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[en] OPERATION CAR WASH: OPTION FOR POLITICAL LAWFARE AND JURISDICTION AS A SOURCE OF EXCEPTION / [pt] OPERAÇÃO LAVA JATO: OPÇÃO PELO LAWFARE E PELA JURISDIÇÃO COMO FONTE DA EXCEÇÃOJOSE DA SILVA RAIMUNDO 28 October 2022 (has links)
[pt] A presente dissertação investiga e analisa a instrumentalização do processo
penal, convertido em arma de guerra – lawfare -, para viabilizar práticas autoritárias
punitivas amparadas no casuísmo, no âmbito da chamada Operação Lava Jato, bem
como analisa o manejo/utilização/implementação de mecanismos de exceção
dentro da rotina democrática brasileira com o fim de eliminar um inimigo
personificado na figura do ex-presidente Lula, objetivando retirá-lo da corrida
eleitoral de 2018, estabelecendo, assim, a consolidação do golpe iniciado em 2016,
com a derrubada da Presidenta Dilma Rousseff. O trabalho discute a Operação Lava
Jato abordando o fenômeno do intercruzamento entre direito e política (ativismo
judicial, judicialização da política e politização da justiça), analisando criticamente
a atuação da grande mídia hegemônica oligopolista brasileira. Desta forma, esta
pesquisa enfrenta essa questão a partir do fenômeno identificado como lawfare. No
capítulo introdutório, é apresentado o tema, problema, hipóteses, objeto da
pesquisa, a justificativa do trabalho, referencial teórico e metodologia da pesquisa.
No segundo capítulo são apresentadas algumas abordagens conceituais sobre o
termo lawfare, desenvolvidas por diversos intelectuais que se debruçaram sobre o
tema, trazendo a discussão para o contexto brasileiro. No terceiro capítulo, analisase
o lawfare para fins geopolíticos e empresariais, a extraterritorialidade coercitiva
universal estadunidense e como esse emaranhado de legislação internacional
impacta na soberania econômica do Brasil. No quarto capítulo defende-se que a
Operação Lava Jato foi um maxiprocesso jurídico-político-midiático utilizado
como instrumento de lawfare, interferindo no realinhamento de forças políticas no
país e abrindo caminho para implantação de um governo neoliberal extremado, com
suporte da mídia hegemônica oligopolista e da ofensiva restauradora do campo
neoliberal ortodoxo. No Anexo 1, apresenta-se parte das mensagens periciadas pela
Polícia Federal no bojo da Operação Spoofing. No anexo 2, apresenta-se a decisão
favorável ao ex-Presidente Lula, proferida pelo Comitê de Direitos Humanos da
ONU. / [en] The present dissertation investigates and analyzes the instrumentalization of
the criminal process, converted into a weapon of war - lawfare -, to enable punitive
authoritarian practices supported by casuism, within the scope of the so-called
Operation Car wash, as well as analyzing the management/use/implementation of
mechanisms of exception within the Brazilian democratic routine in order to
eliminate an enemy personified in the figure of former President Lula, aiming to
remove him from the 2018 electoral race, thus establishing the consolidation of the
coup that began in 2016, with the overthrow of President Dilma Rousseff. The paper
discusses Operation Car Wash addressing the phenomenon of the intersection
between law and politics (judicial activism, judicialization of politics and
politicization of justice), critically analyzing the performance of the Brazilian
oligopolistic hegemonic media. Thus, this research addresses this issue from the
phenomenon identified as lawfare. In the introductory chapter, the theme, problem,
hypotheses, research object, work justification, theoretical framework and research
methodology are presented. The second chapter presents some conceptual
approaches to the term lawfare, developed by several intellectuals who have
focused on the subject, bringing the discussion to the Brazilian context. In the third
chapter, we analyze lawfare for geopolitical and business purposes, the universal
coercive extraterritoriality of the United States and how this tangle of international
legislation impacts Brazil s economic sovereignty. In the fourth chapter it is argued
that Operation Car Wash was a legal-political-media maxi-process used as an
instrument of lawfare, interfering in the realignment of political forces in the
country and opening the way for the implantation of an extreme neoliberal
government, with the support of the oligopolistic hegemonic media. and the
restorative offensive of the orthodox neoliberal camp. In Annex 1, part of the
messages examined by the Federal Police in the context of Operation Spoofing is
presented. Annex 2 presents the decision in favor of former President Lula,
delivered by the UN Human Rights Committee.
