abstract: In enzyme induced carbonate precipitation (EICP), calcium carbonate (CaCO3) precipitation is catalyzed by plant-derived urease enzyme. In EICP, urea hydrolyzes into ammonia and inorganic carbon, altering geochemical conditions in a manner that promotes carbonate mineral precipitation. The calcium source in this process comes from calcium chloride (CaCl2) in aqueous solution. Research work conducted for this dissertation has demonstrated that EICP can be employed for a variety of geotechnical purposes, including mass soil stabilization, columnar soil stabilization, and stabilization of erodible surficial soils. The research presented herein also shows that the optimal ratio of urea to CaCl2 at ionic strengths of less than 1 molar is approximately 1.75:1. EICP solutions of very high initial ionic strength (i.e. 6 M) as well as high urea concentrations (> 2 M) resulted in enzyme precipitation (salting-out) which hindered carbonate precipitation. In addition, the production of NH4+ may also result in enzyme precipitation. However, enzyme precipitation appeared to be reversible to some extent. Mass soil stabilization was demonstrated via percolation and mix-and-compact methods using coarse silica sand (Ottawa 20-30) and medium-fine silica sand (F-60) to produce cemented soil specimens whose strength improvement correlated with CaCO3 content, independent of the method employed to prepare the specimen. Columnar stabilization, i.e. creating columns of soil cemented by carbonate precipitation, using Ottawa 20-30, F-60, and native AZ soil was demonstrated at several scales beginning with small columns (102-mm diameter) and culminating in a 1-m3 soil-filled box. Wind tunnel tests demonstrated that surficial soil stabilization equivalent to that provided by thoroughly wetting the soil can be achieved through a topically-applied solution of CaCl2, urea, and the urease enzyme. The topically applied solution was shown to form an erosion-resistant CaCO3 crust on fine sand and silty soils. Cementation of erodible surficial soils was also achieved via EICP by including a biodegradable hydrogel in the stabilization solution. A dilute hydrogel solution extended the time frame over which the precipitation reaction could occur and provided improved spatial control of the EICP solution. / Dissertation/Thesis / Doctoral Dissertation Civil and Environmental Engineering 2015

abstract: Chemical and physical interactions of flowing ice and rock have inexorably shaped planetary surfaces. Weathering in glacial environments is a significant link in biogeochemical cycles – carbon and strontium – on Earth, and may have once played an important role in altering Mars’ surface. Despite growing recognition of the importance of low-temperature chemical weathering, these processes are still not well understood. Debris-coated glaciers are also present on Mars, emphasizing the need to study ice-related processes in the evolution of planetary surfaces. During Earth’s history, subglacial environments are thought to have sheltered communities of microorganisms from extreme climate variations. On Amazonian Mars, glaciers such as lobate debris aprons (LDA) could have hosted chemolithotrophic communities, making Mars’ present glaciers candidates for life preservation. This study characterizes glacial processes on both Earth and Mars. Chemical weathering at Robertson Glacier, a small alpine glacier in the Canadian Rocky Mountains, is examined with a multidisciplinary approach. The relative proportions of differing dissolution reactions at various stages in the glacial system are empirically determined using aqueous geochemistry. Synthesis of laboratory and orbital thermal infrared spectroscopy allows identification of dissolution rinds on hand samples and characterization of carbonate dissolution signals at orbital scales, while chemical and morphological evidence for thin, discontinuous weathering rinds at microscales are evident from electron microscopy. Subglacial dissolution rates are found to outpace those of the proglacial till plain; biologically-mediated pyrite oxidation drives the bulk of this acidic weathering. Second, the area-elevation relationship, or hypsometry, of LDA in the midlatitudes of Mars is characterized. These glaciers are believed to have formed ~500 Ma during a climate excursion. Hypsometric measurements of these debris-covered glaciers enable insight into past flow regimes and drive predictions about past climate scenarios. The LDA in this study fall into three major groups, strongly dependent on basal elevation, implying regional and climatic controls on ice formation and flow. I show that biologically-mediated mineral reactions drive high subglacial dissolution rates, such that variations within the valley can be detected with remote sensing techniques. In future work, these insights can be applied to examining Mars’ glacial regions for signs of chemical alteration and biosignatures. / Dissertation/Thesis / Doctoral Dissertation Geological Sciences 2015

