La dynamique spatio-temporelle des flux d’oxyde nitreux (N2O) des lacs, rivières, et étangs boréaux

L’oxyde nitreux (N2O), un puissant gaz à effet de serre (GES) ayant plus de 300 fois le potentiel de réchauffement du dioxyde de carbone (CO2), est produit par des processus microbiens du cycle de l’azote (N). Bien que les eaux de surface continentales soient reconnues comme des sites actifs de transformations de l’azote, leur intégration dans les budgets globaux de N2O comporte de nombreuses incertitudes, dont l’absence des lacs dans ces modèles. Le biome boréal est caractérisé par une des plus grandes densités d’eaux douces au monde, pourtant aucune évaluation exhaustive des émissions aquatiques de N2O n’a à date été conduite dans cette région. Dans la présente étude, nous avons mesuré les concentrations de N2O à travers une large gamme de lacs, rivières, et étangs, dans quatre régions boréales du Québec (Canada), et nous avons calculé les flux eau-air résultants. Les flux nets fluctuent entre -23.1 et 177.9 μmol m-2 J-1, avec une grande variabilité inter-système, inter-régionale, et saisonnière. Étonnamment, 40% des systèmes échantillonnés agissaient en tant que puits de N2O durant l’été, et le réseau d’eaux de surfaces d’une des régions était un net consommateur de N2O. Les concentrations maximales de N2O ont été mesurées en hiver dû à l’accumulation de ce gaz sous la glace. Nous avons estimé que l’émission qui en résulte lors de la fonte des glaces représente 20% des émissions annuelles des eaux douces. Parmi les types d’eaux douces échantillonnées, les lacs sont les principaux responsables du flux aquatique net (jusqu’à 90%), et doivent donc être intégrés dans les budgets globaux de N2O. En se basant sur les données empiriques de la littérature, nous avons éstimé l’émission globale de N2O des eaux douces à 0.78 Tg N (N2O) an-1. Ce chiffre est influencé par les émissions des régions de hautes latitudes (tel que le biome boréal) dont les flux nets varient de positif à négatif constituant -9 à 27 % du total.

Dieselmotor-Kraft-Wärme-Kopplungsanlagen im Kontext der Integration Erneuerbarer Energien in die Energieversorgung

In dieser Arbeit werden die sich abzeichnenden zukünftigen Möglichkeiten, Stärken und Schwächen der Kraft-Wärme-Kopplung (KWK) untersucht. Dies geschieht vor dem Hintergrund des Klimawandels, der Integration steigender Anteile Erneuerbarer Energien in die Stromerzeugung und unter Berücksichtigung der sich damit ergebenden Herausforderungen, eine sichere und nachhaltige Stromversorgung zu gestalten. Der Fokus liegt auf der Dieselmotor-KWK und der Nutzung nachwachsender Kraftstoffe. Es wird davon ausgegangen, dass der Übergang zu einer reinen Stromerzeugung aus Erneuerbaren Energiequellen in Deutschland unter erheblicher Einbindung des hohen Potentials der kostengünstigen, umweltfreundlichen, aber in der Leistung extrem fluktuierenden Windenergie erfolgen wird. Als dezentrales Integrationswerkzeug wurde die Kraft-Wärme-Kopplung mit Dieselmotoren untersucht. Sie entspricht aufgrund ihrer großen Flexibilität und ihrer hohen Wirkungsgrade mit vergleichsweise kleinen Leistungen sehr gut den Anforderungen der gleichzeitigen dezentralen Wärmenutzung. In der Dissertation werden die Randbedingungen der Dieselmotor-KWK untersucht und beschrieben. Darauf aufbauend werden unterschiedliche Modelle der Windintegration durch KWK erarbeitet und in diversen Variationen wird der Ausgleich der Stromerzeugung aus Windenergie durch KWK simuliert. Darüber hinaus werden dezentrale KWK-Anlagen hinsichtlich eines koordinierten gemeinsamen Betriebs und hinsichtlich der optimalen Auslegung für den Windenergieausgleich betrachtet. Es wird für den beschriebenen Kontext der Erneuerbaren Energien und der Kraft-Wärme-Kopplung das Thema „Umweltwirkungen“ diskutiert. Es wird dargelegt, dass die heute verwendeten Ansätze zur Bewertung der KWK zu einer Verzerrung der Ergebnisse führen. Demgegenüber wurde mit der so genannten Outputmethode eine Methode der Ökobilanzierung vorgestellt, die, im Gegensatz zu den anderen Methoden, keine verzerrenden Annahmen in die Wirkungsabschätzung aufnimmt und somit eine eindeutige und rein wissenschaftliche Auswertung bleibt. Hiermit ist die Grundlage für die Bewertung der unterschiedlichen Technologien und Szenarien sowie für die Einordnung der KWK in den Kontext der Energieerzeugung gegeben. Mit der Outputmethode wird u.a. rechnerisch bewiesen, dass die gekoppelte Strom- und Wärmeerzeugung in KWK-Anlagen tatsächlich die optimale Nutzung der regenerativen Kraftstoffe „Biogas“ und „Pflanzenöl“ im Hinblick auf Ressourceneinsatz, Treibhausgaseinsparung und Exergieerzeugung ist. Es wurde darüber hinaus die Frage untersucht woher die für die Stromerzeugung durch Dieselmotor-KWK-Anlagen notwendige Bioenergie genommen werden kann. Es ist erwiesen, dass die in Deutschland nutzbare landwirtschaftliche Fläche nur zur Deckung eines Teils der Stromerzeugung ausreichen würde. Einheimisches Biogas und nachhaltiges importiertes Pflanzenöl, das in hohem Maße auf degradierten Böden angebaut werden sollte, können die notwendige Brennstoffenergie liefern. Um im Ausland ausreichend Pflanzenöl herstellen zu können, wird eine landwirtschaftliche Fläche von 6 bis 12 Mio. ha benötigt. Das Ergebnis ist, dass ein voller Ausgleich von Windenergie-Restlast durch KWK mit Erneuerbaren Energieträgern sinnvoll und machbar ist! Dieses Wind-KWK-DSM-System sollte durch ein Stromnetz ergänzt sein, das Wasserkraftstrom für den Großteil der Regelenergieaufgaben nutzt, und das den großräumigen Ausgleich Erneuerbarer Energien in Europa und den Nachbarregionen ermöglicht.

