Caratterizzazione di membrane metalliche e ionomeriche per applicazioni energetiche

The work of this thesis has been focused on the characterization of metallic membranes for the hydrogen purification from steam reforming process and also of perfluorosulphonic acid ionomeric (PFSI) membranes suitable as electrolytes in fuel cell applications. The experimental study of metallic membranes was divided in three sections: synthesis of palladium and silver palladium coatings on porous ceramic support via electroless deposition (ELD), solubility and diffusivity analysis of hydrogen in palladium based alloys (temperature range between 200 and 400 °C up to 12 bar of pressure) and permeation experiments of pure hydrogen and mixtures containing, besides hydrogen, also nitrogen and methane at high temperatures (up to 600 °C) and pressures (up to 10 bar). Sequential deposition of palladium and silver on to porous alumina tubes by ELD technique was carried out using two different procedures: a stirred batch and a continuous flux method. Pure palladium as well as Pd-Ag membranes were produced: the Pd-Ag membranes’ composition is calculated to be close to 77% Pd and 23% Ag by weight which was the target value that correspond to the best performance of the palladium-based alloys. One of the membranes produced showed an infinite selectivity through hydrogen and relatively high permeability value and is suitable for the potential use as a hydrogen separator. The hydrogen sorption in silver palladium alloys was carried out in a gravimetric system on films produced by ELD technique. In the temperature range inspected, up to 400°C, there is still a lack in literature. The experimental data were analyzed with rigorous equations allowing to calculate the enthalpy and entropy values of the Sieverts’ constant; the results were in very good agreement with the extrapolation made with literature data obtained a lower temperature (up to 150 °C). The information obtained in this study would be directly usable in the modeling of hydrogen permeation in Pd-based systems. Pure and mixed gas permeation tests were performed on Pd-based hydrogen selective membranes at operative conditions close to steam-reforming ones. Two membranes (one produced in this work and another produced by NGK Insulators Japan) showed a virtually infinite selectivity and good permeability. Mixture data revealed the existence of non negligible resistances to hydrogen transport in the gas phase. Even if the decrease of the driving force due to polarization concentration phenomena occurs, in principle, in all membrane-based separation systems endowed with high perm-selectivity, an extensive experimental analysis lack, at the moment, in the palladium-based membrane process in literature. Moreover a new procedure has been introduced for the proper comparison of the mass transport resistance in the gas phase and in the membrane. Another object of study was the water vapor sorption and permeation in PFSI membranes with short and long side chains was also studied; moreover the permeation of gases (i.e. He, N2 and O2) in dry and humid conditions was considered. The water vapor sorption showed strong interactions between the hydrophilic groups and the water as revealed from the hysteresis in the sorption-desorption isotherms and thermo gravimetric analysis. The data obtained were used in the modeling of water vapor permeation, that was described as diffusion-reaction of water molecules, and in the humid gases permeation experiments. In the dry gas experiments the permeability and diffusivity was found to increase with temperature and with the equivalent weight (EW) of the membrane. A linear correlation was drawn between the dry gas permeability and the opposite of the equivalent weight of PFSI membranes, based on which the permeability of pure PTFE is retrieved in the limit of high EW. In the other hand O2 ,N2 and He permeability values was found to increase significantly, and in a similar fashion, with water activity. A model that considers the PFSI membrane as a composite matrix with a hydrophilic and a hydrophobic phase was considered allowing to estimate the variation of gas permeability with relative humidity on the basis of the permeability in the dry PFSI membrane and in pure liquid water.

Untersuchung molekularer Erkennungsreaktionen mit einem integriert-optischen Mach-Zehnder-Interferometer

Abstract (deutsch)Zielsetzung des Dissertationsvorhabens war die Beobachtung und Analyse von Gast-Wirt-Wechselwirkungen an oxidischen Oberflächen. Einer der Wechselwirkungspartner sollte dabei auf der Oberfläche immobilisiert, der andere in wäßriger Lösung darüber vorliegen.Eine empfindliche und oberflächensensitive Methode zur Beobachtung der Anlagerung unmarkierter Moleküle ist die Wellenleiterspektroskopie, insbesondere mit dem hier verwendeten und weiterentwickelten integriert-optischen Mach-Zehnder-Interferometer in Siliziumtechnik (Siliziumoxynitrid auf oxidiertem Siliziumwafer). Mit Hilfe des Interferometers wurden unterschiedliche Wirt-Gast-Systeme untersucht. Grundlage der Immobilisierung war jeweils die Funktionalisierung der Sensoroberfläche durch Selbstadsorption von Organosilanen. Durch unterschiedliche Organosilane, die zum Teil im Rahmen dieser Arbeit synthetisiert wurden, ließen sich die Wirtmoleküle beta-Cyclodextrin, Streptavidin, sowie unterschiedliche monoklonale Antikörperfragmente immobilisieren.- Der Einfluß der Oberfläche auf die Bindungsstärke des Wirtmoleküls beta-Cyclodextrin und unterschiedlicher Gastmoleküle wurde konzentrationsabhängig untersucht.- Silan-Biotinderivate mit unterschiedlicher Streptavidin-Affinität wurden an die Oberfläche immobilisiert und die Adsorption von Streptavidin an die Biotinderivate beobachtet. Dabei konnte unter anderem nachgewiesen werden, daß das Streptavidinadsorbat gequollen ist.- Als mögliche Anwendung wurde geprüft, ob das vorgestellte Interferometer durch die Funktionalisierung mit Antikörperfragmenten als Biosensor in Frage kommt. Es konnte nachgewiesen werden, daß sich Antikörper auf der Sensoroberfläche immobilisieren lassen und Antigene spezifisch an diese Antikörper adsorbieren.

