Development of a multi-species method by GC-coupling with inductively coupled plasma isotope dilution mass spectrometry for the simultaneous determination of alkylated lead, mercury and tin compounds

An accurate and sensitive species-specific GC-ICP-IDMS (gas chromatography inductively coupled plasma isotope dilution mass spectrometry) method for the determination of trimethyllead and a multi-species-specific GC-ICP-IDMS method for the simultaneous determination of trimethyllead, methylmercury, and butyltins in biological and environmental samples were developed. They allow the determination of corresponding elemental species down to the low ng g-1 range. The developed synthesis scheme for the formation of isotopically labeled Me3206Pb+ can be used for future production of this spike. The novel extraction technique, stir bar sorptive extraction (SBSE), was applied for the first time in connection with species-specific isotope dilution GC-ICP-MS for the determination of trimethyllead, methylmercury and butyltins. The results were compared with liquid-liquid extraction. The developed methods were validated by the analysis of certified reference materials. The liquid-liquid extraction GC-ICP-IDMS method was applied to seafood samples purchased from a supermarket. The methylated lead fraction in these samples, correlated to total lead, varied in a broad range of 0.01-7.6 %. On the contrary, the fraction of methylmercury is much higher, normally in the range of 80-98 %. The highest methylmercury content of up to 12 µg g-1 has been determined in shark samples, an animal which is at the end of the marine food chain, whereas in other seafood samples a MeHg+ content of less than 0.2 µg g-1 was found. Butyltin species could only be determined in samples, where anthropogenic contaminations must be assumed. This explains the observed broad variation of the butylated tin fraction in the range of <0.3-49 % in different seafood samples. Because all isotope-labelled spike compounds, except trimethyllead, are commercially available, the developed multi-species-specific GC-ICP-IDMS method has a high potential in future for routine analysis.

Investigations on maar-diatreme volcanoes by inversion of magnetic and gravity data from the Eifel area, Germany

A study of maar-diatreme volcanoes has been perfomed by inversion of gravity and magnetic data. The geophysical inverse problem has been solved by means of the damped nonlinear least-squares method. To ensure stability and convergence of the solution of the inverse problem, a mathematical tool, consisting in data weighting and model scaling, has been worked out. Theoretical gravity and magnetic modeling of maar-diatreme volcanoes has been conducted in order to get information, which is used for a simple rough qualitative and/or quantitative interpretation. The information also serves as a priori information to design models for the inversion and/or to assist the interpretation of inversion results. The results of theoretical modeling have been used to roughly estimate the heights and the dip angles of the walls of eight Eifel maar-diatremes — each taken as a whole. Inversemodeling has been conducted for the Schönfeld Maar (magnetics) and the Hausten-Morswiesen Maar (gravity and magnetics). The geometrical parameters of these maars, as well as the density and magnetic properties of the rocks filling them, have been estimated. For a reliable interpretation of the inversion results, beside the knowledge from theoretical modeling, it was resorted to other tools such like field transformations and spectral analysis for complementary information. Geologic models, based on thesynthesis of the respective interpretation results, are presented for the two maars mentioned above. The results gave more insight into the genesis, physics and posteruptive development of the maar-diatreme volcanoes. A classification of the maar-diatreme volcanoes into three main types has been elaborated. Relatively high magnetic anomalies are indicative of scoria cones embeded within maar-diatremes if they are not caused by a strong remanent component of the magnetization. Smaller (weaker) secondary gravity and magnetic anomalies on the background of the main anomaly of a maar-diatreme — especially in the boundary areas — are indicative for subsidence processes, which probably occurred in the late sedimentation phase of the posteruptive development. Contrary to postulates referring to kimberlite pipes, there exists no generalized systematics between diameter and height nor between geophysical anomaly and the dimensions of the maar-diatreme volcanoes. Although both maar-diatreme volcanoes and kimberlite pipes are products of phreatomagmatism, they probably formed in different thermodynamic and hydrogeological environments. In the case of kimberlite pipes, large amounts of magma and groundwater, certainly supplied by deep and large reservoirs, interacted under high pressure and temperature conditions. This led to a long period phreatomagmatic process and hence to the formation of large structures. Concerning the maar-diatreme and tuff-ring-diatreme volcanoes, the phreatomagmatic process takes place due to an interaction between magma from small and shallow magma chambers (probably segregated magmas) and small amounts of near-surface groundwater under low pressure and temperature conditions. This leads to shorter time eruptions and consequently to structures of smaller size in comparison with kimberlite pipes. Nevertheless, the results show that the diameter to height ratio for 50% of the studied maar-diatremes is around 1, whereby the dip angle of the diatreme walls is similar to that of the kimberlite pipes and lies between 70 and 85°. Note that these numerical characteristics, especially the dip angle, hold for the maars the diatremes of which — estimated by modeling — have the shape of a truncated cone. This indicates that the diatreme can not be completely resolved by inversion.

