Age and d18O analysis relating to Cenozoic greenhouse climatesXXX

Past episodes of greenhouse warming provide insight into the coupling of climate and the carbon cycle and thus may help to predict the consequences of unabated carbon emissions in the future.

Molecular and isotopic compositions of hydrocarbons at DSDP Site 76-533

In an investigation of gas hydrates in deep ocean sediments, gas samples from Deep Sea Drilling Project Site 533 on the Blake Outer Ridge in the northwest Atlantic were obtained for molecular and isotopic analyses. Gas samples were collected from the first successful deployment of a pressure core barrel (PCB) in a hydrate region. The pressure decline curves from two of the four PCB retrievals at in situ pressures suggested the presence of small amounts of gas hydrates. Compositional and isotopic measurements of gases from several points along the pressure decline curve indicated that (1) biogenic methane (d13C = -68 per mil; C1/C2 = 5000) was the dominant gas (>90%); (2) little fractionation in the C1/C2 ratio or the C carbon isotopic composition occurred as gas hydrates decomposed during pressure decline experiments; (3) the percent of C3, i-C4, and CO2 degassed increased as the pressure declined, indicating that these molecules may help stabilize the hydrate structure; (4) excess nitrogen was present during initial degassing; and (5) C1/C2 ratios and isotopic ratios of C gases were similar to those obtained from conventional core sampling. The PCB gas also contained trace amounts of saturated, acyclic, cyclic, and aromatic C5-C14 hydrocarbons, as well as alkenes and tetrahydrothiophenes. Gas from a decomposed specimen of gas hydrate had similar molecular and isotopic ratios to the PCB gas (d13C of -68 per mil for methane and a C1/C2 ratio of about 6000). Regular trends in the d13C of methane (about -95 to -60 per mil) and C1/C2 ratios (about 25000 to 2000) were observed with depth. Capillary gas chromatography (GC) and total scanning fluorescence measurements of extracted organic material were characteristic of hydrocarbons dominated by a marine source, though significant amounts of perylene were also present.

Noble gas concentrations of oceanic crust and sediments from the Ninety East Ridge in the Indian Ocean

We have determined the concentrations and isotopic composition of noble gases in old oceanic crust and oceanic sediments and the isotopic composition of noble gases in emanations from subduction volcanoes. Comparison with the noble gas signature of the upper mantle and a simple model allow us to conclude that at least 98% of the noble gases and water in the subducted slab returns back into the atmosphere through subduction volcanism before they can be admixed into the earth's mantle. It seems that the upper mantle is inaccessible to atmospheric noble gases due to an efficient subduction barrier for volatiles.

Table 2 & Appendix A. Properties of operations injecting CO2 into saline aquifers

The experience from CO2 injection at pilot projects (Frio, Ketzin, Nagaoka, US Regional Partnerships) and existing commercial operations (Sleipner, Snøhvit, In Salah, acid-gas injection) demonstrates that CO2 geological storage in saline aquifers is technologically feasible. Monitoring and verification technologies have been tested and demonstrated to detect and track the CO2 plume in different subsurface geological environments. By the end of 2008, approximately 20 Mt of CO2 had been successfully injected into saline aquifers by existing operations. Currently, the highest injection rate and total storage volume for a single storage operation are approximately 1 Mt CO2/year and 25 Mt, respectively. If carbon capture and storage (CCS) is to be an effective option for decreasing greenhouse gas emissions, commercial-scale storage operations will require orders of magnitude larger storage capacity than accessed by the existing sites. As a result, new demonstration projects will need to develop and test injection strategies that consider multiple injection wells and the optimisation of the usage of storage space. To accelerate large-scale CCS deployment, demonstration projects should be selected that can be readily employed for commercial use; i.e. projects that fully integrate the capture, transport and storage processes at an industrial emissions source.

Adsorption Calorimetry for Energy Conversion Technologies: Applications in Organic Photovoltaics, Catalysis, and Atomic Layer Deposition

Thesis (Ph.D.)--University of Washington, 2016-07

Techno-Economic Assessment of LNG and Diesel Production and Global Trading Based on Hybrid PV-Wind Power Plants and PtG, GtL and PtL Technologies

