Desarrollo y Aplicación de Herramientas Teóricas, Numéricas y Códigos Computacionales en Dinámica de Gases para Ingeniería Aeronáutica

Objetivos generales: • Desarrollo de un código utilizando programación orientada objeto y Fortran 2003 para simulación de flujos de gases de alta entalpía incluyendo efectos químicos. • Mejora de técnicas numéricas con la finalidad de simular flujos gas dinámicos con alta entalpía y químicamente activos. • Mejora de la comprensión del fenómeno de intermitencia caótica. • Mejorar en la comprensión, implementación y utilización del código openFOAM para la simulación de flujos de interés en la industria aeroespacial. Objetivos específicos: • Poseer la capacidad de simular las ecuaciones de la dinámica de gases tridimensionales, químicamente activas y dependientes del tiempo usando volúmenes finitos mediante códigos propios. • Continuar con el desarrollo de la nueva teoría que permite una descripción más adecuada y precisa del fenómeno de intermitencia como una de las rutas hacia el caos. • Adaptar el código openFoam para la simulación de la dinámica del flujo de gases con elevada entalpía y/o reactivos. • Aplicación de los códigos desarrollados a la simulación de flujos de interés aeronáutico tales como chorros supersónicos, flujos supersónicos alrededor de objetos en vuelo atmosférico y procesos de combustión difusiva. Resultados esperados • Obtención de un código numérico en volúmenes finitos mediante programación orientada a objeto desarrollado en la UNC con la capacidad de simular flujos gas-dinámicos, tridimensionales, viscosos, químicamente activos y dependientes del tiempo. Este código será la base para un programa de multifísica en flujos gaseosos que en un futuro deberá incluir ionización y simulación de flujos magnetohidrodinámicos compresibles. • Desarrollo y/o mejora de técnicas numéricas para la solución de flujos gas-dinámicos químicamente activos. Se continuará con la investigación que usa distintas funciones limitadoras para distintas ondas. • Mejora del conocimiento sobre fenómenos que presentan intermitencia caótica. Se continuará con la teoría que está actualmente en desarrollo por integrantes del grupo en colaboración con investigadores de universidades de España. Principalmente se pondrá énfasis para obtener una formulación más general de la teoría mediante el desarrollo de una técnica de perturbación que permita aproximar cualquier función no lineal que gobierna el proceso de reinyección. • Implementación del código openFOAM para simular flujos supersónicos y procesos de combustión. Se generarán librerías específicas para utilizar este software en aplicaciones de flujos compresibles. • Se espera alcanza una mejor descripción numérica del fenómeno de chorros supersónicos sub-expandidos que impactan sobre paredes sólidas.

London, England : gas companies' districts, 1884 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of London and its environs : shewing the boundary of the jurisdiction of the metropolitan board of work, also the boundaries of the city of London, and the gas companies' districts. It was published by Edward Standford, April 21, 1884. Scale [ca. 1:31,680]. This map is part of a 5 map set showing various thematic districts and boundaries of the London region. The image inside the map neatline is georeferenced to the surface of the earth and fit to the British National Grid coordinate system (British National Grid, Airy Spheroid OSGB (1936) Datum). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, selected private and public buildings, towns and villages, cemeteries, parks, farms, gas companies' districts, and more. Relief is shown by hachures. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Troubleshooting di un impianto di disidratazione di gas naturale: un caso di studio

Il principale componente non idrocarburico contenuto nel gas naturale è l’acqua che viene rimossa mediante assorbimento con glicole trietilenico, il processo di trattamento più comune nella produzione di gas naturale. La presenza di acqua libera nel gas deve essere rimossa totalmente, per evitare la formazione di condensa nelle condizioni di trasporto e di distribuzione più critiche cioè a pressione elevata e a bassa temperatura. Obiettivo di questa tesi è l’analisi delle cause e dei fenomeni che portano a rilevanti perdite di glicole (TEG) in impianti di disidratazione del gas naturale operanti con elevate concentrazioni di CO2 e H2S nel gas di processo. Le perdite, in relazione alle diverse condizioni operative e concentrazioni dei gas menzionati, possono arrivare a raggiungere valori pari a 3-4 volte l'entità attesa, con punte che raggiungono 10 volte tali valori. Il lavoro di tesi è stato focalizzato su un impianto attualmente in esercizio, situato in Arabia Saudita. L’attività è stata condotta presso la Comart di Ravenna, azienda specializzata nella progettazione di impianti nel settore Oil&Gas. Inizialmente sono state studiate le caratteristiche di un impianto di disidratazione di gas naturale mediante assorbimento con glicole trietilenico. Dopo l’analisi delle possibili fonti di perdita, la colonna di alimentazione del ribollitore (Still Column) e il relativo condensatore, sulla base dei dati operativi degli impianti, sembra essere il punto su cui si concentrano le perdite. Vengono presentati i dettagli costruttivi di tale colonna al fine di determinarne i possibili malfunzionamenti. Scopo della tesi sarà l'identificazione, partendo dall'attuale configurazione dell’impianto, delle cause che portano a tali valori di perdite e l'individuazione di una configurazione colonna/condensatore (con eventuali altri equipment necessari) in grado di minimizzare le perdite contenendo al minimo i costi aggiuntivi della soluzione.

