956 resultados para Made-up story
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Background Long-term treatment of primary HIV-1 infection (PHI) may allow the immune reconstitution of responses lost during the acute viremic phase and decrease of peripheral reservoirs. This in turn may represent the best setting for the use of therapeutic vaccines in order to lower the viral set-point or control of viral rebound upon ART discontinuation. Methods We investigated a cohort of 16 patients who started ART at PHI, with treatment duration of ≥4 years and persistent aviremia (<50 HIV-1 copies/ml). The cohort was characterized in terms of viral subtype, cell-associated RNA, proviral DNA and HLA genotype. Secretion of IFN-γ, IL-2 and TNF-α by CD8 T-cells was analysed by polychromatic flowcytometry using a panel of 192 HIV-1-derived epitopes. Results This cohort is highly homogenous in terms of viral subtype: 81% clade B. We identified 44 epitope-specific responses: all patients had detectable responses to >1 epitope and the mean number of responding epitopes per patient was 3. The mean frequency of cytokines-secreting CD8 T-cells was 0.32%. CD8 T-cells secreting simultaneously IFN-γ, IL-2 and TNF-α made up for about 40% of the response and cells secreting at least 2 cytokines for about 80%, consistent with a highly polyfunctional CD8 T-cell profile. There was no difference in term of polyfunctionality when HLA restriction, or recognized viral regions and epitopes were considered. Proviral DNA was detectable in all patients but at low levels (mean = 108 copies/1 million PBMCs) while cell-associated mRNA was not detectable in 19% of patients (mean = 11 copies/1 million PBMCs when detectable). Conclusion Patients with sustained virological suppression after initiation of ART at PHI show polyfunctional CD8 T-cell and low levels of proviral DNA with an absence of residual replication in a substantial percentage of patients. The use of therapeutic vaccines in this population may promote low level of rebound viremia or control of viral replication upon ART cessation.
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The Oligocene deposits of Montgat are integrated in a small outcrop made up of Cenozoic and Mesozoic rocks located in the Garraf-Montnegre horst, close to the major Barcelona fault. The Oligocene of Montgat consists of detrital sediments of continental origin mainly deposited in alluvial fan environments; these deposits are folded and affected by thrusts and strike-slip faults. They can be divided in two lithostratigraphic units separated by a minor southwest-directed thrust: (i) the Turó de Montgat Unit composed of litharenites and lithorudites with high contents of quartz, feldspar, plutonic and limestone rock fragments; and (ii) the Pla de la Concòrdia Unit composed of calcilitharenites and calcilithorudites with high contents of dolosparite and dolomicrite rock fragments. The petrological composition of both units indicates that sediments were derived from the erosion of Triassic (Buntsandstein, Muschelkalk and Keuper facies), Jurassic and Lower Cretaceous rocks (Barremian to Aptian in age). Stratigraphic and petrological data suggest that these units correspond to two coalescent alluvial fans with a source area located northwestwards in the adjoining Collserola and Montnegre inner areas. Micromammal fossils (Archaeomys sp.) found in a mudstone layer of the Pla de la Concòrdia Unit assign a Chattian age (Late Oligocene) to the studied materials. Thus, the Montgat deposits are the youngest dated deposits affected by the contractional deformation that led to the development of the Catalan Intraplate Chain. Taking into account that the oldest syn-rift deposits in the Catalan Coastal Ranges are Aquitanian in age, this allows to precise that the change from a compressive to an extensional regime in this area took place during latest Oligocene-earliest Aquitanian times. This age indicates that the onset of crustal extension related to the opening of the western Mediterranean Basin started in southern France during latest Eocene-early Oligocene and propagated southwestward, affecting the Catalan Coastal Ranges and the northeastern part of the Valencia trough during the latest Chattian-earliest Aquitanian times.
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This is the second issue of Geologica Acta dedicated to the memory of Professor Francesc Calvet, who passed away in January 2002. Francesc was a man with great human qualities, a distinguished scientist and an inspiring teacher who was held in high esteem by all those who knew him. The first volume contained six papers on specific areas of research in which Francesc was engaged, and a biography (Geologica Acta, volume 2, Nº 4, 2004). This second volume is made up of contributions by colleagues and former students who wish to salute Francesc Calvet as an outstanding geologist and teacher. The papers included in this volume are also subjects in which Francesc was closely involved.
