A ancoragem ortodôntica tem sido motivo de preocupação para os ortodontistas desde o inicio da prática ortodôntica. Os dispositivos transitórios de ancoragem esquelética (miniparafuso) definiram um novo conceito de ancoragem em Ortodontia. A colocação dos dispositivos em uma região extra-alveolar mandibular permite o uso de parafusos de maior diâmetro que podem ser inseridos paralelamente à inclinação axial de molares inferiores sem interferir com as raízes dos dentes que serão movimentados. Na literatura são descritos diferentes tipos faciais que diferem na predominância em relação ao padrão de crescimento facial vertical ou horizontal configurando conformações ósseas mandibulares distintas entre os tipos faciais. Desta forma, o objetivo deste estudo é avaliar se há diferença na espessura do osso vestibular na região do shelf mandibular entre os tipos faciais. Para este estudo retrospectivo foi selecionada uma amostra composta por 84 tomografias computadorizadas por feixe cônico (TCFC) de indivíduos dos gêneros masculino e feminino, adultos, com idade entre 18 e 40 anos. As imagens foram avaliadas no software Dolphin® (versão 11.0, Dolphin Imaging and Management Solutions, Chatsworth, CA - EUA). As tomografias foram divididas em três grupos de acordo com o tipo facial, determinado por meio de reconstruções bidimensionais em norma lateral para realização do traçado da análise cafalométrica proposta por Bjork-Jarabak, sendo: 28 do tipo facial hiperdivergente (Grupo1), 28 do tipo facial neutro (Grupo 2) e 28 do tipo facial hipodivergente (Grupo 3). Para atender aos objetivos do estudo, as medidas foram realizadas nas seguintes regiões: 1- Vestibular da raiz mesial do primeiro molar inferior dos lados esquerdo e direito; 2 - Vestibular da raiz distal do primeiro molar inferior dos lados esquerdo e direito; 3 - Vestibular entre o primeiro e segundo molar inferior dos lados esquerdo e direito; 4 - Vestibular da raiz mesial do segundo molar inferior dos lados esquerdo e direito; 5 - Vestibular da raiz distal do segundo molar inferior dos lados esquerdo e direito. As medidas foram realizadas a 3, 6 e 9 milímetros a partir da junção amelocementária (JAC) dos primeiros e segundos molares, em direção apical, no corte axial, estendendo-se do ponto médio das raízes mesial e distal até a borda mais externa da cortical óssea alveolar adjacente. Os resultados mostraram que, com relação à idade e gênero, não houve diferença estatisticamente significativa entre os grupos. As medidas do Grupo 1 mostraram que na vestibular da raiz distal do 2º molar a 9mm da JAC apresentaram, em média, valores maiores de 5mm, sendo considerada possível de instação de miniparafuso nesta região, em ambos os lados. No grupo 2 observou-se espaço suficiente para instalação de miniparafuso na vestibular da raiz distal do 2º molar a 6 mm e 9 mm da JAC. Para o Grupo 3 observou-se medidas acima de 5 mm na vestibular da raiz mesial dos segundos molares a 9 mm da JAC e na vestibular da raiz distal a 6 mm e 9 mm da JAC. Baseados nos resultados obtidos, consideramos que existe uma diferença de espessura entre os tipos faciais e que este fator deve ser considerado durante o planejamento para instalação de miniparafusos de ancoragem ortodôntica, no entando para todos os grupos a região mais adequada é na vestibular da raiz distal dos segundos molares inferiores. / Orthodontic anchorage has been of concern to orthodontists since the beginning of orthodontic practice. The transitory anchorage devices (miniscrew) have defined a new concept of anchorage in Orthodontics. Placement of the devices in a mandibular extra alveolar region allows the use of larger diameter screws that can be inserted parallel to the axial inclination of lower molars without interfering with the roots of the teeth that will be moved. The literature describes different facial types that differ in the predominance in relation to the vertical or horizontal facial growth pattern, configuring different mandibular bone conformations between the facial types. Thus, the objective of this study is to evaluate if there is difference in the thickness of the buccal bone in the MBS region between the facial types. For this retrospective study, a sample composed of 84 Cone Beam Computed Tomography (CBCT) of males and females adults, aged between 18 and 40 years, was selected. The images were evaluated in Dolphin® software (version 11.0, Dolphin Imaging and Manegement Solutions, Chatsworth, CA - USA). CT scans were divided into three groups according to the facial type, pre-determined by two-dimensional reconstructions in lateral norm for tracing cephalometric analysis proposed for Bjork-Jarabak\'s: 28 of the hyperdivergent facial type (Group 1), 28 of the neutral facial type (Group 2) and 28 of the hypodivergent facial type (Group 3). To respond the objectives of the study, the measurements were performed in the following regions: 1- Mesial root vestibular of the first lower molar of the left and right sides; 2 - Vestibular of the distal root of the first lower molar of the left and right sides; 3 - Vestibular between the first and second lower molars of the left and right sides; 4 - Vestibular mesial root of the second lower molar of the left and right sides; 5 - Vestibular of the distal root of the second lower molar of the left and right sides. Measurements were made at 3, 6 and 9 millimeters from the amelocemental junction of the first and second molars, apically in the axial cut, extending from the midpoint of the mesial and distal roots to the external border of the alveolar cortical bone adjacent. The results showed that, regarding age and gender, there was no significant statistical difference between the groups. The measurements of Group 1 showed that in the distal root of the 2nd molar to 9mm of the JAC presented, in average, values greater than 5mm, being considered possible of insertion of miniscrew in this region, in both sides. In group 2, sufficient space was observed for the installation of a miniscrew in the distal root of the 2nd molar to 6 mm and 9 mm of the JAC. For Group 3, measurements above 5 mm in the mesial root of the 2nd molars were observed at 9 mm from the JAC and in the distal root of 2nd to 6 mm and 9 mm of the JAC. Based on the results obtained, we consider that there is a difference in thickness between the facial types and that this factor should be considered during the planning for installation of orthodontic miniscrew, whereas for all groups the most suitable region is the vestibular of the distal root of second molars.

