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Das biogene Amin Serotonin (5-Hydroxytryptamin, 5-HT) agiert als wichtiger chemischer Botenstoff bei einer Vielzahl von Organismen. Das durch 5 HT vermittelte Signal wird dabei durch spezifische Rezeptoren wahrgenommen und in eine zelluläre Reaktion umgesetzt. Diese 5 HT Rezeptoren gehören überwiegend zur Familie der G Protein gekoppelten Rezeptoren (GPCRs). Die Honigbiene Apis mellifera bietet unter anderem aufgrund ihrer eusozialen Lebensweise vielfältige Ansatzpunkte zur Erforschung der Funktionen des serotonergen Systems in Insekten. Bei A. mellifera wurden bereits vier 5-HT-Rezeptor-Subtypen beschrieben und molekular sowie pharmakologisch charakterisiert: Am5 HT1A, Am5 HT2α, Am5 HT2β und Am5 HT7. Ziel dieser Arbeit war es, gewebespezifische sowie alters- und tageszeitabhängige Expressionsmuster der 5 HT Rezeptor-Subtypen zu untersuchen, um zu einem umfassenden Verständnis des serotonergen Systems der Honigbiene beizutragen und eine Basis zur Hypothesenentwicklung für mögliche physiologische Funktionen zu schaffen.
Es wurde die Expression der 5 HT Rezeptorgene sowohl im zentralen Nervensystem, als auch in Teilen des Verdauungs-, Exkretions- und Speicheldrüsensystems gemessen. Dabei konnte gezeigt werden, dass die untersuchten 5-HT-Rezeptor-Subtypen generell weit im Organismus der Honigbiene verbreitet sind. Interessanterweise unterschieden sich die untersuchten Gewebe hinsichtlich der mRNA-Expressionsmuster der untersuchten Rezeptoren. Während beispielsweise im Gehirn Am5 ht1A und Am5 ht7 stärker als Am5 ht2α und Am5 ht2β exprimiert wurden, zeigte sich in Darmgewebe ein umgekehrtes Muster.
Es war bereits bekannt, dass es bei der Expression der Am5-ht2-Gene zu alternativem Spleißen kommt. Dies führt zur Entstehung der verkürzten mRNA-Varianten Am5 ht2αΔIII und Am5 ht2βΔII. Die daraus resultierenden Proteine können nicht als funktionelle GPCRs agieren. Es konnte gezeigt werden, dass diese verkürzten Spleißvarianten dennoch ubiquitär in der Honigbiene exprimiert werden. Bemerkenswerterweise wurden gewebeübergreifende Ähnlichkeiten der Expressionsmuster der Spleißvarianten gegenüber deren zugehörigen Volllängenvarianten festgestellt, welche auf Funktionen der verkürzten Varianten in vivo hindeuten.
Im Hinblick auf die bei A. mellifera hauptsächlich altersbedingte Arbeitsteilung wurde die Expression der 5 HT Rezeptor-Subtypen in Gehirnen von unterschiedlich alten Arbeiterinnen mit unterschiedlichen sozialen Rollen verglichen. Während auf mRNA-Ebene keines der vier 5 HT Rezeptor-Subtypen eine altersabhängig unterschiedliche Expression zeigte, konnte für das Am5-HT1A-Protein eine höhere Konzentration in den Gehirnen älterer Tiere gefunden werden. Dies deutet auf eine posttranskriptionale Regulation der 5 HT1A Rezeptorexpression hin, welche im Zusammenhang mit der Arbeitsteilung stehen könnte.
Es erfolgte die Untersuchung tageszeitlicher Änderungen sowohl der Expression der 5 HT Rezeptor-Subtypen, als auch des biogenen Amins 5 HT selbst. Während es in den Gehirnen von Arbeiterinnen, welche unter natürlichen Bedingungen gehalten wurden, zu keiner tageszeitabhängigen Veränderung des 5 HT-Titers kam, zeigte die mRNA-Expression von Am5-ht2α und Am5-ht2β eine periodische Oszillation mit Zunahme während des Tages und Abnahme während der Nacht. Diese Regulation wird durch externe Faktoren hervorgerufen und ist nicht auf einen endogenen circadianen Rhythmus zurückzuführen. Dies ging aus der Wiederholung der Expressionsmessungen an Gehirnen von Bienen, welche unter konstanten Laborbedingungen gehalten wurden, hervor.
Weiterhin wurde die Beteiligung des serotonergen Systems an der Steuerung von Aspekten des circadianen lokomotorischen Aktivitätsrhythmus anhand von Verhaltensexperimenten untersucht. Mit 5 HT gefütterte Arbeiterinnen zeigten dabei unter konstanten Bedingungen eine längere Periode des Aktivitätsrhythmus als Kontrolltiere. Dies deutet auf einen Einfluss von 5 HT auf die Modulation der Synchronisation der inneren Uhr hin.
Die vorliegenden Ergebnisse tragen wesentlich zum tieferen Verständnis des serotonergen Systems der Honigbiene bei und bieten Ansatzpunkte für weitergehende Studien zur Funktion von 5 HT im Zusammenhang mit der Modulation von physiologischen Prozessen, Arbeitsteilung und circadianen Rhythmen.
Die sensorisch einwandfreie, konstant gute Qualität von Backprodukten, die beim Verbraucher einen hohen Stellenwert hat, wird maßgeblich durch den Gehalt endogener Getreideenzyme beeinflusst. Seit dem Auftreten züchtungsbedingter Enzymdefizite ist der Einsatz technischer Enzyme zur Gewährleistung dieser geforderten Qualität eine feste Größe in der Backwarenindustrie. Lebensmittelrechtlich werden technische Enzyme nicht als Zutat betrachtet, da sie theoretisch während des Backprozesses umgesetzt werden und im Endprodukt keine technologische Wirkung mehr zeigen. Vor allem in gebackenen Produkten bedarf es der Prüfung, dass die eingesetzten technischen Enzyme nicht mehr als Zutat vorliegen und sich somit einer potentiellen Deklarationspflicht entziehen. Zur Gewährleistung der Wirtschaftlichkeit muss der quantitative Einsatz technischer Enzyme in der Backwarenindustrie gesteuert werden, um optimale Effekte zu erzielen und Kosten zu sparen. Ziel dieser Arbeit war daher die Entwicklung eines Analysenverfahrens, das den simultanen Nachweis verschiedener technischer Enzyme und deren Quantifizierung im Spurenbereich auch in gebackenen Produkten ermöglicht.
Für die Einschätzung der Wirkung der technischen Enzyme Fungamyl (Novozymes), Amylase TXL (ASA Spezialenzyme GmbH) sowie Lipase FE-01 (ASA Spezialenzyme GmbH) wurden Backversuche durchgeführt, die zeigten, dass Fungamyl und Amylase TXL zu einer verbesserten Brotqualität (Volumenausbeute, Feuchtegehalt, Sensorik) beitrugen. Die Zugabe der Lipase FE-01 führte zu einer vermehrten Bildung freier Fettsäuren und wirkte sich negativ auf die sensorische Brotqualität aus. Dieser bisher nicht beschriebene Effekt konnte auf die Nutzung eines Spezialöls als Backzutat zurückgeführt werden, welches ausschließlich aus gesättigten Fettsäuren besteht. Dies bestätigt die Bedeutung der Auswahl eines geeigneten Fettes beim Zusatz technischer Lipase zum Backprozess.
Um die in Fungamyl und Lipase FE-01 enthaltenen Enzyme zu identifizieren, wurden SDS-PAGE und anschließender In-Gel-Verdau angewendet um die Analyse proteolytisch gespaltener Proteine mit MALDI-TOF-MS zu ermöglichen. Es konnte gezeigt werden, dass Fungamyl ein Gemisch aus 9,8 % alpha-Amylase (Aspergillus oryzae) und 5,2 % Endo-1,4-Xylanase (Thermomyces lanuginosus) enthält. Lipase FE-01 besteht aus der Lipase (Thermomyces lanuginosus), Amylase TXL wurde als alpha-Amylase (Aspergillus oryzae) identifiziert.