abstract: The dissimilatory reduction of nitrate, or denitrification, offers the potential of a sustainable, cost effective method for the non-disruptive mitigation of earthquake-induced soil liquefaction. Worldwide, trillions of dollars of infrastructure are at risk for liquefaction damage in earthquake prone regions. However, most techniques for remediating liquefiable soils are either not applicable to sites near existing infrastructure, or are prohibitively expensive. Recently, laboratory studies have shown the potential for biogeotechnical soil improvement techniques such as microbially induced carbonate precipitation (MICP) to mitigate liquefaction potential in a non-disruptive manner. Multiple microbial processes have been identified for MICP, but only two have been extensively studied. Ureolysis, the most commonly studied process for MICP, has been shown to quickly and efficiently induce carbonate precipitation on particle surfaces and at particle contacts to improve the stiffness, strength, and dilatant behavior of liquefiable soils. However, ureolysis also produces copious amounts of ammonium, a potentially toxic byproduct. The second process studied for MICP, denitrification, has been shown to precipitate carbonate, and hence improve soil properties, much more slowly than ureolysis. However, the byproducts of denitrification, nitrogen and carbon dioxide gas, are non-toxic, and present the added benefit of rapidly desaturating the treated soil. Small amounts of desaturation have been shown to increase the cyclic resistance, and hence the liquefaction resistance, of liquefiable soils. So, denitrification offers the potential to mitigate liquefaction as a two-stage process, with desaturation providing short term mitigation, and MICP providing long term liquefaction resistance. This study presents the results of soil testing, stoichiometric modeling, and microbial ecology characterization to better characterize the potential use of denitrification as a two-stage process for liquefaction mitigation. / Dissertation/Thesis / Doctoral Dissertation Civil and Environmental Engineering 2016

abstract: This study explores the possibility of two matrices containing metallic particulates to act as smart materials by sensing of strain due to the presence of the conducting particles in the matrix. The first matrix is a regular Portland cement-based one while the second is a novel iron-based, carbonated binder developed at ASU. Four different iron replacement percentages by volume (10%, 20%, 30% and 40%) in a Portland cement matrix were selected, whereas the best performing iron carbonate matrix developed was used. Electrical impedance spectroscopy was used to obtain the characteristic Nyquist plot before and after application of flexural load. Electrical circuit models were used to extract the changes in electrical properties under application of load. Strain sensing behavior was evaluated with respect to application of different stress levels and varying replacement levels of the inclusion. A similar approach was used to study the strain sensing capabilities of novel iron carbonate binder. It was observed that the strain sensing efficiency increased with increasing iron percentage and the resistivity increased with increase in load (or applied stress) for both the matrices. It is also found that the iron carbonate binder is more efficient in strain sensing as it had a higher gage factor when compared to the OPC matrix containing metallic inclusions. Analytical equations (Maxwell) were used to extract frequency dependent electrical conductivity and permittivity of the cement paste (or the host matrix), interface, inclusion (iron) and voids to develop a generic electro-mechanical coupling model to for the strain sensing behavior. COMSOL Multiphysics 5.2a was used as finite element analysis software to develop the model. A MATLAB formulation was used to generate the microstructure with different volume fractions of inclusions. Material properties were assigned (the frequency dependent electrical parameters) and the coupled structural and electrical physics interface in COMSOL was used to model the strain sensing response. The experimental change in resistance matched well with the simulated values, indicating the applicability of the model to predict the strain sensing response of particulate composite systems. / Dissertation/Thesis / Masters Thesis Civil and Environmental Engineering 2017

