Influência das tensões tectônicas na permeabilidade da formação Açu - Bacia Potiguar

The behavior of the fluid flux in oil fields is influenced by different factors and it has a big impact on the recovery of hydrocarbons. There is a need of evaluating and adapting the actual technology to the worldwide reservoirs reality, not only on the exploration (reservoir discovers) but also on the development of those that were already discovered, however not yet produced. The in situ combustion (ISC) is a suitable technique for these recovery of hydrocarbons, although it remains complex to be implemented. The main objective of this research was to study the application of the ISC as an advanced oil recovery technique through a parametric analysis of the process using vertical wells within a semi synthetic reservoir that had the characteristics from the brazilian northwest, in order to determine which of those parameters could influence the process, verifying the technical and economical viability of the method on the oil industry. For that analysis, a commercial reservoir simulation program for thermal processes was used, called steam thermal and advanced processes reservoir simulator (STARS) from the computer modeling group (CMG). This study aims, through the numerical analysis, find results that help improve mainly the interpretation and comprehension of the main problems related to the ISC method, which are not yet dominated. From the results obtained, it was proved that the mediation promoted by the thermal process ISC over the oil recovery is very important, with rates and cumulated production positively influenced by the method application. It was seen that the application of the method improves the oil mobility as a function of the heating when the combustion front forms inside the reservoir. Among all the analyzed parameters, the activation energy presented the bigger influence, it means, the lower the activation energy the bigger the fraction of recovered oil, as a function of the chemical reactions speed rise. It was also verified that the higher the enthalpy of the reaction, the bigger the fraction of recovered oil, due to a bigger amount of released energy inside the system, helping the ISC. The reservoir parameters: porosity and permeability showed to have lower influence on the ISC. Among the operational parameters that were analyzed, the injection rate was the one that showed a stronger influence on the ISC method, because, the higher the value of the injection rate, the higher was the result obtained, mainly due to maintaining the combustion front. In connection with the oxygen concentration, an increase of the percentage of this parameter translates into a higher fraction of recovered oil, because the quantity of fuel, helping the advance and the maintenance of the combustion front for a longer period of time. About the economic analysis, the ISC method showed to be economically feasible when evaluated through the net present value (NPV), considering the injection rates: the higher the injection rate, the higher the financial incomes of the final project

Influência das tensões tectônicas na permeabilidade da formação Açu - Bacia Potiguar

The behavior of the fluid flux in oil fields is influenced by different factors and it has a big impact on the recovery of hydrocarbons. There is a need of evaluating and adapting the actual technology to the worldwide reservoirs reality, not only on the exploration (reservoir discovers) but also on the development of those that were already discovered, however not yet produced. The in situ combustion (ISC) is a suitable technique for these recovery of hydrocarbons, although it remains complex to be implemented. The main objective of this research was to study the application of the ISC as an advanced oil recovery technique through a parametric analysis of the process using vertical wells within a semi synthetic reservoir that had the characteristics from the brazilian northwest, in order to determine which of those parameters could influence the process, verifying the technical and economical viability of the method on the oil industry. For that analysis, a commercial reservoir simulation program for thermal processes was used, called steam thermal and advanced processes reservoir simulator (STARS) from the computer modeling group (CMG). This study aims, through the numerical analysis, find results that help improve mainly the interpretation and comprehension of the main problems related to the ISC method, which are not yet dominated. From the results obtained, it was proved that the mediation promoted by the thermal process ISC over the oil recovery is very important, with rates and cumulated production positively influenced by the method application. It was seen that the application of the method improves the oil mobility as a function of the heating when the combustion front forms inside the reservoir. Among all the analyzed parameters, the activation energy presented the bigger influence, it means, the lower the activation energy the bigger the fraction of recovered oil, as a function of the chemical reactions speed rise. It was also verified that the higher the enthalpy of the reaction, the bigger the fraction of recovered oil, due to a bigger amount of released energy inside the system, helping the ISC. The reservoir parameters: porosity and permeability showed to have lower influence on the ISC. Among the operational parameters that were analyzed, the injection rate was the one that showed a stronger influence on the ISC method, because, the higher the value of the injection rate, the higher was the result obtained, mainly due to maintaining the combustion front. In connection with the oxygen concentration, an increase of the percentage of this parameter translates into a higher fraction of recovered oil, because the quantity of fuel, helping the advance and the maintenance of the combustion front for a longer period of time. About the economic analysis, the ISC method showed to be economically feasible when evaluated through the net present value (NPV), considering the injection rates: the higher the injection rate, the higher the financial incomes of the final project