Zur Analyse der technischen Enzyme in Backwaren wurde aufgrund seiner Robustheit und Sensitivität das Verfahren der LC-MS/MS gewählt. Die Entwicklung einer solchen Methode zur Detektion spezifischer Peptide ermöglichte den qualitativen Nachweis der 3 Enzyme alpha-Amylase (Aspergillus oryzae), Endo-1,4-Xylanase (Thermomyces lanuginosus) und Lipase (Thermomyces lanuginosus). Durch eine lineare Kalibrierung aus synthetisch hergestellten Peptiden unter Einbeziehung eines Protein-Internen-Standards sowie isotopenmarkierter Peptidstandards erfolgte darüber hinaus die quantitative Bestimmung in selbst hergestellten Referenzmaterialien (Weizenmehl, Toastbrot und Biskuitkeks). In weniger als 20 Minuten Messzeit kann das Enzym alpha-Amylase ab einer Konzentration von 2,58 mg/kg (Mehl, Keks), bzw. 7,61 mg/kg (Brot) quantitativ nachgewiesen werden. Zeitgleich können die Enzyme Endo-1,4-Xylanase ab einer Konzentration von 7,75 mg/kg (Brot), 3,64 mg/kg (Keks) bzw. 15,60 mg/kg (Mehl) sowie Lipase ab einer Konzentration von 1,26 mg/kg (Mehl, Keks), bzw. 2,68 mg/kg (Brot) quantifiziert werden. Die Methode wurde nach allgemein verwendeten Richtlinien im Zuge einer Validierung statistisch geprüft und lieferte sehr robuste und reproduzierbare quantitative Werte mit Wiederfindungsraten zwischen 50 % und 122 %. Das primäre Ziel dieser Arbeit, die Entwicklung eines quantitativen Multiparameterverfahrens zum Nachweis technischer Enzyme in Backwaren, wurde somit erfolgreich umgesetzt.
Earthquakes deform Earth's surface, building long-lasting topographic features and contributing to landscape and mountain formation.
However, seismic waves produced by earthquakes may also destabilize hillslopes, leading to large amounts of soil and bedrock moving downslope. Moreover, static deformation and shaking are suspected to damage the surface bedrock and therefore alter its future properties, affecting hydrological and erosional dynamics. Thus, earthquakes participate both in mountain building and stimulate directly or indirectly their erosion. Moreover, the impact of earthquakes on hillslopes has important implications for the amount of sediment and organic matter delivered to rivers, and ultimately to oceans, during episodic catastrophic seismic crises, the magnitude of life and property losses associated with landsliding, the perturbation and recovery of landscape properties after shaking, and the long term topographic evolution of mountain belts. Several of these aspects have been addressed recently through individual case studies but additional data compilation as well as theoretical or numerical modelling are required to tackle these issues in a more systematic and rigorous manner.
This dissertation combines data compilation of earthquake characteristics, landslide mapping, and seismological data interpretation with physically-based modeling in order to address how earthquakes impact on erosional processes and landscape evolution. Over short time scales (10-100 s) and intermediate length scales (10 km), I have attempted to improve our understanding and ability to predict the amount of landslide debris triggered by seismic shaking in epicentral areas. Over long time scales (1-100 ky) and across a mountain belt (100 km) I have modeled the competition between erosional unloading and building of topography associated with earthquakes. Finally, over intermediate time scales (1-10 y) and at the hillslope scale (0.1-1 km) I have collected geomorphological and seismological data that highlight persistent effects of earthquakes on landscape properties and behaviour.
First, I compiled a database on earthquakes that produced significant landsliding, including an estimate of the total landslide volume and area, and earthquake characteristics such as seismic moment and source depth. A key issue is the accurate conversion of landslide maps into volume estimates. Therefore I also estimated how amalgamation - when mapping errors lead to the bundling of multiple landslide into a single polygon - affects volume estimates from various earthquake-induced landslide inventories and developed an algorithm to automatically detect this artifact. The database was used to test a physically-based prediction of the total landslide area and volume caused by earthquakes, based on seismological scaling relationships and a statistical description of the landscape properties. The model outperforms empirical fits in accuracy, with 25 out of 40 cases well predicted, and allows interpretation of many outliers in physical terms. Apart from seismological complexities neglected by the model I found that exceptional rock strength properties or antecedent conditions may explain most outliers.
Second, I assessed the geomorphic effects of large earthquakes on landscape dynamics by surveying the temporal evolution of precipitation-normalized landslide rate. I found strongly elevated landslide rates following earthquakes that progressively recover over 1 to 4 years, indicating that regolith strength drops and recovers. The relaxation is clearly non-linear for at least one case, and does not seem to correlate with coseismic landslide reactivation, water table level increase or tree root-system recovery. I suggested that shallow bedrock is damaged by the earthquake and then heals on annual timescales. Such variations in ground strength must be translated into shallow subsurface seismic velocities that are increasingly surveyed with ambient seismic noise correlations. With seismic noise autocorrelation I computed the seismic velocity in the epicentral areas of three earthquakes where I constrained a change in landslide rate. We found similar recovery dynamics and timescales, suggesting that seismic noise correlation techniques could be further developed to meaningfully assess ground strength variations for landscape dynamics. These two measurements are also in good agreement with the temporal dynamics of post-seismic surface displacement measured by GPS. This correlation suggests that the surface healing mechanism may be driven by tectonic deformation, and that the surface regolith and fractured bedrock may behave as a granular media that slowly compacts as it is sheared or vibrated.
Last, I compared our model of earthquake-induced landsliding with a standard formulation of surface deformation caused by earthquakes to understand which parameters govern the competition between the building and destruction of topography caused by earthquakes. In contrast with previous studies I found that very large (Mw>8) earthquakes always increase the average topography, whereas only intermediate (Mw ~ 7) earthquakes in steep landscapes may reduce topography. Moreover, I illustrated how the net effect of earthquakes varies with depth or landscape steepness implying a complex and ambivalent role through the life of a mountain belt. Further I showed that faults producing a Gutenberg-Richter distribution of earthquake sizes, will limit topography over a larger range of fault sizes than faults producing repeated earthquakes with a characteristic size.
The relationship between climate and forest productivity is an intensively studied subject in forest science. This Thesis is embedded within the general framework of future forest growth under climate change and its implications for the ongoing forest conversion. My objective is to investigate the future forest productivity at different spatial scales (from a single specific forest stand to aggregated information across Germany) with focus on oak-pine forests in the federal state of Brandenburg. The overarching question is: how are the oak-pine forests affected by climate change described by a variety of climate scenarios. I answer this question by using a model based analysis of tree growth processes and responses to different climate scenarios with emphasis on drought events. In addition, a method is developed which considers climate change uncertainty of forest management planning.
As a first 'screening' of climate change impacts on forest productivity, I calculated the change in net primary production on the base of a large set of climate scenarios for different tree species and the total area of Germany. Temperature increases up to 3 K lead to positive effects on the net primary production of all selected tree species. But, in water-limited regions this positive net primary production trend is dependent on the length of drought periods which results in a larger uncertainty regarding future forest productivity. One of the regions with the highest uncertainty of net primary production development is the federal state of Brandenburg.
To enhance the understanding and ability of model based analysis of tree growth sensitivity to drought stress two water uptake approaches in pure pine and mixed oak-pine stands are contrasted. The first water uptake approach consists of an empirical function for root water uptake. The second approach is more mechanistic and calculates the differences of soil water potential along a soil-plant-atmosphere continuum. I assumed the total root resistance to vary at low, medium and high total root resistance levels. For validation purposes three data sets on different tree growth relevant time scales are used. Results show that, except the mechanistic water uptake approach with high total root resistance, all transpiration outputs exceeded observed values. On the other hand high transpiration led to a better match of observed soil water content. The strongest correlation between simulated and observed annual tree ring width occurred with the mechanistic water uptake approach and high total root resistance. The findings highlight the importance of severe drought as a main reason for small diameter increment, best supported by the mechanistic water uptake approach with high root resistance. However, if all aspects of the data sets are considered no approach can be judged superior to the other. I conclude that the uncertainty of future productivity of water-limited forest ecosystems under changing environmental conditions is linked to simulated root water uptake.
Finally my study aimed at the impacts of climate change combined with management scenarios on an oak-pine forest to evaluate growth, biomass and the amount of harvested timber. The pine and the oak trees are 104 and 9 years old respectively. Three different management scenarios with different thinning intensities and different climate scenarios are used to simulate the performance of management strategies which explicitly account for the risks associated with achieving three predefined objectives (maximum carbon storage, maximum harvested timber, intermediate). I found out that in most cases there is no general management strategy which fits best to different objectives. The analysis of variance in the growth related model outputs showed an increase of climate uncertainty with increasing climate warming. Interestingly, the increase of climate-induced uncertainty is much higher from 2 to 3 K than from 0 to 2 K.
