O controle social na construção e democratização da política de Assistência Social: o papel dos conselhos e a realidade de um município da Baixada Fluminense

A presente dissertação tem como propósito, a partir do processo de construção e democratização da Política de Assistência Social no Brasil, pós SUAS, analisar o controle social tendo como objeto o Conselho Municipal de Assistência Social do município de Mesquita, na região da Baixada Fluminense / RJ e as condições de trabalho dos Assistentes Sociais nesses espaços. Inicialmente, abordamos a Política de Assistência Social no Brasil, desde a criação da extinta Legião Brasileira de Assistência Social (LBA), até os dias atuais, ressaltando os avanços na parte jurídico-legal-normativa desta política, o que tem se tornado um campo propício e amplo para o mercado de trabalho dos assistentes sociais na contemporaneidade. No debate do controle social na Política de Assistência, destacamos três importantes temáticas: a relação das entidades da sociedade civil com os conselheiros governamentais, nos espaços de representação política, democrática, deliberativa e paritária nos conselhos de assistência social; a participação dos segmentos de usuários dos serviços sócio assistenciais do município de Mesquita e, ainda, as condições em que vem ocorrendo à participação dos assistentes sociais nos espaços de controle social no município, através de relações de trabalho precárias, no que se refere à desregulamentação de direitos sociais trabalhistas dos profissionais. Para o estudo, analisamos as Atas do período de 2011-2012, e realizamos entrevistas semi-estruturadas com os conselheiros governamentais e não governamentais do Conselho Municipal de Assistência Social de Mesquita (CMAS), que atuaram no mesmo período, gestão empossada em Dezembro de 2011, após resultado do processo eleitoral das entidades da sociedade civil do CMAS. Dentre os achados da investigação, a partir do material empírico, mediado pelo pensamento de autores que discutem esta temática e pela legislação destacam-se: a superioridade da Representação Governamental sobre a Representação da Sociedade Civil no CMAS; não monitoramento e fiscalização do saldo orçamentário pelo CMAS / Mesquita; precarização das relações de trabalho na SEMAS / Mesquita; descontinuidade do Programa de Capacitação dos Conselheiros do CMAS / Mesquita; despreparo técnico dos conselheiros para apreciação de prestação de contas no CMAS, com ausência de tempo hábil para análise; manipulação política por parte da representação governamental no CMAS; o poder de influência do governo é maior do que da sociedade civil; necessidade de capacitação técnica, e principalmente capacitação ética e política dos conselheiros governamentais e da sociedade civil; precariedade dos equipamentos públicos dos SEMAS / Mesquita; parca participação dos Usuários dos Serviços Socioassistenciais na esfera do conselho, dentre outros aspectos que serão tratados nesta dissertação. Em suma, estes são as principais conclusões de forma resumida e sintética que abordaremos mais detalhadamente nas considerações finais deste trabalho.

An Overview of Guam's Inshore Fisheries

Guam's nearshore reef fishery is a multi-gear, multispecies fishery that has undergone major changes through the years. Methods have evolved and become more modern. This, along with the changing economic status of Guam, has severely stressed the fishery. Top targeted species are being overexploited and "growth overharvesting" is occurring; the more serious form of "recruitment overharvesting," is happening to some of the key species. Major management concerns are discussed with respect to overfishing and habitat destruction. Management recommendations for this fishery include gear restrictions, size restrictions, and the establishment of marine conservation areas.

Se você não quer, faça matrícula no pagou-passou da esquina. Concepções de currículo e avaliação: Diálogos sobre um colégio de excelência

