Relevant bibliographies by topics / Effusive

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Effusive'

Author: Grafiati
Published: 10 December 2022
Last updated: 19 July 2025

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Journal articles on the topic "Effusive"

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D'Souza, Melroy S., Kaitlin Shinn, and Anup D. Patel. "Posttraumatic Subacute Effusive-Constrictive Pericarditis After a Motor Vehicle Accident." Texas Heart Institute Journal 47, no. 3 (2020): 233–35. http://dx.doi.org/10.14503/thij-19-7002.

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Effusive-constrictive pericarditis is typically caused by tuberculosis or other severe inflammatory conditions that affect the pericardium. We report a case of effusive-constrictive pericarditis consequent to a motor vehicle accident. A 32-year-old man with gastroesophageal reflux disease presented with severe substernal chest pain of a month's duration and dyspnea on exertion for one week. Echocardiograms revealed a moderate pericardial effusion, and the diagnosis was subacute effusive-constrictive pericarditis. After thorough tests revealed nothing definitive, we learned that the patient had been in a motor vehicle accident weeks before symptom onset, which made blunt trauma the most likely cause of pericardial injury and effusion. Medical management resolved the effusion and improved his symptoms. To our knowledge, this is the first report of effusion from posttraumatic constrictive pericarditis associated with a motor vehicle accident. We encourage providers to consider recent trauma as a possible cause of otherwise idiopathic pericarditis.
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Adamson, Van W., Jennifer N. Slim, Kenneth M. Leclerc, and Ahmad M. Slim. "A Rare Case of Effusive Constrictive Cholesterol Pericarditis: A Case Report and Review." Case Reports in Medicine 2013 (2013): 1–2. http://dx.doi.org/10.1155/2013/439505.

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Effusive constrictive cholesterol pericarditis is exceedingly rare. Most cases have an unclear etiology but can be associated with rheumatoid arthritis, tuberculosis infection, and hypothyroidism. The hallmark of the effusion is the distinctively high levels of cholesterol. We present the case of a 68-year-old male with prolonged symptoms of dyspnea with associated moderate pericardial effusion that were later determined to be constrictive effusive etiology, and the patient was referred for stripping with pathologic cholesterol crystal formation on pathology review.
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Wang, Wen, Yan Yan, Yeqi Zhou, and Jiahuan Cui. "Review of Advanced Effusive Cooling for Gas Turbine Blades." Energies 15, no. 22 (2022): 8568. http://dx.doi.org/10.3390/en15228568.

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Turbine inlet temperature has continuously increased to improve gas turbine performance during the past few decades. Although internal convection cooling and traditional film cooling have contributed significantly to the current achievement, advanced cooling schemes are needed to minimize the coolant consumption and maximize the cooling efficiency for future gas turbines. This paper conducts a comprehensive review of advanced effusive cooling schemes for gas turbine blades. First, the background and the history of turbine blade cooling are introduced. Then, the metrics of effusive cooling efficiency are defined. Next, effusion cooling, impingement/effusion cooling, and transpiration cooling are reviewed. The flow and heat transfer mechanisms of the cooling schemes are emphasized, and the design trends of the cooling schemes are revealed. Finally, the conclusions and future research perspectives are summarized.
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Erickson, Brandon, Gurpreet Dhaliwal, Mark C. Henderson, Ezra Amsterdam, and Joseph Rencic. "Effusive Reasoning." Journal of General Internal Medicine 26, no. 10 (2011): 1204–8. http://dx.doi.org/10.1007/s11606-011-1785-7.

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Kelly, Bryan, and Darlene Nelson. "RECURRENT LEFT PLEURAL EFFUSION CAUSED BY EFFUSIVE CONSTRICTIVE PERICARDITIS." Chest 156, no. 4 (2019): A1915. http://dx.doi.org/10.1016/j.chest.2019.08.1650.

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SANTARONE, M. "Effusive-constrictive pericarditis." Heart 83, no. 5 (2000): 556. http://dx.doi.org/10.1136/heart.83.5.556.

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Ayan, Mohamed, Aisha Siraj, and Sabha Bhatti. "EFFUSIVE CONSTRICTIVE PERICARDITIS." Journal of the American College of Cardiology 71, no. 11 (2018): A2383. http://dx.doi.org/10.1016/s0735-1097(18)32924-3.

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Sagristà-Sauleda, Jaume, Juan Angel, Antonio Sánchez, Gaietà Permanyer-Miralda, and Jordi Soler-Soler. "Effusive–Constrictive Pericarditis." New England Journal of Medicine 350, no. 5 (2004): 469–75. http://dx.doi.org/10.1056/nejmoa035630.

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Syed, Faisal F., Mpiko Ntsekhe, Bongani M. Mayosi, and Jae K. Oh. "Effusive-constrictive pericarditis." Heart Failure Reviews 18, no. 3 (2012): 277–87. http://dx.doi.org/10.1007/s10741-012-9308-0.

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Zurick, Andrew O., and Allan L. Klein. "Effusive-Constrictive Pericarditis." Journal of the American College of Cardiology 56, no. 1 (2010): 86. http://dx.doi.org/10.1016/j.jacc.2009.10.088.

