Les interactions entre les eaux souterraines et les eaux de surface sont complexes et jouent un rôle prépondérant dans le fonctionnement des hydrosystèmes, tant en termes quantitatifs que qualitatifs. Ces deux compartiments interagissent à travers différentes interfaces emboitées depuis l’échelle locale, notamment la zone d’interface rivière-nappe, appelée zone hyporhéique (ZH) jusqu’à l’échelle régionale. La ZH se définit comme un buffer entre les eaux souterraines et les eaux de surface. Les variations des flux d’eau et de chaleur au niveau de cette zone modulent les processus biogéochimiques. Le but de cette thèse est d’améliorer la compréhension du régime thermique et hydrologique de la ZH et de sa variation spatiale. Cette problématique est abordée par l’utilisation de stations de mesures haute fréquence des échanges nappe-rivière (MOLONARI) sur le bassin des Avenelles (sous bassin de la Seine (46 km2)) et de la modélisation. Le suivi haute fréquence a permis de réaliser une analyse des données expérimentales présentant le régime hydro-climatique du bassin ainsi que l’évolution spatiale et temporelle du fonctionnement des différents compartiments de l’hydrosystème. Un cas synthétique a été réalisé afin de caractériser les différents facteurs contrôlant le régime thermique de l’interface nappe rivière et la variation de stocks d’énergie au sein de la ZH. La démarche de modélisation suivie pour le cas synthétique fournit un cadre d’analyse des données des cinq stations MOLONARI. Les données acquises sur ces stations ont été utilisées afin de déterminer les propriétés hydrodynamiques et thermiques de la ZH ainsi que des couches géologiques sous-jacentes par inversion à l’aide du modèle METIS couplé à un script de balayage de l’espace des paramètres afin de quantifier les flux d’eau et de chaleur à l’interface nappe-rivière le long d'un corridor hydraulique. Les résultats du modèle mettent en lumière la variabilité spatio-temporelle des échanges de chaleur au niveau des cinq stations MOLONARI. La quantification des flux de chaleur a fourni un nouvel éclairage des interactions entre les eaux de surface et les eaux souterraines à l’interface nappe-rivière du bassin des Avenelles. / The river-aquifer interactions are complex and play a preponderant role in hydrosystems functioning, in both qualitative and quantitative terms. These two compartments interact through various nested interfaces from the local scale in particular the river aquifer interface called the Hyporheic Zone (HZ) to the regional scale. The HZ acts as a buffer between the stream and the groundwater. The water and heat fluxes variation at this zone modulates the biogeochemical processes.The aim of this thesis, is to improve the understanding of the thermal and hydrological regime of the HZ and its spatial variation. This problem is approached by the use of high frequency measurement stations of river-aquifer exchanges (LOMOS) in the Avenelles basin (sub-basin of the Seine basin (46 km2)) and by modeling. The high frequency monitoring allowed to realize an analysis of the experimental data characterizing the hydroclimatic regime of the Avenelles basin as well as the spatial and temporal evolution of the hydrosystem various compartments functioning.A synthetic case was realized to characterize the main factors controlling the thermal regime at the river aquifer interface and the energy storage variation within the ZH. The modeling approach followed by the synthetic case provides an analysis framework of the five LOMOS data.The acquired LOMOS data were used to determine the hydrogeological and thermal properties of the HZ and of the underlying aquifers by inversion by means of a 2D finite element thermo-hydrogeological model (METIS) coupled with a parameters screening script to quantify water and heat fluxes through the stream – aquifer interface over along the stream network.The model results highlight the spatiotemporal variability of the heat exchanges at the five LOMOS. The quantification of heat fluxes provided a new lighting of the stream-aquifer interactions of the Avenelles basin.