Life cycle GHG assessment of fossil fuel power plants with carbon capture and storage

The evaluation of life cycle greenhouse gas emissions from power generation with carbon capture and storage (CCS) is a critical factor in energy and policy analysis. The current paper examines life cycle emissions from three types of fossil-fuel-based power plants, namely supercritical pulverized coal (super-PC), natural gas combined cycle (NGCC) and integrated gasification combined cycle (IGCC), with and without CCS. Results show that, for a 90% CO2 capture efficiency, life cycle GHG emissions are reduced by 75-84% depending on what technology is used. With GHG emissions less than 170 g/kWh, IGCC technology is found to be favorable to NGCC with CCS. Sensitivity analysis reveals that, for coal power plants, varying the CO2 capture efficiency and the coal transport distance has a more pronounced effect on life cycle GHG emissions than changing the length of CO2 transport pipeline. Finally, it is concluded from the current study that while the global warming potential is reduced when MEA-based CO2 capture is employed, the increase in other air pollutants such as NOx and NH3 leads to higher eutrophication and acidification potentials.

A unifying framework for metrics for aggregating the climate effect of different emissions

Multi-gas approaches to climate change policies require a metric establishing ‘equivalences’ among emissions of various species. Climate scientists and economists have proposed four kinds of such metrics and debated their relative merits. We present a unifying framework that clarifies the relationships among them. We show, as have previous authors, that the global warming potential (GWP), used in international law to compare emissions of greenhouse gases, is a special case of the global damage potential (GDP), assuming (1) a finite time horizon, (2) a zero discount rate, (3) constant atmospheric concentrations, and (4) impacts that are proportional to radiative forcing. Both the GWP and GDP follow naturally from a cost–benefit framing of the climate change issue. We show that the global temperature change potential (GTP) is a special case of the global cost potential (GCP), assuming a (slight) fall in the global temperature after the target is reached. We show how the four metrics should be generalized if there are intertemporal spillovers in abatement costs, distinguishing between private (e.g., capital stock turnover) and public (e.g., induced technological change) spillovers. Both the GTP and GCP follow naturally from a cost-effectiveness framing of the climate change issue. We also argue that if (1) damages are zero below a threshold and (2) infinitely large above a threshold, then cost-effectiveness analysis and cost–benefit analysis lead to identical results. Therefore, the GCP is a special case of the GDP. The UN Framework Convention on Climate Change uses the GWP, a simplified cost–benefit concept. The UNFCCC is framed around the ultimate goal of stabilizing greenhouse gas concentrations. Once a stabilization target has been agreed under the convention, implementation is clearly a cost-effectiveness problem. It would therefore be more consistent to use the GCP or its simplification, the GTP.

