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    [Ka-shaqaynta haragga I - Lavorazione della pelle I]

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    Odayaashu waxay markan ka hadlayaan hawlaha laga qabto haragga xoolaha, gaar ahaan hawsha kabatolaha, waxay kaloo, si guud ah, uga hadlayaan farsamooyinka gacanta.In questa conversazione gli anziani parlano di un aspetto particolare della lavorazione della pelle, ovvero quello che riguarda il lavoro del calzolaio, e trattano anche, in maniera più generale, del lavoro degli artigiani.In this conversation the elders talk about a particular aspect of leather manufacturing related to shoemakers' activity, also addressing, in a more general way, handicraftsmen's work.Haasaawe badan oo laga duubay siddeetameeyadii odayaal ka shaqaynaayay Akadeemiyada Cilmiga iyo Fanka iyo Suugaanta ee Muqdisho, iyagoo ka hadlaya hiddaha iyo dhaqanka ee bulshada soomaaliyeed.Registrazioni audio di conversazioni intercorse tra anziani dell'Accademia delle Scienze, delle Arti e della Letteratura di Mogadiscio negli anni '80, su temi relativi alla cultura e alla società tradizionali somale.Conversations between Elders of the Academy of Science, Arts and Literature on arguments related with Somali culture, society and traditions, recorded in Mogadishu in the 80's

    Sistemi per il controllo delle risorse distribuite e lo storage in una SmartGrid

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    Le reti elettriche tradizionali sono state progettate per un funzionamento radiale e passivo, con completa separazione della rete passiva dell’utente dalla rete attiva dell’utility in modo da distribuire energia verso milioni di consumatori da impianti di generazione di grandi dimensione. L’efficienza di queste reti è limitata dalla necessità di installare capacità di generazione aggiuntiva per sopperire alla domanda di picco giornaliera. Le smart grid superano questa criticità prevedendo l’uso diffuso di dispositivi di storage, sorgenti di energia rinnovabile e smart meter. Il problema di disporre di una architettura distribuita di controllo efficiente dei dispositivi di accumulo di energia diventa fondamentale in una smart grid. Infatti la ricarica contemporanea di un numero troppo elevato di dispositivi di accumulo nella rete a BT e MT potrebbe sovraccaricare il sistema elettrico, con conseguenti rischi di black out e crescita dei costi di ripristino del servizio. In questo contesto si inserisce il tema di ricerca di questo dottorato sui modelli per la realizzazione di sistemi di controllo per il controllo dello storage e dei carichi passivi in una smart grid. L’attività di ricerca, condotta sotto la direzione del Prof. Del Vecchio, ha esplorato le seguenti tematiche: 1. dispositivi di storage: tecnologie di accumulo, specifiche tecniche e modellamento simulink; 2. progetto e l’implementazione di uno smart agent per il controllo dello storage in una rete in BT che comprende un impianto fotovoltaico; 3. Test di verifica di correttezza delle funzionalità dello smart agent nell’ambiente di simulazione Matlab-Simulink, prendendo in considerazione una sottorete in BT e vari profili di irraggiamento solare; 4. analisi della teoria dei giochi per implementare un sistema di stoccaggio ottimale in una rete estesa dotata di più nodi di generazione, accumulo e carichi programmabili

    La nominalizzazione sintattica in cinese standard

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    Obiettivo di questo lavoro è l’analisi, nel quadro della linguistica generale, della nominalizzazione sintattica in cinese standard. Con nominalizzazione sintattica si intende il fenomeno per cui entità linguistiche che non sono immagazzinate nel lessico come nomi svolgono funzione nominale in una frase (Simone 2003, 2008, Simone & Pompei 2007). Questo lavoro si colloca quindi nell’ambito dello studio delle parti del discorso, un campo d’indagine vivace, che costituisce una sfida teorica particolarmente interessante nelle lingue che fanno scarso ricorso alla morfologia per la resa delle categorie grammaticali, e non permettono quindi di ricorrere al criterio interlinguisticamente più saliente per la suddivisione delle parti del discorso. Per quanto l’oggetto d’analisi privilegiato sia la lingua cinese, si faranno costanti riferimenti all’italiano, che costituisce un punto di confronto tipologicamente distante dal cinese e che permette a chi scrive intuizioni e consapevolezza proprie del parlante nativo. Non mancheranno, ove utili a fornire paragoni clarificatori, esempi da altre lingue, come l’inglese, il francese, il coreano e il turco