Die vorliegende Untersuchung verfolgt das Ziel, kulturelle und religiöse Aspekte der Erneuerung jüdischen Lebens in Berlin seit 1989 zu erforschen. Die Entwicklungen der jüdischen Gemeinschaft in der Hauptstadt seit dem Fall der Mauer und dem Zusammenbruch der Sowjetunion führen zur Wiederannäherung eines Teils der jüdischen Bevölkerung in Deutschland an die eigene Kultur, Religion und Geschichte. Dabei kommt die Pluralität der kulturellen, literarischen und religiösen Ausdrucksformen der jüdischen Identitäten zum Vorschein. Die Arbeit verdeutlicht diese in Berlin nach 1989 einsetzende kulturelle und religiöse „Renaissance“. Vier wichtige Punkte kennzeichnen das jüdische Leben in Berlin nach 1989. Erstens gewinnt Deutschland seit der Wiedervereinigung eine neue Rolle als mögliches Einwanderungsland für Juden. Vor allem mit der massiven jüdischen Einwanderung aus den Staaten der ehemaligen Sowjetunion seit den 1990er Jahren wird Deutschland allmählich als wichtiges Zentrum in der europäischen Diaspora anerkannt. Zweitens bleibt zwar die Shoah tief verankert im Gedächtnis der jüdischen Gemeinschaft; die meisten Kinder oder Enkelkinder von Überlebenden der Shoah weigern sich jedoch, ihre jüdische Identität exklusiv durch die Shoah zu definieren. Sie gründen zur Wiederentdeckung und Forderung ihres kulturellen, religiösen und historischen Erbes jüdische Gruppen und Einrichtungen in Berlin, die in den meisten Fällen alternativ zur Jüdischen Gemeinde entstehen: Künstlergruppen, jüdische Kulturvereine, Konferenzen und Podiumsdiskussionen, religiöse Kongregationen und Lernhäuser. Damit – und dies ist der dritte Punkt – verliert zwar die offizielle Jüdische Gemeinde an Bedeutung als einzige Vertreterin der jüdischen Gemeinschaft Berlins; diese kulturelle und religiöse „Renaissance“ außerhalb der offiziellen Strukturen der Gemeinde bedeutet aber auch eine wachsende Pluralität und Diversifizierung der jüdischen Gemeinschaft in Berlin. Viertens spielt Berlin die Hauptrolle in diesem Prozess. Heute werden viele ehemalige jüdische Orte neu belebt: Synagogen werden wiederentdeckt und renoviert, Denk- und Mahnmale gebaut, Stadtführungen auf der Spur des „jüdischen Berlins“ organisiert, Rabbinerseminare neu gegründet. Die Topographie Berlins bildet auch eine Inspirationsquelle für jüdische (und nichtjüdische) Schriftsteller und Künstler. Die Analyse dieser nach 1989 entstandenen religiösen Initiativen, literarischen Werke und kulturellen Produktionen dient dazu, Aspekte der kulturellen und religiösen „Renaissance“ in Berlin näher zu verdeutlichen.
This thesis presents new approaches of SAR methods and their application to tectonically active systems and related surface deformation. With 3 publications two case studies are presented:
(1) The coseismic deformation related to the Nura earthquake (5th October 2008, magnitude Mw 6.6) at the eastern termination of the intramontane Alai valley. Located between the southern Tien Shan and the northern Pamir the coseismic surface displacements are analysed using SAR (Synthetic Aperture RADAR) data. The results show clear gradients in the vertical and horizontal directions along a complex pattern of surface ruptures and active faults. To integrate and to interpret these observations in the context of the regional active tectonics a SAR data analysis is complemented with seismological data and geological field observations. The main moment release of the Nura earthquake appears to be on the Pamir Frontal thrust, while the main surface displacements and surface rupture occurred in the footwall and along of the NE–SW striking Irkeshtam fault. With InSAR data from ascending and descending satellite tracks along with pixel offset measurements the Nura earthquake source is modelled as a segmented rupture. One fault segment corresponds to high-angle brittle faulting at the Pamir Frontal thrust and two more fault segments show moderate-angle and low-friction thrusting at the Irkeshtam fault. The integrated analysis of the coseismic deformation argues for a rupture segmentation and strain partitioning associated to the earthquake. It possibly activated an orogenic wedge in the easternmost segment of the Pamir-Alai collision zone. Further, the style of the segmentation may be associated with the presence of Paleogene evaporites.
(2) The second focus is put on slope instabilities and consequent landslides in the area of prominent topographic transition between the Fergana basin and high-relief Alai range. The Alai range constitutes an active orogenic wedge of the Pamir – Tien Shan collision zone that described as a progressively northward propagating fold-and-thrust belt. The interferometric analysis of ALOS/PALSAR radar data integrates a period of 4 years (2007-2010) based on the Small Baseline Subset (SBAS) time-series technique to assess surface deformation with millimeter surface change accuracy. 118 interferograms are analyzed to observe spatially-continuous movements with downslope velocities up to 71 mm/yr. The obtained rates indicate slow movement of the deep-seated landslides during the observation time. We correlated these movements with precipitation and seismic records. The results suggest that the deformation peaks correlate with rainfall in the 3 preceding months and with one earthquake event. In the next step, to understand the spatial pattern of landslide processes, the tectonic morphologic and lithologic settings are combined with the patterns of surface deformation. We demonstrate that the lithological and tectonic structural patterns are the main controlling factors for landslide occurrence and surface deformation magnitudes. Furthermore active contractional deformation in the front of the orogenic wedge is the main mechanism to sustain relief. Some of the slower but continuously moving slope instabilities are directly related to tectonically active faults and unconsolidated young Quaternary syn-orogenic sedimentary sequences. The InSAR observed slow moving landslides represent active deep-seated gravitational slope deformation phenomena which is first time observed in the Tien Shan mountains. Our approach offers a new combination of InSAR techniques and tectonic aspects to localize and understand enhanced slope instabilities in tectonically active mountain fronts in the Kyrgyz Tien Shan.
Age of acquisition (AOA) is a psycholinguistic variable that significantly influences behavioural measures (response times and accuracy rates) in tasks that require lexical and semantic processing. Its origin is – unlike the origin of semantic typicality (TYP), which is assumed at the semantic level – controversially discussed. Different theories propose AOA effects to originate either at the semantic level or at the link between semantics and phonology (lemma-level).
The dissertation aims at investigating the influence of AOA and its interdependence with the semantic variable TYP on particularly semantic processing in order to pinpoint the origin of AOA effects. Therefore, three studies have been conducted that considered the variables AOA and TYP in semantic processing tasks (category verifications and animacy decisions) by means of behavioural and partly electrophysiological (ERP) data and in different populations (healthy young and elderly participants and in semantically impaired individuals with aphasia (IWA)).
The behavioural and electrophysiological data of the three studies provide evidence for distinct processing levels of the variables AOA and TYP. The data further support previous assumptions on a semantic origin for TYP but question the same for AOA. The findings, however, support an origin of AOA effects at the transition between the word form (phonology) and the semantic level that can be captured at the behavioural but not at the electrophysiological level.
Background: The engagement in aggressive behavior in middle childhood is linked to the development of severe problems in later life. Thus, identifying factors and processes that con-tribute to the continuity and increase of aggression in middle childhood is essential in order to facilitate the development of intervention programs. The present PhD thesis aimed at expand-ing the understanding of the development of aggression in middle childhood by examining risk factors in the intrapersonal and interpersonal domains as well as the interplay between these factors: Maladaptive anger regulation was examined as an intrapersonal risk factor; processes that occur in the peer context (social rejection and peer socialization) were included as interpersonal risk factors. In addition, in order to facilitate the in situ assessment of anger regulation strategies, an observational measure of anger regulation was developed and validated.
