991 resultados para available phosphorus


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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Pós-graduação em Zootecnia - FMVZ

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Padrões de dispersão de nutrientes em terra preta Amazônica (TPA) podem dar informações sobre atividades antrópicas dos habitantes da Amazônia. Estudos sobre pH, fósforo disponível (P), matéria orgânica (MO) e os cátions trocáveis, Ca2+ e Mg2+, foram realizados em amostras de solos dos horizontes A1 e A2 ao longo de uma área com TPA (norte-sul e leste-oeste) em um sítio arqueológico denominado Ilha de Terra, na Unidade de Conservação Floresta Nacional de Caxiuanã, Município de Melgaço, Brasil. Os resultados indicaram que a MO e o Ca são os que apresentam maior dispersão. Correlações mais elevadas foram encontradas entre OM-Ca-Mg às proximidades da área central e levam a inferir que a dispersão geoquímica de MO, Ca, Mg e P em sítios arqueológicos com TPA está relacionada com atividades humanas pregressas.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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504 (five hundred four) 1 day old male chicks from a commercial broiler line (Ag Ross 308) were used, distributed in 12 treatments, with 6 replicates per treatment. The experimental design was casually blocked and treatments were organized in a 2x2x3 factorial arrangement: two available phosphorus levels (0.45 and 0.34%), two phytase inclusion levels (0 and 1200 FTU/kg) and three crude protein levels (22.5; 20.5 and 18.5%). Tibia calcium percentage was influenced by protein and phosphorus levels in the diet, when using phytase. Tibia ash levels showed a linear effect when enzymes were added and showed a quadractic effect without it, and the higher value was observed with 22.5% crude protein in the diet. With higher phosphorus levels a linear effect was observed between crude protein in the diet and tibia ash weights, as a higher protein level had lower tíbia ash weight.

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Soil CO2 emission (F-CO2) is influenced by chemical, physical and biological factors that affect the production of CO2 in the soil and its transport to the atmosphere. F-CO2 varies in time and space depending on environmental conditions, including the management of the agricultural area. The aim of this study was to investigate the spatial variability structure of F-CO2 and soil attributes in a mechanically harvested sugarcane area (green harvest) using fractal dimension (D-F) derived from isotropic variograms at different scales (fractograms). F-CO2 showed an overall average of 1.51 mu mol CO2 m(-2) s(-1) and correlated significantly (P < 0.05) with soil physical attributes, such as soil bulk density, air-filled pore space, macroporosity and microporosity. Topologically significant DF values were obtained from the characterization of F-CO2 at medium and large scales (above 20 m), with values of 2.92 and 2.90, respectively. The variations in D-F with scales indicate that the spatial variability structure of F-CO2 was similar to that observed for soil temperature and total pore volume and was the inverse of that observed for other soil attributes, such as soil moisture, soil bulk density, microporosity, air-filled pore space, silt and clay content, pH, available phosphorus and the sum of bases. Thus, the spatial variability structure of F-CO2 presented a significant relationship with the spatial variability structure for most soil attributes, indicating the possibility of using fractograms as a tool to better describe the spatial dependence of variables along the scale. (C) 2014 Elsevier B.V. All rights reserved.

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The establishment of pastures in Amazonia is made to replace the woody vegetation by slash and burn process in chemically poor and low available phosphorus soils. The recovery of degraded areas is required and can contribute to reducing deforestation in the region. This study aimed to evaluate the effects of doses of Arad and NPK combinations in the management of maize in soil with low productive capacity. The experiment was conducted in Santo Antonio do Taua, Para State, in an area with degraded pasture, in a dystrophic Oxisol. The experimental design was a randomized block split plot design with four replications. The plots were four phosphate: 50, 100, 200 and 300 kg ha(-1) of P2O5 as Arad and sub-plots combination with NPK, NK, NK liming, and control (no match ). We evaluated the growth characteristics and productivity of corn. Doses of Arad influenced the plant height and number of kernels per row cob. The application of Arad combined with NPK increased grain yield.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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CHARACTERIZATION OF REGOSOLS IN THE SEMIARID REGION OF PERNAMBUCO, BRAZIL Studies on soil characterization in unexplored regions, besides the generation of data banks for the soil classes of the country, also produce scientific information about soil properties, important for the development of good management practices and sustainable land use. One of the main soil classes in the semiarid region of Pernambuco State, the Regosols, cover about 27 % of the state area, and are used mainly for family agriculture. Due to different geological and climatic aspects Regosols with different chemical, physical and mineralogical properties are found in Pernambuco, which were characterized for the semiarid region of the State. Five Regosol profiles were selected in different regions of the State (P1=Sao Caetano; P2=Lagoa do Ouro; P3=Caetes; P4=Sao Joao; P5=Parnamirim). The soils were morphologically characterized and samples collected from all horizons and the bedrock. Routine physical and chemical analyses were carried out for soil classification of all samples and mineralogical analyses of the coarse fractions (gravel and sand) by optical microscopy and of the silt and clay fractions by X ray diffraction (XRD), as well as petrographic analyses of the rock samples. The results showed similarities between the soils, with a low degree of pedogenetic development, varying from medium to very deep, with the horizon sequence A-AC-C-Cr and a sandy to sandy loam texture. In the deeper layers of two profiles (P1 and P5), a solodic character was observed. Organic matter and available phosphorus content were low in all studied soils. Despite the low levels of exchangeable cations, all soil profiles showed high base saturation. The mineralogical composition of gravel, sand and silt fractions consisted, essentially, of quartz, followed by feldspars and mica, supporting the results of the petrographic analysis of the bedrock. Kaolinite was the main clay mineral in all studied profiles and horizons, indicating an important monosialitization process in autochthonous soils of a typical semiarid region. In soil profile P2, at a lower landscape position, smectite minerals were observed, with mixing phases of montmorillonite, beidelite or nontronite, indentified by the Greene-Kelly test in the DRX analysis.