Vulnérabilité cardiaque au stress au cours du remodelage ventriculaire pathologique : rôle de la mitochondrie et du pore de perméabilité transitionnelle (PTP)

L’objectif central de cette thèse de Doctorat était d’investiguer les dysfonctions mitochondriales qui surviennent précocement au cours de la phase compensée du remodelage ventriculaire pathologique et qui pourraient jouer un rôle causal dans la progression vers l’insuffisance cardiaque. Nos travaux antérieurs, réalisés à l’aide d’un modèle de surcharge volumique chronique induite par une fistule aorto-cavale (ACF) chez le Rat WKHA, ont montré qu’au cours du remodelage ventriculaire, les mitochondries développaient une vulnérabilité à l’ouverture du pore de perméabilité transitionnelle (PTP : un élément clé de la signalisation de la mort cellulaire) [1]. Ceci était observable au stade compensé du remodelage en absence des dysfonctions mitochondriales majeures typiquement observées dans le cœur insuffisant. Ces résultats nous ont amenés à suggérer que la vulnérabilité à l’ouverture du PTP pourrait constituer un mécanisme précoce favorisant la progression de la cardiopathie. Dans l’étude 1 de cette thèse, nous avons tenté de tester cette hypothèse en induisant une ACF chez deux souches de rats affichant de très nettes différences au niveau de la propension à développer l’insuffisance cardiaque : les souches WKHA et Sprague Dawley (SD). Nos études in vitro sur organelles isolées et in situ sur l’organe entier ont permis de confirmer que, dans le cœur ACF, les mitochondries développent une vulnérabilité à l’ouverture du PTP et à l’activation de la voie mitochondriale de la mort cellulaire lorsqu’exposées à des stress pertinents à la pathologie (surcharge calcique, ischémie-reperfusion [I-R]). Cependant, bien que comparativement aux animaux WKHA, les animaux SD démontraient un remodelage ventriculaire plus rapide et prononcé et une progression précoce vers l’insuffisance cardiaque, aucune différence n’était observable entre les deux groupes au niveau des dysfonctions mitochondriales, suggérant quelles ne sont pas à l’origine de la progression plus rapide de la pathologie chez la souche SD, à tout le moins en réponse à la surcharge volumique. Nous avons par la suite déterminé, à l’aide des mêmes approches expérimentales, si cette vulnérabilité mitochondriale était observable dans une cardiopathie d’étiologie différente, plus spécifiquement celle qui est associée à la dystrophie musculaire de Duchenne (DMD), une maladie génétique causée par une mutation de la protéine dystrophine. Nos études menées (études 2-4) sur de jeunes souris mdx (le modèle murin de la DMD) exemptes de tout signe clinique de cardiopathie n’ont révélé aucune différence au niveau des fonctions mitochondriales de base. Cependant, tout comme dans le modèle d’ACF, les mitochondries dans le cœur de souris mdx étaient significativement plus vulnérables à l’ouverture du PTP lorsque soumises à une I-R (étude 2). Par ailleurs, nous avons démontré que l’administration aiguë de sildénafil aux souris mdx induisait une abolition de l’ouverture du PTP et de ses conséquences signalétiques, une diminution marquée du dommage tissulaire et une meilleure récupération fonctionnelle à la suite de l’I-R (étude 3). Nous avons ensuite testé chez la souris mdx l’administration aiguë de SS31, un peptide anti-oxydant ciblé aux mitochondries, cependant aucun effet protecteur n’a été observé, suggérant que le tamponnement des radicaux libres est d’une utilité limitée si les perturbations de l’homéostasie calcique typiques à cette pathologie ne sont pas traitées simultanément (étude 4). Globalement, les travaux effectués au cours de cette thèse démontrent que la vulnérabilité à l’ouverture du PTP constitue une dysfonction précoce et commune qui survient au cours de remodelages ventriculaires pathologiques d’étiologies différentes. Par ailleurs, ces travaux suggèrent des stratégies d’intervention pharmacologiques ciblant ce processus, dont l’efficacité pour la prévention de l’insuffisance cardiaque demande à être établie.

