Maximal muscular vascular conductances during whole body upright exercise in humans

[EN] That muscular blood flow may reach 2.5 l kg(-1) min(-1) in the quadriceps muscle has led to the suggestion that muscular vascular conductance must be restrained during whole body exercise to avoid hypotension. The main aim of this study was to determine the maximal arm and leg muscle vascular conductances (VC) during leg and arm exercise, to find out if the maximal muscular vasodilatory response is restrained during maximal combined arm and leg exercise. Six Swedish elite cross-country skiers, age (mean +/-s.e.m.) 24 +/- 2 years, height 180 +/- 2 cm, weight 74 +/- 2 kg, and maximal oxygen uptake (VO(2,max)) 5.1 +/- 0.1 l min(-1) participated in the study. Femoral and subclavian vein blood flows, intra-arterial blood pressure, cardiac output, as well as blood gases in the femoral and subclavian vein, right atrium and femoral artery were determined during skiing (roller skis) at approximately 76% of VO(2,max) and at VO(2,max) with different techniques: diagonal stride (combined arm and leg exercise), double poling (predominantly arm exercise) and leg skiing (predominantly leg exercise). During submaximal exercise cardiac output (26-27 l min(-1)), mean blood pressure (MAP) (approximately 87 mmHg), systemic VC, systemic oxygen delivery and pulmonary VO2(approximately 4 l min(-1)) attained similar values regardless of exercise mode. The distribution of cardiac output was modified depending on the musculature engaged in the exercise. There was a close relationship between VC and VO2 in arms (r= 0.99, P < 0.001) and legs (r= 0.98, P < 0.05). Peak arm VC (63.7 +/- 5.6 ml min(-1) mmHg(-1)) was attained during double poling, while peak leg VC was reached at maximal exercise with the diagonal technique (109.8 +/- 11.5 ml min(-1) mmHg(-1)) when arm VC was 38.8 +/- 5.7 ml min(-1) mmHg(-1). If during maximal exercise arms and legs had been vasodilated to the observed maximal levels then mean arterial pressure would have dropped at least to 75-77 mmHg in our experimental conditions. It is concluded that skeletal muscle vascular conductance is restrained during whole body exercise in the upright position to avoid hypotension.

Astaxanthin determination in marine biological samples : an overview

Máster en Oceanografía

Light energy management in peach: utilization, photoprotection , photodamage and recovery. Maximizing light absorption in orchard is not always the best solution

