松辽盆地南部岩性油藏成藏模式与分布规律

According to the basic geologic conditions, the paper is directed by the modem oil-gas accumulation theory and petroleum system in which typical oil pools are analyzed and the shape of lithologic trap and geologic factors are pointed out. The process during which oil and gas migrate from source rock to lithologic trap is rebuilt, and the accumulation model of oil pool is set up. With the comprehensive application of seismic geologic and log data and paying attention to the method and technology which is used to distinguish lithologic accumulation. Promising structural-lithofacies zones are got and the distribution rule of various lithologic accumulation is concluded. With making use of the biologic mark compound, different reservoirs are compared. As a result, the oil and gas in HeiDimiao come from Nenjiang Group's source rocks; in SaErTu from QingShenkou Group's and Nenjiang Group's, and in PuTaohua. GaoTaizi and FuYang from QingShankou Group's. According to the development and distribution of effective source rock, oil distribution and the comparison in the south of SongLiao basin, the characteristic of basin structure and reservoir distribution is considered, and then the middle-upper reservoir of SongLiao basin south are divided into two petroleum system and a complex petroleum system. Because of the characteristic of migration and accumulation, two petroleum systems can furtherly be divided into 6-7 sub-petroleum systems,20 sub-petroleum systems in all. As a result of the difference of the migration characteristic, accumulation conditions and the place in the petroleum system, the accumulation degree and accumulation model are different. So three accumulation mechanism and six basic accumulation model of lithologic trap are concluded. The distribution of lithologic pools is highly regular oil and gas around the generation sag distribute on favorable structural-lithofacies zones, the type of lithological pool vary regularly from the core of sandstone block to the upper zone. On the basic of regional structure and sedimentary evolution, main factors which control the form of trap are discovered, and it is the critical factor method which is used to discern the lithologic trap. After lots of exploration, 700km~2 potential trap is distinguished and 18391.86 * 10~4 tons geologic reserves is calculated. Oil-water distribution rule of pinch-out oil pool is put up on plane which is the reservoirs can be divided into four sections. This paper presented the law of distribution of oil and water in updip pinch-out reservoir, that is, hydrocarbon-bearing formation in plane can be divided into four zones: bottom edge water zone, underside oil and water zone, middle pure oil zone and above residual water zone. The site of the first well should be assigned to be middle or above pure oil zone, thus the exploration value of this type of reservoir can be recognized correctly. In accordance with the characteristics of seism and geology of low permeability thin sandstone and mudstone alternation layer, the paper applied a set of reservoir prediction technology, that is: (1)seism multi-parameter model identification; (2) using stratum's absorbing and depleting information to predict reservoir's abnormal hydrocarbon-bearing range. With the analysis of the residual resource potential and the research of two petroleum system and the accumulation model, promising objective zones are predicted scientifically. And main exploration aim is the DaRngZi bore in the west of ChangLin basin, and YingTai-SiFangZi middle-upper assembly in Honggang terrace.