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The properties of CD8 T-cells requiredfor protection from infectiousdisease and cancer are only partiallycharacterized, and only limited data isavailable regarding T-cell clonotypes.It has been proposed that dominantT-cell clonotypes may have higherprotective potential than their nondominantcounterparts. Our objectiveswere to assess memory andeffector functions, stage of differentiationand clonotype selection of tumor-reactive T lymphocytes followingpeptide vaccination in melanomapatients.We also characterized dominantversus non-dominant clonotypesto further understand the in vivo functionof these T-cells based on theirprevalence. Using a novel single-cellapproach for simultaneous ex vivomolecular and functional analysis, wereport the preferential selection andexpansion of several tumor-specificco-dominant clonotypes of intermediateto high frequencies, irrespectiveof whether native or analog peptidewas used for vaccination. Theseclonotypes made up 40 - 95% of thedifferentiated "effector-like" T-cells,but only 25% of the less-differentiated"effector-memory" cells. Bothsubsets also contained non-dominantT-cell clonotypes, but these were significantlymore frequent in the lessdifferentiatedcells. Thus, cell differentiationwas clonotype-dependent.Surprisingly however, the acquisitionof memory and effector T-cell propertieswas clonotype independent, as wefound similar functional profiles indominant and low/ non-dominantT-cell clonotypes. In contrast to analogpeptide vaccination, native peptidevaccination induced T-cell functionsthat were more comprehensive,with more pronounced effector functionscombined with memory cellproperties. In summary, this study revealsthat T-cell functions are determinedprimarily by the antigen andthe stage of T-cell differentiation, butare similar in dominant and non-dominantclonotypes participating in aCD8 T-cell response. The identifiedclonotypic basis of T-cell responsescontributes to the rational developmentof vaccines.
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Revisió sobre l’eficàcia de les intervencions dirigides a cuidadorsinformals de malalts amb demència per a reduir els nivells de morbiditatpsicològicaAntecedentsL’envelliment de la població està relacionat amb l’augment de la prevalença dedemències tals com la malaltia d’Alzheimer. El caràcter progressiu, incapacitanti irreversible de la malaltia d’Alzheimer comporta dependència i demanda,obligant l’aparició d’un cuidador informal per cobrir les necessitats del malalt.Amb l’evolució de la malaltia, augmenta l’exigència de les cures i el cuidador esveu en risc de patir alteracions a qualsevol nivell, principalment a nivellpsicològic.Objectius1. Avaluar l’efectivitat de les intervencions dirigides a cuidadors informals depersones amb demència per a reduir la morbiditat psicològica, segons latipologia de les intervencions i els seus components.2. Avaluar l’efectivitat de les intervencions dirigides a cuidadors informals depersones amb demència per a reduir la morbiditat psicològica, segons lescaracterístiques sociodemogràfiques del cuidador i la persona que rep lescures, el tipus de càrrega i els instruments de mesura.Material i mètodesEs va realitzar una revisió bibliogràfica en les bases de dades: MEDLINEPubMed, CSIC-IME, CUIDEN i Biblioteca Cochrane Plus sobre lesintervencions dirigides a cuidadors informals de demència o Alzheimerd’estudis publicats entre el gener de 2002 i febrer de 2013. Els criteris d’inclusióvan ser: cuidadors informals que convisquessin amb la persona a qui donen lescures i sense remuneració econòmica, persones amb demència o Alzheimer noinstitucionalitzades, intervencions comparades entre un grup experimental i ungrup control, prioritat per revisions sistemàtiques i metanàlisis. La mostra finalla van composar 7 estudis.ResultatsLes diferents intervencions analitzades van mostrar dades estadísticamentsignificatives tot i produir efectes discrets en les diferents variables demorbiditat psicològica. Les intervencions psicoeducatives i les intervencionsdirigides als pacients van resultar efectives en la millora de la sensació debenestar i la simptomatologia del malalt. Les intervencions psicològiques vanincidir en la sobrecàrrega i la depressió. Les intervencions de suport vanproduir un augment dels