The relation between the intercepted light and orchard productivity was considered linear, although this dependence seems to be more subordinate to planting system rather than light intensity. At whole plant level not always the increase of irradiance determines productivity improvement. One of the reasons can be the plant intrinsic un-efficiency in using energy. Generally in full light only the 5 – 10% of the total incoming energy is allocated to net photosynthesis. Therefore preserving or improving this efficiency becomes pivotal for scientist and fruit growers. Even tough a conspicuous energy amount is reflected or transmitted, plants can not avoid to absorb photons in excess. The chlorophyll over-excitation promotes the reactive species production increasing the photoinhibition risks. The dangerous consequences of photoinhibition forced plants to evolve a complex and multilevel machine able to dissipate the energy excess quenching heat (Non Photochemical Quenching), moving electrons (water-water cycle , cyclic transport around PSI, glutathione-ascorbate cycle and photorespiration) and scavenging the generated reactive species. The price plants must pay for this equipment is the use of CO2 and reducing power with a consequent decrease of the photosynthetic efficiency, both because some photons are not used for carboxylation and an effective CO2 and reducing power loss occurs. Net photosynthesis increases with light until the saturation point, additional PPFD doesn’t improve carboxylation but it rises the efficiency of the alternative pathways in energy dissipation but also ROS production and photoinhibition risks. The wide photo-protective apparatus, although is not able to cope with the excessive incoming energy, therefore photodamage occurs. Each event increasing the photon pressure and/or decreasing the efficiency of the described photo-protective mechanisms (i.e. thermal stress, water and nutritional deficiency) can emphasize the photoinhibition. Likely in nature a small amount of not damaged photosystems is found because of the effective, efficient and energy consuming recovery system. Since the damaged PSII is quickly repaired with energy expense, it would be interesting to investigate how much PSII recovery costs to plant productivity. This PhD. dissertation purposes to improve the knowledge about the several strategies accomplished for managing the incoming energy and the light excess implication on photo-damage in peach. The thesis is organized in three scientific units. In the first section a new rapid, non-intrusive, whole tissue and universal technique for functional PSII determination was implemented and validated on different kinds of plants as C3 and C4 species, woody and herbaceous plants, wild type and Chlorophyll b-less mutant and monocot and dicot plants. In the second unit, using a “singular” experimental orchard named “Asymmetric orchard”, the relation between light environment and photosynthetic performance, water use and photoinhibition was investigated in peach at whole plant level, furthermore the effect of photon pressure variation on energy management was considered on single leaf. In the third section the quenching analysis method suggested by Kornyeyev and Hendrickson (2007) was validate on peach. Afterwards it was applied in the field where the influence of moderate light and water reduction on peach photosynthetic performances, water requirements, energy management and photoinhibition was studied. Using solar energy as fuel for life plant is intrinsically suicidal since the high constant photodamage risk. This dissertation would try to highlight the complex relation existing between plant, in particular peach, and light analysing the principal strategies plants developed to manage the incoming light for deriving the maximal benefits as possible minimizing the risks. In the first instance the new method proposed for functional PSII determination based on P700 redox kinetics seems to be a valid, non intrusive, universal and field-applicable technique, even because it is able to measure in deep the whole leaf tissue rather than the first leaf layers as fluorescence. Fluorescence Fv/Fm parameter gives a good estimate of functional PSII but only when data obtained by ad-axial and ab-axial leaf surface are averaged. In addition to this method the energy quenching analysis proposed by Kornyeyev and Hendrickson (2007), combined with the photosynthesis model proposed by von Caemmerer (2000) is a forceful tool to analyse and study, even in the field, the relation between plant and environmental factors such as water, temperature but first of all light. “Asymmetric” training system is a good way to study light energy, photosynthetic performance and water use relations in the field. At whole plant level net carboxylation increases with PPFD reaching a saturating point. Light excess rather than improve photosynthesis may emphasize water and thermal stress leading to stomatal limitation. Furthermore too much light does not promote net carboxylation improvement but PSII damage, in fact in the most light exposed plants about 50-60% of the total PSII is inactivated. At single leaf level, net carboxylation increases till saturation point (1000 – 1200 μmolm-2s-1) and light excess is dissipated by non photochemical quenching and non net carboxylative transports. The latter follows a quite similar pattern of Pn/PPFD curve reaching the saturation point at almost the same photon flux density. At middle-low irradiance NPQ seems to be lumen pH limited because the incoming photon pressure is not enough to generate the optimum lumen pH for violaxanthin de-epoxidase (VDE) full activation. Peach leaves try to cope with the light excess increasing the non net carboxylative transports. While PPFD rises the xanthophyll cycle is more and more activated and the rate of non net carboxylative transports is reduced. Some of these alternative transports, such as the water-water cycle, the cyclic transport around the PSI and the glutathione-ascorbate cycle are able to generate additional H+ in lumen in order to support the VDE activation when light can be limiting. Moreover the alternative transports seems to be involved as an important dissipative way when high temperature and sub-optimal conductance emphasize the photoinhibition risks. In peach, a moderate water and light reduction does not determine net carboxylation decrease but, diminishing the incoming light and the environmental evapo-transpiration request, stomatal conductance decreases, improving water use efficiency. Therefore lowering light intensity till not limiting levels, water could be saved not compromising net photosynthesis. The quenching analysis is able to partition absorbed energy in the several utilization, photoprotection and photo-oxidation pathways. When recovery is permitted only few PSII remained un-repaired, although more net PSII damage is recorded in plants placed in full light. Even in this experiment, in over saturating light the main dissipation pathway is the non photochemical quenching; at middle-low irradiance it seems to be pH limited and other transports, such as photorespiration and alternative transports, are used to support photoprotection and to contribute for creating the optimal trans-thylakoidal ΔpH for violaxanthin de-epoxidase. These alternative pathways become the main quenching mechanisms at very low light environment. Another aspect pointed out by this study is the role of NPQ as dissipative pathway when conductance becomes severely limiting. The evidence that in nature a small amount of damaged PSII is seen indicates the presence of an effective and efficient recovery mechanism that masks the real photodamage occurring during the day. At single leaf level, when repair is not allowed leaves in full light are two fold more photoinhibited than the shaded ones. Therefore light in excess of the photosynthetic optima does not promote net carboxylation but increases water loss and PSII damage. The more is photoinhibition the more must be the photosystems to be repaired and consequently the energy and dry matter to allocate in this essential activity. Since above the saturation point net photosynthesis is constant while photoinhibition increases it would be interesting to investigate how photodamage costs in terms of tree productivity. An other aspect of pivotal importance to be further widened is the combined influence of light and other environmental parameters, like water status, temperature and nutrition on peach light, water and phtosyntate management.

Changes in plant metabolism induced by dioxygenase inhibitors and their effect on the epiphytic microbial community and fire blight (Erwinia amylovora) control

Fire blight, caused by the gram negative bacterium Erwinia amylovora, is one of the most destructive bacterial diseases of Pomaceous plants. Therefore, the development of reliable methods to control this disease is desperately needed. This research investigated the possibility to interfere, by altering plant metabolism, on the interactions occurring between Erwinia amylovora, the host plant and the epiphytic microbial community in order to obtain a more effective control of fire blight. Prohexadione-calcium and trinexapac-ethyl, two dioxygenase inhibitors, were chosen as a chemical tool to influence plant metabolism. These compounds inhibit the 2-oxoglutarate-dependent dioxygenases and, therefore, they greatly influence plant metabolism. Moreover, dioxygenase inhibitors were found to enhance plant resistance to a wide range of pathogens. In particular, dioxygenase inhibitors application seems a promising method to control fire blight. From cited literature, it is assumed that these compounds increase plant defence mainly by a transient alteration of flavonoids metabolism. We tried to demonstrate, that the reduction of susceptibility to disease could be partially due to an indirect influence on the microbial community established on plant surface. The possibility to influence the interactions occurring in the epiphytic microbial community is particularly interesting, in fact, the relationships among different bacterial populations on plant surface is a key factor for a more effective biological control of plant diseases. Furthermore, we evaluated the possibility to combine the application of dioxygenase inhibitors with biological control in order to develop an integrate strategy for control of fire blight. The first step for this study was the isolation of a pathogenic strain of E. amylovora. In addition, we isolated different epiphytic bacteria, which respond to general requirements for biological control agents. Successively, the effect of dioxygenase inhibitors treatment on microbial community was investigated on different plant organs (stigmas, nectaries and leaves). An increase in epiphytic microbial population was found. Further experiments were performed with aim to explain this effect. In particular, changes in sugar content of nectar were observed. These changes, decreasing the osmotic potential of nectar, might allow a more consistent growth of epiphytic bacteria on blossoms. On leaves were found similar differences as well. As far as the interactions between E. amylovora and host plant, they were deeply investigated by advanced microscopical analysis. The influence of dioxygenase inhibitors and SAR inducers application on the infection process and migration of pathogen inside different plant tissues was studied. These microscopical techniques, combined with the use of gpf-labelled E. amylovora, allowed the development of a bioassay method for resistance inducers efficacy screening. The final part of the work demonstrated that the reduction of disease susceptibility observed in plants treated with prohexadione-calcium is mainly due to the accumulation of a novel phytoalexins: luteoforol. This 3-deoxyflavonoid was proven to have a strong antimicrobial activity.