The purpose of this project was to evaluate the antioxidant activity in vitro and its effects at the oxidative stability of mechanically deboned poultry meat (MDPM) of five natural extracts. It was studied: the yerba mate (Ilex paraguariensis), the marcela (Achyrocline satureioides), a mixture of yerba mate (50%) and marcela (50%), green tea (Camellia sinensis) and propolis without alcohol. The synthetic antioxidant BHA (Butylated Hydroxianisole) was used as a positive control and the meat treated with no antioxidant was used as negative control. Natural extracts were evaluated in vitro for quantification of phenolic and flavonols total content, for antioxidant activity, by DPPH radicalscavenging, Phosphomolybdenum complex and Reducing Power assay methods. All antioxidants were mixed separately in different and equal portions of mechanically deboned poultry meat, as follow: 0.50% of yerba mate, marcela and the mixture, 0.05% of green tea, 0.10% of própolis without alcohol and 0.02% of BHA. Samples of MDPM were packed and storage at 0 to +4ºC for 10 days. The samples were evaluated each two days and the pH, TBARS and peroxide index were measured, as well as the Total Mesophilic Aerobic counts, Total Coliforms, E. coli, Lactic Bacteria, Clostridium perfringens, Salmonella spp and Staphylococcus aureus. Surface and internal colour ( L*, a*, b*) were measured and pictures of each treatment were done. Green tea extract showed the higher (p<0.05) phenolics contents and the higher (p<0.05) antioxidant activity in vitro compared to the other extracts. Yerba mate extract showed the higher (p<0.05) flavonols content. Propolis without alcohol extract showed the lowest (p<0.05) phenolics, flavonols and antioxidant activity in vitro. Marcela had the best oxidative inhibitory effect at the MDPM, with the lowest TBARS values. Propolis extract showed the best performance for the meat colour stability. Natural antioxidant addition do not interfere at MDPM pH and peroxide values. Salmonella spp was not detected in any of the samples evaluated and the results found to Staphylococcus aureus were in agreement with the Brazilian Mechanically Deboned Meat Legislation. The mixture of extracts showed the lowest (p<0.05) media for Total Mesophilic Aerobic counts. Propolis extract showed the lowest media count for Total Coliforms, E. coli and Clostridium perfringens. Yerba mate extract showed the lowest media count for Lactic Bacteria. The use of natural antioxidants should provide benefits in relation to the MDPM lipid oxidation and the microbiological growth inhibition. More researchs are necessary, looking for a better understanding about the action mechanisms of these extracts. / Este trabalho teve como objetivo avaliar cinco extratos naturais em relação a sua atividade antioxidante in vitro e na Carne Mecanicamente Separada (CMS) de frango. Foram estudadas a erva mate (Ilex paraguariensis), a marcela (Achyrocline satureioides), uma mistura de erva mate (50%) com marcela (50%), o chá verde (Camellia sinensis) e o própolis sem álcool. O antioxidante sintético BHA foi utilizado como controle positivo e o tratamento sem adição de antioxidante como controle negativo. Nos extratos naturais foram identificados o conteúdo total de fenólicos, flavonóides e a atividade antioxidante pelos métodos do DPPH, Fosfomolibdênio e do Poder de Redução. Todos os extratos foram aplicados separadamente em porções distintas e iguais de Carne Mecanicamente Separada (CMS) de frango, sendo os percentuais de aplicação de 0,50% de erva mate, marcela e da mistura, 0,05% de chá verde, 0,10% do própolis sem álcool e 0,02% de BHA. A CMS de frango foi mantida sob refrigeração de 0 a +4ºC durante 10 dias. As amostras foram avaliadas a cada dois dias, em relação ao pH, índice de TBARS, índice de peróxido, em relação a contagem média de Aeróbios Mesófilos Totais, Coliformes Totais, E. coli, Bactérias lácticas, Clostridium perfringens, Salmonella spp e Staphylococcus aureus. A cor objetiva (L*, a*, b*) foi medida na superfície e na parte interna da CMS de frango assim como o registro em foto de cada tratamento. O extrato de chá verde apresentou o maior (p<0,05) conteúdo de fenólicos e a maior (p<0,05) atividade antioxidante in vitro em relação aos demais extratos. O extrato de erva mate apresentou o maior (p<0,05) conteúdo de flavonóides. O extrato de própolis sem álcool apresentou os menores (p<0,05) conteúdos de fenólicos, de flavonóides e a menor atividade antioxidante in vitro. O extrato de marcela teve o melhor