Research question: Agri-environment schemes play an increasingly important role in European CAP (Common Agricultural Policy) to support biodiversity and environment in agricultural landscapes. They have been implemented since 1992 and now cost a yearly 1.7 billion Euro. Still, there is no conclusive evidence that these schemes actually do contribute to the conservation of particularly biodiversity. The primary objective of this project is to evaluate the (cost-) effectiveness of European agri-environment schemes in protecting biodiversity and to determine the primary processes that determine their effectiveness. This project furthermore aims to determine how CAP may be introduced in candidate EU-members without unacceptable loss of biodiversity. It will provide simple guidelines how researchers, governmental authorities may efficiently evaluate agri-environmental measures. Aim: Agri-environment schemes have been used to protect biodiversity and environment in agricultural areas since 1992. Their effectiveness has never been reliably evaluated. This project aims to evaluate the (cost-)effectiveness of agri-environment schemes with respect to biodiversity conservation in five European countries. It will determine the proper scales that have to be addressed for conservation efforts for a range of species groups. It will determine the most important environmental factors that influence the effectiveness of the schemes. Based on this, recommendations will be made how the effectiveness of schemes may be improved and simple guidelines will be produced how ecological effects of agri-environment schemes can be evaluated efficiently by governmental authorities or other institutions. The ecological effects of the introduction of CAP in a candidate EU-member will be investigated to reduce negative side effects of anticipated land-use changes Scientific methods: We will examine the effectiveness of agri-environment schemes by surveying pairs of fields: a field with an agri-environment scheme and a nearby field that is conventionally managed. In five countries, in each country in three areas, and in each area on seven pairs of fields the species richness of birds, plants and three insect groups (pollinators, herbivores, predators) will be determined. Effects of schemes on pollination efficiency and pest control will be examined using indicator communities. Correlative studies will examine the effects of landscape structure, land-use intensity and species pool on the effectiveness of agri-environmental measures. The spatial scale that is relevant to nature conservation efforts will be investigated via the spatial distribution of species groups. The results will be used to formulate recommendations how to improve the effectiveness of agri-environment schemes and to construct a set of simple guidelines how schemes can be evaluated efficiently yet reliably.
The goal of this project is to capture and analyse fluctuations of the fresh water in the western Nordic Seas and to understand the related processes. The East Greenland Current in the Nordic Seas constitutes an important conduit for fresh water exiting the Arctic Ocean towards the North Atlantic. The Arctic Ocean receives huge amounts of fresh water by continental runoff and by import from the Pacific Ocean. Within the Arctic Ocean fresh water is concentrated at the surface through sea ice formation. The East Greenland Current carries this fresh water in variable fractions as sea ice and in liquid form; part of it enters the central Nordic Seas, via branching of the current and through eddies. It controls the intensity of deep water formation and dilutes the water masses which result from convection. The last decades showed significant changes of the fresh water yield and distribution in the Nordic Seas and such anomalies were found to circulate through the North Atlantic. In this project the fresh water inventory, its spatial distribution and its pathways between the East Greenland Current and the interior Greenland and Icelandic seas shall be captured by autonomous glider missions. The new measurements and existing data will, in combination with the modeling work of the research group, serve as basis for understanding the causes of the fresh water variability and their consequences for the North Atlantic circulation and deep water formation.