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / Este trabalho teve como objetivo geral avaliar o potencial das imagens do sensor ASTER, utilizando a região do infravermelho de ondas curtas (SWIR), para discriminação espectral de rochas carbonáticas aflorantes na região Noroeste do Estado do Rio de Janeiro, complementando produtos existentes de mapeamento geológico. As rochas carbonáticas servem de matéria-prima para produção de cimento, que atualmente apresenta forte demanda dado o crescimento de obras civis devido à expansão da infraestrutura do Estado do Rio de Janeiro. Este crescimento no consumo oferece desafios às companhias produtoras, tornando-se de vital importância a identificação de novas áreas para exploração de insumos para a indústria civil. Neste sentido, o carbonato tem sofrido grande pressão com relação a sua produção pois é a principal matéria-prima utilizada na fabricação do cimento. Imagens do sensor Aster vem sendo utilizadas na área da geologia com êxito, discriminando litologias e minerais como quartzo, óxido de ferro e calcita. Na região do intervalo de ondas entre 2,235-2,285 μm e 2,295-2,365 μm , as bandas 7 e 8 do sensor ASTER na região do SWIR, mostram-se adequadas para a identificação de minerais de calcita e dolomita. Como metodologia, foram aplicadas as técnicas de razões de bandas para separação de calcários e dolomitos e para a classificação espectral, foi utilizada a técnica SAM. Tornou-se como referência para a classificação espectral amostras de áreas de rochas carbonáticas aflorantes e espectros da biblioteca espectral da USGS. As classificações espectrais obtiveram resultados significativos na discriminação espectral das áreas carbonáticas, no entanto as técnicas de razões de bandas não obtiveram resultados suficientes para a discriminação de calcários e dolomitos. Para trabalhos futuros sugere-se a realização de trabalho de campo para a coleta de espectros, através da espectrorradiometria dos afloramentos dos carbonatos. / This work had as main objective to evaluate the potential of ASTER images using the region of shortwave infrared (SWIR), for spectral discrimination of carbonate rocks outcropping in the northwestern part of the State of Rio de Janeiro region, complementing existing products geological mapping . The carbonate rocks serve as raw material for cement production, which currently presents strong demand given the growth of civil works due to the expansion of the State of Rio de Janeiro's infrastructure. This growth in consumption offers challenges to production companies, making it vitally important to identify new areas for exploration of inputs for civil industry. In this sense, the carbonate has undergone great pressure with respect to its production as it is the main raw material used in cement production. Aster images sensor is being used in the field of geology successfully discriminating lithologies and minerals such as quartz, iron oxide and calcite. In the interval between waves from 2.235 to 2.285 m and 2.295 to 2.365 μm region, the bands 7 and 8 in the ASTER SWIR region are adequate for identifying minerals calcite and dolomite. As a methodology, techniques of reasons for separation of bands of limestones and dolomites and the spectral classification were applied, the SAM technique was used. Became as reference samples for the spectral classification of areas of outcropping carbonate rocks and spectra from the USGS spectral library. The spectral classifications obtained significant results in the spectral discrimination of the carbonate areas, however the techniques of reasons bands did not achieve sufficient results for the discrimination of limestones and dolomites. For future work is suggested to conduct fieldwork to collect spectra by spectroradiometry outcrops of carbonates