    Seismic assessment of as-built and isolated cases of an existing RC bridge through experimental PsD testing

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    In Italy most of Infrastructures and highway bridge systems have been built before the issue of modern seismic design codes. Chiefly, the existing transportation systems that built in the late 60s and early 70s were designed primarily for gravity loads. As a result, such systems do not employ seismic details and hence their structural performance is inadequate under earthquake ground motions. To decide for any retrofitting operation, the seismic behaviour of existing bridges must be assessed. Because the nonlinear procedures are becoming very popular in the frameworks of structural assessment, there is a need to accurately simulate authentic model to provide reliable indications about the performance required to this kind of structures. Based on these observations, this thesis is devoted to the seismic assessment of existing RC bridges. In particular, the vulnerability of an old RC viaduct with portal frame piers equipped with plain steel bars has been numerically and experimentally investigated. Subsequently, the retrofitting has been evaluated using Friction Pendulum System isolation “FPS”. The nonlinear FE modelling has been executed using OpenSEES software framework. The local behaviour of the bridge has been taking into account, mainly, the bond-slip, strain penetration effect of the plain steel bars, bar buckling and the shear behaviour effect of the transverse beams of the portal frame piers. Depending on a previous experimental campaign consisting of cyclically imposed displacements on 1:4 reduced scale models of a frame pier, belonging to the same RC highway viaduct, a new experimental activity has been proposed within the RETRO project funded by the European Union. In particular, Two specimens (scale 1:2.5), 2 floors (total height is 5.8 m) and 3 floors (total height is 10.3 m) one-bay reinforced concrete frame respectively, were built and tested using the PsD technique with sub-structuring; the modelling of the entire viaduct is considered along with the non-linear behaviour of each pier. During the test campaign, two different configurations for the analysed viaduct have been considered; “As-built” and “Isolated with Friction Bearings”. The response of both cases has been compared to evaluate the effectiveness of the isolation system. To this end, two natural accelerograms were selected based on studying the seismiogenic zone of the bridge to represent, according to current seismic codes, the Serviceability and Ultimate limit states. Analysis and interpretation of the experimental were achieved throughout the data recorded by the instrumentation used in the test campaign. The results have been used to calibrate numerical models and to provide a detailed analysis of the performance of the as-built configuration and to show the effectiveness of friction pendulum systems for seismic protection, which will ultimately lead to guidelines for the assessment and design of similar structures as part of pre-Normative research in support to the Eurocodes

