Phytoplankton mirrors changes in the environment and plays an important role in biogeochemical processes. Phytoplankton dynamics is the outcome of both autogenic succession and external disturbances. This thesis focused on the seasonal variation of water column stability and its effects on phytoplankton, particularly considering the influence of mixing events on phytoplankton development. Lake Erken is a dimictic lake with weak and often interrupted summer stratification, which represents an intermediate case between a polymictic lake and a lake with strong summer stratification. There are two diatom phases annually. The spring bloom is caused by pioneer centric diatoms, and the autumn diatom phase is dominated by meroplanktonic diatoms induced by turnover. A summer Cyanobacteria bloom – mainly Gloeotrichia echinulata, depended on the length and stability of stratification. Winter and spring air temperature is found to play an important role in the annual succession of phytoplankton by initiating changes in ice/snow-cover and lake thermal stability and setting the basic status. Instead of starting from zero, the vernal phytoplankton piles up on the overwintering community, this trans-annual ecological memory influences both the composition and diversity and taxonomic distinctness of spring phytoplankton. Water column stability during summer in Lake Erken is mainly influenced by wind-induced turbulence and internal seiches. As thermal stratification develops from early until late summer, variations in stability and gradual deepening of the thermocline depth influence phytoplankton dynamics directly by changing its distribution, and also indirectly by altering the nutrient and light availability. A new disturbance index (DI) was defined to quantify environmental stability/disturbance and tested well to indicate phytoplankton equilibrium status in two summer stratification periods. The concept of species and functional groups was generally used in this study. However, a next generation sequencing based approach was also tested and proved to provide an excellent candidate for revealing distribution patterns of phytoplankton in inland waters.

En la presente tesis se muestra una nueva metodología de extracción "inteligente" de modelos circuitales lineales y no lineales para dispositivos MESFET y HEMT, además de efectuar numerosas aportaciones en el campo de las medidas radioeléctricas de dichos dispositivos mediante diseño del hardware y del software necesario para la automatización de las mismas. Por otro lado se presenta un novedoso modelo de Gran Señal para dispositivos HEMT de potencia que da cuenta del fenómeno de la compresión de la transconductancia y es fácilmente implementable en simuladores no lineales comerciales del tipo de MDS, LIBRA, HARMONICA, etc. Además se ha aumentado el rango de validez frecuencial de los modelos de pequeña señal mediante la obtención de las expresiones "exactas" de los modelos usuales de pequeña señal Vendelin-Dambrine, Vickes, Berroth & Bosch, etc. Otra novedad aportada por este trabajo de tesis ha sido aplicar estos modelos lineales a los transistores HEMT, evitando la obtención valores carentes de significado físico como ocurría hasta ahora. Como validación del modelo no lineal de HEMT se han llevado a cabo numerosas simulaciones del mismo en MDS que han sido comparadas con las medidas experimentales realizadas en nuestro laboratorio (Scattering, DC, Pulsadas y Pin/Pout) poniendo de manifiesto la exactitud del modelo. Para validar los modelos de pequeña señal se han efectuado simulaciones con el simulador lineal MMICAD utilizando transistores de diferentes tamaños procedentes de distintas foundries con objeto de visualizar el comportamiento del dispositivo independientemente del origen del mismo. / In this thesis a new methodology for the "intelligent" parameter extraction of linear and non-linear model for GaAs MESFET and HEMT devices is shown, besides numerous contributions in the field of Scattering and DC measurements of this kind of devices by means of hardware design and necessary software for the automation of the same have been done. On the other hand a novel Great Signal model for HEMT devices is presented. This model is capable to model the transconductance compression phenomenon and it is easily to built in commercial non-linear simulators like MDS, LIBRA, Microwave HARMONICA, etc. This work has also increased the frequency range for the usual small-signal models by means of calculate "exact" expressions of them. Another novelty contribution of this thesis is to apply for first time these linear models to HEMT transistors, avoiding the lacking of physical meaning values like it occurred up to now. To make possible the validation of non-linear HEMT model, simulations with MDS software and comparisons with experimental measurements made in our laboratory (Scattering, DC, Pulsed and Pin/ Pout) have been carried out and there was very good agreement between measured and simulated data. To validate small-signal models referred before, simulations with MMICAD software and comparisons between simulated and experimental scattering measurements using transistors of different sizes from several foundries and technological processes have been made.

Depuis plus d’un siècle, les changements globaux sont à l’origine de profondes modifications de nos sociétés, nos modes de vie et il en va bien sûr de même pour notre environnement. Cette trajectoire empruntée, bon gré mal gré, par l’ensemble de l’humanité n’est pas sans conséquences pour les systèmes naturels et semble déjà mener les générations futures au-devant de grands défis. Afin de ne pas compromettre notre capacité à relever ces épreuves futures et, devant l’urgence du besoin d’action, une partie de la communauté scientifique a choisi de concentrer ses efforts sur la couche superficielle de notre planète qui soutient la vie terrestre : la Zone Critique. L’émergence de ce concept souligne la nécessité de développer des approches scientifiques pluridisciplinaires intégrant une large variété d’échelles de temps et d’espace. En tant que lien entre les différents compartiments de la Zone Critique (Atmosphère, Biosphère, Hydrosphère, Lithosphère et Pédosphère), l’eau est une molécule essentielle aux échanges d’énergie et de matière dont la dynamique requiert une attention particulière. Compte tenu de la diversité et de la variabilité spatiotemporelle des transferts d’eau et de matière dissoute dans les milieux aquatiques, de nouvelles méthodes d'investigations sont nécessaires. L'objectif général de cette thèse est de décrire l’intérêt et le potentiel qui résident dans l’utilisation des gaz dissous, en particulier lorsqu’ils sont mesurés à haute fréquence sur le terrain, afin de caractériser la dynamique hydrobiogéochimique des eaux naturelles de la Zone Critique à différentes échelles spatiales et temporelles. Pour parfaire cette ambition, ce travail s’est tout d’abord attaché au développement d'une instrumentation innovante puis, à la mise en place de nouveaux traceurs intégrés dans des dispositifs expérimentaux originaux et enfin, à l'acquisition, au traitement et à l'analyse de différents jeux de données de gaz dissous en se focalisant sur les eaux souterraines. / For more than a century, global change has led to a profound modification of our societies, our lifestyles and, of course, our environment. This trajectory followed willy-nilly by all mankind has consequences for natural systems and already seems to lead the future generations ahead of serious challenges. In order not to compromise our ability to meet these future ordeals, and because of the urgent need for action, part of the scientific community has chosen to concentrate on the near-surface environment that supports terrestrial life: the Critical Zone. The emergence of this concept underlines the need to develop multidisciplinary scientific approaches integrating a wide variety of temporal and spatial scales. As the link between the different compartments of the Critical Zone (Atmosphere, Biosphere, Hydrosphere, Lithosphere and Pedosphere), water is an essential molecule controlling the exchanges of energy and matter whose dynamics require special attention. In view of the diversity and spatiotemporal variability of water and matter transfers arising in aquatic environments, new methods of investigation are needed. The general objective of this thesis is to describe the interest and the potential lying in the use of dissolved gases, especially when they are measured at high frequency in the field, in order to characterise the hydrobiogeochemical dynamics of the natural waters of the Critical Zone at different spatial and temporal scales. To perfect this ambition, this work focused first on the development of an innovative instrumentation, then, on the implementation of novel tracers integrated into original experimental setups and finally, on the acquisition, processing and analysis of different dissolved gas datasets focusing on groundwater.