Migração 3D no tempo usando a teoria dos raios paraxiais

O trabalho aqui apresentado visa o estudo da migração 3D no tempo, em amplitudes verdadeiras, de dados da seção afastamento nulo ("zero-offset"), usando a aproximação de segunda ordem do tempo de trânsito de difração. O processo de migração no tempo usa a função difração determinada, corretamente, através de mesmos parâmetros que controlam a função tempo de trânsito de reflexão, além do auxílio dos raios paraxiais. Os parâmetros que controlam a função tempo de trânsito de reflexão são determinados através de pelo menos nove medidas de tempo de trânsito, obtidas a partir de dados pré-empilhados (tiro comum, ponto médio comum - CMP, etc.). Determinada a função difração, pode-se fazer a migração sem a necessidade de que se conheça o modelo de velocidades, pois a função tempo de trânsito de difração, como definido neste trabalho, não necessita do mesmo. O espalhamento geométrico é removido através do processo de migração e aplicação de uma função peso aos dados da seção afastamento nulo. Juntamente com a função peso, aplicou-se um filtro objetivando a recuperação da fase do sinal, ocorrida como consequência do processo de migração. Devido a limitação computacional, fez-se testes com dados sintéticos, em 2D, objetivando verificar a eficiência do programa. Os resultados obtidos foram satisfatórios, mostrando a eficiência e confiabilidade do processo.

Modelagem de eletrorresistividade 2-D a partir do potencial elétrico secundário

Um dos métodos clássicos da geofísica de exploração é o Método de Eletrorresistividade, estabelecido há um século pelos irmãos Schlumberger e desde então amplamente empregado em prospecção mineral, estudos ambientais e hidrogeologia e em pesquisa de fontes geotermais. Conceitualmente o método consiste de injeção de corrente elétrica na subsuperfície e de medida de diferença de potencial elétrico, resultante da interação da corrente com o meio. As localizações dessas fontes e receptores são determinadas pelo arranjo escolhido para o levantamento. Após o processamento, obtém-se pseudo-seções de resistividade aparente que indicam a distribuição de condutividade em subsuperfície. Devido à simplicidade dos fundamentos físicos de sua formulação, o método apresenta fácil implementação computacional quando comparado aos métodos eletromagnéticos de fonte controlada. Na literatura há inúmeros trabalhos de modelagem computacional, onde se calcula a resposta para problemas 2-D e 3-D. Nestes trabalhos, as pseudo-seções são obtidas a partir do cálculo do potencial elétrico total. Neste trabalho, apresentaremos a resposta da modelagem de eletroresistividade 2-D com o arranjo dipolo-dipolo, obtida a partir do potencial elétrico secundário. A solução é calculada através do método de elementos finitos usando malhas não estruturadas. Para efeito de validação, os resultados são comparados com a resposta 2-D obtida a partir dos potencias totais.

Production of β-(1,3)-glucanases by Trichoderma harzianum Rifai: Optimization and Application to Produce Gluco-oligosaccharides from Paramylon and Pustulan

β-(1→3)-Glucanases were produced by Trichoderma harzianum Rifai PAMB-86 cultivated on botryosphaeran in a bench-fermenter and optimised by the response surface method. Maximal enzyme titres occurred at 5 days, initial pH 5.5 and aeration of 1.5vvm. β-(1→3)-The β-glucanolytic enzyme complex produced by T. harzianum Rifai PAMB- 86 was fractionated by gel filtration into 2 fractions (F-I, F-II), and employed to produce gluco-oligosaccharides from algal paramylon ((1→3)-β-D-glucan) and lichen pustulan ((1→6)-β-D-glucan). Both enzymes attacked paramylon to the extent of ~15-20% in 30 min releasing glucose and laminaribiose as major end-products, and laminarioligosaccharides of degree of polymerization (DP) ≥3. Only F-I degraded pustulan resulting in ~2% degradation at 30 min, with glucose, gentiobiose and gentio-oligosaccharides of DP ≥4 as major products. The difference in the nature of the hydrolysis products can be explained by the substrate specificities of each enzyme fraction, and the structural differences of the β-D-glucans attacked.

