931 resultados para 54-424


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Analisa a produção legislativa na Câmara dos Deputados, da 51ª à 54ª legislaturas, traçando uma investigação em três níveis de análise: coalizacional, partidário e parlamentar.

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Hydrothermal sulfide chimneys located along the global system of oceanic spreading centers are habitats for microbial life during active venting. Hydrothermally extinct, or inactive, sulfide deposits also host microbial communities at globally distributed sites. The main goal of this study is to describe Fe transformation pathways, through precipitation and oxidation-reduction (redox) reactions, and examine transformation products for signatures of biological activity using Fe mineralogy and stable isotope approaches. The study includes active and inactive sulfides from the East Pacific Rise 9 degrees 50'N vent field. First, the mineralogy of Fe(III)-bearing precipitates is investigated using microprobe X-ray absorption spectroscopy (RXAS) and X-ray diffraction (mu XRD). Second, laser-ablation (LA) and micro-drilling (MD) are used to obtain spatially-resolved Fe stable isotope analysis by multicollector-inductively coupled plasma-mass spectrometry (MC-ICP-MS). Eight Fe -bearing minerals representing three mineralogical classes are present in the samples: oxyhydroxides, secondary phyllosilicates, and sulfides. For Fe oxyhydroxides within chimney walls and layers of Si-rich material, enrichments in both heavy and light Fe isotopes relative to pyrite are observed, yielding a range of delta Fe-57 values up to 6 parts per thousand. Overall, several pathways for Fe transformation are observed. Pathway 1 is characterized by precipitation of primary sulfide minerals from Fe(II)aq-rich fluids in zones of mixing between vent fluids and seawater. Pathway 2 is also consistent with zones of mixing but involves precipitation of sulfide minerals from Fe(II)aq generated by Fe(III) reduction. Pathway 3 is direct oxidation of Fe(II) aq from hydrothermal fluids to form Fe(III) precipitates. Finally, Pathway 4 involves oxidative alteration of pre-existing sulfide minerals to form Fe(III). The Fe mineralogy and isotope data do not support or refute a unique biological role in sulfide alteration. The findings reveal a dynamic range of Fe transformation pathways consistent with a continuum of micro-environments having variable redox conditions. These micro-environments likely support redox cycling of Fe and S and are consistent with culture-dependent and -independent assessments of microbial physiology and genetic diversity of hydrothermal sulfide deposits.

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Introduction: This study reviews the cases of stapedotomy and evaluates its effectiveness at improving hearing loss in patients with otosclerosis. Materials and methods: Retrospective review of patients’ records who had clinical and audiometric diagnosis of otosclerosis from January to December 2012. Results: A total of 54 stapedotomy surgeries (52 unilateral and 1 bilateral surgeries) were received. Average post-operative ABG for 0.5, 1, 2 and 4 KHz showed that 61.1% had complete closure of ABG (ABG < 10 dB) compared with 1.6% preoperatively and 85.2% had closure of ABG to within 20dB compared with 4.7% preoperatively (t – 13.89, p = 0.000). More than 94% had hearing improvement and 81.5% had ABG closure greater than 10 dB postoperatively (mean gain 23.38 ± 12.37, t = 13.89, p = 0.000). A total of 13% complications were recorded with TM perforation (5.6%) being the commonest complication. Conclusion: Stapedotomy is an effective surgical procedure for the treatment of otosclerosis which leads to improvement in patients’ quality of life. A favorable hearing outcome can be obtained by the combination of experienced hands with minimal surgical trauma and appropriate surgical technique.

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Algae specimens mounted on 133 leaves preceded by printed pages with caption title: (1) List of Dr. Harvey's duplicate Ceylon algae ; (2) List of Dr. Harvey's duplicate Friendly Island Algae ; (3) List of Dr. Harvey's duplicate Australian algae.

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Each year the South Carolina Public Service Commission reports to the Office of State Budget that includes the agency's mission, goals and objectives to accomplish the mission, and performance measures regarding the goals and objectives.

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P>Weight-length relationships (WLRs) are presented for 54 species sampled by several types of fishing gear between February 2004 and May 2007, in the Arade estuary (southern Portugal). WLRs for six species are presented for the first time.