    Woody biomass combustion modeling in moving grate furnaces

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    Woody biomass combustion in moving grate furnaces occurs in two distinct regions: the solid bed region and the freeboard region above the fuel layer. This thesis reports about the work related to the development of a model to simulate the biomass bed combustion. The developed model is a 1-D transient model and it has been applied to study a multidimensional process such as the biomass thermal conversion in moving grate furnaces. This is possible since the physical variable gradients in the direction of the bed height are much higher than those in the direction of the bed length, thus, thermal and mass exchanges in the grate direction can be neglected. Considering these observations, the study of the combustion process in moving grate furnaces can be reduced to the observation of a vertical column of fuel that is moving along the grate inside the furnace and a 1-D transient system can be used to model the thermal conversion of the biomass fuel inside the combustion chamber. Biomass combustion modeling is central to defining the right strategies for controlling and optimizing the combustion process. Indeed, the quality of the biomass fuels in terms of physical and chemical properties can vary significantly. Thus, it is readily apparent that a detailed understanding on what happens when biomass is burned and, in particular, what changes occur when the fuel characteristics and the operational conditions vary, enables us to make the correct decisions with respect to the optimal design and operational principles of the biomass combustion applications. The process of biomass combustion involves a series of physical and chemical phenomena strictly coupled with each other and, irrespective of the complexity of the combustion technology and fuel characteristics, they can be divided in: initial heating, moisture evaporation, devolatilization of volatile matter ad char formation, heterogeneous and homogeneous reactions and bed shrinkage. While these phenomena proceed, the gases flowing through the packed bed and the biomass particles exchange heat and mass between each other. Under a mathematical point of view the simulation model is a 1-D system of partial differential equations (PDE’s). To solve this system, the calculation domain and the PDE’s have been discretized to obtain an algebraic system of equations. The calculation domain was divided into a number of non-overlapping control volumes which surround each grid point. In the meshed geometry, obtained with this procedure, all the variables are defined at the grid points. To discretize the diffusion term of the equations a piecewise linear profile for the variables was assumed, whereas for the convective term the upwind scheme was adopted. In this scheme, the internal conditions of the cell in term of concentration, temperature, velocity and density define the output of the calculation node. Once the system has been discretized, the Modified Newton Method was applied to minimize the equation residuals and find the solution vector. To come to the formulation of the simulation program an accurate literature review on biomass combustion modeling and experiments has been done. This part represents a complete outline on the state of the art on biomass combustion modeling and experiments and enabled us to make the right decisions regarding which mathematical formulations to adopt for the simulation of the different phenomena. The last part of the model development was its validation against experimental results. The comparison between the simulation outcomes and the experimental measurements showed good prediction capability of the developed program and allowed its utilization with the aim to study biomass bed combustion on moving grates furnaces. With this purpose a series of six simulations were performed and their results were presented and discussed. The simulations took into account the same kind of woody biomass with two different amounts of moisture and under different operational conditions in terms of inlet air flow rate and temperature. The results have shown that a higher moisture content increases the combustion time since it reduces the bed temperature and slows down the combustion reaction rate; moreover, a reduction of the inlet air flow rate reduces the combustion time in case of reaction limited regime because of the reduction of the cooling effect of the gases that pass through the bed. Finally, the utilization of pre-heated air reduces the duration of the combustion process because the biomass bed at the reaction front is already drier and warmer. This ensures a higher combustion rate. To conclude it has to be considered that, the outcomes of the developed model, in terms of gas temperature, composition and flow rate, are structured to be used as inlet data for a Computational Fluid Dynamics (CFD) model of the gaseous phase combustion in the chamber above the solid bed, in order to have a comprehensive understanding of the biomass combustion dynamics

    Large-scale Plinian eruptions of the Colli Albani and the Campi Flegrei volcanoes : insights from textural and rheological studies

