Calidad de vida, bienestar psicológico e imagen corportal en la parálisis de Bell

Tesis doctoral inédita leída en la Universidad Autónoma de Madrid, Facultad de Medicina. Fecha de lectura 10 de Diciembre de 2012

La influencia del género en variables de la personalidad que condicionan el aprendizaje : inteligencia emocional y procrastinación académica

La presente investigación analiza la relación entre la procrastinación académica y la inteligencia emocional, así como la influencia del género y la edad en estas variables. La muestra estaba formada por 192 estudiantes de Psicología de la UAB y la UIB, 45 hombres y 147 mujeres. La procrastinación se evaluó a través de la escala D de Demora Académica (CLARIANA & MARTÍN, 2008) y la inteligencia emocional con el EQ-i (BAR-ON, 1997). Los resultados muestran que la procrastinación mantiene una correlación significativa negativa con la inteligencia intrapersonal, el coeficiente emocional y el estado de ánimo. Además, las mujeres puntúan significativamente más alto que los hombres en la inteligencia intrapersonal e interpersonal, mientras que los hombres alcanzan puntuaciones superiores en el manejo del estrés y la adaptabilidadThis research analyses the relationship between academic procrastination and emotional intelligence taking also into account the gender and age influence. Psychology undergraduates from the UAB (Universitat Autónoma de Barcelona, Spain) and the UIB (Universitat de les Illes Balears, Spain), 45 males and 147 females constituted the sample of the study. Academic procrastination was assessed by means of the D scale (CLARIANA & MARTÍN, 2008) and emotional intelligence by means of the EQ-i (BAR-ON, 1997). The results show that academic procrastination has a significant negative relationship with intrapersonal intelligence, emotional quotient and mood. Moreover, female students scored significantly higher than males both in intrapersonal and interpersonal Intelligence while males obtained higher scores in both stress management and adaptabilit

Patrones de descanso, actividades físico-deportivas extraescolares y rendimiento académico en niños y niñas de primaria

El objetivo del trabajo consiste en estudiar si existe una relación entre patrones de descanso (adecuados e inadecuados), realización de determinado número de horas de actividades físico-deportivas extraescolares, y rendimiento académico en una muestra de 573 alumnos de primaria (54,62% niños y 45,38% niñas) de las provincias de Barcelona e Islas Baleares. Un cuestionario con preguntas concernientes a aspectos sociodemográficos y preguntas específicas sobre evaluación cuantitativa y cualitativa del sueño y registro cuantitativo de las actividades extraescolares fue administrado a los padres de los alumnos. Los mejores resultados se observan como consecuencia de unos patrones de descanso adecuados y una práctica moderada del ejercicio físico (entre 2 y 5 horas a la semana). Asimismo, las peores notas escolares se obtienen cuando a unos patrones de descanso inadecuados, se une una práctica de muchas horas de actividades físico-deportivas extraescolares (más de 5 horas a la semana).The aim of this paper was to study the connection between students' rest patterns (appropriate and inappropriate), accumulated hours of extracurricular physical and sports activities, and the academic results of primary school students. The sample includes 573 primary school students from Barcelona and the Balearic Islands (54.62% boys and 45.38% girls). An ad hoc questionnaire gathering both quantitative and qualitative data regarding sociodemographic and psychoeducational questions concerning rest patterns and extracurricular activities was completed by the parents. The study shows that the best academic marks were found as a result of both proper rest patterns and moderate after school exercise (2 to 5 hours a week). The study further reveals that the worst school grades were obtained in cases of inadequate rest patterns combined with a high number of hours of extracurricular sports activities (more than 5 hours a week).O objectivo do trabalho consiste em estudar se existe uma relação entre padrões de descanso (adequados e inadequados), realização de um determinado número de horas de actividades físico-deportivas extra-escolares e o rendimento académico numa amostra de 573 alunos do primeiro ciclo (54.62 rapazes e 45.38% raparigas) das províncias de Barcelona e das Ilhas Baleares. Um questionário com perguntas relativas a aspectos sociodemográficos e perguntas específicas sobre a avaliação qualitativa e quantitativa do sono e registo quantitativo das actividades extra-escolares foi administrado aos pais dos alunos. Os melhores resultados são observados como consequência dos padrões de descanso adequados e uma prática moderada do exercício (entre 2 e 5 horas por semana). Adicionalmente, as piores notas escolares foram obtidas quando aos padrões de descanso inadequados se junta um elevado número de actividades físico-deportivas extra-escolares (mais de 5 horas por semana)

Lexical Networks and Lexicon Profiles in Didactical Texts for Science Education

Peer reviewe

Papel de los factores psicológicos en la diabetes mellitus: morbilidad psiquiátrica y perfil psicopatológico