Mass and surface fractal in supercritical dried silica aerogels prepared with additions of sodium dodecyl sulfate

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

Características estruturais de aerogéis hidrofílicos e hidrofóbicos de sílica modificados com Dodecil Sulfato de Sódio

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Inovação tecnológica em projetos de novos produtos: um estudo exploratório sobre relações gerenciais de integração entre unidades de uma multinacional

Although thetopic of integrationin product development is widely debated in the literature, there are few studies that address the participation by subsidiaries of multinational and R & D centers around the world in development projects of new products. Focusing on the perception of the Brazilian unit, this paper aims to present and analyze integration practices among subsidiaries, headquarters and R&D centers in product development projects in amultinational high tech company. For this purpose, was conducted an exploratory and qualitative researched operationalized by case study. Among the main results, it was noted collaboration betweenlocals marketing and engineering with the R & D centers, important role of senior management in the Brazilian unit to communicate outcomes of the strategic planning of products andtechnologies established by the headquarters to the subsidiary, the adoption of technological and information mechanisms and the application of methods such as technology roadmap.

The 2:1 cycloadducts from [3+2] 1,3-dipolar cycloaddition of nitrile oxide and vinylacetic acid. Synthesis and liquid crystal behaviour

Four liquid crystals (LC) 3,7a-bis(4-alkyloxyphenyl)-7,7a-dihydro-6H-isoxazolo[2,3-d][1,2,4]oxadiazol-6-yl)acetic acid (7a-d) were synthesised and the mesomorphic behaviour reported. The LCs were characterised as 2: 1 bisadducts, which were obtained from a double [3+2] 1,3-dipolar cycloaddition. In the first step, the cycloaddition of 4-alkyloxyphenylnitrile oxide (4a-d) and vinylacetic acid (5) gave the initial unobserved 1:1 cycloadducts 2-[3-(4-alkyloxyphenyl)-4,5-dihydroisoxazol-5-yl]acetic acid (6a-d). In the second step, the addition of a second equivalent of 4 to 6 yielded the 2: 1 bisadducts 7a-d without any traces of 6. All compounds 7a-d were unstable during the transition from the mesophase to the isotropic state upon first heating as evidenced by the large peaks in the differential scanning calorimetry traces. Due to the chemical instability of the compounds upon heating, the transition temperature related to the smectic C to smectic A transitions was acquired by means of an image processing method. X-Ray diffraction experiments were also used to analyse the liquid-crystalline phases. A theoretical calculation was performed using density functional theory (DFT) methods at the PBE1PBE/6-311+G(2d,p) level (with solvent effect) in order to get information about the energetic profile of the 2: 1 cycloaddition. DFT studies revealed that the cycloaddition process is controlled by the HOMO(dipolarophile) - LUMO(1,3-dipole), and that the double [3+2] 1,3-dipolar cycloaddition reaction is quite possible.

New activity in the large circumstellar disk of the Be-shell star 48 Librae

Aims. Spectroscopic, polarimetric, and high spectral resolution interferometric data covering the period 1995-2011 are analyzed to document the transition into a new phase of circumstellar disk activity in the classical Be-shell star 48 Lib. The objective is to use this broad data set to additionally test disk oscillations as the basic underlying dynamical process. Methods. The long-term disk evolution is described using the V/R ratio of the violet and red emission components of H alpha and Br gamma, radial velocities and profiles of He I and optical metal shell lines, as well as multi-band BVRI polarimetry. Single-epoch broad-band and high-resolution interferometric visibilities and phases are discussed with respect to a classical disk model and the given baseline orientations. Results. Spectroscopic signatures of disk asymmetries in 48 Lib vanished in the late nineties but recovered some time between 2004 and 2007, as shown by a new large-amplitude and long-duration V/R cycle. Variations in the radial velocity and line profile of conventional shell lines correlate with the V/R behavior. They are shared by narrow absorption cores superimposed on otherwise seemingly photospheric He I lines, which may form in high-density gas at the inner disk close to the photosphere. Large radial velocity variations continued also during the V/R-quiet years, suggesting that V/R may not always be a good indicator of global density waves in the disk. The comparison of the polarization after the recovery of the V/R activity shows a slight increase, while the polarization angle has been constant for more than 20 years, placing tight limits on any 3-D precession or warping of the disk. The broad H-band interferometry gives a disk diameter of (1.72 +/- 0.2) mas (equivalent to 15 stellar radii), position angle of the disk (50 +/- 9)degrees and a relatively low disk flattening of 1.66 +/- 0.3. Within the errors the same disk position angle is derived from polarimetric observations and from photocenter shifts across Br gamma. The high-resolution interferometric visibility and phase profiles show a double or even multiple-component structure. A preliminary estimate based on the size of the Br gamma emitting region indicates a large diameter for the disk (tens of stellar radii). Overall, no serious contradiction between the observations and the disk-oscillation model could be construed.