Method: The research aims were addressed within the scope of four articles. Data from two measurement time points about ten months apart were available for the analyses. Participants were elementary school children aged from 6 to 10 years at T1 and 7 to 11 years at T2. The first article was based on cross-sectional analyses including only the first time point; in the remaining three articles longitudinal associations across the two time points were analyzed. The first two articles were concerned with the development and cross-sectional as well as longitudinal validation of observational measure of anger regulation in middle childhood in a sample of 599 children. Using the same sample, the third article investigated the longitudinal link between maladaptive anger regulation and aggression considering social rejection as a mediating variable. The frequency as well as different functions of aggression (reactive and proactive) were included as outcomes measures. The fourth article examined the influence of class-level aggression on the development of different forms of aggression (relational and physical) over time under consideration of differences in initial individual aggression in a sample of 1,284 children. In addition, it was analyzed if the path from aggression to social rejection varies as a function of class-level aggression.
Results: The first two articles revealed that the observational measure of anger regulation developed for the purpose of this research was cross-sectionally related to anger reactivity, aggression and social rejection as well as longitudinally related to self-reported anger regula-tion. In the third article it was found that T1 maladaptive anger regulation showed no direct link to T2 aggression, but an indirect link through T1 social rejection. This indirect link was found for the frequency of aggression as well as for reactive and proactive aggression. The fourth article revealed that with regard to relational aggression, a high level of classroom ag-gression predicted an increase of individual aggression only among children with initially low levels of aggression. For physical aggression, it was found that the overall level of aggression in the class affected all children equally. In addition, physical aggression increased the likelihood of social rejection irrespective of the class-level of aggression whereas relational aggression caused social rejection only in classes with a generally low level of relational aggression. The analyses of gender-specific effects showed that children were mainly influenced by their same-gender peers and that the effect on the opposite gender was higher if children engaged in gender-atypical forms of aggressive behavior.
Conclusion: The results provided evidence for the construct and criterion validity of the observational measure of maladaptive anger regulation that was developed within the scope of this research. Furthermore, the findings indicated that maladaptive anger regulation constitutes an important risk factor of aggression through the influence of social rejection. Finally, the results demonstrated that the level of aggression among classmates is relevant for the development of individual aggression over time and that the children´s evaluation of relationally aggressive behavior varies as a function of the normativity of relational aggression in the class. The study findings have implications for the measurement of anger regulation in middle childhood as well as for the prevention of aggression and social rejection.
Molekulare Charakterisierung von CP75, einem neuen centrosomalen Protein in Dictyostelium discoideum
(2016)
Das Centrosom ist ein Zellkern-assoziiertes Organell, das nicht von einer Membran umschlossen ist. Es spielt eine wichtige Rolle in vielen Mikrotubuli- abhängigen Prozessen wie Organellenpositionierung, Zellpolarität oder die Organisation der mitotischen Spindel. Das Centrosom von Dictyostelium besteht aus einer dreischichtigen Core-Struktur umgeben von einer Corona, die Mikrotubuli-nukleierende Komplexe enthält. Die Verdoppelung des Centrosoms in Dictyostelium findet zu Beginn der Mitose statt. In der Prophase vergrößert sich die geschichtete Core-Struktur und die Corona löst sich auf. Anschließend trennen sich die beiden äußeren Lagen der Core-Struktur und bilden in der Metaphase die beiden Spindelpole, die in der Telophase zu zwei vollständigen Centrosomen heranreifen. Das durch eine Proteom-Analyse identifizierte Protein CP75 lokalisiert am Centrosom abhängig von den Mitosephasen. Es dissoziiert von der Core-Struktur in der Prometaphase und erscheint an den Spindelpolen in der Telophase wieder. Dieses Verhalten korreliert mit dem Verhalten der mittleren Lage der Core-Struktur in der Mitose, was darauf hinweist, dass CP75 eine Komponente dieser Schicht sein könnte. Die FRAP-Experimente am Interphase- Centrosom zeigen, dass GFP-CP75 dort nicht mobil ist. Das deutet darauf hin, dass das Protein wichtige Funktionen im Strukturerhalt der centrosomalen Core- Struktur übernehmen könnte. Sowohl die C- als auch die N-terminale Domäne von CP75 enthalten centrosomale Targeting-Domäne. Als GFP-Fusionsproteine (GFP-CP75-N und -C) lokalisieren die beiden Fragmente am Centrosom in der Interphase. Während GFP-CP75-C in der Mitose am Centrosom verbleibt, verschwindet GFP-CP75-N in der Metaphase und kehrt erst in der späten Telophase zurück. GFP-CP75-C und GFP-CP75O/E kolokalisieren mit F-Aktin am Zellcortex, zeigen aber keine Interaktion mit Aktin mit der BioID-Methode. Die N-terminale Domäne von CP75 enthält eine potentielle Plk1- Phosphorylierungssequenz. Die Überexpression der nichtphosphorylierbaren Punktmutante (GFP-CP75-Plk-S143A) ruft verschiedene Phänotypen wie verlängerte oder überzählige Centrosomen, vergrößerte Zellkerne und Anreicherung von detyrosinierten Mikrotubuli hervor. Die ähnlichen Phänotypen konnten auch bei GFP-CP75-N und CP75-RNAi beobachtet werden. Der
Phänotyp der detyrosinierten Mikrotubuli bringt erstmals den Beweis dafür, dass I
in Dictyostelium posttranslationale Modifikation an Tubulinen stattfindet. Außerdem zeigten CP75-RNAi-Zellen Defekte in der Organisation der mitotischen Spindel. Mittels BioID-Methode konnten drei potentielle Interaktionspartner von CP75 identifiziert werden. Diese drei Proteine CP39, CP91 und Cep192 sind ebenfalls Bestandteile des Centrosoms.
This publications-based thesis summarizes my contribution to the scientific field of ultrafast structural dynamics. It consists of 16 publications, about the generation, detection and coupling of coherent gigahertz longitudinal acoustic phonons, also called hypersonic waves. To generate such high frequency phonons, femtosecond near infrared laser pulses were used to heat nanostructures composed of perovskite oxides on an ultrashort timescale. As a consequence the heated regions of such a nanostructure expand and a high frequency acoustic phonon pulse is generated. To detect such coherent acoustic sound pulses I use ultrafast variants of optical Brillouin and x-ray scattering. Here an incident optical or x-ray photon is scattered by the excited sound wave in the sample. The scattered light intensity measures the occupation of the phonon modes.
The central part of this work is the investigation of coherent high amplitude phonon wave packets which can behave nonlinearly, quite similar to shallow water waves which show a steepening of wave fronts or solitons well known as tsunamis. Due to the high amplitude of the acoustic wave packets in the solid, the acoustic properties can change significantly in the vicinity of the sound pulse. This may lead to a shape change of the pulse. I have observed by time-resolved Brillouin scattering, that a single cycle hypersound pulse shows a wavefront steepening. I excited hypersound pulses with strain amplitudes until 1% which I have calibrated by ultrafast x-ray diffraction (UXRD).
On the basis of this first experiment we developed the idea of the nonlinear mixing of narrowband phonon wave packets which we call "nonlinear phononics" in analogy with the nonlinear optics, which summarizes a kaleidoscope of surprising optical phenomena showing up at very high electric fields. Such phenomena are for instance Second Harmonic Generation, four-wave-mixing or solitons. But in case of excited coherent phonons the wave packets have usually very broad spectra which make it nearly impossible to look at elementary scattering processes between phonons with certain momentum and energy.
For that purpose I tested different techniques to excite narrowband phonon wave packets which mainly consist of phonons with a certain momentum and frequency. To this end epitaxially grown metal films on a dielectric substrate were excited with a train of laser pulses. These excitation pulses drive the metal film to oscillate with the frequency given by their inverse temporal displacement and send a hypersonic wave of this frequency into the substrate. The monochromaticity of these wave packets was proven by ultrafast optical Brillouin and x-ray scattering.
Using the excitation of such narrowband phonon wave packets I was able to observe the Second Harmonic Generation (SHG) of coherent phonons as a first example of nonlinear wave mixing of nanometric phonon wave packets.
Neue Systeme für triphile, fluorkohlenstofffreie Blockcopolymere in Form von Acrylat-basierten thermoresponsiven Blockcopolymeren sowie Acrylat- bzw. Styrol-basierten Terblock-Polyelektrolyten mit unterschiedlich chaotropen Kationen des jeweiligen polyanionischen Blocks wurden entwickelt. Multikompartiment-Mizellen, mizellare Aggregate mit ultrastrukturiertem hydrophobem Mizellkern die biologischen Strukturen wie dem Humanalbumin nachempfunden sind, sollten bei der Selbstorganisation in wässriger Umgebung entstehen. Durch Verwendung apolarer und polarer Kohlenwasserstoff-Domänen anstelle von fluorophilen Fluorkohlenstoff-Domänen sollte erstmals anhand solcher triphilen Systeme nachgewiesen werden, ob diese in der Lage zur selektiven Aufnahme hydrophober Substanzen in unterschiedliche Domänen des Mizellkerns sind.
