Agire sui bisogni, condividere responsabilità al tempo di internet: per il disegno di un'applicazione a supporto dello scambio sociale

Dalla volontà di proporre una soluzione al tema delle disabilità fisiche in ambiente cittadino evoluto e tecnologicamente avanzato, è nata l'idea di progettare un'applicazione in grado di generare visibilità attorno ad un tema che dovrebbe progredire nella stessa maniera dello sviluppo tecnologico. Lo scopo di questa tesi è proporre un tentativo concreto per entrare in contatto con una problematica di ordine sociale che lo sviluppo tecnologico dovrebbe tenere in maggiore considerazione. Si vuole cercare di sfruttare Internet come mezzo per enfatizzare un problema concreto come la mancanza di visibilità e coinvolgimento sociale attorno la tematica delle disabilità. I nativi digitali utilizzano costantemente sia social network che piattaforme dedite allo scambio di informazioni e alla creazione di visibilità. Vivono il mondo digitale come una vetrina nella quale potersi mettere in mostra e creare una reputazione. Il mondo digitale, in particolare quello dei social network viene visto dai più come la fonte principale di costruzione dei legami sociali, ciò è sicuramente vero, ma bisogna capire che tipo e quanto profonde possano essere tali relazioni. La mia generazione è cresciuta in un periodo ibrido, coinvolta sia nel mondo analogico sia in quello digitale, molti sono stati risucchiati da un vortice di superficialità e apparenze altamente correlati con gli effetti generati da una società capitalistica perfettamente identificabile nei profili che ogni giorno andiamo a creare per metterci in mostra nei social network. In prima analisi con la collaborazione del Dipartimento disabilità dell'Università di Bologna si era cercato di porre l'attenzione su un approccio più orientativo per venire in contro a problematiche del genere. Qualcosa che permettesse a tutti nella stessa maniera di vivere la realtà accademica e cittadina stimolando l'interazione degli studenti con socialità marginale.

10-Year Survival and Success Rates of 511 Titanium Implants with a Sandblasted and Acid-Etched Surface: A Retrospective Study in 303 Partially Edentulous Patients

Purpose: This retrospective study assessed the 10-year outcomes of titanium implants with a sandblasted and acid-etched (SLA) surface in a large cohort of partially edentulous patients. Materials and Methods: Records of patients treated with SLA implants between May 1997 and January 2001 were screened. Eligible patients were contacted and invited to undergo a clinical and radiologic examination. Each implant was classified according to strict success criteria. Results: Three hundred three patients with 511 SLA implants were available for the examination. The mean age of the patients at implant surgery was 48 years. Over the 10-year period, no implant fracture was noted, whereas six implants (1.2%) were lost. Two implants (0.4%) showed signs of suppuration at the 10-year examination, whereas seven implants had a history of peri-implantitis (1.4%) during the 10-year period, but presented with healthy peri-implant soft tissues at examination. The remaining 496 implants fulfilled the success criteria. The mean Plaque Index was 0.65 (±0.64), the mean Sulcus Bleeding Index 1.32 (±0.57), the mean Probing Depth 3.27 mm (±1.06), and the mean distance from the implant shoulder to the mucosal margin value -0.42 mm (±1.27). The radiologic mean distance from the implant shoulder to the first bone-to-implant contact was 3.32 mm (±0.73). Conclusion: The present retrospective analysis resulted in a 10-year implant survival rate of 98.8% and a success rate of 97.0%. In addition, the prevalence of peri-implantitis in this large cohort of orally healthy patients was low with 1.8% during the 10-year period.

Les juifs dans l'Empire Romain : leur condition juridique, économique et sociale

par Jean Juster

A deep crust–mantle boundary in the asteroid 4 Vesta

The asteroid 4 Vesta was recently found to have two large impact craters near its south pole, exposing subsurface material. Modelling suggested that surface material in the northern hemisphere of Vesta came from a depth of about 20 kilometres, whereas the exposed southern material comes from a depth of 60 to 100 kilometres. Large amounts of olivine from the mantle were not seen, suggesting that the outer 100 kilometres or so is mainly igneous crust. Here we analyse the data on Vesta and conclude that the crust–mantle boundary (or Moho) is deeper than 80 kilometres.