Mg for hydrogen storage: synthesis, nanostructure and thermodynamics properties

Nowadays alternative energies are an extremely important topic and the possibility of using hydrogen as an energy carrier must be explored. Many problems infer the technological application of this abundant and powerful resource, one of them the possibility of storage. In the framework of suitable materials for hydrogen storage, magnesium has been the center of this study because it is cheap and the amount of stored hydrogen that it achieves (7.6 wt%) is extremely appealing. Nanostructure helps to overcome the slow hydrogen diffusion and the functionalization of surfaces with transition metals or oxides favors the hydrogen molecule dissociation/recombination. The aim of this research is the investigation of the metal-hydride transformation in magnesium nanoparticles synthesized by inert-gas condensation, exploiting the fact that they are a simple model system. The so produced nanostructured powder has been analyzed in response to nanoparticles surface functionalization by transition metal clusters, specifically palladium, nickel and titanium, chosen on the basis of their completely different Mg-related phase diagrams. The role of the intermetallic phases formed upon heating and hydrogenation treatments will be presented to provide a comprehensive picture of hydrogen sorption in this class of nanostructured storage materials.

Partial melting within the lower crust – Constraints from bulk rock geochemical data and trace element mineral analyses of granulites and migmatites from Central Finland

This PhD thesis concerns geochemical constraints on recycling and partial melting of Archean continental crust. A natural example of such processes was found in the Iisalmi area of Central Finland. The rocks from this area are Middle to Late Archean in age and experienced metamorphism and partial melting between 2.7-2.63 Ga. The work is based on extensive field work. It is furthermore founded on bulk rock geochemical data as well as in-situ analyses of minerals. All geochemical data were obtained at the Institute of Geosciences, University of Mainz using X-ray fluorescence, solution ICP-MS and laser ablation-ICP-MS for bulk rock geochemical analyses. Mineral analyses were accomplished by electron microprobe and laser ablation ICP-MS. Fluid inclusions were studied by microscope on a heating-freezing-stage at the Geoscience Center, University Göttingen. Part I focuses on the development of a new analytical method for bulk rock trace element determination by laser ablation-ICP-MS using homogeneous glasses fused from rock powder on an Iridium strip heater. This method is applicable for mafic rock samples whose melts have low viscosities and homogenize quickly at temperatures of ~1200°C. Highly viscous melts of felsic samples prevent melting and homogenization at comparable temperatures. Fusion of felsic samples can be enabled by addition of MgO to the rock powder and adjustment of melting temperature and melting duration to the rock composition. Advantages of the fusion method are low detection limits compared to XRF analyses and avoidance of wet-chemical processing and use of strong acids as in solution ICP-MS as well as smaller sample volumes compared to the other methods. Part II of the thesis uses bulk rock geochemical data and results from fluid inclusion studies for discrimination of melting processes observed in different rock types. Fluid inclusion studies demonstrate a major change in fluid composition from CO2-dominated fluids in granulites to aqueous fluids in TTG gneisses and amphibolites. Partial melts were generated in the dry, CO2-rich environment by dehydration melting reactions of amphibole which in addition to tonalitic melts produced the anhydrous mineral assemblages of granulites (grt + cpx + pl ± amph or opx + cpx + pl + amph). Trace element modeling showed that mafic granulites are residues of 10-30 % melt extraction from amphibolitic precursor rocks. The maximum degree of melting in intermediate granulites was ~10 % as inferred from modal abundances of amphibole, clinopyroxene and orthopyroxene. Carbonic inclusions are absent in upper-amphibolite facies migmatites whereas aqueous inclusion with up to 20 wt% NaCl are abundant. This suggests that melting within TTG gneisses and amphibolites took place in the presence of an aqueous fluid phase that enabled melting at the wet solidus at temperatures of 700-750°C. The strong disruption of pre-metamorphic structures in some outcrops suggests that the maximum amount of melt in TTG gneisses was ~25 vol%. The presence of leucosomes in all rock types is taken as the principle evidence for melt formation. However, mineralogical appearance as well as major and trace element composition of many leucosomes imply that leucosomes seldom represent frozen in-situ melts. They are better considered as remnants of the melt channel network, e.g. ways on which melts escaped from the system. Part III of the thesis describes how analyses of minerals from a specific rock type (granulite) can be used to determine partition coefficients between different minerals and between minerals and melt suitable for lower crustal conditions. The trace element analyses by laser ablation-ICP-MS show coherent distribution among the principal mineral phases independent of rock composition. REE contents in amphibole are about 3 times higher than REE contents in clinopyroxene from the same sample. This consistency has to be taken into consideration in models of lower crustal melting where amphibole is replaced by clinopyroxene in the course of melting. A lack of equilibrium is observed between matrix clinopyroxene / amphibole and garnet porphyroblasts which suggests a late stage growth of garnet and slow diffusion and equilibration of the REE during metamorphism. The data provide a first set of distribution coefficients of the transition metals (Sc, V, Cr, Ni) in the lower crust. In addition, analyses of ilmenite and apatite demonstrate the strong influence of accessory phases on trace element distribution. Apatite contains high amounts of REE and Sr while ilmenite incorporates about 20-30 times higher amounts of Nb and Ta than amphibole. Furthermore, trace element mineral analyses provide evidence for magmatic processes such as melt depletion, melt segregation, accumulation and fractionation as well as metasomatism having operated in this high-grade anatectic area.