coneixements, habilitats i de la xarxa social delcuidador. El dia de descans va disminuir l’estrès, l’ansietat i la càrrega objectivaperò els efectes van ser a curt termini. Les intervencions múltiplesestructurades van mostrar una disminució del risc d’institucionalització. Lesintervencions centrades en la resolució de problemes, superiors a 6 sessions oaquelles que havien realitzat seguiment, van mostrar efectes a llarg termini finsals 12 mesos. Altres intervencions pràctiques com les realitzades al domicili oamb tecnologia, no van mostrar suficient evidència científica. El sexe i l’edat delcuidador així com la relació de parentesc amb el malalt van mostrar diferènciesen els efectes de les intervencions.ConclusionsLes intervencions s’han de planificar en funció de les necessitats del cuidadorja que no hi ha cap intervenció que incideixi en totes les variables de morbiditatpsicològica. La variabilitat de tipologia i composició de les intervencions, lesdiferències sociodemogràfiques del cuidador i la persona que rep les cures i lescaracterístiques dels estudis influeixen en l’heterogeneïtat de resultats de larevisió. Aquests fets limiten la contundència de resultats pel que cal seguirinvestigant
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Intermediate phenomena of reality present particular characteristics of systemic self-organization, multilevel interrelations, recursivity, emergence of new «objects» with properties different from those of the elements that form them, and evolutionary dynamics, that probably need the formulation of new theoretical concepts and different paradigm principles. The sciences or perspectives of complexity, or the «complex» thinking, try to respond adequately to this complexity of reality. This approach adopts a multidimensional, integrated and dynamic view of reality: the world is made up of overlapping levels of different elements which produce new properties or new organizations at higher levels. If we conceive what we call languages as simple and decontextualized objects, we can understand some of the more mechanical aspects but we will ignore their conditions of existence, functionality, maintenance, variation, change and extinction.
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El propòsit del Treball de Fi de Grau és dissenyar un document que serveixi als usuaris del Chronojump Boscosystem per aprendre a utilitzar-lo i treure’n el màxim rendiment. Previ a l’elaboració d’aquest, s’ha requerit un treball de documentació teòrica, fet a través de la revisió bibliogràfica i entrevistes a experts en preparació física dintre del món de l’entrenament esportiu, procés que ha servit per a establir les bases i els fonaments del dossier didàctic. Aquest últim està compost per deu pràctiques on, en cadascuna d’elles, es treballen aspectes concrets del programa Chronojump. Cada una d’aquestes consta d’una primera part més teòrica on es defineixen els aspectes a tractar, seguit de la seqüència de passos a fer per a portar a terme la pràctica i, finalment, deu preguntes tipus test per a saber si s’ha comprès la informació donada i el funcionament del programa. En les pràctiques on s’ha de passar algun test, s’afegeix també un suport audiovisual per tal de deixar clar l’execució i la tècnica correcta de la prova en qüestió.
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En aquest projecte es reflexiona sobre l’ensenyament de les ciències al parvulari i com els infants aprenent conceptes relacionats amb el regne animal. La ciència escolar classifica la gran diversitat d’espècies que formen aquest regne en dos grans blocs, els vertebrats i els invertebrats, però en els patrons que ens ofereixen els animals per descobrir a ull nu aquestes particularitats són molt complexes d’observar. La visió que tenen els infants de parvulari sobre els animals del seu entorn sovint és molt allunyada de la realitat i els alumnes es creen concepcions alternatives per entendre els animals que observen. En l’estudi es realitza un recull de dades, a l’inici i el final d’una unitat didàctica, analitzant les representacions i les diferents formes de classificació dels animals de l’entorn que utilitzen els infants. Les conclusions són una reflexió sobre el perquè d’aquests coneixements alternatius i la manera de com aconseguir un canvi conceptual.
