Innovación educativa en la docencia universitaria de la Historia: balance de una década en la ULPGC (2002-2012)

[ES] El presente trabajo analiza las acciones de innovación educativa realizadas en el seno de la Facultad de Geografía e Historia de la Universidad de Las Palmas de Gran Canaria en la década que transcurre entre los años 2002 y 2012. En una primera fase (2002-2009), previa a la constitución formal de los Grupos de Innovación Educativa (GIE) en la ULPGC, las actividades de innovación educativa se realizaron de manera coordinada por un grupo de trabajo formado por varios profesores de los departamentos de Geografía y Ciencias Históricas. A partir de la constitución de los GIE y, en particular, con la creación del GIE Clío 2.0, se inició una nueva fase (2009-2012) que, al igual que la anterior, ha contado con el apoyo del Decanato de la Facultad de Geografía e Historia.

Cuantificación de la recarga natural al acuífero del norte de Gran Canaria mediante el balance diario de agua en el suelo

[ES]La recarga al acuífero noreste de Gran Canaria ha sido calculada dentro del proyecto REDESAC mediante la realización de un balance diario de agua en el suelo. Para llevarlo a cabo ha sido necesario adaptar los datos de partida existentes referentes a la pluviometría, la evapotranspiración (ET0 y ETP) y los parámetros del suelo. La zona se ha dividido en subzonas según la situación de las estaciones pluviométricas y atendiendo a las características climáticas. Los cálculos realizados mediante la utilización del código Easy-Bal han arrojado una recarga de unos 15±4 hm3/a, lo que supone el 13±4% de la precipitación, la mayor parte de la misma concentrada en las zonas altas y de medianías

Modelling the effects of nitrogen deposition and carbon dioxide enrichment on forest carbon balance

Atmospheric CO2 concentration ([CO2]) has increased over the last 250 years, mainly due to human activities. Of total anthropogenic emissions, almost 31% has been sequestered by the terrestrial biosphere. A considerable contribution to this sink comes from temperate and boreal forest ecosystems of the northern hemisphere, which contain a large amount of carbon (C) stored as biomass and soil organic matter. Several potential drivers for this forest C sequestration have been proposed, including increasing atmospheric [CO2], temperature, nitrogen (N) deposition and changes in management practices. However, it is not known which of these drivers are most important. The overall aim of this thesis project was to develop a simple ecosystem model which explicitly incorporates our best understanding of the mechanisms by which these drivers affect forest C storage, and to use this model to investigate the sensitivity of the forest ecosystem to these drivers. I firstly developed a version of the Generic Decomposition and Yield (G’DAY) model to explicitly investigate the mechanisms leading to forest C sequestration following N deposition. Specifically, I modified the G’DAY model to include advances in understanding of C allocation, canopy N uptake, and leaf trait relationships. I also incorporated a simple forest management practice subroutine. Secondly, I investigated the effect of CO2 fertilization on forest productivity with relation to the soil N availability feedback. I modified the model to allow it to simulate short-term responses of deciduous forests to environmental drivers, and applied it to data from a large-scale forest Free-Air CO2 Enrichment (FACE) experiment. Finally, I used the model to investigate the combined effects of recent observed changes in atmospheric [CO2], N deposition, and climate on a European forest stand. The model developed in my thesis project was an effective tool for analysis of effects of environmental drivers on forest ecosystem C storage. Key results from model simulations include: (i) N availability has a major role in forest ecosystem C sequestration; (ii) atmospheric N deposition is an important driver of N availability on short and long time-scales; (iii) rising temperature increases C storage by enhancing soil N availability and (iv) increasing [CO2] significantly affects forest growth and C storage only when N availability is not limiting.