O estudo interroga sobres as articulações entre os sentidos de currículo, avaliação e qualidade que circulam entre os professores no contexto do Colégio de Aplicação da Uerj (CAp/UERJ) e que sustentam a legitimidade da instituição considerada de excelência pelos resultados alcançados pelos seus alunos e tem como objetivo identificar as concepções de conhecimento, de currículo e de avaliação que articulam a produção de sentidos de um ensino de qualidade entre os professores do CAp/UERJ? Dessa forma, utilizando aportes pósestruturais a pesquisa é realizada a partir da apropriação dos conceitos de discurso e hegemonia desenvolvido por Ernesto Laclau na Teoria do discurso para problematizar os processos de exclusão que resultam na significação de qualidade sustentada por padrões de desempenho a priori. Para concretizar o estudo, caracterizado como um Estudo de Caso, foram realizadas entrevistas com oito professores abrangendo todos os segmentos de ensino da instituição. Além dos depoimentos, forma consultados documentos institucionais que permitiram contextualizar e compreender melhor o funcionamento do CAp/UERJ. A Análise de Conteúdo foi a ferramenta utilizada na sistematização, leitura e interpretação do material empírico. É importante destacar que não houve na investigação qualquer pretensão de estabelecer juízos de valor sobre as tensões existentes na instituição acerca das concepções que nela circulam e que as falas dos sujeitos são tomadas como interpretações provisórias que cada entrevistado confere as suas experiências no contexto em que a entrevista acontece. Experiências que, por sua vez, também são reinterpretadas pela pesquisadora. Com o estudo foi possível concluir que a significação do CAp/UERJ como uma escola de excelência é um processo dinâmico em que os professores, juntamente com outros sujeitos sociais, nem sempre diretamente ligados à instituição, lutam por hegemonia em práticas coletivas de produção curricular em meio a conflitos que ultrapassam as fronteiras da escola. Essas práticas predominantemente críticas, são centradas na defesa de um repertório de bens simbólicos que podem até ser transmitidos de formas diferentes, com diversas atividades que contemplem a diversidade da escola, mas é na avaliação que elas realmente se concretizam como críticas ao exigir compreensões semelhantes de sujeitos diferentes, principalmente no anos finais de escolaridade. No entanto, ainda que possam ser consideradas hegemônicas e pareçam persistir há algum tempo, como apontam as análises realizadas, trata-se de uma hegemonia precária que se produz em meio a tensões e conflitos nas práticas curriculares da instituição. Assim a proposta da investigação consiste em desestabilizar hegemonias mais estáveis e seus interesses particulares, autorizando que outras hegemonias brotem, promovendo o antagonismo através dos múltiplos discursos.

Tendências Espaciais e Temporais da Epidemia da AIDS em maiores de 50 Anos no Município de Niterói - RJ

A síndrome de imunodeficiência adquirida (AIDS) é um problema de saúde pública que alcançou grandes proporções. Na ausência de uma vacina eficaz ou tratamento efetivo para a doença, esforços têm ser concentrados na prevenção. As políticas de saúde adotadas pelo governo brasileiro têm resultado em estabilização da enfermidade no país na faixa etária mais jovem, muito embora essa tendência não venha acontecendo nos outros grupos etários mais velhos. Verificar a incidência da AIDS em indivíduos idosos, no município de Niterói, RJ, de acordo com sexo, idade, período e coorte de nascimento de 1982-2011, além de analisar a dinâmica espacial da epidemia de AIDS em idosos (indivíduos com 60 anos ou mais) no estado do Rio de Janeiro no período de 1997-2011, são os objetivos deste estudo. Os dados da população por idade, sexo e grupo, foram obtidos a partir de: censos populacionais, contagem da população (1996), projeções intercensitárias, informações do Sistema de Informações de Agravos de Notificação, de Mortalidade e de Controle de Exames Laboratoriais. As taxas de incidência por 100 000 foram calculadas para as unidades geográficas através da contagem do número de novos casos de AIDS em indivíduos com 60 anos ou mais e tamanho da população do município no mesmo grupo etário. Para avaliar a dependência espacial das taxas foi calculado o índice de Moran global. Moran Mapas foram construídos para mostrar regimes de correlação espacial potencialmente distintos em diferentes subregiões. Distribuições de probabilidade e método Bayes empírico foram aplicados para a correção das taxas de incidência da AIDS. Ocorreram 575 casos de AIDS em residentes de Niterói com ≥50 anos de idade. Tendência crescente de taxas de incidência ao longo do tempo foi detectada em ambos os sexos. No estudo da dinâmica espacial da incidência da AIDS em idosos, Rio de Janeiro, no período de 1997 a 2011, as taxas entre homens e mulheres permaneceram flutuantes ao longo de todo o período. Não foi possível detectar correlação significativa global, usando o índice global de Moran. Na costa sudeste do Estado, onde se localizam as grandes áreas metropolitanas (Rio de Janeiro e Niterói), observaram-se grupos de cidades com taxas de até 20 casos por 100 000 hab. Esta concentração se torna mais pronunciada em períodos subsequentes, quando parece ocorrer propagação gradual da epidemia da costa sul até o norte do Rio de Janeiro.