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Dissertations / Theses on the topic "Effusive"

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Ntsekhe, Mpiko. "Studies of effusive constrictive pericarditis." Doctoral thesis, University of Cape Town, 2011. http://hdl.handle.net/11427/11586.

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Includes abstract.<br>Includes bibliographical references (p.127-140).<br>Tuberculous (TB) pericarditis is associated with a mortality rate of 17-40% despite treatment with anti-tuberculosis drugs. The complications of TB pericarditis that confer mortality and morbidity are pericardial tamponade, effusive constrictive pericarditis, and constrictive pericarditis. Whilst the diagnosis and treatment of pericardial tamponade and constriction are well established, there is a paucity of evidence on the frequency and significance of tuberculous effusive constrictive pericarditis. The primary purpose of this work was to determine the prevalence, predictors, fractal (geometric) structure, biomarker signature, and outcome of effusive constrictive TB pericarditis.
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Cáceres, Acevedo Francisco Andrés. "Magma storage conditions and eruptive dynamics of post-glacial effusive volcanism at Laguna del Maule Volcanic field." Tesis, Universidad de Chile, 2016. http://repositorio.uchile.cl/handle/2250/140208.

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Magíster en Ciencias, Mención Geología<br>Geólogo<br>La mayoría de los campos volcánicos monogenéticos están constituidos principalmente por productos piroclásticos de composición basáltica. Los volúmenes emitidos por cada centro eruptivo tienden a ser pequeños, menores a 1 km3, donde su actividad puede durar días a años, mientras que el campo volcánico completo se puede desarrollar y perdurar por millones de años, pudiendo superar en volumen a un volcán poligenético. En este sentido, el Campo Volcánico Laguna del Maule (CVLdM) representa un caso excepcional con más de 350 km3 de material basáltico a riolítico, eruptado mayormente de manera efusiva desde el Pleistoceno. En este trabajo se propone un modelo volcanológico-petrológico de la dinámica eruptiva de las lavas post-glaciales emplazadas en la parte Oeste del CVLdM, analizando la evolución del magma en profundidad, el ascenso de magma por los conductos eruptivos y el emplazamiento de lavas en superficie. Se estudió la morfometría, mineralogía y química de seis lavas y un domo del CVLdM para modelar las condiciones termodinámicas pre-eruptivas del magma y su evolución, incluyendo posibles procesos magmáticos causantes de su migración y ascenso a la superficie. Las lavas analizadas tienen una composición química andesítica a riolítica, morfología de bloques, volúmenes de 0.03 a 1.16 km3, largos máximos de 10 km, anchos máximos de 5 km y espesores máximos de 140 m. Los resultados indican la presencia de un sistema magmático formado en cuatro etapas, comenzando con la acumulación de magma andesítico basáltico a andesítico debido a múltiples intrusiones. Posteriormente, procesos de cristalización desarrollaron un reservorio tipo mush cristalino (13-17 km, 970-1025 °C) con extracción y ascenso de líquido intersticial. Una tercera etapa de estancamiento del magma en ascenso proveniente de la extracción más profunda (7-11 km, 900-970 °C), permitió la formación de un nuevo mush cristalino más evolucionado. Finalmente, una nueva extracción y ascenso del líquido intersticial riolítico formó un reservorio magmático riolítico pobre en cristales (~5 km, 760-800 °C) bajo el lago. El constante recalentamiento debido a múltiples intrusiones permitó al sistema magmático permanecer activo en el largo plazo, producto de variadas intrusiones de magma máfico en el caso del reservorio profundo y magma silícico en el caso del reservorio más somero.
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Bourgeois, Renée Lise. "Physical characteristics of proximal Cleetwood airfall deposits, Crater Lake, OR : the transition from explosive to effusive eruption /." View full-text version online through Crater Lake Digital Research Collection View online version of CD accompanying Appendix B through Crater Lake Digital Research Collection, 1998. http://craterlakelib.oit.edu/u?/craterlake,125.

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Thesis (M.S.)--University of Oregon, 1998.<br>Typescript. Includes vita and abstract. CD-ROM contains SEM backscatter electron images for appendix B. Includes bibliographical references (leaves 183-186). Also available via the Internet.
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Minghetti, Nicoletta. "Le grandi effusioni basaltiche." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2019. http://amslaurea.unibo.it/18728/.

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Il lavoro di tesi è svolto con l’obiettivo di illustrare le "Grandi Effusioni Basaltiche" e le conseguenze di impatto ambientale che risultano da questo tipo di attività vulcanica. Le effusioni basaltiche sono fenomeni eruttivi sostenuti dalla possibilità del magma di muoversi dalla regione sorgente alla superficie, caratteristica dovuta alla minore densità del magma che nel campo di gravità subisce una forza di galleggiamento che lo spinge verso l’alto. Questi fenomeni eruttivi sono caratterizzati dall'effusione di enormi quantità di lava che si estendono per migliaia di chilometri con volumi dell’ordine di grandezza di alcune migliaia di chilometri cubi e disperdono aerosol nell'atmosfera dovuti al degassamento di magma durante la risalita. Per questi motivi, una grande effusione basaltica ha il potere di causare cambiamenti ambientali ed estinzioni di massa, con effetti sull'evoluzione biologica.
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Preece, Katie. "Transitions between effusive and explosive activity at Merapi volcano, Indonesia : a volcanological and petrological study of the 2006 and 2010 eruptions." Thesis, University of East Anglia, 2014. https://ueaeprints.uea.ac.uk/49599/.