With growing demand for liquefied natural gas (LNG) and liquid transportation fuels, and concerns about climate change and causes of greenhouse gas emissions, this master’s thesis introduces a new value chain design for LNG and transportation fuels and respective fundamental business cases based on hybrid PV-Wind power plants. The value chains are composed of renewable electricity (RE) converted by power-to-gas (PtG), gas-to-liquids (GtL) or power-to-liquids (PtL) facilities into SNG (which is finally liquefied into LNG) or synthetic liquid fuels, mainly diesel, respectively. The RE-LNG or RE-diesel are drop-in fuels to the current energy system and can be traded everywhere in the world. The calculations for the hybrid PV-Wind power plants, electrolysis, methanation (H2tSNG), hydrogen-to-liquids (H2tL), GtL and LNG value chain are performed based on both annual full load hours (FLh) and hourly analysis. Results show that the proposed RE-LNG produced in Patagonia, as the study case, is competitive with conventional LNG in Japan for crude oil prices within a minimum price range of about 87 - 145 USD/barrel (20 – 26 USD/MBtu of LNG production cost) and the proposed RE-diesel is competitive with conventional diesel in the European Union (EU) for crude oil prices within a minimum price range of about 79 - 135 USD/barrel (0.44 – 0.75 €/l of diesel production cost), depending on the chosen specific value chain and assumptions for cost of capital, available oxygen sales and CO2 emission costs. RE-LNG or RE-diesel could become competitive with conventional fuels from an economic perspective, while removing environmental concerns. The RE-PtX value chain needs to be located at the best complementing solar and wind sites in the world combined with a de-risking strategy. This could be an opportunity for many countries to satisfy their fuel demand locally. It is also a specific business case for countries with excellent solar and wind resources to export carbon-neutral hydrocarbons, when the decrease in production cost is considerably more than the shipping cost. This is a unique opportunity to export carbon-neutral hydrocarbons around the world where the environmental limitations on conventional hydrocarbons are getting tighter.

Diversité microbienne associée au cycle du méthane dans les mares de fonte du pergélisol subarctique

La fonte et l’effondrement du pergélisol riche en glace dans la région subarctique du Québec ont donné lieu à la formation de petits lacs (mares de thermokarst) qui émettent des gaz à effet de serre dans l’atmosphère tels que du dioxyde de carbone et du méthane. Pourtant, la composition de la communauté microbienne qui est à la base des processus biogéochimiques dans les mares de fonte a été très peu étudiée, particulièrement en ce qui concerne la diversité et l’activité des micro-organismes impliqués dans le cycle du méthane. L’objectif de cette thèse est donc d’étudier la diversité phylogénétique et fonctionnelle des micro-organismes dans les mares de fonte subarctiques en lien avec les caractéristiques de l’environnement et les émissions de méthane. Pour ce faire, une dizaine de mares ont été échantillonnées dans quatre vallées situées à travers un gradient de fonte du pergélisol, et disposant de différentes propriétés physico-chimiques. Selon les vallées, les mares peuvent être issues de la fonte de palses (buttes de tourbe, à dominance organique) ou de lithalses (buttes de sol à dominance minérale) ce qui influence la nature du carbone organique disponible pour la reminéralisation microbienne. Durant l’été, les mares étaient fortement stratifiées; il y avait un fort gradient physico-chimique au sein de la colonne d’eau, avec une couche d’eau supérieure oxique et une couche d’eau profonde pauvre en oxygène ou anoxique. Pour identifier les facteurs qui influencent les communautés microbiennes, des techniques de séquençage à haut débit ont été utilisées ciblant les transcrits des gènes de l’ARNr 16S et des gènes impliqués dans le cycle du méthane : mcrA pour la méthanogenèse et pmoA pour la méthanotrophie. Pour évaluer l’activité des micro-organismes, la concentration des transcrits des gènes fonctionnels a aussi été mesurée avec des PCR quantitatives (qPCR). Les résultats montrent une forte dominance de micro-organismes impliqués dans le cycle du méthane, c’est-à-dire des archées méthanogènes et des bactéries méthanotrophes. L’analyse du gène pmoA indique que les bactéries méthanotrophes n’étaient pas seulement actives à la surface, mais aussi dans le fond de la mare où les concentrations en oxygène étaient minimales; ce qui est inattendu compte tenu de leur besoin en oxygène pour consommer le méthane. En général, la composition des communautés microbiennes était principalement influencée par l’origine de la mare (palse ou lithalse), et moins par le gradient de dégradation du pergélisol. Des variables environnementales clefs comme le pH, le phosphore et le carbone organique dissous, contribuent à la distinction des communautés microbiennes entre les mares issues de palses ou de lithalses. Avec l’intensification des effets du réchauffement climatique, ces communautés microbiennes vont faire face à des changements de conditions qui risquent de modifier leur composition taxonomique, et leurs réponses aux changements seront probablement différentes selon le type de mares. De plus, dans le futur les conditions d’oxygénation au sein des mares seront soumises à des modifications majeures associées avec un changement dans la durée des périodes de fonte de glace et de stratification. Ce type de changement aura un impact sur l’équilibre entre la méthanogenèse et la méthanotrophie, et affectera ainsi les taux d’émissions de méthane. Cependant, les résultats obtenus dans cette thèse indiquent que les archées méthanogènes et les bactéries méthanotrophes peuvent développer des stratégies pour survivre et rester actives au-delà des limites de leurs conditions d’oxygène habituelles.