The role of bifidobacteria in newborn health and the intestinal microbial balance

Gut microbial acquisition during the early stage of life is an extremely important event since it affects the health status of the host. In this contest the healthy properties of the genus Bifidobacterium have a central function in newborns. The aim of this thesis was to explore the dynamics of the gut microbial colonization in newborns and to suggest possible strategies to maintain or restore a correct balance of gut bacterial population in infants. The first step of this work was to review the most recent studies on the use of probiotics and prebiotics in infants. Secondly, in order to prevent or treat intestinal disorders that may affect newborns, the capability of selected Bifidobacterium strains to reduce the amount of Enterobacteriaceae and against the infant pathogen Streptococcus agalactiae was evaluated in vitro. Furthermore, the ability of several commercial fibers to stimulate selectively the growth of bifidobacterial strains was checked. Finally, the gut microbial composition in the early stage of life in response to the intrapartum antibiotic prophylaxis (IAP) against group B Streptococcus was studied using q-PCR, DGGE and next generation sequencing. The results globally showed that Bifidobacterium breve B632 strain is the best candidate for the use in a synbiotic product coupled to a mixture of two selected prebiotic fibers (galactooligosaccharides and fructooligosaccharides) for gastrointestinal disorders in infants. Moreover, the early gut microbial composition was affected by IAP treatment with infants showing lower counts of Bifidobacterium spp. and Bacteroides spp. coupled to a decrement of biodiversity of bacteria, compared to control infants. These studies have shown that IAP could affect the early intestinal balance in infants and they have paved the way to the definition of new strategies alternative to antibiotic treatment to control GBS infection in pregnant women.

Extracellular glutamate-GABA balance in the developing neocortex

It has been shown in the study that glutamate transporters (EAAT) are capable to modulate GABA transports (GAT). Here we also report that DL-TBOA, a non-transportable glutamate uptake blocker, eliminates GAT-mediated GABA release, while D-aspartate, an EAAT substrate, does not block the latter. The strength or even the operating mode of GABA uptake/release could be influenced by the work of EAATs. Considering the interaction between EAATs and GATs we can conclude that ambient glutamate and GABA levels are mutually dependent. The EAAT-GAT crosstalk observed in this work is mediated by EAAT1 and GAT-2/3. Since both transporters are Na+ dependent and mainly glial, next we investigated the role of [Na+]i in astrocytic-mediated glutamate uptake. We tested whether [Na+]i changes affect paired-pulse plasticity of STCs recorded from cortical layer 2/3 astrocytes. We report that an elevation of [Na+]i induced either by using a high [Na+]i intrapipette solution or by application of GABA slows STCs kinetics and decrease paired-pulse facilitation (PPF) of STCs at short inter-stimulus intervals. Moreover, GAT inhibitors decrease PPF of STCs under control conditions, suggesting that endogenous GABA operating via GATs influences EAAT-mediated transport

Dynamics of Bora wind over the Adriatic sea: atmospheric water balance and role of air-sea fluxes and orography

The Bora wind is a mesoscale phenomenon which typically affects the Adriatic Sea basin for several days each year, especially during winter. The Bora wind has been studied for its intense outbreak across the Dinaric Alps. The properties of the Bora wind are widely discussed in the literature and scientific papers usually focus on the eastern Adriatic coast where strong turbulence and severe gust intensity are more pronounced. However, the impact of the Bora wind can be significant also over Italy, not only in terms of wind speed instensity. Depending on the synoptic pressure pattern (cyclonic or anticyclonic Bora) and on the season, heavy snowfall, severe storms, storm surges and floods can occur along the Adriatic coast and on the windward flanks of the Apennines. In the present work five Bora cases that occurred in recent years have been selected and their evolution has been simulated with the BOLAM-MOLOCH model set, developed at ISAC-CNR in Bologna. Each case study has been addressed by a control run and by several sensitivity tests, performed with the purpose of better understanding the role played by air-sea latent and sensible heat fluxes. The tests show that the removal of the fluxes induces modifications in the wind approching the coast and a decrease of the total precipitation amount predicted over Italy. In order to assess the role of heat fluxes, further analysis has been carried out: column integrated water vapour fluxes have been computed along the Italian coastline and an atmospheric water balance has been evaluated inside a box volume over the Adriatic Sea. The balance computation shows that, although latent heat flux produces a significant impact on the precipitation field, its contribution to the balance is relatively minor. The most significant and lasting case study, that of February 2012, has been studied in more detail in order to explain the impressive drop in the total precipitation amount simulated in the sensitivity tests with removed heat fluxes with respect to the CNTRL run. In these experiments relative humidity and potential temperature distribution over different cross-sections have been examined. With respect to the CNTRL run a drier and more stable boundary layer, characterised by a more pronounced wind shear at the lower levels, has been observed to establish above the Adriatic Sea. Finally, in order to demonstrate that also the interaction of the Bora flow with the Apennines plays a crucial role, sensitivity tests varying the orography height have been considered. The results of such sensitivity tests indicate that the propagation of the Bora wind over the Adriatic Sea, and in turn its meteorological impact over Italy, is influenced by both the large air-sea heat fluxes and the interaction with the Apennines that decelerate the upstream flow.