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The 2010 explosive eruption (VEI 4) of Merapi volcano, Indonesia, was the volcano’s largest since 1872. In contrast, volcanism over the last century has been characterised by dome-building and gravitational dome collapse, such as in 2006 (VEI 1). The driving forces behind effusive and explosive activity, as well as factors that affect transitions in eruptive style are investigated through petrological and textural analysis, using the well-documented 2006 and 2010 eruptions as case-studies. Pre- and syn-eruptive crystallisation and degassing processes are examined via whole rock geochemical analysis, mineral compositions and thermobarometry, quantitative textural analysis of feldspar microlites and analysis of volatiles and light lithophile elements in melt inclusions. These data were gathered from a detailed set of stratigraphically controlled samples, correlated to eruptive chronology and style, which were collected during several field campaigns. Both the 2006 and 2010 eruptions produced basaltic andesite, similar in terms of major and trace element compositions. A major zone of crystallisation is proposed at between ~ 14 and 29 km depth, although crystallisation occurs throughout the crust. Magmatic temperatures are estimated to be ~920–1020 °C. Maximum H2O contents reach 3.94 wt.% in 2010 melt inclusions and up to 3.73 wt.% in those from 2006. CO2 concentrations are < 200 ppm, although they may reach up to 695 ppm in some melt inclusions from the 2010 eruption. An exsolved brine phase was present during both eruptions which “buffered” melt Cl concentrations and enriched Li at shallow depths within the conduit or edifice. Eruptive style and transitions at Merapi are linked to magma ascent rate, crystallisation and open- and closed-degassing processes, which can be influenced by magma influx. The findings of this work are crucial for understanding the full range of eruptive behaviour that Merapi is capable of producing.
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Lesage, Elodie. "Etude du cryovolcanisme sur Europe Cryomagma ascent on Europa Constraints on effusive cryovolcanic eruptions on Europa using topography obtained from Galileo images." Thesis, université Paris-Saclay, 2020. http://www.theses.fr/2020UPASJ008.

