985 resultados para HS-40


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A methodology to analyze organochlorine pesticides (OCPs) in water samples has been accomplished by using headspace stir bar sorptive extraction (HS-SBSE). The bars were in house coated with a thick film of PDMS in order to properly work in the headspace mode. Sampling was done by a novel HS-SBSE system whereas the analysis was performed by capillary GC coupled mass spectrometric detection (HS-SBSE-GC-MS). The extraction optimization, using different experimental parameters has been established by a standard equilibrium time of 120 min at 85 degrees C. A mixture of ACN/toluene as back extraction solvent promoted a good performance to remove the OCPs sorbed in the bar. Reproducibility between 2.1 and 14.8% and linearity between 0.96 and 1.0 were obtained for pesticides spiked in a linear range between 5 and 17 ng/g in water samples during the bar evaluation.

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Changes in the oceanic heat storage (HS) can reveal important evidences of climate variability related to ocean heat fluxes. Specifically, long-term variations in HS are a powerful indicator of climate change as HS represents the balance between the net surface energy flux and the poleward heat transported by the ocean currents. HS is estimated from sea surface height anomaly measured from the altimeters TOPEX/Poseidon and Jason 1 from 1993 to 2006. To characterize and validate the altimeter-based HS in the Atlantic, we used the data from the Pilot Research Moored Array in the Tropical Atlantic (PIRATA) array. Correlations and rms differences are used as statistical figures of merit to compare the HS estimates. The correlations range from 0.50 to 0.87 in the buoys located at the equator and at the southern part of the array. In that region the rms differences range between 0.40 and 0.51 x 10(9) Jm(-2). These results are encouraging and indicate that the altimeter has the precision necessary to capture the interannual trends in HS in the Atlantic. Albeit relatively small, salinity changes can also have an effect on the sea surface height anomaly. To account for this effect, NCEP/GODAS reanalysis data are used to estimate the haline contraction. To understand which dynamical processes are involved in the HS variability, the total signal is decomposed into nonpropagating basin-scale and seasonal (HS(l)) planetary waves, mesoscale eddies, and small-scale residual components. In general, HS(l) is the dominant signal in the tropical region. Results show a warming trend of HS(l) in the past 13 years almost all over the Atlantic basin with the most prominent slopes found at high latitudes. Positive interannual trends are found in the halosteric component at high latitudes of the South Atlantic and near the Labrador Sea. This could be an indication that the salinity anomaly increased in the upper layers during this period. The dynamics of the South Atlantic subtropical gyre could also be subject to low-frequency changes caused by a trend in the halosteric component on each side of the South Atlantic Current.

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Dental lesions represent about 1% of oral cavity tumors being ameloblastoma the most common one. It is a tumor of epithelial origin that mainly affects the jaw, and less commonly the maxilla. Its clinical presentation is that of an asymptomatic slow-growing tumor. Despite being a benign tumor, it has an invasive behavior with a high rate of recurrence if not treated properly. Objective: To describe the cases of ameloblastoma in a reference department. Methods: Retrospective analysis of 40 cases. The variables analyzed were: age, gender, ethnicity, tumor location, type of treatment, complications and recurrence. Results: The most affected gender was male - 21 cases (52.5%); with a predominance of Caucasians - 24 cases (60%). The mean age was 35.45 years; the most common location was in.the jaw - 37 cases (92.5%). Facial asymmetry was the most frequent complaint. Of the 40 cases, 33 were submitted to surgery. Of those submitted to surgery, 24 (72.72%) underwent segmental resection, with recurrence in 4 (12.12%) cases. Conclusion: Ameloblastoma may relapse when treatment is not performed with broad surgical resection of the lesion with wide safety margins.

