4,5-Dihydro-1,3-dioxepine als chirale Bausteine in der enantioselektiven organischen Synthese

Durch asymmetrische Doppelbindungsisomerisierung mittels Me-DuPHOS-modifizierter Dihalogen-Nickel-Komplexe als Katalysatorvorstufen lassen sich aus 2-Alkyl-4,7-dihydro-1,3-dioxepinen hochenantiomerenreine 2-Alkyl-4,5-dihydro-1,3-dioxepine erhalten. Ein Ziel dieser Arbeit war es, die bisher noch unbekannte Absolutkonfiguration dieses Verbindungstyps zu bestimmen und darüber hinaus ihre Einsatzfähigkeit in der enantioselektiven organischen Synthese zu untersuchen. Zu diesem Zweck wurden enantiomerenangereichertes 2-Isopropyl- und 2-tert-Butyl-4,5-dihydro-1,3-dioxepin mit m-Chlorperbenzoesäure epoxidiert. Dabei bildeten sich die entsprechenden 3-Chlorbenzoesäure-(2-alkyl-5-hydroxy-1,3-dioxepan-4yl)-ester in hohen Ausbeuten und Diastereoselektivitäten. Von den vier zu erwartenden Diastereomeren wurden jeweils nur zwei mit einer Selektivität von mehr als 95:5 gebildet. Im Fall des 3-Chlorbenzoesäure-(2-isopropyl-5-hydroxy-1,3-dioxepan-4yl)-esters konnte das Haupt-diastereomer kristallin erhalten werden. Durch röntgenspektroskopische Untersuchung war es möglich, die Relativ-Konfiguration dieser Verbindung zu bestimmen. Die Ester lassen sich unter Ringverengung in 2-Alkyl-1,3-dioxan-4-carbaldehyde umlagern. Ausgehend von diesen Carbaldehyden stehen zwei Synthesewege zur Verfügung, welche zu Verbindungen führen deren Absolutkonfiguration bereits bekannt ist. So erhält man durch Reduktion 2-Alkyl-1,3-dioxan-4-yl-methanole, welche sich in 1,2,4-Butantriol überführen lassen. Oxidation ergibt die 2-Alkyl-1,3-dioxan-4-carbonsäuren, aus denen 3-Hydroxytetrahydrofuran-2-on gewonnen werden kann. Messung des Drehwertes dieser beiden literaturbekannten Verbindungen liefert nicht nur Information über deren Enantiomerenreinheit sondern ebenfalls über die Konfiguration ihres Stereozentrums. In Kombination mit der Relativ-Konfiguration des Esters ist somit ein Rückschluss auf die Absolutkonfiguration der eingesetzten 4,5-Dihydro-1,3-dioxepine möglich. Die auf den beschriebenen Wegen gewonnenen Substanzen finden Anwendung in der stereoselektiven organischen Synthese. Löst man die Chlorbenzoesäureester in Dichlormethan und behandelt sie mit wässriger Salzsäure, so entstehen die bicyclischen 2-Alkyltetrahydrofuro[2,3-d][1,3]dioxole. Auch bei diesen Verbindungen konnten hohe Enantio- und Diastereoselektivitäten erzielt werden. Der intermolekular verlaufende Reaktionsmechanismus der Bicyclus-Bildung, welcher unter Abspaltung eines den Alkylrest tragenden Aldehyds und dessen Neuanlagerung unter Ausbildung eines Acetals verläuft, konnte in dieser Arbeit durch ein Kreuzungsexperiment bestätigt werden. Umacetalisierung der Bicyclen liefert 2-Methoxytetrahydrofuran-3-ol, aus dem durch Acetalspaltung Tetrahydrofuran-2,3-diol erhalten wird, das die Halbacetalform der entsprechenden Desoxytetrose darstellt, die auf diese Weise in einer de novo-Synthese hergestellt werden kann.

Phosphorus placement an acid arenosols of the West African Sahel

Phosphorus (P) deficiency is a major constraint to pearl millet (Pennisetum glaucum L.) growth on acid sandy soils of the West African Sahel. To develop cost-effective fertilization strategies for cash poor farmers, experiments with pearl millet were conducted in southwestern Niger. Treatments comprised single superphosphate hill-placed at rates of 1, 3, 5 or 7 kg P ha^−1 factorially combined with broadcast P at a rate of 13 kg ha^−1. Nitrogen was applied as calcium ammonium nitrate at rates of 30 and 45 kg ha^−1. At low soil moisture, placement of single superphosphate in immediate proximity to the seed reduced seedling emergence. Despite these negative effects on germination, P placement resulted in much faster growth of millet seedlings than did broadcast P. With P application, potassium nutrition of millet was improved and seedling nitrogen uptake increased two- to three-fold, indicating that nitrogen was not limiting early millet growth. Averaged over the 1995 and 1996 cropping seasons, placed applications of 3, 5 and 7 kg P ha^−1 led to 72%, 81% and 88% respectively, of the grain yield produced by broadcasting 13 kg P ha^−1. Nitrogen application did not show major effects on grain yield unless P requirements were met. A simple economic analysis revealed that the profitability of P application, defined as additional income per unit of fertilizer, was highest for P placement at 3 and 5 kg ha^−1.