Acontecimento-Escola: entrecruzamentos do fotográfico, artístico e pedagógico

Somente poderiam advir novas formas de existência, outros modos de ser e estar no mundo, se diferentes sensibilidades também acompanhassem o desdobrar de um determinado acontecimento. Esta pesquisa tem como objeto privilegiado os acontecimentos de criação da escola na sua relação com as visibilidades de mundo, fazendo-se ela mesma em preparação e ressurgência de um acontecimento de criação. Inicialmente seria fundamental à pesquisa envolver-se nos cotidianos do colégio estudado para melhor pensar a via de preparação do acontecimento. Tal feita somente poderia adquirir sentido se o dispositivo investigativo mantivesse seus investimentos ao nível do contato com estudantes, esforçando-se por garantir a maior participação deles em diferentes aspectos da preparação, acentuando a partir de nossos encontros à potência de criação evenemencial. Ceder aos indícios durante a preparação significaria aprofundar os vínculos que mantive com a comunidade escolar. E, tendo como principal convite a fotografia, os estudantes realizaram um número significativo de imagens do colégio que, ao final de um extenso período, nos conduziu à ocupação imagética do espaço escolar. Num segundo momento a pesquisa se voltou para o modo de apreensão do acontecimento por parte de toda a comunidade em meio à ocupação do espaço escolar a partir de suas imagens. Composta por oitenta e uma fotografias do espaço escolar, a ocupação concentrou parte destas imagens em uma instalação confeccionada por fios vermelhos no centro do primeiro pavimento, distribuindo o restante delas por entre paredes, banheiros e corredores. Esta apreensão se fez compreendida pelo dispositivo sob os termos de um profundo engajamento com o campo problemático do acontecimento, tendo como índice o destino investido pelas imagens, prolongando senão os efeitos evenemenciais em franca atualização dos gestos, superfícies e visibilidades. Procurei pensar a multiplicidade de relações estabelecidas entre a comunidade escolar e as imagens fotográficas em meio à ocupação imagética realizada no colégio, tomando a sua aparição momentânea como acontecimento de criação, assim como a ressurgência de outras visibilidades presididas em seus contextos. Para tanto, pesquisa precisou se tornar esta íntima criação de uma obra de aprendizagem.

Redundancy quantification in the safety assessment of existing concrete beam-and-slab bridges

In current practice the strength evaluation of a bridge system is typically based on firstly using elastic analysis to determine the distribution of load effects in the elements and then checking the ultimate section capacity of those elements. Ductility of the components in most bridge structures permits local yield and subsequent redistribution of the applied loads from the most heavily loaded elements. As a result a bridge can continue to carry additional loading even after one member has yielded, which has conventionally been adopted as the "failure criterion" in bridge strength evaluation. This means that a bridge with inherent redundancy has additional reserves of strength such that the failure of one element does not result in the failure of the complete system. For these bridges warning signs will show up and measures can be undertaken before the ultimate collapse is happening. This paper proposes a rational methodology for calculating the ultimate system strength and including in bridge evaluation the warning level due to redundancy. © 2004 Taylor & Francis Group, London.

Climate resilience of schools: a case study

Social and political concerns are frequently reflected in the design of school buildings, often in turn leading to the development of technical innovations. One example is a recurrent concern about the physical health of the nation, which has at several points over the last century prompted new design approaches to natural light and ventilation. The most critical concern of the current era is the global, rather than the indoor, environment. The resultant political focus on mitigating climate change has resulted in new regulations, and in turn considerable technical changes in building design and construction. The vanguard of this movement has again been in school buildings, set the highest targets for reducing operational carbon by the previous Government. The current austerity measures have moved the focus to the refurbishment and retrofit of existing buildings, in order to bring them up to the exacting new standards. Meanwhile there is little doubt that climate change is happening already, and that the impacts will be considerable. Climate scientists have increasing confidence in their predictions for the future; if today’s buildings are to be resilient to these changes, building designers will need to understand and design for the predicted climates in order to continue to provide comfortable and healthy spaces through the lifetimes of the buildings. This paper describes the decision processes, and the planned design measures, for adapting an existing school for future climates. The project is at St Faith’s School in Cambridge, and focuses on three separate buildings: a large Victorian block built as a substantial domestic dwelling in 1885, a smaller single storey 1970s block with a new extension, and an as-yet unbuilt single storey block designed to passivhaus principles and using environmentally friendly materials. The implications of climate change have been considered for the three particular issues of comfort, construction, and water, as set out in the report on Design for Future Climate: opportunities for adaptation in the built environment (Gething, 2010). The adaptation designs aim to ensure each of the three very different buildings remains fit for purpose throughout the 21st century, continuing to provide a healthy environment for the children. A forth issue, the reduction of carbon and the mitigation of other negative environmental impacts of the construction work, is also a fundamental aim for the school and the project team. Detailed modelling of both the operational and embodied energy and carbon of the design options is therefore being carried out, in order that the whole life carbon costs of the adaptation design options may be minimised. The project has been funded by the Technology Strategy Board as part of the Design for Future Climates programme; the interdisciplinary team includes the designers working on the current school building projects and the school bursar, supported by researchers from the University of Cambridge Centre for Sustainable Development. It is hoped that lessons from the design process, as well as the solutions themselves, will be transferable to other buildings in similar climatic regions.

