Una agencia en la cultura física urbana de entreguerras : La trayectoria de Juan Bautista Arrospidegaray en Rosario

El presente trabajo tiene por objetivo explorar las formas de la educación física en Rosario durante la entreguerras. Especialmente nos interesa reconstruir la trayectoria de un maestro de esgrima que estuvo en el centro del desarrollo de estas actividades a lo largo de este período, experimentando en su propia trayectoria las transformaciones de la cultura física urbana. Juan Bautista Arrospidegaray nació en Rosario en 1876 y fue formado como maestro de esgrima. Su trayectoria se inició en una academia privada de esgrima de la ciudad y continuó con la organización de Batallones Escolares del Centenario. Se unió al Cuerpo de Bomberos de Rosario, fue director del Departamento Municipal de Esgrima, miembro de la Comisión Directiva del Tiro Federal de Rosario, profesor de educación física de los colegios confesionales San José y Sagrado Corazón de Rosario, fundador del grupo Vanguardias de la Patria de Rosario, Director del Stadium Municipal e Inspector de Plazas y Campos de Deportes de la Municipalidad de Rosario. Arrospidegaray promovió y se vinculó muy estrechamente con la cultura física de Rosario y ocupó a lo largo de su recorrido profesional algunos puestos clave que le permitieron incidir y prestar cierta tónica al desarrollo de las actividades físicas de la ciudad. La siguiente ponencia intenta reconstruir a través de su figura, las variaciones, las continuidades, los conflictos y las reconfiguraciones de la cultura física de Rosario a lo largo de casi medio siglo

Mineralogy and geochemistry of Mg-phyllosilicates from Middle Valley, northern Juan de Fuca Ridge

We present results of a detailed mineralogical and geochemical study of the progressive hydrothermal alteration of clastic sediments recovered at ODP Site 858 in an area of active hydrothermal venting at the sedimented, axial rift valley of Middle Valley (northern Juan de Fuca Ridge). These results allow a characterization of newly formed phyllosilicates and provide constraints on the mechanisms of clay formation and controls of mineral reactions on the chemical and isotopic composition of hydrothermal fluids. Hydrothermal alteration at Site 858 is characterized by a progressive change in phyllosilicate assemblages with depth. In the immediate vent area, at Hole 858B, detrital layers are intercalated with pure hydrothermal precipitates at the top of the section, with a predominance of hydrothermal phases at depth. Sequentially downhole in Hole 858B, the clay fraction of the pure hydrothermal layers changes from smectite to corrensite to swelling chlorite and finally to chlorite. In three pure hydrothermal layers in the deepest part of Hole 858B, the clay minerals coexist with neoformed quartz. Neoformed and detrital components are clearly distinguished on the basis of morphology, as seen by SEM and TEM, and by their chemical and stable isotope compositions. Corrensite is characterized by a 24 Å stacking sequence and high Si- and Mg-contents, with Fe/(Fe+Mg) ratio of = 0.08. We propose that corrensite is a unique, possibly metastable, mineralogical phase and was precipitated directly from seawater-dominated hydrothermal fluids. Hydrothermal chlorite in Hole 858B has a stacking sequence of 14 Å with Fe/(Fe+Mg) ratios of ? 0.35. The chemistry and structure of swelling chlorite suggest that it is a corrensiteychlorite mixed-layer phase. The mineralogical zonation in Hole 858B is accompanied by a systematic decrease in d18O, reflecting both the high thermal gradients that prevail at Site 858 and extensive sediment-fluid interaction. Precipitation of the Mg-phyllosilicates in the vent region directly controls the chemical and isotopic compositions of the pore fluids. This is particularly evident by decreases in Mg and enrichments in deuterium and salinity in the pore fluids at depths at which corrensite and chlorite are formed. Structural formulae calculated from TEM-EDX analyses were used to construct clay-H2O oxygen isotope fractionation curves based on oxygen bond models. Our results suggest isotopic disequilibrium conditions for corrensite-quartz and swelling chlorite-quartz precipitation, but yield an equilibrium temperature of 300° C ± 30° for chlorite-quartz at 32 m below the surface. This estimate is consistent with independent estimates and indicates steep thermal gradients of 10-11°/m in the vent region.