东海陆架盆地西南部烟囱构造与油气运聚关系研究

In recent years, chimney structure has been proved one of important indicators and a useful guide to major petroleum fields exploration through their exploration history both at home and abroad. Chimney structure, which has been called "gas chimney" or "seismic chimney", is the special fluid-filled fracture swarm, which results from the boiling of active thermal fluid caused by abruptly decreasing of high pressure and high temperature in sedimentary layers of upper lithosphere. Chimney structure is well developed in continental shelf basin of East China Sea, which indicates the great perspectives of petroleum resources there. However, the chimney structure also complicated the petroleum accumulation. So the study of chimney structure on its formation, its effect on occurrence and distribution of petroleum fields is very important not only on theoretical, but also on its applied research. It is for the first time to make a clear definition of chimney structure in this paper, and the existence and practical meaning of chimney structure are illustrated. Firstly, on the viewpoint of exploration, this will amplify exploration area or field, not only in marine, but also on continent. Secondly, this is very important to step-by-step exploration and development of petroleum fields with overpressure. Thirdly, this will provide reference for the study on complex petroleum system with multi-sources, commingled sources and accumulation, multi-stage accumulations, and multi-suits petroleum system in the overlay basin. Fourthly, when the thermal fluid enters the oceanic shallow layer, it can help form gas hydrate under favorable low-temperature and high-pressure conditions. Meanwhile, the thermal fluid with its particular component and thermal content will affect the physical, chemical and ecological environments, which will help solving the problem of global resources and environment. Beginning from the regional tectonic evolution characteristics, this paper discussed the tectonic evolution history of the Taibei depression, then made an dynamical analysis of the tectonic-sedimentary evolution during the Mesozoic and Cenozoic for the East China Sea basin. A numerical model of the tectonic-thermal evolution of the basin via the Basin-Mod technique was carried out and the subsidence-buried history and thermal history of the Taibei depression were inverse calculated: it had undergone a early rapid rift and sag, then three times of uplift and erosion, and finally depressed and been buried. The Taibei depression contains a huge thick clastic sedimentary rock of marine facies, transitional facies and continental facies on the complex basement of ante-Jurassic. It is a part of the back-arc rifting basins occurred during the Mesozoic and Cenozoic. The author analyzed the diagenesis and thermal fluid evolution of this area via the observation of cathodoluminescence, scanning electron microscope and thin section, taking advantage of the evidences of magma activities, paleo-geothermics and structural movement, the author concluded that there were at least three tectonic-thermal events and three epochs of thermal-fluid activities; and the three epochs of thermal-fluid activities were directly relative to the first two tectonic-thermal events and were controlled by the generation and expulsion of hydrocarbon in the source rock simultaneously. Based on these, this paper established the corresponding model between the tectonic-thermal events and the thermal-fluid evolution of the Taibei Depression, which becomes the base for the study on the chimney structures. According to the analyses of the gas-isotope, LAM spectrum component of fluid inclusion, geneses of CO_2 components and geneses of hydrocarbon gases, the author preliminarily verified four sources of the thermal fluid in the Taibei Depression: ① dehydration of mud shale compaction, ② expulsion of hydrocarbon in the source rock; ③ CO_2 gas hydro-thermal decomposition of carbonatite; ④magma-derived thermal fluid including the mantle magma water and volatile components (such as H_2O, CO_2, H_2S, SO_2, N_2 and He etc.). On the basis of the vitrinite reflectance (Ro), homogenization temperature of fluid inclusion, interval transit time of major well-logging, mud density of the wells, measured pressure data and the results of previous studies, this paper analyzed the characteristics of the