中国环境问题与持续发展

人口、资源、环境和灾害问题已刻不容缓地提到人类发展的日程上来,它不仅是自然科学的问题,同时也是社会问题.在国际环境保护的浪潮日益高涨、国内生态环境保护工作日益发展、社会主义市场经济逐渐发育完善的新形势下,我国正在采取一系列措施,保护生态环境,提高全社会的环保意识,大力开展生态建设,控制环境污染,实现经济建设与环境保护的相互配合和协调发展.笔者在上述背景下,分析了国内外人口增长过快、资源逐减少、环境日趋恶化、灾害发生频繁等严重危害社会发展之恶果,讨论了中国政府自1992年巴西“环发”大会之后所采取的一系列行动.

中国土壤侵蚀影响因素及其危害分析

该文从降雨、地貌、植被、土壤及人为因素等方面对中国土壤侵蚀的影响因素进行了系统分析 ,研究了土壤侵蚀使中国土地资源破坏、粮食减产、灾害发生、土壤肥力下降、水资源环境污染、库塘湖泊淤积、城市安全受到威胁等一系列危害 ,可供水土保持及环境整治决策作参考

Non-goal scene analysis for soccer video

The broadcast soccer video is usually recorded by one main camera, which is constantly gazing somewhere of playfield where a highlight event is happening. So the camera parameters and their variety have close relationship with semantic information of soccer video, and much interest has been caught in camera calibration for soccer video. The previous calibration methods either deal with goal scene, or have strict calibration conditions and high complexity. So, it does not properly handle the non-goal scene such as midfield or center-forward scene. In this paper, based on a new soccer field model, a field symbol extraction algorithm is proposed to extract the calibration information. Then a two-stage calibration approach is developed which can calibrate camera not only for goal scene but also for non-goal scene. The preliminary experimental results demonstrate its robustness and accuracy. (c) 2010 Elsevier B.V. All rights reserved.