Mit Hilfe von sequentieller RAFT-Polymerisation wurden diese neuen triphilen Systeme hergestellt, die über einen permanent hydrophilen, eine permanent stark hydrophoben und einen dritten Block verfügen, der durch externe Einflüsse, speziell die Induzierung eines thermischen Coil-to-globule-Übergangs bzw. die Zugabe von organischen, hydrophoben Gegenionen von einem wasserlöslichen in einen polar-hydrophoben Block umgewandelt werden kann. Als RAFT-Agens wurde 4-(Trimethylsilyl)benzyl(3-(trimethylsilyl)-propyl)-trithiocarbonat mit zwei unterschiedlichen TMS-Endgruppen verwendet, das kontrollierte Reaktions-bedingungen sowie die molekulare Charakterisierung der komplexen Copolymere ermöglichte.
Die beiden Grundtypen der linearen ternären Blockcopolymere wurden jeweils in zwei 2 Modell-Systeme, die geringfügig in ihren chemischen Eigenschaften sowie in dem Blocklängenverhältnis von hydrophilen und hydrophoben Polymersegmenten variierten, realisiert und unterschiedliche Permutation der Blöcke aufwiesen.
Als ersten Polymertyp wurden amphiphile thermoresponsive Blockcopolymere verwendet. Modell-System 1 bestand aus dem permanent hydrophoben Block Poly(1,3-Bis(butylthio)-prop-2-yl-acrylat), permanent hydrophilen Block Poly(Oligo(ethylenglykol)monomethyletheracrylat) und den thermoresponsiven Block Poly(N,N‘-Diethylacrylamid), dessen Homopolymer eine LCST-Phasenübergang (LCST, engl.: lower critical solution temperature) bei ca. 36°C aufweist. Das Modell-System 2 bestand aus dem permanent hydrophilen Block Poly(2-(Methylsulfinyl)ethylacrylat), dem permanent hydrophoben Block Poly(2-Ethylhexylacrylat) und wiederum Poly(N,N‘-Diethylacrylamid). Im ternären Blockcopolymer erhöhte sich, je nach Blocksequenz und relativen Blocklängen, der LCST-Übergang auf 50 – 65°C. Bei der Untersuchung der Selbstorganisation für die Polymer-Systeme dieses Typs wurde die Temperatur variiert, um verschieden mizellare Überstrukturen in wässriger Umgebung zu erzeugen bzw. oberhalb des LCST-Übergangs Multikompartiment-Mizellen nachzuweisen. Die Unterschiede in der Hydrophilie bzw. den sterischen Ansprüche der gewählten hydrophilen Blöcke sowie die Variation der jeweiligen Blocksequenzen ermöglichte darüber hinaus die Bildung verschiedenster Morphologien mizellarer Aggregate.
Der zweite Typ basierte auf ein Terblock-Polyelektrolyt-System mit Polyacrylaten bzw. Polystyrolen als Polymerrückgrat. Polymere ionische Flüssigkeiten wurden als Vorlage der Entwicklung zweier Modell-Systeme genommen. Eines der beiden Systeme bestand aus dem permanent hydrophilen Block Poly(Oligo(ethylenglykol)monomethyletheracrylat, dem permanent hydrophoben Block Poly(2-Ethylhexylacrylat) sowie dem Polyanion-Block Poly(3-Sulfopropylacrylat). Die Hydrophobie des Polyanion-Blocks variierte durch Verwendung großer organischer Gegenionen, nämlich Tetrabutylammonium, Tetraphenylphosphonium und Tetraphenylstibonium.
Analog wurde in einem weiteren System aus dem permanent hydrophilen Block Poly(4-Vinylbenzyltetrakis(ethylenoxy)methylether), dem permanent hydrophoben Block Poly(para-Methylstyrol) und Poly(4-Styrolsulfonat) mit den entsprechenden Gegenionen gebildet. Aufgrund unterschiedlicher Kettensteifigkeit in beiden Modell-Systemen sollte es bei der Selbstorganisation der mizellarer Aggregate zu unterschiedlichen Überstrukturen kommen.
Mittels DSC-Messungen konnte nachgewiesen werden, dass für alle Modell-Systeme die Blöcke in Volumen-Phase miteinander inkompatibel waren, was eine Voraussetzung für Multikompartimentierung von mizellaren Aggregaten ist. Die Größe mizellarer Aggregate sowie der Einfluss externer Einflüsse wie der Veränderung der Temperatur bzw. der Hydrophobie und Größe von Gegenionen auf den hydrodynamischen Durchmesser mittels DLS-Untersuchungen wurden für alle Modell-Systeme untersucht. Die Ergebnisse zu den thermoresponsiven ternären Blockcopolymeren belegten , dass sich oberhalb der Phasenübergangstemperatur des thermoresponsiven Blocks die Struktur der mizellaren Aggregate änderte, indem der p(DEAm)-Block scheinbar kollabierte und so zusammen mit den permanent hydrophoben Block den jeweiligen Mizellkern bildete. Nach gewisser Equilibrierungszeit konnten bei Raumtemperatur dir ursprünglichen mizellaren Strukturen regeneriert werden. Hingegen konnte für die Terblock-Polyelektrolyt-Systeme bei Verwendung der unterschiedlich hydrophoben Gegenionen kein signifikanter Unterschied in der Größe der mizellaren Aggregate beobachtet werden.
Zur Abbildung der mizellaren Aggregate mittels kryogene Transmissionselektronenmikroskopie (cryo-TEM) der mizellaren Aggregate war mit Poly(1,3-Bis(butylthio)-prop-2-yl-acrylat) ein Modell-System so konzipiert, dass ein erhöhter Elektronendichtekontrast durch Schwefel-Atome die Visualisierung ultrastrukturierter hydrophober Mizellkerne ermöglichte. Dieser Effekt sollte in den Terblock-Polyelektrolyt-Systemen auch durch die Gegenionen Tetraphenylphosphonium und Tetraphenylstibonium nachgestellt werden. Während bei den thermoresponsiven Systemen auch oberhalb des Phasenübergangs kein Hinweis auf Ultrastrukturierung beobachtet wurde, waren für die Polyelektrolyt-Systeme, insbesondere im Fall von Tetraphenylstibonium als Gegenion Überstrukturen zu erkennen. Der Nachweis der Bildung von Multikompartiment-Mizellen war für beide Polymertypen mit dieser abbildenden Methode nicht möglich. Die Unterschiede in der Elektronendichte einzelner Blöcke müsste möglicherweise weiter erhöht werden um Aussagen diesbezüglich zu treffen.
Die Untersuchung von ortsspezifischen Solubilisierungsexperimenten mit solvatochromen Fluoreszenzfarbstoffen mittels „steady-state“-Fluoreszenzspektroskopie durch Vergleich der Solubilisierungsorte der Terblockcopolymere bzw. –Polyelektrolyte mit den jeweiligen Solubilisierungsorten von Homopolymer- und Diblock-Vorstufen sollten den qualitativen Nachweis der Multikompartimentierung erbringen. Aufgrund der geringen Mengen an Farbstoff, die für die Solubilisierungsexperimente eingesetzt wurden zeigten DLS-Untersuchungen keine störenden Effekte der Sonden auf die Größe der mizellaren Aggregate. Jedoch erschwerten Quench-Effekte im Falle der Polyelektrolyt Modell-Systeme eine klare Interpretation der Daten. Im Falle der Modell-Systeme der thermoresponsiven Blockcopolymere waren dagegen deutliche solvatochrome Effekte zwischen der Solubilisierung in den mizellaren Aggregaten unterhalb und oberhalb des Phasenübergangs zu erkennen. Dies könnte ein Hinweis auf Multikompartimentierung oberhalb des LCST-Übergangs sein. Ohne die Informationen einer Strukturanalyse wie z.B. der Röntgen- oder Neutronenkleinwinkelstreuung (SAXS oder SANS), kann nicht abschließend geklärt werden, ob die Solubilisierung in mizellaren hydrophoben Domänen des kollabierten Poly(N,N‘-Diethylacrylamid) erfolgt oder in einer Mischform von mizellaren Aggregaten mit gemittelter Polarität.