geothermal fields and geo-pressure fields for the various parts in this area, and discussed the transversal distribution of fluid pressure. The Taibei depression on the whole underwent a temperature-loss process from hot basin to cold basin; and locally high thermal anomalies occurred on the regional background of moderate thermal structure. The seal was primarily formed during the middle and late Paleocene. The overpressured system was formed during the middle and late Eocene. The formation of overpressured system in Lishui Sag underwent such an evolutionary process as "form-weaken-strengthen-weaken". Namely, it was formed during the middle and late Eocene, then was weakened in the Oligocene, even partly broken, then strengthened after the Miocene, and finally weakened. The existence of the thermal fluid rich in volatile gas is a physical foundation for the boiling of the fluid, and sharply pressure depletion was the major cause for the boiling of the fluid, which suggests that there exists the condition for thermal fluid to boil. According to the results of the photoelastic simulation and similarity physical experiments, the geological condition and the formation mechanism of chimnestructures are summarized: well compartment is the prerequisite for chimney formation; the boiling of active thermal fluid is the original physical condition for chimney formation; The local place with low stress by tension fault is easy for chimney formation; The way that thermal fluid migrates is one of the important factors which control the types of chimney structures. Based on where the thermal fluid come from and geometrical characteristics of the chimney structures, this paper classified the genetic types of chimney structures, and concluded that there existed three types and six subtypes chimney structures: organic chimney structures generated by the hydrocarbon-bearing thermal fluid in middle-shallow layers, inorganic and commingling-genetic chimney structures generated by thermal fluid in middle-deep layers. According to the seismic profiles interpretations, well logging response analysis and mineralogical and petrological characteristics in the study area, the author summarized the comprehensive identification marks for chimney structures. Especially the horizon velocity analysis method that is established in this paper and takes advantage of interval velocity anomaly is a semi-quantitative and reliable method of chimney structure s identification. It was pointed out in this paper that the occurrence of the chimney structures in the Taibei depression made the mechanism of accumulation complicated. The author provided proof of episodic accumulation of hydrocarbon in this area: The organic component in the boiling inclusion is the trail of petroleum migration, showing the causality between the boiling of thermal fluid and the chimney structures, meanwhile showing the paroxysmal accumulation is an important petroleum accumulation model. Based on the evolutionary characteristics of various types of chimney structures, this paper discussed their relationships with the migration-accumulation of petroleum respectively. At the same time, the author summarized the accumulating-dynamical models associated with chimney structures. The author analyzed such accumulation mechanisms as the facies state, direction, power of petroleum migration, the conditions of trap, the accumulation, leakage and reservation of petroleum, and the distribution rule of petroleum. The author also provides explanation for such practical problems the existence of a lot of mantle-derived CO_2, and its heterogeneous distribution on plane. By study on and recognition for chimney structure, the existence and distribution of much mantle-derived CO_2 found in this area are explained. Caused by tectonic thermal activities, the deep magma with much CO_2-bearing thermal fluid migrate upward along deep fault and chimney structures, which makes two wells within relatively short distance different gas composition, such as in well LF-1 and well LS36-1-1. Meanwhile, the author predicted the distribution of petroleum accumulation belt in middle-shallow layer for this area, pointed out the three favorable exploration areas in future, and provided the scientific and deciding references for future study on the commingling-genetic accumulation of petroleum in middle-deep layer and the new energy-gas hydrate.

