A Ideia de “Quarteirão” na Regeneração Urbana do Centro Histórico do Porto

As intervenções de regeneração urbana quando realizadas através da unidade do quarteirão, tornam-se desafios e oportunidades únicas na preservação da identidade e na valorização dos recursos históricos. Esta escala de abordagem nas intervenções permite não só a renovação arquitetónica dos espaços mas também a inclusão de preocupações de carácter cultural, social, económico e ambiental neste processo, que se considera aqui enquanto princípios base para um desenvolvimento sustentável. Esta investigação tem como objetivo aprofundar conhecimentos acerca da ideia de “quarteirão” e da sua relevância no processo de regeneração urbana no contexto das recentes transformações urbanas no centro histórico do Porto, e tendo em vista a necessidade de um desenvolvimento sustentável, salientando a importância do reforço da identidade como um dos seus principais princípios de atuação. De forma a sustentar o estudo destas temáticas centradas numa abordagem limitada à área da Zona de Intervenção Prioritária (ZIP), são analisados dois casos de estudos de intervenções existentes/a decorrer bem como um terceiro caso desenvolvido no âmbito da presente dissertação. Com base na análise dos casos de estudo, da bibliografia e da documentação relativa ao tema verificou-se que para reforçar a identidade do centro histórico do Porto, a fim de preservar as suas dinâmicas sociais e culturais, os projetos devem evitar intervenções à escala do quarteirão, que desrespeitem as características originais dos edifícios tal como os seus limites. Propõe-se assim o desenvolvimento de uma estratégia de intervenção global que respeitando a singularidade e os desafios arquitetónicos e socioculturais de cada parcela e edifício não deixe nunca de perder uma visão mais alargada sobre a complexidade do território.

Techno-economic analysis of three HVAC retrofitting options

Accounting for around 40% of the total final energy consumption, the building stock is an important area of focus on the way to reaching the energy goals set for the European Union. The relatively small share of new buildings makes renovation of existing buildings possibly the most feasible way of improving the overall energy performance of the building stock. This of course involves improvements on the climate shell, for example by additional insulation or change of window glazing, but also installation of new heating systems, to increase the energy efficiency and to fit the new heat load after renovation. In the choice of systems for heating, ventilation and air conditioning (HVAC), it is important to consider their performance for space heating as well as for domestic hot water (DHW), especially for a renovated house where the DHW share of the total heating consumption is larger. The present study treats the retrofitting of a generic single family house, which was defined as a reference building in a European energy renovation project. Three HVAC retrofitting options were compared from a techno-economic point of view: A) Air-to-water heat pump (AWHP) and mechanical ventilation with heat recovery (MVHR), B) Exhaust air heat pump (EAHP) with low-temperature ventilation radiators, and C) Gas boiler and ventilation with MVHR. The systems were simulated for houses with two levels of heating demand and four different locations: Stockholm, Gdansk, Stuttgart and London. They were then evaluated by means of life cycle cost (LCC) and primary energy consumption. Dynamic simulations were done in TRNSYS 17. In most cases, system C with gas boiler and MVHR was found to be the cheapest retrofitting option from a life cycle perspective. The advantage over the heat pump systems was particularly clear for a house in Germany, due to the large discrepancy between national prices of natural gas and electricity. In Sweden, where the price difference is much smaller, the heat pump systems had almost as low or even lower life cycle costs than the gas boiler system. Considering the limited availability of natural gas in Sweden, systems A and B would be the better options. From a primary energy point of view system A was the best option throughout, while system B often had the highest primary energy consumption. The limited capacity of the EAHP forced it to use more auxiliary heating than the other systems did, which lowered its COP. The AWHP managed the DHW load better due to a higher capacity, but had a lower COP than the EAHP in space heating mode. Systems A and C were notably favoured by the air heat recovery, which significantly reduced the heating demand. It was also seen that the DHW share of the total heating consumption was, as expected, larger for the house with the lower space heating demand. This confirms the supposition that it is important to include DHW in the study of HVAC systems for retrofitting.

Análisis del posicionamiento estratégico del café del Huila y el desarrollo de los cafés especiales

El proyecto de grado titulado “Análisis del posicionamiento estratégico del café del Huila y el desarrollo de los cafés especiales” tiene el objetivo general de estudiar y hacer públicas las ventajas de producir café de alta calidad en el departamento del Huila, puesto que existen algunas zonas del departamento que no tienen una producción de calidad certificada, lo cual ha generado cuellos de botella en relación a la demanda potencial y real con la Unión Europea. En la investigación se busca la manera de incrementar la zona productora de cafés especiales para satisfacer el mercado Europeo que es gustador del tipo de café que se cultiva en la región Huilense por la suavidad, aroma, entre otras variables influyentes. El desarrollo de este proyecto en esta región del país, se sustenta por la mayor producción de café a nivel nacional. Asimismo, también porque es el abanderado en cafés especiales y cuenta con la mayoría de fincas certificadas con algún sello de conducta en Colombia. Lo anterior, se ha alcanzado con la aplicación de buenas prácticas para la sostenibilidad del cultivo, la gran labor de renovación de cafetales y al don cafetero que tiene la gente del Huila debido a que es el negocio agrícola más importante.

