Photoschaltbare Azobenzol-modifizierte selbstorganisierte Monoschichten auf Gold(111)-Oberflächen

Für die Entwicklung photoschaltbarer selbstorganisierter Monoschichten (SAMs) auf Gold(111)-Oberflächen wurden neue Azobenzol-terminierte Asparagussäure - und Liponsäurederivate synthetisiert. Um den Einfluss lateraler Wasserstoffbrückenbindungen auf Qualität und Orientierungsordnung der Schichten zu untersuchen, wurden Monolagen, die durch amid- und esterverknüpfte Verbindungen gebildet wurden, miteinander verglichen. Die Filmbildung aus der Lösung wurde in situ durch optische Frequenzverdopplung (SHG) untersucht und die Photoreaktivität mittels Kontaktwinkelmessungen, Oberflächen-Plasmonenresonanz (SPR) und Ellipsometrie verfolgt. SAMs auf Gold wurden außerdem mit Hilfe von Röntgenphotoelektronenspektroskopie (XPS), Nahkanten-Reflexions-Röntgenabsorptionsspektroskopie (NEXAFS) und Infrarot-Reflexionsabsorptionsspektroskopie (IRRAS) charakterisiert, um die Filmqualität, die Bindung ans Substrat und Orientierungsordnung im Film zu ermitteln. Da die Chemisorption auf polykristallinem Gold formal der Koordinationschemie von 1,2-Dithiolan-Derivaten gegenüber nullwertigen Edelmetall-Zentralatomen entspricht, wurden etliche Pt-Komplexe durch oxidative Addition an [Pt(PPh3)4] dargestellt. Im Zusammenhang mit der Darstellung der Asparagussäure wurde die Kristallstruktur von [pipH]2[WS4] und der neuen Verbindungen [pipH]3[WS4](HS) und [pipH]4[WS4][WOS3] (pip = Piperidin) bestimmt. Wasserstoffbrückenbindungen zwischen den Piperidinium-Kationen und den Thiowolframat-Anionen spielen eine dominante strukturelle Rolle.

Ferrocene-Based Pyridylphosphine Ligands – Coordination Chemistry of Group 10, 11 and 12 Metals

English: The present thesis describes the synthesis of 1,1’-ferrocendiyl-based pyridylphosphine ligands, the exploration of their fundamental coordination chemistry and preliminary experiments with selected complexes aimed at potential applications. One main aspect is the synthesis of the bidentate ferrocene-based pyridylphosphine ligands 1-(Pyrid-2-yl)-1’-diphenylphosphinoferrocene, 1-(Pyrid-3-yl)-1’-diphenylphosphinoferrocene and 1-[(Pyrid-2-yl)methyl]-1’-diphenylphosphinoferrocene. A specific feature of these ligands is the ball-bearing like flexibility of the ferrocenebased backbone. An additional flexibility element is the rotation around the C–C single bonds. Consequently, the donor atoms can realise a wide range of positions with respect to each other and are therefore able to adapt to the coordination requirements of different metal centres. The flexibility of the ligand also plays a role in another key aspect of this work, which concerns the coordination mode, i. e. bridging vs. chelating. In addition to the flexibility, also the position of the donor atoms to each other is important. This is largely affected by the position of the pyridyl nitrogen (pyrid-2-yl vs. pyrid-3-yl) and the methylen group in 1-[(Pyrid-2-yl)methyl]-1’-diphenylphosphinoferrocene. Another interesting point is the combination of a soft phosphorus donor atom with a harder nitrogen donor atom, according to the HSAB principle. This combination generates a unique binding profile, since the pi-acceptor character of the P site is able to stabilise a metal centre in a low oxidation state, while the nitrogen sigma-donor ability can make the metal more susceptible to oxidative addition reactions. A P,N-donor combination can afford hemilabile binding profiles, which would be ideal for catalysis. Beyond 1,2-substituted ferrocene derivatives, which are quite successful in catalytic applications, 1,1’-derivatives are rather underrepresented. While a low-yield synthetic pathway to 1-(Pyrid-2-yl)-1’-diphenylphosphinoferrocene was already described in the literature [I. R. Butler, Organometallics 1992, 11, 74.], it was possible to find a new, improved and simplified synthetic pathway. Both other ligands were unknown prior to this work. Satisfactory results in the synthesis of 1-(Pyrid-3-yl)-1’-diphenylphosphinoferrocene