Copper and zinc stable isotope ratios as tracers of biogeochemical processes, sources and transport of Cu and Zn in soils

Copper and Zn are essential micronutrients for plants, animals, and humans; however, they may also be pollutants if they occur at high concentrations in soil. Therefore, knowledge of Cu and Zn cycling in soils is required both for guaranteeing proper nutrition and to control possible risks arising from pollution.rnThe overall objective of my study was to test if Cu and Zn stable isotope ratios can be used to investigate into the biogeochemistry, source and transport of these metals in soils. The use of stable isotope ratios might be especially suitable to trace long-term processes occurring during soil genesis and transport of pollutants through the soil. In detail, I aimed to answer the questions, whether (1) Cu stable isotopes are fractionated during complexation with humic acid, (2) 65Cu values can be a tracer for soil genetic processes in redoximorphic soils (3) 65Cu values can help to understand soil genetic processes under oxic weathering conditions, and (4) 65Cu and 66Zn values can act as tracers of sources and transport of Cu and Zn in polluted soils.rnTo answer these questions, I ran adsorption experiments at different pH values in the laboratory and modelled Cu adsorption to humic acid. Furthermore, eight soils were sampled representing different redox and weathering regimes of which two were influenced by stagnic water, two by groundwater, two by oxic weathering (Cambisols), and two by podzolation. In all horizons of these soils, I determined selected basic soil properties, partitioned Cu into seven operationally defined fractions and determined Cu concentrations and Cu isotope ratios (65Cu values). Finally, three additional soils were sampled along a deposition gradient at different distances to a Cu smelter in Slovakia and analyzed together with bedrock and waste material from the smelter for selected basic soil properties, Cu and Zn concentrations and 65Cu and 66Zn values.rnMy results demonstrated that (1) Copper was fractionated during adsorption on humic acid resulting in an isotope fractionation between the immobilized humic acid and the solution (65CuIHA-solution) of 0.26 ± 0.11‰ (2SD) and that the extent of fractionation was independent of pH and involved functional groups of the humic acid. (2) Soil genesis and plant cycling causes measurable Cu isotope fractionation in hydromorphic soils. The results suggested that an increasing number of redox cycles depleted 63Cu with increasing depth resulting in heavier 65Cu values. (3) Organic horizons usually had isotopically lighter Cu than mineral soils presumably because of the preferred uptake and recycling of 63Cu by plants. (4) In a strongly developed Podzol, eluviation zones had lighter and illuviation zones heavier 65Cu values because of the higher stability of organo-65Cu complexes compared to organo-63Cu complexes. In the Cambisols and a little developed Podzol, oxic weathering caused increasingly lighter 65Cu values with increasing depth, resulting in the opposite depth trend as in redoximorphic soils, because of the preferential vertical transport of 63Cu. (5) The 66Zn values were fractionated during the smelting process and isotopically light Zn was emitted allowing source identification of Zn pollution while 65Cu values were unaffected by the smelting and Cu emissions isotopically indistinguishable from soil. The 65Cu values in polluted soils became lighter down to a depth of 0.4 m indicating isotope fractionation during transport and a transport depth of 0.4 m in 60 years. 66Zn values had an opposite depth trend becoming heavier with depth because of fractionation by plant cycling, speciation changes, and mixing of native and smelter-derived Zn. rnCopper showed measurable isotope fractionation of approximately 1‰ in unpolluted soils, allowing to draw conclusions on plant cycling, transport, and redox processes occurring during soil genesis and 65Cu and 66Zn values in contaminated soils allow for conclusions on sources (in my study only possible for Zn), biogeochemical behavior, and depth of dislocation of Cu and Zn pollution in soil. I conclude that stable Cu and Zn isotope ratios are a suitable novel tool to trace long-term processes in soils which are difficult to assess otherwise.rn

Elektrochemisch gesteuerte zeitaufgelöste Infrarotspektroskopie an Redox-Membranproteinen in einer biomimetischen Membran-Architektur

Das Protein Cytochrom c Oxidase (CcO) ist ein Enzym der mitochondrialen Atmungskette. Als letzter Komplex (Komplex IV) einer Elektronentransportkette katalysiert sie die Reduktion von molekularem Sauerstoff zu Wasser. Hierbei werden Elektronen von Cytochrom c (Cc) in das Enzym geleitet. Die durch den Redoxprozess freiwerdende freie Enthalpie wird dazu genutzt, einen Protonengradienten über die innere Mitochondrien-Membran aufzubauen. Die zurückwandernden Protonen treiben in der ATP-Synthase die Produktion von Adenosintriphosphat (ATP) an, dem universellen Energieträger in lebenden Organismen. Gegenstand dieser Dissertation sind zeitaufgelöste ATR-FTIR-Messungen des direkten Elektronentransfers in die CcO. Das Protein wird hierzu orientiert auf einer Goldelektrode immobilisiert und in eine künstliche Membran rekonstituiert (Protein-tethered Bilayer Lipid Membrane, ptBLM). Das ptBLM-System wird hinsichtlich einer möglichst hohen Protein-Aktivität optimiert. Elektronen werden durch elektrochemische Anregung von der Elektrode in die CcO injiziert. Die Goldoberfläche wird auf die reflektierende Oberfläche eines Silizium-ATR-Kristalls aufgebracht. Durch die Präparation einer rauen Oberfläche (RMS-Rauigkeit ca. 5 nm) wird eine Verstärkung der IR-Absorption erreicht. Die mit den Ladungstransferprozessen einhergehenden Konformationsänderungen der die Redoxzentren umgebenden Gruppen (CONH-Gerüst und Aminosäure-Seitenketten) können durch Infrarot-Spektroskopie nachgewiesen werden. Phasensensitive Detektion (PSD) wird zur Rauschminderung eingesetzt, um Geschwindigkeitskonstanten für die Redox-Übergänge zu bestimmen. Im Bereich der Amid-I-Bande werden etliche Peaks identifiziert, die sich mit dem Redoxzustand des Proteins ändern. Für das CuA-Zentrum, welches als erstes der vier Redoxzentren der CcO reduziert wird, wird die schnellste Geschwindigkeitskonstante ks=4870/s ermittelt. Für das Häm a3-Zentrum wird eine Geschwindigkeitskonstante von ks=13,8/s ermittelt. Die Ergebnisse sind konsistent zu elektrochemischen und Raman-Spektroskopie-Experimenten, welche ebenfalls in unserer Gruppe durchgeführt wurden. Weitere Themen dieser Dissertation sind der Nachweis der Anwendbarkeit des ptBLM-Systems für andere Membranproteine (Beispiel: bakterielles photosynthetisches Reaktionszentrum) und der Einsatz des ATR-FTIR-Setups für verschiedene künstliche Membransysteme (Aktivitätsnachweis des OR5-Geruchsrezeptors in einer peptidgestützten Membran, Eigenschaften eines Oligoethylenglycol-Spacers).