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Fertilization of grapevines with N is generally accomplished to supply the demand for N. However N should be used with prudence because affect the yield and chemical composition of the grape and your must. The experiment was carried out in 2004/05, to evaluate the effect of N fertilization on the grape yield and on the chemical composition of the grape and must of Cabernet Sauvignon grapevines, at Udorthent soil at Southern Brazil, Bento Gonçalves city. The treatments were control, 15, 30, 45 and 60kg ha-1 N, added during the vegetative and productive period. In the maturation, the grape was collected. Grape yield by plant and by hectare, length and width of bunches were evaluated and 100 berries were weighted. Berries were collected and a part of them was used to evaluate soluble solids in the must, pH, total acidity, tartaric acid, malic acid, total phenols, anthocyanins and N ammonia. The remaining berries were triturated and used to evaluated total N, P, K, Ca and Mg. The results showed that the yield of Cabernet Sauvignon grapevines in soils with medium content of organic matter is maximum with the fertilization of 15 and 30kg ha-1 N. The N fertilization increased the values of ammonia in the must and potassium percentage in the berry, but decreased the values of anthocyanins, what interferes the color of red wines and the formation of precipitate. [ABSTRACT FROM AUTHOR]

[Display omitted] • We investigated and quantified the phosphorus (P) fate in a cropping system. • After 8 years, total P inputs to a sandy soil were up to 2511 kg ha−1. • Vertical movement of P in soil was confined to the top 35 cm layer. • Mass balance indicated that 59–81% of P added was accumulated in the soil pool. • P accounted in grain and runoff were similar, while leaching was a minor P loss. Repeated phosphorus (P) inputs can lead to the accumulation of surplus P in soil with enhanced potential risk of transfer and accelerated eutrophication of aquatic environments. Intensive pork production in Rio Grande do Sul in southern Brazil results in the generation of large quantities of P-rich waste in the form of pig slurry, which is used to fertilise crops. The aim of this study was to assess and quantify the impact of repeated application of pig slurry P over 8 years (2000–2007) on the fate of P in a sandy loam soil maintained under a mixed cropping regime. In a replicated field trial, pig slurry was applied at three rates (20, 40, and 80 m3 ha−1), which resulted in cumulative P inputs over the 8-year period of 628, 1256, and 2511 kg P ha−1. Slurry inputs of 20, 40, and 80 m3 ha−1 resulted in the accumulation of 368, 936, and 2039 kg P ha−1 in soil to 60 cm, respectively. A combination of soil storage (59–81 %), crop removal (7–14 %), and total P transfer in surface runoff (5–15 %) accounted for most of the P applied in pig slurry over 8 years. Our results highlight the potential environmental impacts of runoff P losses in long-term waste-amended and intensively managed subtropical coarse-textured soils. Measures to minimise soil erosion and P transfers from land to water bodies are of utmost importance. [ABSTRACT FROM AUTHOR]