efeito na inibição da oxidação lipídica da CMS de frango, apresentando os menores valores médios de TBARS. O extrato de própolis sem álcool manteve por mais tempo a estabilidade da cor da carne. A adição dos antioxidantes naturais não interferiu no pH e nem no índice de peróxido da CMS de frango. Não foi detectada a presença de Salmonella spp e os resultados de Staphylococcus aureus ficaram dentro dos padrões estabelecidos pela Legislação. O tratamento com a mistura de extratos de erva mate e de marcela apresentou a menor (p<0,05) contagem média de Aeróbios Mesófilos Totais em relação aos demais tratamentos. O extrato de própolis sem álcool apresentou a menor contagem média de Coliformes totais, E. coli e Clostridium perfringens. O extrato de erva mate apresentou a menor contagem média de Bactérias lácticas. O uso de antioxidantes naturais pode trazer benefícios em relação a inibição da população microbiana da CMS de frango. Mais estudos são necessários visando um melhor entendimento dos mecanismos de ação desses extratos na carne mecanicamente separada (CMS) de frango.

Made available in DSpace on 2016-08-17T14:52:57Z (GMT). No. of bitstreams: 1 Paulino de Almeida Cantanhede Filho.pdf: 1682767 bytes, checksum: a5fce1801fd45fddf7e98305e0e9b053 (MD5) Previous issue date: 2005-03-14 / Guidelines for evaluation and selection of COTS (Commercial-Off-The-Shelf) products. Comes a methodology for the Development based on COTS (DBC) in the Requirements Engineering, being approached the evaluation phases and selection of DBC. The method is divided in three phases, that are divided in activities orienting by actions that seek to the quality of the information for a socket of decision in an automated and oriented way for defined evaluation criteria during the Requirements Engineering. This approach divide the requirements in three levels: Fundamental, Contractual and Desirable. The functional and no-functional requirements are treated in an equalitarian way. / Este trabalho apresenta diretrizes para avaliação e seleção de produtos COTS (Commercial- Off-The-Shelf). Apresenta-se uma metodologia para o Desenvolvimento Baseado em COTS (DBC) na Engenharia de Requisitos, abordando-se as fases de avaliação e seleção do DBC. O método está dividido em três fases, que por sua vez estão divididas em atividades direcionadas por ações que visam à qualidade das informações para uma tomada de decisão de forma automatizada e orientada por critérios de avaliação definidos durante a Engenharia de Requisitos. Esta abordagem divide os requisitos em três níveis, são eles: Fundamental, Contratual e Desejável. Os requisitos funcionais e não-funcionais são tratados de forma igualitária.

Fler svenskar vill konsumera mer inhemskt producerad fisk. Scandinavian Aquasystems odlar och försöker introducera fisken tilapia på svenska marknaden. Tilapia är en fisk som precis börjat göra intåg i Europa men är stor runtomkring resten av världen. En smakprofil som berättar hur länge produkten är sensoriskt tjänlig kan vara av hjälp. Denna undersökning syftade till att skapa en sensorisk smakprofil för fisken tilapia och till att se hur smakprofilen förändrades vid lagring i vakuumförpackning. För att skapa smakprofilen användes metoden QDA. Resultatet gav många egenskapsord var av vissa kunde klassificeras som färskhetsrelaterade och vissa som förskämningsrelaterade. Det kunde även konstateras att färsk, odlad tilapia har en antydan av saftigare och mer mjäll textur. Vid lagring finns en möjlighet att tilapia får en intensivare smak av dy och metall, samt en intensivare doft av dy. / A large amount of Swedes has a desire to consume more nationally produced fish. Scandinavian Aquasystems produces and tries to introduce tilapia into the Swedish market. As a fish, tilapia has just begun making ways into Europe but is already a big commodity around the rest of the world. In addition, a sensory profile which tells how long the product remains sensorially suitable could be of help. This study aimed to create a sensory profile and to study its inherent effects of vacuum packaging over time. In creating the sensory profile, a QDA method was used. The study resulted in a variance of different attributes which of some could be categorized as either fresh related or spoilage related. It was found that fresh, farmed tilapia carried an indication of having a juicier and more tender texture. With storage there is chance of tilapia getting a more intense flavor of mud and metal, as well as a more intense odor of mud.