Untersuchungen zur Lebensdauer von NEA-Photokathoden bei der Extraktion sehr hoher mittlerer Ströme

Die Produktion eines spinpolarisierten Strahls mit hohem mittleren Strom ist sowohl für den Betrieb von existierenden polarisierten Quellen als auch in noch stärkerem Maße für geplante zukünftige Projekte wichtig. Die Betriebszeit solcher Quellen wird durch die Abnahme der Quantenausbeute der Photokathode mit der Zeit begrenzt. Die Problematik der Abnahme der Quantenausbeute konnte durch die Reaktion der Kathodenoberfläche mit sauerstoffhaltigen Molekülen sowie durch Ionenbombardement geklärt werden. Im Laufe dieser Arbeit wurden, teilweise zum ersten Mal, Mechanismen untersucht, die zur Entstehung der chemisch aktiven Moleküle und der Ionen beitragen und weitere Effekte, die die Betriebszeit der polarisierten Quellen reduzieren. Die Experimente wurden an einer genauen Kopie der an MAMI vorhandenen polarisierten Quelle durchgeführt. Es wurde demonstriert, dass Erwärmung der Photokathode, Ioneneinfang und Strahlverlust aufgrund der Raumladungskräfte die Kathodenlebensdauer begrenzen können. Der erste Effekt ist Erwärmung der Photokathode. Die Laserleistung wird fast vollständig in Wärmeleistung umgesetzt, was zur Absenkung der Verfügbarkeit der polarisierten Quellen führen kann, und zwar unabhängig davon, ob der Photostrom produziert wird oder nicht. Der zweite Effekt ist Ionenbombardement mit den sowohl in der Beschleunigungsstrecke als auch in der Strahlführung entstehenden Ionen. Es wurde demonstriert, dass der in der Strahlführung entstehende Ionenstrom sogar größer ist als der in der Kanone. Unter bestimmten Bedingungen können die gebildeten Ionen durch das Potenzial des Elektronenstrahls eingefangen werden und die Kanone erreichen und damit zusätzlich zur Zerstörung der negativen Elektronenaffinität beitragen. Der dritte Effekt ist Strahlverlust. Es wurde demonstriert, dass die relativen Strahlverluste kleiner als 1*10-6 sein sollten, um eine Lebensdauer von mehr als 1000 Stunden beim Strom von 100 A zu erreichen, was für die vorhandene Apparatur möglich ist. Zur Erzeugung extrem hoher Ströme wurde zum ersten Mal im Bereich der spinpolarisierten Quellen das Prinzip der „Energierückgewinnung“ eingesetzt. Experimente bei einer mittleren Stromstärke von 11.4 mA und einer Spitzenstromstärke von 57 mA bei 1% Tastverhältnis wurden bereits durchgeführt.