<p>The hydropower industry has altered connectivity in many rivers during the last century. Many fish species depend on both an intact longitudinal connectivity to be able to migrate between spawning, feeding and winter habitats, and vertical connectivity for development and survival of incubating embryos and larvae in the gravel. The objective of this thesis was to examine problems and remedial measures associated with disrupted longitudinal and vertical connectivity in regulated rivers. The issue of longitudinal connectivity was studied in the River Emån by evaluating the efficiency of two nature-like fishways for anadromous brown trout. Telemetry studies showed that the combined efficiency for the two fishways in 2001-2004 was 60.5%. The passage efficiencies of both fishways were high for trout (89-100%), but also for other species such as chub, perch, tench, burbot and roach (74%). The attraction efficiencies were largely dependent on power plant operation, and generally high for the fishway situated next to the tail-race and low for the fishway situated inside the former channel. More than half of the trout spawners were also observed using the fishways for downstream passage. The densities of brown trout yearlings upstream of the fishways were higher after the fishways were built than during pre-fishway years. Smolts produced upstream of the fishways were observed migrating downstream in 2003-2005. The percentage of smolts that passed both power plants in was 51%, with losses being attributed to predation (15%), turbine-induced mortality (16%) and other reasons (18%). Turbine-induced mortality was higher (40%) at the power plant with four small Francis runners, than at the power plant with one large Kaplan runner (12%). The issue of vertical connectivity was studied in three rivers in Värmland, one unregulated, and two regulated, one of which had no minimum flow requirements. In the unregulated river, temporal patterns in hyporheic water chemistry correlated to variation in surface water chemistry and discharge as expected. In the regulated rivers, the hyporheic water chemistry showed little correlation to discharge or surface water chemistry. The intra-gravel water chemistry conditions for brown trout eggs were more favourable in the unregulated river, characterised by high oxygen levels, than in the two regulated rivers. The regulated river with no minimum flow requirements had critically low oxygen levels at the end of the incubation period.</p>

<p>Understanding of the processes affecting solute transport in flowing water is important for the possibility to predict the evolution with time of polluted stream systems. </p><p>This thesis presents tracer experiment methodology and model developments for solute transport in streams, with special focus on retention processes and their effect on solute stream transport. Results are presented from a tracer experiment in the Säva Stream, Uppland County, Sweden, where both a conservative (³H as tritiated water) and a reactive (⁵¹Cr as trivalent chromium ion) tracer were injected simultaneously. The time and length scales of the experiment were prolonged compared to previous studies, which allowed for new critical tests of different model concepts. </p><p>It was found that the hyporheic exchange greatly affected the solute transport of both tracers. However, the retention of chromium was significantly more pronounced. About 76% of the injected chromium was lost from the stream water phase directly after the passage of the pulse 30 km downstream of the injection point. The inventory of chromium in the sediments indicated that the main part was retrieved in the hyporheic zone. </p><p>Both a diffusive and an advective hyporheic exchange model were developed and evaluated versus independent observations in the stream water and hyporheic zone. Analytical expressions for the central temporal moments of the breakthrough curve and semi-analytical solutions for the solute concentration in the Laplace domain were derived. Both models were found useful in representing the observations.</p><p>For the transport of the reactive solute, it was found essential to consider a kinetic sorption on to particulate matter in the hyporheic zone. The time needed for a wash-out of 75% of the maximum uptake in the hyporheic zone was found to be ~85 times longer for the reactive solute, compared to the conservative solute. Neglecting the sorption kinetics in the transport model yielded significant errors in the central temporal moments, which implied an incorrect description of the wash-out process from the hyporheic zone. Independent observations in the stream water and hyporheic zone as well as choice of evaluation method are essential for a correct interpretation of the processes.</p><p>A first attempt was also made to link model parameters such as the residence time in the hyporheic zone with measurable parameters of the stream. Such a relationship offers the possibility to generalize results for other streams and stream conditions. A generic study of the transport of an inert solute in the Lule River, Sweden, using this kind of relationship, indicated that the hyporheic exchange can have a large practical implication.</p>

Understanding of the processes affecting solute transport in flowing water is important for the possibility to predict the evolution with time of polluted stream systems. This thesis presents tracer experiment methodology and model developments for solute transport in streams, with special focus on retention processes and their effect on solute stream transport. Results are presented from a tracer experiment in the Säva Stream, Uppland County, Sweden, where both a conservative (3H as tritiated water) and a reactive (51Cr as trivalent chromium ion) tracer were injected simultaneously. The time and length scales of the experiment were prolonged compared to previous studies, which allowed for new critical tests of different model concepts. It was found that the hyporheic exchange greatly affected the solute transport of both tracers. However, the retention of chromium was significantly more pronounced. About 76% of the injected chromium was lost from the stream water phase directly after the passage of the pulse 30 km downstream of the injection point. The inventory of chromium in the sediments indicated that the main part was retrieved in the hyporheic zone. Both a diffusive and an advective hyporheic exchange model were developed and evaluated versus independent observations in the stream water and hyporheic zone. Analytical expressions for the central temporal moments of the breakthrough curve and semi-analytical solutions for the solute concentration in the Laplace domain were derived. Both models were found useful in representing the observations. For the transport of the reactive solute, it was found essential to consider a kinetic sorption on to particulate matter in the hyporheic zone. The time needed for a wash-out of 75% of the maximum uptake in the hyporheic zone was found to be ~85 times longer for the reactive solute, compared to the conservative solute. Neglecting the sorption kinetics in the transport model yielded significant errors in the central temporal moments, which implied an incorrect description of the wash-out process from the hyporheic zone. Independent observations in the stream water and hyporheic zone as well as choice of evaluation method are essential for a correct interpretation of the processes. A first attempt was also made to link model parameters such as the residence time in the hyporheic zone with measurable parameters of the stream. Such a relationship offers the possibility to generalize results for other streams and stream conditions. A generic study of the transport of an inert solute in the Lule River, Sweden, using this kind of relationship, indicated that the hyporheic exchange can have a large practical implication.