Thesis (MSc)--Stellenbosch University, 2011. / ENGLISH ABSTRACT: This study presents an outcrop characterisation and modelling of the excellently exposed Permian Kookfontein Formation of the Ecca Group in the Tanqua-Karoo sub-Basin. The sedimentary modelling (i.e. facies architecture and geometry) and petrophysical characterisation followed a hierarchical and deterministic approach. Quantitative outcrop data were based on the thirteen sedimentary cycles that characterise this stratigraphic succession at the Pienaarsfontein se Berg locality; and these data were analysed using a combination of detailed sedimentary log, gamma ray log and photopanel analysis, as well as petrographic thin-section and grain size-based petrophysical analysis. Based on texture and sedimentary structures, twelve depofacies are recognised which are broadly grouped into four lithofacies associations i.e. sandstone facies, heterolithic facies, mudstone facies and soft-sediment deformation facies; these depofacies and lithofacies form the basic building blocks for the flooding surface-bounded facies succession (i.e. cycle). Also, based on sediment stacking and cycle thickness patterns as well as relative position to the shelf break, the succession is sub-divided into: (1) the lower Kookfontein member (i.e. cycles 1 to 5) exhibiting overall upward thickening and coarsening succession with progradational stacking pattern; representing deposition of mid-slope to top-slope/shelf-margin succession, and (2) the upper Kookfontein member (i.e. cycles 6 to 13) exhibiting overall upward thickening and coarsening succession with aggradational stacking pattern; representing deposition of top-slope/shelf-margin to outer shelf succession. Lateral juxtaposition of observed vertical facies variations across each cycle in an inferably basinwards direction exhibits upward change in features, i.e. decrease in gravity effects, increase in waves and decrease in slope gradient of subsequent cycles. This systematic upward transition in features, grading vertically from distal to proximal, with an overall upward thickening and coarsening progradational to aggradational stacking pattern indicates a normal regressive prograding delta. However, in detail, cycles 1-3 show some anomalies from a purely thickening and coarsening upward succession. Deposition of each cycle is believed to result from: (1) primary deposition by periodic and probably sporadic mouthbar events governed by stream flow dynamics, and (2) secondary remobilisation of sediments under gravity. The facies distribution, architecture and geometry which governs the sedimentary heterogeneity within the deltaic succession is therefore mainly a consequence of the series of mouthbar flooding events governed by sediment supply and base-level changes. These series of flooding events resulted in the delineation of the studied stratigraphic interval into two main parasequence sets, i.e. transgressive sequence set and the overlying regressive sequence set. This delineation was aided through the identification of a maximum flooding surface (i.e. maximum landwards shift in facies) above Cycle 3 in the field. The architecture and geometry of the ensuing deposystem is interpreted to have been a river-dominated, gravitationally reworked and waveinfluenced shelf edge Gilbert-type delta. Widespread distribution of soft-sediment deformation structures, their growth-style and morphology within the studied succession are empirically related to progradation of Gilbert-type mouthbars over the shelf break as well as the slope gradients of the Kookfontein deltaic clinoformal geometry. Analysis of hypothetical facies stacking and geometrical models suggests that the Kookfontein sedimentary cyclicity might not be accommodation-driven but rather sediment supply-driven. The workflow employed for petrophysical evaluation reveals that the distribution of reservoir properties within the Kookfontein deltaic sandbody geometries is strongly influenced both by depositional processes and by diagenetic factors, the latter being more important with increased burial depth. The reservoir quality of the studied sandstones decreases from proximal mouthbar sands, intermediate delta front to distal delta front facies. The major diagenetic factors influencing the reservoir quality of the studied sandstones are mechanical compaction, chemical compaction (pressure solution) and authigenic pore-filling cements (quartz cement, feldspar alteration and replacement, calcite cement, chlorite and illite). Mechanical compaction was a significant porosity reducing agent while cementation by authigenic quartz and clay minerals (i.e. illite and chlorite) might play a major role in permeability distribution. The porosity-permeability relationship trends obtained for the studied sandstones show that there is a linear relationship between porosity