969 resultados para LEY 9 DE 1989


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Declara infundado el recurso de anulación

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Presentation given at the Al-Azhar Engineering First Conference, AEC’89, Dec. 9-12 1989, Cairo, Egypt. The paper presented at AEC'89 suggests an infinite storage scheme divided into one volume which is online and an arbitrary number of off-line volumes arranged into a linear chain which hold records which haven't been accessed recently. The online volume holds the records in sorted order (e.g. as a B-tree) and contains shortest prefixes of keys of records already pushed offline. As new records enter, older ones are retired to the first volume which is going offline next. Statistical arguments are given for the rate at which an off-line volume needs to be fetched to reload a record which had been retired before. The rate depends on the distribution of access probabilities as a function of time. Applications are medical records, production records or other data which need to be kept for a long time for legal reasons.

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Objetivos Mediante un estudio descriptivo transversal, establecer la presencia de una relación entre los niveles de exposición a plaguicidas con la presencia de hallazgos clínicos neurológicos periféricos en personas expuestas ocupacionalmente a estos. Resultados La muestra poblacional fue de 59 trabajadores, en el área rural del municipio del Espinal, Tolima. El 52% de la población refirió usar organofosforados, 32 % carbamatos, 16% organoclorados, y 66% otros grupos de plaguicidas. Los niveles sanguíneos de carbamatos estuvieron presentes en el 7% de la población, organofosforados en el 66% y organoclorados en el 100%. En el 42% de la población se estableció sospecha de neuropatía a partir de los síntomas y en el 92% a partir de los signos. Se estableció asociación estadísticamente significativa entre los niveles sanguíneos de determinados organoclorados con la sospecha de neuropatía periférica a partir de síntomas; la presencia de sensación de pérdida de la fuerza en extremidades y la presencia de alteraciones en los reflejos osteotendinosos. Conclusiones El presente estudio permitió identificar los plaguicidas a los cuales está expuesta la población agrícola del municipio del Espinal así como corrobora el efecto de bioacumulación y biomagnificación de los organoclorados. Adicionalmente, se detectó la presencia de hallazgos sugestivos de compromiso neurológico periférico, con asociaciones significativas entre ciertas anormalidades y determinados organoclorados. Este estudio es una aproximación a la relación entre la exposición a plaguicidas de la población agrícola de la zona rural del municipio del Espinal con la secuelas neurológicos periféricas asociadas a esta.

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El siguiente documento da a conocer el comportamiento de la Inversión Extranjera Directa (IED) de los países denominados BRIC (Brasil, Rusia, India y China) en Colombia. De acuerdo a lo anterior, en el presente trabajo, se realizó un análisis general de la IED entrante en el país suramericano que buscaba establecer los principales inversores; además de determinar los sectores más atractivos. Posteriormente, se observó la magnitud de la inversión que realizan los países BRIC en Colombia y en el mundo, con el fin de efectuar una comparación que permitiera determinar que tan significativa es la inversión que se realiza en el Estado Colombiano frente a la que es efectuada por estas naciones a nivel global. Igualmente, se consideró las industrias a las que la IED está dirigida, el grado de beneficio que representa para la población y si existe la posibilidad de enfocarla hacia otros sectores estratégicos o si se recomienda encauzarla hacia aquellos que hoy en día son el principal foco de inversión.

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Monográfico con el título: 'Repensar el asesoramiento en educación : ¿qué prácticas para los nuevos retos?'. Resumen basado en el de la publicación

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Monográfico con el título: 'Repensar el asesoramiento en educación : ¿qué prácticas para los nuevos retos?'. Resumen basado en el de la publicación

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Monográfico con el título: 'El conocimiento para la enseñanza'. Resumen basado en el de la publicación

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Resumen basado en el de la publicación

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Resumen basado en el de la publicación

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T??tulo tambi??n en ingl??s

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Combined optical and radar observations of two breakup-like auroral events near the polar cap boundary, within 74–76° MLAT and 1210 – 1240 UT (roughly 1540 – 1610 MLT) on 9 Jan. 1989 are reported. A two-component structure of the auroral phenomenon is indicated, with a local intensification of the pre-existing arc as well as a separate, tailward moving discrete auroral event on the poleward side of the background aurora, close to the reversal between well-defined zones of sunward and tailward ion flows. The all-sky TV observations do not indicate a connection between the two components, which also show different optical spectral composition. The 16 MLT background arc is located on sunward convecting field lines, as opposed to the 12–14 MLT auroral emission observed on this day. Although the magnetospheric plasma source (s) of the 16 MLT events are not easily identified from these ground-based data alone, it is suggested that the lower and higher latitude components, may map to the plasma sheet boundary layer and along open field lines to the magnetopause boundary, respectively. The events occur at the time of enhancements of westward ionospheric ion flow and corresponding eastward electrojet current south of 74° MLAT. Thus, they seem to be very significant events, involving periodic (10 min period), tailward moving filaments of field-aligned current/discrete auroral emission at the 16 MLT polar cap boundary.

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We present observations of a transient event in the dayside auroral ionosphere at magnetic noon. F-region plasma convection measurements were made by the EISCAT radar, operating in the beamswinging “Polar” experiment mode, and simultaneous observations of the dayside auroral emissions were made by optical meridian-scanning photometers and all-sky TV cameras at Ny Ålesund, Spitzbergen. The data were recorded on 9 January 1989, and a sequence of bursts of flow, with associated transient aurora, were observed between 08:45 and 11:00 U.T. In this paper we concentrate on an event around 09:05 U.T. because that is very close to local magnetic noon. The optical data show a transient intensification and widening (in latitude) of the cusp/cleft region, as seen in red line auroral emissions. Over an interval of about 10 min, the band of 630 nm aurora widened from about 1.5° of invariant latitude to over 5° and returned to its original width. Embedded within the widening band of 630 nm emissions were two intense, active 557.7 nm arc fragments with rays which persisted for about 2 min each. The flow data before and after the optical transient show eastward flows, with speeds increasing markedly with latitude across the band of 630 nm aurora. Strong, apparently westward, flows appeared inside the band while it was widening, but these rotated round to eastward, through northward, as the band shrunk to its original width. The observed ion temperatures verify that the flow speeds during the transient were, to a large extent, as derived using the beamswinging technique; but they also show that the flow increase initially occurred in the western azimuth only. This spatial gradient in the flow introduces ambiguity in the direction of these initial flows and they could have been north-eastward rather than westward. However, the westward direction derived by the beamswinging is consistent with the motion of the colocated and coincident active 557.7 nm arc fragment, A more stable transient 557.7 nm aurora was found close to the shear between the inferred westward flows and the persisting eastward flows to the North. Throughout the transient, northward flow was observed across the equatorward boundary of the 630 nm aurora. Interpretation of the data is made difficult by lack of IMF data, problems in distinguishing the cusp and cleft aurora and uncertainty over which field lines are open and which are closed. However, at magnetic noon there is a 50% probability that we were observing the cusp, in which case from its southerly location we infer that the IMF was southward and many features are suggestive of time-varying reconnection at a single X-line on the dayside magnetopause. This IMF orientation is also consistent with the polar rain precipitation observed simultaneously by the DMSP-F9 satellite in the southern polar cap. There is also a 25% chance that we were observing the cleft (or the mantle poleward of the cleft). In this case we infer that the IMF was northward and the transient is well explained by reconnection which is not only transient in time but occurs at various sites located randomly on the dayside magnetopause (i.e. patchy in space). Lastly, there is a 25% chance that we were observing the cusp poleward of the cleft, in which case we infer that IMF Bz was near zero and the transient is explained by a mixture of the previous two interpretations.