山东东营凹陷浊积岩油藏形成机制及预测技术

More and more exploration practises and research results prove that deep-water turbidites and slump turbidites in abrupt slope belt as well as slump turbidites in deposit center are favorable places to find subtle reservoirs. Based on sedimentology, sequence stratigraphy, tectonics and petroleum geology and with the tool of computer, this paper focused a set of questions such as the forming mechanism and m&a of turbidite reservoir in Dongying Sag, and obtained a systematic research result from available information of geology, seismic survey, well logging and testing, etc. Since the structural pattern and tectonic stress are controlling factors on distribution of turbidite reservoirs, deep-water sequence and shallow-water sequence have close relation with various turbidites. The author primarily disclose the regular pattern of the turbidites in the abrupt slope trouth, and predict that the abrupt slope is mainly connected to near-bank slump turbidite fans and deep-water turbidite fans; whereas the depocenter area usually developed with front delta slump fans. According to this, seismic-geology models corresponding to various deposit systems can be set up as a principle for predicting the turbiditea in faulted lacustrine basins. Based on comprehensive study of the turbidite reservoir forming condition and main controlling factors, a differential accumulation model and a multiple migration&accumulation model were also set up for abrupt slope turbidities. Referenced the m

东营凹陷胜坨地区油气成藏模式及其勘探前景研究

利用现代油气成藏理论，综合运用地质、地球物理和地球化学资料，对胜坨油田的油气分布、构造和圈闭、沉积和储层、油气生成和运移、以及油气勘探前景等进行了深人综合研究，进行了成藏模式和成藏机理探讨，阐明了油气富集的地质规律，明确了该区进一步勘探和开发的方向和目标。对整个胜利油区的隐蔽油气藏成因和预测具有重要的指导意义。1．通过精细的油源对比，确定了胜沱地区有效烃源岩的识别标志，查明了附近利津洼陷和民丰洼陷沙河街组烃源岩的地质地球化学特征，阐明了有效烃源岩的分布及其成因规律，说明有效烃源岩对胜佗复式油气聚集带形成的控制作用。2．通过系统的断裂形态学，断裂运动学和动力学分析，阐明了胜北断层对沙河街组沉积体系和储集性砂体分布的控制作用，以及对各种圈闭的控制作用。同时开展了构造应力场分析，再现油气运移和成藏的流体运动方向。3．通过层序地层学和沉积体系研究，建立了沙河街组储集性砂体分布模式，着重建立了Es3"和Es3下储集性砂体成因模式和分布规律，为隐蔽油气藏勘探提供依据。同时利用储层描述方法和技术，对EsZ重点储层进行高分辨率层序格架研究，阐明胜沱大油田储集空间的展布规律。4，在有效烃源岩，断裂构造和储层沉积体系研究的基础上，开展了油气运移通道和油气运移期次分析，查明胜北断裂及其次级断层是沟通研究区储层和圈闭的主要油气运移通道，扇三角洲和水下扇砂体是油气运移的另一种通道。所以与大型断层相连的砂体基本都形成了油气充满度较高的油藏。5．针对研究区沙三段下部和沙四段岩性圈闭比较发育，成藏条件良好的清况，首次利用物理模拟装置进行了单砂体油藏形成的模拟实验。结果表明，在高压异常条件下，孔隙度和渗透率对原油进人由水充满砂岩具有强烈的控制作用。虽然胜沱经过40年不断的油气勘探找到了4亿多吨原油储量，但是作者认为还具有很大的找油潜力。其中胜北断裂下降盘的沙三段下部和沙四段扇三角洲砂体，近岸水下扇砂体和浊积扇砂体具有很好的成藏条件，值得进一步勘探。

Bereavement Assessment Practice in Hospice Settings: Challenges for Palliative Care Social Workers

The management and delivery of bereavement support services in palliative care settings presents practical and ethical challenges. A national survey, conducted in 2007, examined bereavement practice in ten Marie Curie hospices across the United Kingdom. This qualitative study was undertaken using semi-structured telephone interviews with Bereavement Service Leaders located in each hospice. Although findings revealed that bereavement services were in operation and had been reviewed in response to the National Institute for Clinical Excellence Guidance (2004), and all bereaved families were offered support, there was no standardisation of service delivery across sites. Multi-disciplinary team meetings facilitated shared decision-making for bereavement follow-up, and expanded and clarified documentation completed by nursing staff around the time of the patient’s death. However, there was ambiguity regarding professional ‘duty of care’ and agency responses to bereaved individuals who were suicidal. Questions were raised around clinical effectiveness, reliability and professional accountability. The study highlighted ethical issues centred on documentation, user participation and consent, and found staff training was variable across the 10 hospices. The findings have informed the development of a post-bereavement service model which has been subsequently implemented across Marie Curie Cancer Care.

Evaluating periocidities in peat-based climate proxy records.

Proxy records derived from ombrotrophic peatlands provide important insights into climate change over decadal to millennial timescales. We present mid- to late- Holocene humification data and testate amoebae-derived water table records from two peatlands in Northern Ireland. We examine the repli- cation of periodicities in these proxy climate records, which have been precisely linked through teph- rochronology. Age-depth models are constructed using a Bayesian piece-wise linear accumulation model and chronological errors are calculated for each profile. A Lomb-Scargle Fourier transform-based spectral analysis is used to test for statistically significant periodicities in the data. Periodicities of c. 130, 180, 260, 540 and 1160 years are present in at least one proxy record at each site. The replication of these peri- odicities provides persuasive evidence that they are a product of allogenic climate controls, rather than internal peatland dynamics. A technique to estimate the possible level of red-noise in the data is applied and demonstrates that the observed periodicities cannot be explained by a first-order autoregressive model. We review the periodicities in the light of those reported previously from other marine and terrestrial climate proxy archives to consider climate forcing parameters. © 2012 Elsevier Ltd. All rights reserved.