Der Verlauf der atmosphärischen CO2-Konzentrationen während der vergangenen Klimazyklen ist durch ein Sägezahnmuster mit Maxima in Warmzeiten und Minima in Kaltzeiten geprägt. Es besteht derzeit Konsens, dass insbesondere der Süd Ozean (SO) eine Schlüsselfunktion bei der Steuerung der CO2-Entwicklung einnimmt. Allerdings sind die dabei wirksamen Mechanismen, die in Zusammenhang mit Änderungen der Windmuster, Ozeanzirkulation, Stratifizierung der Wassersäule, Meereisausdehnung und biologischer Produktion stehen, noch nicht ausreichend bekannt. Daten zur Wirkung dieser Prozesse im Wechsel von Warm- und Kaltzeiten beziehen sich bislang fast ausschließlich auf den atlantischen SO. Um ein umfassendes Bild der Klimasteuerung durch den SO zu erhalten muss geklärt werden, wie weit sich die aus dem atlantischen SO bekannten Prozesswirkungen auf den pazifischen SO übertragen lassen. Dies ist deshalb von Bedeutung, da der pazifische SO den größten Teil des SO einnimmt. Darüber hinaus stellt er das hauptsächliche Abflussgebiet des Westantarktischen Eisschildes (WAIS) in den SO dar. Im Rahmen des Projektes sollen mit einer neu entwickelten Proxy-Methode Paläoumwelt-Zeitreihen an ausgewählten Sedimentkernen von latitudinalen Schnitten über den pazifischen SO hinweg gewonnen werden. Dabei handelt es sich um kombinierte Sauerstoff- und Siliziumisotopenmessungen an gereinigten Diatomeen und Radiolarien. Es sollen erstmalig die physikalischen Eigenschaften und Nährstoffbedingungen in verschiedenen Stockwerken des Oberflächenwassers aus verschiedenen Ablagerungsräumen und während unterschiedlicher Klimabedingungen beschrieben werden. Dies umfasst Bedingungen von kälter als heute (z.B. Letztes Glaziales Maximum) bis zu wärmer als heute (z.B. Marines Isotopen Stadium, MIS 5.5). Die Untersuchungen geben Hinweise zur (1) Sensitivität des antarktischen Ökosystems auf den Eintrag von Mikronährstoffen (Eisendüngung), (2) Oberflächenwasserstratifizierung und (3) 'Silicic-Acid leakage'-Hypothese, und tragen damit zur Überprüfung verschiedener Hypothesen zur Klimawirksamkeit von SO-Prozessen bei. Die neuen Proxies bilden überdies Oberflächen-Salzgehaltsanomalien ab, die Hinweise zur Stabilität des WAIS unter verschiedenen Klimabedingungen geben. Darüber hinaus kann die Hypothese getestet werden, nach der der WAIS während MIS 5.5 vollständig abgebaut war. Die Projektergebnisse sollen mit Simulationen mit einem kombinierten biogeochemischen (Si-Isotope beinhaltenden) Atmosphäre-Ozean-Zirkulations-Modell aus einem laufenden SPP1158-DFG Projekt an der CAU Kiel (PI B. Schneider) verglichen werden. Damit sollen die jeweiligen Beiträge der Ozeanzirkulation und der biologischen Produktion zum CO2-Austausch zwischen Ozean und Atmosphäre getrennt und statistisch analysiert werden. Informationen zu Staubeintrag, biogenen Flussraten, physikalischen Ozeanparametern und zur Erstellung von Altersmodellen stehen durch Zusammenarbeit mit anderen (inter)nationalen Projekten zur Verfügung.
This subproject aims to analyze the fragmentation of forest policy at both an international and national level for the selected countries, employing a discourse analysis approach. It is split into two sub-subprojects (SSPs). 'SSPa' conducts an analysis of discursive genealogies of forest policy in Germany, Sweden, and the US. 'SSPb' investigates the history of forest related discourses in three global environmental policy processes (UNFF, CBD, and UNFCCC). In doing so, both SSPs follow a three step procedure: In the first work package, relevant literature is reviewed and a theoretical and analytical framework is developed. In the second work package, empirical data (mostly formal and informal policy documents) are gathered and analyzed. In the third work package, emphasis is placed on the role of political 'elites' in the creation of fragmented forest policy discourses at different levels; in-depth interviews with policy stakeholders and experts add another perspective to the analysis in this work package. The project is expected to develop a new understanding not only of the fragmentation of multi-level and multi-sector forest policy discourses, but also of the way in which 'discourse elites' interact with and within these discourses. The results of the work packages will be published in peer reviewed journals and discussed with policy stakeholders and scientists in conferences and workshops.