Untersuchungen zur Struktur und Funktion des Vibrio cholerae Cytolysins

Vibrio cholerae Cytolysin (VCC) gehört zur Gruppe der Exotoxine und bildet auf Membranen heptamere transmembrane Poren. VCC wird als protoxin mit einem Molekulargewicht von 79 kDa sezerniert und benötigt die proteolytische Spaltung der N-terminalen Pro-Region um Poren in der Membran zu bilden. Diese Spaltung erfolgt sowohl in Lösung, als auch nach der Bindung an Membranen, aber nur aktiviertes VCC oligomererisiert in eine lytische Pore. Die Kristallstruktur von VCC zeigt, dass das Monomer vier verschiedenen strukturellen Domänen enthält; die cytolytische Domäne, mit der Pre-Stem-Sequenz, der Pro-Region und den beiden C-terminalen Domänen β-Trefoil und β-Prism. Die porenbildende β-Barrel wird aus je einer Pre-Stem Domäne jedes der einzelnen sieben Untereinheiten gebildet. Da sich die porenbildende Region im Monomer zwischen den Domänen β-Prism und β-Trefoil befindet, sind konformationelle Änderungen des Toxins notwendig, um die Insertion dieser Region in die Membran zu ermöglichen. In dieser Arbeit wurde unter anderem der Mechanismus der Porenbildung durch die Konstruktion von Disulfid-Derivaten untersucht. Die Bildung von Disulfidbrücken wurde verwendet, um die porenbildende Region entweder mit der β-Trefoil oder β-Prism Domäne zu verknüpfen. Unter nicht-reduzierenden Bedingungen bindet das Toxin an Membranen und oligomerisiert zu SDS-labilen Oligomeren. Nach der Reduktion der künstlichen Disulfidbrücke erlangen die gebildeten Oligomere SDS-Stabilität und permeabilisieren die Membran. Durch die Zugabe steigender Konzentrationen des VCC-Derivats zu aktivem Toxin, wird die SDS-Stabilität der gebildeten Oligomere stark reduziert. Die Insertion des aktiven Toxins in die Membran wird allerdings nicht verhindert und daher Poren mit reduziertem funktionellen Durchmesser gebildet. Diese Ergebnisse verdeutlichen, dass die Bildung einer Prä-Pore vor der Insertion des Toxins in die Membran erfolgt und zeigt zum ersten Mal ein solches Zwischenstadium für ein β-porenbildendes Toxin, das von Gram-negativen Organismen produziert wird. Diese Ergebnisse deuten auf einen archetypischen Mechanismus der Porenbildung hin. Zusätzlich wurde die Funktion der beiden C-terminalen Domänen untersucht, und daher verschiedene Deletions- und Substitutionsmutanten konstruiert. Die β-Trefoil Domäne ist nicht essentiell für die Bindung des Toxins an Membranen, ist aber für die korrekte Faltung des Toxins notwendig. Die C-terminale β-Prism Domäne vermittelt die Bindung des Toxins an Membranen über Zuckerrezeptoren.

Bioverkapselung lebender Bakterien (Escherichia coli) mit Poly-(Silicat) nach Transformation mit dem Silicatein-alpha-Gen

Die Bioverkapselung ist eine faszinierende Methode, um biologische Materialien einschließlich Zellen in Siliziumdioxid, Metalloxiden oder hybriden Sol-Gel-Polymeren zu immobilisieren. Bisher wurde nur die Sol-Gel-Vorläufertechnologie genutzt, um Bakterien- oder Hefezellen in Siliziumdioxid zu immobilisieren. Hierfür wurden verschiedene Reagenzien als wässrige Vorläufer getestet, um poly(Silicate) auf Biomolekülen (Bhatia et al., 2000) oder Zellen (Liu und Chen 1999; Coradin und Livage, 2007) zu bilden. Einer der erfolgreichsten bisherigen Methoden verwendet eine Mischung aus Silicaten und kolloidalem Silica. Diese initialen Vorläufer werden durch die Zugabe von Salzsäure neutralisiert, was die Gelbildung fortschreiten lässt und die Verkapselung von Bakterien in einem Silica-Netzwerk zur Folge hat (Nassif et al., 2003). Mit der Entdeckung von Silicatein, einem Enzym, das aus Demospongien isoliert wurde und die Bildung von poly(Silicat) katalysiert, wurde es möglich, poly(Silicat) unter physiologischen Bedingungen zu synthetisieren. Silicatein wurde rekombinant in E. coli hergestellt und ist in der Lage, bei Raumtemperatur, neutralem pH-Wert und in wässrigen Puffersystemen aus Siliziumalkoxiden poly(Silicat) zu bilden (Krasko et al., 2000; Müller et al., 2007b; Zhou et al., 1999). In vivo katalysiert Silicatein die Synthese der Silicathülle der Schwamm-Spiculae (Skelettelemente; Müller et al., 2005b; Müller et al., 2007a; Müller et al., 2007b; Schröder et al., 2007a). Dieses Biosilica wurde in Form von Silica-Nanospheren mit Durchmessern zwischen 100 nm und 250 nm organisiert vorgefunden (Pisera 2003; Tahir et al., 2005). Mit dieser Arbeit konnte gezeigt werden, dass Escherichia coli erfolgreich mit dem Silicatein-Gen transformiert werden kann. Das Level der Proteinexpression kann in Anwesenheit von Isopropyl-β-D-thiogalaktopyranosid (IPTG) effizient erhöht werden, indem man die Bakterienzellen gleichzeitig mit Kieselsäure inkubiert. Dieser Effekt konnte sowohl auf Ebene der Synthese des rekombinanten Proteins durch Western Blot als auch durch Immunfluoreszenzmikroskopie nachgewiesen werden. Das heterolog produzierte Silicatein besitzt enzymatische Aktivität und kann die Polymerisation von Kieselsäure katalysieren. Dies konnte sowohl durch Färbung mit Rhodamin123, als auch durch Reaktion der nicht polymerisierten, freien Kieselsäure mit dem ß-Silicomolybdato-Farbsystem (Silicomolybdänblau) nachgewiesen werden. Elektronenmikroskopische Untersuchungen zeigten, dass nur die silicateinexprimierenden Bakterien während des Wachstums in Anwesenheit von Kieselsäure eine viskose Hülle um Zelle herum bilden. Ebenfalls konnte gezeigt werden, dass Silicatein-α aus Suberites domuncula nach Transformation in E. coli an die Zelloberfläche dieser Zellen transportiert wurde und dort seine enzymatische Funktion beibehielt. Die Silicathülle wurde mittels Raster-Elektronenmikroskopie (REM) analysiert. Die Bakterien, die Silicatein exprimierten und poly(Silicat) an ihrer Oberfläche synthetisierten, zeigten die gleichen Wachstumsraten wie die Bakterien, die das Gen nicht enthielten. Schlussfolgernd lässt sich sagen, dass die silicateinvermittelte Verkapselung von Bakterien mit poly(Silicat) die Bandbreite der Anwendung von Bakterien für die Produktion von rekombinanten Proteinen verbessern, erweitern und optimieren könnte.