Understanding and modelling hydrological and soil erosion processes in burnt forest catchments

Forest fires implications in overland flow and soil erosion have been researched for several years. Therefore, is widely known that fires enhance hydrological and geomorphological activity worldwide as also in Mediterranean areas. Soil burn severity has been widely used to describe the impacts of fire on soils, and has being recognized as a decisive factor controlling post-fire erosion rates. However, there is no unique definition of the term and the relationship between soil burn severity and post-fire hydrological and erosion response has not yet been fully established. Few studies have assessed post-fire erosion over multiple years, and the authors are aware of none which assess runoff. Small amount of studies concerning pre-fire management practices were also found. In the case of soil erosion models, the Revised Universal Soil Loss Equation (RUSLE) and the revised Morgan–Morgan–Finney (MMF) are well-known models, but not much information is available as regards their suitability in predicting post-fire soil erosion in forest soils. The lack of information is even more pronounced as regards post-fire rehabilitation treatments. The aim of the thesis was to perform an extensive research under the post fire hydrologic and erosive response subject. By understanding the effect of burn severity in ecosystems and its implications regarding post fire hydrological and erosive responses worldwide. Test the effect of different pre-fire land management practices (unplowed, downslope plowed and contour plowed) and time-since-fire, in the post fire hydrological and erosive response, between the two most common land uses in Portugal (pine and eucalypt). Assess the performance of two widely-known erosion models (RUSLE and Revised MMF), to predict soil erosion rates during first year following two wildfires of distinctive burn severity. Furthermore, to apply these two models considering different post-fire rehabilitation treatments in an area severely affected by fire. Improve model estimations of post-fire runoff and erosion rates in two different land uses (pine and eucalypt) using the revised MMF. To assess these improvements by comparing estimations and measurements of runoff and erosion, in two recently burned sites, as also with their post fire rehabilitation treatments. Model modifications involved: (1) focusing on intra-annual changes in parameters to incorporate seasonal differences in runoff and erosion; and (2) inclusion of soil water repellency in runoff predictions. Additionally, validate these improvements with the application of the model to other pine and eucalypt sites in Central Portugal. The review and meta-analysis showed that fire occurrence had a significant effect on the hydrological and erosive response. However, this effect was only significantly higher with increasing soil burn severity for inter-rill erosion, and not for runoff. This study furthermore highlighted the incoherencies between existing burn severity classifications, and proposed an unambiguous classification. In the case of the erosion plots with natural rainfall, land use factor affected annual runoff while land management affected both annual runoff and erosion amounts significantly. Time-since-fire had an important effect in erosion amounts among unplowed sites, while for eucalypt sites time affected both annual runoff and erosion amounts. At all studied sites runoff coefficients increase over the four years of monitoring. In the other hand, sediment concentration in the runoff, recorded a decrease during the same period. Reasons for divergence from the classic post-fire recovery model were also explored. Short fire recurrence intervals and forest management practices are viewed as the main reasons for the observed severe and continuing soil degradation. The revised MMF model presented reasonable accuracy in the predictions while the RUSLE clearly overestimated the observed erosion rates. After improvements: the revised model was able to predict first-year post-fire plot-scale runoff and erosion rates for both forest types, these predictions were improved both by the seasonal changes in the model parameters; and by considering the effect of soil water repellency on the runoff, individual seasonal predictions were considered accurate, and the inclusion of the soil water repellency in the model also improved the model at this base. The revised MMF model proved capable of providing a simple set of criteria for management decisions about runoff and erosion mitigation measures in burned areas. The erosion predictions at the validation sites attested both to the robustness of the model and of the calibration parameters, suggesting a potential wider application.