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Europe est une lune de Jupiter couverte de glace d’eau, et abritant un océan interne global d’eau liquide d’une centaine de kilomètres d’épaisseur. L’intérieur d’Europe est réchauffé par les forces de marées induites par la présence de Jupiter, qui fournissent une quantité d’énergie suffisante à maintenir une activité géologique vigoureuse sur ce satellite. La surface d’Europe est très jeune avec un âge estimé à 70-90 Ma, ce qui démontre son ressurfaçage récent. De nombreuses structures géologiques ont été identifiées à la surface d’Europe, et certaines comme les plaines lisses, les dômes ou les dépôts sombres pourraient indiquer la présence de réservoirs d’eau liquide ou de saumures (cryomagma) stockés dans la couche de glace. Nous proposons dans cette thèse un modèle d’éruption cryovolcanique depuis un réservoir de cryomagma contenu dans la couche de glaces. Le moteur de l’éruption est la surpression générée dans le réservoir par le gel du cryomagma, qui peut être suffisante pour entrainer la fracturation de la couche de glaces sus-jacente et laisser les cryolaves se répandre en surface. Ce modèle prédictif permet de connaître les caractéristiques d’une éruption telles que sa durée et le volume de cryolave émis en surface en fonction de la profondeur du réservoir. Il permet aussi d’évaluer la pression dans le réservoir et la vitesse du fluide s’en échappant au court de l’éruption. Nous avons testé l’influence de la composition du cryomagma et de la rhéologie de la couche de glace sur la faisabilité d’une éruption. Nous avons notamment modélisé la déformation d’un réservoir contenu dans une couche de glace viscoélastique. Quelques images d’Europe prises par la sonde Galileo dans les années 1990 montrent des structures lisses quasi-circulaires que nous interprétons comme de possibles écoulements de cryolaves à la surface. Nous avons souhaité utiliser le volume de ces objets afin de contraindre notre modèle d’éruption. Pour ce faire, nous avons généré des modèles numériques de terrain (MNT) de ces images grâce à la photoclinométrie, et plus particulièrement avec l’AMES StereoPipeline (ASP) fourni par la NASA. Nous avons porté une attention particulière à l’estimation des incertitudes sur les MNT en menant une étude de sensibilité de l’ASP. Nous avons pu mesurer le volume de quatre plaines lisses, et en déduire la taille des réservoirs de cryomagma requis pour les créer lors d’éruptions. Les missions JUICE (ESA) et Europa Clipper (NASA) devraient partir dans les prochaines années et permettront une étude plus poussée de la surface d’Europe. Cette thèse a pour vocation d’aider à la sélection des zones les plus susceptibles de présenter des bio-signatures en vue de ces missions. Les plaines lisses étudiées dans cette thèse peuvent possiblement représenter des zones d’échange d’eau liquide entre la surface et la sub-surface d’Europe, et sont donc d’un grand intérêt pour l’exploration future de cette lune<br>Europa is a Jupiter’s moon covered with a water-ice layer, hiding a global liquid water ocean approximately 100 km thick. Europa’s interior is heated by the tidal forces induced by Jupiter, that provide enough energy to maintain a vigorous geological activity on this moon. Europa’s surface is very young, with an age estimated around 70-90 Ma, which demonstrates a recent resurfacing of the moon. Various geological features have been identified at Europa’s surface, and some of them, like the smooth plains, domes and chaos might indicate the presence of sub-surface reservoirs of liquid water or brines (cryomagma). In this thesis, we propose a cryovolcanic eruption model from a cryomagma reservoir stored in the ice crust. The overpressure generated during the cryomagma freezing could be high enough to fracture the ice crust and let the cryolava rise toward the surface and spread on it. This predictive model allows us to know the duration of an eruption, and the total cryolava volume erupted as a function of the reservoir depth in the ice crust. It also allows us to calculate the pressure in the reservoir and the fluid velocity in the fracture during the eruption. We investigated the influence of the cryomagma composition and the ice crust rheology on the possibility of an eruption. We finally modeled the deformation of a reservoir stored in a viscoelastic ice crust. A few images taken by the Galileo spacecraft during the 1990’s show quasi-circular smooth features, that may be interpreted as cryolava flows. We wanted to use these images to constrain our eruption model by measuring the volume of these objects. To do this, we generated digital elevation models (DEMs) of these images thank to the photoclinometry technique. We used the AMES StereoPipeline (ASP) tool, provided by the NASA. We estimated the uncertainties on the DEMs produced by the ASP by doing a sensitivity study of this tool. We also measured the volume of four smooth plains and deduced the size of reservoir needed to generate these thanks to our eruption model. Two missions, JUICE (ESA) and Europa Clipper (NASA) will be launch in the next years and should provide new insights on Europa’s sub-surface. In this context, this thesis could help to select the zones the more likely to show biosignatures. The smooth plains studied in this thesis might be linking the interior and the surface of the Europa, which could present a great interest for the future exploration of this moon
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Garel, Fanny Clémentine. "Modélisation de la dynamique et du refroidissement des coulées de lave : vers une utilisation de la télédétection thermique dans la gestion d'une éruption effusive." Paris 7, 2012. http://www.theses.fr/2012PA077031.

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Pendant une éruption effusive, le principal risque est posé par l'avancée des coulées de lave depuis l'évent. Le débit éruptif contrôle en grande partie cette dynamique, et sa détermination en temps réel est un point-clé dans la gestion du risque volcanique. Un suivi de l'éruption peut être réalisé par satellite, avec des mesures régulières du signal thermique (radiance) émis en surface par le champ de lave. Cette thèse étudie l'évolution du signal thermique de surface pour des courants de gravité qui avancent et se refroidissent simultanément. Pour un fluide dont la viscosité ne dépend pas de la température et injecté à débit constant, des expériences de laboratoire et un modèle théorique montrent que la radiance augmente pendant un premier stade transitoire avant d'atteindre un palier. Pour des paramètres de coulées de lave, la théorie prédit que le signal radié stationnaire dépend principalement du débit éruptif, et la puissance prédite est en bon accord avec des données de terrain. Des expériences avec un matériel de type cire montrent que la solidification ralentit l'étalement du courant, qui se fait au travers de débordements ponctuels. Il n'y a alors pas d'état stationnaire dans le signal thermique de surface, mais le matériel fluide (le plus chaud) radie un flux de chaleur constant, dont la valeur augmente avec le débit imposé à la source. La thèse explore également l'effet de la topographie et de la variation temporelle du débit sur la dynamique et le signal thermique de l'écoulement. L'utilisation quantitative de la télédétection thermique nécessite une modélisation appropriée de la rhéologique effective et de la structure thermique interne des coulées de lave<br>During an effusive eruption, the main hazard is related to how fast and how far lava will spread from the volcanic vent before it stops. The effusion rate exerts an important control on the advance of lava flows, and its real-time estimate during an eruption is a key issue for hazard assessment. The eruption can be monitored by remote-sensing, with periodic satellite acquisitions of the thermal signal (radiance) emitted by the surface of the lava flow field. This thesis investigates the evolution of the surface thermal signal of gravity currents, simultaneously spreading and cooling. For a fluid with a temperature-independent viscosity, supplied at a constant rate, laboratory experiments and a simple theoretical model show that the surface thermal signal first increases during a transient stage before reaching a plateau value. For lava flow parameters, the theoretical model predicts that the steady radiant heat flux mostly dépends on the effusion rate; and the predited power concurs at first-order with data from natural lava flows. Experiments using a wax-like material show that solidification slows down the spreading of the current, which advances with episodic overflow events. There is no steady state for the bulk surface thermal signal, and only the fluid part of the flow (the hottest material) radiates a constant heat flux, whose value increases with increasing input rate. The quantitative use of thermal remote-sensing requires an appropriate modelling of the effective rheology and of the internal thermal structure of lava flows
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Collins, Matthew C. J. "Casing effusion cooling." Thesis, University of Oxford, 2014. https://ora.ox.ac.uk/objects/uuid:8a7204f5-9436-4c11-b6d6-25aef0bff8f7.