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The purpose of this study was to examine the relationship between cardiac autonomic control derived from heart rate variability (HRV), high-sensitivity C-reactive protein (hs-CRP) and physical activity (PA) levels measured using accelerometers. A total of 80 healthy university students volunteered to participate in this study (20.56 +/- 0.82 years, 1.36 +/- 1.5 mg/L of hs-CRP). The participants were divided into groups based on tertiles of hs-CRP. Analysis of covariance adjusted to PA was used to assess group differences in HRV. Associations between hs-CRP, HRV indices and PA were analyzed using Pearson's correlation. The participants at the highest tertile of hs-CRP (tertile 3) had lower cardiac vagal modulation (SDNN, tertile 1=78.05 +/- 5.9,tertile 2=82.43 +/- 5.9,tertile 3=56.03 +/- 6.1; SD1, tertile 1=61.27 +/- 5.3, tertile 2=62.93 +/- 5.4, tertile 3=40.03 +/- 5.5). In addition, vagal indices were inversely correlated with hs-CRP but positively correlated with PA (SDNN r=-0.320, SD1 r=-0.377; SDNN r=0.304, SD1 r=0.299; P<0.05). Furthermore, the most physically active subjects had lower levels of hs-CRP and the highest levels of vagal modulation.

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Impact cratering has been a fundamental geological process in Earth history with major ramifications for the biosphere. The complexity of shocked and melted rocks within impact structures presents difficulties for accurate and precise radiogenic isotope age determination, hampering the assessment of the effects of an individual event in the geological record. We demonstrate the utility of a multi-chronometer approach in our study of samples from the 40 km diameter Araguainha impact structure of central Brazil. Samples of uplifted basement granite display abundant evidence of shock deformation, but U/Pb ages of shocked zircons and the Ar-40/Ar-39 ages of feldspar from the granite largely preserve the igneous crystallization and cooling history. Mixed results are obtained from in situ Ar-40/Ar-39 spot analyses of shocked igneous biotites in the granite, with deformation along kink-bands resulting in highly localized, partial resetting in these grains. Likewise, spot analyses of perlitic glass from pseudotachylitic breccia samples reflect a combination of argon inheritance from wall rock material, the age of the glass itself, and post-impact devitrification. The timing of crater formation is better assessed using samples of impact-generated melt rock where isotopic resetting is associated with textural evidence of melting and in situ crystallization. Granular aggregates of neocrystallized zircon form a cluster of ten U-Pb ages that yield a "Concordia" age of 247.8 +/- 3.8 Ma. The possibility of Pb loss from this population suggests that this is a minimum age for the impact event. The best evidence for the age of the impact comes from the U-Th-Pb dating of neocrystallized monazite and Ar-40/Ar-39 step heating of three separate populations of post-impact, inclusion-rich quartz grains that are derived from the infill of miarolitic cavities. The Pb-206/U-238 age of 254.5 +/- 3.2 Ma (2 sigma error) and Pb-208/Th-232 age of 255.2 +/- 4.8 Ma (2 sigma error) of monazite, together with the inverse, 18 point isochron age of 254 +/- 10 Ma (MSWD = 0.52) for the inclusion-rich quartz grains yield a weighted mean age of 254.7 +/- 2.5 Ma (0.99%, 2 sigma error) for the impact event. The age of the Araguainha crater overlaps with the timing of the Permo-Triassic boundary, within error, but the calculated energy released by the Araguainha impact is insufficient to be a direct cause of the global mass extinction. However, the regional effects of the Araguainha impact event in the Parana-Karoo Basin may have been substantial. (C) 2012 Elsevier Ltd. All rights reserved.

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OBJECTIVE: To evaluate a comprehensive MRI protocol that investigates for cancer, vascular disease, and degenerative/inflammatory disease from the head to the pelvis in less than 40 minutes on a new generation 48-channel 3T system. MATERIALS AND METHODS: All MR studies were performed on a 48-channel 3T MR scanner. A 20-channel head/neck coil, two 18-channel body arrays, and a 32-channel spine array were employed. A total of 4 healthy individuals were studied. The designed protocol included a combination of single-shot T2-weighted sequences, T1-weighted 3D gradient-echo pre- and post-gadolinium. All images were retrospectively evaluated by two radiologists independently for overall image quality. RESULTS: The image quality for cancer was rated as excellent in the liver, pancreas, kidneys, lungs, pelvic organs, and brain, and rated as fair in the colon and breast. For vascular diseases ratings were excellent in the aorta, major branch vessel origins, inferior vena cava, portal and hepatic veins, rated as good in pulmonary arteries, and as poor in the coronary arteries. For degenerative/inflammatory diseases ratings were excellent in the brain, liver and pancreas. The inter-observer agreement was excellent. CONCLUSION: A comprehensive and time efficient screening for important categories of disease processes may be achieved with high quality imaging in a new generation 48-channel 3T system.