The hydropower industry has altered connectivity in many rivers during the last century. Many fish species depend on both an intact longitudinal connectivity to be able to migrate between spawning, feeding and winter habitats, and vertical connectivity for development and survival of incubating embryos and larvae in the gravel. The objective of this thesis was to examine problems and remedial measures associated with disrupted longitudinal and vertical connectivity in regulated rivers. The issue of longitudinal connectivity was studied in the River Emån by evaluating the efficiency of two nature-like fishways for anadromous brown trout. Telemetry studies showed that the combined efficiency for the two fishways in 2001-2004 was 60.5%. The passage efficiencies of both fishways were high for trout (89-100%), but also for other species such as chub, perch, tench, burbot and roach (74%). The attraction efficiencies were largely dependent on power plant operation, and generally high for the fishway situated next to the tail-race and low for the fishway situated inside the former channel. More than half of the trout spawners were also observed using the fishways for downstream passage. The densities of brown trout yearlings upstream of the fishways were higher after the fishways were built than during pre-fishway years. Smolts produced upstream of the fishways were observed migrating downstream in 2003-2005. The percentage of smolts that passed both power plants in was 51%, with losses being attributed to predation (15%), turbine-induced mortality (16%) and other reasons (18%). Turbine-induced mortality was higher (40%) at the power plant with four small Francis runners, than at the power plant with one large Kaplan runner (12%). The issue of vertical connectivity was studied in three rivers in Värmland, one unregulated, and two regulated, one of which had no minimum flow requirements. In the unregulated river, temporal patterns in hyporheic water chemistry correlated to variation in surface water chemistry and discharge as expected. In the regulated rivers, the hyporheic water chemistry showed little correlation to discharge or surface water chemistry. The intra-gravel water chemistry conditions for brown trout eggs were more favourable in the unregulated river, characterised by high oxygen levels, than in the two regulated rivers. The regulated river with no minimum flow requirements had critically low oxygen levels at the end of the incubation period.