Pharmacométrie de la ropivacaïne suivant l’anesthésie locorégionale chez les patients orthopédiques : caractérisation de l’intensité et de la durée du bloc sensitif

Introduction & Objectifs : Pour assurer l’analgésie postopératoire, l’anesthésiste dispose, en plus des différentes classes de médicaments administrés par voie orale ou intraveineuse, de diverses techniques pour bloquer l’influx nerveux douloureux en administrant les anesthésiques locaux (AL) de manière centrale ou périphérique. La ropivacaïne (ROP), un AL à longue durée d’action, est un médicament de première intention partout dans le monde, en raison de sa grande efficacité et de son faible risque de toxicité. Contrairement à certains pays, la ROP n'est toujours pas indiquée au Canada pour la rachianesthésie (bloc central) en raison d'un manque de données probantes. Jusqu'à présent, les efforts de recherche ont essentiellement porté sur la sécurité ainsi que sur la durée d’action du médicament lorsqu’administré par voie spinale. De plus, les doses optimales de ROP pour l’anesthésie régionale périphérique ne sont pas encore précisément connues. La posologie devrait être adaptée au site d’administration ainsi qu’à l’intensité et la durée du stimulus produit par la chirurgie. Ultimement, cela permettrait aux cliniciens d’identifier le régime optimal en fonction des facteurs démographiques qui pourraient affecter la pharmacocinétique (PK) et la pharmacodynamie (PD) de l’AL (objectif global de ces travaux). Validation de la Méthode Analytique Manuscrit 1 : Une méthode analytique spécifique et sensible permettant de déterminer les concentrations plasmatiques de ROP a d’abord été optimisée et validée. Validation du Biomarqueur Manuscrit 2 : Nous avons ensuite mis au point et évalué la fiabilité d’une méthode quantitative basée sur la mesure du seuil de perception sensorielle (CPT) chez le volontaire sain. Ce test nécessite l’application d’un courant électrique transcutané qui augmente graduellement et qui, selon la fréquence choisie, est capable de stimuler spécifiquement les fibres nerveuses impliquées dans le cheminement de l’influx nerveux douloureux. Les résultats obtenus chez les volontaires sains indiquent que la mesure CPT est fiable, reproductible et permet de suivre l’évolution temporelle du bloc sensitif. Études cliniques Manuscrit 3 : Nous avons ensuite caractérisé, pendant plus de 72 h, l’absorption systémique de la ROP lorsqu’administrée pour un bloc du nerf fémoral chez 19 patients subissant une chirurgie du genou. Le modèle PK populationnel utilisé pour analyser nos résultats comporte une absorption biphasique durant laquelle une fraction de la dose administrée pénètre rapidement (temps d’absorption moyen : 27 min, IC % 19 – 38 min) dans le flux sanguin systémique pendant que l’autre partie, en provenance du site de dépôt, est redistribuée beaucoup plus lentement (demi-vie (T1/2) : 2.6 h, IC % 1.6 – 4.3 h) vers la circulation systémique. Une relation statistiquement significative entre l’âge de nos patients et la redistribution de l’AL suggère que la perméabilité tissulaire est augmentée avec l’âge. Manuscrit 4 : Une analyse PK-PD du comportement sensitif du bloc fémoral (CPT) a été effectuée. Le modèle développé a estimé à 20.2 ± 10.1 mg la quantité de ROP nécessaire au site d’action pour produire 90 % de l’effet maximal (AE90). À 2 X la AE90, le modèle prédit un début d’action de 23.4 ± 12.5 min et une durée de 22.9 ± 5.3 h. Il s’agit de la première étude ayant caractérisé le comportement sensitif d’un bloc nerveux périphérique. Manuscrit 5 : La troisième et dernière étude clinique a été conduite chez les patients qui devaient subir une chirurgie du genou sous rachianesthésie. Tout comme pour le bloc du nerf fémoral, le modèle PK le plus approprié pour nos données suggère que l’absorption systémique de la ROP à partir du liquide céphalo-rachidien est biphasique; c.à.d. une phase initiale (T1/2 : 49 min, IC %: 24 – 77 min) suivie (délai: 18 ± 2 min) d'une phase légèrement plus lente (T1/2 : 66 min, IC %: 36 – 97 min). L’effet maximal a été observé beaucoup plus rapidement, soit aux environs de 12.6 ± 4.9 min, avant de revenir aux valeurs de base 210 ± 55 min suivant l’administration de l’agent. Ces données ont permis d’estimer une AE50 de 7.3 ± 2.3 mg pour l'administration spinale. Conclusion : En somme, ces modèles peuvent être utilisés pour prédire l’évolution temporelle du bloc sensitif de l’anesthésie rachidienne et périphérique (fémorale), et par conséquent, optimiser l’utilisation clinique de la ROP en fonction des besoins des cliniciens, notamment en ce qui a trait à l’âge du patient.