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La creciente demanda, en los últimos años, a nivel mundial y nacional de los productos deshidratados hace que esta actividad se perfile como promisoria en la región cuyana. Prácticamente el 100 % de la deshidratación de cebolla (Allium cepa L.) del país se realiza en Mendoza, habiendose hecho sólo producciones aisladas y de escaso volúmen en otras plantas del país. Las estimaciones preveen que se seguirá abasteciendo el mercado local y se incrementaránlas exportaciones de cebolla deshidratada. El objetivo general del presente trabajo fue establecer la influencia de la fertilización y el riego sobre la productividad y calidad de un cultivar mejorado de cebolla de importancia económica para la industria del deshidratado. En el Campo Experimental del INTA La Consulta se llevaron a cabo durante los años 1994-´95 y 1995-´96, dos ciclos de ensayos, con una línea de cebolla para deshidratar derivada del cultivar Southport White Globe. El suelo es de origen aluvial, profundo y de textura franca (Torrifluvente típico). Se determinaron los principales parámetros físicos, químicos e hídricos de la fracción fina del suelo. Para determinar el efecto de la fertilización sobre componentes de crecimiento y calidad y estudiar la variación de la concentración y ritmo de absorción de nutrimentos se ensayaron diferentes tratamientos. En el primer ciclo se ensayaron nueve tratamientos con tres niveles de N (0, 100, 200 kg N ha-1 ) aplicado como urea y tres niveles de P (0, 30, 60 kg P ha-1 ) como superfosfato. En el segundo ciclo se probaron ocho tratamientos con los siguientes niveles de N, P y K, respectivamente: (0 y 100 kg N ha-1), (0 y 40 kg P ha-1) y (0 y 60 kg K ha-1), éste último como sulfato de potasio. Para evaluar el efecto de diferentes regímenes de riego al final del ciclo de cultivo sobre la produccción cuantitativa y cualitativa de cebolla para la industria del deshidratado se programaron cortes anticipados de riegos, según diferentes fechas anteriores a la cosecha. Estas fueron para el primero y segundo ciclo de ensayo, respectivamente: (33, 27, 21, 8) y (21,14, 7) días anteriores a la fecha de cosecha estimada. Las principales conclusiones fueron: A) Con respecto a la fertilización: i) En todos los casos, e independientemente del tratamiento ensayado el mayor incremento relativo de sustancia seca aérea se evidencia durante la II fase de viii desarrollo que tiene lugar entre los primeros días de noviembre y mediados de diciembre ii) En dicha II fase se comienzan a manifestar incrementos absolutos de peso seco aéreo y área foliar atribuibles a la fertilización iii) También en todos los tratamientos se verifica que al finalizar la II fase el peso de los bulbos alcanza el 20 % de su peso de cosecha. En ese momento, los valores determinados para el porcentaje de sólidos totales (% ST) oscilan entre 13 % y 14 % iv) La mayor tasa de crecimiento del bulbo se constató en la III fase en la que se logra el 80% restante de su peso final v) En la III fase el % ST del bulbo sigue en aumento hasta casi el momento de cosecha y alcanzó valores promedios de 20 % y 21 %. La fertilización con diferentes dosis de N, P y K no influyó en el contenido de materia seca de los bulbos aunque sí lo hizo positivamente sobre su peso fresco vi) Los máximos rendimientos de bulbos (37.3 Mg ha-1) y de materia seca (7.92 Mg ha-1) se obtuvieron, en el segundo ciclo de ensayo, con las dosis de 100 kg N ha-1 y 40 kg P ha-1 vii) Los parámetros tisulares aéreos de valor diagnóstico asociados a máximosrendimientos, y al final de la II fase, correspondieron a una Alimentación Global (N, P, K) de 4.96 g % g s. seca y concentraciones de N, P y K respectivamente de: 2.56 g %, 0.22 g % y 2.18 g %. En cuanto a los tenores de Ca y Mg los porcentajes respectivos fueron: 2.10 g % y 0.16 g %. Los valores medios de equilibrios nutricionales fueron: N - P - K: 52 % - 4% - 44%. Con respecto a los micronutrimentos sus concentraciones fueron, en mg kg-1, Fe: 400, Zn: 55, Mn: 35 y Cu:19 y los valores de equilibrios nutricionales : 78.5 % - 11 % - 7 % - 3.5 %, respectivamente viii) La extracción total efectuada por el cultivo para esas máximas producciones, en kg ha-1, de N - P - K - Ca - Mg fueron: 214 - 40 -187 - 184 -19 B) Con respecto a los regímenes de riego: i) El rendimiento máximo obtenido -38.9 Mg ha-1- en el ensayo de cortes anticipados de riego correspondió al tratamiento R7 del ciclo 1995-‘96 ii) El mismo perteneció al tratamiento, que además de la fertilización básica con 100 kg N ha-1, aseguró durante los meses de noviembre, diciembre y enero, ix hasta siete días antes de cosecha, una humedad edáfica mínima (umbral de riego) correspondiente al 50 % del agua disponible. Este tratamiento se caracterizó por un total de 18 riegos y una incorporación de agua de 6120 m3 ha-1. iii) Los rendimientos totales de materia seca fueron afectados detrimentalmente por los otros regímenes de riego de cortes más anticipados iv) Se constató una relación lineal positiva altamente ignificativa entre el rendimiento y la lámina total de agua aplicada al cultivo.