Changes in amino acid enantiomers and microbial performance in soils from a subtropical mountain oasis in Oman abandoned for different periods

An important feature of maintaining the agricultural stability in millennia-old mountain oases of northern Oman is the temporary abandonment of terraces. To analyse the effects of a fallow period on soil microbial performance, i.e. microbial activity and microbial biomass, samples of eight terrace soils abandoned for different periods were collected in situ, assigned to four fallow age classes and incubated for 30 days in the laboratory after rewetting. The younger fallow age classes of 1 and 5 years were based on the records of the farmers’ recollections, the two older fallow age classes of 10–20 and 25–60 years according to the increase in the D -to- L ratio of valine and leucine enantiomers. The increase in these two ratios was in agreement with that of the D -to- L ratio of lysine. The strongest relationship was observed between the increase in the D -to- L ratio of lysine and the decrease in soil microbial biomass C. However, the most stringent coherence between the increase in fallow age and soil properties was revealed by the decreases in cumulative respiration and net N mineralisation rates with decreasing availability of substrate to soil microorganisms. During the 30-day incubation following rewetting, relative changes in microbial activity (respiration and net N mineralisation) and microbial biomass (C and N)indices were similar in the eight terrace soils on a fallow age-class-specific level, indicating that the same basic processes occurred in all of the sandy terrace soils investigated.

Effect of environmental conditions on the N uptake route of soil microorganisms and adaption of a method to determine amino acid oxidase in soil

Soil microorganisms have evolved two possible mechanisms for their uptake of organic N: the direct route and the mobilization-immobilization-turnover (MIT) route. In the direct route, simple organic molecules are taken up via various mechanisms directly into the cell. In the MIT route, the deamination occurs outside the cell and all N is mineralized to NH4+ before assimilation. A better understanding of the mechanisms controlling the different uptake routes of soil microorganisms under different environmental conditions is crucial for understanding mineralization processes of organic material in soil. For the first experiment we incubated soil samples from the long term trial in Bad Lauchstädt with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C. Under the assumption that all added amino acids were taken up or mineralized, the direct uptake route was more important in soil amended with corn residues with a wide C to N ratio. After 21 days of incubation the direct uptake of added amino acids increased in the order addition of corn residue with a: “C to N ratio of 40 & (NH4)2SO4 and no addition (control)” (69% and 68%, respectively) < “C to N ratio of 20” (73%) < “C to N ratio of 40” (95%). In all treatments the proportion of the added amino acids that were mineralized increased with time, indicating that the MIT route became more important over time. To investigate the effects of soil depth on the N uptake route of soil microorganisms (experiment II), soil samples in two soil depths (0-5 cm; 30-40 cm) were incubated with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C and 60% (WHC). The addition of corn residue resulted in a marked increase of protease activity in both depths due to the induction from the added substrate. Addition of corn residue with a wide C to N ratio resulted in a significantly greater part of the direct uptake (97% and 94%) than without the addition of residues (85% and 80%) or addition of residue with a small C to N ratio (90% and 84%) or inorganic N (91% and 79% in the surface soil and subsoil, respectively), suggesting that under conditions of sufficient mineralizable N (C to N ratio of 20) or increased concentrations of NH4+, the enzyme system involved in the direct uptake is slightly repressed. Substrate additions resulted in an initially significantly higher increase of the direct uptake in the surface soil than in the subsoil. As a large proportion of the organic N input into soil is in form of proteinaceous material, the deamination of amino acids is a key reaction of the MIT route. Therefore the enzyme amino acid oxidase contribute to the extracellular N mineralization in soil. The objective of experiment III was to adapt a method to determine amino acid oxidase in soil. The detection via synthetic fluorescent Lucifer Yellow derivatives of the amino acid lysine is possible in soil. However, it was not possible to find the substrate concentration at which the reaction rate is independent of substrate concentration and therefore we were not able to develop a valid soil enzyme assay.