The conceptual subject of this study was to investigate the effects of microbial biofilms of the hyporheic zone of the river Elbe on nutrient dynamics and elimination. This resulted in four aspects, which were carried out separately. One aspect was the investigation of the dynamics of inorganic nitrogen compounds in the upper sediment layers, as highest microbial activity could be expected due to increased import of nutrients. Dissolved oxygen is suggested to control the nitrogen dynamics in the hyporheic zone, as dissolved oxygen in the flowing water varied seasonally and diurnally due to the photosynthetic activity of the algae and infiltrated in the hyporheic zone. The second aspect was the investigation of advective transport of algal cells through porous media. In laboratory columns the retention and retardation of morphological different algae was estimated. In the year 2001, it was possible to use the diving bell of the Office of Water and Navigation Magdeburg. Samples of the river bed at two different sites (Dresden-Übigau and Coswig near Lutherstadt-Wittenberg) were taken. Microbial activity rates, detrital and grain size parameters were detected. This sample material was also used for the detection of the microbial biocoenosis at the two sites. The microorganisms of the flowing water, the interstitial water and associated to the sediment were characterized by means of the fluorescence in situ hybridization (FISH) technique. Multivariate statistical analysis was performed on the FISH data at different spatial and phylogenetic scales. / Das Ziel der vorliegenden Arbeit war die Untersuchung von mikrobiellen Biofilmen in hyporheischen Sedimenten der Elbe sowie deren Auswirkungen auf die Stoffdynamik und die Nährstoffelimination. Daraus ergaben sich vier Teilaspekte, die separat bearbeitet wurden. Ein Aspekt war die Untersuchung der Stickstoffdynamik in den obersten Sedimentschichten, da hier aufgrund des erhöhten Importes von Nährstoffen die höchste mikrobielle Aktivität zu erwarten ist. Wesentliche biologische Steuergröße ist hierbei vermutlich der Gelöstsauerstoff, der saisonal sowie diurnal durch die photosynthische Aktivität der Algen auch die biochemischen Umsätze im hyporheischen Interstitial beeinflußt. Der zweite Aspekt war die Untersuchung des advektiven Transportes von Algen durch poröse Medien. In Laborversuchen wurde die Retention und die Retardation von morphologisch unterschiedlichen Algen untersucht. Im Jahr 2001 konnte der Taucherschacht des Wasser- und Schiffahrtsamtes Magdeburg genutzt werden. Dadurch konnte Probenmaterial aus der Flußmitte an zwei unterschiedlichen Standorten (Dresden-Übigau und Coswig bei Lutherstadt-Wittenberg) entnommen werden. Es wurden mikrobielle Umsatzraten, Detritus- und Korngrößen- Kenngrößen bestimmt. Ebenfalls am Probenmaterial der Taucherschachtaktion wurde die Fluoreszenz in situ Hybridisierung angewendet. Dies ermöglichte eine Bestandsaufnahme der Bakterien sowohl im Freiwasser der beiden Standorte, als auch im Interstitialwasser und den Bakterien assoziiert ans Sediment. Die Ergebnisse wurden auf unterschiedlichen räumlichen und phylogenetischen Ebenen mit multivariaten statistischen Methoden ausgewertet.

L’étude présentée a pour objectif de mieux comprendre l’influence de l’hydrodynamique sur le transfert de produits phytosanitaires lors d’écoulement dans les fossés agricoles. Quatre paramètres ont plus particulièrement été étudiés : i) la vitesse de l’écoulement de surface ; ii) la submergence, définie comme le rapport moyen entre la hauteur des formes du lit et la hauteur d’eau ; iii) la forme du lit et iv) le degré de saturation en eau du lit avant la contamination par les produits phytosanitaires. L’influence de ces paramètres a été étudiée en conditions semicontrôlées à travers la mise en oeuvre d’expérimentations en canal expérimental, au fond duquel a été fixé pour chaque expérimentation un substrat type constitué d’un assemblage de fibres de chanvre utilisé pour approcher de manière simplifiée un système naturel relativement complexe et hétérogène (en considération des nombreux substrats rencontrés dans le lit des fossés naturels : herbes, feuilles mortes, végétation en décomposition, paille, sédiments, …). Les fibres de chanvre ont été choisies après une étude préliminaire en laboratoire visant à comparer les possibilités d’adsorption et de désorption des produits phytosanitaires sélectionnés sur diverses fibres couramment utilisées dans l’industrie géotextile (jute, lin, chanvre, polyamide, polypropylène et polyester). Les expérimentations en canal expérimental ont été menées de manière à tester l’influence spécifique des paramètres étudiés. La comparaison des différentes expérimentations indique qu’une augmentation de la vitesse de l’écoulement de surface augmente la quantité de produits phytosanitaires transférés de l’écoulement de surface vers le lit, ainsi que la cinétique de ce transfert. Le constat est le même lorsqu’on augmente la submergence, ou bien lorsqu’on passe d’une géométrie de petites formes