Aprendizaje reflexivo y colaborativo (ARC) y TAC en la formación de personas adultas : hacia la formación de un alumnado competente con ayuda de las TAC.

Resumen tomado de la publicación

El arc??n literario de dos generaciones

El presente documento recoge los textos creados, tanto por ni??osy ni??as como por mayores, para el Taller Intergeneracional Art??stico-Literario organizado por la Concejal??a de la Infancia del Ayuntamiento de Coslada (Madrid). La experiencia tuvo como base el inter??s de que esas generaciones dejen de ser independientes entre si y constituyan una parte activa de la vida social. La cooperaci??n y la creatividad fueron los soportes sobre los que se sustent?? esta idea.

'Arc Iris'.

Programa emitido el 28 de septiembre de 1994

La Fundació l'Arc Música i la nova Escola Municipal de Can Ponsic. 'La Fundació l'Arc Música y la nueva Escola Municipal de Can Ponsic'.

Resumen basado en el del autor

L'arc : quadern informatiu de l'Institut de Ciències de l'Educació de la Universitat de les Illes Balears

Publicación cerrada : 1996-2002.

Comunicaci??n y autismo : intervenci??n a trav??s del Programa Arc??n

Se describe una experiencia llevada a cabo en el CEIP Arias Montano (Badajoz) que consisti?? en el uso de un software concreto, el Programa Arc??n, para favorecer la comunicaci??n a trav??s de un soporte digital de un alumno con trastorno de espectro autista escolarizado en segundo curso de primaria. Se observ?? una mejora de la socializaci??n del alumno, de su integraci??n y de su capacidad comunicativa

Propuestas de geometr??a para Educaci??n Infantil en la Aplicaci??n de Recursos al Curr??culum (ARC)

Resumen basado en el de la publicaci??n

Propiedades psicom??tricas de la escala ARC-INICO para evaluar la autodeterminaci??n

Resumen basado en el de la publicaci??n

Mathematical and electrical analysis of pulsed tones

This paper discusses a study conducted to perform a mathematical analysis and an electrical analysis of pulsed tones to determine which type of pulsed tone is most suitable.

Acoustic reflex measurements in normals and Meniere's Syndrome using pulsed stimuli

This paper reviews a study to determine the maximum rate the acoustic reflex can follow pulsed stimuli in normal hearing subjects and in subjects with Meniere's Syndrome.

Acoustic reflex measurements in normals and Meniere's Syndrome using pulsed stimuli

This paper reviews a study to determine the maximum rate the acoustic reflex can follow pulsed stimuli in normal hearing subjects and in subjects with Meniere's Syndrome.

Pb-210-Ra-226 and Ra-228-Th-232 systematics in young arc lavas: implications for magma degassing and ascent rates

New data show that island arc rocks have (Pb-210/Ra-226)(o) ratios which range from as low as 0.24 up to 2.88. In contrast, (Ra-22S/Th-232) appears always within error of I suggesting that the large Ra-226-excesses observed in arc rocks were generated more than 30 years ago. This places a maximum estimate on melt ascent velocities of around 4000 m/year and provides further confidence that the Ra-226 excesses reflect deep (source) processes rather than shallow level alteration or seawater contamination. Conversely, partial melting must have occurred more than 30 years prior to eruption. The Pb-210 deficits are most readily explained by protracted magma degassing. Using published numerical models, the data suggest that degassing occurred continuously for periods up to several decades just prior to eruption but no link with eruption periodicity was found. Longer periods are required if degassing is discontinuous, less than 100% efficient or if magma is recharged or stored after degassing. The long durations suggest much of this degassing occurs at depth with implications for the formation of hydrothermal and copper-porphyry systems. A suite of lavas erupted in 1985-1986 from Sangeang Api volcano in the Sunda arc are characterised by deficits of Pb-210 relative to Ra-226 from which 6-8 years of continuous Rn-222 degassing would be inferred from recent numerical models. These data also form a linear (Pb-210)/Pb-(Ra-226)/Pb array which might be interpreted as a 71-year isochron. However, the array passes through the origin suggesting displacement downwards from the equiline in response to degassing and so the slope of the array is inferred not to have any age significance. Simple modelling shows that the range of (Ra-226)/Pb ratios requires thousands of years to develop consistent with differentiation occurring in response to cooling at the base of the crust. Thus, degassing post-dated, and was not responsible for magma differentiation. The formation, migration and extraction of gas bubbles must be extremely efficient in mafic magma whereas the higher viscosity of more siliceous magmas retards the process and can lead to Pb-210 excesses. A possible negative correlation between (Pb-210/Ra-226)(o) and SO2 emission rate requires further testing but may have implications for future eruptions. (C) 2004 Elsevier B.V. All rights reserved.