Na 1 Nachlass Max Horkheimer, 242 - Korrespondenzen u.a. mit Bibliothekaren der Deutschen Bibliothek in Rom (p. V 55, 1-303)

1 Brief an Max Horkheimer von der Oberin, Agnes Karll-Verband Ruth Elster, 1959; 1 Brief von Max Horkheimer an Fernanda Alves Diniz, 1959; 4 Briefe zwischen Journalist Walter Dirks, 1950-1955; 1 Interview mit Max Horkheimer, von Journalist, Tel-Aviv Dr. Dolan, 1952; 2 Briefe zwischen Albert Dragstedt und Max Horkheimer, 1959; 17 Briefe zwischen Ria Drevermann und Max Horkheimer, 1948-1957; 4 Briefe zwischen Architekt Wolf Drevermann und Max Horkheimer, 1950-1952; Professor Kurt Rheindorf: 1 Lebenslauf, 1 Manuskript, (1949); 2 Briefe zwischen Dr. Josef E. Drexel und Max Horkheimer, 1958; 3 Briefe zwischen Professor Tom F. Driver und Max Horkheimer, 1966; 12 Briefe zwischen dem DuMont Schuaberg Verlag und Max Horkheimer, 1961-1966; Deutsch-Amerikanischer Beratungs-Ausschuss für das Land Hessen: Drucksachen, Notizen, Protokolle an Max Horkheimer, 1952-1967; 1 Brief an Max Horkheimer von Hartmut Höschel, 1967; 14 Briefe zwischen Deutsche Bibliothek, Brüssel und Max Horkheimer, 1970-1971; 8 Briefe zwischen Deutsche Bibliothek Frankfurt am Main und Max Horkheimer, 1965-1967; 47 briefe zwischen Johannes Vandenrath, Deutsche Bibliothek Mailand und Max Horkheimer, 1968-1973; 51 Briefe zwischen Michael Freiherr Marschall von Bieberstein, Deutsche Bibliothek Rom, und Max Horkheimer, 1968-1973; Deutsche Bibliothek Rom: siehe Marschall von Bieberstein, Michael Freiherr;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 303 - Rechtfertigung gegenüber Professor Hugo von Meltzl über die ausgebliebene publizistische Tätigkeit anlässlich des 100. Geburtstags Arthur Schopenhauers

u.a.: Nordamerikanische Reise; Versetzung in das Konsulat von Hawaii; Eduard Grisebach;

Stable carbon and oxygen isotope record of foraminifera of IODP Site 303-1307

A major tipping point of Earth's history occurred during the mid-Pliocene: the onset of major Northern-Hemisphere Glaciation (NHG) and of pronounced, Quaternary-style cycles of glacial-to-interglacial climates, that contrast with more uniform climates over most of the preceding Cenozoic and continue until today (Zachos et al., 2001, doi:10.1126/science.1059412). The severe deterioration of climate occurred in three steps between 3.2 Ma (warm MIS K3) and 2.7 Ma (glacial MIS G6/4) (Lisiecki and Raymo, 2005, doi:10.1029/2004PA001071). Various models (sensu Driscoll and Haug, 1998, doi:10.1126/science.282.5388.436) and paleoceanographic records (intercalibrated using orbital age control) suggest clear linkages between the onset of NHG and the three steps in the final closure of the Central American Seaways (CAS), deduced from rising salinity differences between Caribbean and the East Pacific. Each closing event led to an enhanced North Atlantic meridional overturning circulation and this strengthened the poleward transport of salt and heat (warmings of +2-3°C) (Bartoli et al., 2005, doi:10.1016/j.epsl.2005.06.020). Also, the closing resulted in a slight rise in the poleward atmospheric moisture transport to northwestern Eurasia (Lunt et al., 2007, doi:10.1007/s00382-007-0265-6), which probably led to an enhanced precipitation and fluvial run-off, lower sea surface salinity (SSS), and an increased sea-ice cover in the Arctic Ocean, hence promoting albedo and the build-up of continental ice sheets. Most important, new evidence shows that the closing of the CAS led to greater steric height of the North Pacific and thus doubled the low-saline Arctic Throughflow from the Bering Strait to the East Greenland Current (EGC). Accordingly, Labrador Sea IODP Site 1307 displays an abrupt but irreversible EGC cooling of 6°C and freshening by ~2 psu from 3.25/3.16-3.00 Ma, right after the first but still reversible attempt of closing the CAS.

Sandra Visser y Thomas Williams, Anselm, (Great Medieval Thinker), Oxford University Press, Oxford, 2009; 303 p. ISBN 978-0-19-530939-3

Fil: Peretó Rivas, Rubén.