en « dunes » à une géométrie de grandes formes en « créneau ». Enfin, le fait que le lit soit saturé en eau en début d’expérimentation réduit fortement le transfert de la lame d’eau vers le lit. On observe également que l’influence de chaque paramètre semble être interdépendante. Devant le coût en temps et en argent de ces expérimentations, un modèle a été sélectionné dans la littérature, codé et utilisé pour conforter et compléter l’interprétation des données expérimentales. / The aim of this work was to better understand the influence of hydrodynamics on the transfer of pesticides in water flows in agricultural ditches. Special attention was given to four parameters: i) the speed of the surface water flow, ii) the submergence, defined as the mean ratio between the height of the bedforms and the water depth, iii) the shape of the bedforms and iv) the water content of the bed substrate before contamination by pesticides. The influence of these various parameters was investigated with an experimental flume, using a standard of substrate made of hemp fibres. Hemp fibres were chosen as a simplified model of natural substrates such as grass, dead leaves, decaying vegetation, straw and sediments, which are rather complex and heterogeneous. Hemp fibres were selected from preliminary laboratory studies which allowed to compare the adsorption and desorption characteristics of various pesticides for different fibres often used in the geotextile industry (jute, linen, hemp, polyamide, polypropylene and polyester). The flume experiments were designed in order to assess the influence of the four parameters mentioned above. The comparison between the different experiments shows that an increase in surface water speed results in an increase in the amount of pesticides transferred from the water to the bed substrate and the transfer kinetics. A similar result is observed when increasing the submergence, or when going from small sinusoidal bedforms to larger rectangular bedforms. In addition, the data show that the transfer of pesticides from surface water to the bed substrate is strongly decreased when the substrate was saturated with water at the beginning of the experiments. Also, it appears that there is a link between the influence of the differents parameters. When considering the long time duration and the cost of the experiments, it was decided to use a model from the literature which was adapted and used to confirm and extend the interpretation of the experimental data.

Groundwater-surface water interactions between streams and shallow alluvial aquifers can significantly affect their thermal and chemical regimes and thus are critical for effective management of water resources and riparian ecosystems. Of particular significance is the hyporheic zone, an area delineated by subsurface flow paths that begin and end in surface water bodies. Although detailed work has examined hyporheic flow in the vertical dimension, some studies have suggested that the drop in a stream’s elevation as it flows downstream can laterally extend the hyporheic zone. This study examines intra-meander hyporheic flow using extensive field measurements in a full-scale experimental stream-aquifer system. Synoptic head measurements from 2008 and 2009 and a lithium tracer test were conducted to determine the extent and nature of hyporheic flow within the meander. Permeability was measured and sediment cores were analyzed from 2008 to 2009 to assess aquifer properties. Finally, transient head and temperature measurements were collected during flooding events to assess the sensitivity of intra-meander hyporheic flow and temperature to stream discharge. Results verify that hyporheic flow through meanders occurs, but show that it is sensitive to whether a stream is gaining or losing water to the subsurface overall. In addition, permeability and core grain size results indicate moderate heterogeneity in permeability can occur in aquifers composed of relatively uniform sediment. Results also demonstrate that permeability in alluvial aquifers can evolve through time. Such evolution may be driven by groundwater flow, which transports fine particles from areas where porosity and permeability are relatively high and deposits them where they are relatively low, thus creating a positive feedback loop. Finally, measurements during flooding indicate that steady-state hyporheic flow and the thermal regime within the aquifer are largely insensitive to stream discharge. Together, these results expand upon previous field studies of intra-meander hyporheic flow and verify previous modeling work, although they demonstrate a level of complexity within these systems that should be considered in future work. / text