地震P-S波时差耦合作用的斜坡崩滑效应研究

China locates between the circum-Pacific and the Mediterranean-Himalayan seismic belt. The seismic activities in our country are very frequent and so are the collapses and slides of slope triggered by earthquakes. Many collapses and slides of slope take place mainly in the west of China with many earthquakes and mountains, especially in Sichuan and Yunnan Provinces. When a strong earthquake happening, the damage especially in mountains area caused by geological hazards it triggered such as rock collapses, landslides and debris flows is heavier than that it caused directly. A conclusion which the number of lives lost caused by geological hazards triggered by a strong earthquake in mountains area often accounts for a half even more of the total one induced by the strong earthquake can be made by consulting the statistical loss of several representative earthquakes. As a result, geological hazards such as collapses and slides of slope triggered by strong earthquakes attract wide attention for their great costs. Based on field geological investigation, engineering geological exploration and material data analysis, chief conclusions have been drawn after systematic research on formation mechanism, key inducing factors, dynamic characteristics of geological hazards such as collapses and slides of slope triggered by strong earthquakes by means of engineering geomechanics comprehensive analysis, finite difference numerical simulation test, in-lab dynamic triaxial shear test of rock, discrete element numerical simulation. Based on research on a great number of collapses and landslides triggered by Wenchuan and Xiaonanhai Earthquake, two-set methods, i.e. the method for original topography recovering based on factors such as lithology and elevation comparing and the method for reconstructing collapsing and sliding process of slope based on characteristics of seism tectonic zone, structural fissure, diameter spatial distribution of slope debris mass, propagation direction and mechanical property of seismic wave, have been gotten. What is more, types, formation mechanism and dynamic characteristics of collapses and slides of slope induced by strong earthquakes are discussed comprehensively. Firstly, collapsed and slided accumulative mass is in a state of heavily even more broken. Secondly, dynamic process of slope collapsing and sliding consists of almost four stages, i.e. broken, thrown, crushed and river blocked. Thirdly, classified according to failure forms, there are usually four types which are made up of collapsing, land sliding, land sliding-debris flowing and vibrating liquefaction. Finally, as for key inducing factors in slope collapsing and sliding, they often include characteristics of seism tectonic belts, structure and construction of rock mass, terrain and physiognomy, weathering degree of rock mass and mechanical functions of seismic waves. Based on microscopic study on initial fracturing of slope caused by seismic effect, combined with two change trends which include ratio of vertical vs. horizontal peak ground acceleration corresponding to epicentral distance and enlarging effect of peak ground acceleration along slope, key inducing factor of initial slope fracturing in various area with different epicentral distance is obtained. In near-field area, i.e. epicentral distance being less than 30 km, tensile strength of rock mass is a key intrinsic factor inducing initial fracturing of slope undergoing seismic effect whereas shear strength of rock mass is the one when epicentral distance is more than 30 km. In the latter circumstance, research by means of finite difference numerical simulation test and in-lab dynamic triaxial shear test of rock shows that initial fracture begins always in the place of slope shoulder. The fact that fracture strain and shear strength which are proportional to buried depth of rock mass in the place of slope shoulder are less than other place and peak ground acceleration is enlarged in the place causes prior failure at slope shoulder. Key extrinsic factors inducing dynamic fracture of slope at different distances to epicenter have been obtained through discrete element numerical simulation on the total process of collapsing and sliding of slope triggered by Wenchuan Earthquake. Research shows that combined action of P and S seismic waves is the key factor inducing collapsing and sliding of slope at a distance less than 64 km to initial epicenter along earthquake-triggering structure. What is more, vertical tensile action of P seismic wave plays a leading role near epicenter, whereas vertical shear action of S seismic wave plays a leading role gradually with epicentral distance increasing in this range. On the other hand, single action of P seismic wave becomes the key factor inducing collapsing and sliding of slope at a distance between 64 km and 216 km to initial epicenter. Horizontal tensile action of P seismic wave becomes the key factor gradually from combined action between vertical and horizontal tensile action of P seismic wave with epicentral distance increasing in this distance range. In addition, initial failure triggered by strong earthquakes begins almost in the place of slope shoulder. However, initial failure beginning from toe of slope relates probably with gradient and rock occurrence. Finally, starting time of initial failure in slope increases usually with epicentral distance. It is perhaps that the starting time increasing is a result of attenuating of seismic wave from epicenter along earthquake-triggering structure. It is of great theoretical and practical significance for us to construct towns and infrastructure in fragile geological environment along seism tectonic belts and conduct risk management on earthquake-triggered geological hazards by referring to above conclusions.