The relevance of biogeochemical gradients for turnover of organic matter and contaminants is yet poorly understood. This study aims at the identification and quantification of the interaction of different redox processes along gradients. The interaction of iron-, and sulfate reduction and methanogenesis will be studied in controlled batch and column experiments. Factors constraining the accessibility and the energy yield from the use of these electron acceptors will be evaluated, such as passivation of iron oxides, re-oxidation of hydrogen sulfide on iron oxides. The impact of these constraints on the competitiveness of the particular process will then be described. Special focus will be put on the evolution of methanogenic conditions in systems formerly characterized by iron and sulfate reducing condition. As methanogenic conditions mostly evolve from micro-niches, methods to study the existence, evolution and stability of such micro-niches will be established. To this end, a combination of Gibbs free energy calculations, isotope fractionation and tracer measurements, and mass balances of metabolic intermediates (small pool sizes) and end products (large pool sizes) will be used. Measurements of these parameters on different scales using microelectrodes (mm scale), micro sampling devices for solutes and gases (cm scale) and mass flow balancing (column/reactor scale) will be compared to characterize unit volumes for organic matter degradation pathways and electron flow. Of particular interest will be the impact of redox active humic substances on the competitiveness of involved terminal electron accepting processes, either acting as electron shuttles or directly providing electron accepting capacity. This will be studied using fluorescence spectroscopy and parallel factor analysis (PARAFAC) of the gained spectra. We expect that the results will provide a basis for improving reactive transport models of anaerobic processes in aquifers and sediments.
Non wood fuels for small-scale furnaces have attracted increasing interest in several European countries. New technological approaches are on the way, but the verification of any such developments is difficult and there is a large uncertainty about testing procedures and equipment. While for wood combustion standardized European measuring regulations are available and broadly applied, the testing of cereal fuel combustion is generally not following a commonly accepted procedure. Consequently the results of such measurements are not fully comparable. This applies particularly for the international level, which is here of particular relevance due to the fact that a combustion technology development for a niche application can only be economically viable if a sufficiently large marketing area can be taken into focus. The overall objective of the proposal is therefore to contribute through research to the development of uniform and comparable European procedures for testing of small-scale boilers up to a power out of 300 kW for solid biomass from agriculture like straw pellets and energy grain. The driving forces and barriers will be worked out; existing legal regulation for the installation (approval by the local authorities) in the participating countries will be collected. The state of the art of the non wood biomass boiler technology will be identified; the need for standardized tests for type approval tests and the measures to establish a European Standard will be shown. Measurement methods with special emphasis on efficiency and emissions will be worked out and the requirements and specifications of test fuels will be proposed. Test runs will be carried out following preliminary test procedures based on existing European standards for wood boilers. Based on the results of these test runs a draft for a Europe-wide uniform test procedure will be proposed. Preparatory work for a European standardization process including a round robin test will be done.
The project aims to theorize the scalar organization of natural resource governance in the European Union. This research agenda is inspired by critical geographers' work on the politics of scale. The research will examine an analytical framework derived from theories of institutional change and multi-level govern-ance to fill this theoretical gap. Furthermore, it will review conceptualizations of the state in institutional economics, evaluate their adequacy to capture the role of the state in the dynamics identified, and develop them further. The described processes may imply shifts in administrative levels, shifts in relations between different levels and changes in spatial delimitations of competent jurisdictions that result, for example, from decentralization or the introduction of river basin oriented administrative structures. The research investigates the implications of two European Directives: the Water Framework Directive (WFD) and the Marine Strategy Framework Directive (MSFD). They both have potentially great significance for the organization of marine and water governance at the level of Member States and below, and adhere to similar regulatory ideas for achieving good ecological status of waters. A multiple case study on changes in the scalar reorganization of marine and water governance that result from the implementation of the Directives will be carried out. It will rely on qualitative and quantitative data gathering based on semi-structured interviews and review of secondary and tertiary sources looking at Portugal, Spain, and Germany. It specifically addresses the role of social ecological transactions, the structure of decision making processes and the role of changes in contextual factors (such as ideologies, interdependent institutions and technology).
