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, vegetation and atmospheric deposition, affecting nutrient, sediment and pollutant flux (e.g. Hg, POPs). However, because the Arctic remains so sparsely monitored, documenting such changes and their impact is
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properties (e.g. sediment resuspension, impact of nuclear power plant cooling water, changes in wind stress in wind farm areas, changes in seabed configuration) in the Baltic Sea; introduction and application
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between the turbine platform and the surrounding fluid environment. Special attention is given to the hydrodynamic effects on the platform supports and their interaction with seabed sediments, including
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modeling. For more details, please view https://www.ntu.edu.sg/cee. We are looking for a Postdoctoral Researcher to advance innovative research in multiscale clay science and geotechnical engineering. The
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modeling. For more details, please view https://www.ntu.edu.sg/cee . We are seeking a Research Fellow to contribute to cutting-edge research in multiscale clay science and geotechnical engineering. The
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sustainability. For more details, please view https://www.ntu.edu.sg/ase The Organo-Mineral Group (OMG) within the Asian School of the Environment (ASE) is seeking a Research Assistant. This position is part of a
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from the atomic and molecular to the largest scales, from ancient times to the present and into the future. Research in the Department encompasses minerals and rocks, soils and sediments, mountains and
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quantification of microplastics in stormwater and urban sediments. - Integrate the results into the development of a method for estimating microplastic loads discharged to rivers at the territorial scale
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dynamically with the seabed, where repeated dragging and settling cause the sediment to deform and form trenches. These evolving seabed features change the line’s mechanical response and can affect the long
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Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung | Bremerhaven, Bremen | Germany | about 2 months ago
response to anthropogenic climate change. Understanding its state during past warm periods is pivotal to aid our ability to project future changes. Arctic Ocean sediments provide such a window into the