Interação de microorganismos na solubilização de fósforo e potássio de rochas para produção de biofertilizantes

he present model of agriculture is based on intensive use of industrial inputs, due to its rapid response, but it brings harmful consequences to the environment, and it is necessary the use of modern inputs. And an alternative is the use of rock biofertilizers in agriculture, a product easy to use, with higher residual effect and does not harm the environment. The objective of study was to evaluate the inoculation and co-inoculation of different microorganisms in the solubilization of rock phosphate and potash ground microbial evaluating the best performance in the production of biofertilizers comparing with rocks pure in soil chemical properties and, verify effect of inoculation of the bacterium Paenibacillus polymyxa in the absorption of minerals dissolved in the development of cowpea (Vigna unguiculata [L.] Walp.). The first bioassay was conducted in Laboratory (UFRN) for 72 days in Petri dishes, where the rock powder was increased by 10% and sulfur co-inoculated and inoculated with bacterial suspension of Paenibacillus polymyxa grown in medium tryptone soy broth, Ralstonia solanacearum in medium Kelman, Cromobacterium violaceum in medium Luria-Bertani and Acidithiobacillus thiooxidans in medium Tuovinen and Kelly,and fungi Trichoderma humatum and Penicillium fellutanum in malt extract. Every 12 days, samples were removed in order to build up the release curve of minerals. The second bioassay was conducted in a greenhouse of the Agricultural Research Corporation of Rio Grande do Norte in experimental delineation in randomized block designs, was used 10 kg of an Yellow Argissolo Dystrophic per pot with the addition of treatments super phosphate simple (SS), potassium chloride (KCl), pure rock, biofertilizers in doses 40, 70, 100 and 200% of the recommendation for SS and KCl, and a control, or not inoculated with bacteria P. polymyxa. Were used seeds of cowpea BRS Potiguar and co-inoculated with the bacterial suspension of Bradyrhizobium japonicum and P. polymyxa. The first crop was harvested 45 days after planting, were evaluated in the dry matter (ADM), macronutrients (N, P, K, Ca, Mg) and micronutrients (Zn, Fe, Mn) in ADM. And the second at 75 days assessing levels of macro end micronutrients in plants and soil, and the maximum adsorption capacity of P in soil. The results showed synergism in co-inoculations with P. polymyxa+R. solanacearum and, P. polymyxa+C. violaceum solubilizations providing higher P and K, respectively, and better solubilization time at 36 days. The pH was lower in biofertilizers higher doses, but there was better with their addition to P at the highest dose. Significant reduction of maximum adsorption capacity of phosphorus with increasing dose of biofertilizer. For K and Ca was better with SS+KCl, and Mg to pure rock. There was an effect of fertilization on the absorption, with better results for P, K and ADM with SS+KCL, and N, Ca and Mg for biofertilizers. Generally, the P. polymyxa not influence the absorption of the elements in the plant. In treatments with the uninoculated P. polymyxa chemical fertilizer had an average significantly higher for weight and number of grains. And in the presence of the bacteria, biofertilizers and chemical fertilizers had positive values in relation to rock and control. The data show that the rocks and biofertilizers could meet the need of nutrients the plants revealed as potential for sustainable agriculture

Composición isotópica (13C/12C y 18 O/16 O) de las rocas encajantes de los yacimientos Zn-Pb del Cretácico Inferior de Cantabria (Sector Reocín-La Florida).

En este trabajo se presentan datos de la composición isotópica en carbono y oxígeno de rocas carbonáticas (calizas y dolomías) en el sector Reocín-La Florida (Cantabria). Estos materiales constituyen la roca encajante de importantes mineralizaciones dé Zn-Pb (tipo Mississippi Valley) de edad Cretácica. Las calizas analizadas tienen valores medios del ð13C(PDB) y ð18 O(SMOW) de +3,15 y +27,21, respectivamente. y las dolomías de +2,05 y +25,53, respectivamente. Estos datos sugieren una génesis diferente para ambos tipos de carbonatos, de tal forma que un origen singenético para las mineralizaciones debe ser rechazado. También se analizan otros tipos de carbonatos presentes (calizas de dolomitización y espeleotemas), cuyos datos indican un origen relacionado con aguas meteóricas, dado el empobrecimiento que estos materiales poseen en los isótopos pesados.