could be achieved by working in analogy to the new synthetic procedure for 1-(Pyrid-2-yl)-1’-diphenylphosphinoferrocene. The synthesis of 1-[(Pyrid-2-yl)methyl]-1’-diphenylphosphinoferrocene has been handled by the group of Prof. Petr Stepnicka from Charles University, Prague, Czech Republic. The synthesis of tridentate ligands with an analogous heterodentate arrangement, was investigated briefly as a sideline of this study. The major part of this thesis deals with the fundamental coordination chemistry towards transition metals of the groups 10, 11 and 12. Due to the well-established catalytic properties of analogous palladium complexes, the coordination chemistry towards palladium (group 10) is of particular interest. The metals zinc and cadmium (group 12) are also of substantial importance because they are redox-inert in their divalent state. This is relevant in view of electrochemical investigations concerning the utilisation of the ligands as molecular redox sensors. Also mercury and the monovalent metals silver and gold (group 11) are included because of their rich coordination chemistry. It is essential to answer questions concerning aspects of the ligands’ coordination mode bearing in mind the HSAB principle.

Composition and stability of organic matter fractions in soils under different land use regimes

Soil organic matter (SOM) vitally impacts all soil functions and plays a key role in the global carbon (C) cycle. More than 70% of the terrestric C stocks that participate in the active C cycle are stored in the soil. Therefore, quantitative knowledge of the rates of C incorporation into SOM fractions of different residence time is crucial to understand and predict the sequestration and stabilization of soil organic carbon (SOC). Consequently, there is a need of fractionation procedures that are capable of isolating functionally SOM fractions, i.e. fractions that are defined by their stability. The literature generally refers to three main mechanisms of SOM stabilization: protection of SOM from decomposition by (i) its structural composition, i.e. recalcitrance, (ii) spatial inaccessibility and/or (iii) interaction with soil minerals and metal ions. One of the difficulties in developing fractionation procedures for the isolation of functional SOM fractions is the marked heterogeneity of the soil environment with its various stabilization mechanisms – often several mechanisms operating simultaneously – in soils and soil horizons of different texture and mineralogy. The overall objective of the present thesis was to evaluate present fractionation techniques and to get a better understanding of the factors of SOM sequestration and stabilization. The first part of this study is attended to the structural composition of SOM. Using 13C cross-polarization magic-angle spinning (CPMAS) nuclear magnetic resonance (NMR) spectroscopy, (i) the effect of land use on SOM composition was investigated and (ii) examined whether SOM composition contributes to the different stability of SOM in density and aggregate fractions. The second part of the present work deals with the mineral-associated SOM fraction. The aim was (iii) to evaluate the suitability of chemical fractionation procedures used in the literature for the isolation of stable SOM pools (stepwise hydrolysis, treatments using oxidizing agents like Na2S2O8, H2O2, and NaOCl as well as demineralization of the residue obtained by the NaOCl treatment using HF (NaOCl+HF)) by pool sizes, 13C and 14C data. Further, (iv) the isolated SOM fractions were compared to the inert organic matter (IOM) pool obtained for the investigated soils using the Rothamsted Carbon Model and isotope data in order to see whether the tested chemical fractionation methods produce SOM fractions capable to represent this pool. Besides chemical fractionation, (v) the suitability of thermal oxidation at different temperatures for obtaining stable SOC pools was evaluated. Finally, (vi) the short-term aggregate dynamics and the