Oxylipins biosynthesis in Lactobacillus helveticus in the presence of oxidative stress

This PhD thesis is aimed at studying the possible pathways and the mechanisms that can trigger oxylipins biosynthesis, and particularly that of short chain aldehydes and alcohols, in Lactobacillus helveticus, also in the presence of oxidative stress, using a totally labelled linoleic acid as precursor. In plants and fungi these molecules, involved in defence mechanisms against pathogens and in communication systems, derive from the oxidation of cellular unsaturated fatty acids (UFAs) and their accumulation is associated with stress exposure. Since some oxylipins are produced also by lactobacilli, it is possible to hypothesize that a metabolic pathway from UFAs to oxylipins, similar to what happens in plants and fungi, is present also in lactic acid bacteria. The results obtained pointed out that some volatile molecules are the result of UFAs catabolism, since they appear only when cells are incubated in their presence. Labelled linoleic acid is integrated in the membrane and subsequently transformed into aldehydes and alcohols, whose extent and carbon atoms number depend on stress exposure. The enzymes responsible for this metabolic pathway in plants and fungi (e.g. lipoxygenase, dioxygenase) seem to be absent in Lactobacillus helveticus and in other lactobacilli. Proteomic analyses show the over expression of many proteins, including thioredoxin reductase (part of the bacterial oxidative defence system), mainly in cells grown with linoleic acid without oxidative stress exposure, confirming that linoleic acid itself induces oxidative stress. 6 general oxidoreductases (class including dioxygenases and peroxidase) were found and therefore a deeper investigation on them could be productive in elucidating all steps involved in oxylipins biosynthesis in bacteria. Due to the multiple role of oxylipins (flavouring agents, antimicrobial compounds and interspecific signalling molecules) the identification of genes involved and regulating factors should have an important biotechnological impact, also allowing the overproduction of selected bioactive molecules.

NMR spectroscopy and imaging of hyperpolarized gases

Since the discovery of the nuclear magnetic resonance (NMR) phenomenon, countless NMR techniques have been developed that are today indispensable tools in physics, chemistry, biology, and medicine. As one of the main obstacles in NMR is its notorious lack of sensitivity, different hyperpolarization (HP) methods have been established to increase signals up to several orders of magnitude. In this work, different aspects of magnetic resonance, using HP noble gases, are studied, hereby combining different disciplines of research. The first part examines new fundamental effects in NMR of HP gases, in theory and experiment. The spin echo phenomenon, which provides the basis of numerous modern experiments, is studied in detail in the gas phase. The changes of the echo signal in terms of amplitude, shape, and position, due to the fast translational motion, are described by an extension of the existing theory and computer simulations. With this knowledge as a prerequisite, the detection of intermolecular double-quantum coherences was accomplished for the first time in the gas phase. The second part of this thesis focuses on the development of a practical method to enhance the dissolution process of HP 129Xe, without loss of polarization or shortening of T1. Two different setups for application in NMR spectroscopy and magnetic resonance imaging (MRI) are presented. The continuous operation allows biological and multidimensional spectroscopy in solutions. Also, first in vitro MRI images with dissolved HP 129Xe as contrast agent were obtained at a clinical scanner.

The Domon Family of Plant Plasma Membrane B-Type Cytochromes: Heterologous Expression, Biochemical Characterization and Physiological Roles in Vivo

The DOMON domain is a domain widespread in nature, predicted to fold in a β-sandwich structure. In plants, AIR12 is constituted by a single DOMON domain located in the apoplastic space and is GPI-modified for anchoring to the plasma membrane. Arabidopsis thaliana AIR12 has been heterologously expressed as a recombinant protein (recAtAIR12) in Pichia pastoris. Spectrophotometrical analysis of the purified protein showed that recAtAir12 is a cytochrome b. RecAtAIR12 is highly glycosylated, it is reduced by ascorbate, superoxide and naftoquinones, oxidised by monodehydroascorbate and oxygen and insensitive to hydrogen peroxide. The addition of recAtAIR12 to permeabilized plasma membranes containing NADH, FeEDTA and menadione, caused a statistically significant increase in hydroxyl radicals as detected by electron paramagnetic resonance. In these conditions, recAtAIR12 has thus a pro-oxidant role. Interestingly, AIR12 is related to the cytochrome domain of cellobiose dehydrogenase which is involved in lignin degradation, possibly via reactive oxygen species (ROS) production. In Arabidopsis the Air12 promoter is specifically activated at sites where cell separations occur and ROS, including •OH, are involved in cell wall modifications. air12 knock-out plants infected with Botrytis cinerea are more resistant than wild-type and air12 complemented plants. Also during B. cinerea infection, cell wall modifications and ROS are involved. Our results thus suggest that AIR12 could be involved in cell wall modifying reactions by interacting with ROS and ascorbate. CyDOMs are plasma membrane redox proteins of plants that are predicted to contain an apoplastic DOMON fused with a transmembrane cytochrome b561 domain. CyDOMs have never been purified nor characterised. The trans-membrane portion of a soybean CyDOM was expressed in E. coli but purification could not be achieved. The DOMON domain was expressed in P. pastoris and shown to be itself a cytochrome b that could be reduced by ascorbate.

