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infrastructure. Although scientists have studied how rainfall and sediment supply affect debris flows, we still know little about how sediment availability changes across space and time, and how this controls how
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on the project “Impact of terrigenous mineral input on marine silicate alteration and element cycles”. Your job On geological time scales rock weathering controls Earth’s climate by providing a natural CO2
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processes and help collectives envision and develop the organisational and digital tools required for broader participation. You will be part of a cohort of 11 PhD candidates from multiple Dutch universities
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-develop practical approaches through workshops and working sessions. You will embed yourself in ongoing change processes and help collectives envision and develop the organisational and digital tools
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sea ice variability; processing satellite datasets to monitor sea ice and surface melt; investigating how turbulent and radiative heat fluxes from open water and polynyas drive snowfall and melt events
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extinction? The research will initially focus on improving age control by magnetostratigraphy and chemostratigraphy, after which the project can follow different routes, including but not limited
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on improving age control by magnetostratigraphy and chemostratigraphy, after which the project can follow different routes, including but not limited to sedimentology, orbital forcing and palynology, based
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knowledge is established, the processes of transport and burial during turbidity current events remain poorly understood. Previous experimental research into turbidity currents has been fundamental in
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interplay between physical particle deposition, chemical precipitation, and deformation-induced particle remobilisation remains poorly understood. These processes vary fundamentally across rock types – from
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them vulnerable to far-field human interference. While this general knowledge is established, the processes of transport and burial during turbidity current events remain poorly understood. Previous