Existing models of soil organic matter (SOM) formation consider plant material as the main source of SOM. Recent results from nuclear magnetic resonance analyses of SOM and from own incubation studies, however, show that microbial residues also contribute to a large extent to SOM formation. Scanning electron microscopy showed that the soil mineral sur-faces are covered by numerous small patchy fragments (100 - 500 nm) deriving from microbial cell wall residues. We will study the formation and fate of these patchy fragments as continuously produced interfaces in artificial soil systems (quartz, montmorillonite, iron oxides, bacteria and carbon sources). We will quantify the relative contributions of different types of soil organisms to patchy fragment formation and elucidate the effect of redox con-ditions and iron mineralogy on the formation and turnover of patchy fragments. The develop-ment of patchy fragments during pedogenesis will be followed by studying soil samples from a chronosequence in the forefield of the retreating Damma glacier. We will characterize chemical and physical properties of the patchy fragments by nanothermal analysis and microscale condensation experiments in an environmental scanning electron microscope. The results will help understanding the processes at and characteristics of biogeochemical interfaces.
The magnetosphere of a planet is controlled by a number of factors such as the intrinsic magnetic field, the atmosphere and ionosphere, and the solar wind. Different combinations of these control factors are at work at the terrestrial planets Mercury, Venus, Earth, and Mars, hence they form a very suitable set for quantitative comparative studies. A significant intrinsic dipolar magnetic field is present only on Earth and on Mercury. However, the configuration at Mercury differs considerably from that at Earth because Mercury does not support an atmosphere and ionosphere, the dipolar field is much weaker, the solar wind denser, and the interplanetary magnetic field stronger. Both Mars and Venus have atmospheres but lack a global planetary magnetic field, with regional crustal magnetization being present on Mars. This proposal aims at investigating and comparing electrical current systems in the space environments of terrestrial planets using magnetic vector data collected by orbiting spacecraft such as Venus Express, Mars Global Surveyor, CHAMP (Earth), and MESSENGER (Mercury). We propose to construct data-driven and physically meaningful representations that reveal and quantify the influence of various control factors. To achieve this, we will tailor Empirical Orthogonal Function (EOF) analysis and other multivariate methods to the specifics of planetary magnetic field observations. In contrast to representations that build on predefined functions like spherical harmonics, basis functions in the EOF approach are derived directly from the data. EOFs are designed to extract dominant coherent variations for further interpretation in terms of known physical phenomena, and then, in a regression step, for modeling using suitable control variables. The EOF methodology thus allows quantifying the relative importance of control factors for each planet individually, and thus contributes to the solution of topical science questions. The resulting empirical models will facilitate comparative studies of current systems at the terrestrial planets.
Im Auftrag des Bayerischen Landesamtes für Umwelt hat bifa den erstmals 2003 durchgeführten Ökoeffizienzvergleich der Entsorgungsstrukturen Bayerns, Deutschlands und der Schweiz erweitert und aktualisiert. Die Ergebnisse aus dem Jahr 2003 zeigten, dass der bayerische Weg zur Gestaltung der Abfallwirtschaft in seiner Ökoeffizienz im Vergleich mit den Entsorgungsstrukturen der Schweiz und dem deutschen Durchschnitt am besten abschnitt. Nach der, im Rahmen der aktuellen Beauftragung, durchgeführten Datenaktualisierung, der Bilanzierung zusätzlicher Wertstoffströme und der Berücksichtigung des Verbots der Ablagerung nicht vorbehandelter Abfälle rücken die Entsorgungsstrukturen hinsichtlich Ihrer Ökoeffizienz deutlich enger zusammen. Die Entsorgungsstruktur Bayerns weist im Vergleich zur Entsorgungsstruktur Deutschlands zwar noch ein geringfügig besseres ökologisches Gesamtergebnis auf, ist aber gleichzeitig mit leicht höheren Gesamtkosten verbunden. Die Entsorgungsstruktur der Schweiz ist etwas weniger ökoeffizient. Die Ursachen dafür sind eine geringere Umweltentlastung im ökologischen Gesamtergebnis, gepaart mit vergleichsweise hohen Entsorgungskosten. Methoden: Analyse und Moderation sozialer Prozesse, Ökobilanzierung und Systemanalyse, Ökonomie und Managementberatung.
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