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Introdução: A reposição volêmica em pacientes traumatizados tem sido controvérsa. O A.T.L.S. recomenda a infusão de um grande volume de fluidos na fase inicial de tratamento, enquanto outros autores recomendam a administração somente quando do controle da hemorragia. O acesso venoso femoral é contra indicado em pacientes com trauma abdominal por temor de aumento de hemorragia. A solução hipertônica de NaCl a 7,5% (SH) possui benefícios consideráveis de logística e de recuperação hemodinâmica com pequenos volumes de infusão, semelhante as vantagens das soluções padrões isotônicas na fase pré-hospitalar. Objetivos: Criar um modelo de choque hemorrágico induzido por trauma venoso. Avaliar a hemodinâmica e o volume de hemorragia abdominal nos animais submetidos a choque hemorrágico e tratados com SH via acesso femoral e jugular. Métodos: Em 18 porcos da raça landrace, divididos em 3 grupos de 6 animais (Controle, Jugular e Femoral), foi induzido um choque hipovolêmico não controlado pela ruptura da veia cava caudal. Os animais do grupo controle (GC) foram observados por 40 minutos quanto ao seu padrão hemodinâmico de Pressão de Artéria Pulmonar (PAP), Pressão Artérial Média (PAM), Débito Cardíaco (DC) e Fluxo de Veia Porta (FVP), porém sem reposição volêmica. Os animais dos grupos Femoral (GC) e Jugular (GJ) foram tratados com 4 ml/Kg de solução hipertônica de NaCl a 7,5% (SH) aos 20 minutos de experimento. Ao final do experimento, o volume de hemorragia abdominal foi mensurado.Resultados: O grupo controle (GC) apresentou queda dos valores hemodinâmicos aos 10 minutos e estes permaneceram estáveis até o final do experimento. Os animais dos grupos tratamento (GF e GJ) apresentaram melhora da hemodinâmica aos 30 minutos, sem aumento da hemorragia abdominal. Conclusão: A solução hipertônica de NaCl (SH) permitiu a melhora parcial da hemodinâmica no modelo de choque hipovolêmico, sem aumento da hemorragia, independentemente do acesso utilizada para a infusão.

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Gastroesophageal junction (GEJ) adenocarcinoma are uncommon before age of 40 years. While certain clinical, pathological and molecular features of GEJ adenocarcinoma in older patients have been extensively studied, these characteristics in the younger population remain to be determined. In the recent literature, a high sensitivity and specificity for the detection of dysplasia and esophageal adenocarcinoma was demonstrated by using multicolor fluorescence in situ hybridization (FISH) DNA probe set specific for the locus specific regions 9p21 (p16), 20q13.2 and Y chromosome. We evaluated 663 patients with GEJ adenocarcinoma and further divided them into 2 age-groups of or= 50 years, rispectively. FISH with selected DNA probe for Y chromosome, locus 9p21 (p16), and locus 20q13.2 was investigated with formalin fixed and parassin embedded tissue from surgical resections of 17 younger and 11 older patients. Signals were counted in > 100 cells with each given histopathological category. The chromosomal aberrations were then compared in the 2 age-groups with the focus on uninvolved squamous and columnar epithelium, intestinal metaplasia (Barrett's mucosa), glandular dysplasia, and adenocarcinoma. Comparisons were performed by the X2 test, Fisher's exact test, Student's t-test and Mann-Whitney U-test as appropriate. Survival was estimated by the Kaplan-Meier method with univariate analysis by the log-rank. Significance was taken at the 5% level. There was no difference in the surgical technique applied in both age groups and most patients underwent Ivor Lewis esophagectomy. Among clinical variables there was a higher incidence of smocking history in older patient group. We identified a progressive loss of Y chromosome from benign squamos epithelium to Barrett's mucosa and glandular dysplasia, and, ultimately, to a near complete loss in adenocarcinoma in both age groups. The young group revealed significantly more losses of 9p21 in both benign and neoplastic cells when compared to the older patients group. In addition, we demonstrated an increase in the percentage of cells showing gain of locus 20q13.2 with progression from benign epithelium through dysplasia to adenocarcinoma with almost the same trend in both the young and the older patients. When compared with the older age-group, younger patients with GEJ adenocarcinoma possess similar known demographics, environmental factors, clinical, and pathologic characteristics. The most commonly detected genetic aberrations of progressive Y chromosomal loss, 9p21 locus loss, and 20q13 gains were similar in the younger and older patients. However the rate of loss of 9p21 is significantly higher in young patients, in both the benign and the neoplastic cells. The loss of 9p21, and possibly, the subsequent inactivation of p16 gene may be one of the molecular mechanisms responsible for the accelerated neoplastic process in young patients.