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    In this study we investigated the mechanisms responsible for generating largescale Plinian eruptions. First, a detailed discussion of the state of the art of textural and rheological studies, explaining the main theories applied in the present work Then, eruptions with different compositions, and different viscosities, are chosen: phono-tephrites (Pozzolane Rosse) and tephri-phonites (Pozzolane Nere) from the Colli Albani volcano and trachytes (Agnano Monte Spina) from the Campi Flegrei caldera. All these magmas, despite their variability in chemistry and textural parameters, generate high explosive eruptions accompanied by caldera-forming events. Following an introductory part explaining the main features of the Colli Albani volcano, concerning geological setting, geochemical background and volcanic stratigraphy, we carried out combined investigation of textural, physical and chemical characteristics of scoria clasts (density, Vesicle Size Distributions, Crystal Size Distribution, viscosity), structural features of the deposit (grain-size, maximum clast size, composition) and eruption parameters (ejected volume, column height and discharge rate) of two of the largest ignimbrites of the Colli Albani volcano: the Pozzolane Rosse (RED, 457±4 ka) and the Pozzolane Nere (PNR, 407±4 ka) ignimbrites. Scoria clasts were analyzed in order to quantify textural features in scoriae from individual stratigraphic levels and to measure changes in vesicularity and crystallinity during the major shifts in eruptive intensity and style at Colli Albani volcano. Particular attention was given to the PNR fallout phase to reconstruct the main triggering factors and the first phases of the eruption. In order to evaluate the influence of the viscosity during the rise and the effect of crystal on the rheology itself, we carried out experiments with a concentric cylinder viscometer on the remelted PNR fallout. At high temperatures (1100-1225° C) the viscosity falls within the range 101.04 - 103.64 Pa s, while at low temperature (690-800° C) it ranges between 109.23 -1012 .15 Pa s. The effect of the crystals was evaluated by isothermal crystallization experiments in the region of subliquidus, in a range of T between 1193 and 1240° C at constant strain rate of 0.1 s-1. The experimental products were analyzed by the microprobe chemical analyses and observed under an optical microscope and scanning electron (SEM) for the textural analysis. The mineralogical assembly is constituted by the constant presence of leucite and iron oxides. The total percentage of the crystalline phases varies between about 6-22 % depending on the experimental temperature. On the basis of chemical and textural analysis, a model has been developed to predict the variation of the viscosity of the suspension liquid + crystals + bubbles to different water contents along the entire eruption of PNR. The relative influence of magma internal dynamic (viscosity changes) versus external factors (i,e, the vent diameter) responsible for the fall out-flow transition are discussed. We calculated the decompression rates, through the VNDs and determining some peculiar properties of the magma (e.g. diffusivity, density of the magma, surface tension). The decompression rates for the PNR are very fast and tend to decrease arising along the eruption. Subsequently, an implemented version of Conflow model (Mastin and Ghiorso 2000) called Confort2 was presented. The main modifications concern the liquid viscosity and crystal-bearing rheology determination, as well as the fragmentation criteria. The modified Fortran version Confort2 formulated can be applied to all natural magmas compositions, also including the peralkaline melts (pantelleritites) excluded in the original version. Furthermore, the crystal-bearing rheology was improved adding the effect of crystal shape on the rheology of natural magmatic suspensions and expanding the crystal content range in which it could originally be modeled (the original version of Confort works for crystal content up to 30%). This Fortran modified version Confort2 was applied on Pozzolane Nere eruption. Based on the investigations and on simulations, a model for the volcanological evolution of the Colli Albani ignimbrite eruptions is then presented. Then, we analyzed the textural characteristics and physical properties of the three major fallouts (A1, B1bottom and top, D1) and on the respective pyroclastic flows and surges (A2, B2, D2) of the Agnano Monte Spina eruption. The aim of this study was to relate the textural features of the deposit to intrinsic parameters of the magma during ascent along the conduit and to understand to what extent, if any, changes in the intrinsic properties of the magma may have affected the course of the eruption for the Agnano Monte Spina case. A combination of field, grain-size, density, Vesicle size distribution, Crystal size distribution, fine-ash morphologies and experimental viscosity investigations was carried out. The results of this study lead us to propose an eruptive scenario, taking particularly into account the role of volatiles into the different transitions between sustained and collapsed column. FTIR analyses show initial water content for A, B and D members of 1.77, 2.12 and 2.72 wt% (MIs, Arienzo, pers.comm.) and residual water content of 0.88-0.75 wt% (A1-A2), 0.72-0.60 wt% (B1-B2), 0.81-0.74 wt% (D1-D2). Isothermal viscosity measurements in the subliquidus region and their extrapolation at the eruptive temperature of 827°C and 945° C under different water contents, allow us to estimate the effect of crystals and vesicles on the AMS magmas. At estimated eruptive conditions and water content, viscosity of AMS magma reaches very high values compatible with the eruptive style of the eruption. Fragile fragmentation can be expected to occur. Values of viscosity of the AMS suspensions of the various members do not show variations greater than 0.6 logPa s as a function of crystal or bubble content. We can hence suggest that changes in viscosity during the eruption do not contribute significantly to variations in the eruption dynamics. We calculated the decompression rates which present a non-linear behavior. In general, the AMS eruption velocities are lower than the PNR ones (up to 120 m/s for D member), closer to the standard values for Plinian eruptions and mass discharges are comparable with those expected, ranging between 107-108 kg/s. A reconstruction of the eruptive sequence of the AMS eruption was then performed based on all textural, stratigraphic and rheological analyses. Finally, we presented a comparison between textural and rheological results of PNR and AMS eruptions, with special attention to the analyses of the transitions from sustained to collapsed column

    Study of seawater intrusion in the coastal areas of Circeo National Park and Litorale Romano Natural Reserve, for the implementation of numerical modeling methods