Évaluation de l'acquisition de la résistance à la colistine chez Escherichia coli O149 chez le porc.

La diarrhée post-sevrage est une maladie d’importance dans l’industrie porcine et est principalement causée Escherichia coli O149. Le traitement habituellement utilisé est la néomycine. Cependant, en raison de l’antibiorésistance, les vétérinaires se tournent vers la colistine sulfate (CS). La CS lie les lipopolysaccharides (LPS) et provoque un déplacement des cations divalents causant la formation de pores entrainant la mort cellulaire. Le système à deux composantes PmrA/PmrB est le plus incriminé dans la résistance à la colistine en ajoutant un groupement 4-amino-4-déoxy-L-arabinose (L-Ara4N) au lipide A des LPS, augmentant ainsi la charge du LPS et diminuant son affinité pour la CS. L’objectif principal est d’évaluer l’acquisition de la résistance à la CS d’E. coli in vitro et dans un modèle in vivo. Nous avons utilisé des souches associées à des cas cliniques d’E. coli O149 et avons créé 22 mutants résistants à la CS. La concentration minimale inhibitrice (CMI) a été mesurée par une méthode de double dilution et comparée au seuil de résistance. Suite au séquençage des gènes pmrA/pmrB, nous avons identifié sept nouveaux polymorphismes, trois dans PmrA : A80V, N128I, S144G et quatre dans PmrB : V87E, D148Y, D148V et T156M. Pour l’essai in vivo, nous avons suivi une souche expérimentale ETEC:F4 (E. coli O149) et isolé des E. coli de la flore commensale. Le séquençage des gènes pmrA et pmrB de ces isolats a montré un polymorphisme spécifique, G15R et T156M respectivement. Cependant, plusieurs souches récoltées possédaient une résistance à la CS, mais sans polymorphisme de PmrA/PmrB, suggérant d’autre(s) mécanisme(s) de résistance.

Muscarinic MI and Glutamate Receptor Gene Expression and their Functional Role in Pilocarpine Induced Temporal Lobe Epilepsy in rats: Regulation by Bacoside A and Bacopa monnieri Extracts

The present work is to understand the alterations of total muscarinic. muscarinic MI and glutamate receptors in the brain regions of pilocarpine induced epileptic rats. The work focuses on the evaluation of the anti epileptic activity of extracts of Bacopa monnieri, Bacoside A and Carbamazepine in vivo. The molecular changes in the muscarinic M I receptors in the pre- and post-treated epileptic model with Bacopa monnieri, Bacoside A and Carbamazepine were also studied. These studies will help us to elucidate the functional role of muscarinic and glutamate receptors in epilepsy.

Dinâmica de Sedimentação de Lodo em Lagoas de Estabilização

Stabilization ponds are an effective sewage treatment alternative for the climatic conditions prevailing in Brazil. In the present work, a primary facultative pond was studied, in the city of Natal, Rio Grande do Norte, Northeast Brazil. The aim of this study was to evaluate the sedimentation dynamics in the facultative pond. The pond was divided in three section or zones along its length starting from the inlet end namely A1, A2 and A3. The research was accomplished in three phases. In the first the mapping of the sludge layer was done, sludge core samples were also collected for analysis for total, fixed and volatile solids and the depth of the sludge layer was determined using a portable echo sounder. In the second solids sedimentation rates were measured using traps placed in the inlet and outlet zones and in the third phase resuspension sludge was evaluate using a tracer. The amount accumulated sludge since the start operation was 13.583 m3. The sedimentation constant averages changed between 0.93 to 2.94 and 3.90 to 5.80 for the depths of 0.5 and 1.0 m respectively. The relationship between volatile and fixed solids (SV/SF) increased along the pond. The removal efficiencies were 52.12%, 36.09%, and 37.50% for BOD, COD and SS, respectively. The sludge accumulation model proposed had a good adjustment with 0.17 m3/hab.year rate. The results presented here demonstrated that the wind had a direct influence on the sedimentation of solids in this pond affecting the efficiency and sludge accumulation

¿Qué son las llamadas economías alternativas?

