Fahlbusch, Wiebke

[["dc.bibliographiccitation.artnumber","38"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Energy, Sustainability and Society"],["dc.bibliographiccitation.volume","8"],["dc.contributor.author","Fahlbusch, Wiebke"],["dc.contributor.author","Hey, Katharina"],["dc.contributor.author","Sauer, Benedikt"],["dc.contributor.author","Ruppert, Hans"],["dc.date.accessioned","2018-12-13T13:41:10Z"],["dc.date.available","2018-12-13T13:41:10Z"],["dc.date.issued","2018"],["dc.description.abstract","Background Energy crop production for biogas still relies mainly on maize, but the co-digestion of alternative energy crops (legumes, amaranth, ryegrass, flower mixtures) with maize can have several advantages. First, a greater biodiversity in the fields; second, an enrichment of essential trace elements in biogas substrates (cobalt, nickel, manganese, and molybdenum); and third, less use of artificial trace element additives. Methods In two randomized field trials, 12 different variants of field crops in sole, double and intercropping were tested over a 2-year period. Dry matter yield, trace element content of the crops, and soil parameters like soil texture, pH, and soil element concentration were determined. The trace element concentrations in biogas plants resulting from input mixtures of energy crops (legumes, amaranth, faba bean, and ryegrass) and maize are calculated. Results High dry matter yields were obtained for ryegrass, maize, winter faba bean maize, intercropping winter faba bean/triticale-maize, and intercropping rye/vetch-maize. The double croppings with maize reached highest total yields (ca. 30 t DM ha−1). Total element deliveries from the harvest reveal large differences between the variants and the trace elements. Cobalt is provided most by summer faba bean maize and intercropping of winter faba bean/triticale-maize. Ryegrass can deliver the greatest amounts of Manganese and Molybdenum to biogas plants."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2018"],["dc.identifier.doi","10.1186/s13705-018-0180-1"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/15716"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/57112"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.relation.orgunit","Department für Nutzpflanzenwissenschaften"],["dc.relation.orgunit","Fakultät für Agrarwissenschaften"],["dc.relation.orgunit","Abteilung Pflanzenbau"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Trace element delivery for biogas production enhanced by alternative energy crops: results from two-year field trials"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1149"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","1167"],["dc.bibliographiccitation.volume","101"],["dc.contributor.author","Friese, Nadine"],["dc.contributor.author","Vollbrecht, Axel"],["dc.contributor.author","Tanner, David Colin"],["dc.contributor.author","Fahlbusch, Wiebke"],["dc.contributor.author","Weidemann, Miriam"],["dc.date.accessioned","2018-11-07T09:09:00Z"],["dc.date.available","2018-11-07T09:09:00Z"],["dc.date.issued","2012"],["dc.description.abstract","The emplacement of the Mesoproterozoic Gotemar Pluton into Paleoproterozoic granitoid host rocks of the Transscandinavian Igneous Belt is re-examined by microfabric analysis, including cathodoluminescence microscopy. Field data on the pluton-host rock system are used to strengthen the model. The Gotemar Pluton, situated on the Baltic Shield of SE Sweden, is a horizontally zoned tabular structure that was constructed by the intrusion of successive pulses of magma with different crystal/melt ratios, at an estimated crustal depth of 4-8 km. Initial pluton formation involved magma ascent along a vertical dike, which was arrested at a mechanical discontinuity within the granitoid host rocks; this led to the formation of an initial sill. Subsequent sill stacking and their constant inflation resulted in deformation and reheating of existing magma bodies, which also raised the pluton roof. This multi-stage emplacement scenario is indicated by complex dike relationships and the occurrence of several generations of quartz (Si-metasomatism). The sills were charged by different domains of a heterogeneous magma chamber with varying crystal/melt ratios. Ascent or emplacement of magma with a high crystal/melt ratio is indicated by syn-magmatic deformation of phenocrysts. Complex crystallization fabrics (e.g. oscillatory growth zoning caused by high crystal defect density, overgrowth and replacement features, resorbed and corroded crystal cores, rapakivi structure) are mostly related to processes within the main chamber, that is repeated magma mixing or water influx."],["dc.identifier.doi","10.1007/s00531-011-0739-y"],["dc.identifier.isi","000304857400004"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/8103"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/26164"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1437-3254"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Multi-stage emplacement of the Gotemar Pluton, SE Sweden: new evidence inferred from field observations and microfabric analysis, including cathodoluminescence microscopy"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]