Matter retention in streams and rivers is an ecosystem service of outstanding ecological as well as economic importance. Studying and monitoring instream nitrate dynamics is essential to reduce the tremendous consequences of eutrophication of freshwater systems and coastal zones. Moreover, the cycling of nitrate in lotic systems is a paradigm for the instream transport and transformation behavior of any other reactive substance subjected to human perturbation of its natural cycle. Identifying instream processes and drivers that dictate nitrate transport in rivers and quantifying the capacity of rivers to retain nitrate is therefore of scientific as well as political interest and was the motivation for this thesis. Even though understanding and monitoring of instream nitrate dynamics is advanced compared to most other emerging substances of concern (e.g. pharmaceuticals, synthetic and natural hormones), methodologies to directly assess nitrate dynamics are still limited, leaving a high degree of uncertainty to descriptive and predictive models. One major problem of common data acquisition is that the temporal and spatial variability of nitrate processing rates arising from the complex interactions of hydrological and biogeochemical drivers cannot be captured with traditional methods. For technical reasons, most studies have been conducted in small (and rather pristine) streams. Thus, particularly the functional behavior of larger rivers and anthropogenically modified systems is widely uncharacterized. In this work, two methodologies were developed which allow quantitatively assessing nitrate dynamics on two relevant scales: The reach scale (1), which is of particular interest for monitoring strategies and local hyporheic nutrient fluxes (2), with the hyporheic zone being a key compartment in instream solute cycling. In order to assess the seasonal fluctuation in nitrate dynamics (3), a primary demand on the methods was that they operate continuous or over longer time spans. On the reach scale, a combined two-station time-series and longitudinal profiling approach based on measurements from automated sensors, provided novel insights into seasonal variations of nitrogen processing and allowed quantitative comparison of the dynamics in a natural versus a heavily modified reach. Uptake was lower and the influence of season on uptake rates more marked in the modified reach. Continuous implementation of the proposed approach, fully covering the annual variations, can essentially improve existing monitoring practices by quantifying the effect of altered morphology and water chemistry on retention rates. Hyporheic passive flux meters are an efficient tool to quantify time integrative hyporheic nutrient fluxes. In combination with other measurements, the results from a field application unraveled an unexpected hyporheic source-sink behavior for nitrate at the study reach. Different to common observations, not the upper most layer of the hyporheic zone but the layer between 15 and 30 cm was most efficient in removing nitrate, assumedly because substrate limitation is irrelevant in agricultural (nutrient and DOC enriched) streams. Further, higher discharge did not increase hyporheic exchange, because the monotonous morphology and absence of bedforms reduced the usually dominating effect of increased drag resistance with higher flow. The studies presented here deliver empirical evidence that, on both investigated scales, anthropogenic modifications substantially impact instream nitrate dynamics. Alterations to channel morphology, riparian vegetation, hydrology and water quality change principal ecosystem functions relevant for solute retention in streams and rivers. The presented results show that anthropogenically modified systems may therefore behave unexpectedly if predictions are built on the driver-response correlations observed in natural systems. Worldwide a large proportion of rivers and streams are modified by humans. However, altered systems are not adequately represented in studies focusing on solute dynamics. Efficient management of such systems, including evaluation of measures to reduce the nitrogen burden on receiving water bodies, requires quantitative knowledge on instream processes and governing drivers. Continuous or time integrative observations are more representative for the solute cycling characteristics of a system than “snapshot”-like assessments. The new methodologies thereby also facilitate extrapolation of local measurements and linking the resulting data with catchment scale models. Overall synthesis of the presented results suggests that such measurements of nitrate dynamics in streams may be used as an indicator for the ecosystem integrity. / Der Rückhalt von Stoffen in Flüssen und Bächen ist eine Ökosystem-Dienstleistung von grösster ökologischer wie auch wirtschaftlicher Bedeutung. Um die negativen Auswirkungen durch Eutrophierung von Süsswasserkörpern und Küstengebieten zu reduzieren, ist es erforderlich, die Stickstoffdynamik in Fliessgewässern zu untersuchen und zu überwachen. Darüber hinaus, kann der Umsatz von Nitrat in lotischen Systemen als Paradigma für den Transport und die Transformation anderer reaktiver Substanzen von anthropogenem Ursprung gesehen werden. Die Prozesse zu identifizieren, die den Nitrattransport in Fliessgewässern und deren Kapazität Nitrat zurückzuhalten