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    Coastal plains represent the most populated areas of the world because they allow an industrial, urban and agricultural development. Groundwater is the main resource in coastal plains and it can satisfy the water demand for these activities. Coastal aquifers represent the place where continental freshwater and seawater meet. Freshwater tends to overly seawater because of its lower density, creating a fragile balance. Nevertheless some processes, both natural and anthropic, can perturb this balance determining groundwater salinization. The main human induced salinization process is the upconing. Natural processes can be the lateral intrusion, evaporite dissolution, fossil water contamination, sea spray aerosol deposition and salt-wedge intrusion in river mouths. Last two processes were deepened in the present study because they are usually not so diffused in regional researches. The aim of this thesis was the study of groundwater salinization induced by rivers or anthropic canals, determined by the wind action or the variation of fluvial discharge rate in time, in areas where protected and anthropic areas coexist: the Tiber Delta and the Pontina Plain. The areas were chosen because they exhibit analogies: both are composed by multi-layered sedimentary aquifers and coastal morphology is strongly affected by reclamation works of the past centuries. The major difference is represented by the presence of different hydrological bodies: in the Tiber Delta area a great river is present and it influences salinization mechanisms in the hydrogeological system, whereas in the Pontina Plain lakes and reclamation canals determine the distribution and movement of seawater. This study was developed with several methods, such as hydrological and hydrogeological surveys, multitemporal chemo-physical surveys of groundwater, hydrochemical surveys, remote sensing techniques, statistical analyses about meteorological data and the use of the most innovative techniques of numerical modeling. In the Tiber Delta area the importance of the westerly winds for the salinization processes was investigated. In fact the winds determine both a salt-wedge emplacement in the Tiber mouth during the falls, and a groundwater salinization in the Litorale Romano Natural Reserve pine forest because of sea spray aerosols deposition. The salt-wedge presence in the Tiber River, noticed up to 8.8 km from the Tiber mouth, is supposed to be the more likely reason of the seawater intrusion processes identified in the alluvial area of Ostia Antica. Furthermore regional hydrochemical analyses permitted to identify freshening processes ascribable to ionexchange, related to the presence of historical solar salt works in the Ostia Antica area. In the Pontina Plain, along the coastal area which hosts the Circeo National Park, salinization resulted linked to the presence of seawater in reclamation canals and lakes. As suggested by the dissertation title, the final aim of the work was the implementation of a numerical model, to detect salinization processes. The use of numerical modeling is a further investigation tool to analyze and quantify what happens in a complex hydrogeological system. The implementation of numerical modeling was performed using the software FEFLOW 6.0, to understand the relationships between groundwater and a reclamation canal salinization. The 2D model, implemented in a transient flow-mass transport state, was located at the Moscarello Canal mouth (Pontina Plain), where a salt-wedge intrusion was noticed. The canal resulted to be subject to a strong discharge modification, which is able to determine a hydraulic gradient and a consequent mass transport in the adjacent aquifer. This transport through the canal bottom resulted able to induce the movement of a saline plume present in the aquifer, determining hence an enhancement of salinity values collected in a piezometer

    Application of quantitative hydrogeological methodologies in northern sector of Vulsini

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    Perythirrenic volcanic aquifers of Central Italy are important resources for the local water supply. The optimal management of this resource is closely related to the knowledge of groundwater hydrological dynamics. The increasing urbanization, industrialization and agricultural withdrawals lead to several management problems such as the depletion of groundwater and deterioration of water quality. Data about pronounced decreasing in springs discharge and in piezometric levels were described in these aquifers during the last twenty years (Capelli et al. 2005). A detailed hydrogeological survey was performed in umbrian sector of Vulsini Mounts to evaluate the quantitative conservation of the drinking resource in compared to previous works (Pagano et al. 2000, Capelli et al 2005). Several authors focused their attention on natural contamination problems of volcanic aquifers exploited for water supply. Most of studies concern water quality lowering by fluorine and arsenic occurrence due to geogenic contamination. On the contrary shallow aquifers water quality is often affected by anthropogenic activities, i.e. common contamination is due to nitrate in agricultural territory or heavy metal pollution close to industrial areas. Arpa Umbria detected anomalous concentrations of aluminum and iron in volcanic aquifer of the area near Orvieto in January 2010. Analyzed samples did not fulfil guidelines for water human consumption (98/83/EC implemented in Italy with D. Lgs 31/2001), then the authorities forbid the use of public water for drinking use.Al and Fe occur as colloids according to detected pH (6,5-7,5) and oxidizing Eh conditions. Another study area, characterized by similar volcanological and hydrogeological features and by the same colloids contamination in groundwater, was searched to understand similarities in the causes and processes of natural contamination of shallow aquifers near Orvieto. The second monitoring area was detected on the NE flank of Roccamonfina Volcano (Campania Region, Central Italy)

    Hydrogeologic responses to seismic events : three case studies in Italy

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    Libri : pratiche artistiche ed editoriali a Torino nei decenni sessanta e settanta