Niveles de actividad física en escolares de instituciones distritales de Bogotá, Colombia.

Objetivo: Estimar los niveles de actividad física (AF) de escolares de básica primaria durante el recreo, a través del uso del Sistema de Observación de Juego y Tiempo Libre en niños. Metodología: Estudio descriptivo transversal. Cinco instituciones educativas de la localidad de Engativá de Bogotá participaron en el presente estudio. Se contó con una muestra a conveniencia de 2.415 escolares (1.093 niñas y 1.322 niños), los cuales cursaban de 2º a 5º de primaria. Se realizaron 261 observaciones en 87 áreas determinadas. La muestra presentó una confiabilidad del 95%. Resultados: El tiempo de recreo fue de 30 minutos, los niños mostraron mayores porcentajes de AF con respecto a las niñas, sin embargo no se encontraron asociaciones estadísticamente significativas (p=0,506). Las áreas eran totalmente accesibles y utilizables, pero ausentes de actividades organizadas. Se encontró un bajo nivel de AF 9,5% en áreas supervisadas. De los escolares; el 22,5% para niñas, y el 20,6% para niños, tuvieron comportamientos sedentarios durante el recreo. Menos del 15% de los escolares realizaron AF vigorosa en el recreo y un mayor porcentaje 62,8% para niñas vs 64,6% para niños realizaron AF moderada. Conclusión: Los escolares acumularon una cantidad valiosa de AF moderada y vigorosa durante el recreo. Es probable que se aumente el nivel de AF, si el patio de la escuela está equipado y con actividades organizadas. Es esencial que las estrategias específicas se estudien y evalúen para determinar cómo y en qué medida se fomenta la AF entre los escolares.

TECTONIC CONTROLS ON FLUVIAL LANDSCAPE DEVELOPMENT IN CENTRAL-EASTERN PORTUGAL: INSIGHTS FROM LONG PROFILE TRIBUTARY STREAM ANALYSES

This study examines the long profiles of tributaries of the Tejo (Tagus) and Zêzere rivers in central eastern Portugal (West Iberia) in order to provide new insights into the patterns, timing and controls on drainage development during the Pleistocene to Holocene incision stage. The long profiles were extracted from lower order tributary streams associated with the trunk drainage of the Tejo River and one main tributary, the Zêzere River (Fig. 1). These streams flow through a landscape strongly influenced by variations in bedrock lithology (mainly granites and metasediments), fault structures delimiting crustal blocks with distinct uplift rates, and a base-level lowering history (tectonic uplift / eustatic). The long profiles of the tributaries of the Tejo and Zêzere rivers record a series of transient and permanent knickpoints. The permanent knickpoints have direct correlation with the bedrock strength, corresponding to the outcropping of very hard quartzites or to the transition from softer (slates/metagreywaques) to harder (granite) basement. The analyzed streams/rivers record also an older transient knickpoint/knickzone separating: a) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage; and b) a downstream reach displaying a rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final segment, which is often convex (Fig. 2). The rejuvenated reaches testify the upstream propagation of several incision waves that are the response of each stream to continuous or increasing crustal uplift and dominant periods of base-level lowering by the trunk drainages, coeval of low sea level conditions. The long profiles and their morphological configurations enabled spatial and relative temporal patterns of incision to be quantified for each individual tributary stream. The incision values of streams flowing in uplifted blocks of the Portuguese Central Range (PCR) (ca.380-280 m) indicate differential uplift and are higher than the incision values of streams flowing on the adjacent South Portugal planation surface – the Meseta (ca. 200 m). The normalized steepness index, calculated using the method of Wobus et al. (2006), proved to be sensitive to active tectonics, as lower ksn values were found in relict graded profiles of streams located in less uplifted blocks, (e.g. Sertã stream in the PCR), or in those flowing through tectonic depressions. Fig. 1 – Geological map of the study area. 1 – fluvial terraces (Pleistocene); 2 – sedimentary cover (Paleogene and Neogene); 3 – slates and metasandstones (Devonian); 4 – slates and quartzites (Silurian); 5 – quartzites (Ordovician); 6 – slates and metagreywackes (Precambrian to Cambrian); 7 – slates, metagreywackes and limestones (Precambrian); 8 – granites and ortogneisses; 9 – diorites and gabros; 10 - fault. SFf – Sobreira Formosa fault; Sf – Sertã fault; Pf – Ponsul fault; Gf – Grade fault. The differential uplift indicated by the distribution of the ksn values and by the fluvial incision was likely accumulated on a few major faults, as the Sobreira Formosa fault (SFf), thus corroborating the tectonic activity of these faults. Due to the fact that the relict graded profiles can be correlated with other geomorphic references documented in the study area, namely the T1 terrace of the Tagus River (with an age of ca. 1 Myr), the following incision rates can be estimated: a) for the studied streams located in uplifted blocks of the PCR, 0.38 m/kyr to 0.28 m/kyr; b) for the streams flowing on the South Portugal planation surface, 0.20 m/kyr. The differential uplift inferred between crustal blocks in the study area corroborates the neotectonic activity of the bordering faults, which has been proposed in previous studies based upon less robust data. Fig. 2 – Longitudinal profile of the Nisa stream a tributary of the Tejo River. Note the equilibrium relict profile upstream the older transient knickpoint (hatched line) and the downstream rejuvenated profile (continuous line). Legend: tKP – transient knickpoint; rKp – resistant knickpoint; Mt – schist and phyllite; Gr – granite; Hf – hornfels; Og – orthogneisse. In the inset Distance – Slope plots, fill circles correspond to the relict graded profile, crosses correspond to the rejuvenated profile located downstream the older transient knickpoint (tKP).