Contributo dei sistemi di fusione d'immagine mediante ecografia combinata con TAC e o RMN nella diagnosi del piccolo epatocarcinoma (< 2 cm) in pazienti con epatopatia cronica

L’ecografia è la metodica diagnostica più utilizzata come screening e follow-up nei pazienti epatopatici con o senza lesioni focali e questo grazie alle sue peculiari caratteristiche, che sono date dall’essere real-time, maneggevole, priva di radiazioni ionizzanti e con bassi costi. Tuttavia tale metodica se confrontata con la TC o la RMN, può avere importanti limiti, quali l’impossibilità di visualizzare piccole lesioni localizzate in aree anatomicamente “difficili” o in pazienti obesi, che sono già state identificate con altre tecniche, come la TC o la RMN. Per superare queste limitazioni sono stati introdotti dei sistemi di “fusione d’immagine” che consentono di sincronizzare in tempo reale una metodica real time con bassa risoluzione spaziale come l’ecografia ed una statica ad alta risoluzione come la TC o la RMN. Ciò si ottiene creando attorno al paziente un piccolo campo elettromagnetico costituito da un generatore e da un rilevatore applicato al trasduttore ecografico ed introducendo in un computer abbinato all’ecografo il “volume rendering” dell’addome del paziente ottenuto mediante TC multistrato o RM. Il preciso “ appaiamento spaziale “ delle due metodiche si ottiene individuando in entrambe lo stesso piano assiale di riferimento e almeno 3-4 punti anatomici interni. Tale sistema di fusione d’immagine potrebbe essere molto utile in campo epatologico nella diagnostica non invasiva del piccolo epatocarcinoma, che secondo le ultime linee guida, nei noduli di dimensioni fra 1 e 2 cm, richiede una concordanza nel comportamento contrastografico della lesione in almeno due tecniche d’immagine. Lo scopo del nostro lavoro è stato pertanto quello di valutare, in pazienti epatopatici, il contributo che tale sistema può dare nell’identificazione e caratterizzazione di lesioni inferiori a 20 mm, che erano già state identificate alla TC o alla RMN come noduli sospetti per HCC, ma che non erano stati visualizzati in ecografia convenzionale. L’eventuale re-identificazione con l’ecografia convenzionale dei noduli sospetti per essere HCC, può permettere di evitare, alla luce dei criteri diagnostici non invasivi un’ ulteriore tecnica d’immagine ed eventualmente la biopsia. Pazienti e Metodi: 17 pazienti cirrotici (12 Maschi; 5 Femmine), con età media di 68.9 +/- 6.2 (SD) anni, in cui la TC e la RMN con mezzo di contrasto avevano identificato 20 nuove lesioni focali epatiche, inferiori a 20 mm (13,6 +/- 3,6 mm), sospette per essere epatocarcinomi (HCC), ma non identificate all’ecografia basale (eseguita in cieco rispetto alla TC o alla RMN) sono stati sottoposti ad ecografia senza e con mezzo di contrasto, focalizzata su una zona bersaglio identificata tramite il sistema di fusione d’immagini, che visualizza simultaneamente le immagini della TC e della RMN ricostruite in modalità bidimensionale ( 2D), tridimensionale ( 3 D) e real-time. La diagnosi finale era stata stabilita attraverso la presenza di una concordanza diagnostica, secondo le linee guida internazionali o attraverso un follow-up nei casi di discordanza. Risultati: Una diagnosi non invasiva di HCC è stata raggiunta in 15/20 lesioni, inizialmente sospettate di essere HCC. Il sistema di fusione ha identificato e mostrato un comportamento contrastografico tipico in 12/15 noduli di HCC ( 80%) mentre 3/15 HCC (20%) non sono stati identificati con il sistema di fusione d’immagine. Le rimanenti 5/20 lesioni non sono state visualizzate attraverso i sistemi di fusione d’immagine ed infine giudicate come falsi positivi della TC e della RMN, poiché sono scomparse nei successivi mesi di follow-up e rispettivamente dopo tre, sei, nove, dodici e quindici mesi. Conclusioni: I nostri risultati preliminari mostrano che la combinazione del sistema di fusione dell’immagine associata all’ecografia senza e con mezzo di contrasto (CEUS), migliora il potenziale dell’ecografia nell’identificazione e caratterizzazione dell’HCC su fegato cirrotico, permettendo il raggiungimento di una diagnosi, secondo criteri non invasivi e slatentizzazndo casi di falsi positivi della TC e della RMN.