Una población de diabéticos jóvenes, sus madres y hermanos completaron dos inventarios para determinar si existían diferencias en cuanto a morbilidad psiquiátrica y al perfil psicopatológico. Los resultados indican que los pacientes diabéticos mostraban menor morbilidad psiquiátrica que sus madres. Entre sus hermanos no se observó ninguno que cumpliera criterios de caso psiquiátrico. Se realizan pruebas t y análisis de la varianza para estudiar las diferencias entre los tres grupos y se detecta que las variables depresión y somatización distinguen entre diabéticos y no diabéticos, mientras que entre el grupo de madres y sus hijos diabéticos se observaron diferencias significativas en las escalas que conforman la triada neurótica, la psicastenia y la introversión social

Assessing the internal uppermost crustal structure of the central pyrenees by gravity-constrained cross sections

The Pyrenees constitutes an exceptional example of an Alpine orogenic belt characterized by basement thrust sheets involving Paleozoic rocks and Mesozoic and Cenozoic cover units detached on the Triassic evaporites, the main décollement level. This work is located in the Central Pyrenees, where gravity data help to better constrain the internal architecture of the upper crust of the southern half of the Axial Zone and the northern part of the South Pyrenean Zone, a key area to understand the orogenic evolution of the chain. Previous and new gravity, petrophysical and geological data have been used to obtain the Bouguer and residual anomaly maps of the study area and six serial gravity-constrained cross sections perpendicular to the main structural trend. The residual anomaly map shows a good correlation between basement units involved in thrust sheets of the study area and gravity highs whereas negative anomalies are interpreted to correspond with Mesozoic/Cenozoic basins, Triassic evaporites, Late Variscan igneous bodies, and Ordovician gneisses. The six gravity-constrained cross sections highlight strong along-strike variations on the gravity signal due to lateral differences of the superficial and subsurface occurrence of Triassic evaporites, different geometry at depth of the Late Variscan igneous bodies outcropping in the study area, and geometric lateral variations of the basement thrust sheets and their relationship with the Mesozoic-Cenozoic units.This work was funded by projects CGL2017-84901-C2-2-P funded by MCIN/AEI/10.13039/501100011033 and “ERDF A way of making Europe”, PID2020-114273GB-C22 funded by MCIN/AEI/10.13039/501100011033 from the Spanish Ministry of Science and Innovation, and "Severo Ochoa” extraordinary grants for excellence IGME-CSIC (AECEX2021).Peer reviewe

New gravity data in the Central Pyrenees (NE Spain)

El proyecto GeoPiri3D tiene como objetivo caracterizar la geometría y la cinemática de los batolitos permo-carboníferos del Pirineo Central por medio de una combinación de campos potenciales y de datos estructurales. Durante 2018 se han adquirido 824 nuevas estaciones de gravedad y 186 muestras de roca. Los datos de gravedad se han procesado e integrado en la base de datos del IGME y se ha calculado un nuevo mapa de anomalías de Bouguer. Los dos cuerpos graníticos principales (La Maladeta y Andorra-Mount Louis) proporcionan diferentes respuestas gravimétricas. La anomalía sobre el afloramiento de granito de La Maladeta presenta pequeñas variaciones en su amplitud que se asocian con cambios de facies. Los datos petrofísicos proporcionan una densidad media de ca. 2,6 g/ cm3 que son consistentes con su composición, predominantemente granodiorítica. El afloramiento del plutón de Mount Louis-Andorra se caracteriza por un mínimo relativo, lo que sugiere una composición predominantemente granítica (aún no se tienen resultados de las medidas de densidad). Además, el mínimo se extiende en dirección NE, lo que sugiere que parte del plutón está enterrado. El mínimo relativo al SO del granito de La Maladeta probablemente está relacionado con las acumulaciones de evaporitas triásicasThe GeoPiri3D project aims to characterize the geometry and kinematics of the Permo-Carboniferous batholiths of the Central Pyrenees through a combination of potential fields and structural data. During 2018 we have acquired 824 new gravity stations and 186 rock samples. The gravity data were processed and integrated into the IGME database and a new Bouguer anomaly was calculated. The two main granite bodies (La Maladeta and Andorra-Mount Louis) provide different gravimetric responses. The anomaly on the La Maladeta granite outcrop presents a zonation with small variations in its amplitude. The petrophysical data provide an average density of ca. 2.6 g/cm3, which is consistent with its granodioritic composition. The outcrop of the Andorra-Mount Louis pluton is characterized by a relative minimum, suggesting a dominant granitic composition. In addition, the minimum extends in an oblique NE direction indicating that part of the pluton is buried. The relative minimum to the SW of La Maladeta is probably linked to accumulations of Triassic evaporite

Density and magnetic susceptibility relationships in non-magnetic granites; a “wildcard” for modeling potential fields geophysical data