The aim of this thesis was the elucidation of different ionization methods (resonance-enhanced multiphoton ionization – REMPI, electrospray ionization – ESI, atmospheric pressure chemical ionization – APCI) in ion mobility (IM) spectrometry. In order to gain a better understanding of the ionization processes, several spectroscopic, mass spectrometric and theoretical methods were also used. Another focus was the development of experimental techniques, including a high resolution spectrograph and various combinations of IM and mass spectrometry.
The novel high resolution 2D spectrograph facilitates spectroscopic resolutions in the range of commercial echelle spectrographs. The lowest full width at half maximum of a peak achieved was 25 pm. The 2D spectrograph is based on the wavelength separation of light by the combination of a prism and a grating in one dimension, and an etalon in the second dimension. This instrument was successfully employed for the acquisition of Raman and laser-induced breakdown spectra.
Different spectroscopic methods (light scattering and fluorescence spectroscopy) permitting a spatial as well as spectral resolution, were used to investigate the release of ions in the electrospray. The investigation is based on the 50 nm shift of the fluorescence band of rhodamine 6G ions of during the transfer from the electrospray droplets to the gas phase.
A newly developed ionization chamber operating at reduced pressure (0.5 mbar) was coupled to a time-of-flight mass spectrometer. After REMPI of H2S, an ionization chemistry analogous to H2O was observed with this instrument. Besides H2S+ and its fragments, H3S+ and protonated analyte ions could be observed as a result of proton-transfer reactions.
For the elucidation of the peaks in IM spectra, a combination of IM spectrometer and linear quadrupole ion trap mass spectrometer was developed. The instrument can be equipped with various ionization sources (ESI, REMPI, APCI) and was used for the characterization of the peptide bradykinin and the neuroleptic promazine.
The ionization of explosive compounds in an APCI source based on soft x-radiation was investigated in a newly developed ionization chamber attached to the ion trap mass spectrometer. The major primary and secondary reactions could be characterized and explosive compound ions could be identified and assigned to the peaks in IM spectra. The assignment is based on the comparison of experimentally determined and calculated IM. The methods of calculation currently available exhibit large deviations, especially in the case of anions. Therefore, on the basis of an assessment of available methods, a novel hybrid method was developed and characterized.
Understanding the rates and processes of denudation is key to unraveling the dynamic processes that shape active orogens. This includes decoding the roles of tectonic and climate-driven processes in the long-term evolution of high- mountain landscapes in regions with pronounced tectonic activity and steep climatic and surface-process gradients. Well-constrained denudation rates can be used to address a wide range of geologic problems. In steady-state landscapes, denudation rates are argued to be proportional to tectonic or isostatic uplift rates and provide valuable insight into the tectonic regimes underlying surface denudation. The use of denudation rates based on terrestrial cosmogenic nuclide (TCN) such as 10Beryllium has become a widely-used method to quantify catchment-mean denudation rates. Because such measurements are averaged over timescales of 102 to 105 years, they are not as susceptible to stochastic changes as shorter-term denudation rate estimates (e.g., from suspended sediment measurements) and are therefore considered more reliable for a comparison to long-term processes that operate on geologic timescales. However, the impact of various climatic, biotic, and surface processes on 10Be concentrations and the resultant denudation rates remains unclear and is subject to ongoing discussion. In this thesis, I explore the interaction of climate, the biosphere, topography, and geology in forcing and modulating denudation rates on catchment to orogen scales.
There are many processes in highly dynamic active orogens that may effect 10Be concentrations in modern river sands and therefore impact 10Be-derived denudation rates. The calculation of denudation rates from 10Be concentrations, however, requires a suite of simplifying assumptions that may not be valid or applicable in many orogens. I investigate how these processes affect 10Be concentrations in the Arun Valley of Eastern Nepal using 34 new 10Be measurements from the main stem Arun River and its tributaries. The Arun Valley is characterized by steep gradients in climate and topography, with elevations ranging from <100 m asl in the foreland basin to >8,000 asl in the high sectors to the north. This is coupled with a five-fold increase in mean annual rainfall across strike of the orogen. Denudation rates from tributary samples increase toward the core of the orogen, from <0.2 to >5 mm/yr from the Lesser to Higher Himalaya. Very high denudation rates (>2 mm/yr), however, are likely the result of 10Be TCN dilution by surface and climatic processes, such as large landsliding and glaciation, and thus may not be representative of long-term denudation rates. Mainstem Arun denudation rates increase downstream from ~0.2 mm/yr at the border with Tibet to 0.91 mm/yr at its outlet into the Sapt Kosi. However, the downstream 10Be concentrations may not be representative of the entire upstream catchment. Instead, I document evidence for downstream fining of grains from the Tibetan Plateau, resulting in an order-of-magnitude apparent decrease in the measured 10Be concentration.
In the Arun Valley and across the Himalaya, topography, climate, and vegetation are strongly interrelated. The observed increase in denudation rates at the transition from the Lesser to Higher Himalaya corresponds to abrupt increases in elevation, hillslope gradient, and mean annual rainfall. Thus, across strike (N-S), it is difficult to decipher the potential impacts of climate and vegetation cover on denudation rates. To further evaluate these relationships I instead took advantage of an along-strike west-to-east increase of mean annual rainfall and vegetation density in the Himalaya. An analysis of 136 published 10Be denudation rates from along strike of the revealed that median denudation rates do not vary considerably along strike of the Himalaya, ~1500 km E-W. However, the range of denudation rates generally decreases from west to east, with more variable denudation rates in the northwestern regions of the orogen than in the eastern regions. This denudation rate variability decreases as vegetation density increases (R=- 0.90), and increases proportionately to the annual seasonality of vegetation (R=0.99). Moreover, rainfall and vegetation modulate the relationship between topographic steepness and denudation rates such that in the wet, densely vegetated regions of the Himalaya, topography responds more linearly to changes in denudation rates than in dry, sparsely vegetated regions, where the response of topographic steepness to denudation rates is highly nonlinear. Understanding the relationships between denudation rates, topography, and climate is also critical for interpreting sedimentary archives. However, there is a lack of understanding of how terrestrial organic matter is transported out of orogens and into sedimentary archives. Plant wax lipid biomarkers derived from terrestrial and marine sedimentary records are commonly used as paleo- hydrologic proxy to help elucidate these problems. I address the issue of how to interpret the biomarker record by using the plant wax isotopic composition of modern suspended and riverbank organic matter to identify and quantify organic matter source regions in the Arun Valley. Topographic and geomorphic analysis, provided by the 10Be catchment-mean denudation rates, reveals that a combination of topographic steepness (as a proxy for denudation) and vegetation density is required to capture organic matter sourcing in the Arun River.
My studies highlight the importance of a rigorous and careful interpretation of denudation rates in tectonically active orogens that are furthermore characterized by strong climatic and biotic gradients. Unambiguous information about these issues is critical for correctly decoding and interpreting the possible tectonic and climatic forces that drive erosion and denudation, and the manifestation of the erosion products in sedimentary archives.
It is the intention of this study to contribute to further rethinking and innovating in the Microcredit business which stands at a turning point – after around 40 years of practice it is endangered to fail as a tool for economic development and to become a doubtful finance product with a random scope instead. So far, a positive impact of Microfinance on the improvement of the lives of the poor could not be confirmed. Over-indebtment of borrowers due to the pre-dominance of consumption Microcredits has become a widespread problem. Furthermore, a rising number of abusive and commercially excessive practices have been reported.
In fact, the Microfinance sector appears to suffer from a major underlying deficit: there does not exist a coherent and transparent understanding of its meaning and objectives so that Microfinance providers worldwide follow their own approaches of Microfinance which tend to differ considerably from each other.
In this sense the study aims at consolidating the multi-faced and very often confusingly different Microcredit profiles that exist nowadays. Subsequently, in this study, the Microfinance spectrum will be narrowed to one clear-cut objective, in fact away from the mere monetary business transactions to poor people it has gradually been reduced to back towards a tool for economic development as originally envisaged by its pioneers.
Hence, the fundamental research question of this study is whether, and under which conditions, Microfinance may attain a positive economic impact leading to an improvement of the living of the poor.