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Der astrophysikalische r-Prozeß (schneller Neutroneneinfang), ist verantwortlich für die Nukleosynthese einer großen Zahl von Elementen, die schwerer als Eisen sind. Benutzt man das ''waiting-point''-Modell, so kann die Häufigkeitsverteilung der Elemente durch drei nukleare und drei stellare Input-Parameter beschrieben werden. Für einen gegebenen Satz von stellaren Parametern definiert die Neutronenseparationsenergie (Sn) den r-Prozeß-Pfad. Die beta-Zerfall-Halbwertszeit (T1/2) der Kerne im r-Prozeß-Pfad bestimmt die Häufigkeit des Vorläufers und bezieht man die Neutronenemissionswahrscheinlichkeit (Pn) mit ein, so auch die endgültige Häufigkeitsverteilung. Von besonderer Wichtigkeit sind die neutronenreichen ''waiting-point''-Isotope. Zum Beispiel sind die N=82 Isotope verantwortlich für den solaren A~130 Häufigkeits-Peak. Diese Arbeit befaßt sich mit der Identifizierung und der Untersuchung von Zerfallseigenschaften neutronenreicher Isotope des Mangan (A=61 bis 69) und Cadmium (A=130 bis 132). Neutronenreiche Nuklide zu erzeugen und zu detektieren ist ein komplizierter und zeitaufwendiger Prozeß, nichts desto trotz erfolgreich. Das Hauptproblem bei dieser Art von Experimenten ist der hohe isobare Untergrund. Aus diesem Grunde wurden speziell entwickelte Anregungsschemata für Mangan und Cadmium eingesetzt, um die gewünschten Isotope mittels Laser-Resonanzionisation chemisch selektiv zu ionisieren. Bei CERN/ISOLDE war es möglich im Massenbereich von 60^Mn bis 69^Mn neue Halbwertszeiten und Pn-Werte zu bestimmen. Für 64^Mn und 66^Mn konnten darüber hinaus erstmals noch partielle Zerfallsschemata aufgestellt werden. Es zeigte sich, daß die Ergebnisse teilweise recht überraschend waren, da sie nicht durch das QRPA-Modell vorhergesagt wurden. Mit Hilfe vergleichender Studien des Gesamttrends der Niveausystematiken der gg-Kerne von 26_Fe, 30_Zn, 32_Ge, 24_Cr und 28_Ni konnte ein Verschwinden der sphärischen N=40 Unterschale und die Existenz einer neuen Region mit signifikanter Deformation nachgewiesen werden, die vermutlich ihr ''Zentrum'' bei 64^Cr hat. Ebenfalls zeigen Studien der Niveausystematik bei 48Cd und der Vergleich mit 46_Pd, 54_Xe, 52_Te und 50_Sn, erste Hinweise eines Schalenquenchings bei N=82. Es wurde die Messung der Halbwertszeit von 130^Cd verbessert und die Halbwertszeiten von 131^Cd und 132^Cd erstmals bestimmt. Die neuen Daten können nur erklärt werden, wenn man bei der QRPA-Rechnung verbotene Übergänge mitberücksichtigt. Es genügt nicht, die Rechnung für reinen Gamow-Teller-Zerfall durchzuführen.