Probing strongly correlated states of ultracold atoms in optical lattices

This thesis describes experiments which investigate ultracold atom ensembles in an optical lattice. Such quantum gases are powerful models for solid state physics. Several novel methods are demonstrated that probe the special properties of strongly correlated states in lattice potentials. Of these, quantum noise spectroscopy reveals spatial correlations in such states, which are hidden when using the usual methods of probing atomic gases. Another spectroscopic technique makes it possible to demonstrate the existence of a shell structure of regions with constant densities. Such coexisting phases separated by sharp boundaries had been theoretically predicted for the Mott insulating state. The tunneling processes in the optical lattice in the strongly correlated regime are probed by preparing the ensemble in an optical superlattice potential. This allows the time-resolved observation of the tunneling dynamics, and makes it possible to directly identify correlated tunneling processes.

Study of the inter-annual variability of particle vertical fluxes in two moorings in the Ross Sea (Antarctica)

The most ocean - atmosphere exchanges take place in polar environments due to the low temperatures which favor the absorption processes of atmospheric gases, in particular CO2. For this reason, the alterations of biogeochemical cycles in these areas can have a strong impact on the global climate. With the aim of contributing to the definition of the mechanisms regulating the biogeochemical fluxes we have analyzed the particles collected in the Ross Sea in different years (ROSSMIZE, BIOSESO 1 and 2, ROAVERRS and ABIOCLEAR projects) in two sites (mooring A and B). So it has been developed a more efficient method to prepare sediment trap samples for the analyses. We have also processed satellite data of sea ice, chlorophyll a and diatoms concentration. At both sites, in each year considered, there was a high seasonal and inter-annual variability of biogeochemical fluxes closely correlated with sea ice cover and primary productivity. The comparison between the samples collected at mooring A and B in 2008 highlighted the main differences between these two sites. Particle fluxes at Mooring A, located in a polynia area, are higher than mooring B ones and they happen about a month before. In the mooring B area it has been possible to correlate the particles fluxes to the ice concentration anomalies and with the atmospheric changes in response to El Niño Southern Oscillations. In 1996 and 1999, years subjected to La Niña, the concentrations of sea ice in this area have been less than in 1998, year subjected to El Niño. Inverse correlation was found for 2005 and 2008. In the mooring A area significant differences in mass and biogenic fluxes during 2005 and 2008 has been recorded. This allowed to underline the high variability of lateral advection processes and to connect them to the physical forcing.

Photochemie der Troposphäre in niedrigen und mittleren Breiten: Die Rolle von Konvektion