Stress au travail et santé : situation chez les indépendants

Dans le cadre de l'activité professionnelle, des facteurs de stress d'ordre psychologique, social, et liés à l'organisation du travail, peuvent induire des réponses physiologiques et comportementales impliquées dans la survenue de pathologies comme les maladies cardiovasculaires, les troubles de la santé mentale et les troubles musculosquelettiques.Le Régime social des indépendants (RSI) a sollicité l'Inserm afin de disposer d'un bilan des connaissances sur le stress d'origine professionnelle chez les travailleurs indépendants et ses répercussions sur la santé.Regroupant à la fois des compétences en biologie, psychologie, sociologie et économie de la santé, cette expertise collective présente les modèles et les mécanismes explicatifs mettant en relation le stress au travail et les principales pathologies.Les stratégies de prévention individuelle et collective qui se développent dans le milieu des travailleurs salariés peuvent-elles être adaptées aux travailleurs indépendants ? [Ed.]

Stress au travail et santé : situation chez les indépendants : synthèse et recommandations

Dans le cadre de l'activité professionnelle, des facteurs de stress d'ordre psychologique, social, et liés à l'organisation du travail, peuvent induire des réponses physiologiques et comportementales impliquées dans la survenue de pathologies comme les maladies cardiovasculaires, les troubles de la santé mentale et les troubles musculosquelettiques.Le Régime social des indépendants (RSI) a sollicité l'Inserm afin de disposer d'un bilan des connaissances sur le stress d'origine professionnelle chez les travailleurs indépendants et ses répercussions sur la santé.Regroupant à la fois des compétences en biologie, psychologie, sociologie et économie de la santé, cette expertise collective présente les modèles et les mécanismes explicatifs mettant en relation le stress au travail et les principales pathologies.Les stratégies de prévention individuelle et collective qui se développent dans le milieu des travailleurs salariés peuvent-elles être adaptées aux travailleurs indépendants ? [Ed.]

Pourquoi et comment le stress au travail est dangereux pour la santé

Six salariés sur dix ont un travail stressant. Comment fonctionne le stress ? Quels sont ses effets ? Dominique Chouanière présente l'état des connaissances scientifiques. Elle souligne qu'il faut développer la prévention à la source en identifiant les facteurs collectifs liés à l'organisation du travail.

Vulnérabilité cardiaque au stress au cours du remodelage ventriculaire pathologique induit par surcharge volumique : rôle du pore de perméabilité transitionnelle (PTP)

Mémoire numérisé par la Division de la gestion de documents et des archives de l'Université de Montréal.

C9ORF72 Regulates Stress Granule Formation and Its Deficiency Impairs Stress Granule Assembly, Hypersensitizing Cells to Stress

Hexanucleotide repeat expansions in the C9ORF72 gene are causally associated with frontotemporal lobar dementia (FTLD) and/or amyotrophic lateral sclerosis (ALS). The physiological function of the normal C9ORF72 protein remains unclear. In this study, we characterized the subcellular localization of C9ORF72 to processing bodies (P-bodies) and its recruitment to stress granules (SGs) upon stress-related stimuli. Gain of function and loss of function experiments revealed that the long isoform of C9ORF72 protein regulates SG assembly. CRISPR/Cas9-mediated knockdown of C9ORF72 completely abolished SG formation, negatively impacted the expression of SG-associated proteins such as TIA-1 and HuR, and accelerated cell death. Loss of C9ORF72 expression further compromised cellular recovery responses after the removal of stress. Additionally, mimicking the pathogenic condition via the expression of hexanucleotide expansion upstream of C9ORF72 impaired the expression of the C9ORF72 protein, caused an abnormal accumulation of RNA foci, and led to the spontaneous formation of SGs. Our study identifies a novel function for normal C9ORF72 in SG assembly and sheds light into how the mutant expansions might impair SG formation and cellular-stress-related adaptive responses.

TAR DNA-Binding protein 43 (TDP-43) regulates stress granule dynamics via differential regulation of G3BP and TIA-1

TDP-43 est une protéine multifonctionnelle possédant des rôles dans la transcription, l'épissage des pré-ARNm, la stabilité et le transport des ARNm. TDP-43 interagit avec d'autres hnRNP, incluant hnRNP A2, via son extrémité C-terminale. Plusieurs membres de la famille des hnRNP étant impliqués dans la réponse au stress cellulaire, alors nous avons émis l’hypothèse que TDP-43 pouvait y participer aussi. Nos résultats démontrent que TDP-43 et hnRNP A2 sont localisés au niveau des granules de stress, à la suite d’un stress oxydatif, d’un choc thermique, et lors de l’exposition à la thapsigargine. TDP-43 contribue à la fois à l'assemblage et au maintien des granules de stress en réponse au stress oxydatif. TDP-43 régule aussi de façon différentielle les composants clés des granules de stress, notamment TIA-1 et G3BP. L'agrégation contrôlée de TIA-1 est perturbée en l'absence de TDP-43. En outre, TDP-43 régule le niveau d`ARNm de G3BP, un facteur de granule de stress de nucléation. La mutation associée à la sclérose latérale amyotrophique, TDP-43R361S, compromet la formation de granules de stress. Ainsi, la fonction cellulaire de TDP-43 s'étend au-delà de l’épissage; TDP-43 est aussi un composant de la réponse cellulaire au stress central et un acteur actif dans le stockage des ARNs.