Análise energética em central fixa de produção de massas asfálticas

O consumo energético nas indústrias é algo que tem de ser monitorizado, avaliado e orientado, visando a eficiência energética e sustentabilidade, de modo não só a reduzir o consumo de combustíveis fósseis, mas também a auxiliar a redução da fatura económica. O presente trabalho teve como principal objetivo uma análise energética, e incorpora a caracterização térmica dos materiais utilizados na indústria de produção de massas asfálticas, e o desenvolvimento de um modelo térmico que preveja o comportamento dos mesmos, na produção de massas asfálticas, em central fixa com incorporação de material reciclado a frio. Primariamente o estudo passou pela análise dos consumos energéticos da instalação, caracterizando-a segundo o Decretolei 71/2008, de 15 de Abril, tendo-se constatado, que o consumo de gás natural se evidencia como uma das principais fontes de energia e um dos principais responsáveis pela emissão de GEE (Gases de Efeito de Estufa). Posteriormente o consumo de gás natural foi distribuído pelos pontos consumidores, o cilindro exsicador e a caldeira de aquecimento de óleo térmico. O cilindro exsicador é o principal consumidor energético, com um consumo próximo de 90% do gás natural total. Seguidamente foi realizada uma caracterização dos materiais utilizados na produção de massas asfálticas segundo o DSC (Differential Scanning Calorimetry). Os materiais analisados foram o reciclado/fresado, o calcário, o pó de calcário, o seixo, a areia e o granito. Os resultados dos materiais secos demonstraram que o material com maior cp (calor específico) foi a areia e o menor o calcário. Nos resultados dos materiais saturados observou-se que o seixo apresenta maior facilidade de remoção de humidade e o reciclado/fresado apresenta menor. Por último, foi realizado um modelo térmico com utilização de um balanço mássico e energético ao processo de secagem e sobreaquecimento dos agregados no cilindro exsicador. Conclui-se que as principais influências no consumo de gás natural, na produção de massas asfálticas com inclusão de material reciclado a frio, são: a necessidade energética de aquecimento em função da temperatura a obter, e a energia necessária para remover o conteúdo em humidade presente nos diversos materiais (fresado e agregados).

Viabilidade do biodiesel de microalgas: otimização de técnicas de extração

Os problemas relacionados com o consumo energético e as emissões de poluentes relativas ao setor dos transportes representam seguramente a maior preocupação ao nível Europeu no que respeita aos gases com efeito de estufa e à poluição atmosférica. Uma das formas de resolver/minimizar estes problemas é através da aposta em combustíveis alternativos. Em particular, os biocombustíveis poderão ser uma alternativa interessante aos combustíveis convencionais. As microalgas, como matéria-prima para produção de biodiesel, apresentam-se com excelentes perspetivas de futuro e com vantagens competitivas no campo das energias renováveis. É nesta perspetiva que se enquadra o presente trabalho, cujos objetivos consistiram na extração de biodiesel a partir de microalgas secas (Nannochloropsis gaditana e Scenedesmus sp.) e na otimização das respetivas técnicas de extração lipídica. Verificou-se que, em função dos métodos e condições utilizadas, a espécie Nannochloropsis gaditana apresenta um potencial de produção de biodiesel superior à espécie Scenedesmus sp. (eficiências de extração de 24,6 (wt.%) e 9,4 (wt.%) respetivamente). Um método de rotura celular conjugado com o processo de extração lipídica via solvente orgânico é essencial, pois conseguiu-se um acréscimo de 42% no rendimento de extração, sendo 10 minutos o tempo ideal de operação. Solventes como o metanol e sistema de solventes diclorometano/metanol mostraram ser mais eficazes quando se pretende extrair lípidos de microalgas, com valores de eficiência de remoção de 30,9 (wt.%) e 23,2 (wt.%) respetivamente. De forma a valorizar os resultados obtidos no processo de extração recorreu-se à sua conversão em biodiesel através da transesterificação catalítica ácida, onde se obteve uma eficiência de conversão de 17,8 (wt.%) para a espécie Nannochloropsis gaditana.

Identificação do potencial renovável para produção de electricidade na perspectiva da microgeração

Tese submetida à Universidade de Lisboa, Faculdade de Ciências e aprovada em provas públicas para a obtenção do Grau de Doutor em Energia e Ambiente (especialidade em Energia e Desenvolvimento Sustentável).