A urolitíase é um problema recorrente na clínica veterinária considerada como causa de morbidade. As urolitíases são estreitamente associadas ao pH urinário e a nutrição exerce um papel fundamental no controle desta afecção, pois através da manipulação da dieta, pode-se modificar o pH urinário. A dieta possui cátions e ânions na sua composição mineral e a diferença entre íons é medida em miliequivalentes (mEq/kg) e denominado excesso de bases (EB) da dieta, calculado através da equação: (49,9 x Ca) + (82,3 x Mg) + (43,5 x Na) + (25,6 x K) – (64,6 x P) – (62,4 x S) – (28,2 x Cl), sendo a concentração dos elementos em g/kg de MS. A finalidade deste estudo, dividido em dois experimentos, foi avaliar o efeito da adição de fontes de enxofre (S) e cálcio nas dietas de felinos sobre o pH urinário e equilíbrio ácido-básico. A adição de fontes de enxofre objetivou demonstrar a eficácia na acidificação urinária. No primeiro experimento avaliaram-se três diferentes fontes de enxofre: sulfato de cálcio (CaSO4), DL-metionina (DLM) e Metionina hidróxi análoga (MHA) adicionados a uma dieta controle em dois níveis cada um. No tratamento controle não houve adição de acidificantes. No primeiro nível adicionou-se 1,28 g de S/kg e no segundo 2,56 g de S/kg, resultando em sete tratamentos. No segundo experimento duas fontes de cálcio foram avaliadas com o objetivo de pesquisar a eficácia destes sais na alcalinização da urina. No tratamento controle não houve adição de fontes de cálcio. Nos tratamentos 2 e 3 foram adicionados à dieta controle carbonato de cálcio e gluconato de cálcio, respectivamente, nas doses de +160 mEq/kg, resultando em três tratamentos. A urina produzida em cada período de 24 horas teve aferida seu volume, densidade e pH. No segundo experimento foi também medida a excreção urinária de cálcio no período de 72h. O equilíbrio ácido-básico foi avaliado pela hemogasometria de sangue venoso. A DLM no maior nível e o MHA diferiram da dieta controle em relação ao pH urinário (p<0,001) e seu poder acidificante foi maior que o do sulfato de cálcio (p<0,05). As duas fontes de cálcio alcalinizaram a urina, mas o carbonato de cálcio atingiu um pH urinário mais alto que o gluconato de cálcio. Concluiu-se que o efeito diferenciado das fontes de S e cálcio sobre o pH urinário é um indicador de que a participação do cálcio é dependente dos ânions a que está associado, o que leva ao questionamento sobre qual a melhor forma de avaliar sua participação no cálculo do EB. / Urolithiasis is a commom problem in the veterinary clinic considered as a cause of morbidity. The urolithiasis are closely associated with urinary pH and nutrition plays a key role in the control of this disease, because through dietary manipulation, it´s possible modify the urinary pH. The diet has cations and anions in their mineral composition and the difference between ions is measured in milliequivalents (mEq/kg) and called base excess (BE) of the diet, calculated by the equation: (49.9 x Ca) + (82, Mg x 3) + (43.5 x Na) + (25.6 x K) - (64.6 x P) - (62.4 x S) - (28.2 x Cl), being the concentration of elements in g/kg DM. The purpose of this study, divided in two experiments, was to evaluate the effect of addition of sources of sulfur (S) and calcium in the diets of cats on the urinary pH and acid-base balance. The addition of sulfur sources aimed to demonstrate the efficacy in urinary acidification. In the first experiment were evaluated three different sources of sulfur, calcium sulfate (CaSO4), DLMethionine (DLM) and Methionine hydroxy analogue (MHA) added to a control diet at two levels each. In the control treatment there was no addition of acidifying. At the first level was added 1.28 g S/kg and in the second 2.56 g S/kg, resulting in seven treatments. In the second experiment two calcium sources were evaluated in order to research the effectiveness of these salts in alkalinize urine. In the control treatment there was no addition of calcium sources. In treatments 2 and 3 were added to the control diet calcium carbonate and calcium gluconate, respectively, at doses of +160 mEq/kg, resulting in three treatments. The urine produced in each period of 24 hours had measured its volume, density and pH. The second experiment also measured the urinary excretion of calcium in the period of 72 hours. The acid-base balance was evaluated by blood gas analysis of venous blood. The DLM at the highest level and MHA differed of the control diet in relation to urinary pH (p<0.001) and their acidifying power was greater than the calcium sulfate (p<0.05). The two sources of calcium alkalinized the urine, but the calcium carbonate reached a urine pH higher than calcium gluconate. It was concluded that the effect of different sources of S and calcium on urinary pH is an indicator that the participation of calcium is dependent of the anions that is associated, which leads to questions about how is the best way to evaluate its participation in calculation of BE.

