Alterações nos atributos químicos do solo e comportamento de cultivares de feijão em resposta à calagem superficial em sistema plantio direto

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

Deconvolução de perfis de poços através do ajuste de energia

As medidas de resistividade são de fundamental importância para o cálculo da saturação de óleo em reservatórios potencialmente produtores. A combinação das medidas de resistividade rasa e profunda permite a obtenção dos parâmetros R_t, R_xo e d_i. Mas, em reservatórios complexos existem dificuldades em se obter leituras confiáveis de R_t, devido à baixa resolução vertical das ferramentas de investigação profunda. Em reservatórios laminados, por exemplo, as leituras obtidas pela ferramenta de indução profunda (ILD) podem levar a uma interpretação errônea das mesmas, levando a acreditar que as medidas obtidas do perfil referem-se a uma única camada. Este problema pode ser em parte resolvido através de uma metodologia que melhore a resolução vertical dos perfis de investigação profunda, valendo-se do uso de informações obtidas de um perfil de alta resolução vertical, i.e; a curva de resistividade rasa. Uma abordagem neste sentido seria usar um perfil de alta resolução que apresente uma boa correlação com o perfil de investigação profunda. Esta correlação pode ser melhor avaliada se aplicarmos um filtro no perfil de alta resolução, de tal forma que o perfil resultante tenha teoricamente a mesma resolução vertical do perfil de baixa resolução. A obtenção deste filtro, porém, recai na premissa de que as funções respostas verticais para as ferramentas de alta e baixa resolução são disponíveis, o que não ocorre na prática. Este trabalho se propõe mostrar uma nova abordagem onde o filtro pode ser obtido a partir de um tratamento no domínio da freqüência. Tal tratamento visa igualar a energia espectral do perfil de alta resolução à energia espectral do perfil de baixa resolução tendo como base o Teorema de Parseval. Será mostrado que a resolução vertical depende fundamentalmente da energia espectral do perfil em questão. A seguir, uma regressão linear é aplicada sobre os perfis de alta resolução filtrado e de baixa resolução. Para cada ponto amostrado dos perfis, uma rotina de minimização é aplicada visando escolher o melhor intervalo de correlação entre os perfis. Finalmente, um fator de correção é aplicado sobre cada ponto do perfil de baixa resolução. Os resultados obtidos com os perfis de indução são promissores, demonstrando a eficácia da abordagem e mesmo quando aplicada em perfis com diferentes propriedades petrofísicas, a metodologia funcionou satisfatoriamente, sem danificar os perfis originais.

Interpretação do gráfico de Hingle através de rede competitiva angular

A saturação de água é a principal propriedade petrofísica para a avaliação de reservatórios de hidrocarbonetos, pois através da análise dos seus valores é definida a destinação final do poço recém perfurado, como produtor ou poço seco. O cálculo da saturação de água para as formações limpas é, comumente, realizado a partir da equação de Archie, que envolve a determinação da resistividade da zona virgem, obtida a partir de um perfil de resistividade profunda e o cálculo de porosidade da rocha, obtida a partir dos perfis de porosidade. A equação de Archie envolve ainda, a determinação da resistividade da água de formação, que normalmente necessita de definição local e correção para a profundidade da formação e da adoção de valores convenientes para os coeficientes de Archie. Um dos métodos mais tradicionais da geofísica de poço para o cálculo da saturação de água é o método de Hingle, particularmente útil nas situações de desconhecimento da resistividade da água de formação. O método de Hingle estabelece uma forma linear para a equação de Archie, a partir dos perfis de resistividade e porosidade e a representa na forma gráfica, como a reta da água ou dos pontos, no gráfico de Hingle, com saturação de água unitária e o valor da resistividade da água de formação é obtido a partir da inclinação da reta da água. Independente do desenvolvimento tecnológico das ferramentas de perfilagem e dos computadores digitais, o geofísico, ainda hoje, se vê obrigado a realizar a interpretação de ábacos ou gráficos, sujeito a ocorrência de erros derivados da sua acuidade visual. Com o objetivo de mitigar a ocorrência deste tipo de erro e produzir uma primeira aproximação para a saturação de água em tempo real de perfilagem do poço, insere-se o trabalho apresentado nesta dissertação, com a utilização de uma conveniente arquitetura de rede neural artificial, a rede competitiva angular, capaz de identificar a localização da reta da água, a partir da identificação de padrões angulares presentes nos dados dos perfis de porosidade e resistividade representados no gráfico de Hingle. A avaliação desta metodologia é realizada sobre dados sintéticos, que satisfazem integralmente a equação de Archie, e sobre dados reais.