HCHO, H 2 O 2 und CH 3 OOH in der Troposphäre

In dieser Arbeit wurden im Rahmen der UTOPIHAN- und HOHPEX04-Projekte Peroxid- und Formaldehydmessungen in der Troposphäre durchgeführt und wissenschaftlich interpretiert. Die Messungen während UTOPIHAN fanden dabei an Bord eines für Forschungszwecke umgerüsteten Flugzeuges (Learjet 35A) im Wesentlichen in der freien, insbesondere in der oberen Troposphäre über Europa statt. Die Messungen während HOHPEX04 waren hingegen als Bodenmessungen an der sich abwechselnd in der bodennahen Grenzschicht und in von dieser Schicht entkoppelten Luftmassen liegenden Bergstation Hohenpeißenberg (bayerisches Voralpenland) konzipiert. Um eine quantitative Auswertbarkeit der Messungen sicherzustellen, wurden die verwendeten, auf chemischer Derivatisierung und fluorimetrischer Detektion basierenden Messgeräte AL 2001CA (Peroxide) und AL 4021 (Formaldehyd) (AEROLASER) genau charakterisiert. Dabei wurde speziell die bekannte Ozoninterferenz beider Geräte in einer großen Zahl von Laborexperimenten mit unterschiedlichen Randbedingungen bezüglich Wasserdampf- und Kohlenwasserstoffgehalt der Luft untersucht. Für beide Verbindungen wurden Höhen- sowie Breitenprofile erstellt und mit Ergebnissen eines 3D-Chemie-Transport-Modells (CTM) sowie früherer Studien verglichen. In einem weiteren Kapitel werden Ergebnisse einer quantitativen Studie zum Einfluss hochreichender Konvektion auf das HCHO-Budget in der mittleren und oberen Troposphäre präsentiert. Diese Studie kommt zu dem Schluss, dass der rasche Aufwärtstransport von Vorläufergasen von HCHO und HOx wie Methanol, Aceton und sogar gut löslicher Spurengase wie CH3OOH beziehungsweise H2O2 aus der Grenzschicht einen signifikanten, auf Grund der längeren Lebensdauer von NOx über mehrere Tage andauernden und damit großräumigen Einfluss auf die Budgets von HCHO, HOx und auch O3 in der oberen Troposphäre haben kann. Die Befunde der Studie legen desweiteren nahe, dass fehlerhafte Modellvorhersagen für die NO-Mischungsverhältnisse in der Tropopausenregion, die zum Beispiel mit Mängeln des Modells bezüglich der Höhe der Konvektion und des Stratosphären-Troposphären-Austauschs zu tun haben, hauptverantwortlich sind für gefundene Differenzen zwischen Messdaten und dem verwendeten 3D-Chemie-Transport-Modell. Um die Signifikanz der Aussagen zu erhöhen, wurde eine Sensitivitätsstudie durchgeführt, in der die Konzentration einiger chemischer Verbindungen sowie die Photolyseraten variiert wurden. Eine weitere Studie zum Einfluss verschiedener Parameter auf das CH3OOH/H2O2-Verhältnis kommt zu dem Schluss, dass dieses Verhältnis keinen idealen Indikator für Wolkenprozessierung von Luftmassen darstellt, während eine signifikant positive Abweichung vom H2O2/H2O-Verhältnis in der oberen Troposphäre ein guter Indikator für rasch aufwärts transportierte Luftmassen sein kann. Im Rahmen dieser Studie werden auch Höhen- und Breitenprofile des CH3OOH/H2O2-Verhältnisses diskutiert. In einer letzten Untersuchung zu HCHO-Messungen am Observatorium Hohenpeißenberg im Sommer 2004 werden für die in zwei Windrichtungssektoren eingeteilten Daten Korrelationen anderer Spurengase wie O3, PAN, CO, NOy und Isopren mit HCHO interpretiert. In diesem Zusammenhang wird auch versucht, den beobachteten Tagesgang von HCHO zu erklären.

