991 resultados para Berthaud, 1783


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Se re??ne la escasa informaci??n disponible sobre la educaci??n en el municipio de Algaida en la primera mitad del siglo XIX haciendo especial incidencia sobre la evoluci??n de las escuelas y la escolarizaci??n. Por una parte se detalla la situaci??n entre 1783 y 1833, cuando la educaci??n primaria se encontraba en manos de cl??rigos y maestras solteras, y por otro, el periodo de normalizaci??n de la escolarizaci??n, entre 1833 y 1857. Entre otras cuestiones se recoge la figura de Joan Antoni Mulet Munar, que fue alumno en la Escuela Normal de Maestros de Palma y maestro de la escuela de ni??os a partir de 1852, cuando Margalida Tom??s abandonaba la escuela de ni??as en la que hab??a trabajado como maestra desde 1830, y se incorporaba en su puesto Esperan??a Rossell??, sustitu??da posteriormente por Francisca Mas Rigo. Finalmente se comenta la situaci??n de las escuelas de Pina y Randa.

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Relata-se a ocorrência de Contracaecum pelagicum Johnston & Mawson 1942 (Nematoda, Anisakidae) em um novo hospedeiro, Sula leucogaster Boddaert 1783 (Pelecaniformes, Sulidae), espécie conhecida como atobá. Três machos e três fêmeas dessa espécie de nematódeo foram coletados no regurgito da ave. Pela análise morfológica conclui-se que C. pelagicum era a espécie envolvida no parasitismo. Este é o primeiro relato sobre a ocorrência de nematódeos do gênero Contracaecum em S. leucogaster.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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The Scilla rock avalanche occurred on 6 February 1783 along the coast of the Calabria region (southern Italy), close to the Messina Strait. It was triggered by a mainshock of the Terremoto delle Calabrie seismic sequence, and it induced a tsunami wave responsible for more than 1500 casualties along the neighboring Marina Grande beach. The main goal of this work is the application of semi-analtycal and numerical models to simulate this event. The first one is a MATLAB code expressly created for this work that solves the equations of motion for sliding particles on a two-dimensional surface through a fourth-order Runge-Kutta method. The second one is a code developed by the Tsunami Research Team of the Department of Physics and Astronomy (DIFA) of the Bologna University that describes a slide as a chain of blocks able to interact while sliding down over a slope and adopts a Lagrangian point of view. A wide description of landslide phenomena and in particular of landslides induced by earthquakes and with tsunamigenic potential is proposed in the first part of the work. Subsequently, the physical and mathematical background is presented; in particular, a detailed study on derivatives discratization is provided. Later on, a description of the dynamics of a point-mass sliding on a surface is proposed together with several applications of numerical and analytical models over ideal topographies. In the last part, the dynamics of points sliding on a surface and interacting with each other is proposed. Similarly, different application on an ideal topography are shown. Finally, the applications on the 1783 Scilla event are shown and discussed.