Tectonic and lithological controls on fluvial landscape development in central-eastern Portugal: Insights from long profile tributary stream analyses

This study examines the long profiles of tributaries of the Tagus and Zêzere rivers in Portugal (West Iberia) in order to provide new insights into patterns, timing, and controls on drainage development during the Quaternary incision stage. The studied streams are incised into a relict culminant fluvial surface, abandoned at the beginning of the incision stage. The streams flow through a landscape with bedrock variations in lithology (mainly granites and metasediments) and faulted blocks with distinct uplift rates. The long profiles of the analyzed streams record an older transitory knickpoint/knickzone separating (1) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage, and (2) a downstream rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final reach, which is often convex. The rejuvenated reaches testify to the upstream propagation of several incision waves, interpreted as the response of each stream to increasing crustal uplift and prolonged periods of base-level lowering by the trunk drainages, coeval with low sea level conditions. The morphological configurations of the long profiles enabled spatial and relative temporal patterns of incisions to be quantified. The incision values of streams flowing on the Portuguese Central Range (PCR; ca. 380–150 m) are variable but generally higher than the incision values of streams flowing on the adjacent South Portugal Planation Surface (SPPS; ca. 220–110 m), corroborating differential uplift of the PCR relative to the SPPS. Owing to the fact that the relict graded profiles can be correlated with the Tagus River T1 terrace (1.1–0.9 My) present in the study area, incision rates can be estimated (1) for the streams located in the PCR, 0.38–0.15 m/ky and (2) for the streams flowing on the SPPS, 0.22–0.12 m/ky. The differential uplift inferred in the study area supports the neotectonic activity of the bordering faults, as proposed in previous studies based upon other geological evidence.

Tectonic and lithological controls on fluvial landscape development in central-eastern Portugal: Insights from long profile tributary stream analyses

This study examines the long profiles of tributaries of the Tagus and Zêzere rivers in Portugal (West Iberia) in order to provide new insights into patterns, timing, and controls on drainage development during the Quaternary incision stage. The studied streams are incised into a relict culminant fluvial surface, abandoned at the beginning of the incision stage. The streams flow through a landscape with bedrock variations in lithology (mainly granites and metasediments) and faulted blocks with distinct uplift rates. The long profiles of the analyzed streams record an older transitory knickpoint/knickzone separating (1) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage, and (2) a downstream rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final reach, which is often convex. The rejuvenated reaches testify to the upstream propagation of several incision waves, interpreted as the response of each stream to increasing crustal uplift and prolonged periods of base-level lowering by the trunk drainages, coeval with low sea level conditions. The morphological configurations of the long profiles enabled spatial and relative temporal patterns of incisions to be quantified. The incision values of streams flowing on the Portuguese Central Range (PCR; ca. 380–150 m) are variable but generally higher than the incision values of streams flowing on the adjacent South Portugal Planation Surface (SPPS; ca. 220–110 m), corroborating differential uplift of the PCR relative to the SPPS. Owing to the fact that the relict graded profiles can be correlated with the Tagus River T1 terrace (1.1–0.9 My) present in the study area, incision rates can be estimated (1) for the streams located in the PCR, 0.38–0.15 m/ky and (2) for the streams flowing on the SPPS, 0.22–0.12 m/ky. The differential uplift inferred in the study area supports the neotectonic activity of the bordering faults, as proposed in previous studies based upon other geological evidence.