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The design, modelling and testing of a film cooling system intended for the casing of an unshrouded HP turbine rotor is described in this thesis. Due to the dense network of small film cooling holes employed in such a system, this is often referred to as a casing effusion cooling scheme. Though there are patent references to such systems, there is as yet very limited published material on the aero thermal performance of such film cooling schemes. The casing of an unshrouded HP rotor is an incredibly hostile environment, witnessing the periodic passing of the HP rotor tips within close proximity at a frequency of &Tilde;10 kHz. These blade passing events subject the casing to extremely large amplitude fluctuations of pressure and heat load, which may at first seem to preclude the use of a film cooling scheme. This thesis details many theoretical, computational and experimental advancements related to the research topic. Highlights include: The introduction of a new fundamental mechanism to the field of film cooling, the propagation and reflection of pressure waves within film cooling holes and the impact on film cooling performance. The development of new miniature thin film heat flux gauges manufactured using a new process. Sensor resolution is improved by a factor of seven. The first published computational model reporting heat transfer data on a film cooled rotor casing. Improvements to heat transfer data processing techniques and theory. These are applied to experimental work to produce the highest resolution heat transfer data obtained on the casing of a scaled rotating transonic HP rotor for both uncooled and cooled geometries. Computational models are used to demonstrate that coolant injection on the rotor casing reduces the over-tip leakage mass flow, offsetting the spoiling and mixing losses that film cooling schemes introduce. Much of the work in this thesis is based on papers that have been submitted to or are pending submission. To date three papers have been presented at conference with two published in journals and the third recommended and pending journal publication. Two other papers are pending submission. A patent has also been filed with the European and American patent office regarding novel film cooling hole shapes designed to make use of acoustic effects.
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CUNHA, M. N. PINTO DA. "IMMUNOPROFILE IN EFFUSION CYTOLOGY." Doctoral thesis, Università degli Studi di Milano, 2010. http://hdl.handle.net/2434/150058.

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BACKGROUND: Cytology has a crucial role for diagnosing pleural and abdominal effusions. A prompt accurate diagnosis has both prognostic and therapeutic significance. However, cell morphology alone is not always sufficient to formulate such a diagnosis. In human medicine, immunocytochemistry of effusion cytology has now standardized procedures that provide reliable insights into various diagnostic dilemmas. OBJECTIVE: To describe the method of immunocytochemistry in effusion cytology and to estimate the value of a panel of markers in identifying cells in canine and feline effusions. MATERIALS AND METHODS: Human, feline and canine mesothelial cells were isolated in culture. Western‐blot (WB) analysis was used to ascertain antibody cross‐reactivity for all the markers, with the exception of HBME‐1. Forty‐four cytospined or smeared effusion specimens from dogs and cats with a cytological diagnosis of reactive effusion or malignancy of non‐hematopoietic origin were stained with a standard panel of Vimentin, Cytokeratin (CK) AE1/AE3, CK 5/6 and HBME‐1 as mesothelial cell markers; desmin as mesothelial cell malignancy marker; and CK7/CK20 as a marker of metastasis. Malignancy was confirmed by histologic evaluation; non‐malignant conditions were confirmed by follow‐up. Sensitivities, specificities and predictive values were calculated. RESULTS: The WB analysis confirmed the specific crossreactivity of the human antibodies for canine and feline proteins in mesothelial tissue. No significant differences were found between canine and feline results. Vimentin/cytokeratin coexpression had a sensitivity of 79% and a specificity of 92%, HBME‐1 had 89% sensitivity and 23% specificity, and CK5/6 had 26% sensitivity and 100% specificity for mesothelial cells. Desmin had only 20% specificity for benign mesothelial cells, while CK7‐/CK20+ had a specificity of 79% and sensitivity of 30% for metastatic cells on effusions. CONCLUSION: Immunocytochemistry can be applied in effusion samples, and valuable results can be obtained. The most useful marker, with the highest overall accuracy for the identification of mesothelial cells in effusion, is the Vim/CK coexpression, being CK5/6 the more specific and HBME‐1 the more sensitive antibody. Desmin is not useful for discriminating between benign and malignant mesothelial cells. The coordinate expression of CK7‐/CK20+ has not proved to be useful on the identification of metastatic cells on effusions.
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Clive, Amelia Olga. "Management of malignant pleural effusion." Thesis, University of Bristol, 2015. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.683557.

