Situación laboral actual de los terapeutas ocupacionales egresados de la Universidad del Rosario entre los años 1996 al 2002, que residen actualmente en Bogotá

Este trabajo de grado se encuentra dirigido al reconocimiento de la situación laboral de los Terapeutas Ocupacionales egresados de la Universidad del Rosario entre los años 1996 al 2002, que residen actualmente en la cuidad de Bogotá. Dentro de la investigación de toman aspectos como las áreas y funciones de mayor incidencia de estos profesionales, el salario devengado y los estudios posteriores realizados. Esta es una investigación de carácter cualitativo, la cual se llevo a cabo mediante la aplicación de una encuesta telefónica a una muestra de 27 profesionales seleccionadas de la base de datos del Programa de Terapia Ocupacional. Las conclusiones del estudio abarcan desde las principales áreas de desempeño que son: salud y educación, funciones: atención directa en instituciones y salarios devengados entre 2 y 3 salarios mínimos.

Isotope shifts and hyperfine structure in the 555.8-nm S-1(0) -> P-3(1) line of Yb

We apply our technique of using a Rb-stabilized ring-cavity resonator to measure the frequencies of various spectral components in the 555.8-nm 1S0-->3P1 line of Yb. We determine the isotope shifts with 60 kHz precision, which is an order-of-magnitude improvement over the best previous measurement on this line. There are two overlapping transitions, 171Yb(1/2-->3/2) and 173Yb(5/2-->3/2), which we resolve by applying a magnetic field. We thus obtain the hyperfine constants in the 3P1 state of the odd isotopes with a significantly improved precision. Knowledge of isotope shifts and hyperfine structure should prove useful for high-precision calculations in Yb necessary to interpret ongoing experiments testing parity and time-reversal symmetry violation in the laws of physics.

WB Yeats: No Country for Old Men

I originated, developed and wrote this one-hour documentary for RTE Television on newly discovered aspects of the life of WB Yeats. I am credited as producer and co-writer.

JR WB ba

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to sub-rounded. Rotation structures are common in this sample, especially around larger clasts. Lineations and grain crushing is also present within this sample. A few comet structures can also be seen.

J.R WB-3a

Brown sediment with two main domains; a coarse grained domain and a fine grained domain. Clast size in the fine grained domain is mainly small. The coarser domain contains clasts ranging from small to large in size. The clast shape ranges from angular to rounded. Necking structures are commonly seen in the coarser domain. This domain also contains many rotation structures and lineations. The fine grained domain exhibits multiple water escape pathways, along with lineations. There are also minor amounts of grain crushing present within this sample.

J.R WB-6c

Brown sediment with clasts ranging from small to large in size. Grain shape ranges from angular to rounded. Lineations are abundant within this sample. Rotation structures can also be seen. Necking structures, comet structures, and grain crushing can also be seen in minor amounts.

J.R WB-7a

Brown sediment with clasts ranging from small to large. Grain shape ranges from angular to rounded. Rotation structures and necking structures are common throughout this sample. Lineations can also be seen throughout the sample, along with minor amounts of grain crushing and comet structures.

J.R. WB-2

Dark brown sediment with clasts ranging from small to large. Clast shape ranges from angular to rounded. Comet structures and lineations can be commonly seen throughout the sample. There are minor amounts of rotation structures also present. The sample contains clasts that are generally well dispersed.

WB-3b

Dark brown sediment with well dispersed clasts. The clasts range from small to large in size and sub-angular to sub-rounded in shape. The sample is abundant in rotation structures and lineations. It also contains comet structures and minor amounts of grain stacking.

WB-4

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from sub-angular to sub-rounded. Rotation structures are abundant in this sample. They are seen around small and large clasts. A few necking structures can also be seen. These typically occur between larger aggregates. Lineations, comet structures, and grain crushing can also be seen in minor amounts.

WB-6a

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to sub-rounded. Necking structures are abundant within this sample, mainly between larger aggregates. Some rotation structures and lineations can also be seen. Comet structure and grain stacking can be seen in minor amounts.

WB-6b

Dark brown sediment with clasts ranging from small to large in size. Grain shape ranges from sub-angular to rounded. Rotation structures are common throughout the sample. Some necking structures are also present between large and medium sized aggregates. Lineations and grain stacks are also present in minor amounts.