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Petrobrás e o cenário de crise atual: a construção de um escândalo político midiáticoMendes, Rayssa Pereira do Nascimento 23 March 2018 (has links)
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Previous issue date: 2018-03-23 / Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPq / This research aims to investigate the relation between Petrobrás and the current political crisis in Brazil. As part of a strategic sector, the state company was the target of uncountable onslaughts in the beginning of Operation Car Wash, what has spotlighted it in front of public opinion, through certain media approaches. The theoretical framework setting this analysis is the propositions of John B. Thompson about the structuring of political scandals, having the reputation of Petrobrás as its core element under dispute. Firstly, we will describe a historical, economic and geopolitical overview of the state company, which demonstrates its importance and, accordingly, potential interests that it awakes in a global scenery whose actors guide their conflicts by the production and trade of petroleum. We will present elements that compose the context of Petrobrás, aiming to illustrate how such a political crisis was significantly viable thanks to the strategic position of the company. It has allowed the construction and legitimation of the Operation Car Wash in front of public opinion, which constitutes the national political crisis scenery of current years. The operation emerges in a very “convenient” moment: 2014, during the global crisis of petroleum. However, nor the international crisis of petroleum or any of those historical events were mentioned by the major media vehicles at that moment. Thus, the methodology of agenda setting and framing of these major media vehicles is fundamental to understand how the political crisis scenery – and the Operation Car Wash – were shaped by a discourse of crisis of Petrobrás. Finally, we will observe some actors involved in the construction of such scandal – and of the crisis, therefore – in order to understand how they articulate (currently and in the past) through the exercise of symbolic power, which is subjective by definition. Despite this subjectivity, these actors – judicial power and major media vehicles – act with a supposed neutrality and objectivity, expressively influencing the political and economic scenery. Such alliance aims to delegitimise the traditional political class, not contributing to a more consistent and effective articulation of the public debate, majorly affecting Petrobrás and Democracy itself at different levels / Esta pesquisa tem por objetivo investigar a relação entre a Petrobrás e a atual crise política no Brasil. Por se tratar de um setor estratégico, a estatal foi alvo de inúmeras ofensivas no início da Operação Lava Jato, o que contribuiu, a partir de determinadas abordagens midiáticas, para que a operação ganhasse destaque perante a opinião pública. Tal análise tem como referencial teórico as proposições de John B. Thompson no que diz respeito à estruturação dos escândalos políticos, tendo a reputação da Petrobrás como elemento central de disputa. Assim, primeiramente, procuraremos descrever um panorama do contexto histórico, econômico e geopolítico da estatal, que demonstra a sua importância e, por consequência, possíveis interesses que desperta,em um cenário global cujos atores têm seus conflitos pautados pela produção e comercialização do petróleo.Apresentaremos elementos que compõem o contexto da Petrobrás, procurando ilustrar como uma crise política de tal dimensão foi grandemente viabilizada pela posição estratégica da empresa, permitindo a construção e legitimação da Operação Lava Jato perante a opinião pública, que comporiam, ao longo dos últimos anos, um cenário de crise política nacional. Aoperação surge em um momento bastante “propício”: o ano de 2014 vivenciou uma crise do petróleo, em âmbito global. No entanto, nem a crise internacional do petróleo ou qualquer desses elementos históricos foram abordados naquele momento pelos jornais de grande circulação brasileiros. Assim, a utilização de aspectos metodológicos das teorias de agendamento e enquadramento para a análise discursiva, observando a atuação de alguns desses veículos midiáticos, é fundamental para um melhor entendimento de como o cenário de crise política – e a Operação Lava Jato – se emolduraram a partir de um discurso de crise da Petrobrás. Por fim, observaremos alguns dos atores envolvidos na construção desse escândalo – e da crise, por extensão-, procurando entender como se articularam e articulam a partir do exercício do poder simbólico, subjetivo por definição. Apesar dessa subjetividade, esses atores –Poder Judiciário e veículos de comunicação em massa - atuam com pretensa neutralidade e objetividade, influenciando grandemente o cenário político e econômico. Tal aliança visa a deslegitimação da classe política tradicional sem contribuir para que o debate público seja articulado de forma consistente e efetiva,de modo que, em diferentes escalas, seus prejuízos acabam por afetar, majoritariamente, a Petrobrás e a própria Democracia