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L’obra de M. Àngels Anglada constitueix un tramat complex de lectures i influències que s’interpreta a través de nivells de significació i d’interessos que s’entrecreuen. Com a pilar que sosté tot aquest corpus hi ha un gran bagatge clàssic i una vasta formació literària que, juntament amb l’experiència vital i el posicionament ètic de l’autora, proporcionen les claus de lectura dels seus llibres. Partint d’aquesta idea, l’article aprofundeix en els tres aspectes que considerem eixos fonamentals de l’obra de l’escriptora: els elements autobiogràfics, l’art i el compromís social.
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Los acontecimientos pueden contribuir al desarrollo turístico de una ciudad y beneficiar a sus habitantes y empresas. Sin embargo, para poder diseñar los acontecimientos correctamente, es necesario comprender qué características determinan su impacto económico. Esta investigación pretende contribuir a tal entendimiento mediante la estimación y comparación del impacto económico de tres acontecimientos. Para estimar el impacto económico adoptamos un modelo básico de tres factores: (1) número de visitantes por (2) gasto medio por turista por (3) multiplicador. Primero estimamos el número de visitantes particulares y profesionales mediante diversos sistemas de conteo, encuestas personales e información suministrada por el organizador de los eventos. En segundo lugar, obtuvimos los importes y componentes del gasto de los visitantes por medio de una encuesta; también contamos los gastos de organización de los eventos a partir de sus respectivos presupuestos. Y, tercero, utilizamos multiplicadores de tablas input-output para analizar el impacto de los gastos directos sobre la producción, el valor añadido y el empleo y su distribución entre sectores económicos. Además, calculamos y comparamos ratios de rentabilidad de los tres eventos y dimos recomendaciones para aumentar su impacto económico.
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Mayflies (Ephemeroptera) are known to have short adult life-spans. Adults are unable to feed, and they utilize reserves stored during their aquatic larval stage. Energy reserves (fat, glycogen, and free sugars) of mature larvae, subimagoes and imagoes of both sexes of Siphlonurus aestivalis Eaton were compared. All the stages of both sexes had low glycogen and free sugar contents, and the only significant change occurred during the transformation of the mature larva to subimago when almost all the reserves of free sugars were used up. Glycogen and free sugars may serve as energy sources permitting individuals to swim and fly out of the water during emergence. Fat made up most of the energy reserves of mature larvae and was the main source of energy used during the final development of both sexes. Young adult males had high fat reserves which they used as a source of energy for their swarming flights. In contrast, females did not seem to use a significant amount of fat for flight. This difference is probably related to the different mating strategies of the sexes in this species. Males perform long flights waiting for females, whereas females perform only brief flights to mate and reproduce.
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A water quality resource concern has come to the forefront in the Upper Miller Creek watershed in Black Hawk County after five to seven inches of rain fell on the area on May 22nd and 23rd of 2004 and unprecedented amounts of soil and organic debris were washed from cultivated areas, clogging most culverts and roadside ditches. The quantity of soil deposited in ditches gave a good indication of the amounts that were transported into the stream. The estimated total cost to Black Hawk County for cleanup and repair within the road right-of-way was $345,000. There were undetermined environmental costs incurred when the incredibly high volumes of soil washed from the fields into Miller Creek which flows directly into the Cedar River that is identified by the Department of Natural Resources as an impaired water body. The Upper Miller Creek Watershed Project is an innovative, collaborative project intended to meet a specific need identified by a local steering committee made up of concerned community agencies and local landowners. Led by the Soil and Water Conservation District and the Black Hawk County Board of Supervisors, the Miller Creek Watershed Project seeks to reduce soil erosion, improve water quality, and reduce county road infrastructure cost by implementing conservation practices, reducing nutrient and pesticide use and improving wildlife habitat.