TDP-43 régule la dynamique et la fonction des Granules de Stress via G3BP1

Les Granule de Stress (GS) sont des inclusions cytoplasmiques contenant des protéines et des ARNm qui s’assemblent en réponse à l’exposition à un stress. Leur formation fait partie intégrante de la réponse cellulaire au stress et est considérée comme une étape déterminante pour la résistance au stress et la survie cellulaire. Actuellement, les GS sont reliés à divers pathologies allant des infections virales aux maladies neurovégétatives. L’une d’entre elle, la Sclérose Latérale Amyotrophique (SLA) est particulièrement agressive, caractérisée par une perte des neurones moteurs aboutissant à la paralysie et à la mort du patient en cinq ans en moyenne. Les mécanismes de déclenchement de la pathologie restent encore à déterminer. TDP-43 (TAR DNA binding protein 43) et FUS (Fused in liposarcoma) sont deux protéines reliées à la pathologie qui présentent des similarités de structure et de fonction, suggérant un mécanisme commun de toxicité. TDP-43 et FUS sont toutes les deux recrutées au niveau des GS en condition de stress. Nous avons démontré pour la première fois que la fonction des GS est de protéger les ARNm de la dégradation induite par l’exposition au stress. Cette fonction n’était que suspectée jusqu’alors. De plus nous avons mis en évidence que G3BP1 (Ras GTPase-activating protein-binding protein 1) est l’effectrice de cette fonction via son implication dans la dynamique de formation des GS. TDP-43 étant un régulateur de G3BP1, nous prouvons ainsi que la perte de fonction de TDP-43/G3BP1 aboutit à un défaut de réponse au stress aboutissant à une vulnérabilisation cellulaire. Le mécanisme de toxicité emprunter par FUS diffère de celui de TDP-43 et ne semble pas passer par une perte de fonction dans le cadre de la réponse au stress.

Litoestratigrafia e deformação cenzóica na região de Icapuí, Ceará, e implicações para a estruturação de campos de petróleo na borda ocidental da bacia Potiguar(NE do Brasil)