Recanalization after acute deep vein thrombosis

O processo de recanalização das veias dos membros inferiores, após um episódio de trombose venosa profunda aguda em pacientes anticoagulados com heparina e inibidores da vitamina K, faz parte da evolução natural da remodelagem do trombo venoso. Esse complexo processo de remodelagem envolve a adesão do trombo à parede da veia, à resposta inflamatória da parede do vaso, levando à organização e subsequente contração do trombo, à neovascularização e à lise espontânea de áreas no interior do trombo. A presença de fluxo arterial espontâneo em veias com trombose recanalizada tem sido descrita como secundária à neovascularização e se caracteriza pelo desenvolvimento de fluxo com padrão de fístulas arteriovenosas, identificadas por meio de mapeamento dúplex colorido. Nesta revisão, são discutidos alguns aspectos controversos da história natural da trombose venosa profunda, para uma melhor compreensão da sua evolução e do seu impacto sobre a doença venosa.

Long-term clinical and ultrasonographic evaluation of thrombophilic patients with deep venous thrombosis

OBJECTIVE:The purpose of this study was to evaluate the long term clinical and ultrasonographic outcomes of thrombophilic patients with deep venous thrombosis (DVT).METHOD:Cohort study, retrospective case-control with cross-sectional analysis. Thirty-nine thrombophilic patients and 25 non-thrombophilic patients were assessed 76.3 ± 45.8 months after diagnosis. Demographic and family data were collected, as well as data from clinical and therapeutic progress, and physical and ultrasound examinations of the limbs were performed. Groups were matched for age and gender and the variables studied were compared across groups.RESULTS:Deep venous thrombosis was more frequent in women. The most common thrombophilias were antiphospholipid syndrome and factor V Leiden mutation. There was no difference between groups in terms of the number of pregnancies or miscarriages and the majority of women did not become pregnant after DVT. Non-spontaneous DVT prevailed. Proximal DVT and DVT of the left lower limb were more frequent, and the main risk factor was use of oral contraceptives. All patients were treated with anticoagulation. There was a higher frequency of pulmonary embolism in non-thrombophilic patients. Most patients considered themselves to have a normal life after DVT and reported wearing elastic stockings over at least 2 years. Seventy-one percent of patients had CEAP > 3, with no difference between groups. Deep venous reflux was more frequent in thrombophilic patients.CONCLUSION:There were no significant differences between groups with respect to most of the variables studied, except for a higher frequency of pulmonary embolism in non-thrombophilic patients and greater frequency of deep venous reflux in thrombophilic patients.

DNA methylation patterns of steroid receptor genes ESR1, ESR2 and PGR in deep endometriosis compromising the rectum

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

An integrable evolution equation for surface waves in deep water

In order to describe the dynamics of monochromatic surface waves in deep water, we derive a nonlinear and dispersive system of equations for the free surface elevation and the free surface velocity from the Euler equations in infinite depth. From it, and using a multiscale perturbative method, an asymptotic model for small wave steepness ratio is derived. The model is shown to be completely integrable. The Lax pair, the first conserved quantities as well as the symmetries are exhibited. Theoretical and numerical studies reveal that it supports periodic progressive Stokes waves which peak and break in finite time. Comparison between the limiting wave solution of the asymptotic model and classical results is performed.

Prototype Fault Current Limiter Using Transformer and a Modular Device of YBCO Coated Conductor

A superconducting fault current limiter (SCFL) consisted of a transformer with low reactance connected to the power line and with the secondary winding short-circuited by a modular superconducting limiter device with 16 elements connected in series was constructed and tested. The designed coupling transformer has low dispersion reactance in order to limit the voltage drop in the power line within the range of 5 % to 10 %. The experimental results showed that an insertion of a 0.125 Omega resistance limited the peak current to a factor of 2.5 times of the unlimited current. The power dissipation reached 39 kW during 100 ms, with an energy density of 380 J/cm(3). Based on these results, the SCFL will be further tested in a 3 MVA (15 kV/380 V) generator for currents up to 10 kA.

Deep learning architecture for gesture recognition

Pós-graduação em Engenharia Mecânica - FEG

Recanalization Rates after Acute Deep Vein Thrombosis: A Single-center Experience Using a Newly Proposed Vein Diameter Variation Index