滑坡型泥石流转化机理研究—以四川省达县青宁乡滑坡为例

Slide-debris flow is debris flow which is transformed from landslide consecutively in a short time, it comprises of two phases: First, Landslide starts to slide; Second, landslide changes to debris flow. Slide-debris flow which brings great property and life loss happens frequently at home and abroad. In order to forecast the happening possibility and scope of slide-debris flow, transfromation mechanism of Slide-debris flow must be studied. Research on transformation mechanism of slide-debris flow is intersectant science of landslide kinetics and debris flow starting theory, It is a fringe problem as well as front problem of geological hazard. This paper takes Qingning slide-debris flow in Da County, Sichuan Province for example and has studied the mechanism of its instability and transfromation into debris flow through indoor test (including usual soil test and ring shear test) and digital modeling method.The research gets the following conclusions. Qingning Landslide took place mainly because of confined water head arising from rainfall infiltration. Before Landslide occurring, it rained continuously for 22 days, accumulated precipitation arrived at 521.6mm.Investigation shows that strata of Qingning Landslide contains quaternary loose accumulation, slip soil and highly weathered bedrock, which is a good condition for formation of confined water in the slope. Further more, groundwater seepage in the slope body and corresponding slope safety factor before landslide occurring have been computed through finite element method. The result shows that because of infiltration of rainfall, confined water head in the slope arose sharply, accordingly, the safety factor of the slope declined quickly. The result also shows that force put on the slide body by the rock mass detached from Dazhaiyan mountain was the direct factor for landslide occurring. Qingning slide-debris transformation mode has been summarized, the process the landslide changed into debris flow is divided into three phases in the prospective of macroscopic geological condition: landslide occurring, transformation and debris flow. Landslide occurring phase is from slope’ local creeping slide to Landslide occurring; transformation phase contains slide body sliding on the slide bed after slide occurring and sliding on the slope after shearing opening; debris flow phase is that slide body breaks up completely and flows downward into the ditches. The transformation mechanism of Qingning slide-debris flow has been studied through indoor ring shear test of slip soil. The result shows that transformation mechanism contains two points: first, during slide body sliding on the slide bed and slope after shearing opening, shearing shrinkage, grain crushing and grain layering brought about declining of its volume and produced excess pore water pressure, and because producing velocity of excess pore water pressure is much greater than its dissipating velocity, shear strength of slide body decreased sharply because of accumulated pore water pressure. Second, grains crushing and grains layering during slide body sliding brought about thick liquefied layer at the bottom of the slidebody, liquefied layer contained high water content and its shear strength was very low, its thickness increased as the sliding displacement increasing. Liquefied layer makes slide body sliding fast and easily break down to debris flow. Excess pore water pressure and liquefied layer made shear strength of slidebody became very low, furthermore, water in the pit of slope joining in the slidebody was also a facter that made slidebody accelerate the transformation. Influence of slide body thickness and fine grains content to transformation of slide-debris flow has been studied through ring shear test. The result reaches two conclusions. First, thickness of slide body affects transformation of slide-debris flow by two ways, porewater pressure and effect of “soft base” increases as thickness of slide body increasing.so the thicker slide body is ,the easier transformation is. Second, actual dissipating velocity of porewater pressure should be considered when studying the influence of fine grains content to tranformation of slide-debris flow. There should be a critical content of fine grains which makes the difference of producing and dissipating velocity of water pore pressre greatest, this value is the best for slide-debris transformation. The whole process of slide-debris flow transformation is reproduced through discrete element method. Transformation mechanism of slide-debris flow is studied through monitoring various parameters including pore water pressure, grain crushing and grain layering in the slide body during the transformation. The result confirms and supplements the transformation mechanism of slide-debris flow got from ring shear test well.

油气运聚动力学的模拟分析——以准噶尔盆地为例

The petroleum migration, happening in the geologic past, is the very important and complex dynamic processes in the petroleum systems. It plays a linking role among all static factors in a system. The accumulation is in fact the result of the petroleum migration. For the petroleum geology, the dynamics research of the petroleum migration refers to the mechanism and process research, as well as the use of the quantitative methods. In this thesis, combining with the qualitative analysis and quantitative modeling, the author manages to discuss theoretically some key problems dealing with migration processes, which have not been solved yet, and to apply the studied results in petroleum system analysis in actual basins. The basin analysis offers the base of the numerical modeling for geological phenomena occurring in sedimentary basins, that consists of the sedimentary facies analysis, the section reconstructing technique, eroded thickness estimating, etc. The methods to construct the geologic model, which is needed in the research of oil and gas migration and accumulation, are discussed. The basin analysis offers also the possibility for the latter modeling works to get and select the parameters, such as stratum's thickness, age, stratigraphy etc. Modeling works were done by using two basin modeling softwares: Basin_Mod and TPC_Mod. The role of compaction during the secondary migration and the heterogeneity of migrating paths within the clastic carrier are modeled. And the conclusions were applied in the migration studies in the Jungaer Basin, lying on the Northwest part of the China. To construct a reliable migration model, the author studied the characteristics of the sedimentation, the pore fluid pressure evolution, as well as the distribution and the evolution of fluid potential, following the tectonic evolution of the Jungaer Basin. The geochemical prospecting results were used to evidence and to calibrate the migration processes: the oil-source correlation, the distribution of the properties of oil, gas and water. Finally, two important petroleum systems, Permian one and Jurassic one were studied and identified, according, principally, to the studies on the petroleum migration within the Jungaer Basin. Since the oil, as well as the gas, moves mainly in separate phase during the secondary migration, their migrating behaviors would be determined by the dynamics conditions of migration, including the driving forces and pathways. Based on such a consideration, the further understandings may be acquired: the roles played by permeable carriers and low-permeable source rock would be very different in compaction, overpressure generation, petroleum migration, and so on. With the numerical method, the effect of the compaction on the secondary migration was analyzed and the results show that the pressure gradient and the flux resulted from compaction are so small that could be neglected by comparing to the buoyancy of oil. The main secondary migration driving forces are therefore buoyancy and capillary within a hydrostatic system. Modeling with the commercial software-Basin_Mod, the migration pathways of petroleum in clastic carriers seem to be inhomogeneous, controlled by heterogeneity of the driving force, which in turn resulted from the topography of seals, the fabrics and the capillary pressure of the clastic carriers. Furthermore, the direct and indirect methods to study fault-sealing properties in the course of migration were systemically summarized. They may be characterized directly by lithological juxtaposition, clay smear and diagenesis, and indirectly the comparing the pressures and fluid properties in the walls at two apartments of a fault. In Jungaer Basin, the abnormal pressures are found in the formations beneath Badaowan or Baijantan Formation. The occurrence of the overpressure seems controlled by the stratigraphy. The rapid sedimentation, tectonic pressuring, clay sealing, chemical diagensis were considered as the principal pressuring mechanisms. The evolution of fluid pressure is influenced differently at different parts of the basin by the tectonic stresses. So the basin appears different pressure evolution cycles from each part to another during the geological history. By coupling the results of thermal evolution, pressure evolution and organic matter maturation, the area and the period of primary migration were acquired and used to determine the secondary migration time and range. The primary migration in Fengcheng Formation happened from latter Triassic to early Jurassic in the main depressions. The main period of lower-Wuerhe Formation was at latter Jurassic in Changji, Shawan and Pen-1-jing-xi Depression, and at the end of early Cretaceous in Mahu Depression. The primary migration in Badaowan and Sangonghe Formation is at the end of early-Cretaceous in Changji Depression. After then, the fluid potential of oil is calculated at the key time determined from area and time of the primary migration. Generally, fluid potential of oil is high in the depressions and low at the uplifts. Synthetically, it is recognized that the petroleum migration in the Jungaer Basin is very complex, that leads us to classify the evolution of petroleum systems in Northwestern China as a primary stage and a reformed one. The remigration of accumulated petroleum, caused by the reformation of the basin, results in the generation of multiple petroleum systems. The faults and unconformities are usually the linkers among the original petroleum systems. The Permian petroleum system in Jungaer Basin is such a multiple petroleum system. However, the Jurassic petroleum system stays still in its primary stage, thought the strong influences of the new tectonic activities.