A indústria da construção civil é conhecida como umas das atividades econômicas que causam os maiores impactos ambientais desde o processo de extração da matéria prima até a produção dos produtos, incluindo o transporte e manutenção do ambiente construído. A produção de um dos seus principais componentes, o cimento, é o maior contribuinte para a emissão de gases de efeito estufa, principalmente devido a queima de combustíveis fósseis. Por este motivo, pesquisas na área de biotecnologia sustentável são conduzidas para diminuir e até mitigar os efeitos danosos provocados pelos fatores que compõem a construção civil. Dentre estas pesquisas destacam-se as que se baseiam na Biomimética, que é uma ciência que busca na Natureza as soluções tecnológicas para os problemas que os desenvolvimentos humanos geralmente apresentam: a geração de resíduos poluentes, uso de produtos químicos tóxicos e processos que operam com energia e pressão elevadas. Com base nos conceitos biomiméticos, este trabalho se propôs a estudar a biomineralização, que é um processo que ocorre na Natureza a milhares de anos e é responsável pela formação de muitas estruturas biomineralizadas tanto no ambiente terrestre como aquático. A biomineralização é um fenômeno provocado pela ação de diversas espécies de microrganismos que durante o processo de obtenção de energia reciclam minerais presentes no solo e na água e os precipitam na forma de sais inorgânicos. Este material precipitado age como agente ligante de partículas como no caso de formações geológicas (estromatólitos) ou exoesqueletos de animais marinhos, por exemplo. Neste estudo foi avaliado a biomineralização por biodeposição de carbonato de cálcio precipitado na presença da espécie de bactéria ureolítica (Bacillus subtilis) em ensaios em escala laboratorial utilizando corpos de prova de areia, argamassa e concreto. Os corpos de prova em areia e argamassa foram observados em MEV e EDS permitindo a identificação de células de microrganismos, formação de biofilme e provável formação de cristais de carbonato de cálcio na região de biofilme. Os corpos de prova de concreto foram utilizados para avaliar as consequências da biodeposição na absorção de água por capilaridade do material. Resultados indicam redução de 20% na absorção de água por capilaridade. Com os resultados obtidos é possível concluir que a técnica de biodeposição pode ser uma alternativa ao tratamento superficial de estruturas de concreto, contudo requer estudos posteriores de aplicação técnica e viabilidade econômica. / The construction industry has been known as one of the economic activities that cause the major environment impacts since the process of raw material extraction until the products manufacturing including transport and maintenance of the built environment. The production of one of the main compounds, the cement, is the largest contributor to the greenhouse gas emissions, mainly due to burn fossil fuels. For this reason, researches in sustainable biotechnological area are conducted to minimize and even mitigate the damaging effects either promoted by construction industry factors. Among these ones, it stands out researches based on Biomimetic, which is a science that seeks in Nature the technological solutions for problems that human’s development usually presents: the generation of pollutant residues, the use of toxic chemicals and process that operates in high pressure and energy. Based on biomimetic concepts this research proposes to study the biomineralization, which is a process that has occurred in the Nature for thousands of years and it is responsible for the formation of many structures either in soil and water environments. The biomineralization is a phenomenon caused by several specimens of microorganisms that during the process of obtaining energy, they recycle minerals presents at soil and water inducing precipitation as inorganic salts. This precipitated material works as a binder of particles similar to geologic formations (stromatolites) or exoskeleton of sea animal for example. In this study the biomineralization was evaluated through biodeposition of precipitated calcium carbonate by specimen of ureolytic bacteria (Bacillus subtilis). Essays were held using samples made by sand, mortar and concrete. The samples made by sand and mortar were observed at MEV and EDS, allowing the identification of microorganism cells, biofilm formation and probable formation of calcium carbonate crystals at biofilm region. The concrete samples were used to evaluate the consequences of biodeposition on water absorption by capillarity of the material. The results show reduction of 20% on water absorption by capillarity. According the results achieved it possible to conclude that the biodeposition technique can be an alternative to superficial treatment for concrete structures. However, it will be required more studies to evaluate technical application and economical availability.

