catchment areas
01/Aug/2010
Because of its simplicity, the sediment delivery ratio (SDR), based on the ratio of the sediment yield (Y) and the gross erosion (E) in the basin, is widely used to estimate sediment production in watersheds. Since Y and E are complexly linked, several SDR equations were developed. Financial compensation programs resulting from sedimentation abatement, such as the Water Provider Program, often require the estimation of reduction of the downstream sediment yield as a function of erosion reduction upstream. This study […]