beeinflussen, ist somit von wissenschaftlichem wie auch von politischem Interesse und war die Motivation für diese Arbeit. Obwohl unser Wissen über das Verhalten von Nitrat in Fliessgewässern, im Vergleich zu vielen erst neuerdings an Bedeutung gewinnender Substanzen (z.B. Arzneimittelrückstände, synthetische und natürliche Hormone) fortgeschritten ist, fehlen Methoden um die Nitratdynamik im Fliessgewässer zu erfassen. Dadurch ist die Überwachung wie auch der Vorhersage des Nitratexports durch Fliessgewässer mit grossen Unsicherheiten behaftet. Ein Hauptproblem bei der Datenerfassung ist, dass die Umsatzraten von Nitrat aufgrund der komplexen Zusammenspiele von biogeochemischen wie auch hydrologischen Einflussfaktoren, sowohl räumlich wie auch zeitlich stark schwanken. Ausserdem wurden aus technischen Gründen die meisten Studien bislang in kleinen (und eher unberührten) Flüssen durchgeführt. Deshalb bestehen insbesondere über das Exportverhalten grosser und anthropogen veränderter Systeme grosse Unsicherheiten. In dieser Arbeit wurden zwei Methoden entwickelt, die es erlauben, die Nitratdynamiken auf zwei relevanten Grössenskalen zu erfassen: Einmal über eine Flussstrecke von einigen Kilometern und zum anderen lokal in der Hyporheischen Zone. Die erste Skala (Flusstrecke) ist insbesondere für die Entwicklung von Monitoring-Strategien wichtig. Die Hyporheische Zone ist als Schlüsselkompartiment für den Stoffumsatz in Fliessgewässern von Bedeutung. Da zeitliche (z.B. saisonale) Schwankungen im Nitratumsatz erfasst werden sollten, war eine primäre Herausforderung an die Methoden, dass sie für die kontinuierliche Aufzeichnung über länger Zeitspannen geeignet sind. Für die Fliessgewässerstrecke wurde eine Bilanzierung von Zeitreihen zwischen zwei Stationen mit Messungen über das Längsprofil kombiniert. Die Zeitreihen wurden mit automatisierten Sensoren aufgenommen. Der hier entwickelte Ansatz von Messung und Auswertung lieferte neue Erkenntnisse über die saisonale Variation des Stickstoffumsatzes und ermöglichte einen quantitativen Vergleich zwischen einem natürlichen und einem anthropogen überprägten Gewässerabschnitt. Der Nitratrückhalt im veränderten Abschnitt war niedriger und der Einfluss der Jahreszeit auf die Umsatzraten war stärker ausgeprägt. Eine dauerhafte Installierung des Messaufbaus, der die gesamten Jahresschwankungen abdeckt, könnte die existierenden Überwachungsverfahren erheblich verbessern, weil so der Effekt der Fliessgewässermorphologie und der Wasserchemie auf die Umsatzraten berücksichtigt werden können. Hyporheische Passive Flux Meter sind ein Instrument für die zeitlich gemittelte Quantifizierung von Nitratflüsse durch die Hyporheische Zone. In Kombination mit weiteren Messungen brachten die Ergebnisse einer Freilandmessung unerwartete Ergebnisse über die Entstehung und den Abbau von Nitrat in der Hyporheischen Zone des untersuchten Flusses zum Vorschau. Anders als üblicher Weise beobachtet, war der Abbau von Nitrat nicht in der obersten Schicht der Hyporheischen Zone, sondern in einer Tiefe von 15 bis 30 cm am effizientesten. Wahrscheinlich verhalten sich landwirtschaftlich beeinflusste Gewässer (die mit Nitrat und organischen Stoffen angereichert sind) diesbezüglich nicht laut Lehrbuchmeinung, weil es nicht zur Stofflimitierung in tieferen Schichten kommt. Ebenso unerwartet führten höhere Abflüsse nicht zu vermehrtem hyporheischen Austausch. Es zeigte sich, dass durch die Begradigung des Fliessgewässers, der normalerweise auftretende Austausch an Gewässerbettformen, der mit zunehmenden Abfluss steigt, nicht relevant ist. Die hier vorgestellten Studien liefern empirische Beweise, dass auf beiden untersuchten Skalen anthropogene Veränderungen die Nitratdynamik im Fliessgewässer erheblich beeinflussen. Eingriffe in die Morphologie, Ufervegetation, Hydrologie und Wasserqualität verändern wesentliche Ökosystem-Funktionen, die relevant für den Stoffrückhalt in Flüssen und Bächen sind. Die präsentierten Ergebnisse zeigen dass sich anthropogen veränderte Systeme überraschend verhalten, wenn Vorhersagen auf Aktio-Reaktio-Korrelationen getroffen werden, die aus Beobachtungen in natürlichen Systemen abgeleitet wurden. Weltweit ist ein grosser Anteil der Flüsse und Bäche durch Menschen verändert. Solche beeinträchtigten Fliessgewässer sind jedoch nicht angemessen in Studien über Stoffdynamiken vertreten untersuchen. Effizientes Management solcher Fliessgewässer, ebenso wie die Beurteilung von Massnahmen um die Nitratlast auf die empfangenden Fliessgewässer zu reduzieren, benötigen quantitative Aussagen über Prozesse und vorherrschende Auslöser. Kontinuierliche wie auch zeitlich integrierende Beobachtungen sind repräsentativer als Schnappschuss-Aufnahmen. Die neuen Methoden erleichtern damit auch die Übertragung lokaler Messungen und die Einbindung der gewonnenen Daten in Einzugsgebiet Modelle. Die hier vorgestellten Ergebnisse zeigen des Weiteren, dass die Nitratdynamik in einem Fliessgewässer als Indikator für die Intaktheit des Ökosystems verwendet werden kann.