This thesis deals with the sedimentological/stratigraphic and structural evolution of the sedimentary rocks that occur in the NW continental border of the Potiguar Basin. These rocks are well exposed along coastal cliffs between the localities of Lagoa do Mato and Icapuí, Ceará State (NE Brazil). The sedimentological/stratigraphic study involved, at the outcrop scale, detailed facies descriptions, profile mapping of the vertical succession of different beds, and columnar sections displaying inferred lateral relationships. The approach was complemented by granulometric and petrographic analyses, including the characterization of heavy mineral assemblages. The data set allowed to recognize two kinds of lithological units, a carbonate one of very restricted occurrence at the base of the cliffs, and three younger, distinct siliciclastic units, that predominate along the cliffs, in vertical and lateral extent. The carbonate rocks were correlated to the late Cretaceous Jandaíra Formation, which is covered by the siliciclastic Barreiras Formation. The Barreiras Formation occurs in two distinct structural settings, the usual one with nondeformed, subhorizontal strata, or as tilted beds, affected by strong deformation. Two lithofacies were recognized, vertically arranged or in fault contacts. The lower facies is characterized by silty-argillaceous sandstones with low-angle cross bedding; the upper facies comprises medium to coarse grained sandstones, with conglomeratic layers. The Tibau Formation (medium to coarse-grained sandstones with argillite intercalations) occurs at the NW side of the studied area, laterally interlayered with the Barreiras Formation. Eolic sediments correlated to the Potengi Formation overly the former units, either displaying an angular unconformity, or simply an erosional contact (stratigraphic unconformity). Outstanding structural features, identified in the Barreiras Formation, led to characterize a neocenozoic stress field, which generated faults and folds and/or reactivated older structures in the subjacent late cretaceous (to paleogene, in the offshore basin) section. The structures recognized in the Barreiras Formation comprise two distinct assemblages, namely a main extensional deformation between the localities of Ponta Grossa and Redonda, and a contractional style (succeeded by oblique extensional structures) at Vila Nova. In the first case, the structural assemblage is dominated by N-S (N±20°Az) steep to gently-dipping extensional faults, displaying a domino-style or listric geometry with associated roll-over structures. This deformation pattern is explained by an E-W/WNW extension, contemporaneous with deposition of the upper facies of the Barreiras Formation, during the time interval Miocene to Pleistocene. Strong rotation of blocks and faults generated low-angle distensional faults and, locally, subvertical bedding, allowing to estimate very high strain states, with extension estimates varying between 40% up to 200%. Numerous detachment zones, parallel to bedding, help to acommodate this intense deformation. The detachment surfaces and a large number of faults display mesoscopic features analoguous to the ones of ductile shear zones, with development of S-C fabrics, shear bands, sigmoidal clasts and others, pointing to a hydroplastic deformation regime in these cases. Local occurrences of the Jandaíra limestone are controled by extensional faults that exhume the pre-Barreiras section, including an earlier event with N-S extension. Finally, WNWtrending extensional shear zones and faults are compatible with the Holocene stress field along the present continental margin. In the Vila Nova region, close to Icapuí, gentle normal folds with fold hinges shallowly pluging to SSW affect the lower facies of the Barreiras Formation, displaying an incipient dissolution cleavage associated with an extension lineation at high rake (a S>L fabric). Deposition of the upper facies siliciclastics is controlled by pull-apart graben structures, bordered by N-NE-trending sinistral-normal shear zones and faults, characterizing an structural inversion. Microstructures are compatible with tectonic deformation of the sedimentary pile, burried at shallow depths. The observed features point to high pore fluid pressures during deformation of the sediments, producing hydroplastic structures through mechanisms of granular flow. Such structures are overprinted by microfractures and microfaults (an essentially brittle regime), tracking the change to microfracturing and frictional shear mechanisms accompanying progressive dewatering and sediment lithification. Correlation of the structures observed at the surface with those present at depth was tested through geophysical data (Ground Penetrating Radar, seismics and a magnetic map). EW and NE-trending lineaments are observed in the magnetic map. The seismic sections display several examples of positive flower structures which affect the base of the cretaceous sediments; at higher stratigraphic levels, normal components/slips are compatible with the negative structural inversion characterized at the surface. Such correlations assisted in proposing a structural model compatible with the regional tectonic framework. The strong neogenepleistocene deformation is necessarily propagated in the subsurface, affecting the late cretaceous section (Açu and Jandaíra formations), wich host the hydrocarbon reservoirs in this portion of the Potiguar Basin. The proposed structural model is related to the dextral transcurrent/transform deformation along the Equatorial Margin, associated with transpressive terminations of E-W fault zones, or at their intersections with NE-trending lineaments, such as the Ponta Grossa-Fazenda Belém one (the LPGFB, itself controlled by a Brasiliano-age strike-slip shear zone). In a first step (and possibly during the late Cretaceous to Paleogene), this lineament was activated under a sinistral transpressional regime (antithetic to the main dextral deformation in the E-W zones), giving way to the folds in the lower facies of the Barreiras Formation, as well as the positive flower structures mapped through the seismic sections, at depth. This stage was succeeded (or was penecontemporaneous) by the extensional structures related to a (also sinistral) transtensional movement stage, associated to volcanism (Macau, Messejana) and thermal doming processes during the Neogene-Pleistocene time interval. This structural model has direct implications to hydrocarbon exploration and exploitation activities at this sector of the Potiguar Basin and its offshore continuation. The structure of the reservoirs at depth (Açu Formation sandstones of the post-rift section) may be controlled (or at least, strongly influenced) by the deformation geometry and kinematics characterized at the surface. In addition, the deformation event recognized in the Barreiras Formation has an age close to the one postulated for the oil maturation and migration in the basin, between the Oligocene to the Miocene. In this way, the described structural cenario represents a valid model to understand the conditions of hydrocarbon transport and acummulation through space openings, trap formation and destruction. This model is potentially applicable to the NW region of the Potiguar Basin and other sectors with a similar structural setting, along the brazilian Equatorial Atlantic Margin