Dada la compleja situación de vulnerabilidad del tejido social debido al actual modelo de acumulación, las características que asume el trabajo, la desaparición del Estado Protector, comienzan a plantearse, para y desde los sectores más perjudicados, la necesidad de elaborar nuevas estrategias de supervivencia. En este trabajo se intentará analizar aquellas estrategias que conviven con el sistema capitalista, pero que no corresponden completamente a su lógica, que no son generadas ni por el Estado, ni por el sector privado y que intentan elaborar alternativas de desarrollo- comunitario, local, regional- frente a la situación esbozada anteriormente.

Del Movimiento al Frente : Dinámica política en el Frente Popular Darío Santillán

El grado de desintegración social, desigualdad y de fragmentación de las identidades hicieron paradigmática la crisis del ordenamiento social neoliberal en Argentina. Hacia finales de la década del noventa y a través de la politización de las distintas situaciones de precariedad, de los nuevos contextos de sociabilidad territorial y de la recuperación de lazos y redes sociales ya existentes, surgieron novedosas respuestas de acción colectiva y organización popular. Una de esas "novedades", fue la movilización de grandes agrupamientos de desocupados que protagonizaron movilizaciones -primero en el interior del país y luego en el Conurbano Bonaerense- donde alcanzaron masividad y características muy particulares. El presente trabajo se centrará particularmente en el campo de los Movimientos de Desocupados que se sitúan en la perspectiva política autónoma, y dentro de éstos, retomaremos sólo la experiencia Frente Popular Darío Santillán (FPDS) y del Movimiento de Trabajadores Desocupados "Aníbal Verón" ya que éste se constituyó como su antecedente inmediato. De esta manera, nuestra unidad de referencia será el FPDS en tanto organización y nos propondremos analizar sus dinámicas políticas, posicionamientos y reposicionamientos en la nueva coyuntura político-social abierta con el kirchnerismo en el período de la post convertibilidad, a través de la reconstrucción de su trayectoria organizativa

El "conflicto del campo" de 2008 en Argentina : Hegemonía, acumulación y territorio

El artículo se propone como objetivo abordar el conflicto agrario de 2008 en la Argentina a partir de la interrelación de tres ejes: hegemonía, acumulación y territorio. Para esto, analizamos las dinámicas del circuito productivo sojero y su relación con el modelo de acumulación, e ingresamos luego en el estudio de los componentes específicamente políticos e ideológicos del conflicto, que fueron constituyendo una genuina lucha por la hegemonía. Asimismo, indagamos factores de carácter territorial que atravesaron de modo significativo dicho proceso

El subdesarrollo del macrosistema eléctrico en la costa atlántica de la Provincia de Buenos Aires

El macrosistema eléctrico de la costa atlántica bonaerense muestra un desarrollo divergente respecto de las tracciones y expectativas del proceso productivo global y de las condiciones generales de la reproducción social que puede ser calificado como subdesarrollo. Desde 2003, al producirse el sostenido repunte del consumo eléctrico, la problemática del abastecimiento de electricidad se agravó y el territorio local comenzó a atravesar un estado de emergencia energética. El trabajo analiza los principales factores explicativos de dicha situación: la reestructuración capitalista del sector eléctrico llevada a cabo durante los noventa y los funcionamientos impuestos por el marco regulatorio, los cambios político-económicos de la Posconvertibilidad, la aplicación de una estrategia anticrisis basada en medidas paliativas y la marcada estacionalidad de la demanda eléctrica local inducida por la enorme afluencia turística de la zona