下扬子北缘前陆盆地形成演化与油气赋存条件

The foreland basin on the northern margin of the lower reach of the Yangtze river (the lower Yangtze foreland basin) is tectonically situated in the basin-mountain transitional area along the southeastern flank of the Dabie mountains. The early formation and development of the basin is closely related to the open-up of the Mian-Lue paleo-oceanic basin on the southern margin of the Central Orogenic System represented by Qinling-Dabei orogenic belt, while the tectonic evolution of the middle-late stage of the basin is mainly related to development of the Mian-Lue tectonic zone that occurred on the basis of the previous Mian-Lue paleo-suture. The foreland basin of the northern rim of the lower reach of the Yangtze river was formed during the middle-Triassic collision between the Yangtze and North China plates and experienced an evolution of occuirence-development-extinction characterized by marine facies to continental facies and continental margin to intracontinent in terms of tectonic setting.The foreland basin (T2-J2) was developed on the basis of the passive continental marginal basin on the south side of the Mian-Lue paleo-ocean and superimposed by late Jurassic-Tertiary fault basin. The tectonic setting underwent a multiple transformation of rifting-collisional clososing-tensional faulting and depression, which resulted in changes of the property for the basin and the final formation of the superposed compose basin in a fashion of 3-story-building. According to the tectonic position and evolution stages of plate collision happening on the southeastern margin of the Dabie mountains, and tectono-tratigraphic features shown by the foreland basin in its main formational period, the evolution of the foreland basin can be divided into four stages: 1) pre-orogenic passive margin (P2-Ti). As the Mian-Lue ocean commenced subduction in the late-Permian, the approaching of the Yangtze and North China plates to each other led to long-periodical and large-scale marine regression in early Triassic which was 22 Ma earlier than the global one and generated I-type mixed strata of the clastic rocks and carbonate, and I-type carbonate platform. These represent the passive stratigraphy formed before formation of the foreland basin. 2) Foreland basin on continental margin during main orogenic episode (T2.3). The stage includes the sub-stage of marine foreland basin (T2X remain basin), which formed I-type stratigrphy of carbonate tidal flat-lagoon, the sub-stage of marine-continental transition-molasse showing II-type stratigraphy of marine-continental facies lake - continental facies lake. 3) Intracontinental foreland basin during intracontinental orogeny (Ji-2)- It is characterized by continental facies coal-bearing molasses. 4) Tensional fault and depression during post-orogeny (J3-E). It formed tectono-stratigraphy post formation of the foreland basin, marking the end of the foreland evolution. Fold-thrust deformation of the lower Yangtze foreland basin mainly happened in late middle-Jurassic, forming ramp structures along the Yangtze river that display thrusting, with deformation strength weakening toward the river from both the Dabie mountains and the Jiangnan rise. This exhibits as three zones in a pattern of thick-skinned structure involved the basement of the orogenic belt to decollement thin-skinned structure of fold-thrust from north to south: thrust zone of foreland basin on northern rim of the lower reach of the Yangtze river, foreland basin zone and Jiannan compose uplift zone. Due to the superposed tensional deformation on the earlier compressional deformation, the structural geometric stratification has occurred vertically: the upper part exhibits late tensional deformation, the middle portion is characterized by ramp fault -fold deformation on the base of the Silurian decollement and weak deformation in the lower portion consisting of Silurian and Neo-Proterozoic separated by the two decollements. These portions constitutes a three-layered structural assemblage in a 3-D geometric model.From the succession of the lower reach of the Yangtze river and combined with characteristics of hydrocarbon-bearing rocks and oil-gas system, it can be seen that the succession of the continental facies foreland basin overlies the marine facies stratigraphy on the passive continental margin, which formed upper continental facies and lower marine facies hydrocarbon-bearing rock system and oil-gas forming system possessing the basic conditions for oil-gas occurrence. Among the conditions, the key for oil-gas accumulation is development and preservation of the marine hydrocarbon-bearing rocks underlying the foreland basin. The synthetic study that in the lower Yangtze foreland basin (including the Wangjiang-Qianshan basin), the generation-reservoir-cover association with the Permian marine facies hydrocarbon-bearing rocks as the critical portion can be a prospective oil-gas accumulation.Therefore, it should aim at the upper Paleozoic marine hydrocarbon-bearing rock system and oil-gas forming system in oil-gas evaluation and exploration. Also, fining excellent reservoir phase and well-preserved oil-gas accumulation units is extremely important for a breakthrough in oil-gas exploration.

