Das Projekt "Effects of biochar amendment on plant growth, microbial communities and biochar decomposition in agricultural soils" wird vom Umweltbundesamt gefördert und von Forschungsinstitut für biologischen Landbau Deutschland e.V. durchgeführt. Biochar has a great potential to ameliorate arable soils, especially those that are low in organic matter due to intensive use or erosion. Biochar is carbonised organic material with high porosity that brings about changes in physical, chemical and biological soil functions. Biochar amended soils show a higher water and cation exchange capacity with reduced leaching and enhanced availability of plant nutrients. The microbial biomass in biochar amended soils is enhanced and more diverse. Biochar is stabilised organic material, which is likely to remain for hundreds of years in the soil. Photosynthetically fixed atmospheric CO2 stabilised in biochar may thus act as a direct carbon sink and help to mitigate climate change. As feedstock and production conditions produce different biochar qualities predictions of effects in soil need to consider biochar and soil properties case by case. To date biochar has been approved to ameliorate highly weathered tropical soils with positive effects on crop growth and yield. Distinct microbial groups were reported to be enhanced in soils but if this depends on the particular soil or biochar or a combination of both is an open question, especially in temperate climates. Likewise, it is not known if microorganisms colonising biochar surfaces are responsible for its mineralization or if they just use the new niches provided. The aim of the proposed project is to investigate the influence of two biochar types on soil-plant systems by determining i) soil nutrient availability, plant growth and nutrient uptake, ii) structure and function of soil microbial communities, iv) the decomposition and fate of biochar in soils. We will use two loessial soils from the well-known DOK-trial with different soil organic matter content. Other soils from the region will be selected to provide a wider range of soil quality, in particular pH. The biochars will be produced by pyrolysis and hydrothermal carbonization (HTC) from the C4-plant Miscanthus gigantea. Pyrolysis derived material has bigger pore sizes due to the evaporating gasses and is commonly alkaline, whereas the HTC derived biochar has a finer pore size, a much higher oxygen content and more acidic functional groups.
Das Projekt "Ecuador/Bergwald - Stoffhaushalt gestörter und ungestörter Ökosysteme der südecuadorianischen Anden" wird vom Umweltbundesamt gefördert und von Universität Bayreuth, Lehrstuhl für Bodenkunde und Bodengeographie durchgeführt. Mit dem beantragten Projekt werden die 1997 im südecuadorianischen Bergwald begonnenen Arbeiten fortgeführt. Die Ziele der neuen Projektphase sind (1) die abschließende Erfassung und Modellierung des Wasser- und Nährstoffhaushaltes von kleinen Wassereinzugsgebieten unter ungestörtem Bergwald, (2) die Aufklärung der Rolle chemischer Reduktionsprozesse für den Stoffhaushalt des Bergwaldes mithilfe von Redoxelektroden und d34S-Werten, (3) die Aufklärung der Fließpfade im Boden Mithilfe von d18O-Werten und (4) die Untersuchung der Auswirkungen eines ortsüblichen Landnutzungseingriffes (z.B. Brandrodung) auf den Stoffhaushalt des Bergwaldökosystems. Dazu wurden auf der zum Amazonas exponierten Andenabdachung drei etwa 10 ha große Wassereinzugsgebiete mit den erforderlichen Geräten ausgestattet. Von den Ergebnissen erwarten wir Erkenntnisse über Parameter, die den Stoffhaushalt der bisher wenig untersuchten und zunehmend bedrohten tropischen Bergwälder steuern und über die Auswirkungen menschlicher Eingriffe. Darüber hinaus liefert unser Teilprojekt wichtige bodenkundliche Basisdaten für die anderen Arbeitsgruppen.
Das Projekt "Effect of experimentally applied drought and warming stress on three oak species and provenances using C and O stable isotopes in leaves, shoots, stem and roots" wird vom Umweltbundesamt gefördert und von Eidgenössische Forschungsanstalt für Wald, Schnee und Landschaft, Eidgenössisches Institut für Schnee- und Lawinenforschung durchgeführt. The predicted climate change will have a profound effect on ecosystems in Switzerland, including forests. Tree species, for example oaks, which are more adapted to warmer and dryer conditions are expected to profit from the changing climate. Models predict a large increase in the distribution of oaks that are currently covering only 2Prozent of Swiss forests. Unfortunately, no long-term trials exist in Switzerland that could be used to test for climate sensitivity of the various oak species. At the Swiss Federal Institute WSL, therefore, an experiment in 16 open-top chambers was carried out to test how the three native oak species react to drought and warming. Regarding drought tolerance and temperature preference, the natural distribution suggests that Q. pubescens is the most drought-tolerant, followed by Q. petraea and Q. robur. The warming treatment is achieved by selecting two opening angles of the chamber window. Under less opened windows air and soil surface temperatures increases by 1 to 3 C. Automatically closing roofs exclude rain. An artificial drought treatment is achieved by reducing the mean local precipitation from April to October (600 mm) to less than half. While the control and warming treatment, receive water in regular intervals, the drought treatment and the warming and drought combination are only periodically watered. To prevent irreversible damage under drought stress trees usually close the stomata to minimize water loss via transpiration. This, however, reduces the net photosynthesis and thus the carbon fixation. The potential to optimize between water loss and carbon fixation is a key in understanding tree responses to climatic change. Besides stomata closure, photosynthesis is determined by other factors, including temperature. Both, stomata closure and photosynthetic capacity affect the fractionation of the stable carbon and oxygen isotopes. Therefore, the determination of the isotope ratios ?13C and ?18O in plant tissue allows to draw conclusion on how drought and warming affect the trees. The following samples are collected and are intended to be analyzed: a) fresh leaves, b) wood section from shoots, c) stemwood and d) root samples. The proposed study with the stable C and O isotopes will be an ideal complement to the other measurements, such as shoot elongation, biomass change, gas exchange, root growth and leaf size and nutrient content. Based on these results, potentially useful oak species and provenances for future seeding or planting can be identified and recommendations for the forest practice can be made. In addition, the derived isotope ratios would allow the identification of drought stressed trees.