Background: Duplex ultrasound scanning (DUS) is the method of choice for diagnosis of deep vein thrombosis (DVT). However, only a few studies have performed prospective serial DUS after an acute episode of DVT to assess its evolution. This study aimed to report our experience using DUS combined with a thrombosis score (TS) and a newly proposed vein diameter variation index (VDVI) to evaluate the rate of resolution of DVT by assessing and quantifying the early stages of vein recanalization in proximal vein segments within 6 months after an episode of acute lower extremity DVT.Methods: Twelve patients with first episode of acute lower extremity DVT confirmed by DUS as occurring in <= 10 days after the onset of venous thrombosis symptoms were followed up prospectively for 6 months. TS and VDVI were calculated at 1, 3, and 6 months to assess vein recanalization. Intra-thrombus arteriovenous fistula formation was also investigated and related to the recanalization process.Results: Seven (58%) women were included, with a total cohort median age of 53.5 +/- 19 years. The left lower extremity was affected in 7 (58%) patients. DVT was diagnosed in 55 proximal vein segments. All patients had proximal DVT, with involvement of the external iliac, femoral, and popliteal veins. After 6 months, there was a significant decrease in TS and increase in VDVI (P < 0.001) in all proximal vein segments assessed, indicating thrombus regression. The more distal the DVT was, the faster was the VDVI increase, with most popliteal veins being recanalized at 3 months (P < 0.001). Intra-thrombus arteriovenous fistula was identified in 50% of patients at 1 month while on anticoagulation.Conclusions: The combined use of two different DUS-based assessment tools, TS and the proposed VDVI, provided an effective method to prospectively assess vein recanalization rates after an episode of acute lower extremity DVT in this series of patients and may allow a correct evaluation of DVT and its resolution or progression.

Relationship between therapeutic alliance and deep abdominal muscle recruitment in nonspecific low back pain sufferers

Chronic low back pain is a difficult condition to be treated. As some patients respond positively to treatment and others do not present any improvements, one can think there are others conditional factors that need to be elucidated. By means of this study, we sought to investigate the association between the occurrence of the formation of a positive relationship between patient and therapist, assessed by the therapeutic alliance inventory, and the adequate recruitment of the deep abdominal muscles, as well as to verify the effect of a protocol intervention based on motor control exercises on levels of pain and disability. The recruitment of the transverse abdominal and internal oblique muscles was examined by ultrasound imaging in 12 subjects with nonspecific chronic low back pain before and after implementation of a protocol for motor control exercises, with subsequent application of the therapeutic alliance inventory questionnaire. No association was found between the level of therapist/patient alliance and muscle recruitment. The proposed protocol was effective in reducing the levels of pain and disability; however, recruitment of transverse abdominal and internal oblique muscles showed no significant changes in the end of the intervention. Based on these findings, we verified that the therapeutic alliance has no association with muscle recruitment in the short term. However, although there were no changes in muscle recruitment after the intervention program, the level of pain and disability was reduced.

Comparative clinical sample preparation of DNA and RNA viral nucleic acids for a commercial deep sequencing system (Illumina MiSeq (R))

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

Continental degassing of He-4 by surficial discharge of deep groundwater

Radiogenic He-4 is produced by the decay of uranium and thorium in the Earths mantle and crust. From here, it is degassed to the atmosphere(1-5) and eventually escapes to space(1,5,6). Assuming that all of the He-4 produced is degassed, about 70% of the total He-4 degassed from Earth comes from the continental crust(2,-5,7). However, the outgoing flux of crustal He-4 has not been directly measured at the Earths surface(2) and the migration pathways are poorly understood(2-4,7,8). Here we present measurements of helium isotopes and the long-lived cosmogenic radio-isotope Kr-81 in the deep, continental-scale Guarani aquifer in Brazil and show that crustal He-4 reaches the atmosphere primarily by the surficial discharge of deep groundwater. We estimate that He-4 in Guarani groundwater discharge accounts for about 20% of the assumed global flux from continental crust, and that other large aquifers may account for about 33%. Old groundwater ages suggest that He-4 in the Guarani aquifer accumulates over half- to one-million-year timescales. We conclude that He-4 degassing from the continents is regulated by groundwater discharge, rather than episodic tectonic events, and suggest that the assumed steady state between crustal production and degassing of He-4, and its resulting atmospheric residence time, should be re-examined.

Liming in Growing Mango Cultivar Keitt in Production

The tropical soil acidity is one of the main limiting factors for crop productivity. This study aimed to evaluate the effects of application of limestone dose to soil fertility, nutritional status of the crop, and productivity and quality of the fruits of mango, cultivar Keitt. The study was carried out at Selviria, state of Mato Grosso Sul, Brazil, in a Typic Haplustox (pH in CaCl2=4.7), cultivated with mango cultivar Keitt grafted on Coquinho pattern in the production phase (13years old). Treatments were composed of limestone doses (0, 1.55, 3.10, 4.65, and 6.20tha(-1)), arranged in blocks at random with three repetitions. The limestone was applied and incorporated in the surface layer of 0 to 5cm deep in the total area. We evaluated the chemical attributes of the soil [pH, hydrogen (H+) aluminum (Al), calcium (Ca), magnesium (Mg), potassium (K), and sum of bases and base saturation] at 16 and 28months after liming (layer 0 to 20cm deep), the nutrition of plants at 12months after liming, and quality of the fruit in two crop years. Liming promoted improvements in soil chemical attributes, reflected in the nutritional status, productivity, and quality of mango fruit. Also, there was a linear effect with the application of lime dose on the productivity of the fruit, but after the second year of evaluation.