983 resultados para Risorgimento italiano - Reggio Emilia - 1848-1859


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Numbered in series of 12 numbers each.

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Mode of access: Internet.

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Mode of access: Internet.

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"Bibliografia": p. [vii]-xxiii. Bibliographical footnotes.

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Bound with the author's Ragionamento sulla lingua del testo misnico [Reggio, 1819]

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Reggio Emilia is an educational philosophy that encourages teachers, students and their parents to collaborate and actively engage with the environment. This study investigates how the Reggio Emilia design approach was translated architecturally for a kindergarten in an Australian context, and provides insights into the operation of this Reggio kindergarten and the impact that it is now having on the occupants. It evaluates the original architectural design intent of the Reggio Emilia early childhood learning environment against its spatial provision. The relationship that the Reggio Emilia approach facilitates between students and the environment, and the contribution that this approach has on their learning, are also explored. Several key themes emerging from the Reggio values were identified in the literature. These were then used to inform an exploration of the kindergarten spaces and places.. Architects, teachers and a sustainability manager of the kindergarten were interviewed with their experiences constituting the primary data of this study. Using a Grounded Theory methodology, systematic data coding and analysis were then conducted. Themes and concepts that emerged from this process include: differing interpretations of the Reggio Emilia philosophy; motivations for neglect of traditional external structures and play equipment; the impact of education for sustainability; and the positive effects that Reggio Emilia is having on the rest of the institution’s development.

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Within the field of early childhood education, the ideologies of child development and its parent discipline, developmental psychology, dominate both theory and practice. In recent years, educators have attempted to reconceptualise early childhood education by adopting more progressive approaches to teaching and learning. The aim of this present research study was to critically examine the experiences of early childhood educators who have adopted a Reggioinspired approach to educating young children. To explore their experiences, an institutional ethnography was employed involving seven educators from a large child care organization in Hamilton, Ontario. In line with the intent ofthis study, qualitative data were collected through in-depth semi-structured interviews, participant-observations and textual analyses to explore the presence of developmental-psychological ideologies within early childhood education and Reggio-inspired practice. The present study also examined the challenges faced by educators who have adopted a Reggio-inspired approach. The results of this study indicate that ideologies associated with the developmental-psychological paradigm dominate the practice of early childhood educators and that the conflicting ideologies that surround Reggio educators may play a role in some of the challenges educators experience. The findings of this study thus demonstrate a need to adopt alternative approaches toward understanding both children and childhood, in both early childhood educational theory and practice.

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Resumen tomado de la revista

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In its attention to how space can be thoughtfully arranged, Reggio Emilia has “reconceptualised space as a key source of educational provocation and insight” (Strong-Wilson & Ellis, 2007, p. 40). Such an approach advocates that educators pay close attention to the myriad of ways that space can be made to speak and invite interaction. Theorists recognise eight key principles (aesthetics, transparency, active learning, flexibility, collaboration, reciprocity, bringing the outdoors in, and relationships) which are considered essential to the notion of environment as third teacher. Drawing upon a successful capital rebuilding grant, this presentation outlines the process of reconceptualising and building a space for flexible research, teaching and learning within higher education. This presentation interrogates the successes and challenges which arise when innovating within a traditional space.

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Le pietre artificiali ed i cementi artistici utilizzati durante la stagione Liberty rappresentano tutt’oggi un patrimonio artistico non ancora sufficientemente studiato. In seguito ad una ricerca bibliografica su testi e riviste dei primi anni del Novecento, è stata eseguita una ricognizione del patrimonio architettonico emiliano-romagnolo, al fine di valutarne i materiali e le tipologie di degrado più diffuse. Le città e le zone oggetto di studio sono state: Bologna, Ferrara, Modena e provincia, Reggio Emilia, Parma, Firenze, la Romagna e le Marche settentrionali. Tra gli edifici individuati sono state analizzate le decorazioni e gli intonaci di tre edifici ritenuti particolarmente significativi: il villino Pennazzi (noto anche come Villa Gina) a Borgo Panigale (Bologna), villa Verde a Bologna e l’ex-albergo Dorando Pietri a Carpi. Da tali edifici sono stati selezionati campioni rappresentativi delle diverse tipologie di decorazioni in pietra artificiale e successivamente sono stati caratterizzati in laboratorio tramite diffrattometria a raggi x (XRD), termogravimetria (TGA), microscopio ottico in sezioni lucide, microscopio elettronico a scansione (SEM) e porosimetria ad intrusione di mercurio (MIP). In particolare per Villa Verde sono state formulate e caratterizzate diverse tipologie di malte variando il tipo di legante ed il rapporto acqua/cemento, al fine di garantire la compatibilità fisico-meccanica con il supporto negli interventi di risarcimento delle lacune previsti nel restauro. L’attività sperimentale svolta ha permesso di mettere a punto un vero e proprio protocollo diagnostico per il restauro di questo tipo di decorazioni che potrà essere utilizzato sia nei casi di studio analizzati che per ogni futuro intervento.