Seismic sequences analysis for estimation of earthquake source parameters: corner frequency, stress drop, and seismic moment observations

The present study has been carried out with the following objectives: i) To investigate the attributes of source parameters of local and regional earthquakes; ii) To estimate, as accurately as possible, M0, fc, Δσ and their standard errors to infer their relationship with source size; iii) To quantify high-frequency earthquake ground motion and to study the source scaling. This work is based on observational data of micro, small and moderate -earthquakes for three selected seismic sequences, namely Parkfield (CA, USA), Maule (Chile) and Ferrara (Italy). For the Parkfield seismic sequence (CA), a data set of 757 (42 clusters) repeating micro-earthquakes (0 ≤ MW ≤ 2), collected using borehole High Resolution Seismic Network (HRSN), have been analyzed and interpreted. We used the coda methodology to compute spectral ratios to obtain accurate values of fc , Δσ, and M0 for three target clusters (San Francisco, Los Angeles, and Hawaii) of our data. We also performed a general regression on peak ground velocities to obtain reliable seismic spectra of all earthquakes. For the Maule seismic sequence, a data set of 172 aftershocks of the 2010 MW 8.8 earthquake (3.7 ≤ MW ≤ 6.2), recorded by more than 100 temporary broadband stations, have been analyzed and interpreted to quantify high-frequency earthquake ground motion in this subduction zone. We completely calibrated the excitation and attenuation of the ground motion in Central Chile. For the Ferrara sequence, we calculated moment tensor solutions for 20 events from MW 5.63 (the largest main event occurred on May 20 2012), down to MW 3.2 by a 1-D velocity model for the crust beneath the Pianura Padana, using all the geophysical and geological information available for the area. The PADANIA model allowed a numerical study on the characteristics of the ground motion in the thick sediments of the flood plain.

[Only a denture sore? Causes of a possible denture sore from a maxillary complete denture]

This case presentation documents the treatment sequence of a 74 years old patient who complained about a sore spot of the palatal mucosa underneath the complete denture. The intraoral examination revealed a dark spot, redness and swelling of the mucosa around this spot and halitosis. The mucosa exhibited a perforation of 3 x 10 mm in diameter. A radiographic 3-D picture showed an impacted canine tooth, which was partly covered by the palatal bone. Firstly the denture base was relieved and the swelling gradually disappeared. Then a biopsy was taken for histological analysis to exclude any malignant process. In local anesthesia the tooth was extracted, which exhibited a deep carious lesion of the entire crown. After surgery a visible collapse of the jaw crest was observed. During a period of two months the denture was relined with a soft material to improve its fit and to enhance the healing process. With a final rebasement, the existing denture could be adapted again and the patient continued to wear it.