and permeability. The relative timing of diagenetic events as well as the percentages of porosity reduction by compaction and cementation indicates that compaction is much more responsible for porosity reduction than cementation. The described internal heterogeneity in this work is below the resolution (i.e. mm-scale) of most conventional well-logs, and therefore could supplement well-log data especially where there is no borehole image and core data. The combination of ‗descriptive‘ facies model and schematic geological model for this specific delta, and petrophysical characterisation make the results of this study applicable to any other similar ancient deposystem and particularly subsurface reservoir analogue. / AFRIKAANSE OPSOMMING: Hierdie studie bied ‘n dagsoomkarakterisering en -modellering van die duidelik blootgelegde Permiese Kookfontein-formasie van die Ecca-groep in die Tankwa-Karoo-subkom. Wat die sedimentêre modellering (d.w.s. fasiesargitektuur en -geometrie) en petrofisiese karakterisering betref is ‘n hiërargiese en deterministiese benadering gevolg. Kwantitatiewe dagsoomdata is gebaseer op dertien sedimentêre siklusse wat hierdie stratigrafiese opeenvolging in die Pienaarsfontein se Berg-lokaliteit kenmerk; en die data is geanaliseer met behulp van ‘n kombinasie van gedetailleerde sedimentêre seksie, gammastraal-profiel en fotopaneelanalises, asook petrografiese slypplaatjie- en korrelgrootte-gebaseerde petrofisiese analises. Op grond van tekstuur en sedimentêre strukture is twaalf afsettingsfasies onderskei wat rofweg in vier assosiasies van litofasies gegroepeer kan word: sandsteenfasies, heterolitiese fasies, moddersteenfasies en sagtesediment-deformasiefasies. Hierdie afsettingsfasies en litofasies vorm die basiese boustene vir die fasiesopeenvolging (d.w.s. siklus) wat oorstromingsoppervlakgebonde is. Verder word die opeenvolging aan die hand van sedimentstapeling en skilusdiktepatrone, asook relatiewe posisie tot die rakbreuk, in die volgende onderverdeel: (1) die benede-Kookfontein-deel (d.w.s. siklus 1 tot 5), wat in die geheel ‘n opwaartse verdikkings- en vergrowwingsopeenvolging met ‘n progradasiestapelpatroon vertoon en die afsetting van middelhelling-tot-boonstehelling- of rakrand-opeenvolging verteenwoordig, en (2) die benede-Kookfontein-deel (d.w.s. siklus 6 tot 13) wat in die geheel ‘n opwaartse verdikkings- en vergrowwingsopeenvolging met ‘n aggradasiestapelpatroon vertoon en die afsetting van boonste helling- of rakrand-tot-buiterakopeenvolging verteenwoordig. Die laterale jukstaposisie van waargenome vertikale fasiesvariasies oor elke siklus heen, in ‘n afleibare komwaartse rigting, vertoon opwaartse verandering wat kenmerke betref, naamlik afname in gravitasiegevolge, toename in golwe en afname in die hellinggradiënt van daaropvolgende siklusse. Hierdie stelselmatige opwaartse oorgang van kenmerke, wat vertikaal van distaal tot proksimaal gradiënteer en in die geheel opwaartse verdikking en vergrowwing in ‘n progradasie-tot-aggradasie-stapelpatroon vertoon, dui op ‘n normale regressiewe progradasiedelta. Van naby beskou, vertoon siklus 1-3 egter bepaalde afwykings van ‘n suiwer opwaartse verdikkings- en vergrowwingsopeenvolging. Die afsettings van elke siklus is vermoedelik die gevolg van: (1) primêre afsetting deur periodieke en waarskynlik sporadiese mondversperringsgebeure wat deur stroomvloeidinamika beheer word, en (2) sekondêre hermobilisering van sedimente deur gravitasie. Die fasiesverspreiding, -argitektuur en -geometrie wat die sedimentêre heterogeniteit in die deltaïese opeenvolging beheer, is dus hoofsaaklik ‘n gevolg van die reeks oorstromingsgebeure by die mondversperring, wat deur sedimentvoorsiening en basisvlakveranderings beheer word. Hierdie reeks oorstromingsgebeure het gelei tot die delineasie van die bestudeerde stratigrafiese interval volgens twee hoofparasekwensie stelle, naamlik die transgressiewe opeenvolgings- en die oordekkende, regressiewe opeenvolgingsgroep. Dié delineasie word ondersteun deur die feit dat ‘n maksimum oorstromingsoppervlak (d.w.s. maksimum landwaartse verskuiwing in fasies) bo siklus 3 in die veld uitgeken is. Die argitektuur en geometrie van die daaropvolgende afsettingstelsel word geïnterpreteer as behorende tot ‘n Gilbert-rakranddelta wat deur ‘n rivier gedomineer, deur gravitasie herbewerk en deur golfwerking beïnvloed is. Die wye verspreiding van sagtesediment-deformasiestrukture, en die groeiwyse en morfologie daarvan binne die bestudeerde opeenvolging, is empiries verwant aan die progradasie van Gilbertmondversperrings oor die rakbreuk heen, asook aan die hellinggradiënte van die Kookfontein-deltaïese, klinoformele geometrie. Die analise van hipotetiese fasiesstapeling en geometriese modelle dui daarop dat die Kookfontein-sedimentêre siklisiteit dalk nie deur akkommodasieruimte gedryf word nie, maar deur