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Introduction Malignant pleural disease is a growing clinical problem and often results in substantial breathlessness for patients due to the accumulation of malignant pleural effusion. Dedicated pleural services are becoming more prevalent and a wider selection of treatment strategies are now available. This thesis evaluates a number of different aspects relating to the prognostication and treatment of patients with malignant pleural disease through a series of 4 studies. Methods The first study uses data from three, international, prospectively collected databases of patients with malignant pleural effusion to evaluate factors that predict patients' survival. From this data, the LENT prognostic score is developed and validated to assist clinicians in risk stratifying patients and thereby helping them to select appropriate treatment strategies. The second study is a systematic review of the literature, evaluating all the published randomised controlled trial (RCT) data on the management of malignant pleural effusion using network meta-analysis. These results highlight the efficacy of talc poudrage in obtaining a pleurodesis, but also emphasise the heterogeneity of the available evidence and the paucity of robust data on symptom based outcomes and adverse effects. The Zoledronic Acid (ZA) Trial is a pilot, RCT evaluating whether intravenous ZA is an effective potential treatment for MPE. In this small, diverse cohort, no significant difference was seen in the radiology, biomarkers or symptoms of the ZA group compared with those who received placebo. Finally, the SMART trial is a multi-centre RCT, evaluating the role of prophylactic radiotherapy in mesothelioma. 203 patients have been recruited to the study, which is currently in follow up and the results are awaited in winter 2015. Discussion This thesis adds to our understanding regarding the prognostication and management of patients with malignant pleural disease. The data will help to inform clinicians and future research studies regarding the optimal management of these patients
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Books on the topic "Effusive"

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Halwidl, Daniel. Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2.

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editor, Liu Yongren 1958, Zhuang Zhe 1934-, Zhuang Zhe 1934-, and Taibei Shi li mei shu guan, eds. Zhuang Zhe hui gu zhan: Hong meng yu han chang = Chuang Che retrospective exhibition : effusive vitality. Taibei Shi li mei shu guan, 2015.

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G, Brown Kenneth, and United States. National Aeronautics and Space Administration, eds. Low pressure gas flow analysis through an effusive inlet using mass spectrometry: Final report, period ending 31 Dec, 1987. Dept. of Chemical Sciences, College of Sciences, Old Dominion University, 1988.

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Devine, Christine Anne. Origin and emplacement of volcanogenic massive sulfide-hosting, paleoproterozoic volcaniclastic and effusive rocks within the Flin Flon subsidence structure, Manitoba and Saskatchewan, Canada. Laurentian University, School of Graduate Studies, 2003.

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Piracha, Kashif. Pleural Effusion. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-36041-1.

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Mercè, Jordà, and Krishan Awtar, eds. Effusion cytology. Demos Medical Pub., 2011.

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1925-, Stool Sylvan E., and Otitis Media Guideline Panel and Consortium., eds. Otitis media with effusion in children. U.S. Department of Health and Human Services, Public Health Service, Agency for Health Care Policy and Research, 1994.

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United States. Otitis Media Guideline Panel, ed. Otitis media with effusion in children. U.S. Dept. of Health and Human Services, Public Health Service, Agency for Health Care Policy and Research, 1995.

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1925-, Stool Sylvan E., and Otitis Media Guideline Panel, eds. Otitis media with effusion in young children. U.S. Dept. of Health and Human Services, 1994.

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Stool, Sylvan E. Otitis media with effusion in young children. U.S. Department of Health and Human Services, Public Health Service, Agency for Health Care Policy and Research, 1994.

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Book chapters on the topic "Effusive"

1

Crespo, Eric M., Sidney C. Smith, and George A. Stouffer. "Effusive-constrictive pericarditis." In Cardiovascular Hemodynamics for the Clinician. John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781119066491.ch20.

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Lena, Raffaello, Christian Wöhler, James Phillips, and Maria Teresa Chiocchetta. "Effusive Lunar Domes." In Lunar Domes. Springer Milan, 2013. http://dx.doi.org/10.1007/978-88-470-2637-7_7.

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Halwidl, Daniel. "Effusive molecular beam sources." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_3.

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Lena, Raffaello, Christian Wöhler, James Phillips, and Maria Teresa Chiocchetta. "Effusive Bisected Lunar Domes." In Lunar Domes. Springer Milan, 2013. http://dx.doi.org/10.1007/978-88-470-2637-7_6.

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Halwidl, Daniel. "Introduction." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_1.

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Halwidl, Daniel. "Flow of gases." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_2.

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Halwidl, Daniel. "Molecular Beam." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_4.

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Halwidl, Daniel. "Results." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_5.

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Halwidl, Daniel. "Summary and outlook." In Development of an Effusive Molecular Beam Apparatus. Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-13536-2_6.

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Lena, Raffaello, Christian Wöhler, James Phillips, and Maria Teresa Chiocchetta. "Modelling of Lunar Effusive and Intrusive Domes." In Lunar Domes. Springer Milan, 2013. http://dx.doi.org/10.1007/978-88-470-2637-7_4.

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Conference papers on the topic "Effusive"

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Muratkhanov, Daulet, Kanat Bulegenov, and Gulimshat Shakirova1. "ABOUT THE NEW PORPHYRY COPPER MINERALIZATION OBJECT IN THE EASTERN BALKHASH REGION (KAZAKHSTAN)." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.01.