Pirometamorfismo nos arenitos da Formação Açu, Bacia Potiguar, NE do Brasil

Pyrometamorphism results from conditions of high temperatures and very low pressures provoked by the intrusion of hypabyssal basic bodies into sedimentary or metassedimentary hosting rocks. The onshore portion of the Potiguar Basin in NE Brazil offers examples of this type of metamorphism nearby the contacts of Paleogene to Neogene plugs, sills and dikes of diabases and basalts crosscutting sandstones, siltstones and shales of the Açu Formation (Albian-Cenomanian). The thermal effects over these rocks are reflected on textures and minerals assemblages that characterize the sanidinite facies of metamorphism, often with partial melting of the feldspathic and mica-rich matrix. The liquid formed is potassic and peraluminous, with variably colored rhyolitic glass (colorless, yellow, brown) comprising microcrystals of tridymite, sanidine and clinoenstatite, besides residual detrital clasts of quartz and rarely zircon, staurolite and garnet. Lenses of shale intercalated within the sandstones display crystallites of Fe-cordierite (sekaninaite), mullite, sanidine, armalcolite (Fe-Ti oxide) and brown spinel. The rocks formed due to the thermal effect of the intrusions are called buchites for which two types are herein described: a light one derived from feldspathic sandstone and siltstone protoliths; and a dark one derived from black shale protoliths. Textures indicating partial melting and minerals such as sanidine, mullite, tridymite and armalcolite strongly demonstrate that during the intrusion of the basic bodies the temperature reached 1,000-1,150°C, and was followed by quenching. Cooling of the interstitial melts has as consequences the closure of pores and decrease of the permeability of the protolith, which varies from about 17-11% in the unaffected rocks to zero in the thermally modified types. Although observed only at contacts and over small distances, the number of basic intrusions hosted within the Potiguar Basin in both onshore and offshore portions leaves opened the possibility of important implications of the thermal effects over the hydrocarbon exploration in this area as well in other Cretaceous and Paleozoic basins in Brazil

Criação de zonas de alta permeabilidade em fraturas: modelagem numérica do Lajedo de Soledade, Formação Jandaíra, Bacia Potiguar

The fracturing in carbonate rocks has been attracting increasingly attention due to new oil discoveries in carbonate reservoirs. This study investigates how the fractures (faults and joints) behave when subjected to different stress fields and how their behavior may be associated with the generation of karst and consequently to increased secondary porosity in these rocks. In this study I used satellite imagery and unmanned aerial vehicle UAV images and field data to identify and map faults and joints in a carbonate outcrop, which I consider a good analogue of carbonate reservoir. The outcrop comprises rocks of the Jandaíra Formation, Potiguar Basin. Field data were modeled using the TECTOS software, which uses finite element analysis for 2D fracture modeling. I identified three sets of fractures were identified: NS, EW and NW-SE. They correspond to faults that reactivate joint sets. The Ratio of Failure by Stress (RFS) represents stress concentration and how close the rock is to failure and reach the Mohr-Coulomb envelopment. The results indicate that the tectonic stresses are concentrated in preferred structural zones, which are ideal places for carbonate dissolution. Dissolution was observed along sedimentary bedding and fractures throughout the outcrop. However, I observed that the highest values of RFS occur in fracture intersections and terminations. These are site of karst concentration. I finally suggest that there is a relationship between stress concentration and location of karst dissolution in carbonate rocks.

Criação de zonas de alta permeabilidade em fraturas: modelagem numérica do Lajedo de Soledade, Formação Jandaíra, Bacia Potiguar

The fracturing in carbonate rocks has been attracting increasingly attention due to new oil discoveries in carbonate reservoirs. This study investigates how the fractures (faults and joints) behave when subjected to different stress fields and how their behavior may be associated with the generation of karst and consequently to increased secondary porosity in these rocks. In this study I used satellite imagery and unmanned aerial vehicle UAV images and field data to identify and map faults and joints in a carbonate outcrop, which I consider a good analogue of carbonate reservoir. The outcrop comprises rocks of the Jandaíra Formation, Potiguar Basin. Field data were modeled using the TECTOS software, which uses finite element analysis for 2D fracture modeling. I identified three sets of fractures were identified: NS, EW and NW-SE. They correspond to faults that reactivate joint sets. The Ratio of Failure by Stress (RFS) represents stress concentration and how close the rock is to failure and reach the Mohr-Coulomb envelopment. The results indicate that the tectonic stresses are concentrated in preferred structural zones, which are ideal places for carbonate dissolution. Dissolution was observed along sedimentary bedding and fractures throughout the outcrop. However, I observed that the highest values of RFS occur in fracture intersections and terminations. These are site of karst concentration. I finally suggest that there is a relationship between stress concentration and location of karst dissolution in carbonate rocks.

Étude sur simulateur de conduite de la relation entre stress et agressivité au volant

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.