sedimentvoorsiening. Die werkvloei wat vir petrofisiese evaluering gebruik is dui daarop dat die verspreiding van reservoir-eienskappe in die Kookfontein- deltaïese sandliggaam geometries sterk beïnvloed word deur afsettingsprosesse en diagenetiese faktore. Die diagenetiese faktore word belangriker op groter begrawing diepte. Die reservoir-aard van die bestudeerde sandgesteentes neem algaande af van proksimale mondversperring-sandsoorte tot intermediêre deltafront tot distale deltafrontfasies. Die hoof-diagenetiese faktore wat die reservoir-kenmerke van die bestudeerde sandsteensoorte beïnvloed is meganiese verdigting, chemiese verdigting (oplossingsdruk) en outigeniese porievullingsement (kwartssement, veldspaatomsetting en -vervanging, kalsietsement, chloriet en illiet). Meganiese verdigting is ‘n beduidende poreusheidreduseermiddel, terwyl sementering deur outigeniese kwarts- en kleiminerale (d.w.s. illiet en chloriet) moontlik ‘n belangrike rol by permeabiliteitsverspreiding kan speel. Die poreusheid-permeabiliteit-verhoudingstendense wat bekom is vir die bestudeerde sandsteensoorte dui daarop dat daar ‘n lineêre verhouding tussen poreusheid en permeabiliteit bestaan. Die relatiewe tydberekening van diagenetiese gebeure, asook die persentasie poreusheidvermindering deur verdigting en sementering, dui daarop dat verdigting baie meer as sementering tot poreusheidvermindering bydra. Die interne heterogeniteit wat in hierdie werk beskryf word, is onder die resolusie (d.w.s. mm-skaal) van die meeste konvensionele boorgatopnames, en kan dus boorgatopnamedata aanvul, veral waar daar geen boorgatafbeelding en kerndata bestaan nie. Die kombinasie van die 'deskriptiewe‘ fasiesmodel en skematiese geologiese model vir hierdie spesifieke delta, asook petrofisiese karakterisering, beteken dat die resultate van hierdie studie op enige ander soortgelyke antieke afsettingstelsels toegepas kan word, maar veral op suboppervlakreservoir-analoogstelsels.

A comprehensive investigation into the relationship between physical forcing and sus- pended particles in the shallow shelf region of the Western English Channel has been conducted, in order to evaluate the temporal dynamics of suspended particle populations. Measurements were taken across tidal cycles and seasons at station L4, part of the Western Channel Observatory (WCO), using the combination of a free-fall microstructure profiler and holographic imaging. Confirmation that L4 is weakly stratified is given, and that the formation of the seasonal thermocline is substantially altered by the spring-neap cy- cle. Stratification is variable and prone to periodic and partial erosion from atmospheric forcing during any point in any season. L4 undergoes moderate turbulent dissipation, principally as a result of tidal forcing. Typically, values of ε do not exceed 10−4 W kg−1 . L4 also exhibits tidal asymmetry, chiefly in response to stratification which, albeit weak, is frequently able to suppress turbulence when generated from the sea bed. The potential energy anomaly is small at L4, as expected for a weakly-stratified environment. Maxi- mum values in summer were shown to not exceed 50 J m−3 . Values of bed stress, τ0 , are rarely greater than around 0.18 N m−2 . Nonetheless, the critical erosion threshold falls below this, and is therefore smaller than that observed in similar locations around the UK. Seasonality in the amount of material resuspended from the seabed is important at L4. The presence of certain biological particles strongly influence particle size and may also determine if a given particle is lifted from the bed. Particles ≥ 200 μm are relatively rare, the site is dominated by particles smaller than this value in line with many other UK sites. Under certain conditions the theoretical maximum limit of particle size, the Kolmogorov length scale, does not hold and many examples of occasions when this threshold is exceeded are shown. This may generate important consequences in subsequent work undertaken at this site and other temperate shelf locations globally, particularly as these results indicate that maximum particle size appears to be governed less by the size of the local turbulent eddies and more by the presence of biological particles. This is another key seasonal component to particle dynamics in the Western English Channel. Phytoplankton populations are readily advected into and out of the L4 site, calling into question the current sampling strategy of the WCO to rely exclusively upon point measurements. Small increases in atmospheric forcing have the ability to rapidly disperse patches of phytoplankton, possibly to the point of cell mortality. Traditional sampling techniques for assessing zooplankton density have been shown to radically underestimate the number of animals present at L4, which will increase error estimates on current ecosystem models.