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This work presents geochemistry and structural geology data concerning the low enthalpy geothermal circuits of the Argentera crystalline Massif in northwestern Italian Alps. I n this area some thermal springs (50-60 degreesC), located in the small Bagni di Vinadio village, discharge mixtures made up of a Na-Cl end-member and a Na-SO4 component. The latter is also discharged by the thermal springs of Terme di Valdieri located some kilometres apart within the same tectonic complex. Both end-members share the same meteoric origin and the same reservoir temperature, which is close to 150 degreesC. Explanations are thus required to understand how they reach the surface and how waters of the same origin and circulating in similar rocks can attain such different compositions. Sodium-sulphate waters discharged at both sites, likely represent the common interaction product of meteoric waters with the widespread granitic-migmatitic rocks of the Argentera Massif, whereas Na-CI waters originate through leaching of mineralised cataclastic rocks, which are rich in phyllosilicatic minerals and fluid inclusions, both acting as Cl- sources. Due to the relatively low inferred geothermal gradient of the region, -25C/km, meteoric waters have to descend to depths of 5.5-6 km to attain temperatures of similar to 150 degreesC. These relevant depths can be reached by descending meteoric waters, due to the recent extensional stress field, which allows the development of geothermal circulations at greater depths than in other sectors of the Alps by favouring a greater fractures aperture. The ascent of the thermal waters rakes place along brittle shear zones. In both sites, the thermal waters emerge at the bottoms of the valleys, close to either the lateral termination of a brittle shear zone at Terme di Valdieri, or a step-over between two en-echelon brittle shear zones at Bagni di Vinadio. These observations attest to a strong control operated on the location of outlet regions by both brittle tectonics and the minima in hydraulic potential inside the fractured massif.
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Velocity-density tests conducted in the laboratory involved small 4-inch diameter by 4.58-inch-long compacted soil cylinders made up of 3 differing soil types and for varying degrees of density and moisture content, the latter being varied well beyond optimum moisture values. Seventeen specimens were tested, 9 with velocity determinations made along two elements of the cylinder, 180 degrees apart, and 8 along three elements, 120 degrees apart. Seismic energy was developed by blows of a small tack hammer on a 5/8-inch diameter steel ball placed at the center of the top of the cylinder, with the detector placed successively at four points spaced 1/2-inch apart on the side of the specimen involving wave travel paths varying from 3.36 inches to 4.66 inches in length. Time intervals were measured using a model 217 micro-seismic timer in both laboratory and field measurements. Forty blows of the hammer were required for each velocity determination, which amounted to 80 blows on 9 laboratory specimens and 120 blows on the remaining 8 cylinders. Thirty-five field tests were made over the three selected soil types, all fine-grained, using a 2-foot seismic line with hammer-impact points at 6-inch intervals. The small tack hammer and 5/8-inch steel ball was, again, used to develop seismic wave energy. Generally, the densities obtained from the velocity measurements were lower than those measured in the conventional field testing. Conclusions were reached that: (1) the method does not appear to be usable for measurement of density of essentially fine-grained soils when the moisture content greatly exceeds the optimum for compaction, and (2) due to a gradual reduction in velocity upon aging, apparently because of gradual absorption of pore water into the expandable interlayer region of the clay, the seismic test should be conducted immediately after soil compaction to obtain a meaningful velocity value.
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The study area. located north of Konva (Central Turkey), is composed of Silurian to Cretaceous metamorphosed rocks. The lower unit of the oldest formation (Silurian-Early Permian) is mostly made up of Silurian-Early Carboniferous metacarbonates. These rocks pass laterally and vertically to Devonian-Early Permian series having continental margin, shallow water and pelagic characteristics. They are intruded or juxtaposed to different kinds of metamagmatic rocks. which show MORB. continental arc and within plate characteristics. The Palaeozoic units are covered unconformably by Triassic-Cretaceous metasedimentary units. All these rocks are overthrusted by Mesozoic ophiolites. The Palaeozoic sequence can be seen as a northern Palaeotethys passive, then active margin. The northward subduction of the Palaeotethys ocean during the Carboniferous-Triassic times, induced the development of a magmatic arc and fore-arc sequence (Carboniferous-Permian). Before the Early Triassic (?Late Permian) time. the fore-arc sequence was uplifted above sea level and eroded. The Triassic sequences are regarded as marking the onset of back-arc opening and detachment of the Anatolian Konya block from the active Eurasian margin. Finally. a suture zone formed during the Carman between the Konya region and the Menderes-Tauride Cimmerian block due to the closing of Palaeotethvs. This geodynamic evolution can be correlated with the evolution of the Karaburun sequence in western Turkey.