Na costa do leste do Brasil, destacam-se importantes acumulações de carbonatos lacustres do Cretáceo (Aptiano) relacionadas à fase de rift que precede a abertura do Oceano Atlântico, estes carbonatos consistem principalmente em espessos pacotes de bivalves associados a sedimentos siliciclásticos finos. Na bacia de Campos este intervalo equivale a Formação Coqueiros e é portador de hidrocarbonetos sendo reservatório nos campos de Badejo, Linguado, Pampo e Trilha. Estes reservatórios são o foco deste estudo, que teve como objetivo aprofundar o conhecimento desses depósitos através da análise das fácies e associações de fácies para definição de sequências seguindo a compreensão atual dos conceitos de estratigrafia de sequência. Foram descritos testemunhos de poços associados a análise de dados de perfil e sísmica através das quais foram definidas dezesseis fácies. A classificação das fácies utilizou critérios sedimentológicos associados a conceitos tafonômicos o que permitiu a intepretação dos processos sedimentares envolvidos em sua deposição Estas fácies foram agrupadas em associações de acordo com gradiente hidrodinâmico de uma plataforma dominada por ondas o que permitiu a interpretação dos padrões de empilhamento e definição de tratos de sistema transgressivos e regressivos. Foi proposto um ciclo ideal de alta frequência com a sucessão esperada de fácies para cada trato que serviu de base para interpretação de sequências de alta e média frequência. Esta análise permitiu a definição de três sequências internas no intervalo conhecido como Coquina Inferior, correlacionadas entre os poços que possuíam a melhor amostragem do intervalo permitindo assim analisar a variação vertical e lateral de fácies. A metodologia proposta permite a intepretação da estratigrafia em uma escala de maior detalhe auxiliando a interpretação da ocorrência de fácies e sua distribuição espacial na escala de dezenas a centenas de metros. Este tipo de análise é importante para desenvolvimento da produção de campos de hidrocarbonetos sendo útil na construção de modelos geológicos. Pode ser aplicável a ambientes análogos com similaridades quanto à composição das rochas e os processos envolvidos em sua deposição, como a Formação Itapema análoga na Bacia de Santos. / On the eastern Brazilian coast there is an important accumulation of Cretaceous lacustrine carbonates linked to the rift phase, which precedes the opening of the Atlantic Ocean. These carbonates consist mainly of bivalve packages associated with fine siliciclastic sediments. In the Campos Basin this interval is denominated Coqueiros Formation and constitutes a hydrocarbon reservoir in the fields of Badejo, Linguado, Pampo and Trilha. These reservoirs are the focus of this study, which aimed to detail the knowledge of these deposits through the analysis of facies and their associations in order to define sequences according to the present understanding of sequence stratigraphy concepts. Core samples description, well logs and seismic data analyses have been carried out, allowing the definition of sixteen facies. The facies classification was based on sedimentary characteristics associated with taphonomic concepts that allowed the interpretation of sedimentary processes involved in the deposition. These facies were grouped in associations according to a hydrodynamic gradient of a wave-dominated platform, which allowed the interpretation of stacking patterns and the definition of both transgressive and regressive system tracts It was proposed an ideal high frequency cycle with the facies succession from each tract which was used for the interpretation of high and medium frequency sequences. This analysis allowed the definition of three internal sequences in the so-called Lower Coquina Interval correlated among the best sampled wells, and the analysis of vertical and lateral variation of facies. The proposed methodology allows the interpretation of the stratigraphy in a small scale contributing to the interpretation of the occurrence of facies and their spatial distribution in a scale of tens to hundreds of meters. This type of analysis is important for the development of production in a hydrocarbon field and is useful for the construction of geological models and is applicable to similar environments with same composition of the rocks and similarities in the processes involved in their deposition, such as the Itapema Formation in the Santos Basin.