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La clase de educación física es un espacio en el cual los niños y adolescentes pueden incrementar los niveles de actividad física y alcanzar las recomendaciones emitidas por la Organización Mundial de la Salud (OMS), sin embargo, existe poca evidencia científica a nivel nacional sobre las actividades físicas que realizan los estudiantes dentro del ámbito escolar, específicamente dentro de las clases de educación física y sus relaciones con el contexto; es por esto que el objetivo de este estudio fue evaluar los niveles de actividad física de niños y adolescentes durante las clases de educación física en tres colegios oficiales de Bogotá, Colombia, por medio de la herramienta SOFIT. Estudio de diseño descriptivo y transversal realizado entre octubre de 2014 y mayo de 2015. Las observaciones se llevaron a cabo en tres colegios oficiales de la ciudad de Bogotá ubicados en las localidades de Tunjuelito y Ciudad Bolívar que aceptaron su participación en la investigación. Se obtuvo la aprobación para participar de 1361 estudiantes (682 niñas y 679 niños) de 5 a 17 años de los cuales 180 estudiantes (93 niños y 87 niñas) fueron seleccionados de manera aleatoria sistemática, siguiendo el protocolo SOFIT para observar su nivel de actividad física durante las clases de educación física. El 45,23% del tiempo de la clase de educación física los estudiantes mantuvieron un comportamiento sedentario; mientras que el 30.91% y el 23.86% del tiempo de la clase presentaron un nivel de actividad física moderada (AFM) y vigorosa (AFV) respectivamente. El nivel de actividad física moderada a vigorosa (AFMV), fue de 54,78% es decir, 35,27 minutos de la clase. Los docentes no promovieron la actividad física en un 56,47% del tiempo de la clase y se encontró que ningún docente promovió la actividad física fuera de la clase, es decir, alentando a sus estudiantes a que practicaran cualquier forma de actividad física en horas extraescolares. El contexto de la clase que más se desarrolló fue la condición física con un 35,66% del tiempo de la clase, seguido por los contextos de generalidades 24,83% y habilidades 23,84%. El contexto de la clase generalidades está asociada significativamente y de manera negativa (β=-0,32, p=0,006) con menor porcentaje de tiempo en AFM y AFV, las variables activas de SOFIT, lo que sugiere que las clases deben invertir menos tiempo en este contexto e incrementar el porcentaje de tiempo en los otros contextos como condición física y habilidades para aumentar la cantidad de minutos de AFMV en los estudiantes.

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A importância de se conhecer detalhadamente o sistema radicular de uma cultura está relacionada com estratégias técnico-cientificas, tanto para tomadas de decisões técnicas (por exemplo, manejo de adubação) como também para estimar a contribuição no estoque e ciclagem de nutrientes no solo. O presente trabalho avaliou a biomassa abaixo do solo em um plantio comercial de híbrido interespecífico de palma de óleo (Elaeis oleifera cortés x Elaeis guineensis jacq.), cultivar BRS Manicoré, no município de Moju, nordeste do estado do Pará. Amostras de raízes foram obtidas por meio de coleta de monólitos em trincheiras com 400 cm de comprimento, 50 cm de largura e 300 cm de profundidade. Portanto, em cada camada amostrada (0-15, 15-30 e 30-60 cm), foram coletados oito monólitos. Em laboratório, as raízes foram classificadas de acordo com seu diâmetro em primárias, secundárias e terciárias. A massa seca das raízes foi determinada após secagem em estufa de circulação forçada de ar a 65 °C por 96 horas. Do total de raízes no perfil amostrado, 65,6% são raízes primárias, 29,8% secundárias e 4,6% terciárias. A camada 15-30 cm concentra 54,2% da biomassa total de raízes. Nas camadas 0-15 e 30-60 cm, estão concentrados, respectivamente, 32,5 e 13,2% da biomassa total de raízes.

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A low temperature synthesis method based on the decomposition of urea at 90°C in water has been developed to synthesise fraipontite. This material is characterised by a basal reflection 001 at 7.44 Å. The trioctahedral nature of the fraipontite is shown by the presence of a 06l band around 1.54 Å, while a minor band around 1.51 Å indicates some cation ordering between Zn and Al resulting in Al-rich areas with a more dioctahedral nature. TEM and IR indicate that no separate kaolinite phase is present. An increase in the Al content however, did result in the formation of some SiO2 in the form of quartz. Minor impurities of carbonate salts were observed during the synthesis caused by to the formation of CO32- during the decomposition of urea.

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The infrared (IR) spectroscopic data and Raman spectroscopic properties for a series of 13 “pinwheel-like” homoleptic bis(phthalocyaninato) rare earth complexes M[Pc(α-OC5H11)4]2 [M = Y and Pr–Lu except Pm; H2Pc(α-OC5H11)4 = 1,8,15,22-tetrakis(3-pentyloxy)phthalocyanine] have been collected and comparatively studied. Both the IR and Raman spectra for M[Pc(α-OC5H11)4]2 are more complicated than those of homoleptic bis(phthalocyaninato) rare earth analogues, namely M(Pc)2 and M[Pc(OC8H17)8]2, but resemble (for IR) or are a bit more complicated (for Raman) than those of heteroleptic counterparts M(Pc)[Pc(α-OC5H11)4], revealing the decreased molecular symmetry of these double-decker compounds, namely S8. Except for the obvious splitting of the isoindole breathing band at 1110–1123 cm−1, the IR spectra of M[Pc(α-OC5H11)4]2 are quite similar to those of corresponding M(Pc)[Pc(α-OC5H11)4] and therefore are similarly assigned. With laser excitation at 633 nm, Raman bands derived from isoindole ring and aza stretchings in the range of 1300–1600 cm−1 are selectively intensified. The IR spectra reveal that the frequencies of pyrrole stretching and pyrrole stretching coupled with the symmetrical CH bending of –CH3 groups are sensitive to the rare earth ionic size, while the Raman technique shows that the bands due to the isoindole stretchings and the coupled pyrrole and aza stretchings are similarly affected. Nevertheless, the phthalocyanine monoanion radical Pc′− IR marker band of bis(phthalocyaninato) complexes involving the same rare earth ion is found to shift to lower energy in the order M(Pc)2 > M(Pc)[Pc(α-OC5H11)4] > M[Pc(α-OC5H11)4]2, revealing the weakened π–π interaction between the two phthalocyanine rings in the same order.

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