The study is structured in five parts: the three main parts (II.-IV.) are surrounded by an introduction (I.) and conclusion (V.). In part II., the Microfinance sector is analysed critically aiming to identify the challenges persisting as well as their root causes. In the third part, a change to the macroeconomic perspective is undertaken in oder to learn about the potential and requirements of small-scale finance to enhance economic development, particularly within the economic context of less developed countries. By consolidating the insights gained in part IV., the elements of a new concept of Microfinance with the objecitve to achieve economic development of its borrowers are elaborated.
Microfinance is a rather sensitive business the great fundamental idea of which is easily corruptible and, additionally, the recipients of which are predestined victims of abuse due to their limited knowledge in finance. It therefore needs to be practiced responsibly, but also according to clear cut definitions of its meaning and objectives all institutions active in the sector should be devoted to comply with. This is especially relevant as the demand for Microfinance services is expected to rise further within the years coming. For example, the recent refugee migration movement towards Europe entails a vast potential for Microfinance to enable these people to make a new start into economic life. This goes to show that Microfinance may no longer mainly be associated with a less developed economic context, but that it will gain importance as a financial instrument in the developed economies, too.
Die empirische Studie hat die Verwissenschaftlichung der Physiotherapie und deren Relevanz für die berufliche Praxis in Deutschland zum Gegenstand. Unter Verwissenschaftlichung werden Prozesse der wissenschaftlichen Disziplinbildung und Akademisierung verstanden. Die Praxisrelevanz drückt sich in Veränderungsbestrebungen der Physiotherapie vom Beruf hin zur Profession aus.
Ausgehend von wissenschaftstheoretischen Ansätzen zur Disziplinbildung, Akademisierung und Professionalisierung sowie dem diesbezüglichen physiotherapeutischen Forschungsstand wendet sich die Arbeit aus den Perspektiven historischer und gegenwärtiger wissenschaftlicher Formierungsprozesse der empirischen Analyse des beschriebenen Gegenstandes zu.
Die zentralen Fragestellungen der vorliegenden Arbeit sind:
Auf welcher theoretischen Basis werden welche der Physiotherapie impliziten Gegenstände im Kontext welchen Theorie-Praxis-Verständnisses konstituiert?
Und: Gibt es ein theoretisches Fundament in Form von Theorien und Modellen, aus welchem sich forschungsmethodologische und wissenschaftstheoretische Zugänge begründen lassen und inwieweit zeigt sich hier das Potential zur Heranbildung einer wissenschaftlichen Disziplin?
Wie bezieht sich die Wissenschaft dabei auf eine professionelle Praxis und umgekehrt?
Der empirische Zugang zum Gegenstand erfolgte auf zwei Wegen:
1. Fachzeitschriftenanalyse zur Erfassung der Historizität,
2. Experteninterviews zur Erfassung der Kontextualität der Verwissenschaftlichung.
Die vorliegende Arbeit versteht sich als Beitrag zum wissenschaftlichen Diskurs in der Physiotherapie. Sie verfolgt das Ziel, eine empirisch belastbare Aussage bezüglich des Gelingens einer Disziplinbildung sowie des Akademisierungsprozesses in Deutschland zu treffen und diese in Beziehung zum Praxisfeld zu setzen. Empirisch relevant ist hierfür die Analyse der Historie. Letztere wiederum definiert den Weg zu einer ebenfalls zu analysierenden gegenwärtigen gesellschaftlichen Verortung. Die vorliegenden Analysen rekonstruieren die Emanzipation der Physiotherapie in Deutschland von einem Heilhilfsberuf hin zu einer eigenständigen Profession mit dem Fokus auf Prozesse der Disziplinbildung und Akademisierung.
Die Ergebnisse der Arbeit sind vielfältig und zeigen, dass die deutsche Physiotherapie sich unter anderem durch die Akademisierung auf dem Weg zu einer Wissenschaft sowie einer Profession befindet. Allerdings führt die Parallelität von Theoriebildung und Praxishandeln im Sinne einer kaum nachweisbaren Verschränkung beider Handlungsebenen zu dem Schluss, dass die untersuchten Prozesse bislang nicht zwangsläufig zu wissenschaftlich emanzipatorischem Erfolg führen müssen.
Flood generation at the scale of large river basins is triggered by the interaction of the hydrological pre-conditions and the meteorological event conditions at different spatial and temporal scales. This interaction controls diverse flood generating processes and results in floods varying in magnitude and extent, duration as well as socio-economic consequences. For a process-based understanding of the underlying cause-effect relationships, systematic approaches are required. These approaches have to cover the complete causal flood chain, including the flood triggering meteorological event in combination with the hydrological (pre-)conditions in the catchment, runoff generation, flood routing, possible floodplain inundation and finally flood losses.
In this thesis, a comprehensive probabilistic process-based understanding of the causes and effects of floods is advanced. The spatial and temporal dynamics of flood events as well as the geophysical processes involved in the causal flood chain are revealed and the systematic interconnections within the flood chain are deciphered by means of the classification of their associated causes and effects. This is achieved by investigating the role of the hydrological pre-conditions and the meteorological event conditions with respect to flood occurrence, flood processes and flood characteristics as well as their interconnections at the river basin scale.
Broadening the knowledge about flood triggers, which up to now has been limited to linking large-scale meteorological conditions to flood occurrence, the influence of large-scale pre-event hydrological conditions on flood initiation is investigated. Using the Elbe River basin as an example, a classification of soil moisture, a key variable of pre-event conditions, is developed and a probabilistic link between patterns of soil moisture and flood occurrence is established. The soil moisture classification is applied to continuously simulated soil moisture data which is generated using the semi-distributed conceptual rainfall-runoff model SWIM. Applying successively a principal component analysis and a cluster analysis, days of similar soil moisture patterns are identified in the period November 1951 to October 2003.
The investigation of flood triggers is complemented by including meteorological conditions described by a common weather pattern classification that represents the main modes of atmospheric state variability. The newly developed soil moisture classification thereby provides the basis to study the combined impact of hydrological pre-conditions and large-scale meteorological event conditions on flood occurrence at the river basin scale.
A process-based understanding of flood generation and its associated probabilities is attained by classifying observed flood events into process-based flood types such as snowmelt floods or long-rain floods. Subsequently, the flood types are linked to the soil moisture and weather patterns. Further understanding of the processes is gained by modeling of the complete causal flood chain, incorporating a rainfall-runoff model, a 1D/2D hydrodynamic model and a flood loss model. A reshuffling approach based on weather patterns and the month of their occurrence is developed to generate synthetic data fields of meteorological conditions, which drive the model chain, in order to increase the flood sample size. From the large number of simulated flood events, the impact of hydro-meteorological conditions on various flood characteristics is detected through the analysis of conditional cumulative distribution functions and regression trees.
The results show the existence of catchment-scale soil moisture patterns, which comprise of large-scale seasonal wetting and drying components as well as of smaller-scale variations related to spatially heterogeneous catchment processes. Soil moisture patterns frequently occurring before the onset of floods are identified. In winter, floods are initiated by catchment-wide high soil moisture, whereas in summer the flood-initiating soil moisture patterns are diverse and the soil moisture conditions are less stable in time. The combined study of both soil moisture and weather patterns shows that the flood favoring hydro-meteorological patterns as well as their interactions vary seasonally. In the analysis period, 18 % of the weather patterns only result in a flood in the case of preceding soil saturation. The classification of 82 past events into flood types reveals seasonally varying flood processes that can be linked to hydro-meteorological patterns. For instance, the highest flood potential for long-rain floods is associated with a weather pattern that is often detected in the presence of so-called ‘Vb’ cyclones. Rain-on-snow and snowmelt floods are associated with westerly and north-westerly wind directions. The flood characteristics vary among the flood types and can be reproduced by the applied model chain. In total, 5970 events are simulated. They reproduce the observed event characteristics between September 1957 and August 2002 and provide information on flood losses. A regression tree analysis relates the flood processes of the simulated events to the hydro-meteorological (pre-)event conditions and highlights the fact that flood magnitude is primarily controlled by the meteorological event, whereas flood extent is primarily controlled by the soil moisture conditions.
Describing flood occurrence, processes and characteristics as a function of hydro-meteorological patterns, this thesis is part of a paradigm shift towards a process-based understanding of floods. The results highlight that soil moisture patterns as well as weather patterns are not only beneficial to a probabilistic conception of flood initiation but also provide information on the involved flood processes and the resulting flood characteristics.