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Análise molecular da adaptabilidade hospedeira de Cowpea aphid-borne mosaic virus e caracterização de um novo tymovírus infectando Cassia hoffmannseggiiNICOLINI, Cícero 01 September 2011 (has links)
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Previous issue date: 2011-09-01 / Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPq / Brazil is the world’s largest passion fruit producer. The sanitary problems, mainly diseases caused by viruses are among the limiting factors for increasing productivity and longevity of the plantations. In Brazil, passion fruit woodiness, caused by Cowpea aphid-borne mosaic virus (CABMV) is the major viral disease of this crop. CABMV is also causing agent of the potyvirus mosaic, a viral disease that produces serious damages in cowpea. This crop in Brazil is important mainly in the Northeastern region and represents a relevant source of protein and starch for the population. Some years ago, in the state of Pernambuco it was found a potyvirus naturally infecting “lava-pratos”, leguminous plant native to Atlantic Forest commonly found on the margins of passionflower and cowpea crops. In the city of Paudalho it was found a group of “lava-pratos” plants presenting very intense symptoms with yellow spot on the leaves. From those plants, preparations examined in a transmission electron microscope showed the presence of elongated flexuous particles and cylindrical inclusions typical of potyvirus as well as isometric particles in high concentration and vesicles on the periphery of the chloroplasts which suggested the occurrence of a tymovirus. Serological analyses and coat protein sequencing to identify the potyvirus as well as studies on host adaptation in passionflower and cowpea, using isolates from these crops were undertaken. The virus with isometric particles was chemically purified to produce polyclonal antiserum and subjected to serological studies, host range and genome sequencing for characterization. It was concluded that the potyvirus found in “lava-pratos” is CABMV and phylogenetically observed the host adaptation of this virus to the families Fabaceae and Passifloraceae. For some strains geographical distance was not the strongest factor for genetic grouping and the Brazilian isolates form a large group distinct to other countries. According to the criteria of taxonomy, using amino acid sequence of coat protein and conserved region "tymobox", it was determined the presence of a tymovirus in “lava-pratos”, for which was proposed to be a new species named Cassia yellow mosaic-associated virus (CAYMaV). / O Brasil é o maior produtor mundial de maracujá. Os problemas fitossanitários especialmente as doenças ocasionadas por vírus estão entre os fatores limitantes ao aumento de produtividade e longevidade dos plantios. A principal virose do maracujazeiro no Brasil é o endurecimento dos frutos causado por Cowpea aphid-borne mosaic virus (CABMV). O CABMV também é o agente do mosaico de potyvírus em feijão-caupi, virose que provoca sérios danos nessa cultura. No Brasil, o feijão-caupi é produzido principalmente na Região Nordeste e representa fonte importante de proteína e amido para a população. Há alguns anos atrás, um potyvírus foi encontrado em Pernambuco infectando naturalmente o lava-pratos, uma leguminosa nativa da Mata Atlântica comumente encontrada nas bordas de cultivos de maracujá e feijão-caupi. No município de Paudalho foi observado um grupo de plantas de lava-pratos apresentando sintomas muito intensos com manchas amarelas nas folhas. Dessas plantas, ao ser analisadas preparações em microscópio eletrônico de transmissão, além da presença de partículas alongadas flexuosas e de inclusões cilíndricas típicas de potyvírus foram detectadas partículas isométricas em alta concentração e vesículas nas bordas dos cloroplastos, o que sugeria ser de um tymovírus. Foram realizadas análises sorológicas e seqüenciamento da capa protéica para identificação do potyvírus, assim como estudar a adaptação hospedeira a maracujazeiro e feijão-caupi, utilizando-se isolados obtidos dessas culturas. O vírus com partículas isométricas foi purificado quimicamente para produção de antissoro policlonal e submetido a estudos sorológicos, gama de hospedeiros e seqüenciamento de parte do genoma para caracterização. Concluiu-se que o potyvírus encontrado em lava-pratos é o CABMV e filogeneticamente se observou que ocorre adaptação hospedeira deste vírus em plantas das famílias Fabaceae e Passifloraceae. Para alguns isolados, a distância geográfica não foi o fator mais forte para agrupamento genético e os isolados brasileiros formam um grande grupo distinto aos de outros países. De acordo com os critérios de taxonomia, usando-se seqüência de aminoácidos da capa protéica e região conservada “tymobox”, foi determinada a presença em lava-pratos de um tymovírus, para o qual foi proposto ser uma nova espécie nomeada Cassia yellow mosaic-associated virus (CAYMaV).