Ozon (O3) ist in der Atmosphäre ein wichtiges Oxidanz und Treibhausgas. Während die höchsten Konzentrationen in der Stratosphäre beobachtet werden und die vor der gefährlichen UV-Strahlung schützende Ozonschicht bilden, können sich signifikante Änderungen der Ozon-Konzentration in der Region der Tropopause auf das Klima der Erde auswirken. Des Weiteren ist Ozon eine der Hauptquellen für das Hydroxylradikal (OH) und nimmt damit entscheidend Einfluss auf die Oxidationskraft der Atmosphäre. Der konvektive Transport von Ozon und seinen Vorläufergasen aus Regionen nahe der Erdoberfläche in die freie Troposphäre beeinflusst das Budget dieser Spezies in der Tropopausenregion.rnDie Datengrundlage der Studie in der vorliegenden Arbeit basiert auf den flugzeuggetragenen Messkampagnen GABRIEL 2005 (Suriname, Südamerika) sowie HOOVER I 2006 und HOOVER II 2007 (beide in Europa). Mit dem zur Verfügung stehenden Datensatz wird das Ozonbudget in der freien, unbelasteten Hintergrundatmosphäre und in der durch hochreichende Konvektion gestörten, oberen Troposphäre untersucht. Anhand der auf in-situ Messungen von O3, NO, OH, HO2 und dem aktinischen Strahlungsfluss basierten Berechnung der Netto-Ozonproduktionsrate (NOPR) werden für das Messgebiet Ozontendenzen in der unbelasteten Troposphäre abgeleitet und mit Simulationen des globalen Chemie-Transport-Modells MATCH-MPIC verglichen. Mit Hilfe zweier Fallstudien in den Tropen in Südamerika und den mittleren Breiten in Europa werden die Auswirkungen von hochreichender Konvektion auf die obere Troposphäre quantifiziert.rnDie Ergebnisse zeigen für die Grenzschicht in niedrigen und mittleren Breiten eine eindeutige Tendenz zur Produktion von Ozon, was für den tropischen Regenwald in der Messregion nicht der allgemeinen Erwartung entsprach, nach der diese Region durch die Zerstörung von Ozon charakterisiert sein sollte. In der oberen Troposphäre ab etwa 7 km wird für die beiden Regionen eine leichte Tendenz zur Ozonproduktion beobachtet. Signifikante Unterschiede zeigen die Ergebnisse für die mittlere Troposphäre. Während die Tropen in dieser Region durch eine eindeutige Tendenz zur Zerstörung von Ozon charakterisiert sind, lässt sich über den mittleren Breiten zwar eine hohe photochemische Aktivität aber keine derart klare Tendenz feststellen. Die hohen Breiten zeichnen sich durch eine neutrale Troposphäre in Bezug auf die Ozontendenz aus und weisen kaum photochemische Aktivität auf. Der Vergleich dieser Ergebnisse mit dem MATCH-MPIC Modell zeigt in weiten Teilen der Messregionen eine grundlegende Übereinstimmung in der Tendenz zur Produktion oder Zerstörung von Ozon. Die absoluten Werte werden vom Modell aber generell unterschätzt. Signifikante Unterschiede zwischen in-situ Daten und Modellsimulationen werden in der Grenzschicht über dem tropischen Regenwald identifiziert.rnDer Einfluss der Konvektion ist durch eine signifikant erhöhte NOPR gekennzeichnet. In dieser Arbeit wird in den Tropen mit einem Median-Wert von 0.20 ppbv h−1 eine um den Faktor 3.6 erhöhte NOPR im Vergleich zur ungestörten oberen Troposphäre abgeschätzt. In den mittleren Breiten führt die um eine Größenordnung höhere NO-Konzentration zu einem Wert von 1.89 ppbv h−1, was einer Überhöhung um einen Faktor 6.5 im Vergleich zum ungestörten Zustand entspricht. Diese Ergebnisse zeigen für beide Regionen in der oberen Troposphäre eine erhöhte Ozonproduktion als Folge konvektiver Aktivität. rnrnHochreichende Konvektion ist zudem ein sehr effektiver Mechanismus für den Vertikaltransport aus der Grenzschicht in die obere Troposphäre. Die schnelle Hebung in konvektiven Wolken führt bei Spurengasen mit Quellen an der Erdoberfläche zu einer Erhöhung ihrer Konzentration in der oberen Troposphäre. Die hochgradig löslichen Spurenstoffe Formaldehyd (HCHO) und Wasserstoffperoxid (H2O2) sind wichtige Vorläufergase der HOx-Radikale. Es wird angenommen, dass sie aufgrund ihrer Löslichkeit in Gewitterwolken effektiv ausgewaschen werden.rnIn der vorliegenden Arbeit wird eine Fallstudie von hochreichender Konvektion im Rahmen des HOOVER II Projekts im Sommer 2007 analysiert. Am 19.07.2007 entwickelten sich am Nachmittag am Südostrand eines in nordöstlicher Richtung ziehenden mesoskaligen konvektiven Systems drei zunächst isolierte konvektive Zellen. Flugzeuggetragene Messungen in der Aus- und der Einströmregion einer dieser Gewitterzellen stellen einen exzellenten Datensatz bereit, um die Auswirkungen von hochreichender Konvektion auf die Verteilung verschiedener Spurengase in der oberen Troposphäre zu untersuchen. Der Vergleich der Konzentrationen von Kohlenstoffmonoxid (CO) und Methan (CH4) zwischen der oberen Troposphäre und der Grenzschicht deutet auf einen nahezu unverdünnten Transport dieser langlebigen Spezies in der konvektiven Zelle hin. Die Verhältnisse betragen (0.94±0.04) für CO und (0.99±0.01) für CH4. Für die löslichen Spezies HCHO und H2O2 beträgt dieses Verhältnis in der Ausströmregion (0.55±0.09) bzw. (0.61±0.08). Dies ist ein Indiz dafür, dass diese Spezies nicht so effektiv ausgewaschen werden wie angenommen. Zum besseren Verständnis des Einflusses der Konvektion auf die Budgets dieser Spezies in der oberen Troposphäre wurden im Rahmen dieser Arbeit Boxmodell-Studien für den Beitrag der photochemischen Produktion in der Ausströmregion durchgeführt, wobei die gemessenen Spezies und Photolysefrequenzen als Randbedingungen dienten. Aus den Budgetbetrachtungen für HCHO und H2O2 wird eine Auswascheffizienz von (67±24) % für HCHO und (41±18) % für H2O2 abgeschätzt. Das für H2O2 überraschende Ergebnis lässt darauf schließen, dass dieses Molekül in einer Gewitterwolke deutlich effektiver transportiert werden kann, als aufgrund seiner hohen Löslichkeit aus der Henry-Konstanten zu erwarten wäre. Das Ausgasen von gelöstem H2O2 beim Gefrieren eines Wolkentropfens, d.h. ein Retentionskoeffizient kleiner 1, ist ein möglicher Mechanismus, der zum beobachteten Mischungsverhältnis dieser löslichen Spezies in der Ausströmregion beitragen kann.

