Settling of porous particles through a pycnocline
ORAL
Abstract
Downward carbon flux in the Ocean is largely governed by particle settling. Most marine particles are highly porous and settle at low Reynolds numbers. We present results of an experimental investigation of porous spheres settling through a thin density interface at $O(0.1)
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Authors
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Kolja Kindler
MIT
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Arzhang Khalili
MPI for Marine Microbiology
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Roman Stocker
Massachusetts Institute of Technology, MIT