Development and application of an analytical method for the determination of total atmospheric biogenic non-methane organic carbon

Ein wesentlicher Anteil an organischem Kohlenstoff, der in der Atmosphäre vorhanden ist, wird als leichtflüchtige organische Verbindungen gefunden. Diese werden überwiegend durch die Biosphäre freigesetzt. Solche biogenen Emissionen haben einen großen Einfluss auf die chemischen und physikalischen Eigenschaften der Atmosphäre, indem sie zur Bildung von bodennahem Ozon und sekundären organischen Aerosolen beitragen. Um die Bildung von bodennahem Ozon und von sekundären organischen Aerosolen besser zu verstehen, ist die technische Fähigkeit zur genauen Messung der Summe dieser flüchtigen organischen Substanzen notwendig. Häufig verwendete Methoden sind nur auf den Nachweis von spezifischen Nicht-Methan-Kohlenwasserstoffverbindungen fokussiert. Die Summe dieser Einzelverbindungen könnte gegebenenfalls aber nur eine Untergrenze an atmosphärischen organischen Kohlenstoffkonzentrationen darstellen, da die verfügbaren Methoden nicht in der Lage sind, alle organischen Verbindungen in der Atmosphäre zu analysieren. Einige Studien sind bekannt, die sich mit der Gesamtkohlenstoffbestimmung von Nicht-Methan-Kohlenwasserstoffverbindung in Luft beschäftigt haben, aber Messungen des gesamten organischen Nicht-Methan-Verbindungsaustauschs zwischen Vegetation und Atmosphäre fehlen. Daher untersuchten wir die Gesamtkohlenstoffbestimmung organische Nicht-Methan-Verbindungen aus biogenen Quellen. Die Bestimmung des organischen Gesamtkohlenstoffs wurde durch Sammeln und Anreichern dieser Verbindungen auf einem festen Adsorptionsmaterial realisiert. Dieser erste Schritt war notwendig, um die stabilen Gase CO, CO2 und CH4 von der organischen Kohlenstofffraktion zu trennen. Die organischen Verbindungen wurden thermisch desorbiert und zu CO2 oxidiert. Das aus der Oxidation entstandene CO2 wurde auf einer weiteren Anreicherungseinheit gesammelt und durch thermische Desorption und anschließende Detektion mit einem Infrarot-Gasanalysator analysiert. Als große Schwierigkeiten identifizierten wir (i) die Abtrennung von CO2 aus der Umgebungsluft von der organischen Kohlenstoffverbindungsfaktion während der Anreicherung sowie (ii) die Widerfindungsraten der verschiedenen Nicht-Methan-Kohlenwasserstoff-verbindungen vom Adsorptionsmaterial, (iii) die Wahl des Katalysators sowie (iiii) auftretende Interferenzen am Detektor des Gesamtkohlenstoffanalysators. Die Wahl eines Pt-Rd Drahts als Katalysator führte zu einem bedeutenden Fortschritt in Bezug auf die korrekte Ermittlung des CO2-Hintergrund-Signals. Dies war notwendig, da CO2 auch in geringen Mengen auf der Adsorptionseinheit während der Anreicherung der leichtflüchtigen organischen Substanzen gesammelt wurde. Katalytische Materialien mit hohen Oberflächen stellten sich als unbrauchbar für diese Anwendung heraus, weil trotz hoher Temperaturen eine CO2-Aufnahme und eine spätere Abgabe durch das Katalysatormaterial beobachtet werden konnte. Die Methode wurde mit verschiedenen leichtflüchtigen organischen Einzelsubstanzen sowie in zwei Pflanzenkammer-Experimenten mit einer Auswahl an VOC-Spezies getestet, die von unterschiedlichen Pflanzen emittiert wurden. Die Pflanzenkammer-messungen wurden durch GC-MS und PTR-MS Messungen begleitet. Außerdem wurden Kalibrationstests mit verschiedenen Einzelsubstanzen aus Permeations-/Diffusionsquellen durchgeführt. Der Gesamtkohlenstoffanalysator konnte den tageszeitlichen Verlauf der Pflanzenemissionen bestätigen. Allerdings konnten Abweichungen für die Mischungsverhältnisse des organischen Gesamtkohlenstoffs von bis zu 50% im Vergleich zu den begleitenden Standardmethoden beobachtet werden.