Airborne in situ measurements of ice particles in the tropical tropopause layer

Ice clouds have a strong effect on the Earth-atmosphere radiative energy balance, on the distribution of condensable gases in the atmosphere, as well as on the chemical composition of the air. The ice particles in these clouds can take on a variety of shapes which makes the description of the cloud microphysical properties more difficult. In the tropical upper troposphere/lower stratosphere (UTLS), a region where ice cloud abundance is relatively high, different types of ice clouds can be observed. However, in situ measurements are rare due to the high altitude of these clouds and the few available research aircraft, only three worldwide, that can fly at such altitudes.rnThis work focuses on in situ measurements of the tropical UTLS clouds performedrnwith a Cloud Imaging Probe (CIP) and a Forward Scattering Spectrometer Probern(FSSP-100), whereof the CIP is the key instrument of this thesis. The CIP is anrnairborne in situ instrument that obtains two-dimensional shadow images of cloud particles. Several cloud microphysical parameters can be derived from these measurements, e.g. number concentrations and size distributions. In order to obtain a high quality data set, a careful image analysis and several corrections need to be applied to the CIP observations. These methods are described in detail.rnMeasurements within the tropical UTLS have been performed during two campaigns:rnSCOUT-O3, 2005 in Northern Australia and SCOUT-AMMA, 2006 inWest Africa. Thernobtained data set includes first observations of subvisible cirrus clouds over a continental area and observations of the anvils of deep convective clouds. The latter can be further divided into clouds in mesoscale convective system outflows of different ages and clouds in overshooting cloud turrets that even penetrated the stratosphere. The microphysical properties of these three cloud types are discussed in detail. Furthermore, the vertical structure of the ice clouds in the UTLS is investigated. The values of the microphysical parameters were found to decrease with increasing altitude in the upper troposphere. Particle numbers and maximum sizes were also decreasing with increasing age of the outflow clouds. Further differences between the deep convective clouds and subvisible cirrus were found in the particle morphology as well as in the ratio of the observed aerosol particles to cloud particles which indicates that the different freezing processes (deposition, contact, immersion freezing) play different roles in the formation of the respective clouds. For the achievementrnof a better microphysical characterisation and description numerical fits have been adjusted onto the cloud particle size distributions of the subvisible cirrus as well as on the size distributions of the clouds at different altitudes in the UTLS.

Räumliche und jahreszeitliche Verteilung von OH- und HO 2-Radikalen in der Troposphäre über Europa

Durch geologische Prozesse freigesetzte sowie biogen und anthropogen emittierte Gase werden hauptsächlich von der untersten Atmosphärenschicht, der Troposphäre, aufgenommen und abgebaut. Durch in die Troposphä¬re einfallende solare Strahlung wird ein Abbau des Großteils der emittierten Spurengase durch reaktive Radikale initiiert. Der wichtigste Vertreter dieser reaktiven Radikale in der Troposphäre ist das Hydroxylradikal (OH-Radikal), welches im schnellen Gleichgewicht mit Hydroperoxyradikalen (HO2-Radikal) vorliegt, sodass die Summe aus OH- und HO2-Radikalen oft als HOx zusammengefasst wird. HOx-Radikale bilden tagsüber den Hauptteil der Oxidationskapazität der Troposphäre und sind somit verantwortlich für den oxidativen Abbau vieler, auch chemisch und photolytisch stabiler, Spurengase. Daher wird die Oxidationskapazität als Selbstreinigungskraft der Troposphäre verstanden. rnIm Rahmen meiner Arbeit wurde die wissenschaftliche Fragestellung auf die Oxidationskapazität der Troposphäre über Europa fokussiert. Die Höhen- und Breitenverteilung der OH- und HO2-Mischungsverhältnisse und ihre jahreszeitliche Variation wurde während der flugzeuggestützten HOOVER-Kampagnen (HOOVER 1 & 2) charakterisiert, wobei ein Fokus auf der oberen Troposphäre lag. Es wird gezeigt, welchen Einfluss die einfallende Strahlung, die Variation von HOx-Vorläufersubstanzen (wie z. B. Ozon) und die Variation von Substanzen, die das HOx-Gleichgewicht beeinflussen (z. B. Stickstoffmonoxid), auf das HOx-Budget haben. rnEs wird beispielhaft für den Höhenbereich zwischen 8 und 9.5 km gezeigt, dass die Oxidationskapazität in der oberen Troposphäre des Sommers im Ver¬gleich zu der des Herbstes aufgrund von einer verstärkten HO2-Zyklierung im Mittel deutlich erhöht ist (500 %). rnDurch konvektiven Transport werden im Sommer im Gegensatz zum Herbst regelmäßig Luftmassen aus der planetaren Grenzschicht in die obere Troposphäre eingemischt. Daher wurden der konvektive Luftmassentransport und der Einfluss der eingemischten Spurengase auf die Oxidationskapazität der oberen Troposphäre anhand eines konvektiven Elements über Südostdeutschland untersucht. Wie in dieser Arbeit berichtet wird, wurden in den Luftmassen der Ausströmregion mit bis zu 3.5 pmol/mol (Maximum 10 s-Mittelwert) sehr hohe OH-Mischungsverhältnisse gefunden, die aus der HO2-Konversion mit NO gebildet wurden. Das modellierte HOx-Budget zeigt, dass die HOx-Chemie - unter den beobachteten Bedingungen in der Ausströmregion - durch HOx-Zyklierungsreaktionen beherrscht wird. rnDie gemessenen OH-Mischungsverhältnisse in der Ausströmregion liegen etwa um einen Faktor fünf höher, als die während dieses Fluges in der konvektiv unbeeinflussten oberen Troposphäre gemessenen OH-Mischungsverhältnisse. Am Beispiel der NO2- und CH4-Lebensdauer wird ein schnellerer Abbau von Spurengasen aufgrund der erhöhten Oxidationskapazität nachgewiesen. Aus der NO2-Lebensdauer wird abgeschätzt, wie lange die Oxidationskapazität aufgrund des konvektiven Transports von NOx in den Luftmassen des Ausströmgebietes erhöht ist.rnDie während den Kampagnen durchgeführten Messungen wurden genutzt, um Modellberechnungen des vertikalen HOx-Budgets (über Südschweden) und des meridionalen HOx-Budgets zwischen Nordeuropa und Korsika durchzuführen. Es wurde gezeigt, dass das Modell die OH- und HO2-Mischungsverhältnisse im Allgemeinen gut reproduziert (Modell/Messung: OH im Sommer 94 %, HO2 im Sommer 93 % im Herbst 95 %), wohingegen die vergleichsweise kleinen OH-Mischungsverhältnisse im Herbst aufgrund von einer überschätzten H2O2 abhängigen OH-Produktion stark überschätzt wurden (Modell/Messung: 147 %). rnZur Charakterisierung der Oxidationskapazität innerhalb der planetaren Grenzschicht wurden die DOMINO-Kampagnen durchgeführt. Dabei wurde die Zusammensetzung unterschiedlicher Luftmassen untersucht, die aus verschiedenen Herkunftsorten zum Messort transportiert wurden und aufgrund ihres Ursprungs kaum prozessierte bis prozessierte anthropogen emittierte Spurengase enthielten. Zusätzlich enthielt ein Teil der Luftmassen biogen emittierte Spurengase. Komplementäre Messungen ermöglichen die Berechnung der totalen OH-Produktion und den Vergleich mit den bekannten OH-Quellen. Der Vergleich zeigt, dass offenbar wichtige OH-Produktionskanäle durch die gemessenen Spurengase oder die durchgeführten Berechnungen nicht abgebildet werden. Es wird gezeigt, dass die Stärke der unbekannten OH-Quellen, vor allem unter niedrigen NO-Bedingungen, groß ist und mit den Isopren-, RO2- und HO2-Mischungsverhältnissen korreliert.rn