Ogasawara winter Sr/Ca and U/Ca data of coral core OGA-02-1 and PDO reconstruction (coral-geoduck index)

The Pacific Decadal Oscillation (PDO), the leading mode of sea surface temperature (SST) anomalies in the extratropical North Pacific Ocean, has widespread impacts on precipitation in the Americas and marine fisheries in the North Pacific. However, marine proxy records with a temporal resolution that resolves interannual to interdecadal SST variability in the extratropical North Pacific are extremely rare. Here we demonstrate that the winter Sr/Ca and U/Ca records of an annually-banded reef coral from the Ogasawara Islands in the western subtropical North Pacific are significantly correlated with the instrumental winter PDO index over the last century. The reconstruction of the PDO is further improved by combining the coral data with an existing eastern mid-latitude North Pacific growth ring record of geoduck clams. The spatial correlations of this combined index with global climate fields suggest that SST proxy records from these locations provide potential for PDO reconstructions further back in time.

Mineral composition of 356 sediment profiles from the Arctic seas

This data set contains the mineralogical analyses (binocular counting) of the 100-50 µm grain size fraction from bottom sediments collected by scientists of the V.P. Zenkovich Laboratory of Shelf and Sea Coasts (P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences) during the Project ''Arctic Shelf of the Eurasia in the Late Quaternary'' in a number of expeditions to the Barents, Kara, East Siberian and Chukchi Seas on board research vessels R/V Professor Shtokman, H/V Dmitry Laptev, H/V Malygin, and icebreaker Georgy Sedov between 1978 and 1990. The analyses have been carried out according to the methods published by Petelin V.P. (1961) in the Analytical Laboratory of the P.P. Shirshov Institute of Oceanology. Archiving and electronic publication was performed through a data rescue by Evgeny Gurvich in 2003.

Chemical composition of 169 sediment profiles from the Arctic seas

This data set contains chemical composition of bottom sediments collected by scientists from the V.P. Zenkovich Laboratory of Shelf and Sea Coasts (P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences) during the Project ''Arctic Shelf of the Eurasia in the Late Quaternary'' in a number of expeditions to the Barents, Kara, East Siberian and Chukchi Seas on board research vessels R/V Professor Shtokman, H/V Dmitry Laptev, H/V Malygin, and icebreaker Georgy Sedov between 1978 and 1990. The analyses have been carried out in the Analytical Laboratory of the P.P. Shirshov Institute of Oceanology. Archiving and electronic publication was performed through a data rescue by Evgeny Gurvich in 2003.

Discarge compilation from The Global River Discharge (RivDIS) Project

The Global River Discharge (RivDIS) data set contains monthly discharge measurements for 1018 stations located throughout the world. The period of record varies widely from station to station, with a mean of 21.5 years. These data were digitized from published UNESCO archives by Charles Voromarty, Balaze Fekete, and B.A. Tucker of the Complex Systems Research Center (CSRC) at the University of New Hampshire. River discharge is typically measured through the use of a rating curve that relates local water level height to discharge. This rating curve is used to estimate discharge from the observed water level. The rating curves are periodically rechecked and recalibrated through on-site measurement of discharge and river stage.

Demostración del sentido verdadero de las autoridades de que se vale el Doctor Don Juan Antonio de Llorente, canónigo de la Catedral de Toledo, en el tomo I de "Las noticias históricas de las tres provincias vascongadas" : y de lo que en verdad resulta de los historiadores que cita, con respecto solamente al Muy Noble y Muy Leal Señorío de Vizcaya / por Francisco de Aranguren y Sobrado.

Digitalización Vitoria-Gasteiz Archivos y Bibliotecas Abril 1994 18-6

Repetitio. ru. [et] ca. p[er] v[est]ras de donationib[us] int[er] virum [et] vxorem / edita a Joa[n]ne lupi de palacios ruuios ...

Sign.: []2, a-z8, [et]8, [cum]8, [rum]8, 2a-2d8, 2e-2f6, A10, a8, b10

Biografia de Juan de Juanes : Su vida y obras, sus discipulos e influencias...

Ejemplar deteriorado y falto de cubierta

Sermon panegirico que en la solemne fiesta que celebró la Santa Iglesia Metropolitana de Valencia por la ... beatificacion de ... Juan de Ribera ... en el dia 27 de agosto ... de 1797

Hay un ejemplar encuadernado con: Sermon en la Solemne fiesta que en honra de la canonización de S. Josef de Calasanz, fundador de las Escuelas Pias celebró la ... Parroquia de los Santos Juanes (NP08/35).

Compendio historico-chronologico de la vida virtudes y milagros del Beato Padre Joseph de Calasanz fundador ... de la Religion de Clerigos Regulares Pobres ... de las Escuelas Pìas

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