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    La relazione tra artisti e libri costituisce un aspetto centrale degli studi sui decenni Sessanta e Settanta. Le prime proposte critiche degli anni Settanta analizzano il tema alla luce di un rinnovamento delle procedure artistiche e del concetto di opera, rispetto alle quali il libro assume nuovi statuti: “luogo della ricerca”, “lavoro d'arte”, “libro d'artista”. Dopo la cesura degli anni Ottanta, gli anni Novanta segnano l'aprirsi di una nuova stagione di interesse per questi materiali dalla natura ibrida; risalgono a questi anni l’individuazione di alcune significative questioni critiche e la prima considerevole opera di repertorializzazione, in cui si iscrive ancora oggi la fortuna di un genere. Restano tuttavia insolute alcune questioni di definizione intorno alle quali il dibattito è ancora aperto. Soprattutto, risulta ancora lacunoso lo stato degli studi di storia dell'arte, che a tutt'oggi non sembrano interessarsi di una questione affidata agli specialisti del genere. Emerge, dunque, la necessità di ricomporre questa frattura, con lo scopo di fornire un nuovo contributo all'analisi critica di questi oggetti d'arte e di proporre una nuova metodologia di indagine che consideri i “libri d'artista” come documenti per una storia dell'arte contemporanea. Il caso torinese, per la vivacità delle vicende artistiche ed editoriali che lo caratterizza, mette in luce un tessuto di esperienze che attraversano due decenni, descrivendo la storia di una progressiva trasformazione. Gli anni Sessanta si aprono all'insegna dell'attività della casa editrice Einaudi nello specifico della collana «Opere di maestri contemporanei», con la pubblicazione tra il 1957 e il 1965 di cinque raccolte di opere grafiche di altrettanti maestri del Novecento in edizioni di particolare pregio. A questo modello comincia a contrapporsi un'idea diversa di libro d'arte, caratterizzata dalla diretta partecipazione degli artisti alla progettazione e, in alcuni casi, alla realizzazione dello stesso. Simili esperienze maturano nel laboratorio di Ezio Gribaudo presso la poligrafica Fratelli Pozzo di Moncalieri, insieme ad artisti come Alechinsky e Jorn, e assumono i contorni di una vicenda sintomatica di quel processo di ibridazione tra pratiche artistiche ed editoriali che assumerà formule più avanzate. La cesura, in questo senso, avviene tra il 1966 e il 1969. In questo segmento si inseriscono le esperienze di alcuni artisti come Paolini, Pistoletto, Lora Totino e De Alexandris: al libro-opera si affiancano materiali assimilabili al manifesto programmatico, dell'opera a stampa prodotta in più esemplari e al multiplo. L'esperienza degli artisti trova una corrispondenza nelle edizioni Geiger dei fratelli Spatola, in particolare nei libri della collana Geiger Sperimentale: un progetto che si articola tra poesia sperimentale e arti visive, dando luogo ad un'attività esoeditoriale che intrattiene con Torino importanti relazioni, definendo uno scambio con altre geografie artistiche. A partire dai primissimi anni Settanta si intensifica il numero di esperienze di natura editoriale basate sull'intervento dell'artista. Gli interlocutori sono i galleristi, che operano seguendo percorsi diversificati: da un lato quelle gallerie che, come Sperone e Martano, promuovono il “libro d'artista” nel contesto di una più strutturata attività editoriale; dall'altro un fronte composito, con LP 220, Stein e Persano, che si inserisce in diversa misura nel panorama dei “libri d'artista” offrendo esempi di interesse (come i libri di Fabro e Ciam, o la serie di tre libri di Paolini, Parmiggiani e Gastini) tuttavia non riconducibili ad un progetto univoco. Chiude il profilo di questa vicende l'esperienza di Einaudi Letteratura, avviata nel 1969 su iniziativa di Giulio Bollati e di Paolo Fossati: un progetto di opere appartenenti ai settori della letteratura, delle arti visive, del teatro e della musica, in cui si inserisce una serie di libri dedicati ad artisti contemporanei realizzati in dialogo con gli artisti o ad essi affidati, come nei casi di Munari, Paolini, Penone e Fabro. È in quest'esperienza che precipita il portato innovativo di una stagione artistica approdata all'editoria ufficiale

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