Interacting bosons and fermions in three-dimensional optical lattice potentials

This thesis reports on the realization, characterization and analysis of ultracold bosonic and fermionic atoms in three-dimensional optical lattice potentials. Ultracold quantum gases in optical lattices can be regarded as ideal model systems to investigate quantum many-body physics. In this work interacting ensembles of bosonic 87Rb and fermionic 40K atoms are employed to study equilibrium phases and nonequilibrium dynamics. The investigations are enabled by a versatile experimental setup, whose core feature is a blue-detuned optical lattice that is combined with Feshbach resonances and a red-detuned dipole trap to allow for independent control of tunneling, interactions and external confinement. The Fermi-Hubbard model, which plays a central role in the theoretical description of strongly correlated electrons, is experimentally realized by loading interacting fermionic spin mixtures into the optical lattice. Using phase-contrast imaging the in-situ size of the atomic density distribution is measured, which allows to extract the global compressibility of the many-body state as a function of interaction and external confinement. Thereby, metallic and insulating phases are clearly identified. At strongly repulsive interaction, a vanishing compressibility and suppression of doubly occupied lattice sites signal the emergence of a fermionic Mott insulator. In a second series of experiments interaction effects in bosonic lattice quantum gases are analyzed. Typically, interactions between microscopic particles are described as two-body interactions. As such they are also contained in the single-band Bose-Hubbard model. However, our measurements demonstrate the presence of multi-body interactions that effectively emerge via virtual transitions of atoms to higher lattice bands. These findings are enabled by the development of a novel atom optical measurement technique: In quantum phase revival spectroscopy periodic collapse and revival dynamics of the bosonic matter wave field are induced. The frequencies of the dynamics are directly related to the on-site interaction energies of atomic Fock states and can be read out with high precision. The third part of this work deals with mixtures of bosons and fermions in optical lattices, in which the interspecies interactions are accurately controlled by means of a Feshbach resonance. Studies of the equilibrium phases show that the bosonic superfluid to Mott insulator transition is shifted towards lower lattice depths when bosons and fermions interact attractively. This observation is further analyzed by applying quantum phase revival spectroscopy to few-body systems consisting of a single fermion and a coherent bosonic field on individual lattice sites. In addition to the direct measurement of Bose-Fermi interaction energies, Bose-Bose interactions are proven to be modified by the presence of a fermion. This renormalization of bosonic interaction energies can explain the shift of the Mott insulator transition. The experiments of this thesis lay important foundations for future studies of quantum magnetism with fermionic spin mixtures as well as for the realization of complex quantum phases with Bose-Fermi mixtures. They furthermore point towards physics that reaches beyond the single-band Hubbard model.