Latitudinal variation of the effect of aviation NOx emissions on atmospheric ozone and methane and related climate metrics

We evaluate the response to regional and latitudinal changes in aircraft NOx emissions using several climate metrics (radiative forcing (RF), Global Warming Potential (GWP), Global Temperature change Potential (GTP)). Global chemistry transport model integrations were performed with sustained perturbations in regional aircraft and aircraft-like NOx emissions. The RF due to the resulting ozone and methane changes is then calculated. We investigate the impact of emission changes for specific geographical regions (approximating to USA, Europe, India and China) and cruise altitude emission changes in discrete latitude bands covering both hemispheres. We find that lower latitude emission changes (per Tg N) cause ozone and methane RFs that are about a factor of 6 larger than those from higher latitude emission changes. The net RF is positive for all experiments. The meridional extent of the RF is larger for low latitude emissions. GWPs for all emission changes are positive, with tropical emissions having the largest values; the sign of the GTP depends on the choice of time horizon.

A simple framework for assessing the trade-off between the climate impact of aviation carbon dioxide emissions and contrails for a single flight

Persistent contrails are an important climate impact of aviation which could potentially be reduced by re-routing aircraft to avoid contrailing; however this generally increases both the flight length and its corresponding CO emissions. Here, we provide a simple framework to assess the trade-off between the climate impact of CO emissions and contrails for a single flight, in terms of the absolute global warming potential and absolute global temperature potential metrics for time horizons of 20, 50 and 100 years. We use the framework to illustrate the maximum extra distance (with no altitude changes) that can be added to a flight and still reduce its overall climate impact. Small aircraft can fly up to four times further to avoid contrailing than large aircraft. The results have a strong dependence on the applied metric and time horizon. Applying a conservative estimate of the uncertainty in the contrail radiative forcing and climate efficacy leads to a factor of 20 difference in the maximum extra distance that could be flown to avoid a contrail. The impact of re-routing on other climatically-important aviation emissions could also be considered in this framework.

Radiative forcing and climate metrics for ozone precursor emissions: the impact of multi-model averaging

Multi-model ensembles are frequently used to assess understanding of the response of ozone and methane lifetime to changes in emissions of ozone precursors such as NOx, VOCs (volatile organic compounds) and CO. When these ozone changes are used to calculate radiative forcing (RF) (and climate metrics such as the global warming potential (GWP) and global temperature-change potential (GTP)) there is a methodological choice, determined partly by the available computing resources, as to whether the mean ozone (and methane) concentration changes are input to the radiation code, or whether each model's ozone and methane changes are used as input, with the average RF computed from the individual model RFs. We use data from the Task Force on Hemispheric Transport of Air Pollution source–receptor global chemical transport model ensemble to assess the impact of this choice for emission changes in four regions (East Asia, Europe, North America and South Asia). We conclude that using the multi-model mean ozone and methane responses is accurate for calculating the mean RF, with differences up to 0.6% for CO, 0.7% for VOCs and 2% for NOx. Differences of up to 60% for NOx 7% for VOCs and 3% for CO are introduced into the 20 year GWP. The differences for the 20 year GTP are smaller than for the GWP for NOx, and similar for the other species. However, estimates of the standard deviation calculated from the ensemble-mean input fields (where the standard deviation at each point on the model grid is added to or subtracted from the mean field) are almost always substantially larger in RF, GWP and GTP metrics than the true standard deviation, and can be larger than the model range for short-lived ozone RF, and for the 20 and 100 year GWP and 100 year GTP. The order of averaging has most impact on the metrics for NOx, as the net values for these quantities is the residual of the sum of terms of opposing signs. For example, the standard deviation for the 20 year GWP is 2–3 times larger using the ensemble-mean fields than using the individual models to calculate the RF. The source of this effect is largely due to the construction of the input ozone fields, which overestimate the true ensemble spread. Hence, while the average of multi-model fields are normally appropriate for calculating mean RF, GWP and GTP, they are not a reliable method for calculating the uncertainty in these fields, and in general overestimate the uncertainty.