Severidade de mancha de alternaria em genótipos de girassol no Cerrado do Distrito Federal.

RESUMO: Este trabalho teve como objetivo comparar a severidade da mancha de Alternaria de genótipos de girassol em ambientes do Cerrado do Distrito Federal. Três experimentos foram avaliados, dois na Embrapa Cerrados (Planaltina, DF) e um localizado na Embrapa Produtos e Mercado (Recanto das Emas, DF). Foram feitas análises ao longo do ciclo da cultura com um intervalo de 15 dias, sendo a primeira aos 35 dias após emergência. Cada planta foi analisada em três partes: terço inferior, terço médio e terço superior. Ao final de cada experimento, a área abaixo da curva de progresso da doença (AACPD) foi calculada para cada genótipo. De acordo com os resultados observados, o ambiente de sequeiro na Embrapa Cerrados, que deteve a maior média da severidade da doença, entre os ambientes avaliados. Dentre os genótipos avaliados, MG 360 mostrou menor severidade da doença no sequeiro e AGUARA 06 no irrigado da Embrapa Cerrados. O genótipo BSG 42 na Embrapa Produtos e Mercado, se destacou pela menor severidade do fungo. Houve influência significativa do ambiente nos resultados de severidade da doença, que está estreitamente relacionada com os fatores climáticos como temperatura e umidade relativa do ar. A compreensão dessas condições favoráveis ao desenvolvimento do fungo é essencial quando se avalia a resistência em genótipos de girassol. ABSTRACT: This study had the purpose of comparing the severity of Alternaria leaf spot on genotypes of sunflower in the Brazilian Cerrado. Three field trials were established, two at Embrapa Cerrados (Planaltina, DF) and one at Embrapa Produtos e Mercados (Recanto das Emas, DF). Evaluations were made during the crop cycle every 15 days, the first one happening 35 days after crop emergency. Each plant was analyzed in three parts: lower, middle and upper thirds. At the end of each trial the average area under the disease progress curve (AUDPC), for each third, was calculated for all genotypes. According to the observed results, the dryland environment at Embrapa Cerrados had the highest mean disease severity, among the studied environments. Between the evaluated genotypes, MG360 showed less severity in dryland and AGUARA 06 in the irrigated environment at Embrapa Cerrados. At Embrapa Produtos e Mercado the genotype that presented the best performance was BRS G42. Environmental conditions deeply affected the trials, mainly temperature and relative humidity. Their influence on Alternaria leaf spot epidemics in the Cerrado region must be studied in more detail, to avoid misinterpreting data when evaluating sunflower genotypes for resistance to this important fungal disease.