Obwohl der Bedeutung von hyporheischen Zonen als Übergangsbereiche zwischen Flüssen und angrenzenden alluvialen Aquiferen eine wachsende Anerkennung zuteilwird, sind dynamische hyporheische Reaktionen auf instationäre hydrologische Bedingungen weiterhin signifikant untererforscht. Um diese Lücke zu schließen, liegt der Fokus dieser Doktorarbeit insbesondere auf den Effekten transienter Abflussverhalten und Temperaturschwankungen in Flüssen auf die raumzeitliche Variabilität von hyporheischen Austauschprozessen. Unter Beachtung dieser Ziele wird ein neues physikalisch basiertes numerisches Modell vorgeschlagen und schließlich angewandt, um systematisch die hyporheischen, durch Sedimentoberflächenstrukturen ausgelösten Reaktionen auf eine Reihe von künstlichen und natürlichen Abflussregimen abzuschätzen. Parameter wie das räumliche Ausmaß der hyporheischen Zone, hyporheische Austauschrate, mittlere Aufenthaltszeit, Temperatur des hyporheischen Flusses sowie das Denitrifikationspotenzial werden definiert, um den Einfluss der Antriebskräfte und Regulatoren auf dynamische hyporheische Reaktionen zu quantifizieren. Die Ergebnisse zeigen, dass mit zunehmendem Abfluss generell das räumliche Ausmaß der hyporheischen Zone vergrößert wird; jedoch bestimmen geomorphologische Bedingungen und Grundwasserflüsse erheblich das Ausdehnen und Zusammenziehen hyporheischer Zonen zusammen mit Strömungen, Wärme- und Stoffaustausch zwischen Fluss und Grundwasser. Temperaturvariabilität, ein wichtiger Faktor, welcher oft in hydrodynamischen Studien vernachlässigt wird, zeigt direkte kontrollierende Effekte beim Bestimmen hyporheischer Austauschraten und mittlerer Aufenthaltszeiten. Weiterhin spielt die Dynamik von Grundwasserständen eine entscheidende Rolle bei hyporheischen Austauschprozessen. Das Optimieren der Terminierung von Grundwasserförderung ist ausschlaggebend für die Regulierung von Wasserqualität, Nährstoffkreisläufen und der Entstehung thermischer hyporheischer Refugien. / Although there is a growing recognition of the importance of hyporheic zones as transitional areas connecting rivers and adjacent alluvial aquifers, the dynamic hyporheic responses to unsteady hydrological conditions are still significantly understudied. To bridge this gap, the present PhD thesis primarily focuses on the effects of transient river discharge and temperature fluctuations on the spatiotemporal variability of hyporheic exchange processes. With these objectives in mind, a novel physically based numerical model is proposed and then applied to systematically evaluate bedform-induced hyporheic responses to a series of synthetic and natural hydrological regimes. Metrics including spatial hyporheic extent, hyporheic exchange rate, mean residence time, temperature of hyporheic flux, and denitrification potential are defined to quantify the impact of drivers and modulators of dynamic hyporheic responses. Results indicate that increasing river discharge generally enlarges the spatial hyporheic extent; however, geomorphological settings and groundwater fluxes substantially modulate the expansion and contraction of hyporheic zones along with flow, heat and solute exchange between river and groundwater. Temperature variability, an important factor which is often neglected in hydrodynamic studies, displays direct controlling effects in determining hyporheic exchange rates and mean residence times. Groundwater table dynamics also play a critical role in hyporheic exchange processes. Optimizing the timing of aquifer pumping is crucial for regulation of water quality, nutrient cycling, and the formation of thermal hyporheic refugia. The findings largely advanced our mechanistic understandings of dynamic hyporheic responses to varying transient flow and temperature conditions, and therefore shed lights on improving river management and restoration strategies.