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In Experimenten an lasergekühlten, in einer linearen Paulfalle gespeicherten $Ca^+$-Ionen wurde dieLebensdauer des metastabilen $3D_{5/2}$-Niveaus durch Beobachtung von Quantensprüngen einzelner Ionen zu 1100(18)msbestimmt. Systematische Fehler durch quenchende Stöße oder Stark-Mischen durch das Speicherfeld liegen unterhalb dererreichten Genauigkeit. Abweichungen von früheren Messungen konnten durch eine vernachlässigte Abhängigkeit derLebensdauer von der Laserleistung des Rückpumplasers erklärt werden. Das Endergebnis zeigt gute Übereinstimmung mitneueren theoretischen Werten. In weiteren Messungen an zehn Ionen wurde in einigen Messreihen eine deutliche Reduktionder Lebensdauer gegenüber einem einzelnen Ion festgestellt. Dabei wurden mehr koinzidente Zerfälle von zwei und dreiIonen beobachtet als für unabhängige Teilchen zu erwarten. In einem Ionenkristall wurde eine räumliche Trennung atomarer Zustände erreicht. Dabei wurde ein Teil der Ionen einesKristalls aus einigen hundert Ionen in den metastabilen Zustand gepumpt, der von den Kühllasern vollständig entkoppeltist. Durch sympathetische Kühlung werden diese Ionen weiterhin gekühlt und der Kristall schmilzt nicht. Durch denLichtdruck, den die Kühllaser ausgeüben, werden die Ionen nach atomaren Zuständen sortiert, weil die lasergekühltenIonen einen Rückstoß erfahren, die übrigen aber nicht. Für zukünftige Experimente wurden Verbesserungen des experimentellen Aufbaus auf den Weg gebracht. So wurden Methodenund Komponenten für eine verbesserte Frequenzstabilisierung der Diodenlaser entwickelt.

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In linearen Paulfallen gespeicherte und lasergekühlte Ionen stellen in weiten Bereichen der Physik ideale Objekte hinsichtlich störungsfreier und präziser Messungen atomarer Übergangsfrequenzen und der gezielten Manipulation von Quantenzuständen dar. Eine Einschränkung dieser optimalen Bedingungen erfolgt durch Heizmechanismen, die aus Abweichungen des Speicherpotentials von der idealen Quadrupolform resultieren. Höhere Potentialordnungen führen zu einer Kopplung der radialen Bewegungsmoden und bei bestimmten Speicherparametern zu nichtlinearen Resonanzen. Hierbei werden die Ionenbahnen durch eine Energieaufnahme aus dem Speicherfeld destabilisiert. Dieses kann zu Linienverbreiterungen, einer Limitierung der Kohärenzzeiten und unter Umständen zu einem Ionenverlust führen. Die systematische Untersuchung dieser Instabilitäten in einer linearen Paulfalle erfolgt durch Spektroskopie an einer kleinen Anzahl lasergekühlter ^40Ca^+ - Ionen. Der experimentell zugängliche Speicherbereich wird mit hoher Auflösung abgetastet. Durch eine eingehende Quantifizierung der Falleneigenschaften werden die nichtlinearen Resonanzen eindeutig den erzeugenden Potentialtermen zugeordnet. Die Resonanzlinien zeigen eine charakteristische Aufspaltung, deren Größe vom angelegten Axialpotential bestimmt wird. Diese zusätzliche Kopplung der Radialbewegung an die Axialbewegung führt zu einer modifizierten Resonanzbedingung. Nichtlineare Resonanzen treten massenspezifisch auf. Da eine präzise Kontrolle der Axialpotentiale sehr einfach ist, könnten die beobachteten radial-axial koppelnden Resonanzen eine Anwendung in der Massenspektrometrie finden.

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Forschungsreisen, deutsche Forschungsreisende, Wissenschaftsgeschichte, Ethnographie, ethnographische Quellen, Karawanenreisen, Sklaverei, Kolonialismus, Portugiesen in Afrika, westliches Zentralafrika, Angola