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In Kazakhstan, the main porphyry copper deposits are located in the Northern Balkhash region. The Konyrat, Aktogay, Aidarly, and Borly copper-porphyry deposits have been explored and exploited in this area. The main reserves of the country's copper raw materials are associated with these deposits. The Eastern Balkhash region is part of the North Balkhash ore zone. Previous studies on the Eastern Balkhash region focused on the Aktogay region and did not pay due attention to the southern part of the East Balkhash region, despite the fact that this region borders the Aktogay ore field and has prerequisites for the discovery of new ore sites. The geological structure of the area includes devonian and carboniferous terrigenous-effusive formations which are broken through by granitoid intrusions. Hydrothermal changes are widespread in the host rock and intrusive massifs. We have conducted cosmogeological studies and compiled a cosmogeological scheme of the territory with the allocation of ore-controlling annular and linear structures, the spread of areal bodies of intrusive rocks and metasomatic changes. According to the data of geological and cosmogeological studies, promising areas have been identified, within which geological and geophysical prospecting works have been carried out. According to the data of geophysical work, local anomalies have been identified for drilling mapping and prospecting wells. As a result of geological, geophysical, drilling, mineralogical and petrographic studies in the buried intrusion of granitoids, a new promising sulfide copper-molybdenum mineralization was revealed.
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Schmitt, G., B. Sadlowsky, J. Noga, and G. Siegmund. "Inhibition of Hydrogen Effusion from Steel-An Overlooked and Underestimated Phenomenon." In CORROSION 2000. NACE International, 2000. https://doi.org/10.5006/c2000-00466.

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Abstract Inhibition of the recombination of electrochemically formed hydrogen promotes the hydrogen entry into the steel. It was found that the recombination of atomic hydrogen at the hydrogen effusion side can be inhibited likewise hindering the hydrogen from effusion. Under steady state permeation conditions this increases the average hydrogen concentration in the steel and, hence, the danger of hydrogen induced material failures. The effusion experiments were performed with hollow tensile probes under constant load simulating pipeline conditions.
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Battisti, Lorenzo, Roberto Fedrizzi, and Giovanni Cerri. "Novel Technology for Gas Turbine Blade Effusion Cooling." In ASME Turbo Expo 2006: Power for Land, Sea, and Air. ASMEDC, 2006. http://dx.doi.org/10.1115/gt2006-90516.

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Gas turbine combustion chambers and turbine blades require better cooling techniques to cope with the increase in operating temperatures with each new engine model. Current gas turbine inlet temperatures are approaching 2000 K. Such extreme temperatures, combined with a highly dynamic environment, result in major stress on components, especially combustion chamber and blades of the first turbine stages. A technique that has been extensively investigated is transpiration cooling, for both combustion chambers and turbine blades. Transpiration-cooled components have proved an effective way to achieve high temperatures and erosion resistance for gas turbines operating in aggressive environments, though there is a shortage of durable and proven technical solutions. Effusion cooling (full-coverage discrete hole film cooling), on the other hand, is a relatively simpler and more reliable technique offering a continuous coverage of cooling air over the component’s hot surfaces. This paper presents an innovative technology for the efficient effusion cooling of the combustor wall and turbine blades. The dedicated electroforming process used to manufacture effusive film cooling systems, called Poroform®, is illustrated. A numerical model is also presented, developed specifically for designing the distributions of the diameter and density of the holes on the cooled surface with a view to reducing the metal’s working temperature and achieving isothermal conditions for large blade areas. Numerical simulations were used to design the effusive cooling system for a first-stage gas turbine blade. The diameter, density and spacing of the holes, and the adiabatic film efficiency are discussed extensively to highlight the cooling capacity of the effusive system.
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Kestay (Keszthelyi), Laszlo. "TECTONIC SETTINGS FAVORING HIGH-FLUX EFFUSIVE ERUPTIONS." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-394763.

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Scarrow, Jane H., Axel K. Schmitt, Martin Danišík, et al. "Forensic Geochronology of an Explosive-Effusive Transition: Ascension Island." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2294.

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Costa, Fidel, Sri Budhi Utami, and Hanik Humaida. "Quantifying magma ascent rates for explosive and effusive eruptions." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.16891.

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Herbst, Thomas, Alan Whittington, Mattia Pistone, James Schiffbauer, and Tara Selly. "THE VOLCANIC EXPLOSIVE-EFFUSIVE TRANSITION EXPLAINED BY COMPETING OUTGASSING MECHANISMS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359881.

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Murashko, T. V. "Diagnostic signs of the non-effusive feline infectious peritonitis: case analysis." In DEVELOPMENT OF THE AGRICULTURAL SECTOR, FOOD AND VETERINARY MEDICINE IN UKRAINE AND EU COUNTRIES. Baltija Publishing, 2024. https://doi.org/10.30525/978-9934-26-518-1-15.

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Belden, Casey, Isabella Harnett, Ella Saunders, and Keith Brunstad. "DYNAMIC FLOW MODELING OF INFLATION AND DEFLATION CHARACTERISTICS FOR EFFUSIVE LAVA ERUPTIONS." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-396163.