Pb-210-Ra-226 and Ra-228-Th-232 systematics in young arc lavas: implications for magma degassing and ascent rates

New data show that island arc rocks have (Pb-210/Ra-226)(o) ratios which range from as low as 0.24 up to 2.88. In contrast, (Ra-22S/Th-232) appears always within error of I suggesting that the large Ra-226-excesses observed in arc rocks were generated more than 30 years ago. This places a maximum estimate on melt ascent velocities of around 4000 m/year and provides further confidence that the Ra-226 excesses reflect deep (source) processes rather than shallow level alteration or seawater contamination. Conversely, partial melting must have occurred more than 30 years prior to eruption. The Pb-210 deficits are most readily explained by protracted magma degassing. Using published numerical models, the data suggest that degassing occurred continuously for periods up to several decades just prior to eruption but no link with eruption periodicity was found. Longer periods are required if degassing is discontinuous, less than 100% efficient or if magma is recharged or stored after degassing. The long durations suggest much of this degassing occurs at depth with implications for the formation of hydrothermal and copper-porphyry systems. A suite of lavas erupted in 1985-1986 from Sangeang Api volcano in the Sunda arc are characterised by deficits of Pb-210 relative to Ra-226 from which 6-8 years of continuous Rn-222 degassing would be inferred from recent numerical models. These data also form a linear (Pb-210)/Pb-(Ra-226)/Pb array which might be interpreted as a 71-year isochron. However, the array passes through the origin suggesting displacement downwards from the equiline in response to degassing and so the slope of the array is inferred not to have any age significance. Simple modelling shows that the range of (Ra-226)/Pb ratios requires thousands of years to develop consistent with differentiation occurring in response to cooling at the base of the crust. Thus, degassing post-dated, and was not responsible for magma differentiation. The formation, migration and extraction of gas bubbles must be extremely efficient in mafic magma whereas the higher viscosity of more siliceous magmas retards the process and can lead to Pb-210 excesses. A possible negative correlation between (Pb-210/Ra-226)(o) and SO2 emission rate requires further testing but may have implications for future eruptions. (C) 2004 Elsevier B.V. All rights reserved.

A narrow band pulsed eddy current instrument for materials testing

The principles of operation of an experimental prototype instrument known as J-SCAN are described along with the derivation of formulae for the rapid calculation of normalized impedances; the structure of the instrument; relevant probe design parameters; digital quantization errors; and approaches for the optimization of single frequency operation. An eddy current probe is used As the inductance element of a passive tuned-circuit which is repeatedly excited with short impulses. Each impulse excites an oscillation which is subject to decay dependent upon the values of the tuned-circuit components: resistance, inductance and capacitance. Changing conditions under the probe that affect the resistance and inductance of this circuit will thus be detected through changes in the transient response. These changes in transient response, oscillation frequency and rate of decay, are digitized, and then normalized values for probe resistance and inductance changes are calculated immediately in a micro processor. This approach coupled with a minimum analogue processing and maximum of digital processing has advantages compared with the conventional approaches to eddy current instruments. In particular there are: the absence of an out of balance condition and the flexibility and stability of digital data processing.