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Compositional and mineralogical relationships between mafic inclusions and host lavas as key to andesite petrogenesis at Mount Hood Volcano, OregonWoods, Melinda Michelle 01 January 2004 (has links)
Throughout its eruptive history, Mount Hood has produced compositionally similar calc-alkaline andesite as lava flows and domes near the summit and basaltic andesitic flows from flank vents. Found within the andesite are slightly more mafic inclusions that are compositionally similar to the host andesite (or host lavas); no inclusions were found in the flank lavas. Host lavas and inclusions have the following mineral assemblage: plag + opx ± cpx ± amp + oxides. Flank lava mineralogy is similar to the inclusions and host lavas, but since they are more mafic they contain olivine instead of amphibole. Average silica content among samples analyzed ranges from 57.6 to 62.7 weight percent; however the incompatible trace element composition is more variable at lower silica contents and becomes less variable at higher silica contents. In terms of incompatible trace element composition, the host lavas and inclusions are either depleted (no amp) or enriched (amp± cpx).
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Geochemistry of the Boring Lava along the West Side of the Tualatin Mountains and of Sediments from Drill Holes in the Portland and Tualatin Basins, Portland, OregonBarnes, Michelle Lynn 06 October 1995 (has links)
Instrumental Neutron Activation Analysis (INAA) was used to identify geochemical groups in Boring Lava along the west side of the Tualatin Mountains, and in sediments of the Portland and Tualatin basins. Samples of Boring Lava were obtained from TriMet drill core collected during planning of the tunnel alignment for the Westside Light Rail line. Additional samples of Boring Lava were collected from outcrops along the west side of the Tualatin Mountains. Samples of sediment from the Tualatin and Portland basins were obtained from drill core collected during an Oregon Department of Geology and Mineral Industries (DOGAMI) Earthquake Hazards Mapping project. INAA of Boring Lava samples resulted in the identification of three geochemical groups. Additional data sets, including x-ray fluorescence geochemistry, magnetic polarity, and age dates, allowed for the distinction of three Boring Lava units. The Boring Lava of Barnes Road is a young, normal unit, the Boring Lava of Sylvan Hill is an older normal unit, and the Boring Lava of Cornell Mountain is the oldest, reversed unit. The surf ace distribution, identified using topography and outcrop geochemistry, is consistent with the subsurface distribution, identified using boring logs and core geochemistry. Volcanic vent locations are proposed at topographic highs within the identified surface distribution of the Boring Lava of Barnes Road. INAA of sediment samples resulted in the identification of seven groups: (1) Columbia River source sediments, (2) lower Troutdale Formation, (3) Reed Island ashes, (4) young Columbia River sediments, (5) highalumina basalt sediments, (6) episodic Cascadian volcanic sediments, and (7) Columbia River Basalt Group (CRBG) sediments. Only the CRBG sediments group was identified in the Tualatin basin, while all seven groups were identified in the Portland basin. This appears to demonstrate that the sediment packages in the two basins are different. Finally, each sediment group can be placed into one of three broad geochemical categories: Columbia River source sediments and lower Troutdale Formation represent a Columbia River or continental source; Reed Island ashes, young Columbia River sediments, high-alumina basalt sediments, and episodic Cascadian volcanic sediments represent a Cascadian or local source; and CRBG sediments represent residual soils or sediments overlying Columbia River basalt flows.
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Rhyolitic magmatism of the High Lava Plains and adjacent Northwest Basin and Range, Oregon : implications for the evolution of continental crustFord, Mark T., 1973- 14 December 2011 (has links)
Understanding continental crust formation and modification is a fundamental and longstanding geologic problem. Influx of mantle-derived basaltic magma and partial melting of the crust are two ways to drive crustal differentiation. This process results in a low density upper crust and denser, more refractory lower crust, creating significant and vastly different geochemical reservoirs over time. The High Lava Plains (HLP) and Northwestern Basin and Range (NWBR) in central and eastern Oregon provide an excellent example of intraplate volcanism where we can examine the beginnings of segregation of a relatively young, recently accreted crust.