Studio del metodo "systolic volume balance" per la stima non invasiva della portata media cardiaca

La portata media cardiaca, (cardiac output “CO”) è un parametro essenziale per una buona gestione dei pazienti o per il monitoraggio degli stessi durante la loro permanenza nell’unità di terapia intensiva. La stesura di questo elaborato prende spunto sull’articolo di Theodore G. Papaioannou, Orestis Vardoulis, and Nikos Stergiopulos dal titolo “ The “systolic volume balance” method for the non invasive estimation of cardiac output based on pressure wave analysis” pubblicato sulla rivista American Journal of Physiology-Heart and Circulatory Physiology nel Marzo 2012. Nel sopracitato articolo si propone un metodo per il monitoraggio potenzialmente non invasivo della portata media cardiaca, basato su principi fisici ed emodinamici, che usa l’analisi della forma d’onda di pressione e un metodo non invasivo di calibrazione e trova la sua espressione ultima nell’equazione Qsvb=(C*PPao)/(T-(Psm,aorta*ts)/Pm). Questa formula è stata validata dagli autori, con buoni risultati, solo su un modello distribuito della circolazione sistemica e non è ancora stato validato in vivo. Questo elaborato si pone come obiettivo quello di un’analisi critica di questa formula per la stima della portata media cardiaca Qsvb. La formula proposta nell'articolo verrà verificata nel caso in cui la circolazione sistemica sia approssimata con modelli di tipo windkessel. Dallo studio svolto emerge il fatto che la formula porta risultati con errori trascurabili solo se si approssima la circolazione sistemica con il modello windkessel classico a due elementi (WK2) e la portata aortica con un’onda rettangolare. Approssimando la circolazione sistemica con il modello windkessel a tre elementi (WK3), o descrivendo la portata aortica con un’onda triangolare si ottengono risultati con errori non più trascurabili che variano dal 7%-9% nel caso del WK2 con portata aortica approssimata con onda triangolare ad errori più ampi del 20% nei i casi del WK3 per entrambe le approssimazioni della portata aortica.

Chronic impact of topiramate on acid-base balance and potassium in childhood

Topiramate, which is commonly prescribed for seizure disorders and migraine prophylaxis, sometimes causes metabolic acidosis and hypokalemia. Since the effects of topiramate on acid-base balance and potassium levels have not been well explored in children, acid-base balance, anion gap and potassium were assessed in 24 patients (8 females and 16 males) aged between 4.6 and 19 years on topiramate for more than 12 months and in an age-matched control group. Plasma bicarbonate (21.7 versus 23.4 mmol/L; P<0.03), carbon dioxide pressure (39.7 versus 43.2mm Hg; P<0.05), and potassium (3.7 versus 4.0 mmol/L; P<0.03) were on the average lower and chloride (109 versus 107 mmol/L; P<0.03) higher in patients treated with topiramate than in controls. Blood pH, plasma sodium and the anion gap were similar in patients on topiramate and in controls. In patients on topiramate no significant correlation was observed between the dosage of this agent and plasma bicarbonate or potassium as well as between topiramate blood level and the mentioned electrolytes. In conclusion long-term topiramate treatment is associated with a mild, statistically significant tendency towards compensated normal anion gap metabolic acidosis and hypokalemia.