Detección de proteínas urinarias por iTRAQ asociadas a complicaciones del trasplante renal y su modificación con la terapia

Propósito y Método del Estudio: Determinar los perfiles de expresión de proteínas en orina en pacientes agrupados de acuerdo a las complicaciones presentadas post trasplante (TR) y detectar su variación al modificar la terapia. Fue un estudio observacional, longitudinal, analítico y retrospectivo. Se incluyeron pacientes que fueron sometidos a trasplante y estuvieron de acuerdo en participar en el protocolo. Se recolectaron muestras de orina pretrasplante y cada tercer día desde el momento del trasplante. Las muestras fueron almacenadas a -70ºC hasta el momento de su análisis por marcaje peptídico mediante isótopos isobáricos para la cuantificación relativa (iTRAQ). Se agrupó a los pacientes con complicaciones por infección confirmado por cultivos y rechazo agudo confirmado por biopsia. Se establecieron 4 fases de estudio: pre trasplante, post TR previo a complicación, post TR con complicación en curso y post TR complicación tratada. Contribuciones y Conclusiones: De Enero de 2009 a Mayo de 2013 se incluyeron a 22 pacientes: 10 mujeres (45%) y 12 hombres (55%) con una edad promedio de 45+ 15 años. Solo 12 pacientes presentaron complicaciones en el post TR: 2 pacientes con rechazo agudo al injerto (GR) (1hombre, 1 mujer); y 10 pacientes (6 hombres, 4 mujeres) en el grupo de infecciones (GI). Para el análisis por iTRAQ se hizo la cuantificación relativa comparando la presencia de las proteínas en las diferentes fases de estudio. Para el grupo de rechazo agudo, se encontraron 345 proteínas, de las cuales solo 15 cumplieron los criterios de aceptación de la técnica (score >30, > 2 péptidos identificados con el 95% de confianza). Para el grupo de infecciones se encontraron 113 de las cuales 28 cumplieron los criterios de aceptación de la técnica. Conclusiones: La albúmina fue la única proteína encontrada en ambos grupos de estudio, el resto de las proteínas 14 en el GR y 27 en GI fueron diferentes. Las 5 proteínas con mayor scores en GR fueron alfa 1 microglobulina, 5' nucleosidasa citosólica, Proteína 4 de unión a retinol, proteína de membrana 4 palmitolada y serin carboxipeptidasa mientras que en GI: acetil coenzima A sintetasa mitocondrial, adenosil homocisteinasa 2, proteína de dedo de zinc GLIS1isoforma X1, proteína putativa de la isoforma FAM157B, proteína de dedo de zinc 615 isoforma X6. Queda por dilucidar la participación de cada una de éstas en los pacientes con trasplante renal.

The transition to agriculture in south-wertern Europe : new isotopic insights from Portugal's Atlantic coast

For the past 15 years, a succession of stable isotope studies have documented the abrupt dietary transition from the Mesolithic to the Neolithic in Western and Northern Europe. Portugal, with its Late Mesolithic shell middens and burials apparently coexisting with the earliest Neolithic, further illustrates the nature of that transition. Individuals from Neolithic contexts there had significantly different diets to their Mesolithic counterparts. No evidence was found for a transitional phase between the marine oriented Mesolithic subsistence regimes and the domesticated, terrestrial Neolithic diet. Two later Neolithic individuals, however, showed evidence for partial reliance on marine or aquatic foods. This raises questions about the possible persistence of marine dietary regimes beyond the Mesolithic period. This article is followed by a brief note by Mary Jackes and David Lubell.

Microbiologia do ciclo do nitrogênio em solos do cerrado

Dissertação (mestrado)—Universidade de Brasília, Instituto de Ciências Biológicas, Programa de Pós-Graduação em Biologia Microbiana, 2016.

Síntese e caracterização de catalisadores nanométricos de LaSrNiO4 para aplicação em dessulfurização de tiofeno

The mixed metal oxides constitute an important class of catalytic materials widely investigated in different fields of applications. Studies of rare earth nickelates have been carried by several researchers in order to investigate the structural stability afforded by oxide formed and the existence of catalytic properties at room temperature. So, this study aims synthesize the nanosized catalyst of nickelate of lanthanum doped with strontium (La(1-x)SrxNiO4-d; x = 0,2 and 0,3), through the Pechini method and your characterization for subsequent application in the desulfurization of thiophene reaction. The precursor solutions were calcined at 300ºC/2h for pyrolysis of polyester and later calcinations occurred at temperatures of 500 - 1000°C. The resulting powders were characterized by thermogravimetric analysis (TG / DTG), surface area for adsorption of N2 by BET method, X-ray diffraction (XRD), scanning electron microscopy (HR_SEM) and spectrometry dispersive energy (EDS). The results of XRD had show that the perovskites obtained consist of two phases (LSN and NiO) and from 700ºC have crystalline structure. The results of SEM evidenced the obtainment of nanometric powders. The results of BET show that the powders have surface area within the range used in catalysis (5-50m2/g). The characterization of active sites was performed by reaction of desulfurization of thiophene at room temperature and 200ºC, the relation F/W equal to 0,7 mol h-1mcat -1. The products of the reaction were separated by gas chromatography and identified by the selective detection PFPD sulfur. All samples had presented conversion above 95%

Química da vida : centros activos em metaloproteínas

Académico - Licenciaturas

Viver no campo ou na cidade? resposta dos morcegos (Mammalia, Chiroptera) à antropização da paisagem

Dissertação (mestrado)—Universidade de Brasília, Instituto de Ciências Biológicas, Departamento de Ecologia, Programa de Pós-Graduação em Ecologia, 2015.

Utilização agrícola de composto de resíduo sólido urbano.

