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Mobilization of wildfire ash by wind and water erosion
Immediately after a wildfire, burnt landscapes are typically black due to the widespread deposition of an ash layer and, with time-since-fire, then loose again this blackness because of the disappearance of this ash layer and/or g ...
Supervisor: Jantiene Baartman
Department: Soil Physics and Land Management group |
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What affects the moisture regime of the sand surface of beach and dune?
In the past decade, sand nourishments (or sand supply) to Dutch fore-shores and beaches have been undertaken to provide an additional protection against the sea. One of the protective mechanisms is that sand transports over the be ...
Supervisor: Sjoerd vd Zee
Department: Soil Physics and Land Management group |
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Plastic biodegradation What if microorganismes could do the job?
Project description
Problemcontext
Plasticsandmicroplasticsarecurrentlyenvironmentalissuesinagriculturalsoils.Althoughsomeplasticsaresoldasbiodegradable,researchersarestillfindingmicroplasticsandplasticscontainingpolybutylenea ...
Supervisor: Davi Munhoz and Ke Meng
Department: Soil Physics and Land Management group |
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Litter and fire risk: new technologies
Leaf litter is the forgotten layer between soils and forestry, despite its strong importance for fire risk and fire impact. Yet standard methodologies to measure soil physical properties are not readily applicable to litter beca ...
Supervisor: Main supervisor: dr Cathelijne Stoof
Second supervisor: dr Martine van der Ploeg, ing. Harm Gooren
Department: Soil Physics and Land Management group |
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Detecting small areas burned through Sentinel data
Wildland fire occurrence and size is quantified around the world using satellite imagery, which allows rapid detection of area burned even in inaccessible and remote terrain. Yet the downside of current burned area products is tha ...
Supervisor: Supervisors: dr Cathelijne Stoof (SGL), dr. Harm Bartholomeus (GRS)/ ir. Onno Roosenschoon/ COBRA
Department: Soil Physics and Land Management group |
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Modeling drought and oxygen stress in clay soils
Potentially clay soils are very fertile. Nevertheless proper cultivation of clay soils is hard as they may change rapidly with respect to too wet and too dry conditions. Also proper simulation of drought- and oxygen stress in clay ...
Supervisor: Jos van Dam, Marius Heinen (WENR)
Department: Soil Physics and Land Management group |
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Assessing soil and water related risks with GIS in 5 watersheds in Burundi
Burundi is among the poorest countries in the world, with 58 per cent of its inhabitants living on less than a dollar per day. In order to improve food security, a project to boost communal fish farming is under development in 5 p ...
Supervisor: Aad Kessler
Department: Soil Physics and Land Management group |
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Pesticide effects in soil biota and soil functions
Pesticides are heavily used in agriculture to reduce crop losses due to pests, weeds and pathogens. Between 1961 and 2011 the global agricultural production more than tripled, largely due to pesticide use. Currently, global pestic ...
Supervisor: Violette Geissen, Esperanza Huerta Lwanga & Tamas Salanki
Department: Soil Physics and Land Management group |
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Litter and fire risk: field, lab and modeling
Leaf litter is the forgotten layer between soils and forestry, despite its strong importance for carbon storage, water fluxes, fire risk and fire impact. In this project you will work on one of the many unknowns regarding litter ...
Supervisor: Main supervisor: dr Cathelijne Stoof
Second supervisor: dr Martine van der Ploeg, dr Jetse Stoorvogel, dr Elmar Veenendaal, depending on the focus of your research
Department: Soil Physics and Land Management group |
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