A chemical approach to Heusler compounds and nanoparticles

Heusler Materialien wurden bisher vor allem in Volumen- und Dünnfilmproben aufgrund ihrer technischen Bedeutung untersucht. In dieser Arbeit berichtet über die experimentellen Untersuchungen der chemischen Synthese, Struktur, und der magnetischen Eigenschaften von ternären Heusler-Nanopartikeln. Die grundlegenden Aspekte der Physik, Chemie und Materialwissenschaft bezüglich der Heusler Nanopartiikel wurden untersucht. Außerdem wurde eine silicatgestützte Herstellungsmethode für Karbon-ummantelte, ternäre intermetallische Co2FeGa Nanopartikel entwickelt. Die Bildung der L21 Co2FeGa Phase wurde mit Röntgenbeugung (XRD), Extended X-ray Absorption Fine Structure Spektroskopie (EXAFS), und 57Fe Mössbauer Spektroskopie bestätigt. Die Abhängigkeit der Phase und der der Größe der Co2FeGa Nanopartikel vom der Zusammensetzung der Precursor und des Silicats wurden untersucht. Durch das Koppeln der aus Transmissions-Elektronen-Mikroskopie (TEM) gewonnen Teilchengröße und der Mössbauerspektroskopie konnte die kritische Größe für den Übergang von superparamgnetischem zu ferromagnetischem Verhalten von Co2FeGa Nanopartikel ermittelt werden. Die silicatgestützte chemische Synthese von Co2FeGa Nanopartikeln besitzt großes Potential für eine generelle Herstellungsmethode für Co-basierte Heuser Nanopartikel. Des weiteren wurde auch eine chemische Herstellungsmethode von metallischen Nanopartikeln mit Synchrotronstrahlung untersucht, die so gewonnen Nanopartikel sind vielversprechende Materialien für die Nanobiotechnologie und die Nanomedizin.

Simulations of physics and chemistry of polar stratospheric clouds with a general circulation model

A polar stratospheric cloud submodel has been developed and incorporated in a general circulation model including atmospheric chemistry (ECHAM5/MESSy). The formation and sedimentation of polar stratospheric cloud (PSC) particles can thus be simulated as well as heterogeneous chemical reactions that take place on the PSC particles. For solid PSC particle sedimentation, the need for a tailor-made algorithm has been elucidated. A sedimentation scheme based on first order approximations of vertical mixing ratio profiles has been developed. It produces relatively little numerical diffusion and can deal well with divergent or convergent sedimentation velocity fields. For the determination of solid PSC particle sizes, an efficient algorithm has been adapted. It assumes a monodisperse radii distribution and thermodynamic equilibrium between the gas phase and the solid particle phase. This scheme, though relatively simple, is shown to produce particle number densities and radii within the observed range. The combined effects of the representations of sedimentation and solid PSC particles on vertical H2O and HNO3 redistribution are investigated in a series of tests. The formation of solid PSC particles, especially of those consisting of nitric acid trihydrate, has been discussed extensively in recent years. Three particle formation schemes in accordance with the most widely used approaches have been identified and implemented. For the evaluation of PSC occurrence a new data set with unprecedented spatial and temporal coverage was available. A quantitative method for the comparison of simulation results and observations is developed and applied. It reveals that the relative PSC sighting frequency can be reproduced well with the PSC submodel whereas the detailed modelling of PSC events is beyond the scope of coarse global scale models. In addition to the development and evaluation of new PSC submodel components, parts of existing simulation programs have been improved, e.g. a method for the assimilation of meteorological analysis data in the general circulation model, the liquid PSC particle composition scheme, and the calculation of heterogeneous reaction rate coefficients. The interplay of these model components is demonstrated in a simulation of stratospheric chemistry with the coupled general circulation model. Tests against recent satellite data show that the model successfully reproduces the Antarctic ozone hole.

The factorization method for real elliptic problems

The Factorization Method localizes inclusions inside a body from measurements on its surface. Without a priori knowing the physical parameters inside the inclusions, the points belonging to them can be characterized using the range of an auxiliary operator. The method relies on a range characterization that relates the range of the auxiliary operator to the measurements and is only known for very particular applications. In this work we develop a general framework for the method by considering symmetric and coercive operators between abstract Hilbert spaces. We show that the important range characterization holds if the difference between the inclusions and the background medium satisfies a coerciveness condition which can immediately be translated into a condition on the coefficients of a given real elliptic problem. We demonstrate how several known applications of the Factorization Method are covered by our general results and deduce the range characterization for a new example in linear elasticity.