Dissolved CO2 and Alkane Gas in Clay Formations

Characterization of dissolved CO2 and alkane gas in clayrocks may help assessing the confinement properties of geological barriers considered as potential host rocks for a deep geological disposal as well as for caprocks of gas storages. A monitoring of alkanes with CO2, combined with carbon isotopes was performed on core samples coming from Underground Research Laboratories (Bure, Mont Terri, Tournemire) and the Schlattingen borehole in France and Switzerland. Composition of hydrocarbon gas and delta C-13 of methane strongly suggest a dominant thermogenic origin of methane which is mixed with a bacterial origin for the Toarcian shales, Pliensbachien and Callovian-Oxfordian clayrocks. Results also evidence the contrasted behavior of CO2, which is controlled by chemical equilibrium between pore water and carbonate mineralogy, compared to the alkanes which are present in the porosity as a stock of dissolved gases which can be depleted during degassing experiments. (C) 2015 The Authors. Published by Elsevier B.V.

Total organic carbon, delta13C, biomarker, gas compilations and hopanoids analysis from IODP Sites 307-U1317 and 307-U1318

During the Integrated Ocean Drilling Program (IODP) Expedition 307 for the first time a cold-water coral carbonate mound was drilled down through its base into the underlying sediments. In the current study, sample material from within and below Challenger Mound, located in the Belgica carbonate mound province in the Porcupine Basin offshore Ireland, was investigated for its distribution of microbial communities and gas composition using biogeochemical and geochemical approaches to elucidate the question on the initiation of carbonate mounds. Past and living microbial populations are lower in the mound section compared to the underlying sediments or sediments of an upslope reference site. A reason for this might be a reduced substrate feedstock, reflected by low total organic carbon (TOC) contents, in the once coral dominated mound sequence. In contrast, in the reference site a lithostratigraphic sequence with comparatively high TOC contents shows higher abundances of both past and present microbial communities, indicating favourable living conditions from time of sedimentation until today. Composition and isotopic values of gases below the mound base seem to point to a mixed gas of biogenic and thermogenic origin with a higher proportion of biogenic gas. Oil-derived hydrocarbons were not detected at the mound site. This suggests that at least in the investigated part of the mound base the upward flow of fossil hydrocarbons, being one hypothesis for the initiation of the formation of carbonate mounds, seems to be only of minor significance.

Organic carbon, calcium carbonate and carbon/nitrogen ratio at DSDP Leg 93 sites

A large number of samples of nonlithified and lithified sediments from Leg 93 sites were analyzed for their contents of organic carbon and calcium carbonate. An average of two samples was selected from every core for carbonate determination; organic carbon was measured in most of these samples. Nearly all of these analyses were performed on board Glomar Challenger for samples from Sites 603 and 604. Site 605 samples, plus some of the deeper samples from Hole 603B, were analyzed at the University of Michigan. The procedures used in both cases were virtually the same, and their results compared well. Organic carbon analyses were done using a Hewlett- Packard 185-B CHN Analyzer. Portions of samples selected for calcium carbonate determinations were treated with dilute HC1 to remove carbonate, washed with deionized water, and dried at 110°C. A Cahn Electrobalance was used to weight 20-mg samples of sediment for CHN analysis. Samples were combusted at 1050°C in the presence of an oxidant, and the volumes of the evolved gases determined as measures of the C, H, and N contents of sediment organic matter. Areas of gas peaks were determined and compared to those of rock standards of known carbon and nitrogen contents. These values were used to standardize instrument response so that C/N atomic ratios could be reported. Organic carbon concentrations were calculated on the basis of sediment dry weight. Hydrogen elemental analysis with the procedure used is untrustworthy because of the variable amounts of clay minerals and their hydrates, hence hydrogen values are not reported for samples analyzed by this method.