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Herbst, Thomas, Alan Whittington, Mattia Pistone, James D. Schiffbauer, and Tara Selly. "THE VOLCANIC EXPLOSIVE-EFFUSIVE TRANSITION: INSIGHTS FROM A CRYSTALLINITY-BASED PERMEABILITY MODEL." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370759.

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Reports on the topic "Effusive"

1

Scanlan, E. J., M. Leybourne, D. Layton-Matthews, A. Voinot, and N. van Wagoner. Alkaline magmatism in the Selwyn Basin, Yukon: relationship to SEDEX mineralization. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328994.

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Several sedimentary exhalative (SEDEX) deposits have alkaline magmatism that is temporally and spatially associated to mineralization. This report outlines interim data from a study of potential linkages between magmatism and SEDEX mineralization in the Selwyn Basin, Yukon. This region is an ideal study site due to the close spatial and temporal relationships between SEDEX deposits and magmatism, particularly in the MacMillan Pass, where volcanic rocks have been drilled with mineralization at the Boundary deposit. Alkaline volcanic samples were analysed from the Anvil District, MacMillan Pass, Keno-Mayo and the Misty Creek Embayment in the Selwyn Basin to characterise volcanism and examine the relationship to mineralization. Textural and field relationships indicate a volatile-rich explosive eruptive volcanic system in the MacMillan Pass region in comparison to the Anvil District, which is typically effusive in nature. High proportions of calcite and ankerite in comparison to other minerals are present in the MacMillan system. Cathodoluminescence imaging reveals zoning and carbonate that displays different luminescent colours within the same sample, likely indicating multiple generations of carbonate precipitation. Barium contents are enriched in volcanic rocks throughout the Selwyn Basin, which is predominately hosted by hyalophane with rare barite and barytocalcite. Thallium is positively correlated with Ba, Rb, Cs, Mo, As, Sb and the calcite-chlorite-pyrite index and is negatively correlated with Cu. Anvil District samples display a trend towards depleted mid-ocean ridge mantle on a plot of Ce/Tl versus Th/Rb. Hydrothermal alteration has likely led to the removal of Tl from volcanic rocks in the region. Ongoing research involves: i) the analysis of Sr, Nd, Pb and Tl isotopes of volcanic samples; ii) differentiating magmatic from hydrothermal carbonate using O, C and Sr isotopes; iii) examining sources of Ba in the Selwyn Basin; iv) and constraining age relationships through U-Th-Pb geochronology.
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Zeng, Yulin, Liwei Wang, Hai Zhou, and Yu Qi. Th1/Th2 cytokine profiles differentiating tuberculous from malignant pleural effusions: A systematic review and meta-analysis. INPLASY - International Platform of Registered Systematic Review and Meta-analysis Protocols, 2022. http://dx.doi.org/10.37766/inplasy2022.1.0005.

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Review question / Objective: To clarify which one has a different predominance of Th1 and Th2 immune responses in malignant and tuberculous pleural effusions. We did a meta-analysis of the results published previously to assess the levels of Th1/Th2 cytokines in two types of pleural effusion and evaluated its ability to distinguish TPE from MPE. Condition being studied: Malignant and tuberculous pleural effusions are the two most common types of exudative pleural effusions, both of which can be seen with the typical accumulation of lymphocytes. Immune responses mediated by either the Th1 or Th2 subset dominate, depending on different types of pleural effusion. Thus, we performed a meta-analysis of all available studies to quantitatively evaluate the levels of Th1/Th2 cytokine profiles in TPE and MPE, as well as to assess the potential diagnostic value of these cytokines in discriminating TPE from MPE.
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Pengilly, Paula L. Adherence to the Otitis Media with Effusion Clinical Practice Guideline By Providers in a United States Air Force Medical Treatment Facility. Defense Technical Information Center, 1999. http://dx.doi.org/10.21236/ad1012175.

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Lin, Zhen, Mengyuan Jiang, Lirong Gao, and Huachun Zhang. The clinical efficacy of traditional Chinese medicine in the treatment of malignant pleural effusion: A protocol of systematic review and meta-analysis. INPLASY - International Platform of Registered Systematic Review and Meta-analysis Protocols, 2020. http://dx.doi.org/10.37766/inplasy2020.8.0105.

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Wang, Jingyi, Jichang Du, and Muhammad Usman. Incidence and mortality of Neonatal pericardial effusion associated with central venous catheters: A meta-analysis of retrospective cohort studies, case series and case reports. INPLASY - International Platform of Registered Systematic Review Protocols, 2020. http://dx.doi.org/10.37766/inplasy2020.3.0014.

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Miao, Fang, Yaru Guo, Yan Yuan, Juzhou Chen, and Yong Xin. Bevacizumab combined with pemetrexed plus carboplatin or cisplatin in the treatment of malignant pleural effusion of lung cancer : A meta-analysis of randomized controlled trials. INPLASY - International Platform of Registered Systematic Review and Meta-analysis Protocols, 2022. http://dx.doi.org/10.37766/inplasy2022.4.0096.

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