Sources and pathways of methane formed in oxidative environments

Methane is the most abundant reduced organic compound in the atmosphere. As the strongest known long-lived greenhouse gas after water vapour and carbon dioxide methane perturbs the radiation balance of Earth’s atmosphere. The abiotic formation of methane requires ultraviolet irradiation of organic matter or takes place in locations with high temperature and/or pressure, e.g. during biomass burning or serpentinisation of olivine, under hydrothermal conditions in the oceans deep or below tectonic plates. The biotic methane formation was traditionally thought to be formed only by methanogens under strictly anaerobic conditions, such as in wetland soils, rice paddies and agricultural waste. rnIn this dissertation several chemical pathways are described which lead to the formation of methane under aerobic and ambient conditions. Organic precursor compounds such as ascorbic acid and methionine were shown to release methane in a chemical system including ferrihydrite and hydrogen peroxide in aquatic solution. Moreover, it was shown by using stable carbon isotope labelling experiments that the thio-methyl group of methionine was the carbon precursor for the methane produced. Methionine, a compound that plays an important role in transmethylation processes in plants was also applied to living plants. Stable carbon isotope labelling experiments clearly verified that methionine acts as a precursor compound for the methane from plants. Further experiments in which the electron transport chain was inhibited suggest that the methane generation is located in the mitochondria of the plants. The abiotic formation of methane was shown for several soil samples. Important environmental parameter such as temperature, UV irradiation and moisture were identified to control methane formation. The organic content of the sample as well as water and hydrogen peroxide might also play a major role in the formation of methane from soils. Based on these results a novel scheme was developed that includes both biotic and chemical sources of methane in the pedosphere.rn

Entwicklung und Anwendung massenspektrometrischer Methoden zur Spurenanalytik iodhaltiger Verbindungen und aliphatischer Amine in der marinen Umwelt

In der marinen Grenzschicht beeinflussen reaktive Iodspezies wie z.B. I2 sowie aliphatische Amine eine Vielzahl atmosphärischer Prozesse, vor allem bei der Partikelneubildung spielen sie eine entscheidende Rolle. Allerdings stellt die Quantifizierung dieser Verbindungen im Spurenbereich immer noch eine große analytische Herausforderung dar. rnAus diesem Grund wurde im Rahmen der vorliegenden Arbeit das GTRAP-AMS (Gaseous compound trapping in artificially generated particles – aerosol mass spectrometry) entwickelt, um gasförmiges I2 und aliphatische Amine zu bestimmen. Hierbei wird ein Flugzeit-Aerosolmassenspektrometer (ToF-AMS), das ursprünglich für die on-line Charakterisierung von Aerosolen entwickelt wurde, mit einer GTRAP-Einheit gekoppelt. Im Fall von I2 werden mit Hilfe eines pneumatischen Zerstäubers a-Cyclodextrin/NH4Br-Partikel erzeugt, die mit dem gasförmigen I2 innerhalb der GTRAP-Einheit eine Einschlussverbindung bilden und dieses dadurch selektiv in die Partikelphase aufnehmen. Für die on-line Bestimmung gasförmiger aliphatischer Amine dagegen wurde Phosphorsäure als partikulärer Reaktionspartner eingesetzt. Nach Optimierung des GTRAP-AMS Systems wurde sowohl für I2 als auch für die aliphatischen Amine eine Nachweisgrenze im sub-ppb-Bereich für eine Zeitauflösung zwischen 1 und 30 min erhalten. Als erstes wurde das GTRAP-AMS System zur Charakterisierung von Permanentdenudern eingesetzt, um deren I2-Aufnahmefähigkeit und Wiederverwendbarkeit im Vergleich zu den herkömmlichen einmal verwendbaren a-Cyclodextrin Denudern zu testen.rnIm Anschluss daran wurde das GTRAP-AMS für die Bestimmung zeitlich aufgelöster I2- Emissionsraten ausgewählter Makroalgen unter dem Einfluss von Ozon eingesetzt. Die Kenntnis der Emissionsraten iodhaltiger Verbindungen der wichtigsten weltweit vorkommenden Makroalgen ist für die Modellierung der Iodchemie in der marinen Grenzschicht von besonderer Bedeutung. Die Resultate zeigen, dass verschiedene Makroalgen sowohl unterschiedliche zeitlich aufgelöste I2-Emissionsprofile als auch Gesamtemissionsraten liefern. Im Vergleich zu den iodorganischen Verbindungen ist die Gesamtemissionsrate an I2 allerdings eine bis zwei Größenordnungen größer. Dies und die deutlich kürzere atmosphärische Lebensdauer von I2 im Vergleich zu den iodorganischen Verbindungen führen dazu, dass I2 die dominierende iodhaltige Verbindung für die Bildung reaktiver Iodatome in der marinen Grenzschicht ist. rnDa über dem tropischen Atlantischen Ozean bislang jedoch nur ein geringer Anteil der IO-Konzentration durch die Oxidation von iodorganischen Verbindungen erklärt werden kann, wurden weitere Quellen für I2 erforscht. Deshalb wurden Kammerexperimente mit Mikrolagen durchgeführt, um deren Einfluss auf die I2-Freisetzung in die Atmosphäre zu untersuchen. Hierbei konnte gezeigt werden, dass die Anwesenheit von Mikroalgen (z.B. Coscinodiscus Wailesii) im Meerwasser zu einer erhöhten Freisetzung von I2 aus dem Meerwasser in die Atmosphäre führen kann. rnDes Weiteren wurden auch Versuche zu abiotischen Bildungswegen von I2 durchgeführt. Die Ergebnisse der Atmosphärensimulationsexperimente haben gezeigt, dass partikuläre Iodoxide durch organische Verbindungen zu I2 reduziert werden können, welches im Anschluss von der Partikelphase in die Gasphase übergehen kann und dort wieder für Gasphasenprozesse zur Verfügung steht.rn