Entwicklung kohärenter Lichtquellen im XUV-Regime

Plasmabasierte Röntgenlaser sind aufgrund ihrer kurzen Wellenlänge und schma-rnlen spektralen Bandbreite attraktive Diagnose-Instrumente in einer Vielzahl potentieller Anwendungen, beispielsweise in den Bereichen Spektroskopie, Mikroskopie und EUV-Lithografie. Dennoch sind Röntgenlaser zum heutigen Stand noch nicht sehr weit verbreitet, was vorwiegend auf eine zu geringe Pulsenergie und für manche Anwendungen nicht hinreichende Strahlqualität zurückzuführen ist. In diesem Zusammenhang wurden in den letzten Jahren bedeutende Fortschritte erzielt. Die gleichzeitige Weiterentwicklung von Pumplasersystemen und Pumpmechanismen ermöglichte es, kompakte Röntgenlaserquellen mit bis zu 100 Hz zu betreiben. Um gleichzeitig höhere Pulsenergien, höhere Strahlqualität und volle räumliche Kohärenz zu erhalten, wurden intensive Studien theoretischer und experimenteller Natur durchgeführt. In diesem Kontext wurde in der vorliegenden Arbeit ein experimenteller Aufbau zur Kombination von zwei Röntgenlaser-Targets entwickelt, die sogenannte Butterfly-Konfiguration. Der erste Röntgenlaser wird dabei als sogenannter Seed für das zweite, als Verstärker dienende Röntgenlasermedium verwendet (injection-seeding). Aufrndiese Weise werden störende Effekte vermieden, welche beim Entstehungsprozessrndes Röntgenlasers durch die Verstärkung von spontaner Emission zustande kom-rnmen. Unter Verwendung des ebenfalls an der GSI entwickelten Double-Pulse Gra-rnzing Incidence Pumpschemas ermöglicht das hier vorgestellte Konzept, erstmaligrnbeide Röntgenlasertargets effizient und inklusive Wanderwellenanregung zu pum-rnpen.rnBei einer ersten experimentellen Umsetzung gelang die Erzeugung verstärkter Silber-Röntgenlaserpulse von 1 µJ bei 13.9 nm Wellenlänge. Anhand der gewonnenen Daten erfolgte neben dem Nachweis der Verstärkung die Bestimmung der Lebensdauer der Besetzungsinversion zu 3 ps. In einem Nachfolgeexperiment wurden die Eigenschaften eines Molybdän-Röntgenlaserplasmas näher untersucht. Neben dem bisher an der GSI angewandten Pumpschema kam in dieser Strahlzeit noch eine weitere Technik zum Einsatz, welche auf einem zusätzlichen Pumppuls basierte. In beiden Schemata gelang neben dem Nachweis der Verstärkung die zeitliche und räumliche Charakterisierung des Verstärkermediums. Röntgenlaserpulse mit bis zu 240 nJ bei einer Wellenlänge von 18.9 nm wurden nachgewiesen. Die erreichte Brillanz der verstärkten Pulse lag ca. zwei Größenordnungen über der des ursprünglichen Seeds und mehr als eine Größenordnung über der Brillanz eines Röntgenlasers, dessen Erzeugung auf der Verwendung eines einzelnen Targets basierte. Das in dieser Arbeitrnentwickelte und experimentell verifizierte Konzept birgt somit das Potential, extrem brillante plasmabasierte Röntgenlaser mit vollständiger räumlicher und zeitlicher Kohärenz zu erzeugen.rnDie in dieser Arbeit diskutierten Ergebnisse sind ein wesentlicher Beitrag zu der Entwicklung eines Röntgenlasers, der bei spektroskopischen Untersuchungen von hochgeladenen Schwerionen eingesetzt werden soll. Diese Experimente sind amrnExperimentierspeicherring der GSI und zukünftig auch am High-Energy StoragernRing der FAIR-Anlage vorgesehen.rn