EGU2020: Sharing Geoscience Online, 4-8 May 2020Geophysical surveying (both gravity and magnetic) is of great help in 3D modeling of granitic bodies at depth. As in any potential-field geophysics study, petrophysical data (density [r], magnetic susceptibility [k] and remanence) are of key importance to reduce the uncertainty during the modeling of rock volumes. Several works have already demonstrated that ¿18O or [SiO2] display a negative correlation to density and to magnetic susceptibility. These relationships are particularly stable (and linear) in the so-called ¿non-magnetic¿ granites (susceptibilities falling within the paramagnetic range; between 0 and 500 10-6 S.I.) and usually coincident with calc-alcaline (CA) compositions (very common in Variscan domains). In this work we establish robust correlations between density and magnetic susceptibility at different scales in CA granites from the Pyrenees. Other plutons from Iberia were also considered (Veiga, Monesterio). The main goal is to use the available and densely sampled nets of anisotropy of magnetic susceptibility (AMS) data, performed during the 90¿s and early 2000¿s, together with new data acquired in the last few years, as an indirect measurement of density in order to carry out the 3D modelling of the gravimetric signal. We sampled some sections covering the main range of variability of magnetic susceptibility in the Mont Louis-Andorra, Maladeta and Marimanha granite bodies (Pyrenees), all three characterized by even and dense nets of AMS sites (more than 550 sites and 2500 AMS measurements). We performed new density and susceptibility measurements along two main cross-sections (Maladeta and Mont Louis-Andorra). In these outcrops, numerous measurements (usually more than 50) were taken in the field with portable susceptometers (SM20 and KT20 devices). Density data were derived from the Arquimedes principle applied on large hand samples cut in regular cubes weighting between 0.3 and 0.6 kg (whenever possible). These samples were subsampled and measured later on with a KLY-3 susceptibility bridge in the laboratory. Additionally, some density data were derived from the geometry and weighting of AMS samples. After the calibration of portable and laboratory susceptometers, density and magnetic susceptibility were plotted together. Regressions were derived for every granite body and they usually followed a linear function similar to: r = 2600 kg/m3 + (0.5 * k [10-6 S.I.]). As previously stated, this relationship is only valid in CA and paramagnetic granites, where iron is mostly fractioned in iron-bearing phyllosilicates and the occurrence of magnetite is negligible (or at least its contribution to the bulk susceptibility). These relationships allow transforming magnetic susceptibility data into density data helping in the 3D modelling of the gravimetric signal when density data from rock samples are scarce. Given the large amount of AMS studies worldwide, together with the quickness and cost-effectiveness of susceptibility measurements with portable devices, this methodology allows densifying and homogenizing the petrophysical data when modelling granite rock volumes based on both magnetic and gravimetric signal

Towards 3D databases and harmonized 3D models at IGME-CSIC

IGME-CSIC has a highly relevant geological and geophysical database that includes a continuous digital geological cartography at 1:50000; 1:200000 and 1:1000000 scales and a fair amount of geophysical data: gravity, magnetic, well-logs in tiff and LAS format, seismic lines in tiff and SEG-Y format, borehole and petrophysical data, together with other geophysical and geological studies. Since the 2004, an important effort has been done to undertake 3D geological and geophysical modelling ranging from local studies (mineral exploration or CO2 storage sites) to regional geology for a better understanding of the subsurface structure and its geodynamic evolution as a base for other studies on natural hazards or mineral resources. These studies were ¿stand alone¿ and now IGME is designing a new strategy. It includes the available data and models harmonization (stratigraphy sequences, structural interpretations, faults distribution, seismic velocity models, spatial distribution of physical properties such as density and magnetic susceptibility, workflows, methodologies, evaluation of uncertainties, visualization, etc.) to comply with the FAIR (Findable, Accessible, Interoperable and Reusable) data standardization. In this way, the new 3D models will be easily integrated and available from the databases. This strategy includes collaboration with the Bureau de Recherches Géologiques et Minières of France (BRGM) and Laboratório Nacional de Energia e Geologia of Portugal (LNEG) in order to harmonize the Spanish geological data and models with their neighbours across national borders. The first step is being done in the framework of GeoERA projects. Plain-language Summary IGME-CSIC owns a large database that includes a highly valuable geological and geophysical data and geophysical studies containing the interpretation of some of the data of Spain (onshore and offshore) Since 2004 the authors of this work have been working in 3D geological and geophysical modelling that includes local (mineral exploration or CO2 storage sites) and regional studies. The goal is to improve our understanding of the subsurface structures and processes as a base for deepening our knowledge in how the natural hazards occur, how to improve the exploration for mineral resources, etc. These studies were made ad hoc within different projects and now IGME-CSIC is designing a workflow to harmonize these models in order to comply with the FAIR (Findable, Accessible, Interoperable and Reusable) data standardization so the models will be available to being used beyond the initial objectives that generated their creation. This strategy includes collaboration with other European institutions like the Bureau de Recherches Géologiques et Minières of France (BRGM) and Laboratório Nacional de Energia e Geologia of Portugal (LNEG) in order to harmonize the models across national borders. The first step is already being done in the framework of the GeoERA projects