Zooplankton assemblages were examined from waters off the west coast of Scotland encompassing the Firths of Lorn and Clyde, the North Channel, and the Malin Shelf. Size fractionated samples (coarse, >1000μm; medium, 1000μm-330μm; fine, 330μm-180μm) were collected with a submersible pump from 10m and 30m depth in March (1987) and May (1986) providing a composite picture of the fauna in early and late spring conditions, respectively. The feasibility of using image analysis as a method for processing zooplankton samples was examined. Although a programme was successfully operated to obtain individual measurement data, much work is still required before a fully automated programme for routine use by planktologists is available. Total zooplankton numbers and biomass, and species distributions and relative abundances were examined. Species assemblages were identified using multivariate analyses. Biomass and abundance spectra by size were examined for the major station groupings. In general, meroplankton dominated the fauna in the Firth of Lorn while large numbers of Calanus spp. occurred in the Firth of Clyde. Small copepods such as Oithona spp. were characteristic of the assemblage on the Malin Shelf. Salinity, followed by temperature, showed the strongest association with the observed station clusters. Chlorophyll a and depth did not generally appear to influence station groupings. The potential for the mixing and exchange of zooplankton between the regions of the study area was evaluated. The results suggest that zooplankton may be entrained from the Firth of Clyde by the Scottish Coastal Current during the spring period. The Malin Shelf may also be an important source of zooplankton for the Firth of Lorn during winter months when an onshore flow of Atlantic water occurs.

Four modern shoals on the Louisiana continental shelf are proposed to have formed through transgression, marine reworking, and submergence of Mississippi River deltaic lobes. However, one of these shoals, the St. Bernard Shoals, is dissimilar to the other shoals in morphology and stratigraphy. Understanding the processes that lead to these differences resulted in the development of a wholly new model for subaqueous shoal evolution. The results of this study suggest that the St. Bernard Shoals are transgressive remnants of a near shelf-edge delta lobe that was transgressed and truncated by marine processes after fluvial abandonment. Subsequent to truncation, the shoals formed through subaqueous excavation and reworking of coarse grained sediment contained within underlying distributary channels by hurricane related marine currents. As a result the shoals are bound at their base by a ravinement surface and lie directly upon progradational facies associated with previously unrecognized southern progradation of the La Loutre distributary network.

A formação de águas profundas na Antártica afeta diretamente o clima global, uma vez que este processo conecta os ramos superior e inferior da circulação termohalina global (MOC). Avaliar os impactos das mudanças climáticas nestes processos é importante para compreensão do transporte global de calor pelos oceanos e para realização de projeções climáticas. Aplicando a forçante interanual Coordinated Ocean-Ice Reference (CORE), foi realizada uma simulação de 60 anos (1948-2007) utilizando o ROMS com módulos de gelo marinho e plataforma de gelo ativos. Uma rodada preliminar de 100 anos foi realizada com forçante do ano normal CORE, para gerar campos estáveis de inicialização da rodada interanual. Para ambos os experimentos adotou-se uma grade circumpolar periódica com resolução variável, alcançando cerca de 5 km na borda sul. Para investigar as massas de água foi aplicada a Análise Multiparamétrica Ótima - OMP. As principais massas de água do Mar de Ross foram identificadas: Água de Superfície Antártica (AASW), Água Circumpolar Profunda (CDW), Água de Fundo Antártica (AABW) e Água de Plataforma (SW), posteriormente separadas em Água da Plataforma de Gelo (ISW) e Água de Plataforma de Alta Salinidade (HSSW). Os resultados são consistentes com observações prévias (Bergamasco, 2002; Orsi & Wiederwohl, 2009; Budillon, 2011). A simulação interanual sugere que o Oceano Austral vem sofrendo um processo de aquecimento e diminuição de salinidade. Houve um aumento do calor advectado pela CDW e uma diminuição da salinidade das águas de plataforma e da AABW, consistente com as observações de Johnson & Doney (2006). A capacidade do modelo regional ROMS de reproduzir as águas de plataforma ISW, HSSW e a AABW é uma importante contribuição para estudos climáticos, visto que os modelos globais não conseguem representar tais processos. A inclusão de parametrizações explícitas dos processos de gelo marinho e plataforma de gelo capacita o ROMS para reproduzir os processos associados a criosfera, possibilitando a obtenção de projeções mais realísticas. / Dense water formation around Antarctica is recognized as a significant process that significantly impacts the global climate, since that\'s where the linkage between the upper and lower limbs of Global Thermohaline Circulation takes place. Assessing whether these processes may be affected by rapid climate changes and all the eventual feedbacks is crucial to fully understand the ocean heat transport and to provide quality future climate projections. Applying the Coordinated Ocean-Ice Reference (CORE) interannual forcing we have run a 50-year simulation (1948-2007) using ROMS with a new sea ice/ice shelf thermodynamics module. Another 100-year simulation forced with CORE normal year was previously run to provide stable starting fields. The normal year consists of single annual cycle of all the data that are representative of climatological conditions over decades and can be applied repeatedly for as many years of model integration as necessary. The 60-year forcing has interannually varying data from 1948 to 2007, which allows validation of model output with ocean observations. Both experiments employed a periodic circumpolar variable resolution grid reaching less than 5 km at the southern border. By applying the OMP water masses separating scheme, we were able to identify the main Ross Sea water masses: Antarctic Surface Water (AASW), Circumpolar Deep Water (CDW), Antarctic Bottom Water (AABW) and Shelf Water (SW), further separated into Ice Shelf Water (ISW) and High Salinity Shelf Water (HSSW). Results are consistent with previous observational studies (Bergamasco, 2002; Orsi & Wiederwohl, 2009; Budillon, 2011). The interannual simulation indicates that the Southern Ocean is becoming warmer and less salty. The CDW poleward heat transport increased while shelf waters salinity as well as the AABW salinity decreased during the simulation period, consistent with Johnson & Doney (2006), who have reported the export of less dense AABW. ROMS capability to represent ISW, HSSW and AABW is an important contribution to climate studies, since IPCC class models seem unable to provide reliable representations of such important processes, which may lead to projections of more realistic scenarios. This is significantly improved in this study by including more explicit sea ice/ice shelf parameretization. ROMS is able to reproduce cryosphere-linked mechanisms of dense water formation around Antarctica.