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Para medir la disponibilidad de los micronutrientes en la zona de mayor densidad radical de los frutales de pepita y carozo y sugerir pautas de manejo que permitan un uso sustentable del recurso suelo, se tomaron muestras representativas de 25 montes cultivados con manzanos a lo largo del Alto Valle del río Negro (Argentina). Se extrajeron muestras a 0-25 y 25-50 cm de profundidad y se determinó la concentración disponible de Fe, Cu, Mn y Zn; granulometría; pH; materia orgánica (MO); carbonatos; P y capacidad de intercambio catiónico (CIC). Los resultados muestran que los micronutrientes se concentran mayoritariamente en la primera capa de suelo analizada, disminuyendo abruptamente en el estrato 25-50 cm. En la capa superficial, la disponibilidad de Cu y Zn está influenciada por el P mientras que el pH afecta la del Fe, Cu, y Mn en el estrato de suelo de 25-50 cm. En conclusión, es posible mejorar la nutrición mineral de los cultivos si se crean condiciones favorables para el crecimiento radical en la capa superficial del suelo.

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Mangrove forest structure and sediment characteristics were examined in the extensive mangroves of Bocas del Toro, Republic of Panama. Forest structure was characterized to determine if spatial vegetation patterns were repeated over the Bocas del Toro landscape. Using a series of permanent plots and transects we found that the forests of Bocas del Toro were dominated by Rhizophora maugle with very few individuals of Avicennia germinans and Laguncularia racemosa. Despite this low species diversity, there was large variation in forest structure and in edaphic conditions (salinity, concentration of available phosphorus, Eh and sulphide concentration). Aboveground biomass varied 20-fold, from 6.8 Mg ha(-1) in dwarf forests to 194.3 Mg ha(-1) in the forests fringing the land. But variation in forest structure was predictable across the intertidal zone. There was a strong tree height gradient from seaward fringe (mean tree height 3.9 m), decreasing in stature in the interior dwarf forests (mean tree height 0.7 m), and increasing in stature in forests adjacent to the terrestrial forest (mean tree height 4.1 m). The predictable variation in forest structure emerges due to the complex interactions among edaphic and plant factors. Identifying predictable patterns in forest structure will aid in scaling up the ecosystem services provided by mangrove forests in coastal landscapes.

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Invasive plant species are major threats to the biodiversity and ecosystem stability. The purpose of this study is to understand the impacts of invasive plants on soil nutrient cycling and ecological functions. Soil samples were collected from rhizosphere and non-rhizosphere of both native and exotic plants from three genera, Lantana, Ficus and Schinus, at Tree Tops Park in South Florida, USA. Experimental results showed that the cultivable bacterial population in the soil under Brazilian pepper (invasive Schinus) was approximately ten times greater than all other plants. Also, Brazilian pepper lived under conditions of significantly lower available phosphorus but higher phosphatase activities than other sampled sites. Moreover, the respiration rates and soil macronutrients in rhizosphere soils of exotic plants were significantly higher than those of the natives (Phosphorus, p=0.034; Total Nitrogen, p=0.0067; Total Carbon, p=0.0243). Overall, the soil biogeochemical status under invasive plants was different from those of the natives.