Análise de desempenho de um refrigerador de pequeno porte com drop in de refrigerantes hidrocarbonetos

From what was stated in the Montreal Protocol, the researchers and refrigeration industry seek substitutes for synthetic refrigerants -chlorofluorocarbons (CFCs) and HCFCs (HCFC) - that contribute to the depletion of the ozone layer. The phase-out of these substances was started using as one of the replacement alternatives the synthetic fluids based on hydro fluorocarbons (HFCs) that have zero potential depletion of the ozone layer. However, contribute to the process of global warming. HFC refrigerants are greenhouse gases and are part of the group of gases whose emissions must be reduced as the Kyoto Protocol says. The hydrocarbons (HC's), for not contribute to the depletion of the ozone layer, because they have very low global warming potential, and are found abundantly in nature, has been presented as an alternative, and therefore, are being used in new home refrigeration equipment in several countries. In Brazil, due to incipient production of domestic refrigerators using HC's, the transition refrigerants remain on the scene for some years. This dissertation deals with an experimental evaluation of the conduct of a drinking fountain designed to work with HFC (R-134a), operating with a mixture of HC's or isobutane (R-600a) without any modification to the system or the lubricating oil. In the refrigeration laboratory of Federal University of Rio Grande do Norte were installed, in a drinking fountain, temperature and pressure sensors at strategic points in the refrigeration cycle, connected to an acquisition system of computerized data, to enable the mapping and thermodynamics analysis of the device operating with R-134a or with a mixture of HC's or with R-600a. The refrigerator-test operating with the natural fluids (mixture of HC's or R-600a) had a coefficient of performance (COP) lower than the R-134a

Emissões de poluentes em centrais hidrelétricas: aspectos técnicos, econômicos e ecológicos

Pós-graduação em Engenharia Mecânica - FEG

Uso da avaliação do ciclo de vida para a determinação na redução de emissões de gases do efeito estufa e do consumo de energia associados a reciclagem de EPS

Pós-graduação em Engenharia Mecânica - FEG

Flow Boiling Characteristics for R1234ze(E) in 1.0 and 2.2 mm Circular Channels

Experimental flow boiling heat transfer results are presented for horizontal 1.0 and 2.2 mm I. D. (internal diameter) stainless steel tubes for tests with R1234ze(E), a new refrigerant developed as a substitute for R134a with a much lower global warming potential (GWP). The experiments were performed for these two tube diameters in order to investigate a possible transition between macro and microscale flow boiling behavior. The experimental campaign includes mass velocities ranging from 50 to 1500 kg/m(2) s, heat fluxes from 10 to 300 kW/m(2), exit saturation temperatures of 25, 31 and 35 degrees C, vapor qualities from 0.05 to 0.99 and heated lengths of 180 mm and 361 mm. Flow pattern characterization was performed using high speed videos. Heat transfer coefficient, critical heat flux and flow pattern data were obtained. R1234ze(E) demonstrated similar thermal performance to R134a data when running at similar conditions. [DOI: 10.1115/1.4004933]

Life Cycle Assessment of Peach Nectar: a comparative analysis between conventional and bioenergy-from-waste integrated food chains

Modern food systems are characterized by a high energy intensity as well as by the production of large amounts of waste, residuals and food losses. This inefficiency presents major consequences, in terms of GHG emissions, waste disposal, and natural resource depletion. The research hypothesis is that residual biomass material could contribute to the energetic needs of food systems, if recovered as an integrated renewable energy source (RES), leading to a sensitive reduction of the impacts of food systems, primarily in terms of fossil fuel consumption and GHG emissions. In order to assess these effects, a comparative life cycle assessment (LCA) has been conducted to compare two different food systems: a fossil fuel-based system and an integrated system with the use of residual as RES for self-consumption. The food product under analysis has been the peach nectar, from cultivation to end-of-life. The aim of this LCA is twofold. On one hand, it allows an evaluation of the energy inefficiencies related to agro-food waste. On the other hand, it illustrates how the integration of bioenergy into food systems could effectively contribute to reduce this inefficiency. Data about inputs and waste generated has been collected mainly through literature review and databases. Energy balance, GHG emissions (Global Warming Potential) and waste generation have been analyzed in order to identify the relative requirements and contribution of the different segments. An evaluation of the energy “loss” through the different categories of waste allowed to provide details about the consequences associated with its management and/or disposal. Results should provide an insight of the impacts associated with inefficiencies within food systems. The comparison provides a measure of the potential reuse of wasted biomass and the amount of energy recoverable, that could represent a first step for the formulation of specific policies on the integration of bioenergies for self-consumption.