Product Distributions Following Hyperthermal Collisions Between C2H4 And O(3P)

Transient Diode Laser Absorption Spectroscopy (TDLAS) was used to perform vibrational state population studies of the CO2 product from the hyperthermal reaction between C2H4 and O(3P) at room temperature using O3 as the O-atom precursor. Photodissociation of O3 using a frequency quadrupled Q-switch Nd:YAG laser pulse at 266 nm produced O(3P) atoms at high velocities which subsequently reacted with C2H4, producing several primary and secondary products including CO2. The CO2 product was detected using high-resolution TDLAS under five unique sets of reaction conditions. The vibrational distribution of the CO2 product did not follow a Boltzmann distribution at all five sets of conditions. The experiments showed a distribution in which there was a surprisingly high population in the (1000) (symmetric stretching) state compared with the other states probed, all of which contained bend excitation. In general, the CO2 population in the (1000) state was about 15-20% more populated than the Boltzmann distribution predicts. A possible explanation for this result may lie in the mechanism of CO2 evolution from the C2H4 + O(3P) reaction.

Effects of carbonation on the mineral composition of cement kiln dust

Due to their relatively high calcium oxide content, industrial mineral oxide wastes are potential candidates for mineral sequestration of carbon dioxide (CO2). Cement kiln dust (CKD), a byproduct of cement manufacturing contains 20-60% CaO making it a possible candidate for CO2 sequestration. In this study, three types of CKD are characterized, before and after carbonation, using environmental scanning electron microscopy and energy dispersive x-ray microanalysis to determine the mineralogical and morphological changes occurring due to carbonation. The reactants, products, and precipitation mechanisms were investigated to enhance understanding of the governing processes and allow better utilization of CKD for CO2 sequestration. The results of multiple independent analyses confirmed the formation of CaCO3 during carbonation. Examinations of the reaction pathways found that CaO and calcium hydroxide (Ca(OH)2) were the major reactants. Three types of CaCO3 precipitation mechanisms were observed: (1) diffusion of CO2 into Ca(OH)2 particles causing precipitation in the pores of the particle and the growth of a CaCO3 ring from the outside inward, (2) precipitation onto existing particles, and (3) precipitation from aqueous solution. The growth of a CaCO3 ring on the outside of a particle may slow further diffusion of CO2 into a particle slowing iv the overall sequestration rate. Additionally, changes caused by carbonation in the solubility of trace metals were studied by mixing pre- and post-carbonated CKD with water and analyzing the solution using inductively coupled plasma mass spectrometry. Decreases in the leaching of chromium, lead, and copper were observed, and is an incentive for use of CKD for CO2 sequestration. Equilibrium modeling using PHREEQC confirmed that CaO and Ca(OH)2 would carbonate readily and form CaCO3.