A dinâmica sedimentar sobre um trecho da plataforma continental leste brasileira foi analisada através da abordagem combinada entre a análise do clima de ondas (WAVEWATCH III), modelagem da propagação das ondas para águas rasas (MIKE 21 SW) e aplicação de equações que estimam o transporte de partículas em função da tensão de cisalhamento causada pelas ondas sobre o fundo marinho. Assim, baseado no clima de ondas da região, são estimados os potenciais de mobilidade sedimentar como resposta a diversas condições forçantes. O clima de ondas em frente a Ilhéus é caracterizado pela predominância de ondas do quadrante leste (60%), com 20% provenientes de sudeste e 15% de sul. Em frente a Caravelas, o espectro de ondas é caracterizado por 40% de ondas de leste, 15% do quadrante sudeste e 35% provenientes de sul. O clima de ondas é influenciado pelas descontinuidades na largura da plataforma continental nesse trecho da costa, atenuando a influência das ondas de swell provenientes do quadrante sul em frente a Ilhéus. Os resultados indicam mobilidade sedimentar até 50 m de profundidade na plataforma de Ilhéus e até 20 m na plataforma de Abrolhos ao longo do ano, no entanto, eventos esporádicos mais energéticos são capazes de mobilizar sedimentos até cerca de 200 m de profundidade na plataforma de Ilhéus e até 100 m na plataforma de Caravelas. A mobilidade de partículas de maiores dimensões, como os rodolitos da plataforma de Abrolhos, maior campo de rodolitos conhecido do mundo, foi analisada através do parâmetro de Shields, que leva em consideração tamanho e densidade das partículas. Os resultados indicam que a mobilidade dos rodolitos de Abrolhos está principalmente condicionada pela ocorrência de eventos mais energéticos, especialmente no outono. As regiões com maior mobilidade são a porção norte, próxima a quebra da plataforma e a porção centro-sul da plataforma, ambas com profundidades entre 20 e 40 m. O detalhamento do conhecimento sobre o transporte de sedimentos na plataforma continental leste brasileira contribui para o entendimento na dinâmica sedimentar na região. A morfologia complexa da plataforma, combinada com o clima de ondas incidente, são fatores fundamentais no potencial de mobilização de sedimentos. / The sedimentary dynamics on a stretch of the Brazilian continental shelf was analyzed through a combined approach between wave climate analysis (WAVEWATCH III), shallow water wave propagation modeling (MIKE 21 SW) and equations estimating the transport of particles as a function of bed shear stress by the waves. Thus, based on the wave climate of the region, sediment mobility potentials are estimated in response to several forcing conditions. Wave climate is characterized by the predominance of east waves in front of Ilhéus (60%), 20% from southeast quadrant and 15% from south. In front of Caravelas a wave spectrum is characterized by 40% from east quadrant, 15% from southeast and 35% from south. Continental shelf width discontinuity influences wave climate at Ilhéus, attenuating waves from south quadrant. The results indicate sediment mobility up to 50 m depth on the Ilhéus shelf and up to 20 m on the Abrolhos shelf along the entire year; however, more sporadic energetic events are able to mobilize sediments up to 200 m depth on the Ilhéus shelf and up to 100 m on the Caravelas shelf. Larger particle mobility, such as the rhodoliths of the Abrolhos shelf, the largest known rhodolite field in the world, was analyzed using the Shields parameter, which takes into account particle size and density. The results indicate that the mobility of Abrolhos rhodolites is mainly conditioned by the occurrence of more energetic events, especially in autumn. The regions with the greatest mobility are the northern portion, near the shelf break and the center-south portion of the shelf, both with depths between 20 and 40 m. The detailed knowledge on sediment transport in the Brazilian continental shelf contributes to the understanding of sedimentary dynamics in the region. The complex morphology of the continental shelf, combined with the incident wave climate, are fundamental factors in sediment mobilization potential.