Valutazione dell'eco-sostenibilità di un impianto di digestione anaerobica cogenerativo e ipotesi di conversione impiantistica per la produzione di biometano

Considerando l'elevato grado di inquinamento del pianeta e la forte dipendenza delle attività antropiche dai combustibili fossili, stanno avendo notevole sviluppo e incentivazione gli impianti per la produzione di energia elettrica da fonti rinnovabili. In particolare, la digestione anaerobica è in grande diffusione in Italia. Lo studio in oggetto si prefigge l'obiettivo di determinare, mediante analisi di Life Cycle Assessment (LCA), i carichi ambientali di un impianto di digestione anaerobica, e della sua filiera, per valutarne l'effettiva ecosostenibilità. L'analisi considera anche gli impatti evitati grazie all'immissione in rete dell'energia elettrica prodotta e all'utilizzo del digestato in sostituzione dell'urea. Lo studio analizza sei categorie d'impatto: Global warming potential (GWP), Abiotic depletion potential (ADP), Acidification potential (AP), Eutrophication potential (EP), Ozone layer depletion potential (ODP) e Photochemical oxidant formation potential (POFP). I valori assoluti degli impatti sono stati oggetto anche di normalizzazione per stabilire la loro magnitudo. Inoltre, è stata effettuata un'analisi di sensitività per investigare le variazioni degli impatti ambientali in base alla sostituzione di differenti tecnologie per la produzione di energia elettrica: mix elettrico italiano, carbone e idroelettrico. Infine, sono stati analizzati due scenari alternativi all'impianto in esame che ipotizzano la sua conversione ad impianto per l'upgrading del biogas a biometano. I risultati mostrano, per lo scenario di riferimento (produzione di biogas), un guadagno, in termini ambientali, per il GWP, l'ADP e il POFP a causa dei notevoli impatti causati dalla produzione di energia elettrica da mix italiano che la filiera esaminata va a sostituire. I risultati evidenziano anche quanto gli impatti ambientali varino in base alla tipologia di alimentazione del digestore anaerobica: colture dedicate o biomasse di scarto. I due scenari alternativi, invece, mostrano un aumento degli impatti, rispetto allo scenario di riferimento, causati soprattutto dagli ulteriori consumi energetici di cui necessitano sia i processi di purificazione del biogas in biometano sia i processi legati alla digestione anaerobica che, nel caso dello scenario di riferimento, sono autoalimentati. L'eventuale conversione dell'attuale funzione dell'impianto deve essere fatta tenendo anche in considerazione i benefici funzionali ed economici apportati dalla produzione del biometano rispetto a quella del biogas.

Effective water treatment for rural communities in Suriname : a comparison of point-of-use ceramic filters and centralized treatment with sand filters

For countless communities around the world, acquiring access to safe drinking water is a daily challenge which many organizations endeavor to meet. The villages in the interior of Suriname have been the focus of many improved drinking water projects as most communities are without year-round access. Unfortunately, as many as 75% of the systems in Suriname fail within several years of implementation. These communities, scattered along the rivers and throughout the jungle, lack many of the resources required to sustain a centralized water treatment system. However, the centralized system in the village of Bendekonde on the Upper Suriname River has been operational for over 10 years and is often touted by other communities. The Bendekonde system is praised even though the technology does not differ significantly from other failed systems. Many of the water systems that fail in the interior fail due to a lack of resources available to the community to maintain the system. Typically, the more complex a system becomes, so does the demand for additional resources. Alternatives to centralized systems include technologies such as point-of-use water filters, which can greatly reduce the necessity for outside resources. In particular, ceramic point-of-use water filters offer a technology that can be reasonably managed in a low resource setting such as that in the interior of Suriname. This report investigates the appropriateness and effectiveness of ceramic filters constructed with local Suriname clay and compares the treatment effectiveness to that of the Bendekonde system. Results of this study showed that functional filters could be produced from Surinamese clay and that they were more effective, in a controlled laboratory setting, than the field performance of the Bendekonde system for removing total coliform. However, the Bendekonde system was more successful at removing E. coli. In a life-cycle assessment, ceramic water filters manufactured in Suriname and used in homes for a lifespan of 2 years were shown to have lower cumulative energy demand, as well as lower global warming potential than a centralized system similar to that used in Bendekonde.

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.