A Portable Image Overlay Projection Device for Computer-Aided Open Liver Surgery

Image overlay projection is a form of augmented reality that allows surgeons to view underlying anatomical structures directly on the patient surface. It improves intuitiveness of computer-aided surgery by removing the need for sight diversion between the patient and a display screen and has been reported to assist in 3-D understanding of anatomical structures and the identification of target and critical structures. Challenges in the development of image overlay technologies for surgery remain in the projection setup. Calibration, patient registration, view direction, and projection obstruction remain unsolved limitations to image overlay techniques. In this paper, we propose a novel, portable, and handheld-navigated image overlay device based on miniature laser projection technology that allows images of 3-D patient-specific models to be projected directly onto the organ surface intraoperatively without the need for intrusive hardware around the surgical site. The device can be integrated into a navigation system, thereby exploiting existing patient registration and model generation solutions. The position of the device is tracked by the navigation system’s position sensor and used to project geometrically correct images from any position within the workspace of the navigation system. The projector was calibrated using modified camera calibration techniques and images for projection are rendered using a virtual camera defined by the projectors extrinsic parameters. Verification of the device’s projection accuracy concluded a mean projection error of 1.3 mm. Visibility testing of the projection performed on pig liver tissue found the device suitable for the display of anatomical structures on the organ surface. The feasibility of use within the surgical workflow was assessed during open liver surgery. We show that the device could be quickly and unobtrusively deployed within the sterile environment.

Early ship-based upper-air data and comparison with the Twentieth Century

Extension of 3-D atmospheric data products back into the past is desirable for a wide range of applications. Historical upper-air data are important in this endeavour, particularly in the maritime regions of the tropics and the southern hemisphere, where observations are extremely sparse. Here we present newly digitized and re-evaluated early ship-based upper-air data from two cruises: (1) kite and registering balloon profiles from onboard the ship SMS Planet on a cruise from Europe around South Africa and across the Indian Ocean to the western Pacific in 1906/1907, and (2) ship-based radiosonde data from onboard the MS Schwabenland on a cruise from Europe across the Atlantic to Antarctica and back in 1938/1939. We describe the data and provide estimations of the errors. We compare the data with a recent reanalysis (the Twentieth Century Reanalysis Project, 20CR, Compo et al., 2011) that provides global 3-D data back to the 19th century based on an assimilation of surface pressure data only (plus monthly mean sea-surface temperatures). In cruise (1), the agreement is generally good, but large temperature differences appear during a period with a strong inversion. In cruise (2), after a subset of the data are corrected, close agreement between observations and 20CR is found for geopotential height (GPH) and temperature notwithstanding a likely cold bias of 20CR at the tropopause level. Results are considerably worse for relative humidity, which was reportedly inaccurately measured. Note that comparing 20CR, which has limited skill in the tropical regions, with measurements from ships in remote regions made under sometimes difficult conditions can be considered a worst case assessment. In view of that fact, the anomaly correlations for temperature of 0.3–0.6 in the lower troposphere in cruise (1) and of 0.5–0.7 for tropospheric temperature and GPH in cruise (2) are considered as promising results. Moreover, they are consistent with the error estimations. The results suggest room for further improvement of data products in remote regions.

Deep ocean ventilation, carbon isotopes, marine sedimentation and the deglacial CO2 rise

The link between the atmospheric CO2 level and the ventilation state of the deep ocean is an important building block of the key hypotheses put forth to explain glacial-interglacial CO2 fluctuations. In this study, we systematically examine the sensitivity of atmospheric CO2 and its carbon isotope composition to changes in deep ocean ventilation, the ocean carbon pumps, and sediment formation in a global 3-D ocean-sediment carbon cycle model. Our results provide support for the hypothesis that a break up of Southern Ocean stratification and invigorated deep ocean ventilation were the dominant drivers for the early deglacial CO2 rise of ~35 ppm between the Last Glacial Maximum and 14.6 ka BP. Another rise of 10 ppm until the end of the Holocene is attributed to carbonate compensation responding to the early deglacial change in ocean circulation. Our reasoning is based on a multi-proxy analysis which indicates that an acceleration of deep ocean ventilation during early deglaciation is not only consistent with recorded atmospheric CO2 but also with the reconstructed opal sedimentation peak in the Southern Ocean at around 16 ka BP, the record of atmospheric δ13CCO2, and the reconstructed changes in the Pacific CaCO3 saturation horizon.