O porquê do uso agronõmico do composto de lixo. Critérios de aplicação e de manejo do composto. Efeitos sobre as propriedades do solo. Capacidade de troca catiônica (CTC). rEAÇÃO DO SOLO. Nutrientes. Relação C/N. Nitrogênio. Fósforo. Potássio, cálcio, magnésio e sódio. Enxofre e micronutrientes. Salinidade e sociedade. Elementos inorgânicos potencialmente tóxicos. Efeitos sobre as plantas.

Estádios fenológicos e marcha de absorção de nutrientes da soja.

Estádios fenológicos: fase reprodutiva (crescimento indeterminado e determinado); fase vegetativa. Marcha de absorção de nutrientes da soja: macronutrientes (nitrogênio, cálcio, fósforo, magnésio, potássio e enxofre) e micronutrientes (Boro, manganês, cobre, zinco). Extração e exportação de macro e micronutrientes em diferentes cultivares de soja: BRS 184, SYN 1059, DM 6563 - Intacta RR2 PRO (tm).

Contribuição da catodoluminescência para o entendimento da diagênese da formação Jandaíra: áreas do campo de petróleo da fazenda Belém e Lajedo do Rosário

The general objective of this study was to contribute to the understanding of the chemical evolution of fluids that percolate through carbonate rocks of the Jandaíra Formation. The oxidation and reduction conditions in which grains, source and cement were formed was investigated using the cathodoluminescence technique (CL). The study area is located in the west part of the Potiguar Basin (Fazenda Belém field) and Rosário Ledge (Felipe Guerra municipality, State of Rio Grande do Norte, Brazil). The analysis of thin sections of carbonate rocks under CL revealed that grains (allochemical or not) and diagenetic products (micritization, dolomitization, neomorphism and cementation) exhibit since absence of luminescence the various luminescence colors (yellow, orange, red, brown, and blue) in a variety of intensities. As pure calcite shows dark blue luminescence, the occurrence of different luminescence colors in calcite crystals suggest one or more punctual crystal defects such as free electron, free space and impurity. The dyeing of thin sections with alizarin and potassium ferrocyanide revealed the absence of ferrous carbonate in the different lithotypes of Jandaíra Formation. Therefore, the different colors and intensities of CL observed in these rocks are probably caused by the presence of ion activators such as Mn2+ and is not an activator/inhibitor combination. In the same way, the absence of luminescence is very probably caused by the absence of activator ions and not due to the low concentration of inhibitor ions such as Fe2+. The incorporation of Mn2+ in the different members of the Jandaíra Formation must have been controlled by the redox state of the depositional environment and diagenesis. Therefore, it is possible that the luminescent members have been formed (e.g.,ooids) or have been modified (gastropod neomorphism) under reduction conditions in the depositional environments, in subsurface during the burial, or, in the case of Rosario Ledge samples , during the post-burial return to surface conditions. As regards the sudden changes from low to moderate and to strong luminescence, these features should indicate the precipitation of a fluid with chemical fluctuations, which formed the frequent zonations in the block cement of the Rosario Ledge samples. This study suggests that the different intensities and colors of CL should be correlated with the Mn2+ and Fe2+ contents, and stable isotopes of samples to determine the salinity, temperature, pH e Eh conditions during deposition

Partição de nicho isotópico por pequenos mamíferos em formações florestais de uma savana neotropical

Dissertação (mestrado)—Universidade de Brasília, Instituto de Ciências Biológicas, Departamento de Ecologia, Programa de Pós-Graduação em Ecologia, 2016.

Avaliação da biodessulfurização de 4-metildibenzotiofeno por Rhodococus rhodochrous (NRRL B-2149)

Crude oil has between 0.04 up to 5% of sulphur, the higher the oil the higher the sulphur levels. Sulphur usually gives problems such as corrosion in refinery, and once burnt produces SO2 that goes to atmosphere. This work aim to investigate the capacity of Rhodococcus rhodochrous (NRRL B-2149) to metabolize the model compound 4-methyldibenzotiophene (4-MDBT), to remove the sulphur and transform it in 2-hydroxybiphenyl (2-HBF) and sulphite using the 4S pathway. Kynetic runs were carried out in shaker at 120 rpm and 32°C. Samples were taken every 12h to assay substrate consume as well as cells production using HPLC. Results showed that R. rhodochrous NRRL B-2149 can use the 4S pathway in order to remove sulphur without change the carbon chain of the molecule as well as that cells and 4-MDBT affects the product formation. The production of 2-hydroxybiphenyl has interest for industry once it is a potent biocide. However, evaluation is necessary in order to obtain better results compatible with industry needs

Resposta da lagarta-do-cartucho à aplicação do fosfito em milho doce e divergência genética de populações de lagartas-da-espiga

Dissertação (mestrado)—Universidade de Brasília, Faculdade de Agronomia e Medicina Veterinária, Programa de Pós-Graduação em Agronomia, 2016.

Calda sulfocálcica - preparo e indicações.

2016