factors that impact macroaggregate formation and C stabilization were investigated by means of an incubation study using treatments with and without application of 15N labeled maize straw of different degradability (leaves and coarse roots). All treatments were conducted with and without the addition of fungicide. Two study sites with different soil properties and land managements were chosen for these investigations. The first one, located at Rotthalmünster, is a Stagnic Luvisol (silty loam) under different land use regimes. The Ah horizons of a spruce forest and continuous grassland and the Ap and E horizons of two plots with arable crops (continuous maize and wheat cropping) were examined. The soil of the second study site, located at Halle, is a Haplic Phaeozem (loamy sand) where the Ap horizons of two plots with arable crops (continuous maize and rye cropping) were investigated. Both study sites had a C3-/C4-vegetational change on the maize plot for the purpose of tracing the incorporation of the younger, maize-derived C into different SOM fractions and the calculation of apparent C turnover times of these. The Halle site is located near a train station and industrial areas, which caused a contamination with high amounts of fossil C. The investigation of aggregate and density fractions by 13C CPMAS NMR spectroscopy revealed that density fractionation isolated SOM fractions of different composition. The consumption of a considerable part (10–20%) of the easily available O-alkyl-C and the selective preservation of the more recalcitrant alkyl-C when passing from litter to the different particulate organic matter (POM) fractions suggest that density fractionation was able to isolate SOM fractions with different degrees of decomposition. The spectra of the aggregate fractions resembled those of the mineral-associated SOM fraction obtained by density fractionation and no considerable differences were observed between aggregate size classes. Comparison of plant litter, density and aggregate size fractions from soil under different land use showed that the type of land use markedly influenced the composition of SOM. While SOM of the acid forest soil was characterized by a large content (> 50%) of POM, which contained high amounts of spruce-litter derived alkyl-C, the organic matter in the biologically more active grassland and arable soils was dominated by mineral-associated SOM (> 95%). This SOM fraction comprised greater proportions of aryl- and carbonyl-C and is considered to contain a higher amount of microbially-derived organic substances. Land use can alter both, structure and stability of SOM fractions. All applied chemical treatments induced considerable SOC losses (> 70–95% of mineral-associated SOM) in the investigated soils. The proportion of residual C after chemical fractionation was largest in the arable Ap and E horizons and increased with decreasing C content in the initial SOC after stepwise hydrolysis as well as after the oxidative treatments with H2O2 and Na2S2O8. This can be expected for a functional stable pool of SOM, because it is assumed that the more easily available part of SOC is consumed first if C inputs decrease. All chemical treatments led to a preferential loss of the younger, maize-derived SOC, but this was most pronounced after the treatments with Na2S2O8 and H2O2. After all chemical fractionations, the mean 14C ages of SOC were higher than in the mineral-associated SOM fraction for both study sites and increased in the order: NaOCl < NaOCl+HF ≤ stepwise hydrolysis << H2O2 ≈ Na2S2O8. The results suggest that all treatments were capable of isolating a more stable SOM fraction, but the treatments with H2O2 and Na2S2O8 were the most efficient ones. However, none of the chemical fractionation methods was able to fit the IOM pool calculated using the Rothamsted Carbon Model and isotope data. In the evaluation of thermal oxidation for obtaining stable C fractions, SOC losses increased with temperature from 24–48% (200°C) to 100% (500°C). In