The origins of continental magmatism and its relationship to plate tectonics, especially away from the continental margins, are only slowly becoming revealed. The western United States is the most volcanically active part of North America during Cenozoic time, and this activity includes the enigmatic volcanism of the HLP and NWBR. Rhyolitic volcanism in the HLP and NWBR is age-progressive but in a direction that is nearly perpendicular to North American Plate motion. Despite being erupted through a similar crust and with a similar composition of mafic input, the HLP province
is strongly bimodal (basalt-rhyolite) while the NWBR province exhibits a continuum of compositions. High silica rhyolites are commonplace in the HLP, with approximately a 1:1 ratio of rhyolite to basalt, even though the crust is comprised of mafic accreted terranes.
Asthenospheric flow, mantle melting and crustal extension coupled with southwesterly North American plate motion explain the age-progressive volcanism of the HLP and NWBR. Differential asthenopheric counterflow and mantle upwelling created by the down-going Cascadia slab, coupled with transtensional stresses related to the rotation of the North American plate and Basin and Range extension, decreasing to the north, can produce the observed variations in rhyolite compositions and volumes in the two adjacent provinces. These differences are caused by fundamentally different petrogenetic processes that take place in the crust.
In the HLP, an increase in mantle-derived magma flux into the lower crust has created low silica rhyolite via partial melt that separated, coalesced and rose buoyantly. This low silica rhyolite may erupt, solidify in the upper crust, or differentiate by fractional crystallization to produce high-iron, high-silica rhyolite containing an anhydrous phase assemblage. In the NWBR, a smaller flux of basaltic magma, coupled with greater transtension resulted in small crustal processing zones where fractional crystallization coupled with magma mixing and recharge created a wide range of compositions. Partial melting to form rhyolites was limited. These rhyolites have lower iron, and hydrous phases (biotite, amphibole) are common. These processes modify the crust in different ways, leaving a stratified crust in the HLP but a less modified crust in the NWBR. Recent geophysical and isotopic studies bear out these differences and allow for a unified, internally consistent model for both provinces, one that relies only on partial melt generation driven by current plate movements and do not require a mantle plume contribution.
The bimodal volcanism of the HLP is a direct consequence of the processes that cause the gravitational differentiation of the continental crust into upper and lower units. The model for the HLP is generally applicable to other localities that have predominantly mafic crust and a similar balance of crustal transtension and mantle-derived basaltic flux.
One such place is Iceland, which has strongly bimodal (basalt – rhyolite) volcanism. In areas where silicic crust has become substantially more mafic due to a high flux of intraplated basalts, such as in the bimodal Snake River Plain, the model is also applicable. / Graduation date: 2012 / In order for the .age files to run, the add-in called ArArCalc for Excel (version 200 or 2003) must be installed. ArArCalc is available from the website Earthref.org
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A trace element study of plagioclase and clinopyroxene phenocrysts in historical lavas from Mt. Etna, Sicily, by laser ablation ICP-MSRusso, Christopher J. 20 July 2001 (has links)
Graduation date: 2002
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Genesis and geochronology of alkaline volcanism in the Pinacate Volcanic Field Northwestern Sonora, MexicoLynch, Daniel James, 1940- January 1981 (has links)
No description available.
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Eruptive Processes of Mafic Arc Volcanoes – Subaerial and Submarine PerspectivesDeardorff, Nicholas D., 1980- 09 1900 (has links)
xviii, 179 p. : ill. (some col.). Includes 3 video files. / Mafic arc volcanoes have eruption styles that range from explosive to effusive. In a broad sense, eruption style is controlled by the rate of magma supply to the vent. In this dissertation I examine relationships between eruption rate and style in two separate studies: (1) an investigation of ongoing activity at NW Rota-1, a submarine volcano in the Mariana arc, and (2) a morphologic study of the Collier Cone lava flow field in the Central Oregon Cascades.