Foam fractionation of surfactant and protein solutions is a process dedicated to separate surface active molecules from each other due to their differences in surface activities. The process is based on forming bubbles in a certain mixed solution followed by detachment and rising of bubbles through a certain volume of this solution, and consequently on the formation of a foam layer on top of the solution column. Therefore, systematic analysis of this whole process comprises of at first investigations dedicated to the formation and growth of single bubbles in solutions, which is equivalent to the main principles of the well-known bubble pressure tensiometry. The second stage of the fractionation process includes the detachment of a single bubble from a pore or capillary tip and its rising in a respective aqueous solution. The third and final stage of the process is the formation and stabilization of the foam created by these bubbles, which contains the adsorption layers formed at the growing bubble surface, carried up and gets modified during the bubble rising and finally ends up as part of the foam layer.
Bubble pressure tensiometry and bubble profile analysis tensiometry experiments were performed with protein solutions at different bulk concentrations, solution pH and ionic strength in order to describe the process of accumulation of protein and surfactant molecules at the bubble surface. The results obtained from the two complementary methods allow understanding the mechanism of adsorption, which is mainly governed by the diffusional transport of the adsorbing protein molecules to the bubble surface. This mechanism is the same as generally discussed for surfactant molecules. However, interesting peculiarities have been observed for protein adsorption kinetics at sufficiently short adsorption times. First of all, at short adsorption times the surface tension remains constant for a while before it decreases as expected due to the adsorption of proteins at the surface. This time interval is called induction time and it becomes shorter with increasing protein bulk concentration. Moreover, under special conditions, the surface tension does not stay constant but even increases over a certain period of time. This so-called negative surface pressure was observed for BCS and BLG and discussed for the first time in terms of changes in the surface conformation of the adsorbing protein molecules. Usually, a negative surface pressure would correspond to a negative adsorption, which is of course impossible for the studied protein solutions. The phenomenon, which amounts to some mN/m, was rather explained by simultaneous changes in the molar area required by the adsorbed proteins and the non-ideality of entropy of the interfacial layer. It is a transient phenomenon and exists only under dynamic conditions.
The experiments dedicated to the local velocity of rising air bubbles in solutions were performed in a broad range of BLG concentration, pH and ionic strength. Additionally, rising bubble experiments were done for surfactant solutions in order to validate the functionality of the instrument. It turns out that the velocity of a rising bubble is much more sensitive to adsorbing molecules than classical dynamic surface tension measurements. At very low BLG or surfactant concentrations, for example, the measured local velocity profile of an air bubble is changing dramatically in time scales of seconds while dynamic surface tensions still do not show any measurable changes at this time scale. The solution’s pH and ionic strength are important parameters that govern the measured rising velocity for protein solutions. A general theoretical description of rising bubbles in surfactant and protein solutions is not available at present due to the complex situation of the adsorption process at a bubble surface in a liquid flow field with simultaneous Marangoni effects. However, instead of modelling the complete velocity profile, new theoretical work has been started to evaluate the maximum values in the profile as characteristic parameter for dynamic adsorption layers at the bubble surface more quantitatively.
The studies with protein-surfactant mixtures demonstrate in an impressive way that the complexes formed by the two compounds change the surface activity as compared to the original native protein molecules and therefore lead to a completely different retardation behavior of rising bubbles. Changes in the velocity profile can be interpreted qualitatively in terms of increased or decreased surface activity of the formed protein-surfactant complexes. It was also observed that the pH and ionic strength of a protein solution have strong effects on the surface activity of the protein molecules, which however, could be different on the rising bubble velocity and the equilibrium adsorption isotherms. These differences are not fully understood yet but give rise to discussions about the structure of protein adsorption layer under dynamic conditions or in the equilibrium state.
The third main stage of the discussed process of fractionation is the formation and characterization of protein foams from BLG solutions at different pH and ionic strength. Of course a minimum BLG concentration is required to form foams. This minimum protein concentration is a function again of solution pH and ionic strength, i.e. of the surface activity of the protein molecules. Although at the isoelectric point, at about pH 5 for BLG, the hydrophobicity and hence the surface activity should be the highest, the concentration and ionic strength effects on the rising velocity profile as well as on the foamability and foam stability do not show a maximum. This is another remarkable argument for the fact that the interfacial structure and behavior of BLG layers under dynamic conditions and at equilibrium are rather different. These differences are probably caused by the time required for BLG molecules to adapt respective conformations once they are adsorbed at the surface.
All bubble studies described in this work refer to stages of the foam fractionation process. Experiments with different systems, mainly surfactant and protein solutions, were performed in order to form foams and finally recover a solution representing the foamed material. As foam consists to a large extent of foam lamella – two adsorption layers with a liquid core – the concentration in a foamate taken from foaming experiments should be enriched in the stabilizing molecules. For determining the concentration of the foamate, again the very sensitive bubble rising velocity profile method was applied, which works for any type of surface active materials. This also includes technical surfactants or protein isolates for which an accurate composition is unknown.
In this thesis, the two prototype catalysts Fe(CO)₅ and Cr(CO)₆ are investigated with time-resolved photoelectron spectroscopy at a high harmonic setup. In both of these metal carbonyls, a UV photon can induce the dissociation of one or more ligands of the complex. The mechanism of the dissociation has been debated over the last decades. The electronic dynamics of the first dissociation occur on the femtosecond timescale.
For the experiment, an existing high harmonic setup was moved to a new location, was extended, and characterized. The modified setup can induce dynamics in gas phase samples with photon energies of 1.55eV, 3.10eV, and 4.65eV. The valence electronic structure of the samples can be probed with photon energies between 20eV and 40eV. The temporal resolution is 111fs to 262fs, depending on the combination of the two photon energies.
The electronically excited intermediates of the two complexes, as well as of the reaction product Fe(CO)₄, could be observed with photoelectron spectroscopy in the gas phase for the first time. However, photoelectron spectroscopy gives access only to the final ionic states. Corresponding calculations to simulate these spectra are still in development. The peak energies and their evolution in time with respect to the initiation pump pulse have been determined, these peaks have been assigned based on literature data. The spectra of the two complexes show clear differences. The dynamics have been interpreted with the assumption that the motion of peaks in the spectra relates to the movement of the wave packet in the multidimensional energy landscape. The results largely confirm existing models for the reaction pathways. In both metal carbonyls, this pathway involves a direct excitation of the wave packet to a metal-to-ligand charge transfer state and the subsequent crossing to a dissociative ligand field state. The coupling of the electronic dynamics to the nuclear dynamics could explain the slower dissociation in Fe(CO)₅ as compared to Cr(CO)₆.
This dissertation uses a common grammatical phenomenon, light verb constructions (LVCs) in English and German, to investigate how syntax-semantics mapping defaults influence the relationships between language processing, representation and conceptualization. LVCs are analyzed as a phenomenon of mismatch in the argument structure. The processing implication of this mismatch are experimentally investigated, using ERPs and a dual task. Data from these experiments point to an increase in working memory. Representational questions are investigated using structural priming. Data from this study suggest that while the syntax of LVCs is not different from other structures’, the semantics and mapping are represented differently. This hypothesis is tested with a new categorization paradigm, which reveals that the conceptual structure that LVC evoke differ in interesting, and predictable, ways from non-mismatching structures’.
The cell interior is a highly packed environment in which biological macromolecules evolve and function. This crowded media has effects in many biological processes such as protein-protein binding, gene regulation, and protein folding. Thus, biochemical reactions that take place in such crowded conditions differ from diluted test tube conditions, and a considerable effort has been invested in order to understand such differences.
In this work, we combine different computationally tools to disentangle the effects of molecular crowding on biochemical processes. First, we propose a lattice model to study the implications of molecular crowding on enzymatic reactions. We provide a detailed picture of how crowding affects binding and unbinding events and how the separate effects of crowding on binding equilibrium act together. Then, we implement a lattice model to study the effects of molecular crowding on facilitated diffusion. We find that obstacles on the DNA impair facilitated diffusion. However, the extent of this effect depends on how dynamic obstacles are on the DNA. For the scenario in which crowders are only present in the bulk solution, we find that at some conditions presence of crowding agents can enhance specific-DNA binding. Finally, we make use of structure-based techniques to look at the impact of the presence of crowders on the folding a protein. We find that polymeric crowders have stronger effects on protein stability than spherical crowders. The strength of this effect increases as the polymeric crowders become longer. The methods we propose here are general and can also be applied to more complicated systems.