the Halle maize Ap horizon, losses of the young, maize-derived C were considerably higher than losses of the older C3-derived C, leading to an increase in the apparent C turnover time from 220 years in mineral-associated SOC to 1158 years after thermal oxidation at 300°C. Most likely, the preferential loss of maize-derived C in the Halle soil was caused by the presence of the high amounts of fossil C mentioned above, which make up a relatively large thermally stable C3-C pool in this soil. This agrees with lower overall SOC losses for the Halle Ap horizon compared to the Rotthalmünster Ap horizon. In the Rotthalmünster soil only slightly more maize-derived than C3-derived SOC was removed by thermal oxidation. Apparent C turnover times increased slightly from 58 years in mineral-associated SOC to 77 years after thermal oxidation at 300°C in the Rotthalmünster Ap and from 151 to 247 years in the Rotthalmünster E horizon. This led to the conclusion that thermal oxidation of SOM was not capable of isolating SOM fractions of considerably higher stability. The incubation experiment showed that macroaggregates develop rapidly after the addition of easily available plant residues. Within the first four weeks of incubation, the maximum aggregation was reached in all treatments without addition of fungicide. The formation of water-stable macroaggregates was related to the size of the microbial biomass pool and its activity. Furthermore, fungi were found to be crucial for the development of soil macroaggregates as the formation of water-stable macroaggregates was significantly delayed in the fungicide treated soils. The C concentration in the obtained aggregate fractions decreased with decreasing aggregate size class, which is in line with the aggregate hierarchy postulated by several authors for soils with SOM as the major binding agent. Macroaggregation involved incorporation of large amounts maize-derived organic matter, but macroaggregates did not play the most important role in the stabilization of maize-derived SOM, because of their relatively low amount (less than 10% of the soil mass). Furthermore, the maize-derived organic matter was quickly incorporated into all aggregate size classes. The microaggregate fraction stored the largest quantities of maize-derived C and N – up to 70% of the residual maize-C and -N were stored in this fraction.

Diazafluoren-9-yliden als Bindungsmotiv für Metallfragmente in kreuzkonjugierten π-Systemen

In der vorliegenden Dissertation wurden kreuzkonjugierte organische Verbindungen basierend auf Diazafluorenmethyliden- sowie Dipyridylmethyliden-Bausteinen synthetisiert, die zum einen photoredoxaktive Metallfragmente komplexieren können und zum anderen erweiterte π-konjugierte Pfade auf der Grundlage von Alkineinheiten ermöglichen. Das kreuzkonjugierte Motiv wurde über die Kupplung von Alkineinheiten an halogenierte Methyliden-Einheiten, den so genannten Dibromolefinen, zugänglich gemacht. Zur Synthese von Dibromolefinen wurden verschiedene Methoden untersucht. Literaturbekannte Methoden wie die Wittig-Reaktion und ihre Modifikationen sowie die Corey-Fuchs-Reaktion konnten für die Diazafluoreneinheit nicht erfolgreich angewendet werden. Bei einer mikrowellenunterstützten Reaktion konnte sowohl ausgehend von Diazafluoren-9-on als auch von Di-2-pyridylketon eine Dibromolefinierung (55 % und 65 %) erreicht werden. Die Eignung der Mikrowellenstrahlung für Dibromolefinierungsreaktionen nach Corey und Fuchs wurde weiterhin an verschiedenen Aldehyden und Ketonen untersucht. In den meisten Fällen konnten gute bis sehr gute Ergebnisse erzielt werden. Durch die erfolgreiche Synthese von Dibromolefinen über Mikrowellensynthese wurde die Realisierung von diversen π-konjugierten Systemen möglich. Dies erfolgte exemplarisch durch die Kupplung der Alkine 5-Ethinyl-2,2’-bipyridin, 1-(Ferrocenylethinyl)-4-(ethinyl)benzol, Tri(tolyl)propin sowie der TIPS- und TMS-Acetylene. Neben der Vielfalt an Möglichkeiten zur Funktionalisierung von Dipyridyl- und