The eruptions of NW Rota-1 range from effusive to moderately explosive; eruptions are effusive when mass eruption rate (MER) is low and explosive when MER increases. The explosivity of submarine eruptions is suppressed by seawater because of increased hydrostatic pressure, rapid cooling, and the high viscosity of water relative to air (which limits expansion). The combination of seawater and relatively low MERs limit pyroclast deposition to within meters to tens of meters of the vent. In fact, many pyroclasts fall back into the vent and are recycled. Evidence for recycling includes microcrystalline inclusions within erupted pyroclasts and elevated Cl and Na concentrations in matrix glass. Enrichment of Cl and Na suggests that seawater assimilation provides a geochemical signature of recycling. Recycling is limited to low MER explosive eruptions and is not observed in either effusive lava or deposits from high MER explosions.
Direct observations of eruptions allow measurements of eruption rate. However, it is more challenging to estimate MERs of eruptions that were not observed. To address this problem, I develop and test methods of constraining the eruption rate (and duration) of the c. 1600 year old Collier Cone lava flow using the flow morphology. To quantify flow morphology I combine field observations with GIS analysis of Lidar-derived digital topography. Channel dimensions constrain emplacement rates; dominant wavelengths and amplitudes of surface folds constrain spatial and temporal changes in flow rheology.
Three videos of eruption activity accompany this dissertation as supplemental files.
This dissertation includes both previously published and unpublished co-authored material. / Committee in charge: Dr. Katharine V. Cashman, Chair;
Dr. Joshua J. Roering, Member;
Dr. Paul J. Wallace, Member;
Dr. Patricia F. McDowell, Outside Member;
Dr. William W. Chadwick, Outside Member
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Tratamento biológico de efluentes de lava-jatoCosta, Maria José Comandante 21 February 2006 (has links)
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Previous issue date: 2006-02-21 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / The research was realized in four phases. In the 1st phase, interviews were accomplished with proprietors of car-washes with the objective of knowing your environmental and social impacts. In the 2nd phase synthetic effluents of car-washes were treated during 147 days in batch anaerobic reactors with five different oil and detergent concentrations. In the 3rd phase six reactors were monitored in batch form, during 20 days, with substrate containing high oil concentrations (0,5 to 2,5 g.l-1) and surfactants concentrations (5,0g.L-1). These treatments were realized with purpose to verified the relation between oil concentration and inhibition of the biologic activity. In the 4th phase six batch anaerobic reactors, with different proportions of the surfactant, were monitored during 35 days. The concentrations of organic matter influent and effluent were analyzed in all the treatments and in the sludge were determined solid concentration. Daily the biogas produced was measures and characterized. In the 2nd phase the average removal of soluble COD was about 82%, for a monitoring period of 18 days. For raw COD during 100 days of operation the average removal was approximately 76% and the production of methane was directly proportional the substrate concentrations. It was verified that the anaerobic biological activity occurs in surfactant concentration below 0,5 g.L-1, and starting from that concentration it begins to happen inhibition of the process / O presente trabalho foi desenvolvido em quatro fases. A primeira fase teve o objetivo de levantar dados sobre os impactos ambientais e sociais causados pelos lava-jatos. Para tanto, foram realizadas entrevistas com seus proprietários. Na segunda fase, foram tratados anaerobiamente, durante 147 dias, em reatores de batelada, efluentes sintéticos de lava-jatos com cinco diferentes concentrações de óleo e detergente. Na terceira fase, foram monitorados seis reatores anaeróbios, em regime de batelada, durante 20 dias, com substratos contendo altas concentrações de óleo (0,5 a 2,5 g.L-1) e surfactantes (5,0 g.L-1). Estes tratamentos tiveram por finalidade verificar se, com o aumento da concentração de óleo, haveria inibição da atividade biológica. Na quarta fase, foram realizados, anaerobiamente, em reatores de batelada, durante 35 dias, seis experimentos com diferentes concentrações de surfactante para verificar que concentração inibiria o processo biológico anaeróbio. Para todos os tratamentos foram analisadas as concentrações de matéria orgânica (DQO) afluente e efluente, bem como as concentrações de sólidos do lodo. Diariamente, foram realizadas leituras do volume e da composição do biogás. Como resultados da segunda fase, verificaram-se remoções de DQO solúvel média de 82% aos 18 dias e para DQO bruta em torno de 76% para os cinco tratamentos, durante 100 dias de operação. A produção de metano foi diretamente proporcional às concentrações dos substratos. Constatou-se que a atividade biológica anaeróbia ocorre numa concentração de surfactante de até aproximadamente 0,5 g.L-1, sendo que a partir daí, começa a ocorrer inibição do processo
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