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Water is the driving force in nature. We use water for washing cars, doing laundry, cooking, taking a shower, but also to generate energy and electricity. Therefore water is a necessary product in our daily lives (USGS. Howard Perlman, 2013). The model that we created is based on the urban water demand computer model from the Pacific Institute (California). With this model we will forecast the future urban water use of Emilia Romagna up to the year of 2030. We will analyze the urban water demand in Emilia Romagna that includes the 9 provinces: Bologna, Ferrara, Forli-Cesena, Modena, Parma, Piacenza, Ravenna, Reggio Emilia and Rimini. The term urban water refers to the water used in cities and suburbs and in homes in the rural areas. This will include the residential, commercial, institutional and the industrial use. In this research, we will cover the water saving technologies that can help to save water for daily use. We will project what influence these technologies have to the urban water demand, and what it can mean for future urban water demands. The ongoing climate change can reduce the snowpack, and extreme floods or droughts in Italy. The changing climate and development patterns are expected to have a significant impact on water demand in the future. We will do this by conducting different scenario analyses, by combining different population projections, climate influence and water saving technologies. In addition, we will also conduct a sensitivity analyses. The several analyses will show us how future urban water demand is likely respond to changes in water conservation technologies, population, climate, water price and consumption. I hope the research can contribute to the insight of the reader’s thoughts and opinion.

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Landslide hazard and risk are growing as a consequence of climate change and demographic pressure. Land‐use planning represents a powerful tool to manage this socio‐economic problem and build sustainable and landslide resilient communities. Landslide inventory maps are a cornerstone of land‐use planning and, consequently, their quality assessment represents a burning issue. This work aimed to define the quality parameters of a landslide inventory and assess its spatial and temporal accuracy with regard to its possible applications to land‐use planning. In this sense, I proceeded according to a two‐steps approach. An overall assessment of the accuracy of data geographic positioning was performed on four case study sites located in the Italian Northern Apennines. The quantification of the overall spatial and temporal accuracy, instead, focused on the Dorgola Valley (Province of Reggio Emilia). The assessment of spatial accuracy involved a comparison between remotely sensed and field survey data, as well as an innovative fuzzylike analysis of a multi‐temporal landslide inventory map. Conversely, long‐ and short‐term landslide temporal persistence was appraised over a period of 60 years with the aid of 18 remotely sensed image sets. These results were eventually compared with the current Territorial Plan for Provincial Coordination (PTCP) of the Province of Reggio Emilia. The outcome of this work suggested that geomorphologically detected and mapped landslides are a significant approximation of a more complex reality. In order to convey to the end‐users this intrinsic uncertainty, a new form of cartographic representation is needed. In this sense, a fuzzy raster landslide map may be an option. With regard to land‐use planning, landslide inventory maps, if appropriately updated, confirmed to be essential decision‐support tools. This research, however, proved that their spatial and temporal uncertainty discourages any direct use as zoning maps, especially when zoning itself is associated to statutory or advisory regulations.

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Vols. 5-20 include Atti of the society.

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The Cervarola Sandstones Formation (CSF), Aquitanian-Burdigalian in age, was deposited in an elongate, NW-stretched foredeep basin formed in front of the growing Northern Apennines orogenic wedge. The stratigraphic succession of the CSF, in the same way of other Apennine foredeep deposits, records the progressive closure of the basin due to the propagation of thrust fronts toward north-east, i.e. toward the outer and shallower foreland ramp. This process produce a complex foredeep characterized by synsedimentary structural highs and depocenters that can strongly influence the lateral and vertical turbidite facies distribution. Of consequence the main aim of this work is to describe and discuss this influence on the basis of a new high-resolution stratigraphic framework performed by measuring ten stratigraphic logs, for a total thickness of about 2000m, between the Secchia and Scoltenna Valleys (30km apart). In particular, the relationship between the turbidite sedimentation and the ongoing tectonic activity during the foredeep evolution has been describe through various stratigraphic cross sections oriented parallel and perpendicular to the main tectonic structures. On the basis of the high resolution physical stratigraphy of the studied succession, we propose a facies tract and an evolutionary model for the Cervarola Sandstones in the studied area. Thanks to these results and the analogies with others foredeep deposits of the northern Apennines, such as the Marnoso-arenacea Formation, the Cervarola basin has been interpreted as a highly confined foredeep controlled by an intense synsedimentary tectonic activity. The most important evidences supporting this hypothesis are: 1) the upward increase, in the studied stratigraphic succession (about 1000m thick), of sandstone/mudstone ratio, grain sizes and Ophiomorpha-type trace fossils testifying the high degree of flow deceleration related to the progressive closure and uplift of the foredeep. 2) the occurrence in the upper part of the stratigraphic succession of coarse-grained massive sandstones overlain by tractive structures such as megaripples and traction carpets passing downcurrent into fine-grained laminated contained-reflected beds. This facies tract is interpreted as related to deceleration and decoupling of bipartite flows with the deposition of the basal dense flows and bypass of the upper turbulent flows. 3) the widespread occurrence of contained reflected beds related to morphological obstacles created by tectonic structures parallel and perpendicular to the basin axis (see for example the Pievepelago line). 4) occurrence of intra-formational slumps, constituted by highly deformed portion of fine-grained succession, indicating a syn-sedimentary tectonic activity of the tectonic structures able to destabilize the margins of the basin. These types of deposits increase towards the upper part of the stratigraphic succession (see points 1 and 2) 5) the impressive lateral facies changes between intrabasinal topographic highs characterized by fine-grained and thin sandstone beds and marlstones and depocenters characterized by thick to very thick coarse-grained massive sandstones. 6) the common occurrence of amalgamation surfaces, flow impact structures and mud-draped scours related to sudden deceleration of the turbidite flows induced by the structurally-controlled confinement and morphological irregularities. In conclusion, the CSF has many analogies with the facies associations occurring in other tectonically-controlled foredeeps such as those of Marnoso-arenacea Formation (northern Italy) and Annot Sandstones (southern France) showing how thrust fronts and transversal structures moving towards the foreland, were able to produce a segmented foredeep that can strongly influence the turbidity current deposition.