Diazafluorenbausteinen zeigte sich zudem, dass sogar räumlich anspruchsvolle Verbindungen wie die geminale angeordneten voluminösen Tri(tolyl)propinyl-Substituenten an der Doppelbindung erfolgreich synthetisiert werden können. Die Koordinationseigenschaften der neu synthetisierten Verbindungen konnten durch Umsetzungen der Diazafluoren- und Dipyridylverbindungen mit PdCl2 und [RuCl2(bpy)2] erfolgreich gezeigt werden. Im Hinblick auf die Herstellung von Funktionsmaterialien eignen sich die Endiin-Strukturmotive aufgrund von diversen Variationsmöglichkeiten wie Koordination von Übergangsmetallen sowie Funktionalisierung der Peripherie gut. Dadurch können die elektronischen Eigenschaften wie die Absorption oder elektrochemische Potentiale der Verbindungen modifiziert werden. Die UV/Vis-Spektren der neu synthetisierten Verbindungen zeigen, dass Absorptionen in längerwelligen Bereichen durch Verlängerung des Konjugationspfades gesteuert werden können. Zudem lassen sich weitere photophysikalische Eigenschaften wie MC-, LC-, LMCT- oder MLCT-Übergänge durch Koordination von Metallen generieren. Die elektrochemischen Potentiale der Dipyridyl- und Diazafluorenbausteine konnten durch Anbindung von verschiedenen Substituenten beeinflusst werden. Es zeigte sich, dass sich die Reduktionswellen im Vergleich zu denen der Ketone zu niedrigeren Potentialen verschieben, wenn Alkine an die Dipyridylmethyliden- und Diazafluorenmethyliden-Bausteine geknüpft wurden. Zudem konnte beobachtet werden, dass die Signale nicht immer reversibel sind. Insbesondere die Dipyridylverbindungen zeichneten sich durch irreversible Reduktionswellen aus. Die Realisierung von π-konjugierten Systemen gelang auch mit cyclischen kohlenstoffbasierten Verbindungen. Über das separat synthetisierte 2,2’-Diethinyltolan konnte eine cyclische Verbindung, ein dehydroannulen-radialenisches System, erfolgreich hergestellt werden. Die Koordination von redoxaktiven Metallzentren wie [Ru(bpy)2] konnte für diese Verbindung ebenfalls erfolgreich gezeigt werden. Die elektronische Wechselwirkung zwischen dem Metallzentrum und dem dehydroannulenischen System könnte sowohl über theoretische Methoden (zeitabhängige Dichtefunktionaltheorie) als auch experimentell wie z. B. über transiente Absorptionsspektroskopie untersucht werden. Diese zukünftig durchzuführenden Untersuchungen können Aufschluss über die Ladungstransferraten und -dauer geben. Im Hinblick auf die Realisierung von Modellverbindungen für molekulare Drähte wurden lineare Systeme basierend auf der Diazafluoreneinheit synthetisiert. Zur Synthese von derartigen Systemen war es zunächst notwendig, die Dibromolefine unsymmetrisch zu alkinylieren. Die unsymmetrische Substitution gestaltete sich als Herausforderung, da eine Einfachkupplung mit einem Acetylen nicht möglich war. In den meisten Fällen wurden zweifach substituierte Spezies mit den identischen Alkinen erhalten. Die besten Ausbeuten konnten durch die konsekutive Zugabe von TIPS-Acetylen und darauffolgend TMS-Acetylen in die Reaktionsmischung erhalten werden. Offenbar spielt der räumliche Anspruch des Erstsubstituenten in diesem Zusammenhang eine Rolle. Die selektive Entschützung der unterschiedlich silylierten Verbindungen erfolgte mit K2CO3 in MeOH/THF (1:1). Die oxidative Homokupplungsreaktion erfolgte ohne Isolierung der entschützten Spezies, da diese instabil ist und zur Polymerisation neigt. Aufgrund der Instabilität der entschützten Spezies sowie möglichen Nebenreaktionen waren die Ausbeuten sowohl bei der TIPS-geschützten Verbindung als auch bei der TTP-geschützten Verbindung gering. Versuche, lineare Systeme von dipyridylbasierten Verbindungen zu erhalten, schlugen fehl. Die π-konjugierten Systeme lassen aufgrund der effektiven Überlappung der beteiligten π-Orbitale hohe Ladungsträgermobilitäten vermuten. Die im Rahmen dieser Arbeit synthetisierten Verbindungen könnten mit Schwefelverbindungen die Anbindung an Elektroden zulassen, worüber die Leitfähigkeiten der Verbindungen gemessen werden könnten.