Phytosociology of the remaining xerophytic woodland associated to an environmental gradient at the banks of the São Francisco river - Petrolina, Pernambuco, Brazil1

Floristic and phytosociological surveys were carried out for 12 months in the Embrapa-SPSB, Petrolina, Pernambuco, Brazil. A transect was laid on starting at the river bank extending for 790 m away from the river and divided into 140 10 × 10 m contiguous plots. In each plot, all standing plants, alive or dead, with stem diameter at soil level ? 3 cm and total height ? 1 m were sampled. Along this transect, an elevation range of 9.40 m was registered and five topographical environments were identified: riverside (MR), dike (D), floodable depression (DI), boundary terrace (TL) - all of them belonging to the fluvial terrace with Fluvic Neosol and Haplic Cambisol both silty textured eutrophic soils - and the inlander tableland (TS), with medium sandy-textured Red-Yellow Argisols. Fourty-eight species/morphospecies, distributed into 39 genera and 21 families, were identified. Four phytogeoenvironments (MR, D + TL, DI + TL, and TS) were registered based on environmental variations and floristic similarities among plots using cluster analyses. The MR environment showed the largest total density, total basal area, maximum and medium heights and maximum diameter. Moreover, it had 8.1% of plants with heights above 8 m against 0.6% for D + TL, 0.2% for DI + TL, and 0% for TS. The species with the largest importance value were Inga vera subsp. affinis (DC.) T.D. Pennington in MR, Mimosa bimucronata Kunth in D + TL and DI + TL and M. tenuiflora (Willd.) Poir. in TS.

DESLIZAMIENTOS EN LA CUENCA MEDIA Y SUPERIOR DEL RIO REVENTADO, CARTAGO, COSTA RICA

La cuenca del río Reventado, situada en la vertiente sur del Volcán Irazú, Costa Rica, presenta actualmente un riesgo para la ciudad de Cartago (aproximadamente 30.000 habitantes), especialmente para algunos asentamientos cercanos al río mismo.  Este riesgo consiste, en primer lugar, en un deslizamiento con grandes extensiones en la parte inferior de la cuenca media, el deslizamiento llamado San Blas. Este deslizamiento está formado por la antigua terraza de Banderilla de material de avalanchas holocenas y que fue activado en el comienzo de la década de los setenta por la destrucción de su sostén por la explotación de materiales en tajos. Anteriormente, la última vez en los años 63-65, el riesgo era diferente:Erupciones del Irazú con grandes cantidades de cenizas originaron un cambio violento del régimen hidrológico, intensas lluvias causaron crecidas y avalanchas, profundizando en la cuenca superior los cauces y provocando así deslizamientos. En la cuenca baja estas avalanchas provocan inundaciones y acumulaciones de los abanicos diferentes. Los deslizamientos activados por estos eventos actualmente muestran poca o ninguna actividad, pero el riesgo de repeticiones de estos eventos persiste. SUMMARYThe Rio Reventado watershed, situated in the southern slope of the Irazú volcano, Costa Rica, presents a risk for the town of Cartago (30.000 inhabitants) and specially for some settlements near the river.  In first place, this risk consists of a huge landslide in the lower part of the watershed, the<<San Blas- landslide, which is formed by the labaric material of a Holocene terrace of the Reventado, called <<Banderilla- terrace>>. At the beginning of the seventies this terrace was activated due the explotation of its materials in two quarries.  The risks existing before in this watershed were of an other nature, an example give the events of years 1963-65:A violent hydrologic change in the upper part of the Reventado watershed due to the ashfall of an eruption of the Irazú caused big mudflows whish depend the river beds and thus provoked landslides.  These mud flows caused inundations and accumulations in the lower watershed. Today, the land slides activated in the sixties are stable or semistable, but the risk of repetitions still persists.

THE POETRY OF CONVERGENCE AND THE MIRROR IMAGE IN GUIMARÃES ROSA

Affiliated with a literary context in which the poet seeks reconciliation between the self and the universe without rejecting the consciousness of the poetic process and the renovation of language, the poems of Guimarães Rosa in his book Ave, Palavra, are close to what Octavio Paz called "poetry of convergence." Such analogical point of view turns into metaphor in the poems through the myth of Narcissus and images that associate a reflexion and the meeting with the Other as a way to know yourself. This work presents a reading of these poetic compositions by examining how the analogy is established, relating those poems to his other works, identifying them, not as an accident in his trajetory, but as a work that carries Guimarães Rosa’s concerns explored in his literary career.