Einfluss der 6 1 S - 6 3 P-Resonanz auf die Lyman-alpha-Erzeugung in Quecksilber

In dieser Arbeit wird eine kontinuierliche, kohärente Strahlungsquelle bei 121,56nm, der Lyman-alpha Linie in Wasserstoff, vorgestellt. Diese Lyman-alpha Quelle soll zur zukünftigen Laserkühlung von Antiwasserstoff dienen. Die Strahlung wird durch Vier-Wellen-Mischen in Quecksilberdampf produziert. Dabei wird ein Festkörperlasersystem zur Erzeugung der Fundamentalstrahlen eingesetzt. Zur Erhöhung der nichtlinearen Suszeptibilität wird die 6^1S-7^1S Zwei-Photonen-Resonanz ausgenutzt. Zusätzlich wird mit Hilfe eines durchstimmbaren ultravioletten Lasersystems die 6^1S-6^3P Ein-Photon-Resonanz genutzt, was es erlaubt, die nichtlineare Suszeptibilität des Mischprozesses um Größenordnungen zu erhöhen. Um den Einfluss der 6^1S-6^3P Ein-Photon-Resonanz zu untersuchen, wurden zunächst die Phasenanpassungstemperaturen bei verschiedenen Verstimmungen der ultravioletten Strahlung zur 6^3P Resonanz vermessen und festgestellt, dass kleinere Verstimmungen zu niedrigeren Phasenanpassungstemperaturen führen. Es konnte sowohl theoretisch wie auch experimentell gezeigt werden, dass diese niedrigeren Phasenanpassungstemperaturen bei kleinen Verstimmungen der Erhöhung der Lyman-alpha Erzeugung durch die größere nichtlineare Suszeptibilität bei kleinen Verstimmungen entgegenwirken. Bei immer kleineren Verstimmungen zur 6^3P Resonanz limitiert die Absorption der ultravioletten Strahlung die Lyman-alpha Erzeugung. Ein positiver Effekt der niedrigeren Phasenanpassungstemperaturen ist, dass es möglich wird, auf das bisher nötige Puffergas in der Quecksilber-Dampfzelle zu verzichten, was die Lyman-alpha Erzeugung um einen Faktor 1,7 erhöht. Damit war es möglich, die bisherige Effizienz der Lyman-alpha Erzeugung zu verbessern. Es wurde eine Lyman-alpha Leistung von 0,3nW erreicht. Zusätzlich zum Einfluss der 6^3P Resonanz auf die Lyman-alpha Erzeugung wurde ein weiterer Effekt beobachtet. Durch die Nähe der 6^1S-6^3P Ein-Photon-Resonanz wird auch mehr Besetzung in das obere 7^1S Niveau der Zwei-Photonen-Resonanz gepumpt. Dadurch konnte erstmals eine kontinuierliche Lasertätigkeit auf der 6^1P-7^1S Linie in Quecksilber bei 1014nm beobachtet werden.

Volatile organic compounds at the air-sea interface : gas exchange rates, oceanic emissions and the effect of ocean acidification

Oceans are key sources and sinks in the global budgets of significant atmospheric trace gases, termed Volatile Organic Compounds (VOCs). Despite their low concentrations, these species have an important role in the atmosphere, influencing ozone photochemistry and aerosol physics. Surprisingly, little work has been done on assessing their emissions or transport mechanisms and rates between ocean and atmosphere, all of which are important when modelling the atmosphere accurately.rnA new Needle Trap Device (NTD) - GC-MS method was developed for the effective sampling and analysis of VOCs in seawater. Good repeatability (RSDs <16 %), linearity (R2 = 0.96 - 0.99) and limits of detection in the range of pM were obtained for DMS, isoprene, benzene, toluene, p-xylene, (+)-α-pinene and (-)-α-pinene. Laboratory evaluation and subsequent field application indicated that the proposed method can be used successfully in place of the more usually applied extraction techniques (P&T, SPME) to extend the suite of species typically measured in the ocean and improve detection limits. rnDuring a mesocosm CO2 enrichment study, DMS, isoprene and α-pinene were identified and quantified in seawater samples, using the above mentioned method. Based on correlations with available biological datasets, the effects of ocean acidification as well as possible ocean biological sources were investigated for all examined compounds. Future ocean's acidity was shown to decrease oceanic DMS production, possibly impact isoprene emissions but not affect the production of α-pinene. rnIn a separate activity, ocean - atmosphere interactions were simulated in a large scale wind-wave canal facility, in order to investigate the gas exchange process and its controlling mechanisms. Air-water exchange rates of 14 chemical species (of which 11 VOCs) spanning a wide range of solubility (dimensionless solubility, α = 0:4 to 5470) and diffusivity (Schmidt number in water, Scw = 594 to 1194) were obtained under various turbulent (wind speed at ten meters height, u10 = 0:8 to 15ms-1) and surfactant modulated (two different sized Triton X-100 layers) surface conditions. Reliable and reproducible total gas transfer velocities were obtained and the derived values and trends were comparable to previous investigations. Through this study, a much better and more comprehensive understanding of the gas exchange process was accomplished. The role of friction velocity, uw* and mean square slope, σs2 in defining phenomena such as waves and wave breaking, near surface turbulence, bubbles and surface films was recognized as very significant. uw* was determined as the ideal turbulent parameter while σs2 described best the related surface conditions. A combination of both uw* and σs2 variables, was found to reproduce faithfully the air-water gas exchange process. rnA Total Transfer Velocity (TTV) model provided by a compilation of 14 tracers and a combination of both uw* and σs2 parameters, is proposed for the first time. Through the proposed TTV parameterization, a new physical perspective is presented which provides an accurate TTV for any tracer within the examined solubility range. rnThe development of such a comprehensive air-sea gas exchange parameterization represents a highly useful tool for regional and global models, providing accurate total transfer velocity estimations for any tracer and any sea-surface status, simplifying the calculation process and eliminating inevitable calculation uncertainty connected with the selection or combination of different parameterizations.rnrn