Hydrocarbon gas concentrations in sediments from ODP Leg 164 sites

Residual concentrations and distributions of hydrocarbon gases from methane to n-heptane were measured in sediments at seven sites on Ocean Drilling Program (ODP) Leg 164. Three sites were drilled at the Cape Fear Diapir of the Carolina Rise, and one site was drilled on the Blake Ridge Diapir. Methane concentrations at these sites result from microbial generation which is influenced by the amount of pore-water sulfate and possible methane oxidation. Methane hydrate was found at the Blake Ridge Diapir site. The other hydrocarbon gases at these sites are likely the product of early microbial processes. Three sites were drilled on a transect of holes across the crest of the Blake Ridge. The base of the zone of gas-hydrate occurrence was penetrated at all three sites. Trends in hydrocarbon gas distributions suggest that methane is microbial in origin and that the hydrocarbon gas mixture is affected by diagenesis, outgassing, and, near the surface, by microbial oxidation. Methane hydrate was recovered at two of these three sites, although gas hydrate is likely present at all three sites. The method used here for determining amounts of residual hydrocarbon gases has its limitations and provides poor assessment of gas distributions, particularly in the stratigraphic interval below about ~100 mbsf. One advantage of the method, however, is that it yields sufficient quantities of gas for other studies such as isotopic determinations.

(Table 3) Noble gas composition of dissociated gas hydrate specimens from ODP Leg 164 sites

Fractionation of the noble gases should occur during formation of a Structure I gas hydrate from water and CH4 such that CH4 hydrate is greatly enriched in Xenon. Noble gas concentrations and fractionation factors (F[4He], F[22Ne], F[86Kr], and F[132Xe] as well as R/Ra) were determined for eight gas hydrate specimens collected on Leg 164 to evaluate this theoretical possibility and to assess whether sufficient quantities of Xe are hosted in oceanic CH4 hydrate to account for Xe "missing" from the atmosphere. The simplest explanation for our results is that samples contain mixtures of air and two end-member gases. One of the end-member gases is depleted in Ne, but significantly enriched in Kr and Xe, as anticipated if the source of this gas involves fractionation during Structure I gas hydrate formation. However, although oceanic CH4 hydrate may be greatly enriched in Xe, simple mass balance calculations indicate that oceanic CH4 hydrate probably represents only a minor reservoir of terrestrial Xe. Noble gas analyses may play an important role in understanding the dynamics of gas hydrate reservoirs, but significantly more work is needed than presented here.

Light hydrocarbons in gas pockets and sediments of ODP Site 131-808

A suite of gas samples obtained from gas pockets and sediments of the Nankai accretionary prism (Site 808) has been analyzed for their gas composition and carbon and hydrogen isotope ratios. Gases collected from gas pockets between 10 and 555 mbsf consist of CH4 and CO2. Stable carbon isotope ratios of these two components point to a bacterial formation of methane via CO2-reduction that is also supported by D/H ratios of methane. Methane desorbed from sediments by a vacuum/acid treatment is of bacterial and thermal origin. Mixing between these gas types is indicated by molecular composition and carbon isotope ratios. Diagenetic processes at low temperatures can explain ethane to pentane concentrations from 0 to 850 mbsf. Between 850 mbsf and the basaltic basement hydrocarbon occurrences are related to catagenetic processes at elevated temperatures. Thermal alteration of organic matter is reflected through different gas parameters. Propane carbon isotope values of a sample from the zone of the frontal thrust indicate that the gas likely migrated from sediments of a higher maturity into the immature sediments at 366 mbsf.

Helium isotope ratios and pore gases in deep-sea sediments of the Japan Sea

We have measured the 3He/4He and 4He/20Ne ratios and chemical compositions of gases exsolved from deep-sea sediments at two sites (798 and 799) in the Japan Sea. The 3He/4He and 4He/20Ne ratios vary from 0.642 Ratm (where Ratm is the atmospheric 3He/4He ratio of 1.393*10**-6) to 0.840 Ratm, and from 0.41 to 4.5, respectively. Helium in the samples can be explained by the mixing between atmospheric helium dissolved in bottom water of the Japan Sea and crustal helium in the sediment. The sedimentary helium is enriched in mantle-derived 3He compared with those from the Japan Trench and the Nankai Trough. This suggests that the basement of the Japan Sea has relatively large remnants of mantle-derived helium compared with that of the Pacific. Major chemical compositions of the samples are methane and nitrogen. There is a positive correlation between methane content and helium content corrected for air component. Based on the 3He/4He-Sum C/3He diagram, the major part of methane can be attributed to crustal and/or organic origin.