abstract: Microbially induced calcium carbonate precipitation (MICP) is attracting increasing attention as a sustainable means of soil improvement. While there are several possible MICP mechanisms, microbial denitrification has the potential to become one of the preferred methods for MICP because complete denitrification does not produce toxic byproducts, readily occurs under anoxic conditions, and potentially has a greater carbonate yield per mole of organic electron donor than other MICP processes. Denitrification may be preferable to ureolytic hydrolysis, the MICP process explored most extensively to date, as the byproduct of denitrification is benign nitrogen gas, while the chemical pathways involved in hydrolytic ureolysis processes produce undesirable and potentially toxic byproducts such as ammonium (NH4+). This thesis focuses on bacterial denitrification and presents preliminary results of bench-scale laboratory experiments on denitrification as a candidate calcium carbonate precipitation mechanism. The bench-scale bioreactor and column tests, conducted using the facultative anaerobic bacterium Pseudomonas denitrificans, show that calcite can be precipitated from calcium-rich pore water using denitrification. Experiments also explore the potential for reducing environmental impacts and lowering costs associated with denitrification by reducing the total dissolved solids in the reactors and columns, optimizing the chemical matrix, and addressing the loss of free calcium in the form of calcium phosphate precipitate from the pore fluid. The potential for using MICP to sequester radionuclides and metal contaminants that are migrating in groundwater is also investigated. In the sequestration process, divalent cations and radionuclides are incorporated into the calcite structure via substitution, forming low-strontium calcium carbonate minerals that resist dissolution at a level similar to that of calcite. Work by others using the bacterium Sporosarcina pasteurii has suggested that in-situ sequestration of radionuclides and metal contaminants can be achieved through MICP via hydrolytic ureolysis. MICP through bacterial denitrification seems particularly promising as a means for sequestering radionuclides and metal contaminants in anoxic environments due to the anaerobic nature of the process and the ubiquity of denitrifying bacteria in the subsurface. / Dissertation/Thesis / M.S. Engineering 2013

abstract: Of the potential technologies for pre-combustion capture, membranes offer the advantages of being temperature resistant, able to handle large flow rates, and having a relatively small footprint. A significant amount of research has centered on the use of polymeric and microporous inorganic membranes to separate CO2. These membranes, however, have limitations at high temperature resulting in poor permeation performance. To address these limitations, the use of a dense dual-phase membrane has been studied. These membranes are composed of conductive solid and conductive liquid phases that have the ability to selectively permeate CO2 by forming carbonate ions that diffuse through the membrane at high temperature. The driving force for transport through the membrane is a CO2 partial pressure gradient. The membrane provides a theoretically infinite selectivity. To address stability of the ceramic-carbonate dual-phase membrane for CO2 capture at high temperature, the ceramic phase of the membrane was studied and replaced with materials previously shown to be stable in harsh conditions. The permeation properties and stability of La0.6Sr0.4Co0.8Fe0.2O3-&delta; (LSCF)-carbonate, La0.85Ce0.1Ga0.3Fe0.65Al0.05O3-&delta; (LCGFA)-carbonate, and Ce0.8Sm0.2O1.9 (SDC)-carbonate membranes were examined under a wide range of experimental conditions at high temperature. LSCF-carbonate membranes were shown to be unstable without the presence of O2 due to reaction of CO2 with the ceramic phase. In the presence of O2, however, the membranes showed stable permeation behavior for more than one month at 900oC. LCGFA-carbonate membranes showed great chemical and permeation stability in the presence of various conditions including exposure to CH4 and H2, however, the permeation performance was quite low when compared to membranes in the literature. Finally, SDC-carbonate membranes showed great chemical and permeation stability both in a CO2:N2 environment for more than two weeks at 900oC as well as more than one month of exposure to simulated syngas conditions at 700oC. Ceramic phase chemical stability increased in the order of LSCF < LCGFA < SDC while permeation performance increased in the order of LCGFA < LSCF < SDC. / Dissertation/Thesis / Ph.D. Chemical Engineering 2013