TIME LAPSE SEISMIC OBSERVATIONS AND EFFECTS OF RESERVOIR COMPRESSIBILITY AT TEAL SOUTH OIL FIELD

One of the original ocean-bottom time-lapse seismic studies was performed at the Teal South oil field in the Gulf of Mexico during the late 1990’s. This work reexamines some aspects of previous work using modern analysis techniques to provide improved quantitative interpretations. Using three-dimensional volume visualization of legacy data and the two phases of post-production time-lapse data, I provide additional insight into the fluid migration pathways and the pressure communication between different reservoirs, separated by faults. This work supports a conclusion from previous studies that production from one reservoir caused regional pressure decline that in turn resulted in liberation of gas from multiple surrounding unproduced reservoirs. I also provide an explanation for unusual time-lapse changes in amplitude-versus-offset (AVO) data related to the compaction of the producing reservoir which, in turn, changed an isotropic medium to an anisotropic medium. In the first part of this work, I examine regional changes in seismic response due to the production of oil and gas from one reservoir. The previous studies primarily used two post-production ocean-bottom surveys (Phase I and Phase II), and not the legacy streamer data, due to the unavailability of legacy prestack data and very different acquisition parameters. In order to incorporate the legacy data in the present study, all three poststack data sets were cross-equalized and examined using instantaneous amplitude and energy volumes. This approach appears quite effective and helps to suppress changes unrelated to production while emphasizing those large-amplitude changes that are related to production in this noisy (by current standards) suite of data. I examine the multiple data sets first by using the instantaneous amplitude and energy attributes, and then also examine specific apparent time-lapse changes through direct comparisons of seismic traces. In so doing, I identify time-delays that, when corrected for, indicate water encroachment at the base of the producing reservoir. I also identify specific sites of leakage from various unproduced reservoirs, the result of regional pressure blowdown as explained in previous studies; those earlier studies, however, were unable to identify direct evidence of fluid movement. Of particular interest is the identification of one site where oil apparently leaked from one reservoir into a “new” reservoir that did not originally contain oil, but was ideally suited as a trap for fluids leaking from the neighboring spill-point. With continued pressure drop, oil in the new reservoir increased as more oil entered into the reservoir and expanded, liberating gas from solution. Because of the limited volume available for oil and gas in that temporary trap, oil and gas also escaped from it into the surrounding formation. I also note that some of the reservoirs demonstrate time-lapse changes only in the “gas cap” and not in the oil zone, even though gas must be coming out of solution everywhere in the reservoir. This is explained by interplay between pore-fluid modulus reduction by gas saturation decrease and dry-frame modulus increase by frame stiffening. In the second part of this work, I examine various rock-physics models in an attempt to quantitatively account for frame-stiffening that results from reduced pore-fluid pressure in the producing reservoir, searching for a model that would predict the unusual AVO features observed in the time-lapse prestack and stacked data at Teal South. While several rock-physics models are successful at predicting the time-lapse response for initial production, most fail to match the observations for continued production between Phase I and Phase II. Because the reservoir was initially overpressured and unconsolidated, reservoir compaction was likely significant, and is probably accomplished largely by uniaxial strain in the vertical direction; this implies that an anisotropic model may be required. Using Walton’s model for anisotropic unconsolidated sand, I successfully model the time-lapse changes for all phases of production. This observation may be of interest for application to other unconsolidated overpressured reservoirs under production.

A Novel Approach to Carbon Dioxide Capture and Storage

The novel approach to carbon capture and storage (CCS) described in this dissertation is a significant departure from the conventional approach to CCS. The novel approach uses a sodium carbonate solution to first capture CO2 from post combustion flue gas streams. The captured CO2 is then reacted with an alkaline industrial waste material, at ambient conditions, to regenerate the carbonate solution and permanently store the CO2 in the form of an added value carbonate mineral. Conventional CCS makes use of a hazardous amine solution for CO2 capture, a costly thermal regeneration stage, and the underground storage of supercritical CO2. The objective of the present dissertation was to examine each individual stage (capture and storage) of the proposed approach to CCS. Study of the capture stage found that a 2% w/w sodium carbonate solution was optimal for CO2 absorption in the present system. The 2% solution yielded the best tradeoff between the CO2 absorption rate and the CO2 absorption capacity of the solutions tested. Examination of CO2 absorption in the presence of flue gas impurities (NOx and SOx) found that carbonate solutions possess a significant advantage over amine solutions, that they could be used for multi-pollutant capture. All the NOx and SOx fed to the carbonate solution was able to be captured. Optimization studies found that it was possible to increase the absorption rate of CO2 into the carbonate solution by adding a surfactant to the solution to chemically alter the gas bubble size. The absorption rate of CO2 was increased by as much as 14%. Three coal combustion fly ash materials were chosen as the alkaline industrial waste materials to study the storage CO2 and regeneration the absorbent. X-ray diffraction analysis on reacted fly ash samples confirmed that the captured CO2 reacts with the fly ash materials to form a carbonate mineral, specifically calcite. Studies found that after a five day reaction time, 75% utilization of the waste material for CO2 storage could be achieved, while regenerating the absorbent. The regenerated absorbent exhibited a nearly identical CO2 absorption capacity and CO2 absorption rate as a fresh Na2CO3 solution.

Historical and idealized climate model experiments: an intercomparison of Earth system models of intermediate complexity

Both historical and idealized climate model experiments are performed with a variety of Earth system models of intermediate complexity (EMICs) as part of a community contribution to the Intergovernmental Panel on Climate Change Fifth Assessment Report. Historical simulations start at 850 CE and continue through to 2005. The standard simulations include changes in forcing from solar luminosity, Earth's orbital configuration, CO2, additional greenhouse gases, land use, and sulphate and volcanic aerosols. In spite of very different modelled pre-industrial global surface air temperatures, overall 20th century trends in surface air temperature and carbon uptake are reasonably well simulated when compared to observed trends. Land carbon fluxes show much more variation between models than ocean carbon fluxes, and recent land fluxes appear to be slightly underestimated. It is possible that recent modelled climate trends or climate–carbon feedbacks are overestimated resulting in too much land carbon loss or that carbon uptake due to CO2 and/or nitrogen fertilization is underestimated. Several one thousand year long, idealized, 2 × and 4 × CO2 experiments are used to quantify standard model characteristics, including transient and equilibrium climate sensitivities, and climate–carbon feedbacks. The values from EMICs generally fall within the range given by general circulation models. Seven additional historical simulations, each including a single specified forcing, are used to assess the contributions of different climate forcings to the overall climate and carbon cycle response. The response of surface air temperature is the linear sum of the individual forcings, while the carbon cycle response shows a non-linear interaction between land-use change and CO2 forcings for some models. Finally, the preindustrial portions of the last millennium simulations are used to assess historical model carbon-climate feedbacks. Given the specified forcing, there is a tendency for the EMICs to underestimate the drop in surface air temperature and CO2 between the Medieval Climate Anomaly and the Little Ice Age estimated from palaeoclimate reconstructions. This in turn could be a result of unforced variability within the climate system, uncertainty in the reconstructions of temperature and CO2, errors in the reconstructions of forcing used to drive the models, or the incomplete representation of certain processes within the models. Given the forcing datasets used in this study, the models calculate significant land-use emissions over the pre-industrial period. This implies that land-use emissions might need to be taken into account, when making estimates of climate–carbon feedbacks from palaeoclimate reconstructions.

Long-term climate change commitment and reversibility: An EMIC Intercomparison

This paper summarizes the results of an intercomparison project with Earth System Models of Intermediate Complexity (EMICs) undertaken in support of the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5). The focus is on long-term climate projections designed to 1) quantify the climate change commitment of different radiative forcing trajectories and 2) explore the extent to which climate change is reversible on human time scales. All commitment simulations follow the four representative concentration pathways (RCPs) and their extensions to year 2300. Most EMICs simulate substantial surface air temperature and thermosteric sea level rise commitment following stabilization of the atmospheric composition at year-2300 levels. The meridional overturning circulation (MOC) is weakened temporarily and recovers to near-preindustrial values in most models for RCPs 2.6-6.0. The MOC weakening is more persistent for RCP8.5. Elimination of anthropogenic CO2 emissions after 2300 results in slowly decreasing atmospheric CO2 concentrations. At year 3000 atmospheric CO2 is still at more than half its year-2300 level in all EMICs for RCPs 4.5-8.5. Surface air temperature remains constant or decreases slightly and thermosteric sea level rise continues for centuries after elimination of CO2 emissions in all EMICs. Restoration of atmospheric CO2 from RCP to preindustrial levels over 100-1000 years requires large artificial removal of CO2 from the atmosphere and does not result in the simultaneous return to preindustrial climate conditions, as surface air temperature and sea level response exhibit a substantial time lag relative to atmospheric CO2.

Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics: a multi-model analysis

The responses of carbon dioxide (CO2) and other climate variables to an emission pulse of CO2 into the atmosphere are often used to compute the Global Warming Potential (GWP) and Global Temperature change Potential (GTP), to characterize the response timescales of Earth System models, and to build reduced-form models. In this carbon cycle-climate model intercomparison project, which spans the full model hierarchy, we quantify responses to emission pulses of different magnitudes injected under different conditions. The CO2 response shows the known rapid decline in the first few decades followed by a millennium-scale tail. For a 100 Gt-C emission pulse added to a constant CO2 concentration of 389 ppm, 25 ± 9% is still found in the atmosphere after 1000 yr; the ocean has absorbed 59 ± 12% and the land the remainder (16 ± 14%). The response in global mean surface air temperature is an increase by 0.20 ± 0.12 °C within the first twenty years; thereafter and until year 1000, temperature decreases only slightly, whereas ocean heat content and sea level continue to rise. Our best estimate for the Absolute Global Warming Potential, given by the time-integrated response in CO2 at year 100 multiplied by its radiative efficiency, is 92.5 × 10−15 yr W m−2 per kg-CO2. This value very likely (5 to 95% confidence) lies within the range of (68 to 117) × 10−15 yr W m−2 per kg-CO2. Estimates for time-integrated response in CO2 published in the IPCC First, Second, and Fourth Assessment and our multi-model best estimate all agree within 15% during the first 100 yr. The integrated CO2 response, normalized by the pulse size, is lower for pre-industrial conditions, compared to present day, and lower for smaller pulses than larger pulses. In contrast, the response in temperature, sea level and ocean heat content is less sensitive to these choices. Although, choices in pulse size, background concentration, and model lead to uncertainties, the most important and subjective choice to determine AGWP of CO2 and GWP is the time horizon.